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  • 1
    Series available for loan
    Series available for loan
    Boulder : The Geological Society of America
    Associated volumes
    Call number: S 90.0095(265)
    In: Special paper
    Type of Medium: Series available for loan
    Pages: VI, 309 S.
    ISBN: 0813722659
    Series Statement: Special paper / Geological Society of America 265
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Macmillan
    Call number: M 95.0691
    Type of Medium: Monograph available for loan
    Pages: vii, 304 S.
    ISBN: 0023788119
    Classification:
    Applied Geology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Call number: SR 90.0002(1538-M)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, M-18 S. + 3 pl.
    Series Statement: U.S. Geological Survey professional paper 1538-M
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    New York : Springer
    Call number: PIK N 531-19-92656
    Description / Table of Contents: In this book, plant biology is considered from the perspective of plants and their surrounding environment, including both biotic and abiotic interactions. The intended audience is undergraduate students in the middle or final phases of their programs of study. Topics are developed to provide a rudimentary understanding of how plant-environment interactions span multiple spatiotemporal scales, and how this rudimentary knowledge can be applied to understand the causes of ecosystem vulnerabilities in the face of global climate change and expansion of natural resource use by human societies. In all chapters connections are made from smaller to larger scales of ecological organization, providing a foundation for understanding plant ecology. Where relevant, environmental threats to ecological systems are identified and future research needs are discussed. As future generations take on the responsibility for managing ecosystem goods and services, one of the most effective resources that can be passed on is accumulated knowledge of how organisms, populations, species, communities and ecosystems function and interact across scales of organization. This book is intended to provide some of that knowledge, and hopefully provide those generations with the ability to avoid some of the catastrophic environmental mistakes that prior generations have made.--
    Type of Medium: Monograph available for loan
    Pages: XXIII, 659 Seiten , Illustrationen, Diagramme, Tabellen , 24 cm
    ISBN: 9781461475002
    Series Statement: The plant sciences 8
    Language: English
    Note: Contents: Plant-environment interactions across multiple scales -- Plant biodiversity and population dynamics -- Assembly of plant communities -- Plant pollination and dispersal -- Plant phenotypic expression in variable environments -- Evolutionary ecology of chemically mediated plant-insect interactions -- Plant-microbe interactions -- Patterns and controls of terrestrial primary production in a changing world -- Ecology of tropical rain forests -- Ecology of temperate forests -- Plants in deserts -- Plants in alpine environmnets -- Plants in arctic environments -- Grassland ecology -- Coastal wetland ecology and challenges for environmental management -- Near-coastal seagrass ecosystem -- Ecology of marine phytoplankton -- Plants in changing environmental conditions of the anthropocene -- Plant influences on atmospheric chemistry -- Biofuel development from cellulosic sources -- Plant ecology and sustainability science
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Call number: ZSP-201-90/9
    In: CRREL Report, 90-9
    Description / Table of Contents: In 1986, a mobility model was developed for predicting the traction and motion resistance of both wheeled and tracked vehicles on shallow snow, and a winter field season was dedicated to gathering mobility data for a diverse family of vehicles (including four on wheels and three tracked) to validate the model. The original version of the model, SSM 1.0, used the Mohr-Coulomb shear failure equation from soil mechanics to predict gross traction. This required input of the snow strength parameters c and ȹ. Motion resistance is predicted by calculating the amount of work done by the tire in compacting snow and only requires snow depth and density values as input snow properties. Some effort was expended in determining an easy and reliable method of obtaining snow strength established from past instrumented vehicle test results. Historically, shear annulus apparati have been used to obtain Mohr-Coulomb strength parameters. A comparison of snow strength obtained via these three methods (shear annulus, instrumented vehicle, calculated from initial density using the relationship in SSM 1.0) for individual snow covers showed no agreement. SSM 1.0 assumed that snow strength parameters for mobility prediction were a function of initial snow density; however, traction is developed in the compacted snow under the driving element, whose strength properties bore little relation to those of the initial snow. It appears that the shear strength of the compacted snow is essentially a constant for all of the vehicles and snow covers tested here. Based on this finding, a new traction algorithm was developed, resulting in the creation of a second generation model, SSM 2.0. This algorithm predicts gross traction, on the average for the vehicles tested, within 7% of the measured value. Motion resistance prediction remains unchanged in SSM 2.0. This quantity is still not predicted with a desirable level of accuracy.
    Type of Medium: Series available for loan
    Pages: v, 72 Seiten , Illustrationen
    Series Statement: CRREL Report 90-9
    Language: English
    Note: CONTENTS Preface Nomenclature Introduction Background Field experiments Test location and test sites Test vehicles Test procedures Results CIV traction and motion resistance Wheels/trackcs vehicles traction and motion resistance Shear annulus device Accuracy and limitations of data Snow conditons Analysis Determination of snow strength parameters Traction analysis Traction model predictions Resistance analysis Resistance model predictions Conclusions and recommendations Literature cited Appendix A: Shallow snow mobility model, version 1.0 Appendix B: Test vehicle data Appendix C : Selected test data Appendix D : Snow data Appendix E: Shallow snow mobility model code, version 2.0 Abstract
    Location: AWI Archive
    Branch Library: AWI Library
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  • 6
    Call number: SR 90.0001(2000-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, E-40 S.
    Series Statement: U.S. Geological Survey bulletin 2000-E
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 7
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-264
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Physical properties of ice fog. - Mie scattering computations. - Results. - Literature cited.
    Description / Table of Contents: Ice-fog crystals consisting of many spherical particles, and some hexagonal plates and columns, were observed at ambient temperatures of about -40°C in the Fairbanks, Alaska area during mid-winter. The concentrations and the size distributions of the ice-fog crystals were measured. The attenuation and backscattering of infrared radiation by ice-fog crystals were computed for optical wavelengths of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My] using the Mie theory. The minimum attenuation coefficients and backscattering functions of ice fog were found to be at 9.7[My] wavelength in the observed wavelengths. Optical attenuation coefficients and volume backscattering functions of water fogs were also computed using the Mie theory. The minimum attenuation coefficients and backscattering functions of water fog were found to be at 10.9[My] wavelength in the region of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My]. Both the attenuation coefficients and backscattering functions of ice fog are within the same order of magnitude as water fog for equivalent fog concentrations and wavelengths.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 264
    Language: English
    Branch Library: AWI Library
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  • 8
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1271-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, B-14 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1271-B
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 9
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1211-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, A-13 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1211-A
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 10
    Call number: SR 90.0001(1787-W)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, W-25 S.
    Series Statement: U.S. Geological Survey bulletin 1787-W
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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