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  • English  (7,356)
  • Russian  (355)
  • Hindi  (2)
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  • 1995-1999  (2,144)
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  • 1975-1979  (2,028)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Moscow : Mir Publ.
    Call number: PIK L 110-11-0182
    Description / Table of Contents: Contents: Part One: Fundamentals of Soil Formation and Properties of Soils ; 1. Principles of soil formation ; 2. Mineral part of soil and its origin ; 3. Soil physics ; 4. Soil chemistry ; 5. Physical chemistry of soils ; 6. Soil biochemistry ; 7. Elementary processes of soil formation ; Part Two: Natural Factors of Soil Evolution ; 8. Rocks and soil formation ; 9. The relationship between weathering and soil-forming processes under tropical conditions ; 10. Biological factors of soil formation ; 11. Climate and soil formation ; 12. Soil formation as a function of relief and soil age ; Part Three: Classification and Characteristics of Main Soil Types ; 13. Fundamentals of soil classification ; 14. Experience in grouping the soils in the tropics and subtropics ; 15. Siallitic neutral-alkaline soils ; 16. Allitic (ferrallitic) soils ; 17. Podzolic ferrallitic tropical soils ; 18. Yellow quartz-allitic soils ; 19. Red ferritic soils ; 20. Volcanic soils (Andosols) ; 21. Hydromorphic soils (Gleysols) ; 22. Saline (Halomorphic) soils ; 23. Alluvial soils ; 24. Problems of soil conservation ; 25. Problems of soil fertility improvement ; 26. Soil cartography and its practical importance
    Type of Medium: Monograph available for loan
    Pages: 422 S. : graph. Darst.
    Uniform Title: Osnovy tropičeskogo počvovedenija
    Language: English
    Location: A 18 - must be ordered
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  • 2
    Call number: MOP 47545 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 165 S.
    ISBN: 5286005195
    Language: Russian
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 3
    Call number: MOP Per 283(411)
    In: Trudy
    Type of Medium: Monograph available for loan
    Pages: 124 S.
    Series Statement: Trudy / Glavnaja Geofiziceskaja Observatorija Imeni A. I. Voejkova 411
    Language: Russian
    Note: In kyrill. Schr.
    Location: MOP - must be ordered
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  • 4
    Call number: AWI A12-89-0486
    In: Itogi nauki i techniki : Serija geomagnetizm i vysokie sloi atmosfery, 11
    Type of Medium: Series available for loan
    Pages: 208 S. : Ill., graph. Darst.
    ISSN: 0202-7275
    Series Statement: Itogi nauki i techniki : Serija geomagnetizm i vysokie sloi atmosfery 11
    Language: Russian
    Note: In kyrill. Schr.
    Location: AWI Reading room
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  • 5
    Call number: AWI G2-87-0348
    Description / Table of Contents: The book by E. I. Saruhanian, N. P. Smirnov "Water masses and circulation of the South Ocean" deals with the formation, localization and spreading of the South Ocean water masses, the methods of marking them out by an indication complex. The main features of the South Ocean circulation determined on the basis of geostrophic calculations and those based on the diagnostic model, and also characteristics derived from the data of drifting buoys are described. The analysis of spatial structure and changeability of the Antarctic circumpolar current and connected frontal polar zone is given on the basis of the data obtained in different South Ocean regions during conduction of the multiscale scientific experiments according to the programmes "Polar experiment - South" and "International South Ocean Research" in 1975-1982.
    Type of Medium: Monograph available for loan
    Pages: 287 S.
    Language: Russian
    Note: In kyrill. Schr.
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  • 6
    Call number: AWI A9-89-0434
    Type of Medium: Monograph available for loan
    Pages: 231 S.
    ISBN: 5-02-000727-7
    Language: Russian
    Note: In kyrill. Schr.
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  • 7
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 44964 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 181 S. : Kt.
    Language: Russian
    Location: MOP - must be ordered
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  • 8
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 44645 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 335 S.
    Uniform Title: Monsoon meteorology
    Language: Russian
    Location: MOP - must be ordered
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  • 9
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Academic Press
    Call number: M 98.0230
    Type of Medium: Monograph available for loan
    Pages: 890 S.
    Edition: 9th print.
