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  • Books  (4,612)
  • English  (4,446)
  • Russian  (163)
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  • 2005-2009  (1,446)
  • 2000-2004  (931)
  • 1980-1984  (2,251)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Practising interdisciplinarity (2000)
    Toronto [u.a.] : Univ. of Toronto Press
    Details Availability
    Call number: IASS 18.91704
    Type of Medium: Monograph available for loan
    Pages: XVI, 294 S , graph. Darst , 24 cm
    ISBN: 0802043283 (cloth) , 0802081398 (paper) , 9780802081391 (paper)
    URL: Inhaltsverzeichnis
    Language: English
    Branch Library: RIFS Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    The model-based archaeology of socionatural systems (2007)
    Santa Fe, NM : School for Advanced Research Press
    Details Availability
    Call number: IASS 18.91705
    Type of Medium: Monograph available for loan
    Pages: XIII, 290 S., [8] Bl , Ill., graph. Darst., Kt , 26 cm
    Edition: 1. ed
    ISBN: 1930618875 (pa) , 9781930618879 (pa)
    Series Statement: A School Of Advanced Research Resident Scholar Book
    URL: http://www.gbv.de/dms/bowker/toc/9781930618879.pdf
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Martian gullies and their earth analogues (2006)
    London : The Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(467)
    In: Geological Society Special Publication
    Description / Table of Contents: Gullies on Mars resemble terrestrial gullies involved in the transport of abundant material down steep slopes by liquid water. However, liquid water should not be stable at the Martian surface. The articles in this volume present the two main opposing theories for Martian gully formation: climate-driven melting of surficial water-ice deposits and seasonal dry-ice sublimation. The evidence presented ranges from remote-sensing observations, to experimental simulations, to comparison with Earth analogues. The opposing hypotheses imply either that Mars has been unusually wet in the last few million years or that it has remained a cold dry desert – both with profound implications for understanding the water budget of Mars and its habitability. The debate questions the limits of remote-sensing data and how we interpret active processes on extra-terrestrial planetary surfaces, even beyond those on Mars, as summarized by the review paper at the beginning of the book.
    Type of Medium: Monograph available for loan
    Pages: vi, 434 Seiten , Illustrationen
    ISBN: 978-1-78620-360-1
    Series Statement: Geological Society Special Publication 467
    URL: https://sp.lyellcollection.org/content/467/1
    Language: English
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  • 4
    Monograph available for loan
    Monograph available for loan
    Friction : an ethnography of global connection (2005)
    Princeton [u.a.] : Princeton Univ. Press
    Details Availability
    Call number: IASS 18.91773
    Type of Medium: Monograph available for loan
    Pages: XIV, 321 S. , Ill
    ISBN: 0691120641 (alk. paper) , 9780691120645 (alk. paper) , 069112065X (pbk.) , 9780691120652 (pbk.)
    URL: http://www.loc.gov/catdir/description/prin051/2004043422.html
    URL: http://www.loc.gov/catdir/enhancements/fy0654/2004043422-d.html
    URL: http://www.loc.gov/catdir/enhancements/fy0654/2004043422-t.html
    URL: http://www.loc.gov/catdir/enhancements/fy0734/2004043422-b.html
    URL: https://external.dandelon.com/download/attachments/dandelon/ids/CH0018BD1CF2836C9E094C1257846002A2DD0.pdf
    Language: English
    Branch Library: RIFS Library
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  • 5
    Series available for loan
    Series available for loan
    The effectiveness and influences of the navigation ice booms on the St. Marys River (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-201-84/4
    In: CRREL Report, 84-4
    Description / Table of Contents: Ice problems developed in the Sault Ste. Marie, Michigan, portion of the St. Marys River because of winter navigation. Passing ships and natural influences moved ice from Soo Harbor into Little Rapids Cut in sufficient quantities to jam, cause high water in the harbor, and prevent further ship passage. After physical model and engineering studies, two ice booms with a total span of 1375 ft (419 m) with a 250-ft (76-m) navigation opening between were installed at the head of Little Rapids Cut in 1975. A modest field study program on the booms was conducted for the ensuring four winters to determine ice and boom interaction and the effects of ship passages on the system. Forces on some anchors were recorded and supplemental data were taken by local personnel. Several reports have been written about the booms' early operations. This paper presents four-year summary of the main effects of the booms on ice and ship interaction and vice versa. Throughout the four winter seasons, the small quantities of ice lost over and between the booms were manageable. Ships usually passed through the boom without influencing the boom force levels, but at time they brought about large changes. One boom needed strengthening, and artificial islands were added for upstream ice stability. Coast Guard icebreakers were also a necessary part of winter navigation in this area.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 84-4
    URL: https://apps.dtic.mil/docs/citations/ADA139908
    URL: https://hdl.handle.net/11681/9281
    Language: English
    Note: CONTENTS Abstract Preface Introduction St. Marys River Ice problems Remedial measures Field studies Highlights, trends, and major findings Modifications to boom Maximum forces Ship traffic Characteristics Effect of boom forces Effect on ice Conclusion Literature cited Appendix A: Ice boom forces
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  • 6
    Series available for loan
    Series available for loan
    Force distribution in a fragmented ice cover (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-201-84/7
    In: CRREL Report, 84-7
    Description / Table of Contents: Experiments were conducted in CRREL's refrigerated flume facility to examine the two-dimensional force distribution of a floating, fragmented ice cover restrained by a boom in a simulated river channel. To determine the force distribution, a vertically walled channel, instrumented for measuring normal and tangential forces, and an instrumented restraining boom were installed in a 40.0- by 1.3-m flume. Two sizes of polyethylene blocks and two similar sizes of fresh-water ice blocks were tested using water velocities ranging from 10 to 30 cm/s. The forces measured at the instrumented boom leveled off with increasing cover length. The contribution of the increasing shear forces developed along theshorelines to this leveling off in the data was clearly evident. The shear coefficients of the polyethylene blocks averaged 0.43, and the freshwater ice averaged 0.044. The normal force measured along the instrumented shoreline could not be related simply by a K coefficient to the longitudinal force; another expression was required, with a term being a function of the cover thickness and independent of the undercover shear stress or cover length. By adding this term, good agreement was then found between the measured and predicted values of the boom forces and the shoreline normal and shear forces
    Type of Medium: Series available for loan
    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 84-7
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a142100.pdf
    URL: https://hdl.handle.net/11681/9284
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experiments Test flume facility Experimental apparatus Experimental procedure Results Plastic versus freshwater ice Shoreline forces Boom forces Average shear stress under ice cover Internal forces Discussion Data scatter Summary and conclusions Literature cited Appendix A: Experimental results
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  • 7
    Monograph available for loan
    Monograph available for loan
    Geosimulation : automata-based modeling of urban phenomena (2005)
    Chichester : Wiley
    Details Availability
    Call number: PIK T 060-18-91853
    Type of Medium: Monograph available for loan
    Pages: XXIII, 287 Seiten , Illustrationen, Diagramme, Karten
    Edition: Reprinted
    ISBN: 0470843497 , 9780470843499
    URL: http://www.loc.gov/catdir/toc/wiley041/2004004938.html
    Language: English
    Note: Contents: 1. Introduction to urban Geosimulation ; 2. Formalizing Geosimulation with Geographic Automata Systems (GAS) ; 3. System Theory, Geography, and Urban Modelling ; 4. Modelling urban land usage with cellular automata ; 5. Modelling Urban Dynamics with Multi-Agent Systems ; 6. Finale: Epistemology of Geosimulation
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  • 8
    Series available for loan
    Series available for loan
    Ice forces on rigid, vertical, cylindrical structures (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-201-84/33
    In: CRREL Report, 84-33
    Description / Table of Contents: A small-scale experimental study was conducted to characterize the magnitude and nature of ice forces during continuous crushing of ice against a rigid, vertical, cylindrical structure. The diameter of the structure was varied from 50 to 500 mm, the relative velocity from 10 to 210 mm/s, and the ice thickness from 50 to 80 mm. The ice tended to fail repetitively, with the frequency of failure termed the characteristic frequency. The characteristic frequency varied linearly with velocity and to a small extent with structure diameter. The size of the damage zone was 10 to 50% of the ice thickness, with an average value of 30%. The maximum and mean normalized ice forces were strongly dependent on the aspect ratio (structure diameter/ice thickness). The forces increased significantly with decreasing aspect ratio, but were constant for large aspect ratios. The maximum normalized forces appeared to be independent of strain rate. The effect of velocity on the normalized ice forces depended on structure diameter. The mean effective pressure or specific energy of ice crushing depended on both aspect ratio and ice-structure relative velocity. The energy required to crush the ice for the one failure cycle was obtained from the ice force records for each test, and was compared to the energy calculated from an idealized sawtooth shape for the force record, the maximum force, velocity and characteristic frequency data. Originator - supplied keywords included: Cold regions, Cold regions construction, Cylindrical test structures, Ice, Ice crushing, Ice forces, and Test facilities.
    Type of Medium: Series available for loan
    Pages: vi, 47 Seiten , Illustrationen
    Series Statement: CRREL Report 84-33
    URL: https://hdl.handle.net/11681/9351
    Language: English
    Note: Contents Abstract Preface Nomenclature Introduction Test objectives Experimental setup and procedures Facilities Test fixture Data acquisiton system Ice sheets Measurement of ice properties Daily test summary Experimental results and discussion Observations Ice force records Frequency of ice force variations Discussion Maximum crushing forces Mean effective pressure or specific energy of ice in crushing Failure energy of ice Ratio of maximum force to mean force Summary and conclusions Literature cited Appendix A: Data for continuous crushing tests
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  • 9
    Monograph available for loan
    Monograph available for loan
    Workshop on Arctic glaciology and the magics annual meeting : Abstracts ; Zakopane, Poland 22-26 February 2003 (2003)
    Details Availability
    Call number: AWI G7-18-91974
    Type of Medium: Monograph available for loan
    Pages: 38 Seiten , 1 Beilage
    Language: English
    Note: Contents: Preface. - Abstracts (in the alphabetic order). - The natural environment and cryosphere of the Tatra Mountains by Bogdan Gądek. - IASC Working Group on Arctic Glaciology. - General programme.
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  • 10
    Monograph available for loan
    Monograph available for loan
    Case studies and theory development in the social sciences (2005)
    Cambridge, Massachusetts : The MIT Press
    Details Availability
    Call number: IASS 19.91995
    Description / Table of Contents: Winner of the 2006 Giovanni Sartori Book Award, given by the American Political Science Association's Qualitative Methods Section. The use of case studies to build and test theories in political science and the other social sciences has increased in recent years. Many scholars have argued that the social sciences rely too heavily on quantitative research and formal models and thus have attempted to develop and refine rigorous methods for using case studies. This text presents a comprehensive analysis of research methods using case studies and examines the place of case studies in social science methodology. It argues that case studies, statistical methods, and formal models are complementary rather than competitive. The book explains how to design case study research that will produce results useful to policymakers and it emphasizes the importance of developing policy-relevant theories. It offers three major contributions to case study methodology: an emphasis on the importance of within-case analysis, a detailed discussion of process tracing, and development of the concept of typological theories. Case Studies and Theory Development in the Social Sciences will be particularly useful to graduate students and scholars in social science methodology and the philosophy of science, as well as to those designing new research projects, and will contribute greatly to the broader debate about scientific methods.
    Type of Medium: Monograph available for loan
    Pages: xv, 331 Seiten , 24cm
    ISBN: 0262072572 , 9780262072571 , 0262572222 , 9780262572224
    Series Statement: BCSIA studies in international security
    URL: http://ecx.images-amazon.com/images/I/31F9RZ2B9XL._SL500_AA300_.jpg
    URL: Inhaltsverzeichnis
    Language: English
    Branch Library: RIFS Library
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  • 11
    Series available for loan
    Series available for loan
    National Antarctic Research Report to SCAR : I. Record of activities (past and ongoing) April 1983-October 1984 ; II. Planned activities October 1984-October 1985 (1984)
    Bremerhaven : Federal Republic of Germany, National Commitee on Antarctic Research
    Associated volumes
    Details Availability
    Call number: ZSP-SCAR-570-6
    In: Antarctic Research Report to SCAR, No. 6
    Type of Medium: Series available for loan
    Pages: 38 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 6
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 83-October 84. - II. Planned Activities, October 84-October 85. - References.
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  • 12
    Series available for loan
    Series available for loan
    National Antarctic Research Report to SCAR : I. Record of activities (past and ongoing) April 1980-October 1981 ; II. Planned activities October 1981-October 1982 (1981)
    Bremerhaven : Federal Republic of Germany, National Commitee on Antarctic Research
    Associated volumes
    Details Availability
    Call number: ZSP-SCAR-570-3
    In: National Antarctic Research Report to SCAR, No. 3
    Type of Medium: Series available for loan
    Pages: 16 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 3
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 80-October 81. - II. Planned Activities, October 81-October 82. - References.
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  • 13
    Monograph available for loan
    Monograph available for loan
    Proceedings of the human role in reindeer/caribou systems workshop : Rovaniemi, Finland, 10-14 February 1999 (2000)
    Oslo : Norsk Polarinstitutt
    Associated volumes
    Details Availability
    Call number: AWI P1-19-92149
    In: Polar Research
    Type of Medium: Monograph available for loan
    Pages: 142 Seiten , Illustrationen
    ISSN: 0800-0395
    Series Statement: Polar Research 19,1
    Language: English
    Note: Contents: Preface / Helle V. Goldman, Bruce Forbes & Gary Kofinas. - Research planning in the face of change: the human role in reindeer/caribou systems / Gary Kofinas, Gail Osherenko, David Klein & Bruce Forbes. - Reindeer husbandry/hunting in Russia in the past, present and future / Leonid M. Baskin. - Chukotkan reindeer husbandry in the post-socialist transition / Patty A. Gray. - Nenets reindeer herders on the lower Yenisei River: traditional economy under current conditions are responses to economic change / Konstantin B. Klokov. - Reindeer pastoralism in modern Siberia: research and survival during the time of crash / Igor Krupnik. - Managing reindeer and wildlife on Alaska's Seward Peninsula / Jim Dau. - Response of reindeer and caribou to human activities / Scott A. Wolfe, Brad Griffith & Carrie A. Gray Wolfe. - High voltage transmission lines and their effect on reindeer: a research programme in progress / Eigil Reimers, Kjetil Flydal & Rune Stenseth. - Responses of West Greenland caribou to the approach of humans on foot / Peter Aastrup. - Arctic grazing systems and industrial development: can we minimize conflicts? / David R. Klein. - Regional effects of climate change on reindeer: a case study of the Muotkatunturi region in Finnish Lapland / Susan E. Lee, Malcolm C. Press, John A. Lee, Tim Ingold & Terhi Kurttila. - Reindeer in tundra ecosystems: the challenges of understanding system complexity / Feodor V. Kryazhimskii & Alexey N. Danilov. - Status, directions and priorities of reindeer husbandry research in Sweden / Öje Danell. - Need and opportunity for a North American caribou knowledge cooperative / Don Russell, Gary Kofinas & Brad Griffith. - Native reindeer herders' priorities for research / Johan Mathis Turi. - Letter from Varandei / Andrei V. Golovnev.
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  • 14
    Series available for loan
    Series available for loan
    HIRLAM newsletter; No. 41 (2002)
    Norrköping : HIRLAM-5 Projekt, SMHI
    Associated volumes
    Details Availability
    Call number: AWI A13-19-92153
    In: HIRLAM newsletter, No. 41
    Type of Medium: Series available for loan
    Pages: 174 Seiten , Illustrationen
    Series Statement: HIRLAM newsletter 41
    URL: http://hirlam.org/index.php/component/docman/cat_view/77-hirlam-official-publications/78-hirlam-newsletters/173-hirlam-newsletter-no-41?Itemid=70
    Language: English
    Note: CONTENTS: Introduction - All Staff meeting 2002 / Per Undén. - Report of Hirlam Management Group visit to Met Éireann / Per Undén. - The operational HIRLAM at the Finnish Meteorological Institute / Kalle Eerola. - Recent changes in the operational suites at Météo-France / Dominique Giard. - HIRLAM operational activities in Met Éireann / Ray McGrath. - Operational HIRLAM at met.no / Ole Vignes. - SMHI operational HIRLAM systems / Lars Meuller. - Revision of the ECMWF humidity analysis 1: Construction of a gaussian control variable / Elías Valur Hólm. - A nudging procedure to assimilate analyses of cloud and precipitation in a version of HIRLAM / Bent Hansen Sass and Claus Petersen. - HIRLAM 4DVAR / Xiang-Yu Huang, Xiaohua Yang, Nils Gustafsson, Kristian Mogensen and Magnus Lindskog. - Progress in the investigation of problems in the operational 4d-var assimilation at Météo-France / Dominique Giard. - Recent and future developments in the turbulence modeling in HIRLAM / Geert Lenderink. - Parametrization of the effects of subgrid-scale orography / Laura Rontu and Kai Sattler. - ISBA tests in a Nordic area - an update / Simo Järvenoja. - Results of the SAT-MAP-CLIMATE project / Niels Woetmann Nielsen, Charlotte Hasager, Henrik Søgaard, Jens H Chrisensen, Niels Otto Jensen and Eva Bøgh. - Progress and problems in the Functional Boxes / Erik Bazile. - Status Kain Fritsch Rash Kristjansson and Hirlam 22 km experiences / Sander Tijm, Roy Wichink, Oscar van de Velde, Ben Wichers Schreur and Toon Moene. - The representation of shallow cumulus convection and associated cloud fields in the Rossby Centre Atmospheric modell / Colin Jones and Enrique Sanchez. - Parametrization of mountain-related effects in fine-scale HIRLAM - items for discussion / Laura Rontu. - Testing alternative lateral boundary strategies: A progress report / Aidan McDonald. - Current situation with the NH HIRLAM / Aarne Mannik and Rein Room. - Manipulations to determine the hybrid coordinate in HIRLAM / Per Undén and Nils Gustafsson. - Comparison of convection and condensation schemes under non-hydrostatic Hirlam model: A case study / Sami Niemela and Carl Fortelius. - Real time solution of forward and inverse air pollution problems with a numerical dispersion model based on short-term weather forecasts / Mikhail Sofiev. - Asyncronous I/O in HIRLAM / Ole Vignes. - HIRLAM coding styles / Gerard Cats. - NWP on a GRID compute environment / Gerard Cats. - HIRLAM verification scores, 1st quarter 2002 / Per Undén. - Validation test for HIRLAM 5.1.4: winter condition / Xiaohua Yang. - Recent tests of proposed revisions to the STRACO cloud scheme / Bent Hansen Sass and Xiaohua Yang.
