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  • 2020-2023
  • 1980-1984  (85)
  • 1975-1979  (346,520)
  • 1935-1939  (6)
  • 1979  (183,583)
  • 1975  (163,003)
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  • 1
    Call number: ZSP-SCAR-570-1
    In: Report to SCAR on Antarctic research activities of Germany (FRG), 1
    Type of Medium: Series available for loan
    Pages: 21 Seiten
    ISSN: 0179-0072
    Series Statement: Report to SCAR on Antarctic research activities of Germany (FRG) 1
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research of the Federal Republic of Germany. - Introduction. - Station. - Field Activities 1974-1979. - Planned Activities 1979/80. - References.
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  • 2
    Call number: MOP 41424 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 31 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 3
    Call number: MOP 44901 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 218 Seiten
    Edition: 19., völlig überarbeitete Auflage
    Language: German
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  • 4
    Monograph available for loan
    Monograph available for loan
    Stroudsburg : Dowden, Hutchinson & Ross
    Associated volumes
    Call number: G 8115
    In: Benchmark papers in geology
    Type of Medium: Monograph available for loan
    Pages: XV, 468 Seiten , Illustrationen
    ISBN: 0-471-13540-2
    Series Statement: Benchmark papers in geology 15
    Language: English
    Location: Upper compact magazine
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  • 5
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/13
    In: CRREL Report, 79-13
    Description / Table of Contents: Heat transfer in turbulent flow was measured in a rectangular channel with a width of 0.254 m and a flow depth of 0.0254 m. Correlations between the Nusselt and Reynolds numbers are given for a range of 3020 Re 22360. A Prandtl number range of 9.90 or = Pr or = 12.28 for water was used in the tests. The results are compared with those of other investigations and show that some well-known correlations underpredict the heat transfer by about 35%.
    Type of Medium: Series available for loan
    Pages: ii, 5 Seiten , Illustrationen
    Series Statement: CRREL Report 79-13
    Language: English
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  • 6
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/10
    In: CRREL Report, 79-10
    Description / Table of Contents: Ice cores from Byrd Station and Little America V have been used to test an ultrasonic technique for evaluating crystal anisotropy in the Antarctic Ice Sheet. P-wave velocities measured parallel and perpendicular to the vertical axes of cores from the 2164-m-thick ice sheet at Byrd Station have yielded results in excellent agreement with the observed c-axis fabric profile and with the in-situ P-wave velocity profile measured parallel to the bore hole axis. Velocity differences in excess of 140 m/s for core samples from deeper than 1300 m attest to the strong single pole clustering of crystallographic c-axes about the vertical, especially in the zone from 1300-1800 m. Such oriented structure is compatible only with strong horizontal shearing in this zone. The existence in an ice sheet of widespread shearing several hundred meters above its bed raises serious questions as to the validity of current concepts of the flow of large ice masses that tend to gloss over or ignore crystal alignments of this magnitude.
    Type of Medium: Series available for loan
    Pages: IV, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 79-10
    Language: English
    Note: CONTENTS Abstract Preface Introduction Laboratory measurements Sample sources Ultrasonic velocity measurements Effects of inclined drilling at Byrd Station Results Byrd Station Little America V Summary and conclusions Literature cited
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  • 7
    Monograph available for loan
    Monograph available for loan
    Braunschweig : Westermann
    Call number: MOP 44380 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 162 Seiten , 9 graphische Darstellungen, Karten
    Series Statement: Das geographische Seminar
    Language: German
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  • 8
    Call number: MOP 44808 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 152 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 9
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill Book Company
    Call number: MOP 44210 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XV, 523 Seiten , graphische Darstellungen
    ISBN: 978-0-070-56042-0
    Language: English
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  • 10
    Call number: AWI A3-20-93434
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 1
    Type of Medium: Series available for loan
    Pages: 121 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,1
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 11
    Call number: MOP 45557 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 221 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 12
    Call number: MOP 43837 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 64 Seiten
    Series Statement: Agra-buch Empfehlungen für die Praxis
    Language: German
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  • 13
    Monograph available for loan
    Monograph available for loan
    Leipzig : VEB Deutscher Verlag für Grundstoffindustrie
    Associated volumes
    Call number: MOP 43711 / Mitte
    In: Technik und Umweltschutz : Luft, Wasser, Boden, Lärm, 10
    Type of Medium: Monograph available for loan
    Pages: 172 Seiten
    Edition: 1. Auflage
    Series Statement: Technik und Umweltschutz : Luft, Wasser, Boden, Lärm 10
    Language: German
    Note: Inhaltsverzeichnis Die Rolle des sozialistischen Rechts im Prozeß der planmäßigen Gestaltung einer sozialistischen Landeskultur unter Mitwirkung gesellschaftlicher Kräfte / Günther Boccarius 1. Das sozialistische Recht als Hauptmethode der staatlichen Leitung 2. Die Erhöhung der Wirksamkeit des sozialistischen Rechts ; wichtige Voraussetzung für die planmäßige Gestaltung der sozialistischen Landeskultur 3. Die Entwicklung einer sozialistischen Gemeinschaftsarbeit zwischen Staatsorganen, Betrieben, Kombinaten, staatlichen Einrichtungen und gesellschaftlichen Kräften des Territoriums - unentbehrliches Element der planmäßigen und effektiven Gestaltung der sozialistischen Landeskultur 4. Zusammenfassung 5. Quellenangaben HEINZ WERNER Die Eindämmung von Staub und Lärm beim Umschlag und Transport fester Brennstoffe, ein wichtiger Beitrag zur Verbesserung des Umweltschutzes / Heinz Werner 1. Einleitung 2. Aufgaben des VEB Kohlehandels 3. Umweltprobleme im Kohlehandel 4. Lösungswege zur Verminderung von Staub und Lärm 4.1. Leitungs- und Planungsprozeß 4.2. Technisch-organisatorische Maßnahmen 4.3. Entwicklungskonzeption 5. Schlußfolgerungen 6. Zusammenfassung Übersicht über das Produktionsprogramm des VEB Entstaubungstechnik "Edgar André", Magdeburg, unter Berücksichtigung der perspektivischen Aufgaben des Betriebes / Gerhard Nindelt und Ulf Richter 1. Einleitung 2. Grundlagen der Entstaubungstechnik 3. Verschiedene Entstaubungsapparate 4. Typische Anwendungsfälle 5. Entwicklungstendenzen 5.1. Anlagengrößen 5.2. Verfahrenstechnik 5.3. Investitionsgeschehen 6. Aufgaben des VEB Entstaubungstechnik zur Erzielung der Anwenderforderungen 7. Zusammenfassung 8. Quellenangaben Aufbau, Inhalt und Form der Ausrüstungs-und Berechnungskataloge der Luft-und Kältetechnik, speziell der Entstaubungstechnik / Fritz Hockun 1. Einleitung 2. Ergebnisse der Analyse der Projektierungstätigkeit 3. Darstellung des Projektierungskataloges "Entstaubungstechnik" 3.1. Forderungen an Projektierungskataloge 3.2. Inhalt des Ausrüstungskataloges "Entstaubungstechnik" 3.3. Inhalt des Berechnungskataloges "Entstaubungstechnik" 3.4. Inhalt des Programmkataloges "Entstaubungstechnik" 4. Schlußfolgerungen 5. Zusammenfassung Lufthygienische Probleme in petrolchemischen Anlagen / Erhard Kaufmann, Lothar Eremit und Herbert Mohry 1. Einleitung 2. Petrolchemische Ausgangs-, Zwischen- und Endprodukte 2.1. Aufzählung und Darstellung der Wertsteigerung 2.2. Wichtige petrolchemische Ausgangsprodukte 2.3. Petrolchemische Reaktionen 2.3.1. Ungesättigte Kohlenwasserstoffe 2.3.2. Aromatische Kohlenwasserstoffe 2.3.3. Gesättigte Kohlenwasserstoffe 3. Petrolchemische Verfahren der DDR 3.1. Allgemeines 3.2. Technologie und Emissionen petrolchemischer Anlagen der DDR 3.2.1. Äthyleneneugung 3.2.2. Polyäthylenerzeugung 3.2.3. Butadieriextraktion 3.2.4. Acrylnitrilerzeugung 3.2.5. Terephtalsäureerzeugung 3.2.6, Kalkammonsalpetererzeugung 4. Zusammenfassung 5. Quellenangabe Lufthygienische Aspekte beim Erdgaseinsatz im Bezirk Magdeburg / Alfred Hellwig und Reinhard Hiller 1. Einleitung 2. Senkung der Schwefeldioxidemission durch Erdgaseinsatz