    ISBN: 0125649223
    Series Statement: Probability and mathematical statistics : a series of monographs and textbooks
    Classification:
    Geodynamics
    Language: English
    Location: Upper compact magazine
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  • 10
    Call number: AWI A4-89-0036-2 ; AWI A4-78-0791-2 ; MOP 45231/B / Mitte
    In: Spravočnik po klimatu Antarktidy / pod red. I. M. Dolgina, Tom 2
    Description / Table of Contents: Contents: Foreword. - PART 1. - Organization of meteorological observations in Antarctica and techniques of climatological data reduction. - Publications of meteorological observations by Antarctic stations. - Explanations to tables. - TABLES. - Section 1. Air temperature. - Section 2. Air pressure. - Section 3. Wind. - Section 4. Air humidity. - Section 5. Cloudiness. - Section 6. Precipitation. - Section 7. Atmospheric phenomena. - Section 8. Visibility. - Section 9. Complex characteristics. - Alphabetic index of stations. - Meteorological stations location map. - List of meteorological stations. - PART 2. - Explanations to tables. - TABLES. - Section 1. Air temperature. - Section 2. Air pressure. - Section 3. Wind. - Section 4. Air humidity. - Section 5. Cloudiness. - Section 6. Precipitation. - Section 7. Atmospheric phenomena. - Meteorological stations location map. - Appendix. - List of literature.
    Type of Medium: Monograph available for loan
    Pages: 492 Seiten , Illustrationen
    Series Statement: Spravočnik po klimatu Antarktidy / pod red. I. M. Dolgina 2
    Language: Russian
    Note: In kyrillischer Schrift , Inhaltsverzeichnis in englischer Sprache (Seite 6- 8])
    Location: AWI Reading room
    Location: AWI Reading room
    Location: MOP - must be ordered
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  • 11
    Monograph available for loan
    Monograph available for loan
    Tartu : Akademija Nauk Ėstonskoj SSR, Institut Astrofiziki i Fiziki Atmosfery
    Call number: MOP 44366 / Mitte ; AWI A19-19-23195
    Type of Medium: Monograph available for loan
    Pages: 176 Seiten , Illustrationen , 1 Beilage
    Language: Russian
    Note: Contents: Foreword by the Pilot-Astronaut of the U.S.S.R A. G. Nikolayev. - Information of the TASS. - Programme of the Optical investigation of the Emission of the Atmosphere, Auroae and Noctilucent clouds aboard the Orbital Station "Salyut-4" / A. I. Lazarev, V. N. Sergeyevich. - Observations of Aurorae from Space / D. S. Yevlashin, P. I. Klimuk, I. I. Koksharov, A. I. Lazarev, V. I. Sevastyanov, V. N. Sergyevich. - Visual observations and photography of noctilucent clouds aboard orbital station "Saljut-4" / Ch. I. Willmann, P. I. Klimuk, P. I. Koksharov, V. I. Sevastyanov, V. N. Sergeyevich. - The physical interpretation of the spectra of noctilucent clouds / O. A. Avaste, A. M. Alekseyev, U. K. Veismann, Ch. I. Willmann, P. I. Klimuk, I. I. Koksharov, A. I. Lazarev, V. I. Sevastyanov, V. N. Sergeyevich, E. O. Fedorova, K. A. Eerme. - The determination of the daytime and twilight profiles of the O2(1Δg) at 1.27 µm from measurements aboard the orbital station "Salyut-4" / O. A. Avaste, U. K. Veismann, Ch. I. Willmann, G. M. Grechko, A. A. Gubarev, P. I. Klimuk, G. I. Lobanova, O. I. Popov, V. I. Sevastyanov, E. O. Fedorova, K. A. Eerme. - Horizontal optical inhomogeneity of the Upper Atmosphere in middle and equatorial latitudes according to the observations aboard the orbital station "Salyut-4" / S. V. Avakyan, P. I. Klimuk, I. I. Koksharov, A. I. Lazarev, V. I. Sevastyanov. - Observations of the earth's night and twilight horizons from the orbital station "Salyut-4" / P. I. Klimuk, I. I. Koksharov, A. I. Lazarev, G. I. Lobanova, E. M. Saar, V. I. Sevastyanov, V. N. Sergeyevich. - Meteor observation and cosmic dust investigation / Ch. I. Willmann, P. I. Klimuk, V. N. Lebedinets, V. I. Sevastyanov. - Ultraviolet radiation measurements of the moon and of the earth's upper atmosphere from the orbital station "Salyut-4" / V. B. Vasilyev, G. M. Grechko, A. A. Gubarev, B. M. Stolberg, V. M. Tiit, N.-R. A. Elmet, R. V. Shatskina. - Observations of the first expedition aboard the orbital station "Salyut-4" / A. I. Lazarev, G. M. Grechko, A. A. Buznikov. - Appendix. , In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-339
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Analytical procedures. - Thick section analysis. - Measurements of inclusion pressure. - Gas volume measurements. - Density and porosity measurements. - Results and discussion. - Sizes, shapes and distributions of bubbles. - Sizes, shapes and distributions of cavities. - Inclusion abundances. - Gas pressures in bubbles and cavities. - Total gas content. - Case for lattice diffusion. - Literature cited.