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  • 15
    Series available for loan
    Series available for loan
    National Antarctic Research Report to SCAR : I. Record of Activities (past and ongoing) April 1981-October 1982 ; II. Planned activities October 1982-October 1983 (1982)
    Bremerhaven : Federal Republic of Germany, National Commitee on Antarctic Research
    Associated volumes
    Details Availability
    Call number: ZSP-SCAR-570-4
    In: National Antarctic Research Report to SCAR, No. 4
    Type of Medium: Series available for loan
    Pages: 24 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 4
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 81-October 82. - II. Planned Activities, October 82-October 83. - References.
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  • 16
    Monograph available for loan
    Monograph available for loan
    An integrated study of the structure and thermomechanical properties of the European lithosphere (2009)
    Details Availability
    Call number: M 19.92455
    Type of Medium: Monograph available for loan
    Pages: 178 Seiten , Illustrationen
    ISBN: 9789090240619
    Language: English
    Location: Upper compact magazine
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  • 17
    Monograph available for loan
    Monograph available for loan
    Global glacier changes : facts and figures (2008)
    Zürich : World Glacier Monitoring Service
    Details Availability
    Call number: AWI G7-19-92411
    Type of Medium: Monograph available for loan
    Pages: 88 Seiten , Illustrationen
    ISBN: 9789280728989
    URL: http://www.grid.unep.ch/glaciers/pdfs/glaciers.pdf
    Language: English
    Note: Contents Foreword by UNEP Foreword by WGMS Summary 1 Introduction 2 Glaciers and climate 3 Global distribution of glaciers and ice caps 4 Glacier fluctuation series 5 Global glacier changes 6 Regional glacier changes 6.1 New Guinea 6.2 Africa 6.3 New Zealand 6.4 Scandinavia 6.5 Central Europe 6.6 South America 6.7 Northern Asia 6.8 Antarctica 6.9 Central Asia 6.10 North America 6.11 Arctic Islands 7 Conclusions References Appendix 1 - National Correspondents of the WGMS Appendix 2 - Meta-data on available fluctuation data
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  • 18
    Non-book medium
    Non-book medium
    Standard Practice for Use of Distributed Optical Fiber Sensing Systems for Monitoring the Impact of Ground Movements During Tunnel and Utility Construction on Existing Underground Utilities1 (2004)
    West Conshohocken, PA : ASTM International
    Details
    Type of Medium: Non-book medium
    Pages: Online-Ressource
    URL: http://bib.gfz-potsdam.de/intern/pubint/2275712.pdf
    Language: English
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  • 19
    Series available for loan
    Series available for loan
    Radar detection of ice wedges in Alaska (1982)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-201-82/43
    In: CRREL Report, 82-43
    Description / Table of Contents: The radar signatures of ice wedges and wedge-like structures have been investigated for a variety of soil conditions. The radar used for this study emitted short sinusoidal pulses of about 10-ns duration with an approximate center frequency of 150 MHz. Most of the ice wedges existed at depths of about 1 m in a variety of silty and sandy soils with both frozen and thawed active layers. The position of the wedges was usually identified from corresponding surface features. An artificial ice wedge in coarse-grained alluvium was also profiled as well as wedge-like structures of fine silt in a coarse-grained glacial outwash. All wedges and wedge-like structures produced a hyperbolic reflection profile except when an active layer of thawed, saturated silt was present which eliminated returns from the wedges. The peaks of the hyper-bolas were sometimes masked by reflections from the permafrost table or other material interfaces, and multiple hyperbolas occurred at some sites. The dielectric constant of the host medium was often calculated from the linear portions of the hyperbolas and the results were verified by laboratory time domain reflectometry measurements per-formed on field samples. In some cases, hyperbolic profiles originated at several meters depth suggesting that deep ice wedges could be detected in areas of cold permafrost.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 82-43
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a124571.pdf
    URL: https://hdl.handle.net/11681/9324
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Objectives and procedures Equipment used Radar TDR Definitions Massive ice Results Artificial wedge: Norwich, Vermont Ice wedges in sand: Fish Creek, Alaska Ice wedges: Prudhoe Bay, Alaska Ice wedges under thawed fine-grained soils: North Slope, Alaska Wedge-like soil structures: Ft. Greely, Alaska TDR measurements Summary and concluding remarks Literature cited Appendix A: Brief discussion of dispersion
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  • 20
    Series available for loan
    Series available for loan
    Radar profiling of buried reflectors and the groundwater table (1983)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-201-83/11
    In: CRREL Report, 83-11
    Description / Table of Contents: Investigations of ground radar performance over thawed and seasonally frozen silts, and sands and gravels containing artificial and natural reflectors were carried out in Alaska. The radar emitted 5-10 ns pulses, the center frequency of which was approximately 150 MHz. The artificial reflectors were metal sheets and discs and the natural reflectors were the groundwater table and interfaces between frozen and thawed material. The water table was profiled at three sites where the subsurface material was coarse-grained alluvium. Dielectric constants of 16 to 18 were measured for the thawed silts, 6 to 7 for the frozen silts and 3 to 9 for the sands and gravels. Signal penetration in the thawed high moisture content silts may be achieved only by use of a lower frequency radar, whereas in the sands and gravels greater depths may be detected with more sophisticated signal processing.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: CRREL Report 83-11
    URL: https://apps.dtic.mil/docs/citations/ADA130225
    URL: https://hdl.handle.net/11681/9337
    Language: English
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  • 21
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    A comparison of sea ice model results using three different wind forcing fields (1983)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-201-83/17
    In: CRREL Report, 83-17
    Description / Table of Contents: A sea ice model was applied to the East Greenland Sea to examine a 60-day ice advance period beginning 1 October 1979. This investigation compares model results using driving geostrophic wind fields derived from three sources. Winds calculated from sea-level pressures obtained from the National Weather Service's operational analysis system resulted in strong velocities concentrated in a narrow band adjacent to the Greenland coast, with moderate velocities elsewhere. The model showed excessive ice transport and thickness build-ups in the coastal region. The extreme pressure gradient parallel to the coast resulted partially from a pressure reduction procedure that was applied to the terrain-following sigma coordinate system to obtain sea-level pressures. Additional sea-level pressure fields were obtained from an independent optimal interpolation analysis that merged FGGE buoys drifting in the Arctic basin with high latitude land stations and from manual digitization of the NWS hand-analyzed Northern Hemisphere Surface Charts. Modeling results using winds from both of these fields agreed favorably.
    Type of Medium: Series available for loan
    Pages: 19 Seiten , Illustrationen
    Series Statement: CRREL Report 83-17
    URL: https://apps.dtic.mil/docs/citations/ADA134462
    URL: https://hdl.handle.net/11681/9339
    Language: English
    Note: CONTENTS Abstract Preface Introduction Description of study Model results The problem Conclusions Literature cited
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  • 22
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    Sensitivity of plant communities and soil flora to seawater spills, Prudhoe Bay, Alaska (1983)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-201-83/24
    In: CRREL Report, 83-24
    Description / Table of Contents: Secondary recovery of oil at Prudhoe Bay, Alaska, will involve transporting large quantities of seawater in elevated pipelines across tundra for injection into oil-bearing rock strata. The possibility of a pipeline rupture raises questions concerning the effects of seawater on tundra vegetation and soils. To evaluate the relative sensitivities of different plant communities to seawater, eight sites representing the range of vegetation types along the pipeline route were treated with single, saturating applications of seawater during the summer of 1980. Within a month of the treatment 30 of 37 taxa of shrubs and forbs in the experimental plots developed clear symptoms of stress, while none of the 14 graminoid taxa showed apparent adverse affects. Live vascular plant cover was thus reduced by 89 and 91% in the two dry sites and by 54, 74 and 83% in the three moist sites, respectively. Live(green) bryophyte cover was markedly reduced in the moist experimental sites in 1981. Bryophytes in all but one of the wet-site experimental plots were apparently unaffected by the seawater treatment. Two species of foliose lichens treated with seawater showed marked deterioration in 1981. All other lichen taxa were apparently unaffected by the seawater treatment. The absorption and retention of salts by the soil is inversely related to the soil moisture regime. In the wet sites, conductivities approached prespill levels within about 30 days. In such sites, spills at the experimental volumes are quickly diluted and the salts flushed from the soil. In the dry sites, on the other hand, salts are retained in the soil, apparently concentrating at or near the seasonal thaw line.
    Type of Medium: Series available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: CRREL Report 83-24
    URL: https://apps.dtic.mil/docs/citations/ADA136619
    URL: https://hdl.handle.net/11681/9299
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods Site selection and preparation Prespill assessment Seawater application Postspill assessment Enzyme assay and analysis of soil flora Results and discussion Soil-solution conductivities Vascular plant response Cryptogam response Site factors and plant response Soil flora and extracellular soil enzymes Limitations of this study Summary and conclusions Literature cited Appendix: Plant taxa included in this study
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  • 23
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    Calibration of sediment traps and particulate organic carbon export using 234Th in the Barents Sea (2002)
    Elsevier BV
    Associated volumes
    Details
    In: Marine Chemistry, 3664
    Description / Table of Contents: Profiles of particulate and dissolved 234Th (t1/2=24.1 days) in seawater and particulate 234Th collected in drifting traps were analyzed in the Barents Sea at five stations during the ALV3 cruise (from June 28 to July 12, 1999) along a transect from 78°15′N–34°09′E to 73°49′N–31°43′E. 234Th/238U disequilibrium was observed at all locations. 234Th data measured in suspended and trapped particles were used to calibrate the catchment efficiency of the sediment traps. Model-derived 234Th fluxes were similar to 234Th fluxes measured in sediment traps based on a steady-state 234Th model. This suggests that the sediment traps were not subject to large trapping efficiency problems (collection efficiency ranges from 70% to 100% for four traps). The export flux of particulate organic carbon (POC) can be calculated from the model-derived export flux of 234Th and the POC/234Th ratio. POC/234Th ratios measured in suspended and trapped particles were very different (52.0±9.9 and 5.3±2.2 μmol dpm−1, respectively). The agreement between calculated and measured POC fluxes when the POC/234Th ratio of trapped particles was used confirms that the POC/234Th ratio in trap particles is representative of sinking particles. Large discrepancies were observed between calculated and measured POC fluxes when the POC/234Th ratio of suspended particles was used. In the Barents Sea, vertical POC fluxes are higher than POC fluxes estimated in the central Arctic Ocean and the Beaufort Sea and lower than those calculated in the Northeast Water Polynya and the Chukchi Sea. We suggest that the latter fluxes may have been strongly overestimated, because they were based on high POC/234Th ratios measured on suspended particles. It seems that POC fluxes cannot be reliably derived from thorium budgets without measuring the POC/234Th ratio of sediment trap material or of large filtered particles.
    Type of Medium: 13
    ISSN: 0304-4203 , 1872-7581
    URL: https://doi.org/10.1016/S0304-4203(02)00071-3
    URL: https://cat.telegrafenberg.de/cgi-bin/koha/opac-image.pl?thumbnail=1&imagenumber=850
    Language: English
    Note: Outline Abstract Keywords 1. Introduction 2. Methods 2.1. Sample collection 2.2. 234Th analyses 2.3. Particulate organic carbon analyses 3. Results 3.1. Hydrography 3.2. Nutrients 3.3. 234Th activities and POC concentrations 3.4. Trapped material 4. Discussion 4.1. Origins of 234Th/238U disequilibrium 4.2. Determining 234Th fluxes 4.3. Calibration of sediment trap with 234Th 4.4. Vertical flux of particulate organic carbon and the POC/234Thp ratio 5. Conclusion Acknowledgements References
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  • 24
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    Rukovodstvo po ispol'zovaniju sputnikovych dannych v analize i prognoze pogody (1982)
    Leningrad : Gidrometeoizdat
    Details Availability
    Call number: MOP 45570 / Mitte ; MOP 47512 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 298 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 25
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    Erosion of perennially frozen streambanks (1983)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-201-83/29
    In: CRREL Report, 83-29
    Description / Table of Contents: A literature review indicated that the effects or permafrost on streambank erodibility and stability are not yet understood because systematic and quantitative measurements are seriously lacking. Consequently, general controversy exists as to whether perennially frozen ground inhibits lateral erosion and bankline recession, or whether it increases bank recession rates. Perennially frozen streambanks erode because of modification of the bank's thermal regime by exposure to air and water, and because of various erosional processes. Factors that determine rates and locations of erosion include physical, thermal and structural properties of bank sediments, stream hydraulics and climate. Thermal and physical modification of streambanks may also induce accelerated erosion within permafrost terrain removed from the immediate river environment. Bankline or bluffline recession rates are highly variable, ranging from less than 1 m/year to over 30 m/year and, exceptionally, to over 60 m/year. Long-term observations of the physical and thermal erosion processes and systematic ground surveys and measurements of bankline-bluffline recession rates are needed.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 83-29
    URL: https://apps.dtic.mil/docs/citations/ADA138410
    URL: https://hdl.handle.net/11681/9290
    Language: English
    Note: CONTENTS Abstract Preface Introduction Stream bank erosional processes Permafrost and related factors Permafrost and erosion General Erosional processes Bank zone processes Bluff zone processes Factors affecting perm afrost erodibility Exposure to currents and wind waves Texture and stratigraphy Ice content, distribution and type Slope aspect Coriolis force Timing and depth of thaw Water level and temperature Vegetation Ice and snow cover Groundwater Rates and timing of erosion and recession Overall effects of permafrost Recommendations for research Literature cited Appendix A : Processes of stream bank modifications
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  • 26
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    Shoreline erosion processes : Orwell Lake, Minnesota (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-84/32
    In: CRREL Report, 84-32
    Description / Table of Contents: Orwell Lake, in west-central Minnesota, is a flood-control, water-management reservoir first impounded in 1953. Subsequent erosion of the shoreline and a lack of knowledge of slope erosion processes in this region prompted this study to identify and quantify the processes there. The processes were measured at selected sites between June 1980 and June 1983. Erosion of the banks is primarily caused by three processes: rain, frost thaw, and waves. The first two processes tend to move sediment to the base of the steep slopes, forming 4 relatively gentle surface of accumulation. Wave action then tends to move this sediment into the lake. Analysis of the data collected over three years has confirmed that wave action is the dominant erosion process, providing almost 77% of the erosion during the 1981-82 study year. During the 1981 high pool level, 2,089 Mg of sediment, mostly colluvium, was removed from the lower slopes by wave action striking the 1.62 km of eroding shoreline. More than 4,300 Mg was eroded by waves accompanying the higher pool levels of 1982., During years in which the pool level does not exceed 325.5 m in elevation, the colluvium slope builds up at the expense of the steeper slope. But during successive years with higher pool levels, the resulting thin colluvium is quickly eroded. Erosion of the primary sediment, a compact till, then occurs, forming the S typical nearly vertical banks. In winter the upland surface adjacent to the lake freezes to a depth of between 1 and 2 m, depending on the surface temperature, the mow cover, and the distance from exposed banks. In late winter soil aggregates, released by the sublimation of interstitial ice within the banks, begin to accumulate at the base of the slopes, often veneering snowbanks there. Once thaw begins, slab failure of bank sediment is followed by mudflows and earthflows. Thaw failure at Orwell Lake in the winter of 1981-82 accounted for over 20% of the erosion; in the spring of 1982, 824 Mg was eroded by this process and 746 Mg the following spring. Such slope failure is most intense along north-facing banks and considerably less intense on south-facing banks, where more effective desiccation and sublimation reduce the soil moisture content. Summer rainfall is responsible for the remaining 3% of the total erosion, amounting to 102 Mg in 1981 and 208 Mg in 1982. Because the banks are steep and relatively short, rainwash is infrequent; rainsplash is the most consistent process during the summer, but the infrequent storms during which rainwash occurscause greater total erosion. Erosion by rain has increased in each of the past three summers, largely because of increased precipitation. Infrequent massive slope failures (slumps) have occurred at the east end of the lake where a buried clay rich unit is stratigraphically and topographically positioned to favor such failures. Drought years followed by heavy spring rains probably will result in additional slope failures of this type at the east end. Unless changes are made, the banks at Orwell Lake will continue to recede. Restriction of the pool level to less than 325.5-m elevation is the least expensive solution to the problem.