im Bezirk Magdeburg 2.1. Methodik der Ermittlung 2.2. Berechnungsergebnisse 2.2.1. Territoriale Schwerpunkte 2.2.2. Verhältnis Emission-Immission 3. Stickoxidemission erdgasgefeuerter Anlagen 3.1. Chemismus der Bildung der Stickoxide 3.2. Quellen der Stickoxide 3.3. Berechnung der Stickoxide 3.3.1. Formel nach I. J. Sigal 3.3.2. Praktische Erfahrungen mit der Formel von I. J. Sigal 3.4.NOx-Emissionsmessungen an ausgewählten Dampferzeugern 4.4.Schlußfolgerungen 5. Zusammenfassung 6. Quellenangaben Luftreinhaltung und Gesundheitsschutz in der DDR / Karlwilhelm Horn, Armin Knauer und Peter Loderitz 1. Einleitung 2. Aufgaben der Kommunalhygiene 3. Anwendung von Begrenzungsvorschriften 4. Epidemiologische Untersuchungen 5. Soziologische Studien 6. Zusammenfassung Krebsverhütung durch Umweltschutz / Tilo Schramm Theoretische und experimentelle Grundlagen für Maßnahmen zur primären Krebsprophylaxe 1. Krebsursachen bei Mensch und Tier 2. Chemische Karzinogene als Krebsursache 3. Wirkungsweisen chemischer Karzinogene 4. Zur Frage der Irreversibilität der Wirkungen chemischer Karzinogene 5. Möglichkeiten zum Nachweis karzinogener Eigenschaften chemischer Substanzen 6. Zusammenfassung 7. Quellenangaben Notwendigkeit und Aufgabenstellung der präventiven Krebsforschung / Wolfgang Gibel 1. Einleitung 2. Neue Kenntnisse über kanzerogene Umweltfaktoren 3. Vordringliche Aufgaben der präventiven Onkologie 4. Zusammenfassung 5. Quellenangaben Neuere Ergebnisse zur umweltbedingten Kontamination von Lebensmitteln mit krebserregenden Kohlenwasserstoffen / Walter Fritz und Rudolf Engst 1. Einleitung 2. Methodik 3. Ergebnisse 3.1. Bodenkontamination 3.2. Kontamination von Erntegütern 3.3. Übergang aus kontaminierten Böden in Erntegüter 3.4. Übergang aus kontaminiertem Boden in Trinkwasser 4. Schlußfolgerungen 5. Zusammenfassung 6. Quellenangaben
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  • 14
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: MOP 44941 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 24 Seiten
    Language: English
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  • 15
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/29
    In: CRREL Report, 79-29
    Description / Table of Contents: An analytical study of the propagation of shock waves in snow was carried out to evaluate the response of medium density snow to high rates of loading. One solution was developed for steady shock waves; this resulted in calculation of pressure jump, density jump and stress wave speed. Correlation with available experimental data was found to be good. Nonsteady shock waves were also considered in order to evaluate wave attenuation rates in snow. Very few data were available to compare with the analytical results, so no definite conclusions on the part of the study could be made. The results show, however, that shock waves that produce plastic deformation attenuate at extremely high rates and that differences in pressure between two waves are quickly eliminated within a short distance. Calculations were also made to evaluate the effect of wave frequency on attenuation rates. The results show that, for plastic waves, frequency is not a predominant factor for determining attenuation rates.
    Type of Medium: Series available for loan
    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-29
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature I. Introduction II. A constitutive law for snow and balance principles III. Compatibility laws and jump equations for stress waves IV. Steady shock waves in snow V. Comparison of steady-wave theory with experimental results VI. A numerical solution to the nonsteady wave problem VII. Jump equations for nonsteady shock waves VIII. Reduced jump equations Discussion and conclusions Literature cited
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  • 16
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/28
    In: CRREL Report, 79-28
    Description / Table of Contents: Transmission and scanning electron micrographs of Umiat bentonite revealed thin, mica-like grains with irregular shapes. Most of the bentonite showed electron diffraction ring patterns, but some showed hexagonal net patterns as well as ring patterns. The lengths of the unit cells were calculated to be 5.18 A along the a-axis and 8.97 A along the b-axis. Semiquantitative analyses were made using an energy dispersive spectrometer. Common elements such as Si, Ti, Al, Fe, Mg, Na and K were determined. The molecular ratio of SiO2:Al2O3 was calculated to be 492:100 for the bulk sample, indicating that Umiat bentonite is similar in most respects to Wyoming bentonite, and is classified as a mont-morillonite. The microstructure of frozen Umiat bentonite was observed at a specimen temperature of -100 C using a scanning electron microscope equipped with a cold stage. Frozen bentonite and segregated ice patterns formed from wet bentonite were examined using an X-ray map and Si X-ray line scan. Sublimation processes of ice in the frozen bentonite were observed at specimen temperatures of -60 and -80 C. After sublimation of the ice the bentonite displayed a honeycomb structure. It was concluded that the freezing-sublimation cycle in frozen soil increases the permeability of water vapor due to the three-dimensional structure of the coagulated clay formed by freezing.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-28
    Language: English
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  • 17
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/25
    In: CRREL Report, 79-25
    In: Charged dislocation in ice, I.
    Description / Table of Contents: The motion of dislocations in single crystal ice under an electric field was observed by using X-ray topographic methods. Electric charge density on these dislocations was deduced from the amplitude and length of the dislocation segment under the known AC electrical field. The most likely linear charge density was about +5x10^-11 c/m, although considerable variation is possible depending on the effective field acting on the dislocation lines.
    Type of Medium: Series available for loan
    Pages: iii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-25
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theory Experimental apparatus and procedure Results Discussion Concluding remarks Selected bibliography Appendix A. Mosotti type field on core of cylindrical cavity
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/24
    In: CRREL Report, 79-24
    Description / Table of Contents: By using a new thermocoring technique, a hole was successfully drilled through the 416-m thickness of the Ross Ice Shelf at J-9 Camp. This report provides a description of the drill and an account of this drilling project. A provisional examination of the core shows the ice shelf to consist of 410 m of snow and glacial ice underlain by 6 m of sea ice formed by direct freezing of sea water to the bottom of the Ross Ice Shelf.
    Type of Medium: Series available for loan
    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-24
    Language: English
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  • 19
    Call number: ZSP-201-79/23
    In: CRREL Report, 79-23
    Description / Table of Contents: The performance of surface impedance and magnetic induction electromagnetic subsurface exploration techniques was studied seasonally at various sites in Alaska where permafrost and massive ground ice occurred. The surface impedance method, which uses radiowaves in the LF and VLF bands, and the magnetic induction method, which uses low-frequency magnetic induction fields, distinguish subsurface materials by the electrical resistivity of the materials. The methods used have greatest sensitivity within about 20 m of the surface and are, therefore, most applicable for shallow subsurface investigations. The selection of study sites was based on anticipated contrasts in electrical resistivity between ground ice and adjacent earth materials. A magnetic induction instrument, using a separation of 3.66-m between the transmitter and receiver antennas, in general was able to detect near-surface zones of massive ice and to provide data regarding permafrost distribution in both the Fairbanks and Prudhoe Bay areas. At this antenna separation, the depth of magnetic field penetration was sufficient to include mainly the zone containing maximum contrasts in resistivity between ground ice and other earth materials. In the Fairbanks area, contrasts, in this zone were greatest in late winter when the seasonally thawed surface layer was completely frozen. When thawed, this layer usually becomes more conductive and often masks the deeper resistivity contrasts. In the Prudhoe Bay area, maximum ground resistivity contrasts were detected in late summer when shallow subsurface temperatures had risen sufficiently to permit resistivity contrasts between the massive ice and the ice-rich ground to appear.