    Description / Table of Contents: Cores obtained to the bottom of the Antarctic Ice Sheet at Byrd Station were used to analyze the physical properties of air bubbles trapped in the ice. These bubbles originate as pockets of air in the upper layers of snow and approximately 10 ml of air/100 cm^3 of ice; i.e., 10% by volume is retained permanently when the snow transforms into ice. Parameters measured were the sizes, shapes, abundances, spatial distributions, gas volumes and pressures of bubbles, and their variations with depth in the ice sheet. Bubbles occur abundantly in the top 800 m of ice but then gradually disappear until they can no longer be detected optically below 1100 m. This disappearance is not accompanied by any significant loss of air from the ice and all available evidence indicates that the air actually diffuses into the ice in response to increasing overburden pressure. The possibility exists that the dissolved gases are retained in the form of a gas hydrate or clathrate which, because of release of confining pressures, begins to decompose soon after ice cores are pulled to the surface. This decomposition is accompanied by the growth of gas-filled bubble-like cavities, and as much as 40% of the dissolved air has exsolved already from some cores in the space of less than three years. Bubble pressure measurements show that 1) bubbles with pressures exceeding about 16 bars begin to relax back to this value soon after in situ pressures are relieved by drilling, 2) further slow decompression occurs with time, and 3) the rate of decompression is controlled to some extent by the intrinsic structural properties of the ice and its thermal and deformational history. Only small variations were observed in the entrapped air content of the ice cores; they probably reflect variations in the temperature and/or pressure of the air at the time of its entrapment, but the data are not sufficient to draw any firm conclusions regarding past variations in ice sheet thickness. Only ice from the bottom 4.83 m was found to lack any detectable trace of air. Since this absence of air coincided precisely with the first appearance of stratified moraine in the cores, it is concluded that this ice originated from the refreezing of air-depleted water produced under pressure melting conditions at the bottom of the ice sheet.
    Type of Medium: Series available for loan
    Pages: v, 18 Seiten , Illlustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 339
    Language: English
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  • 13
    Monograph available for loan
    Monograph available for loan
    Sebastopol : O'Reilly
    Call number: PIK M 033-14-0214
    Type of Medium: Monograph available for loan
    Pages: XXII, 407 S.
    Edition: 2. ed., [Nachdr.]
    ISBN: 9781565922259
    Series Statement: UNIX power tools
    Language: English
    Location: A 18 - must be ordered
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  • 14
    Call number: ZSP-202-331
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - An overview of the model structure and operation. - Operation of subroutines. - TSTART. - FOMO. - REAWEA. - SEARCH. - STEMP. - TUNPIC. - Development history of the simulator. - The simulation of snow fence effects. - Urbanization and meltout. - Conclusion. - Literature cited. - Appendix A: Mathematical notation. - Appendix B: Computerprogram. - Abstract.
    Description / Table of Contents: An annual snow-soil simulator for Arctic tundra was developed using coupled models of surface equilibrium temperature and substrate thermal diffusion. Snow ripening, melt and accumulation are modeled in the simulator which is forced with daily weather data. The simulator predicts that a snow fence array capable of producing drift deeper than 4.2 meters will initiate a permanent snowfield at Barrow, Alaska. Such a man-induced snowfield could serve as a reliable source of fresh water for Barrow and similar villages in the North Slope region of Alaska. Further analysis indicated that albedo reduction due to dust fall, snow removal, etc., is dominant over aerodynamic effects in producing the early spring meltout observed at Barrow Village.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 331
    Language: English
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  • 15
    Series available for loan
    Series available for loan
    Hanover, N.H. : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-350
    In: Research report / Cold Regions Research and Engineering Laboratory, 350
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 350
    Language: English
    Note: CONTENTS: Abstract. - Preface. - Introduction. - Sample preparation. - Apparatus and testing procedure. - Test results. - Uniaxial strength. - Initial tangent and 50% strength moduli. - Specific energy. - Discussion. - Testing method. - Compressive strength. - Tensile strength. - Ductile and brittle fracture.. - Initial tangent and 50% stress moduli. - Specific energy. - Conclusions and recommendations. - References. - Appendix A: Description of soil and calculations. - Appendix B: Description of the LVDT and averaging circuits. - Appendix C: Determination of strain in the neck section of a dumbbell specimen.