    Type of Medium: Series available for loan
    Pages: ix, 110 Seiten , Illustrationen
    Series Statement: CRREL Report 84-32
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a152952.pdf
    URL: https://hdl.handle.net/11681/9266
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Location Purpose of study Previous work Chapter 2. Methodology Geology Overland erosion Wave erosion Frost penetration and heave Thaw failure Bank recession Ground water Soil moisture Chapter 3. Results Geology Geotechnical properties Overland erosion Wave erosion Freeze-thaw phenomena Ground water fluctuations Other slope failures Chapter 4. Discussion Overland erosion Wave erosion Thaw failure Universal soil loss equation Chapter 5. Summary and conclusions Techniques Erosion processes at Orwell lake Bank recession Literature cited Appendix A1: Average cumulative change of surface at erosion stations #2-12, 1980-81 Appendix A2: Cumulative net changes at overland erosion stations #1-12, 1980-81 Appendix A3: Cumulative net changes at overland erosion stations #1 -12, 198 1-82 Appendix A4: Cumulative average erosion at overland erosion stations #1-12, 1980-81 Appendix AS: Cumulative average erosion at overland erosion stations #1-12, 1981-82 Appendix A6: Cumulative average erosion at overland erosion stations #1 -1 2A, 1982 Appendix B: Dimensions of erosion sections, Orwell Lake, Minnesota Appendix C: Piezometer installation data, Orwell Lake, Minneso
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  • 27
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    A collection of extended abstracts presented at The Symposium on the Radiation Transfer in the Oceans and Remote Sensing of Ocean Properties : IAMAP Third Scientific Assembly 17-28 August 1981, Hamburg, Federal Republic of Germany (1981)
    Boulder, Colorado : International Association of Meteorology and Atmospheric Physics (IAMAP), Radiation Commission
    Details Availability
    Call number: MOP 46646 / Mitte
    Type of Medium: Monograph available for loan
    Pages: IX, 221 Seiten
    Language: English
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  • 28
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    A collection of extended abstracts presented at The Symposium on the Solar Constant and the Spectral Distribution of Solar Irradiance : IAMAP Third Scientific Assembly 17-28 August 1981, Hamburg, Federal Republic of Germany (1982)
    Boulder, Colorado : International Association of Meteorology and Atmospheric Physics (IAMAP), Radiation Commission
    Details Availability
    Call number: MOP 46647 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VIII, 162 Seiten
    Language: English
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  • 29
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    Standartnye makety tablic agrometeorologičeskogo ežegodni : (Priloženie 2 k "Metodičeskomu posobiju po podgotovke k zaneseniju na technositeli dannych agrometeorologičeskich ežegodnikov") (1981)
    Moskva : Moskovskoe Otdelenie Gidrometeoizdata
    Details Availability
    Call number: MOP 45174 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 55 Seiten , 20х28 см
    Language: Russian
    Note: In kyrillischer Schrift
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  • 30
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    Fifth symposium on turbulence, diffusion, and air pollution of the American Meteorological Society : March 9-13, 1981, Atlanta, Ga. (1980)
    Boston, Massachusetts : American Meteorological Society
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    Call number: MOP 46673 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XIV, 276 Seiten
    Language: English
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  • 31
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    Subsea permafrost in Harrison Bay, Alaska : an interpretation from seismic data (1982)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-201-82/24
    In: CRREL Report, 82-24
    Description / Table of Contents: Velocity data derived from petroleum industry seismic records from Harrison Bay show that high-velocity material ( or = 2 km/s) interpreted to be ice-bonded permafrost is common. In the eastern part of the bay, the depth to high velocity material increases and velocity decreases in an orderly manner with increasing distance from shore until the layer is no longer apparent. The western part of the bay is less orderly, possibly reflecting a different geological and thermal history. This western part may be an inundated section of the low coastal plain characterized by the region north of Teshekpuk Lake, and could have contained deep thaw lakes, creating low velocity zones. Along some seismic lines, the high-velocity material extends approximately 25 km offshore. Two anomalies have been found which could be associated with rapidly degrading permafrost. One is strong attenuation, which was interpreted as an indication of gas in the shallow deposits. The other is the presence of considerable seismic noise, including identifiable small seismic events. The origin of this noise has not been positively established, and it is proposed that it may indicate that some movement is occurring in the sediments due to thaw.
    Type of Medium: Series available for loan
    Pages: 65 Seiten , Illustrationen
    Series Statement: CRREL Report 82-24
    URL: https://apps.dtic.mil/docs/citations/ADA121020
    URL: https://hdl.handle.net/11681/9361
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods Reading records Refractions Reflections Rayleigh waves Spatial resolution Anomalies Results and discussion Seismic velocity distribution Attenuation Low-level natural seismicity Summary Literature cited Appendix A: Error estimates Appendix B: Velocity profiles Appendix C: Seismic cross sections
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  • 32
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    Hydrology and climatology of the Caribou-Poker Creeks research Watershed, Alaska (1982)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-82/26
    In: CRREL Report, 82-26
    Description / Table of Contents: The Caribou-Poker Creeks Research Watershed is a small (101.5-sq km) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations within the watershed range from 210 to 826 m, and approximately 28% of its area is underlain by permafrost. Climatic differences between the watershed and Fairbanks are primarily due to the higher elevation of the watershed. Generally the watershed climatic sites are warmer in winter and cooler in summer than Fairbanks. Within the watershed the greatest temperature contrasts exist in winter, when the valley-bottom sites are beneath the regional air temperature inversion, and the higher sites are above it. From May through September the total precipitation averages 270 mm, 1.47 times that received at Fairbanks. The annual precipitation is about 1.7 times that of Fairbanks. The historical precipitation record at Fairbanks indicates that summer precipitation was below the long-term normal in eight of the eleven years of watershed measurements (1969-1980); no climatic extremes occurred during this period. An analysis of annual streamflow data showed an inconsistency of baseflow recessions from year to year. The runoff-rainfall ratio for individual summer storms averaged 0.35 for Caribou Creek. Comparisons of spot discharge measurements of predominantly permafrost and non-permafrost subwatersheds showed that permafrost-dominated watersheds have a much flashier response to precipitation than non-permafrost watersheds. A comparison of the annual flow distribution of the watershed indicated that Caribou Creek has lower summer and higher winter discharges per unit area than the Chena or Salcha Rivers.
    Type of Medium: Series available for loan
    Pages: 42 Seiten , Illustrationen
    Series Statement: CRREL Report 82-26
    URL: https://apps.dtic.mil/docs/citations/ADA122402
    URL: https://hdl.handle.net/11681/9369
    Language: English
    Note: CONTENTS Abstract Preface Introduction Setting Geology and soils Vegetation Climate Air temperature Precipitation Hydrology Annual and monthly runoff Individual storms Baseflow recessions Spatial flow variability Temporal flow variability Summary and conclusions Literature cited Appendix A: Station histories
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  • 33
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    Scala Macrosismica Europea 1998 : EMS-98 (2009)
    Luxembourg : European Seismological Commission
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    Call number: 8/M 19.92771 ; S 02.0465(32)
    In: Cahiers du Centre Européen de Géodynamique et de Séismologie
    Type of Medium: Series available for loan
    Pages: 97 Seiten , Illustrationen
    ISBN: 9789995904630
    Series Statement: Cahiers du Centre Européen de Géodynamique et de Séismologie 32
    Uniform Title: European Macroseismic Scale 1998
    Classification:
    Seismology
    Language: Spanish
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  • 34
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    Ice growth on Post Pond, 1973-1982 (1983)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-83/4
    In: CRREL Report, 83-4
    Description / Table of Contents: Measurements and analysis of seasonal ice growth and decay on Post Pond, New Hampshire, for the period 1973-1982 are presented. Observations included ice thickness measurements, examination of the various ice types contributing to the ice cover, and measurements of meteorological parameters for correlation with and modeling of the ice growth process. The overall nature of ice growth and decay (ice loss) on the Post Pond has been ascertained, the seasonal variability in the timing of freeze-up and ice-out and the duration of the ice cover have been determined, and the relationship of ice growth to freezing-degree-day (deg C) records evaluated on the basis of a Stefan conduction equation modified to deal with ice sheets covered with or free of snow. Ice growth occurs predominantly by the direct freezing of lake water, but snow ice may compose as much as 50% of the ice cover in winters with higher than average snowfall. Freeze-up leading to the establishment of a stable ice cover occurs during the 4-week period from the end of November to the end of December. Maximum seasonal ice thicknesses were from 45 to 67 cm and are generally attained during the first two weeks of March; ice-out, marking the final disappearance of ice from Post Pond, usually occurs by the third week of April. The overall rate of the ice loss is three to four times that of ice growth, and is dominated initially by melting from the top. As much as 50% of the ice may be lost in this way before the onset of any bottom melting. Final dissipation of the ice cover is usually expedited by candling resulting from preferential melting and disintegration of the ice at crystal boundaries.
    Type of Medium: Series available for loan
    Pages: iv, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 83-4
    URL: https://apps.dtic.mil/docs/citations/ADA126334
    URL: https://hdl.handle.net/11681/9277
    Language: English
    Note: CONTENTS Abstract Preface Introduction Location of study Study methods Ice thickness Ice-cover composition Surface air temperatures Freeze-up and ice-out characteristics Results and discussion Ice-growth record Freezing-degree-day records Ice-growth predictions Summary and conclusions Literature cited Appendix A: Ice-growth records Appendix B: Measured and computed ice-growth curves
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  • 35
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    Marine minerals (1981)
    Washington, D.C. : Mineralogical Society of America
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    Call number: 11/M 19.92803
    In: Reviews in mineralogy, 6
    Type of Medium: Monograph available for loan
    Pages: ix, 380 Seiten , Illustrationen, Diagramme
    Edition: second printing
    ISBN: 978-0-939950-06-5
    Series Statement: Reviews in mineralogy 6
    Language: English
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  • 36
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    Minerals and reactions at the atomic scale : transmission electron microscopy (1981)
    Washington, D.C. : Mineralogical Society of America
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    Call number: 11/M 19.92819
    In: Reviews in mineralogy, 27
    Type of Medium: Monograph available for loan
    Pages: xv, 516 Seiten , Illustrationen, Diagramme
    Edition: second printing
    ISBN: 0-939950-32-4
    Series Statement: Reviews in mineralogy 27
    URL: https://www.degruyter.com/view/books/9781501509735/9781501509735-toc/9781501509735-toc.xml
    Language: English
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  • 37
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    Aguas subterráneas, paisaje y vida : acuíferos de España (2002)
    Madrid : Instituto Geológico y Minero de España
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    Call number: AWI G4-19-92520
    Type of Medium: Monograph available for loan
    Pages: 470 Seiten , Illustrationen , 29 cm
    ISBN: 84-7840-429-5
    Series Statement: Publicaciones del Instituto Geológico y Minero de España : Serie Hidrogeología y aguas subterráneas 2
    Language: Spanish
    Note: ÍNDICE Presentación A MODO DE IN'TRODUCCION Los caminos del agua subterránea: esos grandes desconocidos PARTE PRIMERA: ACUÍFEROS Y RIOS Los acuíferos son los ríos Los Montes Universales: cuna de cursos fluviales El Guadiana: ¿un río?, ¿dos ríos? Dos acuíferos El Mundo, un río de alta cuna ¿Un nacimiento doble para un mismo río? El Ebro Guadalquivir y Segura: ríos hermanos PARTE SEGUNDA: ACUÍFEROS Y ABASTECIMIENTO URBANO Con cimientos de agua Castellón de la Plana: capital del agua subterránea faén y las aguas subterráneas: una dependencia ancestral El acuífero de Madrid: en la raíz del madroño Palma de Mallorca: agua subterránea motor de progreso Arteta: agua de manantial para Pamplona PARTE TERCERA: LOS HUMEDALES Y LAS AGUAS SUBTERRÁNEAS Aguazales y acuíferos Banyoles: el agua que recorre las entrañas de la tierra Las Lagunas de Villafáftla: un reducto húmedo estepario entre cultivos de secano, dehesas y pinares La Laguna de Gallocanta: un oasis palustre sobre el erial de la Depresión del Ebro La Albufera de Valencia: pozos, canales y arroz Delta del Ebro: dendritas de agua dulce en un mar de agua salada De la Laguna de Fuente de Piedra y de la "Fons Divinus" Doñana: filigrana de agua en la marisma PARTE CUARTA: AGUA SUBTERRÁNEA Y PATRIMONIO NATURAL Hidrogeología y naturaleza La Sierra de las Nieves: Gea,Agua, Vida El acuífero kárstico yesífero de Sorbas Los Picos de Europa, un depósito de agua construído por la Naturaleza La Serranía de Cuenca: las arquitecturas del agua Ojo Guareña, el complejo subterráneo más grande de España Larra y Urbasa: dos destacados sistemas kársticos navarros El Torcal de Antequera, ciudad de piedra con cimientos de agua El sistema acuífero del Parque Natural del Garajonay PARTE QUINTA: ACUÍFEROS LIGADOS AL DESARROLLO SOCIOECONÓMICO Las aguas subterráneas: una profunda transformación de nuestra geografia económica De un erial a un lago de plástico Una cultura del manejo del agua durante 500 años Un enclave de prosperidad en la estepa aragonesa Unas aguas misteriosas con mágicos poderes Bibliografia Créditos fotográficos , In spanischer Sprache
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  • 38
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    Glacier mass balance bulletin : a contribution to the Global Climate Observing System (GCOS), the Global Terrestrial Observing System (GTOS), the Global Environment Monitoring System (GEMS) and the International Hydrological Programme (IHP); No. 7: (2000-2001) (2003)
    [Zürich] : World Glacier Monitoring Service (WGMS)
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    Call number: AWI G7-19-92930
    In: Glacier mass balance bulletin, No. 7
    Type of Medium: Series available for loan
    Pages: 87 Seiten , Illustrationen
    Series Statement: Glacier mass balance bulletin 7
    URL: https://wgms.ch/downloads/wgms_2003_gmbb7.pdf
    Language: English
    Note: CONTENTS 1. INTRODUCTION 2. SUMMARY DATA 2.1 SUMMARY TABLE (NET BALANCE, ELA, ELA0, AAR, AAR0) 2.2 CUMULATIVE SPECIFIC NET BALANCE GRAPHS 3. EXTENSIVE INFORMATION 3.1 WHITE (CANADA) 3.1.1 Topography and observational network 3.1.2 Net balance maps 1999/2000 and 2000/2001 3.1.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.1.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.2 PEYTO (CANADA) 3.2.1 Topography and observational network 3.2.2 Net balance maps 1999/2000 and 2000/2001 3.2.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.2.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.3 ZONGO (BOLIVIA) 3.3.1 Topography and observational network 3.3.2 Net balance maps 1999/2000 and 2000/2001 3.3.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.3.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.4 WALDEMARBREEN (NORWAY/SVALBARD) 3.4.1 Topography and observational network 3.4.2 Net balance maps 1999/2000 and 2000/2001 3.4.3 Net balance altitude (1999/2000 and 2000/2001) 3.4.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.5 NIGARDSBREEN (NORWAY) 3.5.1 Topography and observational network 3.5.2 Net balance maps 1999/2000 and 2000/2001 3.5.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.5.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.6 STORGLACIÄREN (SWEDEN) 3.6.1 Topography and observational network 3.6.2 Net balance maps 1999/2000 and 2000/2001 3.6.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.6.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.7 VERNAGTFERNER (AUSTRIA) 3.7.1 Topography and observational network 3.7.2 Net balance maps 1999/2000 and 2000/2001 3.7.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.7.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.8 DJANKUAT (RUSSIA) 57 3.8.1 Topography and observational network 3.8.2 Net balance map 2000/2001 3.8.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.8.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.9 TSENTRALNIY TUYUKSUYSKIY (KAZAKHSTAN) 3.9.1 Topography and observational network 3.9.2 Net balance maps 1999/2000 and 2000/2001 3.9.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.9.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.10 MALIYAKTRU (RUSSIA) 3.10.1 Topography and observational network 3.10.2 Net balance maps 1999/2000 and 2000/2001 3.10.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.10.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.11 URUMQIHE S. NO. 1 (CHINA) 3.11.1 Topography and observational network 3.11.2 Net balance maps 1999/2000 and 2000/2001 3.11.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.11.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 4. FINAL REMARKS AND ACKNOWLEDGEMENTS 5. PRINCIPAL INVESTIGATORS AND NATIONAL CORRESPONDENTS 5.1 PRINCIPAL INVESTIGATORS 5.2 NATIONAL CORRESPONDENTS OF WGMS
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  • 39
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    Pulse transmission through frozen silt (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-84/17
    In: CRREL Report, 84-17
    Description / Table of Contents: VHF-band radiowave short pulses were transmitted within the permafrost tunnel at Fox, Alaska, over distances between 2.2 and 10.5 m. The propagation medium was a frozen silt containing both disseminated and massive ice with temperatures varying from -7°C near the transmitter to probably -2 C near the center of the tunnel overburden. The short pulses underwent practically no dispersion in the coldest zones but did disperse and refract through the warmer overburden, as suggested by calculations of the effective dielectric constant. Most significantly the measured frequency content decreased as the effective dielectric constant increased. The results indicate that deep, cross-borehole pulse transmissions over distances greater than 10 m might be possible, especially when the ground is no warmer than -4°C. The information thus pined could be used for identifying major subsurface variations, including ground ice features.