    Type of Medium: Series available for loan
    Pages: v, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 79-23
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Obiectives and procedures Ground electrical resistivity in permafrost regions Electromagnetic techniques General Magnetic induction method Surface impedance fradiowave method Direct current method General description of field sites Results Site 1 CRREL permafrost station, Fairbanks, Alaska Site 2 Planned road cut for Steese Highway near Fox, Alaska Site 3 Relic floodplain near Fairbanks, Alaska Site 4 Pingos, Prudhoe Bay, Alaska Site 5 Ice wedges, Prudhoe Bay, Alaska Comparisons between the surface impedance and magnetic induction methods Conclusions and recommendations Literature cited Appendix A. Discussion of the depth of sensitivity of the magnetic induction method using two- and three-layer apparent resistivity curves
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  • 20
    Call number: MOP 46654 / Mitte
    In: World weather program : plan for fiscal year, 1980 and 1981
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    Language: English
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  • 21
    Call number: MOP 42980 / Mitte
    Type of Medium: Monograph available for loan
    Language: English
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/27
    In: CRREL Report, 79-27
    Description / Table of Contents: Some Bessel function identities found by solving problems of the deflection of a floating ice plate by two different methods are rigorously proved. The master formulas from which all the identities are derived are in a Fourier reciprocal relationship, connecting a Hankel function to an exponential function. Many new formulas can be derived from the master formulas. The analytical method presented here now opens the way to study a hitherto impossible type of problem--the deflection of floating elastic plates of various shapes and boundary conditions.
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    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 79-27
    Language: English
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  • 23
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/26
    In: CRREL Report, 79-26
    Description / Table of Contents: A 19-year record of the annual closing and opening dates of operation of the Lake Champlain ferry at Grand Isle, Vermont, which are controlled by the lake's ice cover, was made available to CRREL. These navigation records accurately approximated the freeze-over and breakup dates for the ferry crossing area between Gordon Landing, Vermont, and Cumberland Head, New York. When compared statistically with water temperature and climatological data for the same years at nearby Lake Champlain locations, the dates allowed accurate predictions of ice formation. From nearby air temperature records, cumulative freezing degree-day (deg C) curves were plotted for each year of record, and ice formation dates and standard deviations were predicted with considerable accuracy. Several methods of predicting ice formation on Lake Champlain were attempted. The most accurate approach used a combination of water temperatures and freezing degree-days. The influence of wind speed on ice cover formation and prediction are also discussed in the report.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Data tabulation and collection Air temperatures 11-reezing degree-days Water temperatures Closing and opening dates Results Air temperature Freezing degree-days Water temperatures Analysis: Attempted methods of predicting ice formation Predicting air temperatures 8Summer water temperatures Fall water temperatures and freezing degree-days Wind speed influence on closing of the lake Water temperature vs surface air temperature analysis Prediction of ice-out dates Conclusions Literature cited Appendix A. Freezing degree-day curves with ice notations and watertemperature notations Appendix B. Summary
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  • 24
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Plenum Press
    Call number: 9790
    Type of Medium: Monograph available for loan
    Pages: XV, 508 Seiten , Illustrationen
    ISBN: 0306307391
    Language: English
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  • 25
    Monograph available for loan
    Monograph available for loan
    Leipzig : Akademische Verlagsgesellschaft Geest u. Portig
    Associated volumes
    Call number: 11539
    In: Technisch-physikalische Monographien
    Type of Medium: Monograph available for loan
    Pages: 467 Seiten , Illustrationen , 22 cm
    Edition: 1. Aufl
    Series Statement: Technisch-physikalische Monographien 37
    Language: Undetermined
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  • 26
    Call number: AWI G3-22-94980
    In: Bochumer geographische Arbeiten, 35
    Type of Medium: Series available for loan
    Pages: XI, 211 Seiten , Illustrationen
    ISBN: 3-506-71215-2
    Series Statement: Bochumer geographische Arbeiten 35
    Language: German
    Note: Zugleich: Dissertation, Ruhr-Universität Bochum, 1978 , lnhal tsverzeichnis Verzeichnis der Abbildungen Verzeichnis der tabellarischen Übersichten 1. Einleitung 1.1 Terminologische Fragen 2. Die bisherige Diskussion um die Definition des Periglaziarbegriffes 3. Einführung in die Problematik und Schwerpunkte dieser Untersuchung 3.1 Unterschiedliche Definitionsansätze 3.2 Das Problem aus geographischer Sicht 3.3 Das Problem aus palaoqeographisch-geologischer Sicht 3.4 Schwerpunkte und Arbeitsweise der weiteren Untersuchung 4. Die Einflußnahme periglaziärer Milieufaktoren im Überblick 4.1 Direkt- und indirekt-klimatische Steuerungsfaktoren 4.2 Aklimatische Steuerunqsfaktoren 5. Klimatische und geographische Bodenqefrornistypen 5.1 Dauerfrostboden mit jahreszeitlicher Auftauschicht 5.1.1 Terminologische Fragen und die räumliche Gliederung des Dauerfrostbodens 5.1.2 Die thermische Vertikalqliederung des oberflächennahen Dauerfrostbodens 5.1.3 Zur Verbreitung und klimatischen Abgrenzung des Dauerfrostbodens 5.2 Jahreszeitliche Bodengefrornis 5.3 Tageszeitliche und kurzperiodische Bodengefrornis 5.4 Kammeis 6. Analyse der Bildung, Verbreitung und Differenzierunq wichtiger rezenter Periglaziarerscheinungen und Bewertung ihrer Verwendbarkeit als Definitionskriterien des Periglaziärs 6.1 Periglaziäre Prozesse und periglaziäre Formen im engeren Sinne (Periglaziäre Mikroformung) 6.1.1 Formen der Bodenmusterung ohne Detritussortierung (Texturböden) 6.1.1.1 Kongelikontraktionsformen mit Spalteneis (Eiskeilpolygone) 6.1.1.2 Kongelikontraktionsformen ohne Spalteneis (Sandkeilpolygone) 6.1.1.3 Frostspaltenmakropolygone und Mollisolfrostkeile 6.1.1.4 Spaltenmikropolygone ('Zellenböden') 6.1.1.5 Erdbülten (Thufur) 6.1.1.6 Nichtsortierte Feinerdekreise (Mudpits) 6.1. 2 Frost- und Eishügelformen 6.1.2.1 Saisonale Frosthügel 6.1.2.2 Palsas 6.1.2.3 Pingos und pingoähnliche Formen 6.1.3 Strangmoore 6.1.4 Formen der Bodenmusterung mit Detritussortierung (Strukturböden) 6.1.5 Periglaziär-denudative Prozesse und Formen im engeren Sinne - Kleinformen der Gelisolifluktion 6.1. 5.1 Erscheinungen der amorphen Gelisolifluktion 6.1.5.2 Kleinformen der differenzierten Gelisolifluktion 6.1.5.3 Zusammenfassung und Ergebnisse 6.1.6 Blockgletscher 6.1.7 Vorgänge und Formen der Nivation und Kryoplanation 6.1.8 Dauerfrostboden-Degradation und Depergelationsformen 6.1.8.1 Depergelationsformen infolge vertikaler Dauerfrostboden-Degradation 6.1.8.2 Depergelationsformen infolge lateraler Dauerfrostboden-Degradation 6.2 Periglaziäre Prozesse und Formen im weiteren Sinne (Periglaziäre Meso- und Makroformung) 6.3 Zusammenfassung der klimageomorphologischen Leitformenwerte 7. Zur räumlichen Abgrenzung und regionalen Differenzierung der periglaziären Zone und Höhenstufe - planetarischer und hypsometrischer Wandel der periglaziären Formung 7.1 Grundlagen und Kriterienl der räumlichen Abgrenzung des Periglaziärs 7.2 Kriterien der regionalen Differenzierung des Periglaziärs 7.3 Die Abgrenzung und regionale Differenzierung der periglaziären Zone 7.3.1 Subpolar-ozeanisches Periglaziär 7.3.1.1 Subpolar-hochozeanisches Periglaziär 7.3.2 Subpolar-kontinentales Periqlaziär (subpolares Subperiglaziär) 7.3.3 Polares Periglaziär 7.3.3.1 Polares Tundrenperiglaziär 7.3.3.2 Polares Frostschuttperiglaziär 7.3.4 Hochpolares Frostschuttperiglaziär und antarktisches Periglaziär 7.3.5 Hochkontinentales Boreal-Periglaziär 7.3.6 Zusammenfassung und Ergebnisse 7.4 Abgrenzung, Untergrenzverlauf und hypsometrische Differenzierung der periglaziären Höherstufe 7.4.1 Subpolar-periglaziäre Höhenstufe 7.4.2 Mediolatitudinal-periglaziäre Höhenstufe 7.4.3 Zur Frage einer periglaziären Höhenstufe in den Sub- und Randtropen 7.4.4 Tropisch-periglaziäre Höhenstufe 7.4.5 Zusammenfassung 8. Zusammenfassung und Ergebnisse Summary Literaturverzeichnis , Zusammenfassung in deutscher und englischer Sprache
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  • 27
    Call number: MOP 44818 / Mitte
    Type of Medium: Monograph available for loan
    Pages: vii, 50 Seiten , 28 cm
    Language: English
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  • 28
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/9
    In: CRREL Report, 79-9
    Description / Table of Contents: Sedimentation at the terminus of the Matanuska Glacier has been found to be primarily subaerial in a 100- to 300-m wide, ice-cored zone paralleling the edge of the active ice. Certain physical and chemical characteristics of the ice and debris of the superglacial, englacial and basal zones of the glacier indicate the debris of the basal zone, the primary source of sediment, is entrained during freeze-on of meltwater, probably surficially derived, to the glacier sole. Till formation results from the melting of buried ice of the basal zone. Melt-out till inherits the texture and particle orientations of basal ice debris; other properties are not as well preserved. Most deposits result from resedimentation of till and debris by sediment gravity flows, meltwater sheet and rill flow, slump, spall, and ice ablation. Depositional processes are interrelated in the process of backwasting of ice-cored slopes. Sediment flows are the primary process of resedimentation. Their physical characteristics, multiple mechanisms of flow and deposition, and characteristics of their deposits vary with the water content of the flow mass. Deposits of each process are distinguished from one another by detailed analysis of their internal organization, geometry and dimensions, and the presence of other internal and related external features. Genetic facies are defined by these characteristics. The interrelationship of processes develops a composite depositional sequence defined in terms of genetic facies associations; an upper, resedimented facies association, a middile, till facies association, and a lower, subglacial-resedimental facies association. The lateral and vertical distribution of genetic facies within the associations is mainly nonrepetitive.