    Location: AWI Archive
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  • 16
    Call number: ZSP-202-338
    In: Detecting structural heat losses with mobile infrared thermography / R.H. Munis, S.J. Marshall and M.A. Bush, Part II
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 338
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Discussion of heat loss survey of six housing units. - Survey of base facilities. - Conclusions. - Literature cited.
    Description / Table of Contents: During the winter of 1973-74 a mobile infrared thermography system was used to survey housing units and base facilities at Pease Air Force Base, Portsmouth, New Hampshire. This report provides both qualitative and quantitative evidence regarding heat flow out of the eave vents of these housing units. Calculations indicate that a significant amount of heat is being lost in this manner due to inadequate attic (cap) insulation. Possible evidence of incomplete ventilation could explain the presence of condensation in the housing units. Analyses of thermograms are presented to show the possible existence of low and high pressure areas around a structure and how they relate to heat loss.
    Type of Medium: Series available for loan
    Pages: iii, 29 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 338
    Language: English
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  • 17
    facet.materialart.
    Unknown
    Innsbruck : Univ.-Verl. Wagner ; Nachgewiesen 2.1979 -
    Call number: ZSP-387
    Language: English
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  • 18
    Monograph available for loan
    Monograph available for loan
    Boston [u.a.] : Artech House
    Associated volumes
    Call number: M 92.1079/2
    In: Optical fiber sensors
    Type of Medium: Monograph available for loan
    Pages: XXII S., S. 329-799
    ISBN: 0890063761
    Classification:
    C.5.1.
    Language: English
    Location: Upper compact magazine
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  • 19
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(964-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 307-359 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 964-D
    Language: English
    Location: Lower compact magazine
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  • 20
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(969-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 29-53 + 5 pl.
    Series Statement: U.S. Geological Survey bulletin 969-B
    Language: English
    Location: Lower compact magazine
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  • 21
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(975-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 45 S. + 6 pl.
    Series Statement: U.S. Geological Survey bulletin 975-A
    Language: English
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  • 22
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(974-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 51-100
    Series Statement: U.S. Geological Survey bulletin 974-C
    Language: English
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  • 23
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(969-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 87-103 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 969-D
    Language: English
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  • 24
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(974-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 135-175 + V S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 974-E
    Language: English
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  • 25
    Call number: SR 90.0001(1787-A-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 36 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1787-A-C
    Language: English
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  • 26
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(977)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 273 S.
    Series Statement: U.S. Geological Survey bulletin 977
    Language: English
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  • 27
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(984)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IX, 183 S. + 19 pl.
    Series Statement: U.S. Geological Survey bulletin 984
    Language: English
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  • 28
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(988-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 69-87 + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 988-F
    Language: English
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  • 29
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1002-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 63-121
    Series Statement: U.S. Geological Survey bulletin 1002-B
    Language: English
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  • 30
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1005)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 53 S. + 7 pl.
    Series Statement: U.S. Geological Survey bulletin 1005
    Language: English
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  • 31
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(995-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 201-253 + 13 pl.
    Series Statement: U.S. Geological Survey bulletin 995-F
    Language: English
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  • 32
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1008)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VII, 155 S. + 12 pl.
    Series Statement: U.S. Geological Survey bulletin 1008
    Language: English
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  • 33
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1022-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 71-133
    Series Statement: U.S. Geological Survey bulletin 1022-B
    Language: English
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  • 34
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1022-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 135-203
    Series Statement: U.S. Geological Survey bulletin 1022-C
    Language: English
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  • 35
    Call number: AWI G7-11-0028 ; AWI G7-88-0245 ; MOP 47452 / Mitte ; MOP 46967 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 246 Seiten , Illustrationen , 1 Karte , 23 cm
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 36
    Call number: MOP Per 283(430)
    In: Trudy
    Type of Medium: Monograph available for loan
    Pages: 162 S.
    Series Statement: Trudy / Glavnaja Geofiziceskaja Observatorija Imeni A. I. Voejkova 430
    Language: Russian
    Note: In kyrill. Schr.
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  • 37
    Monograph available for loan
    Monograph available for loan
    Warszawa : Polish Scient. Publ.
    Call number: PIK N 456-11-0194
    Description / Table of Contents: Contents: 1. Climatology as a science ; 2. Climate-forming factors ; 3. Geographical distribution and variation of major meteorological elements ; 4. A brief survey of major types of climate ; 5. Changes and fluctuations of climates
    Type of Medium: Monograph available for loan
    Pages: XIV, 422 S. : graph. Darst., 1 Kt.