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    Pages: ii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 84-17
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a147108.pdf
    URL: https://hdl.handle.net/11681/9519
    Language: English
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  • 40
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    The effects of soluble salts on the unfrozen water contents of the Lanzhou, P.R.C., silt (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-84/16
    In: CRREL Report, 84-16
    Description / Table of Contents: Phase composition curves are presented for a typical saline silt from Lanzhou, P.R.C., and compared to some silts from Alaska. The unfrozen water content of the Chinese silt is much higher than that of the Alaskan silts due to the large amount of soluble salts present in the silts from China, which are not present in silt from interior Alaska. When the salt is removed, the unfrozen water content is then similar for both the Chinese and Alaskan silt. Here we introduce a technique for correcting the unfrozen water content of partially frozen soils due to high salt concentrations. We calculate the equivalent molality of the salts in the unfrozen water at various temperatures from a measurement of the electrical conductivity of the extract from saturated paste.
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    Pages: iii, 25 Seiten , Illustrationen
    Series Statement: CRREL Report 84-16
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a152825.pdf
    URL: https://hdl.handle.net/11681/9520
    Language: English
    Note: Contents Abstract Preface Introduction Background Materials Sample preparation Nuclear magnetic resonance Specific surface area Electrical conductivity Results and discussion Summary Literature cited Appendix A: Unfrozen water content vs temperature data for Lanzhou silt
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  • 41
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    Sea ice data buoys in the Weddel Sea (1984)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-84/11
    In: CRREL Report, 84-11
    Description / Table of Contents: Data obtained from two sets of data buoys either air-dropped or deployed by ship onto the Weddell Sea pack ice during the period from Dec 1978 to Nov 1980 are presented. The buoy data include position, pressure and temperature information and to date represent the most complete combined weather and pack ice drift records for the ice-covered Southern Ocean regions. The buoys tended to drift north initially and then to turn east generally between latitudes 62°S and 64°S. Buoy 1433 turned east farther south at approximately 67°S but at about the same time as buoy 0527, implying that the westerly wind belt was farther south than usual in 1979. The range of air pressures-from about 950 mb to about 1020 mb is typical of the circumpolar low pressure trough in the Southern Hemisphere. All buoys were equipped with an internal or compartment temperature sensor. The 1980 buoys also contained an external air temperature sensor in a ventilated, shielded can at 1-m height. Although differences of 10°C or more between recorded air and compartment temperatures are common, the correlation between the two measured temperatures is generally very good. The compartment temperatures are higher probably because the buoy is radiationally heated. We found that subtracting 3°C from the average daily compartment temperature yielded a good estimate of the average air temperature for any given day. This technique can be used to construct average daily air temperature records for the 1979 buoys which only contained the internal or compartment temperature sensor.
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    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 84-11
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a144953.pdf
    URL: https://hdl.handle.net/11681/9504
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods and instrumentation Results Drift tracks Pressure data Temperature data Discussion Conclusions Literature cited
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  • 42
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    Tectono-morphology of the Ligurian Alps and adjacent basins (NW Italy) : an integrated study of their neogene to present evolution (2004)
    Amsterdam : Vrije Universiteit
    Details Availability
    Call number: M 19.92943
    Type of Medium: Dissertations
    Pages: ix, 192 Seiten , Illustrationen
    ISBN: 90-9018106-7
    Language: English
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  • 43
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    Osobennosti struktury atmosfery poljarnych rajonov (1981)
    Leningrad : Gidrometeoizdat
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    Call number: ZSP-799-370
    In: Trudy Ordena Lenina Arktičeskogo i Antarktičeskogo Naučno-Issledovatelʹskogo Instituta, Tom 370
    Type of Medium: Series available for loan
    Pages: 163 Seiten , Illustrationen
    Series Statement: Trudy Ordena Lenina Arktičeskogo i Antarktičeskogo Naučno-Issledovatelʹskogo Instituta 370
    Language: Russian
    Note: In kyrillischer Schrift
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  • 44
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    Supplement to Interregional Training Course on Radiochemistry : Leipzig, GDR, 17th May - 25th June 1982 ; ZfI-13 (1982)
    Leipzig : Academy of Sciences of the GDR, Central Institute for Isotope and Radiation Research
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    Call number: AWI G6-19-93042-2
    In: Interregional Training Course on Radiochemistry, [Supplement]
    Type of Medium: Monograph available for loan
    Pages: 88 Seiten , Illustrationen
    Language: English
    Note: Contents Manual 2.2 The relative measurement of aktivity Lectures 1.3 Statistics / H. Baumbach 2.2 Sealed sources / K. Vormum 2.4 Energy dispersive x-ray fluorescence analysis / H.-K. Bothe 3.1 The use of carriers / H. Koch 4.3 Autoradiography / K. Freyer 6.1 Radiometric methods in environmental control / H.-J. Große
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  • 45
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    Wissenschaftstheorie und gestaltungsorientierte Wirtschaftsinformatik (2009)
    Heidelberg : Physica-Verlag
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    Call number: IASS 20.93369
    Type of Medium: Monograph available for loan
    Pages: XVI, 243 Seiten , graphische Darstellungen , 235 mm x 155 mm
    ISBN: 9783790823356 , 9783790823363 (electronic; eISBN)
    URL: Inhaltsverzeichnis
    Language: German , English
    Note: Beitr. teilw. dt., teilw. engl.
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  • 46
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    Heat and mass transfer from freely falling drops at low temperatures (1980)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-80/18
    In: CRREL Report, 80-18
    Description / Table of Contents: The use of ice as a structural material is common practice for certain applications in cold regions. Techniques such as surface flooding or water spraying are used to accelerate ice growth rates, thereby lengthening the winter construction season. This report examines the heat and mass transfer rates from freely falling water drops in cold air. Design equations which predict the amount of supercooling of the drops as a function of outdoor ambient temperature, drop size and distance of fall are given
    Type of Medium: Series available for loan
    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 80-18
    URL: https://apps.dtic.mil/docs/citations/ADA090522
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Velocity problem Heat and mass transfer problem - A single drop Heat and mass transfer - A system of drops Literature cited Appendix A: FORTRAN IV program to calculate final drop temperature, air temperatureand humidity
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  • 47
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    Environmental engineering and ecological baseline investigations along the Yukon River-Prudhoe Bay Haul Road (1980)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-80/19
    In: CRREL Report, 80-19
    Description / Table of Contents: During the period 1975-1978 the Federal Highway Administration sponsored a series of environmental engineering in­vestigations along the Yukon River to Prudhoe Bay Haul Road. In 1976 the Department of Energy joined these in­vestigations with a series of ecological projects which continue to the present. Both agencies research efforts were con­ducted on a cooperative basis with CRREL’s in-house research program. The objectives of the research focused on 1) an evaluation of the performance of the road, 2) an assessment of changes in the environment associated with the road, 3) documentation of flora and vegetation along the 577-km-long transect, 4) methodologies for revegetation and restoration, and 5) an assessment of biological parameters as indicators of environmental integrity. In support of these objectives, specific studies were undertaken that investigated the climate along the road, thaw and subsidence beneath and adjacent to the road, drainage and side slope performance, distribution and properties of road dust, vegetation distribution, vegetation disturbance and recovery, occurrence of weeds and weedy species, erosion and its control, revegetation and restoration, and construction of the fuel gas line. This report presents background, information on the region, detailed results of the road thaw subsidence and dust investigations, and summaries of revegetation, fuel gas line, vegetation distribution, soil, and weed studies.
    Type of Medium: Series available for loan
    Pages: xv, 187 Seiten , Illustrationen
    Series Statement: CRREL Report 80-19
    URL: https://cdm16021.contentdm.oclc.org/digital/collection/p266001coll1/id/6433
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Chapter 1. The road and its environment Introduction General physiography Regional climate Surficial and bedrock geology Permafrost and ground ice General biota Vegetation Floristic survey Vegetation mapping Soils and mapping Chapter 2. Roadbed performance and associated investigations Roadbed investigations Roadbed performance Performance of drainage features Performance of sideslopes Conclusions from road, drainage and sideslope performance studies Fuel gas line construction Chapter 3. Distribution and properties of road dust along the northern portion of the Haul Road Introduction Methods Results of wind direction and velocity measurements Dust load and distribution Particle size analyses of dust Chemical composition properties of dust and related samples Soil cation composition Dust impacts on vegetation Discussion and conclusions Chapter 4. Revegetation and restoration investigations Introduction Revegetation approaches Alyeska erosion control and revegetation program Weeds and weedy plants Performance of revegetation Alyeska willow cutting program CRREL restoration experiments Conclusions Revegetation recommendations General report recommendations Literature cited Appendix A: General environmental guidelines applicable to subarctic and arctic road construction Appendix B: University-based studies along the Yukon River-Prudhoe Bay Haul Road Appendix C: CRREL maps of Haul Road showing locations of all study Sites Appendix D: Additional Haul Road cross-sectional profiles Appendix E: Clay mineralogy of road-related materials Appendix F: List of reports in the Joint State/Federal Fish and Wildlife Ad­visory Team series
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  • 48
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    Snow pads used for pipeline construction in Alaska, 1976 : construction, use and breakup (1980)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-80/17
    In: CRREL Report, 80-17
    Description / Table of Contents: Construction pads made of snow were used to build two sections of the Trans Alaska Pipeline and a small gas pipeline during the winter of 1975-76. Construction during the winter has become increasingly common in the Arctic. Surface travel and the use of heavy construction equipment on the unprotected tundra have been severely restricted, even during the winter, so the use of temporary winter roads and construction pads built of snow and ice has been advocated and is being adopted. The three snow construction pads mentioned above were the first snow roads and construction pads used on a large scale in Alaska. Snow roads and construction pads have two objectives: to protect the underlying vegetation and upper layers of the ground, and to provide a hard, smooth surface for travel and the operation of equipment. Several types have been built, and a brief discussion is given of their history and classification systems. The three snow construction pads used in construction of the Trans-Alaska Pipeline and the small gas pipeline in 1975-76 were visited and observed while in use. The Globe Creek snow pad, about 50 miles north of Fairbanks, was built primarily of manufactured snow hauled to the site and watered. With very high densities this pad withstood heavy traffic and use by heavy construction equipment except on one steep slope. There, the use of tracked vehicles and vehicles without front wheel drive disaggregated the snow on and near the surface so that vehicles without front wheel drive were unable to climb the hill. The Toolik snow pad, just north of the Brooks Range, was built of compacted snow and proved capable of supporting the heaviest traffic and construction equipment. The fuel gasline snow pad ran from the northern Brooks Range to the Arctic Coast and also proved capable of supporting the necessary traffic. Both the Toolik snow pad and the fuel gasline snow pad failed in very early May because of unseasonably warm and clear weather before the associated construction projects were completed. However, the three snow pads must be considered successful. Common problems were the lack of snow, slopes, unseasonably warm spring weather, and inexperience on the part of contractors and construction personnel.
    Type of Medium: Series available for loan
    Pages: v, 28 Seiten , Illustrationen
    Series Statement: CRREL Report 80-17
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a090521.pdf
    Language: English
    Note: CONTENTS Abstract Preface Introduction History of snow and ice roads Classification of snow and ice roads Snow pads used by Alyeska during the winter of 1975-1976 The Globe Creek snow pad The Toolik snow pad The gasline snow pad Summary and conclusions Literature cited
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  • 49
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    FGGE III-B daily global analyses : March 1979 - May 1979; Part 2 (1981)
    Reading : European Centre for Medium-Range Weather Forecasts
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    Call number: MOP 45206 / Mitte
    In: Daily Global Analyses
    Type of Medium: Monograph available for loan
    Pages: 6, 381 Seiten , graphische Darstellungen
    Series Statement: Daily Global Analyses Part 2
    Language: English
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  • 50
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    FGGE III-B daily global analyses : June 1979 - August 1979; Part 3 (1981)
    Reading : European Centre for Medium-Range Weather Forecasts
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    Call number: MOP 45206 / Mitte
    In: Daily Global Analyses
    Type of Medium: Monograph available for loan
    Pages: 6, 371 Seiten , graphische Darstellungen
    Series Statement: Daily Global Analyses Part 3
    Language: English
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  • 51
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    Workshop on Stochastic Dynamic Forecasting : 17-19 October 1979 (1980)
    [Reading, Berkshire] : [European Centre for Medium Range Weather Forecasts]
    Details Availability
    Call number: MOP 44987 / Mitte
    Type of Medium: Monograph available for loan
    Pages: i, 97 Seiten , Illustrationen , 30 cm
    Language: English
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  • 52
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    Workshop on radiation and cloud-radiation interaction in numerical modelling : 15-17 October 1980 (1981)
    [Reading] : European Centre for Medium Range Weather Forecasts
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    Call number: MOP 47169 / Mitte
    Type of Medium: Monograph available for loan
    Pages: I, 209 Seiten , Illustrationen , 30 cm
    Language: English
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  • 53
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    Vremennye metodičeskie ukazanija po ocenke ėkonomičeskoj ėffektivnosti i kačestva okeanografičeskich issledovanij (1982)
    Moskva : Moskovskoe Otdelenie Gidrometeoizdata
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    Call number: MOP 45862 / Mitte
    Type of Medium: Monograph available for loan
    Language: Russian
    Note: In kyrillischer Schrift
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  • 54
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    Aeronauts and space report of the president : 1983 activities (1983)
    Washington, D.C. : National Aeronautics and Space Administration
    Details Availability
    Call number: MOP 47316 / Mitte
    Type of Medium: Journal available for loan
    Pages: 83 Seiten
    Language: English
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  • 55
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    Ground-truth observations of ice-covered North Slope lakes imaged by radar (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/19
    In: CRREL Report, 81-19
    Description / Table of Contents: Field observations support the interpretation that differences in the strength of radar returns from the ice covers of lakes on the North Slope of Alaska can be used to determine where the lake is frozen completely to the bottom. An ice/frozen soil interface is indicated by a weak return and an ice/ water interface by a strong return. The immediate value of this result is that SLAR (side-looking airborne radar) imagery can now be used to prepare maps of large areas of the North Slope showing where the lakes are shallower or deeper than 1.7m (the approximate draft of the lake ice at the time of the SLAR flights). The bathymetry of these shallow lakes is largely unknown and is not obvious from their sizes or outlines. Such information could be very useful, for example in finding suitable year-round water supplies.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 81-19
    URL: https://hdl.handle.net/11681/9424
    Language: English
    Note: CONTENTS Abstract Preface Introduction The experiment Results Maps of completely frozen North Slope lakes Literature cited
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  • 56
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    Shallow snow model for predicting vehicle performance (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/20
    In: CRREL Report, 81-20
    Description / Table of Contents: A historical review of research is presented to establish the state- of-the-art for analyzing the behavior of vehicles in shallow snow. From this review, the most comprehensive and promising model is put together to establish a first-cut performance prediction model for vehicles operating in shallow snow, slush, ice and thawing soils.
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    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 81-20
    URL: https://hdl.handle.net/11681/9422
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Historical review Model selection Traction Resistance Slush and thawing soils Ice, hard-packed snow, packed snow River and lake ice Model use Conclusions Literature cited
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  • 57
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    Chena River Lakes Project revegetation study : three-year summary (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/18
    In: CRREL Report, 81-18
    Description / Table of Contents: During the growing seasons of 1977, 1978, and 1979, revegetation techniques were studied on the Chena River Lakes Project, a flood control dam and levee near Fairbanks, Alaska, to find an optimal treatment for establishing permanent vegetation cover on the gravel structures. The treatments tested on plots at the dam andor levee involved three main variables 1 vegetation grass and clover seed andor willow cuttings, 2 mulch, mulch blanket, andor sludge, and 3 substrate gravel or fine-grained soil over the gravel base. The mulches were hay, wood-cellulose-fiber, peat moss, and Conwed Hydro Mulch 2000, which is a wood-cellulose-fiber mulch with a polysaccharide tackifier. A constant rate of fertilizer was applied to all plots except the control. A section of each plot was refertilized again in their third growing season to compare annual and biannual fertilization. The high fertilization rate produced above-average growth. Fescue, brome, and foxtail were the most productive species on the dam, while alsike cover was the most productive on the wetter levee site. When grass seed and willow cuttings were planted at the same time, willow survival and growth were reduced. Fertilization is required for at least two years to produce an acceptable permanent vegetation cover, although fine- grained soil or sludge reduces the amount of fertilizer needed in the second year. Third-year fertilization may not be necessary since the benefits of the second fertilization continue for at least two years. A sludge treatment refertilized during its second growing season produces the highest biomass recorded in this study.
    Type of Medium: Series available for loan
    Pages: ix, 59 Seiten , Illustrationen
    Series Statement: CRREL Report 81-18
    URL: https://hdl.handle.net/11681/9427
    Language: English
    Note: CONTENTS Abstract Preface Abbreviations Conversion factors Summary Introduction Background Site characterization Climate Purpose Materials and methods General Moose Creek Dam site Tanana Levee site Sampling and measurement Abiotic controls on vegetation Meteorological data Soil moisture as a limiting factor Soil chemical analysis Vegetation growth and survival Moose Creek Dam site Tanana Levee site Biomass by species Roof penetration Seedling density of invading woody species Weeds Supplemental observations Sediment loss Sludge and runoff-water composition Cost analysis Conclusions Literature cited Appendix A: 1977 grass growth on 1977 dam treatments Appendix B: 1978 grass growth on 1977 dam treatments Appendix C: 1979 grass growth on 1977 dam treatments Appendix D: Grass growth on 1978 dam treatments Appendix E: 1977, 1978, and 1979 survival of willow treatments Appendix F: Grass growth on Tanana levee treatments Appendix C: Chemical analysis of sludge and runoff water
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  • 58
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    Near-infrared reflectance of snow-covered substrates (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/21
    In: CRREL Report, 81-21
    Description / Table of Contents: The reflection of solar radiation by a snow cover in situ and the apparent influence of selected substrates were examined in wavelength bands centered at 0.81, 1.04, 1.10, 1.30, 1.50 and 1.80 micrometers. Substrates included winter wheat, timothy, corn, alfalfa, grass, concrete and subsurface layers of 'crusty' snow and ice. Reasonable qualitative agreement between measurements and theoretical predictions was demonstrated, with indications of quantitative agreement in the definition of a 'semi-infinite depth' of snow cover. It was concluded that ultimate quantitative agreement between theory and measurement will require that an 'optically effective grain size' be defined in terms of physically measuarable dimensions or meteorologically predictable characteristics of the ice crystals composing the snowpack.