    Type of Medium: Series available for loan
    Pages: X, 112 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 79-9
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Field site Historical background Chapter 2. Characteristics of the debris and ice Characteristics of the facies and subfacies Basal zone Characteristics of the debris Discussion Chapter 3. Oxygen isotope analysis Sampling and analysis Results Discussion Chapter 4. Depositional processes—till formation Methods of analysis Environmental setting Till formation Chapter 5. Depositional processes—resedimentation Sediment flows Other resedimentation processes Resedimentation process relationships Chapter 6. Process distribution, sediment dispersal and depositional patterns Physical characteristics Sediment dispersal Sedimentary facies Patterns of terminus sedimentation Chapter 7. Conclusions Literature cited
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  • 29
    Call number: MOP 45476 / Mitte
    Type of Medium: Monograph available for loan
    Pages: [400] Seiten , Illustrationen , 28 cm
    Language: English
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  • 30
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/21
    In: CRREL Report, 79-21
    Description / Table of Contents: The report studies the question of whether Great Lakes freighters could move effectively through ice-clogged channels with the aid of tows provided by warping or kedging systems. Ten operational concepts are outlined, and their advantages and disadvantages are noted. The crushing resistance of floating brash ice is then analyzed. The neutral, active and passive states of stress for laterally confined brash ice are considered, and the resistance to horizontal thrusting by a smooth vertical wall is calculated for cohesionless brash ice, and for ice in which there is finite cohesion between the ice fragments. The thickening of the ice cover in the vicinity of a "pusher", and the formation of pressure ridges, are analyzed in order to estimate the amount of pile-up that can occur against a ship hull. The analysis then moves on to consideration of ship resistance by brash ice, taking into account crushing resistance at the bow, tangential friction at the bow, and hull friction aft of the bow section. Comparisons are made between thrust from the ship’s screws and the calculated ice resistance. The next section of the report estimates the force requirements for a warping or kedging system in terms of thrust augmentation for existing vessels. Tow cable requirements are given, and estimates are made for cable anchors and for anchorage of underwater structures. The force and power requirements for winches and windlasses are given, the practical problems involved in the pickup or transfer of cables are mentioned, and the report concludes with a brief appraisal. The conclusion is that a simple warping tug system is appropriate for a full scale experiment, a chain ferry with auxiliary barge seems attractive for an operational system, and a chain ferry plow may be an efficient way to clear ice from channels.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Operational concepts A. Warping tug system B. Chain ferry system C. Chain ferry with auxiliary barge D. Ski tow system E. Dual winch warping system F. Simple kedging G. Trailing-line system H. Above-surface dual winch system I. Pulley systems J. Chain ferry plow Crushing resistance of fragmented ice covers Resistance to ship passage by broken ice Crushing resistance at the bow Tangential friction at the bow Hull friction aft of the bow section Total ship resistance from brash ice Comparison of ship thrust and ice resistance Force requirements for a warping or kedging system Tow cable requirements Anchors and anchorages Force and power requirements for winches and windlasses Pickup or transfer of cable General appraisal Literature cited
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  • 31
    Monograph available for loan
    Monograph available for loan
    Berlin : Akademie-Verlag
    Call number: PIK N 106-19-93041
    Type of Medium: Monograph available for loan
    Pages: XIII, 527 Seiten , Diagramme
    Edition: 4. Aufl
    Series Statement: Lehrbuch der theoretischen Physik von L. D. Landau; E. M. Lifschitz. In dt. Sprache hrsg. von Paul Ziesche ; Bd. 5
    Language: German
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  • 32
    Call number: AWI A3-20-93434-2
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 2
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,2
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 33
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Physikalisch-Bioklimatische Forschungsstelle der Fraunhofer-Gesellschaft zur Förderung der angewandten Forschung
    Call number: MOP 40082 / Mitte
    Type of Medium: Monograph available for loan
    Pages: ca. 100 Seiten
    Series Statement: AEC Document Number NYO - 3425 - 10
    Language: English
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  • 34
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/14
    In: CRREL Report, 79-14
    Description / Table of Contents: Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presented which clearly show the effect of frazil ice porosity on ice cover growth rates and the numerical model using air temperature as the major input is compared with field data on ice thickness in a small river laden with frazil ice beneath its cover.
    Type of Medium: Series available for loan
    Pages: ii, 4 Seiten , Illustrationen
    Series Statement: CRREL Report 79-14
    Language: English
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  • 35
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/22
    In: CRREL Report, 79-22
    Description / Table of Contents: Field observations at 60 Sites located in the fast or near-fast ice along a 1200-km stretch of the north coast of Alaska between Bering Strait and Barter Island have shown that the great majority of the ice samples (95%) exhibit striking c-axis alignments within the horizontal plane. Such alignments were usually well developed by the time the ice was 50 cm thick and in some cases when the ice was 20 cm thick. In all cases the degree of preferred orientation increased with depth in the ice. Representative standard deviations around a mean direction in the horizontal plane are commonly less than ± 10° for samples collected near the bottom of the ice. The general patterns of the alignments support a correlation between the preferred c-axis direction and the current direction at the ice/water interface. A comparison between c-axis alignments and spot current measurements made at 42 locations shows that the most frequent current direction coincides with the mean c-axis direction. Such alignments are believed to be the result of geometric selection with the most favored orientation being that in which the current flows normal to the (0001) plates of ice that compose the dendritic sea ice/sea water interface.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-22
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Techniques and sampling Observations Crystal alignments “Odd” sites Causes Conclusions Literature cited Appendix A: Current observations
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  • 36
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/19
    In: CRREL Report, 79-19
    Description / Table of Contents: The critical velocities of loads moving over floating ice plates have been determined by several authors. In all these analyses it was assumed that the in-plane force field in the ice cover is zero. However, due to constrained thermal strains, in-plane forces do occur in the field. The purpose of the present paper is to determine their effect upon the critical velocities of the moving loads. It is shown that a uniform compression force field reduces the critical velocity, whereas a tension force field has the opposite effect.
    Type of Medium: Series available for loan
    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-19
    Language: English
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  • 37
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/17
    In: CRREL Report, 79-17
    Description / Table of Contents: Six test roofs of two different slopes — 16.3° and 39.8°, and three different roof coverings — asphalt shingles, cedar shingles, and corrugated aluminum sheeting, were constructed at USACRREL, Hanover, New Hampshire, and were instrumented with thermocouples, heat flow meters, and calibrated gutters. Measurements were recorded for the winters of 1971-72 and 1972-73. The degree of icing and the chronological changes in the snow cover were recorded on 35-mm Kodachrome slides. It was found that eave icing is a sensitive function of the slope, roof covering composi­tion, and solar radiation. The effects of wind were not investigated; the data were screened to remove all informa­tion corresponding to windspeeds over 8 km/h. In order of increasing tendency to form ice dams on the eaves, the roofs were high-slope asphalt, high-slope cedar, high-slope aluminum, low-slope asphalt, low-slope cedar, and low- slope aluminum.
    Type of Medium: Series available for loan
    Pages: vi, 40 Seiten , Illustrationen
    Series Statement: CRREL Report 79-17
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Experimental procedure Description of roofs Meteorological data Procedure Analysis General Temperature profiles Temperature rankings Heat flow Snow depths and meltwater volumes Degree of icing Results and conclusions General Temperature profiles of the roofs Comparative temperatures of roofs by section — rankings Heat flow and accumulation Snow depth, coverage, and meltwater Degree of icing Discussion of the icing problem Literature cited
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  • 38
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/16
    In: CRREL Report, 79-16
    Description / Table of Contents: In 1973 two membrane encapsulated soil layer (MESL) test sections were constructed into existing gravel surfaced roads at Elmendorf A FB and at Ft. Wainwright in Anchorage and Fairbanks, Alaska, respectively. The Elmendorf AFB MESL contains a silty clay soil and the Ft. Wainwright MESL contains a nonplastic silt. Both sections were constructed at soil moisture contents of approximately 2% to 3% below optimum for the CE-12 compactive effort. There were no indica­tions of soil moisture migration during freezing in either test section and after-thaw field California Bearing Ratio values were nearly equal to values measured before freezing. There is growing evidence of a slight increase in the overall soil moisture content in the Elmendorf AFB MESL possibly from moisture entering through the single layer polyethylene sidewalls which were not treated with asphalt emulsion. There is good evidence that the membrane of the same section might have received damage during a soil sampling operation which allowed localized moisture infiltration. A two-layer polyethylene membrane used in the Ft. Wainwright MESL is considered a more positive moisture barrier than the single sheet and a justifiable added cost for permanent construction.
    Type of Medium: Series available for loan
    Pages: v, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 79-16
    Language: English
    Note: CONTENTS Preface Introduction Laboratory studies General Elmendorf AFB silty clay Fairbanks silt Field studies Elmendorf AFB MESL Ft. Wainwright MESL Traffic use Elmendorf AFB MESL Ft. Wainwright MESL Performance observations Elmendorf AFB MESL Ft. Wainwright MESL Conclusions Elmendorf AFB MESL Ft. Wainwright MESL General Literature cited Appendix A. The MESL concept Appendix B. Classification, compaction, freezing and CBR test results for Fairbanks silt
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  • 39
    Call number: MOP 40015 / Mitte
    Type of Medium: Monograph available for loan
    Pages: Seite 307-713 , Illustrationen, Diagramme
    Series Statement: Seminars of scientific foundation of medium range weather forecasts 2
    Language: English
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  • 40
    Call number: MOP 44126/2 / Mitte
    In: Proceedings of the tenth international symposium on remote sensing of environment, Volume 2
    Type of Medium: Monograph available for loan
    Pages: Seiten XLIX, 671-1456
    Series Statement: Proceedings of the tenth international symposium on remote sensing of environment 2
    Language: English
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  • 41
    Monograph available for loan
    Monograph available for loan
    Washington : Special Committee for Solar-Terrestrial Physics (SCOSTEP), National Academy of Sciences
    Call number: MOP 43858/1 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 142 Seiten , Illustrationen , 28 cm
    Language: English
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  • 42
    Call number: AWI G3-23-95343
    In: Trudy Instituta Geologii i Geofiziki, Vypusk 297
    Description / Table of Contents: According to the fossils study of 44 borings the stratigraphy of Paleozoic of the West-Siberian lowland is considered. The first stratigraphical scheme from Devonian to Lower Permian is given for this region. The paper gives the formational analysis as well as notions concerning the tectonic nature of the region, which are based both on this analysis and geophysical data. There are some data on paleozoic geological history of the region. The monography may be of great interest for geologists - specialists in oil geology, stratigraphists, paleontologists, lecturers and students of higher colleges.
    Description / Table of Contents: На основании анализа органических остатков, встреченных в разрезах 44 скважин, рассматривается стратиграфия палеозоя Западно-Сибирской равнины. Для девона и карбона нижней nерми приводятся первые для этой области стратиграфические схемы. Дается информационный анализ и основанные на нем и геофизических данных представления о тектонической природе области в палеозое. Работа представляет интерес для широкого круга геолоrовстратиграфов, палеонтологов, преподавателей и студентов вузов.
    Type of Medium: Monograph available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: Trudy Instituta Geologii i Geofiziki Vypusk 297
    Language: Russian
    Note: Contents Introduction / V. S. Bochkarev Stratigraphy of palaeozoic deposits of the West-Siberian lowland / O. I. Bogush, V. S. Bochkarev, O. V. Yuferev Tectonics of the Palaeozoic of the West-Siberian lowland / V. S. Bochkarev Prinicpal features of the Palaeozoic history of the West-Siberian lowland / O. I. Bogush, V. S. Bochkarev, O. V. Yuferev References Appendix Palaeontological tables I-III , In kyrillischer Schrift , Mit englischer Zusammenfassung und Inhaltsverzeichnis
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  • 43
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: AWI G2-24-95716
    Description / Table of Contents: Сборник включает материалы симпозиума "Поздиечетвертичная история и седиментогенез окраинных и внутренних морей", проведенного Океанографической комиссией АН СССР в 1977 г. На симпозиуме были рассмотрены результаты исследований последних лет в области стратиграфии и литологии четвертичных осадков морей СССР и шельфовой зоны Мирового океана, поздиечетвертичная история южных и дальневосточных морей СССР и некоторых морей европейского Севера. Сборник представляет интерес для геологов-четвертичников, географов, литологов, океанологов, морских геоморфологов и геологов.
    Description / Table of Contents: Translation of abstract: The collection includes materials from the symposium “Late Quaternary history and sedimentogenesis of marginal and inland seas”, held by the Oceanographic Commission of the USSR Academy of Sciences in 1977. The symposium examined the results of recent research in the field of stratigraphy and lithology of Quaternary sediments of the seas of the USSR and the shelf zone of the World Ocean, the late Quaternary history of the southern and the Far Eastern seas of the USSR and some seas of the European North. The collection is of interest to Quaternary geologists, geographers, lithologists, oceanologists, marine geomorphologists and geologists.