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    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 81-21
    URL: https://hdl.handle.net/11681/9419
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experimental method Substrate preparation Experimental configuration Radiometric measurements Snow characterization Reflectance standards Data analysis Reflectance measurements Snow replica analysis Discussion of results Comparative reflectance of various substrates under snow Ablation of a snow cover Reflectance from a very light, fresh snow cover Measurements at angles other than vertical Reflectance from substrates Concluding observations Literature cited
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  • 59
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    Consolidated report on the voluntary co-operation programme including projects approved for circulation in 1983 (1984)
    Geneva : Secretariat of the World Meteorological Organization
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    Call number: MOP 46028/1983 / Mitte
    In: World weather watch : Consolidated report on the voluntary co-operation programme including projects approved for circulation, 1983
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    Language: English
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  • 60
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    Workshop on the planetary boundary layer : 14-18 August 1978, Boulder, Colorado (1980)
    Boston, Mass. : American Meteorological Society
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    Call number: MOP 45485 / Mitte
    Type of Medium: Monograph available for loan
    Pages: iv, 322 Seiten , Illustrationen, Diagramme
    ISBN: 0933876513
    Language: English
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  • 61
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    Tropical Cyclone Programme : plan of action (1981)
    Geneva : Secretariat of the World Meteorological Organization
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    Call number: MOP 45477 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 2, II, 47, 4 Seiten , Illustrationen
    Series Statement: Report 4
    Language: English
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  • 62
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    The politics of method in the human sciences : positivism and its epistemological others (2005)
    Durham : Duke University Press
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    Call number: IASS 20.95309
    Type of Medium: Monograph available for loan
    Pages: 620 Seiten , 25 cm
    ISBN: 0822335182 , 9780822335184 , 0822335069 , 9780822335061
    Series Statement: Politics, history, and culture
    URL: http://www.loc.gov/catdir/toc/ecip051/2004022945.html
    Language: English
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  • 63
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    United States Antarctic Research Report Number 24 to SCAR : I April 1981-October 1982 record of activities ; II October 1982-October 1983 planned activities (1982)
    Washington, D.C. : Polar Research Board
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    Call number: MOP 46293/B / Mitte
    In: United States Antarctic Research Report to SCAR, No. 24
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    Series Statement: United States Antarctic Research Report to SCAR 24
    Language: English
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  • 64
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    Report on United States Antarctic research activities : United States National Committee on Antarctic Research Report Number 26 to SCAR ; I February 1983-October 1984 record of activities ; II October 1984-September 1985 planned activities (1984)
    Washington, D.C. : Polar Research Board
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    Call number: MOP 46293/A / Mitte
    In: United States Antarctic Research Report to SCAR, No. 26
    Type of Medium: Series available for loan
    Series Statement: United States Antarctic Research Report to SCAR 26
    Language: English
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  • 65
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    USSR national report No. 25 to SCAR (1983)
    Moscow : Academy of Sciences of the USSR, Soviet Committee on Antarctic Research
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    Call number: MOP 46294/A / Mitte
    In: USSR national report to SCAR, No. 25
    Type of Medium: Series available for loan
    Series Statement: USSR national report to SCAR 25
    Language: English
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  • 66
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    Analyzing oppression (2006)
    New York : Oxford Univ. Press
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    Call number: IASS 20.94162
    Type of Medium: Monograph available for loan
    Pages: XII, 278 S , Ill , 24 cm
    ISBN: 9780195187434 , 0195187431 , 019518744X , 9780195187441
    Series Statement: Studies in feminist philosophy
    URL: http://www.loc.gov/catdir/enhancements/fy0638/2005049873-t.html
    URL: http://www.loc.gov/catdir/enhancements/fy0639/2005049873-d.html
    URL: http://www.loc.gov/catdir/enhancements/fy0725/2005049873-b.html
    URL: http://www.gbv.de/dms/hbz/toc/ht014766812.pdf
    Language: English
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    Twenty-fourth Plenary Meeting, Committee on Space Research : XXIV COSPAR ; abstracts ; Ottawa, Canada, 16 May - 2 June 1982 (1982)
    Paris, France : COSPAR Secretariat
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    Call number: MOP 46270 / Mitte
    Type of Medium: Monograph available for loan
    Pages: viii, 545 Seiten , 28 cm
    Language: English
    Note: Prefatory material in French
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  • 68
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    Asphalt concrete for cold regions : a comparative laboratory study and analysis of mixtures containing soft and hard grades of asphalt cement (1980)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-80/5
    In: CRREL Report, 80-5
    Description / Table of Contents: This research comprised laboratory testing to determine the properties of asphalt-aggregate mixtures containing three grades of asphalt cements, and analyses to project the performance of pavements containing each of the asphalts, in resisting thermally induced distress and traffic-associated distress. From the results it is concluded that only the softest asphalt cement tested (AC 2.5) would perform satisfactorily in a cold climatic zone. The moderately soft (AC 5) and moderately hard (AC 20) asphalt cements showed little susceptibility to thermal cracking in a moderate and a warm climatic zone, respectively. The AC 2.5 and AC 5 asphalts are not recommended for use in warm climates, however, owing to increased susceptibility to rutting under traffic.
    Type of Medium: Series available for loan
    Pages: vi, 55 Seiten , Illustrationen
    Series Statement: CRREL Report 80-5
    URL: https://apps.dtic.mil/docs/citations/ADA082198
    URL: https://hdl.handle.net/11681/9528
    Language: English
    Note: CONTENTS Abstract Preface Introduction Research setting Objectives Materials, mixture designs, and tests Materials Mixture design tests Brazil test Resilient modulus test Data analysis Marshall tests Asphalt grade Compactive effort Aggregate type Data analysis Brazil tests Indirect tensile strength Tensile strain Vertical deformation Summary of Brazil test results Data analysis-resilIient modulus. Comparison of mixture susceptibility to temperature cracking General asphalt concrete stiffness Thermal cracking. Influence of asphalt cement properties Summary Comparison of mixture susceptibility to traftic-load-associated distress Stress/strain analysis Fatigue damage analysis Rutting analysis Strength correlations Marshall stability and indirect tensile strength Indirect tensile strength and resilient modulus Summary Summary and conclusions Recapitulation of investigations Summary of results Conclusions Literature cited Appendix A: Asphalt adggregate mixture properties by Marshall method Appendix B: Equations for calculating specimen properties from Brazil tests Appendix C: Calculated displacements, strains and stresses
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  • 69
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    Environmental analysis of the Upper Susitna River Basin using Landsat imagery (1980)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-80/4
    In: CRREL Report, 80-4
    Description / Table of Contents: The primary objectives of this study were to 1) prepare a map from Landsat imagery of the Upper Susitna River Basin drainage network, lakes, glaciers and snowfields, 2) identify possible faults and lineaments within the upper basin and within a 100-km radius of the proposed Devil Canyon and Watana dam sites as observed on Landsat imagery, and 3) prepare a Landsat-derived map showing the distribution of surficial geologic materials and poorly drained areas. The EROS Digital Image Enhancement System (EDIES) provided computer- enhanced images of Landsat-1 scene 5470-19560. The EDIES false color composite of this scene was used as the base for mapping drainage network, lakes, glaciers and snowfields, six surficial geologic materials units and poorly drained areas. We used some single-band and other color composites of Landsat images during interpretation. All the above maps were prepared by photointerpretation of Landsat images without using computer analysis, aerial photographs, field data, or published reports. These other data sources were used only after the mapping was completed to compare and verify the information interpreted and delineations mapped from the Landsat images. Four Landsat-1 MSS band 7 winter scenes were used in the photomosaic prepared for the lineament mapping. We mapped only those lineaments related to reported regional tectonics, although there were many more lineaments evident on the Landsat photomosaic.
    Type of Medium: Series available for loan
    Pages: iii, 41 Seiten , Illustrationen
    Series Statement: CRREL Report 80-4
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a084900.pdf
    URL: https://hdl.handle.net/11681/9039
    Language: English
    Note: CONTENTS Abstract Preface Summary Objectives Conclusions Introduction Background Previous cooperative investigations Project rationale and coordination Approach Landsat imagery Interpretation techniques Part I. Use of Landsat imagery in mapping the drainage network, lakes, glaciers and snowfields (Lawrence W. Gatto) Objective Methods Results Conclusions Part II. Use of Landsat imagery in mapping and evaluating geologiclineaments and possible faults (Carolyn J. Merry) Objective Geologic structure Methods Results Conclusions Part Ill. Use of Landsat imagery in mapping surficial materials Section A. Landsat mapping (Harlan L. McKim) Objective Methods Results Section B. Field evaluation (Daniel E. Lawson) Objectives Methods Results Discussion Section C. Conclusions (Daniel E. Lawson and Harlan L. McKim) Literature cited Glossary
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  • 70
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    A statistical evaluation of soil and climatic parameters affecting the change in pavement deflection during thawing of subgrades (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/15
    In: CRREL Report, 81-15
    Description / Table of Contents: This report analyzes the results of a field study previously reported by Scrivner et al. (1969) for the National Cooperative Highway Research Program. These authors studied the seasonal pavement deflection characteristics of 24 test sites on roads in service in regions with freezing indexes ranging from 100 F-days to 2100 F-days. They used the Dynaflect cyclic pavement loading device to determine the pavement system response. Of specific interest to my analysis was the increased pavement deflection after freezing and thawing and the time to recovery of normal deflection characteristics. These characteristics were related to soil and climatic factors using statistical techniques. The most significant observations of this statistical analysis are: (1) that the freezing index is not a significant parameter in determining the percent increase in pavement deflection during thawing, and (2) that the recovery time is inversely proportional to the depth of freezing. As was expected, the most significant variable affecting the increase in pavement deflection was the frost susceptibility classification. This observation reinforces the necessity for careful selection of soil materials used in pavement systems.
    Type of Medium: Series available for loan
    Pages: v, 10 Seiten , Ilustrationen
    Series Statement: CRREL Report 81-15
    URL: https://hdl.handle.net/11681/9492
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Description of test site Test results Method of analysis Results of analysis Change in resilient deflection due to thawing, A Recovery time after onset of thawing, t20 Discussion of results Change in resilient deflection due to thawing, A. Recovery time after thawing, t20 Conclusions Literature cited ILLUSTRATIONS Figure Pavement deflection and frost penetration vs time Data points and regression line for A and t2 0 versus F Data points and regression line for A and t2 0 versus W Data points and regression line for A and t2 0 versus I Data points and regression line for A and t20 versus N Data points and regression line for A and t20 versus D Data points and regression line for t20 versus A Permeability vs void ratio for the Toledo Penn 7 material TABLES Properties of test sections Test results from Scrivner et al Results of regression analysis
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  • 71
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    Cold regions testing of an air-transportable shelter (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/16
    In: CRREL Report, 81-16
    Description / Table of Contents: An air-transportable shelter designed and built at CRREL for use in cold regions underwent testing in Hanover, New Hampshire, and Ft. Greely, Alaska. The shelter demonstrated some of its capabilities for mobility by being towed for more than 60 miles behind various vehicles and by being transported on a C-130 cargo airplane, a CH-47 helicopter, and a trailer truck. The shelter proved to be very easy for a crew of two to four to set up in all weather conditions including -40 F cold. However, the gasoline-powered generator, which was a source for space heat as well as electricity, functioned very poorly. Overall, the prototype successfully demonstrated qualities of self-reliance, ease of operation and thermal efficiency.
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    Pages: v, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 81-16
    URL: https://hdl.handle.net/11681/9412
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion factors Summary Introduction Description of shelter Test procedures and results Mobility Ease of erecting and striking Therinal efficiency and performance Heat output Electrical system Habitation Safety features Water system Shelter reliability Structure Performance of other shelters Conclusions Future studies Literature cited
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  • 72
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    Subsea trenching in the Arctic (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/17
    In: CRREL Report, 81-17
    Description / Table of Contents: Environmental conditions are described for the continental shelf of the western Arctic, and for the shelf of Labrador and Newfoundland. Special emphasis is given to the gouging of bottom sediments by ice pressure ridges and icebergs, and an approach to systematic risk analysis is outlined. Protection os subsea pipelines and cables by trenching and direct embedment is discussed, touching on burial depth, degree of protection, and environmental impact. Conventional land techniques can be adapted for trenching across the beach and through the shallows, but in deeper water special equipment is required. The devices discussed include hydraulic dredges, submarine dredges, plows, rippers, water jets, disc saws and wheel ditchers, ladder trenchers and chain saws, routers and slot millers, ladder dredges, vibratory and percussive machines, and blasting systems. Consideration is given to the relative merits of working with seabed vehicles, or alternatively with direct surface support from vessels or from the sea ice
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    Pages: 38 Seiten , Illustrationen
    Series Statement: CRREL Report 81-17
    URL: https://hdl.handle.net/11681/9409
    Language: English
    Note: CONTENTS Abstract Preface Introduction The western Arctic of North America The continental shelf of Newfoundland and Labrador Burial depth for pipes and cables Degree of protection offered by burial Environmental impact Trenching the beach and the shallows in the western Arctic Trenching beyond the shallows Suction, or hydraulic, dredging Bottom-t raveling cutterhead dredges Plows Rippers Water jets Subsea disc saws and wheel ditchers Subsea ladder trenchers and chain saws Subsea routers and slot millers Bucket ladder trenchers Vibratory and percussive devices Hard rock excavation under water Control and monitoring of subsea machines Vessels and vehicles Trenching from the sea ice Costs of subsea trenching Reference Appendix: Description of waters off Alaska and Newfoundland
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  • 73
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    Hydraulic model study of a water intake under frazil ice conditions (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/3
    In: CRREL Report, 81- 3
    Description / Table of Contents: Abstract: A 1:24 scale hydraulic model study of water intake under frazil ice conditions is presented. The intake, located 9 m below the surface of the St. Lawrence River in Massena, New York,has a through flow of 0.14 m^3/s. The model study, conducted in the refrigerated flume facility of the U.S. Army Cold Regions Research and Engineering Laboratory, investigated methods of minimizing the frazil ice blockage on the intake. Two protective structures were modeled and the relative benefits of each are presented. The additional cross-sectional area provided by the protective structures lowered the vertical velocity component of the intake water to 0.0027 m/s. At this velocity the buoyant force acting on the frazil ice particle is larger than the downward drag force, causing the particle to rise. The results demonstrate that under certain low flow conditions a protective structure can minimize frazil ice blockage problems.
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    Pages: 11 Seiten , Illustrationen
    Series Statement: CRREL Report 81-03
    URL: https://hdl.handle.net/11681/9573
    Language: English
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  • 74
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    Hyperbolic reflections on Beaufort Sea seismic records (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/2
    In: CRREL Report, 81-2
    Description / Table of Contents: Abstract: Many hyperbolic reflections have been observed on marine seismic records obtained during oil exploration in the Beaufort Sea, and on USGS seismic sub-bottom profiles from the Prudhoe Bay vicinity. A hyperbolic projection system was designed to rapidly measure seismic velocities from the curves on the records. The velocities observed were approximately the velocity of sound in water. The hyperbolic signals also showed dispersion properties similar to acoustic normal modes in shallow water. These observations indicate that the signals responsible for the hyperbolic reflections propagate as normal modes within the water layer, with very limited penetration of the seabed. Determinations of the dominant frequency of these signals indicate that the penetration into the seabed has a characteristic attenuation depth (skin depth) of about 1.5 m for the sub-bottom profiles and 12 m for the marine records. It therefore appears that some hyperbolic reflections may be generated by variations in materials that occur near the seabed. There is some evidence of linearity of the anomalies, possibly related to sediment-filled or open ice gouges, or other changes in material properties at shallow depths.
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    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 81-2
    URL: https://hdl.handle.net/11681/9571
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods of analysis Marine seismic records Seismic sub-bottom profiles Results and discussion Distribution of hyperbolic reflections Hyperbolas on oil exploration records Hyperbolas on sub-bottom profiles Conclusions Literature cited Appendix A: Hyperbola projector
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  • 75
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    Revegetation and selected terrain disturbances along the trans-Alaska pipeline, 1975-1978 (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/12
    In: CRREL Report, 81-12
    Description / Table of Contents: Revegetation techniques along the trans-Alaska pipeline as employed by Alyeska Pipeline Service Company during the 1975-1978 summers were observed. Objectives included determining the success of treatments, identifying problem areas, and noticing long-term implications. Observations and photographs at 60 sites located along the trans-Alaska pipeline indicated frequent occurrence of successful revegetation as well as frequent problems, such as erosion, slope instability, poor scheduling of seed application, occurrence of weed species, failure to optimally reuse topsoil and fine-grained soil, and low rates of native species reinvation. Alyeska's visual impact engineering was observed to be very successful, as shown by high first-season survival. However, a related program for establishing willow cuttings was unsuccessful in 1977 but appeared very promising in 1978 largely due to improved management and more favorable growing conditions. Terrain disturbances due to the construction of the fuel gas line, snowpads, and oil spills were examined to identify and describe related environmental impacts on natural vegetation. Proper construction and use of snowpads minimized the extent and severity of disturbance. Crude oil spills, although damaging to vegetation did not cause total kill of vegetation, and certain types of spills may have only short-term effects. Results of restoration research by CRREL along the trans-Alaska pipeline are discussed.