    Type of Medium: Monograph available for loan
    Pages: 211 Seiten , Illustrationen , 2 Kartenbeilagen
    Language: Russian
    Note: СОДЕРЖАНИЕ Особенности седиментогенеза на континентальных окраинах океанов и во внутренних морях / Ф. А. Щербаков Строение плиоцен-четвертичной толщи дна Баренцева моря на разрезе полуостров Рыбачий - острова Земля Франца-Иосифа / А. И. Блажчишин, Т. И. Линькова, О. В. Кириллов, Е. П. Шкатов К палеогеографии Баренцева моря в позднеледниковье и голоцене / Б. Н. Котенев Эволюция осадконакопления в прибрежных районах Баренцева и Белого морей в поздне- и послеледниковое время / В. Я. Евзеров Стратиграфия верхнечетвертичных отложений северной части Белого моря / Р. Н. Джиноридзе, Е. А. Кириенко, Л. В. Калугина, А. Е. Рыбалко, М. А. Спиридонов, Е. А. Спиридонова Палинологический и диатомовый анализ донных отложений Балтийского моря / Г. И. Клейменова, В. И. Хомутова, Е. М. Вишневская Стратиграфия позднечетвертичных отложений Черного моря / Ф. А. Щербаков, Е. В. Коренева, Э. К. Забелина Палеогеография Черноморского бассейна в позднечетвертичное время по данным палинологического анализа глубоководных отложений / А. В. Комаров Особенности седиментогенеза в морских подводных каньонах кавказского шельфа Черного моря / К. И. Джанджгава Об изменении биопродуктивности вод Черного моря в голоцене / Н. М. Андреева, Б. Н. Котенев, Л. Н. Розов Закономерности формирования и распределения водно-физических свойств глубоководных осадков Черного моря / В. А. Емельянов, А. Ю. Митропольский Геологическая история Керченского пролива в позднечетвертичное время / Е. Ф. Шнюков, В. М. Аленкин, А. В. Григорьев, А. Л. Путь, Н. А. Ломаев Отражение глубинных структур в морских четвертичных отложениях центральной части Азовского моря / В. Н. Семененко, О. Г. Сиденко Марганцеворудный процесс в позднем антропогене Азово-Черноморского бассейна / Г. Н. Орловский Палеоклиматы, водный баланс и уровни Черного и Каспийского морей в позднем плейстоцене-голоцене / И. Г. Авенариус Гипотетическая климатическая кривая основных этапов осадконакопления Каспийского моря в позднем плейстоцене / В.К Шкатова Процессы седиментогенеза в море Леванта / А. А. Мусса, А. Ю. Митропольский Петрографо-минералогическая характеристика современных отложений Бенгальского залива и Андаманского моря / Д. Е. Гершанович, А. И. Конюхов, И. А.Назаревич Терригенно-минералогические провинции прибрежно-шельфовой зоны Западного Индостана / О. К. Тареева Морфотектоника материкового побережья юга Дальнего Востока и морские трансгрессии позднего плейстоцена-голоцена / А. П. Кулаков Последние этапы голоценовой трансгрессии в бассейнах Японского и Охотского морей / А. М. Короткий, П. Ф. Бровко, И. И. Задкова, В. С. Пушкарь, И. Г. Шахгельдян Основные черты геологического строения шельфа и материкового склона Японского моря у побережья СССР / И. И. Берсенев, И. К. Пущин Четвертичные отложения шельфа Южного приморья на примере залива Петра Великого (Японское море) / Ю. Д. Марков Позднеnлейстоценовые бассейны Юго-Западной Камчатки и их связь с неотектоническими движениями / Р. Б. Крапивнер Криолитозона арктического шельфа Азии / З. Н. Антипина, Ф. Э. Арэ, В. В. Войченко, E. H. Молочушкин Опыт количественной оценки голоценовых тектонических движений в области шельфа / Н. Н. Дунаев Об использовании метода измерения магнитной восприимчивости морских осадков для восстановления условий их формирования на шельфе / Ю. В. Кочемасов , Translation of Table of Contents Features of sedimentogenesis on the continental margins of the oceans and in inland seas / F. A. Shcherbakov Structure of the Pliocene-Quaternary strata of the Barents Sea bottom in the section of the Rybachy Peninsula - Franz Josef Land Islands / A. I. Blazhchishin, T. I. Linkova, O. V. Kirillov, E. P. Shkatov On the paleogeography of the Barents Sea in the Late Glacial and Holocene / B. N. Kotenev Evolution of sedimentation in the coastal areas of the Barents and White Seas in late and post-glacial times / V. Ya. Evzerov Stratigraphy of Upper Quaternary sediments of the northern part of the White Sea / R. N. Dzhinoridze, E. A. Kiriyenko, L. V. Kalugina, A. E. Rybalko, M. A. Spiridonov, E. A. Spiridonova Palynological and diatom analysis of bottom sediments of the Baltic Sea / G. I. Kleimenova, V. I. Khomutova, E. M. Vishnevskaya Stratigraphy of Late Quaternary sediments of the Black Sea / F. A. Shcherbakov, E. V. Koreneva, E. K. Zabelina Paleogeography of the Black Sea basin in the late Quaternary according to palynological analysis of deep-sea sediments / A. V. Komarov Features of sedimentogenesis in marine underwater canyons of the Caucasian shelf of the Black Sea / K. I. Dzhandzhgava On changes in the bioproductivity of the Black Sea waters in the Holocene / N. M. Andreeva, B. N. Kotenev, L. N. Rozov Regularities of formation and distribution of water-physical properties of deep-sea sediments of the Black Sea / V. A. Emelyanov, A. Yu. Mitropolsky Geological history of the Kerch Strait in the late Quaternary / E. F. Shnyukov, V. M. Alenkin, A. V. Grigoriev, A. L. Put, N. A. Lomaev Reflection of deep structures in marine Quaternary sediments of the central part of the Azov Sea / V. N. Semenenko, O. G. Sidenko Manganese ore process in the late Anthropogene of the Azov-Black Sea basin / G. N. Orlovsky Paleoclimates, water balance and levels of the Black and Caspian Seas in the Late Pleistocene-Holocene / I. G. Avenarius Hypothetical climate curve of the main stages of sedimentation of the Caspian Sea in the Late Pleistocene / V.K Shkatova Processes of sedimentogenesis in the Levant Sea / A. A. Mussa, A. Yu. Mitropolsky Petrographic-mineralogical characteristics of modern sediments of the Bay of Bengal and the Andaman Sea / D. E. Gershanovich, A. I. Konyukhov, I. A. Nazarevich Terrigenous-mineralogical provinces of the coastal-shelf zone of Western Hindustan / O. K. Tareeva Morphotectonics of the continental coast of the south of the Far East and marine transgressions of the late Pleistocene-Holocene / A. P. Kulakov The last stages of the Holocene transgression in the basins of the Sea of Japan and the Sea of Okhotsk / A. M. Korotkiy, P. F. Brovko, I. I. Zadkova, V. S. Pushkar, I. G. Shakhgeldyan Main features of the geological structure of the shelf and continental slope of the Sea of Japan off the coast of the USSR / I. I. Bersenev, I. K. Pushchin Quaternary sediments of the Southern Primorye shelf using the example of Peter the Great Bay (Sea of Japan) / Yu. D. Markov Late Leistocene basins of Southwestern Kamchatka and their connection with neotectonic movements / R. B. Krapivner Cryolithozone of the Arctic shelf of Asia / Z. N. Antipina, F. E. Are, V. V. Voichenko, E. H. Molochushkin Experience in quantitative assessment of Holocene tectonic movements in the shelf area / N. N. Dunaev On the use of the method of measuring the magnetic susceptibility of marine sediments to restore the conditions of their formation on the shelf / Yu. V. Kochemasov , In kyrillischer Schrift
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  • 44
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    Pages: 39 S. : Ill.
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  • 45
    Call number: MOP 44018 ; MOP B 15744 ; MOP B 15730
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    Pages: XII, 1337 S. : 486 Ill.
    Edition: 1. Aufl.
    ISBN: 387144149X
    Uniform Title: Poradnik in±zyniera, matematyka
    Language: German
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  • 47
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  • 48
    Call number: MOP Per 607(216)
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  • 49
    Call number: MOP 45718
    In: Meteorologisches Institut der Universität Bonn
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    Pages: 83, xv S. : graph. Darst.
    Series Statement: Meteorologisches Institut der Universität Bonn 102
    Note: Bonn, Univ., Diplomarbeit, 1979
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  • 50
    Call number: MOP B 17467
    In: The Institute of Mathematics and its applications conference series : N.S.
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  • 51
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    Pages: 28 S. + 8 Beil.
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    Call number: PIK D 012-11-0267
    Description / Table of Contents: Contents: 1. Bedeutung, Geschichte und Möglichkeiten der urgeschichtlichen Chronologie ; 2. Die Methoden ; 3. Ergebnisse durch Kombination der Methoden
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    Series Statement: Wissenschaftliche Beiträge der Martin-Luther-Universität Halle-Wittenberg 1974, 4 : L, [Vor- und frühgeschichtl. Beitr.]; 10
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  • 56
    Call number: ZSP-403-27
    In: Jare Data Reports
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    Call number: ZSP-403-28
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  • 59
    Call number: MOP Per 682(54)
    In: Mitteilungen aus dem Max-Planck-Institut für Aeronomie
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  • 60
    Call number: MOP 44026 / Mitte
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    Delhi : Manager of Publ., Civil Lines ; 26.1975 - 29.1978
    Call number: MOP Per 56
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    ISSN: 0376-4796
    Former Title: Vorg. ---〉 Indian journal of meteorology & geophysics
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  • 62
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    In: Modern developments in hydrometry
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  • 63
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    Tokyo : National Institute of Polar Research
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    In: Memoirs of National Institute of Polar Research
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  • 64
    Call number: MOP 45774 / Mitte ; MOP 45773 / Mitte
    In: Münchener geographische Abhandlungen
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    Pages: VI, 85 Seiten , Illustrationen
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    Series Statement: Münchener geographische Abhandlungen 15
    Language: German
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    Call number: S 12.0222(62)
    In: Acta phytogeographica Suecica
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    ISBN: 9172100621 , 91-7210-462-7
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  • 67
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    Pages: 178 S.