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    Pages: 115 Seiten , Illustrationen
    Series Statement: CRREL Report 81-12
    URL: https://hdl.handle.net/11681/9467
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Revegetation procedures 1975-1978 construction seasons Willow cutting program Visual impact engineering program Selected terrain disturbances Fuel gas line and snowpads Island Lake and oil line snowpads Oil spills and revegetation CRREL restoration sites Conclusions Recommendations Literature cited Appendix A: List of sites observed during 1975 Appendix B: Annotated photographs of permanent revegetation observation sites-1975-1978 Appendix C: Photographic record of fuel gas line observation sites
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  • 76
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    VHF electrical properties of frozen ground near Point Barrow, Alaska (1981)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-81/13
    In: CRREL Report, 81-13
    Description / Table of Contents: Electrical properties of frozen ground were measured using radio frequency interferometry (RFI) in the very high frequency (VHF) radiowave band. Ice-rich organic silts and sands and gravels of variable ice content were investigated during early April of both 1979 and 1980. Frequencies between 10 and 150 MHz were used with best results obtained between 40 and 100 MHz. Surface impedance and magnetic induction techniques were also used to obtain an independent measure of low frequency resistivity and to obtain a separate control on vertical inhomogeneity. Soil samples were tested for organic and water content. The dielectric constants determined for the ice-rich organic silts ranged from 4.0 to 5.5 while those for the sands and gravels were about 5.1. Dielectric loss was due to d.c. conduction and was very low for the silts but significant for the sands and gravels. The higher values for the sands and gravels were most likely due to the higher concentrations of salt that are reported to exist in the old beach ridges in this region. All the RFI measurements are believed to be indicative of only the first few meters of the ground although the radiowaves could penetrate to tens of meters.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 81-13
    URL: https://hdl.handle.net/11681/9466
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Objectives and procedures Theory and instrumentation Radio frequency interferometry Case 1: Homogeneous ground model Case 2: Two-layer ground model RFI instrumentation Low frequency methods Point Barrow sites Results and discussion Site 1: Tundra Site 2: Beach ridge Site 3: Marsh Conclusions Literature cited Appendix A: Discussion of low-frequency geophysical methods
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    United Kingdom Antarctic research 1983 report : April 1982-September 1983: record of activities ; October 1983-September 1984: planned activities (1983)
    London : The Royal Society, British National Committee on Antarctic Research
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    Call number: MOP 46292/A / Mitte
    In: United Kingdom Antarctic research report, 1983
    Type of Medium: Series available for loan
    Series Statement: United Kingdom Antarctic research report 1983
    Language: English
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    Reconstructing macroeconomics : structuralist proposals and critiques of the mainstream (2004)
    Cambridge, Mass. [u.a.] : Harvard Univ. Press
    Details Availability
    Call number: PIK B 100-20-94186
    Type of Medium: Monograph available for loan
    Pages: IX, 442 Seiten , Diagramme , 26 cm
    ISBN: 0674010736 (alk. paper)
    URL: Inhaltsverzeichnis
    Language: English
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    Seminar on graphical applications in meteorology : 19-23 October 1981 (1981)
    Reading, Berkshire : European Centre for Medium Range Weather Forecasts
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    Call number: MOP 45661 / Mitte
    Type of Medium: Monograph available for loan
    Language: English
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    Manufacturing processes for design professionals (2007)
    London : Thames & Hudson
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    Call number: IASS 21.94677
    Type of Medium: Monograph available for loan
    Pages: 528 S , zahlr. Ill., graph. Darst , 29cm
    Edition: 1. publ.
    ISBN: 0500513759 (hbk.) , 9780500513750 (hbk.)
    URL: http://www.gbv.de/dms/weimar/toc/53748101X_toc.pdf
    Language: English
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    The politics of unsustainability : eco-politics in the post-ecologist era (2008)
    London [u.a.] : Routledge
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    Call number: IASS 20.94318
    Type of Medium: Monograph available for loan
    Pages: 207 Seiten , 24cm
    ISBN: 9781138882331 , 9780415466202
    Series Statement: Environmental politics
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    A guide for references and distribution for the class Bacillariophyceae in Chile between 18°28'S and 58°S (1983)
    Vaduz : Cramer
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    Call number: AWI Bio-21-94346
    In: Bibliotheca diatomologica, 3
    Type of Medium: Monograph available for loan
    Pages: 386 Seiten
    ISBN: 3768213757
    Series Statement: Bibliotheca diatomologica 3
    Language: English
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    Report of the meeting of the JSC Working Group on Alpex and focal points : (Geneva, 28-30 April 1980) (1980)
    Geneva : WMO
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    Call number: MOP 45063 / Mitte
    Type of Medium: Monograph available for loan
    Language: English
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    Floristic list of the non marine diatoms (Bacillariophyceae) of Iberian peninsula, Balearic Islands and Canary Islands : updated taxonomy and bibliography (2003)
    Ruggell : Gantner
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    Call number: AWI Bio-21-94353
    Type of Medium: Monograph available for loan
    Pages: 639 Seiten , Illustrationen
    ISBN: 3906166082
    Series Statement: Diatom monographs 4
    Language: English
    Note: Contents Introduction Taxonomic classification adopted and floristic list References Nomenclatural proposals Index of taxa
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    Non-marine and littoral diatoms from Antarctic and subantarctic regions : distribution and updated taxonomy (2002)
    Vaduz : Gantner
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    Call number: AWI Bio-21-94352
    Type of Medium: Monograph available for loan
    Pages: 795 Seiten
    ISBN: 3904144731
    Series Statement: Diatom monographs 1
    Language: English
    Note: CONTENTS Introduction Objectives and Scope of this Volume Taxonomic Considerations Varieties and Formae The "typifying variety" concept Taxonomic Citations Limitations Taxonomic Errors Some Observations on Antarctic Diatoms Antarctic Diatom Localities Antarctic Interior And Ice Shelves Transantarctic Mountains etc East Antarctic Coast Ross Sea Embayment Amundsen Sea Antarctic Peninsula Area Subantarctic Islands and Southern Continents Acknowledgments What This Compilation Includes Antarctic and Subantarctic Diatoms References Index of Species
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    Diversity and ecology of benthic diatom communities in relation to acidity, acidification and recovery of lakes and rivers (2007)
    Ruggell : Gantner
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    Call number: AWI Bio-21-94355
    Type of Medium: Monograph available for loan
    Pages: 168 Seiten , Illustrationen
    ISBN: 9783906166568
    Series Statement: Diatom monographs 9
    URL: Table of Contents
    Language: English
    Note: CONTENTS ABSTRACT 1. INTRODUCTION 2. AIMS AND SCOPE 3. NATURAL AND ANTHROPOGENIC ACIDIFICATION AND ITS ECOLOGICAL CONSEQUENCES 3.1. The role of water pH 3.2. Description of natural and anthropogenic acid sources 3.3. Anthropogenic acidification and its ecological consequences 3.4. Diatoms as indicators of water acidity and related factors 4. MATERIAL AND METHODS 4.1. Field samples 4.2. Laboratory methods 4.3. Data analysis 5. DESCRIPTION OF THE STUDY AREAS 6. RESULTS 6.1. Diatom community patterns vs. water chemistry in relation to different water types 6.2. Diatom community patterns in relation to altitude 6.3. Diatom community patterns in relation to dijf'erent geographical regions in Poland and Finland 6.4. Diatoms as indicators of pH, alkalinity and TOC 6.5. Restoration and recovery of acidified aquatic ecosystems 6.5.1. Diatoms as indicators of restoration: effect of water neutralization 6.5.2. Diatoms as indicators of lake recovery 7. DISCUSSION 8. NOTES ON AUTECOLOGY OF SELECTED DIATOM TAXA 9. SUMMARY AND CONCLUSIONS ACKNOWLEDGEMENTS REFERENCES APPENDIX (Codes of diatom taxa used in the graphs and tables) PLATES
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  • 87
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    Automatic diatom identification (2002)
    New Jersey : World Scientific
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    Call number: AWI Bio-21-94357
    Type of Medium: Monograph available for loan
    Pages: XI, 316 Seiten , Illustrationen
    ISBN: 9810248865
    Series Statement: Series in machine perception and artificial intelligence 51
    URL: http://bvbr.bib-bvb.de:8991/exlibris/aleph/a22_1/apache_media/MT5REBU8BIFF6GNRK4JBJ83M9YS9DF.pdf
    Language: English
    Note: Contents Preface Acknowledgments Authors' Affiliations 1 Introduction to ADIAC and This Book / Hans du Buf and Micha M. Bayer 2 Diatoms: Organism and Image / David G. Mann 3 Diatom Applications / Richard J. Telford, Steve Juggins, Martyn G. Kelly, and Bertrand Ludes 4 ADIAC Imaging Techniques and Databases / Micha M. Bayer and Steve Juggins 5 Human Error and Quality Assurance in Diatom Analysis / Martyn G. Kelly, Micha M. Bayer, Joachim Hurlimann, and Richard J. Telford 6 Contour Extraction / Stefan Fischer, Hamid R. Shahbazkia, and Horst Bunke 7 Identification Using Classical and New Features in Combination with Decision Tree Ensembles / Stefan Fischer and Horst Bunke 8 Identification by Curvature of Convex and Concave Segments / Robert E. Lake and Hans du Buf 9 Identification by Contour Profiling and Legendre Polynomials / Adrian Ciobanu and Hans du Buf 10 Identification by Gabor Features / Luis M. Santos and Hans du Buf 11 Identification by Mathematical Morphology / Michael H. F. Wilkinson, Andrei C. Jalba, Erik R. Urbach, and Jos B. T. M. Roerdink 12 Mixed-Method Identifications / Michel A. Westenberg and Jos B. T. M. Roerdink 13 Automatic Slide Scanning / Jose L. Pech-Pacheco and Gabriel Cristobal 14 ADIAC Achievements and Future Work / Hans du Buf and Micha M. Bayer Appendix: The Mixed Genera Data Set
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    facet.materialart.12
    The geological evolution of the Eastern Mediterranean (1984)
    Oxford [u.a.] : Blackwell
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    Details
    Call number: 10.1144/GSL.SP.1984.017.01.68 (e-book)
    In: Special publications / the Geological Society, London, Volume 17
    Description / Table of Contents: The Eastern Mediterranean is an excellent ‘field laboratory’ for the study of fundamental processes of continental rifting, passive margin development, ophiolite generation and emplacement and the tectonic, magmatic and sedimentary effects of continental collision. Since its publication in 1984, The Geological Evolution of the Eastern Mediterranean has proved to be an invaluable aid to research in this important region. Many of the papers are classics that report basic data and tectonic interpretations that still remain valid today. The individual papers summarize a large amount of international research that was carried out in the Eastern Mediterranean region during the previous decade. This volume was the first integrated overview of one of the world’s most complex orogenic areas. The editors have added an outline of the main research developments since 1984 and key references to the more recent literature; several figures have been redrawn and the volume is now fully indexed.
    Type of Medium: 12
    Pages: 1 Online-Ressource (VII, 836 Seiten) , Illustrationen
    ISBN: 0632011440 , 1-897799-66-7 , 1897799667
    Series Statement: Special publications / the Geological Society, London 17
    URL: https://doi.org/10.1144/GSL.SP.1984.017.01.68
    DOI: 10.1144/GSL.SP.1984.017.01.68
    Language: English
    Note: Contents Recent research developments / Geological Society, London, Special Publications, 17:xi-xii, doi:10.1144/GSL.SP.1984.017.01.01 --- A. H. F. Robertson and J. E. Dixon: Introduction: aspects of the geological evolution of the Eastern Mediterranean / Geological Society, London, Special Publications, 17:1-74, doi:10.1144/GSL.SP.1984.017.01.02 --- 1. Palaeotethys --- Editor’s introduction / Geological Society, London, Special Publications, 17:75-76, doi:10.1144/GSL.SP.1984.017.01.03 --- A. M. C. Şengör, Y. Yılmaz, and O. Sungurlu: Tectonics of the Mediterranean Cimmerides: nature and evolution of the western termination of Palaeo-Tethys / Geological Society, London, Special Publications, 17:77-112, doi:10.1144/GSL.SP.1984.017.01.04 --- Olivier Monod and Ergün Akay: Evidence for a Late Triassic-Early Jurassic orogenic event in the Taurides / Geological Society, London, Special Publications, 17:113-122, doi:10.1144/GSL.SP.1984.017.01.05 --- I. E. Kerey: Facies and tectonic setting of the Upper Carboniferous rocks of Northwestern Turkey / Geological Society, London, Special Publications, 17:123-128, doi:10.1144/GSL.SP.1984.017.01.06 --- E. Demirtaşh: Stratigraphic evidence of Variscan and early Alpine tectonics in Southern Turkey / Geological Society, London, Special Publications, 17:129-145, doi:10.1144/GSL.SP.1984.017.01.07 --- 2. Neoththys --- Levant and North African offshore: Editor’s introduction / Geological Society, London, Special Publications, 17:147-149, doi:10.1144/GSL.SP.1984.017.01.08 --- M. Delaune-Mayere: Evolution of a Mesozoic passive continental margin: Baër-Bassit (NW Syria) / Geological Society, London, Special Publications, 17:151-159, doi:10.1144/GSL.SP.1984.017.01.09 --- G. Sestini: Tectonic and sedimentary history of the NE African margin (Egypt—Libya) / Geological Society, London, Special Publications, 17:161-175, doi:10.1144/GSL.SP.1984.017.01.10 --- Gdaliahu Gvirtzman and Tuvia Weissbrod: The Hercynian Geanticline of Helez and the Late Palaeozoic history of the Levant / Geological Society, London, Special Publications, 17:177-186, doi:10.1144/GSL.SP.1984.017.01.11 --- Z. Garfunkel and B. Derin: Permian-early Mesozoic tectonism and continental margin formation in Israel and its implications for the history of the Eastern Mediterranean / Geological Society, London, Special Publications, 17:187-201, doi:10.1144/GSL.SP.1984.017.01.12 --- Yehezkeel Druckman: Evidence for Early-Middle Triassic faulting and possible rifting from the Helez Deep Borehole in the coastal plain of Israel / Geological Society, London, Special Publications, 17:203-212, doi:10.1144/GSL.SP.1984.017.01.13 --- Abdulkader M. Abed: Emergence of Wadi Mujib (Central Jordan) during Lower Cenomanian time and its regional tectonic implications / Geological Society, London, Special Publications, 17:213-216, doi:10.1144/GSL.SP.1984.017.01.14 --- F. Hirsch: The Arabian sub-plate during the Mesozoic / Geological Society, London, Special Publications, 17:217-223, doi:10.1144/GSL.SP.1984.017.01.15 --- Michel Delaloye and Jean-Jacques Wagner: Ophiolites and volcanic activity near the western edge of the Arabian plate / Geological Society, London, Special Publications, 17:225-233, doi:10.1144/GSL.SP.1984.017.01.16 --- 3. Neotethys: Turkey --- Editor’s introduction / Geological Society, London, Special Publications, 17:235-240, doi:10.1144/GSL.SP.1984.017.01.17 --- A. Poisson: The extension of the Ionian trough into southwestern Turkey / Geological Society, London, Special Publications, 17:241-249, doi:10.1144/GSL.SP.1984.017.01.18 --- A. H. F. Robertson and N. H. Woodcock: The SW segment of the Antalya Complex, Turkey as a Mesozoic-Tertiary Tethyan continental margin / Geological Society, London, Special Publications, 17:251-271, doi:10.1144/GSL.SP.1984.017.01.19 --- J. W. F. Waldron: Structural history of the Antalya Complex in the ‘Isparta angle’, Southwest Turkey / Geological Society, London, Special Publications, 17:273-286, doi:10.1144/GSL.SP.1984.017.01.20 --- A. B. Hayward: Miocene clastic sedimentation related to the emplacement of the Lycian Nappes and the Antalya Complex, S.W. Turkey / Geological Society, London, Special Publications, 17:287-300, doi:10.1144/GSL.SP.1984.017.01.21 --- Hubert Whitechurch, Thierry Juteau, and Raymond Montigny: Role of the Eastern Mediterranean ophiolites (Turkey, Syria, Cyprus) in the history of the Neo-Tethys / Geological Society, London, Special Publications, 17:301-317, doi:10.1144/GSL.SP.1984.017.01.22 --- Ingrid Reuber: Mylonitic ductile shear zones within tectonites and cumulates as evidence for an oceanic transform fault in the Antalya ophiolite, S.W. Turkey / Geological Society, London, Special Publications, 17:319-334, doi:10.1144/GSL.SP.1984.017.01.23 --- Pınar O. Yılmaz: Fossil and K-Ar data for the age of the Antalya complex, S W Turkey / Geological Society, London, Special Publications, 17:335-347, doi:10.1144/GSL.SP.1984.017.01.24 --- L. E. Ricou, J. Marcoux, and H. Whitechurch: The Mesozoic organization of the Taurides: one or several ocean basins? / Geological Society, London, Special Publications, 17:349-359, doi:10.1144/GSL.SP.1984.017.01.25 --- A. Michard, H. Whitechurch, L. E. Ricou, R. Montigny, and E. Yazgan: Tauric subduction (Malatya-Elazıǧ provinces) and its bearing on tectonics of the Tethyan realm in Turkey / Geological Society, London, Special Publications, 17:361-373, doi:10.1144/GSL.SP.1984.017.01.26 --- G. Aktaş and A. H. F. Robertson: The Maden Complex, SE Turkey: evolution of a Neotethyan active margin / Geological Society, London, Special Publications, 17:375-402, doi:10.1144/GSL.SP.1984.017.01.27 --- Cahit Helvaci and William L. Griffin: Rb-Sr geochronology of the Bitlis Massif, Avnik (Bingöl) area, S.E. Turkey / Geological Society, London, Special Publications, 17:403-413, doi:10.1144/GSL.SP.1984.017.01.28 --- Ömer T. Akıncı: The Eastern Pontide volcano-sedimentary belt and associated massive sulphide deposits / Geological Society, London, Special Publications, 17:415-428, doi:10.1144/GSL.SP.1984.017.01.29 --- A. I. Okay and N. Özgül: HP/LT metamorphism and the structure of the Alanya Massif, Southern Turkey: an allochthonous composite tectonic sheet / Geological Society, London, Special Publications, 17:429-439, doi:10.1144/GSL.SP.1984.017.01.30 --- Teoman N. Norman: The role of the Ankara Melange in the development of Anatolia (Turkey) / Geological Society, London, Special Publications, 17:441-447, doi:10.1144/GSL.SP.1984.017.01.31 --- Ayla Tankut: Basic and ultrabasic rocks from the Ankara Melange, Turkey / Geological Society, London, Special Publications, 17:449-454, doi:10.1144/GSL.SP.1984.017.01.32 --- A. I. Okay: Distribution and characteristics of the north-west Turkish blueschists / Geological Society, London, Special Publications, 17:455-466, doi:10.1144/GSL.SP.1984.017.01.33 --- N. Görür, F.Y. Oktay, İ. Seymen, and A. M. C. Şengör: Palaeotectonic evolution of the Tuzgölü basin complex, Central Turkey: sedimentary record of a Neo-Tethyan closure / Geological Society, London, Special Publications, 17:467-482, doi:10.1144/GSL.SP.1984.017.01.34 --- J. P. Lauer: Geodynamic evolution of Turkey and Cyprus based on palaeomagnetic data / Geological Society, London, Special Publications, 17:483-491, doi:10.1144/GSL.SP.1984.017.01.35 --- 4. Neotethys: Greece and the Balkans --- Editor’s introduction / Geological Society, London, Special Publications, 17:493-498, doi:10.1144/GSL.SP.1984.017.01.36 --- Robert Hall, M. G. Audley-Charles, and D. J. Carter: The significance of Crete for the evolution of the Eastern Mediterranean / Geological Society, London, Special Publications, 17:499-516, doi:10.1144/GSL.SP.1984.017.01.37 --- Michel Bonneau: Correlation of the Hellenide nappes in the south-east Aegean and their tectonic reconstruction / Geological Society, London, Special Publications, 17:517-527, doi:10.1144/GSL.SP.1984.017.01.38 --- M. Okrusch, P. Richter
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    Biology of bryophytes (2005)
    New Dehli : New Age International Publishers
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    Call number: AWI Bio-22-94883
    Type of Medium: Monograph available for loan
    Pages: XI, 349 Seiten , Illustrationen
    Edition: Reprint 2005
    ISBN: 0470213590 , 085226240X , 81-224-1343-9
    URL: http://digitale-objekte.hbz-nrw.de/storage/2008/10/23/file_14/2621664.pdf
    Language: English
    Note: Contents Foreword, by Professor Dr. Martin Bopp Preface Acknowledgements 1. EXPERIMENTS ON SPORES AND GEMMAE Spore Germination in Liverwort - Jungermanniales, Marchantiales, Anthocerotales, Sphaerocarpales; Types of Spore Germination in Mosses - Sphagnales, Andreaeales, Tetraphidales, Bryales Factors Affecting Spore Germination - Light, Temperature, Sugars, Minerals, Growth Regulators, Hydrogen-ion concentration (pH), OtheT Factors Mechanism of Spore Germination Experiments on Gemmae - light, Temperature, Humidity and other Physical Factors, Growth Regulators, Nitrogenous Substances, Hydrogen-ion concentration (pH), Other Chemical Factors References 2. PROTONEMAL DIFFERENTIATION AND BUD FORMATION IN MOSSES Protonemal Differentiation Bud Formation Factors Affecting Bud Formation - Light, Temperature, Auxins, Cytokinins, Gibberellins, Adenosine 3', 5'-cyclic monophosphate, Adenine and Amino Acids, Minerals and Chelates Vitamins, Abscisic Acid, Sugars, pH, Influence of Other Organisms References. 3. REGENERATION Potentialities of Various Organs for Regeneration - Regeneration from Leaves, Regeneration from Setae Morphology of Régénérants Factors Affecting Regeneration - Light. Radiation, pH, Season, Humidity. Wounding, Temperature, Size of the Fragment Reserve Food Material. Location in the Plant, Age, Correlative Inhibition. Polarity and Apical Dominance Changes Occurring in Regenerating Cells References 4. REPRODUCTIVE BIOLOGY Factors Affecting Gametangial Induction - Light Duration, Light Level, Light Quality. Temperature, Temperature-Photoperiod Interaction. Humidity. Hydration. Carbohydrates. Nitrogenous Substances, Growth Regulators, Chelating Agents, pH and Other Factors References 5. ALTERNATIVE PATHWAYS IN LIFE CYCLE Apogamy - Occurrence of Apogamy in Diplophase and Haplophase, Spore Production in Apogamous Sporophytes, Differentiation of Apogamous Sporophytes from Callus, Factors Controlling Differentiation of Apogamous Sporophytes: Exogenous Factors, Endogenous Factors, Differentiation of Sporophyte and Gametophyte, Role of Calyptra in Sporogon Development Apospory Callus Formation and its Differentiation - Formation of Callus. Differentiation in Callus Controls in Differentiation Alternation of Generations References 6. PHOTOMORPHOGENESIS Spore Germination - Liverworts, Mosses Growth - Liverworts, Mosses Vegetative Propagation - Liverworts, Mosses Metabolism - Liverworts. Mosses; Senescence Bud Induction in Mosses Tropic Responses - Liverworts, Mosses References. 7. ULTRASTRUCTURAL STUDIES Spore Protonema Stem Leaf Gametangia - Antheridium Gametogenesis - Spermatogenesis, Oogenesis Sporogenesis - Spore Sac or Tapetum. Fluctuation in Plastid Number, Structural Changes in Plastids, Cytoplasm, and Other Organelles. Meiosis. Spore Wall Formation Sporophyte-Ganietophyte Junction Seta Histoenzymological Studies - Localization of Enzymes in the Haustorial Foot References 8. CHEMICAL CONSTITUENTS OF BRYOPHYTES Antibiotics Growth Substances - Specified Growth Substances, Non-specified Growth Substances Lipids - Alkanes, Fatty Acids, Cuticular Components Terpenoids - Monoterpenoids, Sesquiterpenoids, Ditetpenoids, Triterpenoids and Sterols Flavonoids - Flavones, Isoflavones, Flavonols, Dihydrofiavonoids and Biflavonyls, Aurones and Chalcones, Acylated Flavonoids, Anthocyanins and Proanthocyanidins, Sphagnorubins Lignins; Other Constitutents - Carotenoids, Carbohydrates, Organic Acids, Dihydrostilbenes, Enzymes, Amino Acids and Quinones, Inorganic Compounds, Miscellaneous, Antitumour Activities, Allergenic Activities References 9. BRYOPHYTES AS INDICATORS OF POLLUTION Heavy Metals - Lead, Cadmium, Zinc, Mercury, Arsenates, Chromium, Nickel. Vanadium Stability Pattern of Metal Ions Metal Tolerance - Copper Mosses, Peat Mosses Gaseous Pollutants - Sulphur dioxide. Fluorides, Ozone Radionuclides (Radio Isotopes) - Cesium. Strontium, Uranium; Radiations References. 10. PROTOPLAST CULTURE Isolation of Protoplasts - Mechanical Method, Enzymatic Method, Source Material for Protoplasts, Factors Affecting Protoplast Isolation: Culture of Protoplasts—Liquid Culture Agar Plating of Protoplasts: Regeneration of Protoplasts - Factors Affecting Regeneration Protoplast Fusion and Somatic Hybrids Induction and Isolation of Mutants References. 11. CONDUCTION IN BRYOPHYTES External Conduction - Gametophyte. Sporophyte, Significance of External Conduction Internal Conduction - Cells Involved in Conduction, Anatomy of the Horizontal Axis, Midribs and Leaf Traces. Conducting Strand in Seta and Capsule, Development and Structure of Mature Conducting Tissues. The Interphase, Internal Conduction of Water, Conduction of Organic Compounds; Evolutionary Trends in the Conducting Strands References. 12. WATER RELATIONS Absorption and Conduction of Water - Endohydric.' Ectohydric, Myxohydric Water Holding Capacity and Growth Rate Desiccation and Rehydration Mechanism of Damage Growth-Forms References SUBJECT INDEX PLANT INDEX AUTHOR INDEX
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    Počvy alasov Leno-Amginskogo meždureč'ja (1984)
    Jakutsk : Jakutskij Filial SO AN SSSR
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    Call number: AWI G3-22-94893
    Description / Table of Contents: В книге приводится обстоятельная и разносторонняя характеристика основных генетических типов почв аласов. Выявлено влияние термокарстового аласообразования на почвообразовательный процесс. Полученные результаты позволяют рассматривать почвы аласов как самостоятельные типы, возникновение которых связано со своеобразным аласным процессом, присущим, только термокарстовым ландшафтам. Впервые охарактеризованы особенности структуры почвенного покрова аласов и раскрыты причины ее дифференциации . Книга предназначена для почвоведов, мелиораторов, агрохимиков, а также для других специалистов сельского хозяйства и проектных организаций, связанных с использованием и освоением земель в области широкого распространения многалетнемерзлых пород.
    Description / Table of Contents: Translation of the abstract: The book provides a detailed and versatile description of the main genetic types of Alas soils. The influence of thermokarst alas formation on the soil-forming process was revealed. The results obtained allow us to consider alas soils as independent types, the occurrence of which is associated with a peculiar alas process, inherent only in thermokarst landscapes. For the first time the features of the structure of the soil cover of the alas were characterized and the reasons for its differentiation were revealed. The book is intended for soil scientists, land reclamators, agrochemists, as well as for other agricultural specialists and design organizations involved in the use and development of land in the area of ​​widespread permafrost.
    Type of Medium: Monograph available for loan
    Pages: 168 Seiten , Illustrationen
    Language: Russian
    Note: ОГЛАВЛЕНИЕ Введение 3 Глава 1. Природно-климатические условия 1.1. Геология и геоморфология 1.2. Многолетняя мерзлота 1.3. Почвообразующие породы 1.4. Климат 1.5. Поверхностные воды 1.6. Растительность Глава 2. Особенности почвообразования в аласах 2.1. Краткая история исследования почв аласов 2.2. Аласный термокарстовый рельеф 2.3. Влияние аласов на почвообразование 2.4. Аласный тип почвообразования Глава 3. Почвы 3.1. Зональные почвы 3.1.1. Мерзлотные палевые почвы 3.1.2. Мерзлотные палевые осолоделые почвы 3.1 .3. Мерзлотные таежные оподз аленные почвы 3.2. Почвы аласов 3.2.1. Аласные болотные и заболоченные почвы 3.2.2. Аласные луговые почвы 3.2.3. Аласные остепненные почвы Глава 4. Структура почвенного покрова аласов 4.1. Условия дифференциации почвенного покрова аласов 4.2. Структура почвенного покрова различных по рельефу аласов 4.3. Неоднородность почвенного покрова разновозрастных термокарстовых котловин Заключение Список литературы
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  • 91
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    Monograph available for loan
    Stroenie i teplovoj režim merzlych porod (1981)
    Novosibirsk : Izdatel'stvo "Nauka", Sibirskoe otdelenie
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    Call number: AWI G3-22-94892
    Description / Table of Contents: Приводятся новые материалы о составе, льдистости и криогенном строении аллювиальных и склоновых отложений, о диагенетическом минералообразовании в условиях вечной мерзлоты. Делается опыт прогнова изменений минимальных температур сезоннопротаивающего слоя на основе ыявленных 14- и 70-летних циклов колебаний температур вовдуха; рассматриваются особенности прибрежно-шельфовой криолитозоны. В двух статьях содержатся результаты теплобалансовых наблюдений в Центральной Лкутии, особое внимание уделяется рассмотрению теплового потока через дневную поверхность водоема, теплообмена водных масс с донными отложениями. Интересны данные о мощности и температуре многолетнемерзлых толщ, геотермическом градиенте, теплопроводности и тепловом потоке в породах равличных районов Сибири, об особенностях поведения температурного и электрического поля ПС вблизи нижней границы мерзлоты. Сборник представляет интерес для широкого круга специалистов: мерзлотоведов, теплофизиков, географов, строителей.
    Description / Table of Contents: Translation of the abstract: New materials are presented on the composition, ice content and cryogenic structure of alluvial and slope deposits, on diagenetic mineral formation in permafrost conditions. An experiment is made to test the changes in the minimum temperatures of the seasonally thawing layer on the basis of the identified 14- and 70-year cycles of air temperature fluctuations; the features of the coastal-shelf cryolithozone are considered. Two articles contain the results of heat-balance observations in Central Lukutia, special attention is paid to the consideration of the heat flow through the daytime surface of the reservoir, the heat exchange of water masses with bottom sediments. Of interest are the data on the thickness and temperature of permafrost, the geothermal gradient, thermal conductivity, and heat flow in the rocks of various regions of Siberia, and on the behavior of the temperature and electric field of the SL near the lower permafrost boundary. The collection is of interest to a wide range of specialists: permafrost scientists, thermal physicists, geographers, builders.