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    Call number: S 12.0222(65)
    In: Acta phytogeographica Suecica
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    ISBN: 9172100656 , 91-7210-465-1
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  • 69
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    In: Memoirs of National Institute of Polar Research
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  • 70
    Call number: S 12.0222(66)
    In: Acta phytogeographica Suecica
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  • 71
    Call number: MOP 44043
    In: Physiker über Physiker
    In: Studien zur Geschichte der Akademie der Wissenschaften der DDR
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  • 73
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    Offenbach, M : Dt. Wetterdienst
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  • 74
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    In: Die chemische Zusammensetzung der unteren Atmosphäre
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  • 75
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  • 77
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    Leningrad [u.a.] : Gidrometeorog. Izd-vo
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    In: Trudy Ukrainskogo Naučno-Issledovatel'skogo Gidrometeorologičeskogo Instituta
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    Pages: 159 S.
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  • 78
    Call number: MOP Per 29/D(107)
    In: NOAA technical memorandum
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  • 79
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    Geneva : Secretariat of the World Meteorological Organization
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    Call number: MOP Per 800(530) ; MOP Per 800(530, 2. Ex.)
    In: WMO
    In: Technical note
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    Pages: 201 S. : Ill.
    ISBN: 9263105308
    Series Statement: WMO / World Meteorological Organization 530
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  • 80
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    In: Trudy
    Type of Medium: Monograph available for loan
    Pages: 118 S.
    Series Statement: Trudy / Glavnaja Geofiziceskaja Observatorija Imeni A. I. Voejkova 415
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  • 81
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    Call number: MOP 44629(1974-1975) / Mitte
    In: Obščee soderžanie atmosfernogo ozona i spektral'naja prozračnost' atmosfery
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  • 82
    Call number: MOP 43949 / Mitte ; AWI A5-18-20118
    Description / Table of Contents: Wie wird das Wetter morgen? Wird der Winter schneereich oder der Sommer warm und trocken sein? Verändert sich das Klima in größeren Zeiträumen? Hatten unsere Urväter anderes Wetter als wir heute? Wohl jeder von uns beschäftigt sich - bewußt oder unbewußt - mit Fragen der Meteorologie. Oftmals wünschen wir uns, das Wettergeschehen exakt vorhersagen zu können, ja schadenbringende Wettererscheinungen zu verhindern. Die Autoren Choren P. Pogosjan und Sinaida L. Turketti legen ein Buch vor, das alle diese Probleme sehr ausführlich behandelt. Sie bringen uns den Aufbau der Atmosphäre sowie moderne Methoden zu ihrer Erforschung nahe, erklären unter vielem anderen die Entstehung des Windes, die Wolkenbildung und die Wolkenklassifikation. Auch die Grundlagen und Techniken der kurzfristigen und langfristigen Wetterprognose werden beschrieben, so daß wir einen Einblick in die praktische Arbeit der Wetterdienststellen gewinnen. Ein Teil des Buches ist den Problemen der Wetter- und Klimaveränderungen gewidmet. Wir erfahren von Plänen über die künstliche Einwirkung des Menschen auf den Kreislauf in der Atmosphäre. Bereits der norwegische Polarforscher Fridtjof Nansen schlug vor, durch eine Verbreiterung der schmalen Beringstraße das Klima der Arktis zu erwärmen. Ähnliche und grundlegend andere Projekte gibt es noch viele. In der Sowjetunion wies man auf die Möglichkeit hin, die Eisbedeckung des Nördlichen Eismeeres aufzulösen. Man brauchte dazu die Eisfläche nur mit schwarzem Pulver zu bestreuen. Aus Berechnungen folgt, daß sich - nachdem das Eis geschmolzen wäre - keine stabile Eiskruste mehr bilden könnte. Alle diese Vorhaben sind vorläufig noch theoretischer Natur. Die Wissenschaftler haben noch zu prüfen, welchen praktischen Nutzen die Realisierung der Pläne bringen würde. Das Ziel der Meteorologie ist, die Lufthülle der Erde immer tiefer zu erforschen, um künftig exaktere Wetterprognosen zu erstellen und auf ungünstige Wettererscheinungen einwirken zu können. Vielleicht wird der Mensch eines Tages in der Lage sein, das Klima der Erde langfristig und gezielt verändern zu können?
    Type of Medium: Monograph available for loan
    Pages: 338 Seiten , Illustrationen
    Edition: 1. Auflage
    Uniform Title: Atmosfera zemli (dt.)
    Language: German
    Note: Inhalt: EINFÜHRUNG. - DIE LUFTHÜLLE DER ERDE. - Moderne Methoden zur Erforschung der Atmosphäre. - Aerologische Beobachtungen. - Erstes Vordringen des Menschen in den Luftozean. - Meteorologische Raketen und künstliche Erdsatelliten. - Neue Erkenntnisse über die Zusammensetzung der Atmosphäre. - Der Luftdruck. - Der Aufbau der Atmosphäre. - ÜBER DIE SONNENEINSTRAHLUNG. - Die Sonnenenergie. - Das Strahlungsgleichgewicht. - Die direkte und die diffuse Sonnenstrahlung. - Die Wärmebilanz der Erdoberfläche und der Atmosphäre. - Der Glashauseffekt. - Die Nutzung der Sonnenenergie. - Die Temperaturverhältnisse in der Stratosphäre und Mesosphäre. - DIE LUFTTEMPERATUR. - Die mittlere Lufttemperatur. - Die Temperaturamplitude in der bodennahen Luftschicht. - Der Einfluß von Land und Meer auf die Temperatur in der bodennahen Luftschicht. - Die Lufttemperatur über Land und Meer. - Die Lufttemperatur in niederen und hohen Breiten. - Die Lufttemperatur in höheren Schichten der Atmosphäre. - Die unterschiedliche physikalische Beschaffenheit der Troposphäre. - Die Veränderung von Luftschichtungen und deren Einfluß auf den Wetterverlauf. - Die Lufttemperaturen in der Troposphäre und Stratosphäre. - Der Wärmeaustausch zwischen unteren und hohen Schichten - Die Wärmeübertragung durch Meeresströmungen. - LUFTDRUCK UND WIND. - Die Entstehung des Windes. - Kräfte, die in der Atmosphäre wirksam sind, und ihr Einfluß auf den Wind. - Monatsmittelkarten der Druck- und Strömungsverteilung an der Erdoberfläche. - Beziehungen zwischen dem Temperatur-, Druck- und Windfeld in der Höhe. - TROPOSPHÄRISCHE FRONTEN UND FRONTALZONEN - ATMOSPHÄRISCHE WIRBEL. - Die Entstehung von Frontalzonen und Fronten. - Das Wetter beim Durchzug von Fronten. - Gewaltige atmosphärische Wirbel - Zyklonen und Antizyklonen. - Die Entstehung und Entwicklung von Zyklonen und Antizyklonen. - Tropische Zyklonen. - Kleinräumige atmosphärische Wirbel. - ORKANARTIGE HÖHENWINDE - STRAHLSTRÖME. - Höhenfrontalzonen und Strahlströme. - Der Zusammenhang zwischen Temperaturfeld und Strahlstrom. - Einige Merkmale von Strahlströmen über Europa und dem asiatischen Territorium der UdSSR. - Die Häufigkeit von Strahlströmen über der Nordhalbkugel. - Die Entstehung von Strahlströmen. - DIE ALLGEMEINE ZIRKULATION IN DER ATMOSPHÄRE. - Die Entdeckungsgeschichte der planetarischen Zirkulation. - Grundgrößen der allgemeinen Zirkulation. - Die Luftzirkulation in außertropischen Breiten. - Passate. - Monsune. - Modelle der allgemeinen Zirkulation in der Atmosphäre. - BEWÖLKUNG UND NIEDERSCHLÄGE. - Die Wolkenbildung. - Die Wolkenklassifikation. - Die Mikrophysik der Wolken. - Der Wasserkreislauf in der Atmosphäre. - Verdunstung und Niederschläge in begrenzten Gebieten. - Die planetarischen Niederschläge. - WETTERPROGNOSEN. - Wetter und Klima. - Kurzfristige Wetterprognosen. - Numerische Methoden der Wetterprognose. - Langfristige Wetterprognosen. - Besonderheiten des Aufbaus der Atmosphäre über Osteuropa und Westsibirien am 2. Mai 1965. - Wetterprognosen anhand örtlicher Erscheinungen und Wetterzeichen. - PROBLEME DER WETTER- UND KLIMAVERÄNDERUNG. - Künstliche Wetter- und Klimabeeinflussung. - Künstliche Einwirkung auf Wolken und Nebel. - Die Beeinflussung des Klimas in der bodennahen Luftschicht. - KLIMASCHWANKUNGEN UND KLIMAÄNDERUNGEN. - Die Merkmale des Klimas. - Derzeitige Hypothesen über Klimaänderungen. - Klimaänderungen der Erde in verschiedenen geologischen Epochen. - Klimaänderungen in der Vergangenheit. - Über Klimaänderungen in der nächsten Zukunft. - Der Einfluß der Städte auf Ihre Atmosphäre. , Aus dem Russischen übersetzt
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  • 83
    Call number: K-13-0019(1-6)
    Pages: 1 Kt. in 6 Bl. : mehrfarb.
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  • 84
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP 38234/8
    In: Wörterbuch der modernen Technik
    Type of Medium: Monograph available for loan
    Pages: 598 S.
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  • 85
    Monograph available for loan
    Monograph available for loan
    Tartu
    Call number: MOP 44041
    Type of Medium: Monograph available for loan
    Pages: 251 S. : Ill.
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  • 86
    Call number: AWI G7-84-0849
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 86 S.
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  • 87
    Monograph available for loan
    Monograph available for loan
    Reading ; 1979 - 1986 nachgewiesen
    Call number: MOP 45206
    Type of Medium: Monograph available for loan
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  • 88
    Monograph available for loan
    Monograph available for loan
    Moskva : Mosk. Otdel. Gidromet.
    Call number: MOP 44801 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 29 S.
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  • 89
    Monograph available for loan
    Monograph available for loan
    [Berlin] : [Univ.]
    Call number: MOP 45221
    Type of Medium: Monograph available for loan
    Pages: 88 S.
    Note: Berlin, Humboldt-Univ, Diplomarbeit, 1979
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  • 90
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-345
    In: Research report / Cold Regions Research and Engineering Laboratory, 345
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols. - Introduction. - Previous work. - Experimental design. - The radioisotope 22Na. - Description of apparatus. - Experimental procedure. - Correction of profiles. - Assumptions. - Decay correction. - Boundary correction. - Error analysis. - Results. - Salinity data. - Temperature data. - Growth velocity. - Discussion. - Brine and ice properties. - Brine salinity. - Brine density. - Brine volume. - Brine latent heat of freezing. - Brine viscosity, specific heat, and thermal conductivity. - Ice properties. - Theoretical brine expulsion model. - Continuity equations. - Thermal energy equation. - Simplified brine expulsion equations. - Brine expulsion in NaCl ice. - Results. - Discussion. - Gravity drainage in NaCl ice. - Application of results to natural sea ice. - Effective distribution coefficient. - Previous work. - Experimental procedure and results. - Conclusions. - Literature cited. - Appendix A: Profile correction data. - Appendix B: Program "correct" and sample output. - Appendix C: Tabulation of salinity data. - Appendix D: Tabulation of profile data. - Appendix E: Time-ice thickness equations (Runs 2 and 3). - Appendix F: Tabulation of distribution coefficient data.
    Description / Table of Contents: To obtain a better understanding of the desalination of natural sea ice, an experimental technique was developed to measure sequential salinity profiles of a growing sodium chloride ice sheet. Using radioactive 22Na as a tracer, it was possible to determine both the concentration and movement of the brine within the ice without destroying the sample. A detailed temperature and growth history of the ice was also maintained so that the variation of the salinity profiles could be properly interpreted. Since the experimental salinity profile represented a smoothed, rather than a true salinity distribution, a deconvolution method was devised to restore the true salinity profile. This was achieved without any significant loss of end points. In all respects, the salinity profiles are similar to those of natural sea ice. They have a characteristic C-shape, and clearly exhibit the effects of brine drainage. Not knowing the rates of brine expulsion or gravity drainage, the variation of the salinity profiles during the period of ice growth could be explained by either process. To determine the relative importance of the desalination mechanisms, a theoretical brine expulsion model was derived and compared to the experimental data. As input for the model, equations describing the variation of some properties of NaCl brine with temperature were derived. These included the brine salinity, viscosity, specific heat, thermal conductivity, and latent heat of freezing. The theoretical brine expulsion model was derived by performing mass and energy balances over a control volume of NaCl ice. A simplified form of the model, when compared to the experimental results, indicated that brine expulsion was only important during the first several hours of ice growth, and later became a minor desalination process relative to gravity drainage which continued to be the dominant mechanism for the remainder of the study period (up to 6 weeks). The rate of gravity drainage was found to be dependent on the brine volume and the temperature gradient of the ice. As either the brine volume or temperature gradient was increased, the rate of change of salinity due to gravity drainage increased. The equation commonly used to calculate the effective distribution coefficient (Weeks and Lofgren 1967) was modified and improved by taking brine drainage into account. An expression was also derived to give the distribution coefficient at very low growth velocities.
    Type of Medium: Series available for loan
    Pages: vii, 85 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 345
    Language: English
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  • 91
    Monograph available for loan
    Monograph available for loan
    Boulder, Colo. : Environmental Research Laboratories
    Call number: MOP 41125 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VIII, 499 Seiten
    Language: English
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  • 92
    Monograph available for loan
    Monograph available for loan
    Berlin : Dietz
    Call number: MOP 44987 ; MOP 44953 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 284 S. : graph. Darst.
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  • 93
    Call number: MOP Per 745(112)
    In: Voprosy geografii
    Type of Medium: Monograph available for loan
    Pages: 222 S. : Kt.
    Series Statement: Voprosy geografii 112
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  • 94
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP Per 666(9,1)
    In: Sturmfluten und Seegang
    Type of Medium: Monograph available for loan
    Pages: 32 S. : Ill., graph. Darst.
    Series Statement: 9,1
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  • 95
    Monograph available for loan
    Monograph available for loan
    Offenbach, M : Dt. Wetterdienst
    Associated volumes
    Call number: MOP Per 666(9,2-3)
    In: Promet
    Type of Medium: Monograph available for loan
    Pages: 64 S. : graph. Darst., Kt.
    Series Statement: Promet 9,2-3
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  • 96
    Monograph available for loan
    Monograph available for loan
    Offenbach, M : Dt. Wetterdienst
    Associated volumes
    Call number: MOP Per 666(9,4)
    In: Promet
    Type of Medium: Monograph available for loan
    Pages: 32 S. : Ill., graph. Darst., Kt.
    Series Statement: Promet 9,4
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  • 97
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP Per 666(5,4)
    In: GATE
    Type of Medium: Monograph available for loan
    Pages: 32 S. : Ill., graph. Darst.
    Series Statement: 5,4
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  • 98
    Call number: MOP 44020
    Type of Medium: Monograph available for loan
    Pages: 378 S. :
    Edition: 1. Aufl.
    Series Statement: Mathematik für Ingenieure
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  • 99
    Monograph available for loan
    Monograph available for loan
    Nr. 1.1968 - 28.1997; damit Ersch. eingest.
    Call number: MOP Per 122/A
    Type of Medium: Monograph available for loan
    ISSN: 0169-3581
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  • 100
    facet.materialart.
    Unknown
    Stuttgart : Bundesanstalt für Geowissenschaften und Rohstoffe
    Associated volumes
    Call number: K 94.0039 ; K 93.0010/CC7102
    In: Geologische Übersichtskarte
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