    Type of Medium: Monograph available for loan
    Pages: 89 Seiten , Illustrationen
    Language: Russian
    Note: СОДЕРЖАНИЕ Криолитологические особенности отложений малых рек в Центральной Якутии / Е.Г. Катасонова, Х.Г. Зигерт Минералообразование в области вечной мерзлоты / Х.Г. Зигерт Криогенное строение склоновых отложений на севере Среднесибирского плоскогорья / В.В. Куницкий Перелетки и основные типы сезонвомерзлых пород / Е.А. Втюрина Особенности прибрежно-шельфовой криолитозоны / А.И. Фартышев Многолетние экстремумы отрицательной температуры грунтов сезоннопротаивающего слоя в Центральной Якутии / П.А. Соловъев, Л.П. Голубых Интенсивность сезонного промерзания почвогрунтов в Заилийском Алатау / Э.В. Северский, М. В. Попов Теплопроводность крупнообломочных грунтов в горах Северного Тянь-Шаня / А. А. Мандаров Тепловой баланс крупного озера и прилегающей территории в Центральной Якутии / А.В. Павлов, М.И. Тишин Геотермические параметры Уренгойского месторождения / А.И. Левченко Теплофизические свойства многолетнемерзлых пород Мастахского месторождения газа / Н.Р. Колушев, В.Т. Балобаев, Р.И. Гаврилъев О некоторых особенностях поведения температурного и электрического поля ПС вблиаи нижней границы мерзлоты в терригенных толщах / В.О. Володько Геотермия вмещающих пород карьера "Мир" (Западная Якутия) / В.Н. Девяткин, Р.И. Гаврилъев Геотермические условия бассейна рек Курунг-Юрях и Хатат (Западная Якутия) / В.Н. Девяткин Тепловой баланс орошаемых посевов кормовых культур в Центральной Якутии / П.Н. Скрябин, О.И. Алексеева Расчет промерзания намывно й насыпи и ее основания / Н.И. Вотякова , In kyrillischer Schrift
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    Biodiversity, ecology and conservation of littoral ecosystems in southeastern Madagascar, Tolagnaro (Fort Dauphin) (2007)
    Washington, DC : Smithsonian Institution
    Details Availability
    Call number: MR 22.94991
    Type of Medium: Monograph available for loan
    Pages: 186, XVI, 187 - 410 Seiten , Illustrationen [zum Teil farbig], graphische Darstellungen, Karten
    ISBN: 978-1893912-00-7
    Series Statement: SI/MAB Series 11
    Language: English
    Note: Sprache der Zusammenfassung: Französisch
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  • 93
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    Monograph available for loan
    SEM petrology atlas (1984)
    Tulsa, Oklahoma : American Ass. of Petroleum Geologists
    Details Availability
    Call number: MR 22.94992
    Type of Medium: Monograph available for loan
    Pages: 237 Seiten , überwiegend Illustrationen, graphische Darstellungen
    ISBN: 0-89181-653-4
    Series Statement: AAPG methods in exploration series 4
    URL: http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=001391560&sequence=000002&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
    Language: English
    Note: INTRODUCTION WHY SEM ANALYSIS? FORMAT SAMPLE PREPARATION HOW THE SEM WORKS THE SEM MICROGRAPH ELEMENTAL ANALYSIS BY SEM EDX ANALYSIS OF MINERALS SILICATES Silica Quartz Cristobalite (Opal-CT) Opal (Opal-A) Feldspars Potassium Feldspar Resorbed Potassium Feldspar Plagioclase Feldspar with K-Feldspar Overgrowths Resorbed Plagioclase Feldspar Clays Chlorite Illite Kaolinite Halloysite Smectite Nontronite Hectorite Illite-smectite Corrensite Glauconite Rectorite Palygorskite Vermiculite Zeolites Analcime Chabazite Clinoptilolite Erionite Heulandite Laumontite Mordenite Phillipsite Thomsonite Yugawaralite Micas Biotite Muscovite Phlogopite Amphiboles Hornblende Actinolite Riebeckite Pyroxenes Augite Hypersthene Others Talc Chrysotile Sphene CARBONATES Calcite Dolomite Ferroan Dolomite/Ankerite Siderite Chalk PHOSPHATES Apatite Collophane Florencite HALIDES Halite SULFIDES Pyrite Sphalerite SULFATES Gypsum Anhydrite Copiapite Melanterite Barite OXIDES Hematite and Goethite Rutile Magnetite llmenite MISCELLANEOUS Wood ENERGY TABLE OF CHARACTERISTIC X-RAY TRANSITIONS GLOSSARY REFERENCES
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    The geology of the Calvinia area : explanation sheet 3118 Calvinia; scale 1:250.000 (2002)
    Pretoria : Council for Geoscience
    Details Availability
    Call number: MR 22.94996
    Type of Medium: Monograph available for loan
    Pages: V, 92 Seiten , zahlreiche Illustrationen, graphische Darstellungen
    ISBN: 1-919908-12-9
    Language: English
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  • 95
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    Monograph available for loan
    Field guide for hydrologic responses to degrading permafrost : August 9-12, 2005 ; University of Alaska Fairbanks (2005)
    Fairbanks : University of Alaska
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    Call number: AWI G3-23-94993
    Type of Medium: Monograph available for loan
    Pages: 24 Seiten , Illustrationen
    Language: English
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  • 96
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    Monograph available for loan
    The cryosphere and global environmental change (2007)
    Malden, Mass. [u.a.] : Blackwell
    Details Availability
    Call number: AWI G3-23-95310
    Type of Medium: Monograph available for loan
    Pages: XVIII, 261 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 140512976X , 1-4051-2976-X , 978-1-4051-2976-3
    Series Statement: Environmental systems and global change series 1
    URL: Inhaltsverzeichnis
    Language: English
    Note: Contents Preface 1 The evidence for cryospheric change 1.1 Introduction 1.2 The geomorphic and hydrologic effects of cryospheric change 1.3 Sub-arctic and alpine hydrology 1.4 Glacier loss and mountain permafrost 1.5 Permafrost 1.6 The carbon balance of the cryosphere 1.7 River and lake ice break-up and freeze-up 1.8 Ocean circulation 1.9 The mass balance of the polar ice sheets 1.10 Sea level 1.11 Importance of sea ice. 1.12 Ecological impacts 1.13 Socio-economic effects 1.14 Conclusions (Text word count-including figure captions and tables but excluding references- 9,015) 2 The monitoring of cryospheric change 2.1 Introduction 2.2 In situ measurements 2.2.1 Land surface air temperature 2.2.2 Terrestrial snow and snow on sea ice 2.2.3 Sea ice 2.2.4 Ice sheets and alpine glaciers 2.2.5 Permafrost and seasonally frozen ground 2.2.6 River runoff 2.2.7 River and lake ice freeze-up and break-up 2.3 Conclusions 3 Processes of cryospheric change 3.1 Introduction 3.2 Snow and ice as energy regulators 3.2.1 The energetics of the snow surface 3.2.2 The energetics of the snowpack 3.2.3 The energetics of glaciers 3.2.4 The energetics of sea ice and various terrain types 3.2.5 Permafrost 3.3 Snow and ice reservoir functions 3.3.1 Mass budget for snow 3.3.2 Mass balance for glacier ice 3.3.3 The mass balance of an ice sheet 3.3.4 Mass balance of sea ice 3.4 Snowfall 3.4.1 Interception by vegetation 3.4.2 Snow accumulation 3.4.3 Snow cover structure 3.5 Snow avalanches 3.6 Snow melt, runoff and streamflow generation 3.7 Snow chemistry 3.8 Snow ecology 3.9 Glacier melt 3.10 Formation of an ice cover 3.11 River and lake ice 3.12 Sediment budgets 4 Patterns of the contemporary cryosphere at local to global scales 4.1 Introduction 4.2 Remote sensing observations 4.3 Land and sea surface temperature 4.3.1 Terrestrial snow and snow on sea ice 4.3.2 Sea ice 4.3.3 Ice sheets & glaciers: estimation of volume 4.3.4 Ice sheets & glaciers: mass balance components 4.3.5 Permafrost 4.3.6 River runoff 4.3.7 River and lake ice freeze-up/break-up 4.4 Numerical Models 4.5 Conclusions: validation, coordinated projects and climate data records 5 The evidence for past cryospheric changes 5.1 Introduction 5.2 The uniqueness of the Quaternary Period 5.3. Initiation of glacial ages 5.4 Reconstructing extent of glacial environments 5.5 Extreme events 5.6 Ice sheet modelling 5.6.1 The Antarctic Ice Sheet 5.6.2 Greenland 5.6.3 North America: Innuitian, Laurentide and Cordilleran ice sheets 5.6.4 British Isles, Scandinavian and Barents ice sheets 5.6.5 The Patagonian and New Zealand ice caps 5.7 Non-glacial Quaternary environments 5.7.1 Late Quaternary permafrost in North America and Europe 5.7.2 Treeline variations 5.7.3 Climatic snowline 5.7.4 Glacier fluctuations 5.7.5 Paraglaciation 6 The transience of the cryosphere and transitional landscapes 6.1 Introduction 6.1.1 The landscape as palimpsest 6.2 Glacial landscapes: macro scale 6.2.1 Cirque landscapes 6.2.2 Fjord and strandflat landscapes 6.3 Periglacial landscapes: macro-scale 6.4 Paraglacial landscapes: macro-scale 6.5 Glacial landscapes: medium-scale 6.5.1 The transition from glacial to fluvial dominance 6.6 Proglacial landscapes: medium-scale 6.6.1 Glacifluvial landforms 6.6.2 The Channeled Scablands 6.6.3 Sub-glacial channels 6.6.4 Sub-glacial, ice-marginal and supraglacial sediment-landform associations 6.7 Periglacial landscapes: medium scale 6.7.1 The transition from periglacial to fluvial dominance 6.8 Paraglacial landscapes: medium-scale 6.9 Glacial landscapes: local-scale 6.9.1 Primary glacigenic deposits 6.9.2 Small scale erosional forms 6.10 Proglacial landscapes: local-scale 6.11 Periglacial landscapes: local scale 6.13 Paraglacial landscapes: local-scale 6.13 Landscape resistance, collapse and recovery 6.14 Transitional landscapes at Quaternary, Holocene and Anthropocene timescales 7 Cryospheric change and vulnerability at Quaternary, Holocene and Anthropocene time scales 7.1 Introduction 7.2 Panarchy 7.2.1 Panarchy, sustainability and transformability 7.2.2 Collapse and the vulnerability of socio-economic systems 7.3 Changing ice cover and biomes since the Last Glacial Maximum 7.3.1 The Last Glacial Maximum 7.3.2 The Holocene Optimum 7.4 The first explorers in North America 7.5 Implications of cryospheric change/collapse 7.5.1 Snow quantity 7.5.2 Snow quality 7.5.3 River and lake ice 7.5.4 Permafrost 7.5.5 Glaciers 7.5.6 River basins 7.5.7 Sea ice 7.5.8 Ice sheets 7.5.9 Sea level change 7.5.10 Carbon sequestration 7.5.11 Vegetation 7.5.12 Polar bears 7.5.13 Human health 7.5.14 Persistent organic pollutants 7.5.15 Socio-cultural conditions and health status 7.5.16 Livelihoods and socio-economic conditions 7.5.17 Governance 7.6 Concluding thoughts References Index
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    Teplovodoobmen v merzlotnych landšaftach Vostočnoj Sibiri i ego faktory (2007)
    Moskva : [Izdatel'stvo "Triada"]
    Details Availability
    Call number: AWI G3-23-95315
    Description / Table of Contents: In the monograph results of long-term ground and remote sensing experimental and theoretical investigations of heat-water exchange of typical permafrost landscapes and small river basins of Eastern Siberia and its factors situated in subarctic tundra, plain taiga and southern mountain taiga are generalized. Detailed maps of landscape structure of range grounds as well as results of analysis of wide range of parameters and variables of permafrost landscapes characterizing spatial and temporal variability of their state in daily, seasonal and long-term scales are presented. Zonal-landscape features of heat and water exchange as well as water regime of small river basins have been revealed. Spatial distribution of vertical turbulent heat and moisture flows in the boundary layer of the atmosphere above heterogeneous surface by measurements from board a plane has been investigated. Spatial and temporal analysis of thermo- and water-physical properties of perennially frozen grounds, which are applied as parameters in hydro-climatic models, has been fulfilled. Processes of interaction of surface and underground waters on plain and in the mountains have been considered, as well as cryogenic phenomena, which have considerable impact upon water regime of rivers and permafrost landscapes.
    Type of Medium: Monograph available for loan
    Pages: 575 Seiten , Illustrationen
    ISBN: 978-5-89658-033-1 , 978-5-94789-232-1
    Language: Russian
    Note: Contents Introduction / A.G. Georgiadi, A.N. Zolotokrylin CHAPTER 1. SUBARCTIC TUNDRA 1.1. Characteristics of subarctic polygon and a complex of field experimental investigations / A.G. Georgiadi 1.2. Landscapes and their characteristics 1.2.1. Types and distribution over territory / R.V. Desyatkin, L.D. Hinzman 1.2.2. Seasonal changes of spectral characteristics of landscapes by data of remote sensing measurements / V.B. Malyshev, N. S. Ozerov 1.3. The active layer of subarctic landscapes: typology and geography 1.3.1. Spatial variabi!ity of the active layer thickness / A.G. Georgiadi, V.G. Onischenko 1.3.2. Hydrophysical characteristics of the seasonal-melting layer / A.G. Georgiadi,V.G. Onischenko 1.4. Radiation and thermal characteristics of landscapes in the summer period 1.4.1. Systematization of experimental information on albedo and surface temperature / A.N. Zolotokrylin 1.4.2. Analysis of experimental information on the surface temperature / A.N. Zolotokrylin, V.V. Vinogradova 1.5. Heat exchange in tundra landscapes 1.5.1. Structure of heat exchange and its seasonal features / A.N. Zolotokrylin 1.5.2. Theoretical analysis of the process of heat transfer in the surface thawed layer of soil grounds / A.B. Kazansky, A.N. Zolotokrylin 1.6. Features of water regime and water exchange in tundra 1.6.1. Water regime and water balance of river basins by results of experimental measurements / A.G. Georgiadi 1.6.2. Interrelationship of underground and surface waters and underground alimentation of rivers in different year seasons / V.V. Shepelev CHAPTER 2. CENTRAL PLAIN TAIGA 2.1. Geographical characteristics of Spasskaya Pad polygon / A.N. Fedorov 2.2. Types of landscapes, their distribution over territory and seasonal dynamics / A.N. Fedorov, Ya. I. Torgovkin, S.P. Varlamov 2.3. Characteristics of the active layer and its physical properties 2.3.1. Spatial and seasonal variability of the active layer thickness 2.3.1.1. Inter-landscape variability of the seasonal-thawing layer thickness / I.S. Vasiliev 2.3.1.2. Variability of the active layer thickness at experimental sites / E.Yu. Gerasimov 2.3.1.3. Freezing of the active layer / P.Ya. Konstantinov 2.3.2. Physical properties of soils of the seasonal-thawing layer under larch forest / A.G. Georgiadi, V.G. Onischenko 2.3.3. Inter-landscape differences of physical properties of the active layer / P.Ya. Konstantinov, I.S. Ugarov, R.N. Argunov 2.3.4. Features of thermal conductivity of soil grounds / V.G. Onischenko, I.S. Lisker, A.G. Georgiadi 2.4. Radiation balance and thermal regime of landscapes 2.4.1. Radiation balance and its components / I.S. Ugarov 2.4.2. Temperature regime of the active layer / P.P. Gavriliev, I.S. Ugarov, P.V. Efremov 2.4.3. Temperature regime of the upper layers of perennially frozen grounds / P.Ya. Konstantinov 2.5.Heat exchange in permafrost landscapes of plain taiga / P.P. Gavriliev 2.6. Features of heat and moisture balance in taiga-alas landscapes / R.V. Desyatkin, I. Ishii, Kh. Yabuki, A.R. Desyatkin, P.P. Fedorov, T.N. Semenova 2.7. Turbulent energy- and moisture exchange in the atmospheric boundary layer (ABL) over thermally heterogeneous surface (over the Lena River lowland in the Yakutsk area) / M.A. Strunin 2.7.1. Some aspects of the atmospheric boundary layer (ABL) observations using the aircraft laboratory 2.7.2. Aircraft experiment of the atmospheric boundary layer (ABL) observations in the Yakutsk area 2.7.2.1. Aicraft laboratory IL-18d and its instruments for investigations of ABL 2.7.2.2. Scheme and conditions of the aircraft experiment 2.7.2.3. Radiosounding, surface measurements and satellite observations 2.7.2.4. Turbulence and turbulent fluxes data processing and analyzing 2.7.3. Some features of the convective boundary layer (CBL) development over thermally heterogeneous surface 2.7.3.1. Seasonal variability of turbulent fluxes 2.7.3.2. Fine spatial ABL structure 2.7.3.3. Conditions of appearance and development of the mesoscale thermal internal boundary layer (MTIBL) inside the CBL 2.7.3.4. Appearance of the local circulation over thermal mesoscale patch on the underlying surface 2.7.3.5. The local circulation and the problem of energy balance in the atmospheric boundary layer 2.7.3.6. Conditions of applying the scaling models for the CBL developing over heterogeneous underlying surface 2.7.3.7. The spectral structure of fluxes 2.7.3.8. Flux separating into turbulent and mesoscale portions 2.7.3.9. Separating approach models for mesoscale and turbulent fluxes in the CBL 2.7.3.10. Some f eatures of mesoscale and turbulent fluxes seasonal variations 2.7.4. The main results of observations of the CBL, developing over the thermally heterogeneous surface 2.8 Moisture exchange in plain taiga landscape 2.8.1. Moisture regime of the active layer 2.8.1.1. Landscape features of moisture dynamics of the active layer / P.P. Gavriliev, I.S. Ugarov, P.V. Efremov, R.N. Argunov 2.8.1.2. Spatial and temporal distribution of moisture reserves in the active layer / A.N. Fedorov, Ya.I.Torgovkin, R.N. Arguniov, P.P. Gavriliev, I.S. Vasiliev, J.S. Ugarov, P.V. Efremov 2.8.2. Interrelationship of underground and surface waters and underground alimentation of rivers in different seasons / V.V. Shepelev CHAPTER 3. SOUTHERN MOUNTAIN TAIGA 3.1. Natural conditions of the region / V.S. Vuglinsky, M.L. Markov 3.1.1. Climate 3.1.2. Relief and geological structure 3.1.3. Permafrost and hydrogeological conditions 3.1.4. Hydrography and hydrological conditions 3.1.5. Interrelationship of surface and underground waters, underground alimentation of rivers 3.1.5.1. lntraannual dynamics of water exchange of rivers with drained aquifers 3.1.5.2. Seasonal glaciation and its impact upon formation of river runoff 3.2. Results of study of regularities of heat- and moisture exchange at an experimental SHI Mogot polygon / N.G. Vasilenko, S.A. Zhuravin 3.2.1. General characteristics of the Mogot polygon and program of investigations 3.2.2. Landscape and soil characteristics of catchments of the Mogot polygon 3.2.2.1. Landscapes of the Mogot polygon 3.2.2.2. Landscape-hydrology complexes 3.2.2.3. Types of soils and their water physical characteristics 3.2.3. Features of climate in the region of the Mogot polygon 3.2.4. Radiation and heat balances 3.2.4.1. Radiation balance 3.2.4.2. Heat balance 3.2.5. Water balance 3.2.5.1. Methods of identification of the main components of water balance 3.2.5.2. Features of fo rmation of water balance elements 3.2.5.3. Results of calculation of water balances List of literature SUPPLEMENT TO PART 2.7. INSTRUMENTS AND METHODS FOR INVESTIGATION OF THE ATMOSPHERE USING THE AIRCRAFT LABORATORY / M.A. Strunin S.2.7.1. Methods of wind speed and direction, air temperature and humidity and turbulence measurements based on aircraft data S.2.7.2. Aircraft laboratory IL-18d and its instruments for investigation of the atmosphere S.2.7.3. Database of aircraft observations and preliminary data processing S.2.7.4. Errors of turbulent fluxes calculations based on aircraft data S.2.7.5. Methods of spectral analysis of turbulence data S.2.7.6. Calculations of spectral characteristics of fluctuations based on Fourier analysis S.2.7.7. Using the wavelet-transformations for the spectral analysis List of literature to Supplement 2.7 , In kyrillischer Schrift , Einführung und Inhaltsverzeichnis in englischer Sprache
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    Proceedings of the International Workshop on Physics of Active Fault : 26 - 27 Feb., 2002, Tsukuba, Japan , NIED (2009)
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    The history of econometric ideas (2003)
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