    Uniform Title: Klimatologia ogólna
    Language: English
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  • 38
    Call number: MOP 44357 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 227 S.
    Series Statement: Problemy Konstruktivnoj Geografii
    Language: Russian
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  • 39
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45412 / Mitte ; MOP B 17056
    Description / Table of Contents: The history of climate by A. S. Monin, Yu. A. Shishkov presents the history of the earth's climate from the contemporary positions of the general history of our planet based on the latest achievements in the field of planetology, geology, geophysics, oceanology, meteorology and climatology. The book deals with the factors responsible for climate formation on the earth, presents the major stages of the earth's history, the results of the most recent paleogeographic reconstructions. Further the book presents the history of climate proper from Pre-Cambrian to the recent time in increasing detail. The methods used for paleoclimatic reconstructions are described. Data on Pre-Cambrian glaciations and the major Fanerozoic climatological events are discussed. The book is meant, first of all, for the inquisitive reader, however, it will undoubtedly be of interest for the specialists climatologists, meteorologists, oceanographers and geophysicists.
    Type of Medium: Monograph available for loan
    Pages: 407, [1] S. , graph. Darst., Ill.
    Language: Russian
    Note: In kyrill. Schr.
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  • 40
    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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  • 41
    Call number: AWI G7-90-0312 ; MOP 44730 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 63 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 42
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Associated volumes
    Call number: AWI A4-87-0846
    In: Developments in atmospheric science
    Type of Medium: Monograph available for loan
    Pages: 261 S. : graph. Darst
    Series Statement: Developments in atmospheric science 15
    Uniform Title: Weather and climate of the Antarctic
    Language: Russian
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  • 43
    Call number: AWI A13-87-0849 ; MOP 46754 / Mitte
    Description / Table of Contents: Modelling of the Glaciers-Ocean-Atmosphere system by M. Ya. Verbitsky and D. V. Chalikov presents an earth's climate model based on one-dimensional non-steady thermohydrodynamical equations for the atmosphere, ocean, glaciers, and the asthenosphere. The model takes into account the main mechanisms responsible for the formation of global climate, but it is simple enough to allow simulation of climate evolution for a period up to one million years. The present climate is reconstructed, sensitivity of the system to changes in the initial conditions is investigated and evidence for non-uniqueness of climate for the present distribution of the continents is obtained. Climate sensitivity to changes in the isolation is calculated. Oscillations of climate similar to the Pleistocene ice ages are modelled. Climatic conditions for the Late Mesozoic and Late Pleistozoic are estimated. The book is intended for specialists on climate, oceanologists, meteorologists, glaciologists and also for students of appropriate specialities.
    Type of Medium: Monograph available for loan
    Pages: 130 Seiten , Illustrationen
    Language: Russian
    Note: Contents: Preface. - Introduction Global climate modeling. - Chapter 1. An ice sheet model. - 1.1. Present glaciation. - 1.2. Motion equation for viscous ice in a thin boundary layer approximation. - 1.3. An ice sheet steady model. - 1.4. Numerical simulation of the evolution of the ice cover. - Chapter 2. A model of the world ocean. - 2.1. Zonal structure of the ocean. - 2.2. A one-dimensional ocean climate model. - 2.3. A simulation of the present ocean climate for assigned atmospheric climate. - Chapter 3. A model of the atmosphere. - 3.1. Zonal structure of the atmosphere. - 3.2. A one-dimensional atmospheric climate model. - 3.3. A simulation of the present atmospheric climate for assigned ocean climate. - 3.4. Estimates of climate variations in the Cenozoic. - Chapter 4. Numerical experiments with a model of the glaciers-ocean-atmosphere system. - 4.1. Glaciers, ocean and atmosphere interaction. - 4.2. A simulation of the present climate. - 4.3. On clarification of the "White Earth" concept. - 4.4. Nonuniqueness of climate. - 4.5. Sensitivity of the system to changes in the solar heat influx. - 4.6. Ice Ages. - 4.7. Influence of continent distribution on climate. - 4.8. On the change in the level of the World Ocean for possible climate warming. - 4.9. Estimates of the influence of the ocean oil pollution on climate. - Conclusion. - Abstract. - References. , In kyrillischer Schrift , Zusammenfassung in englischer Sprache
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  • 44
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-342
    In: Research report / Cold Regions Research and Engineering Laboratory
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental procedure. - Results. - Work-hardening effect. - Strain rate sensitivity of flow stress. - Discussion. - Conclusions. - Literature cited.
    Description / Table of Contents: Single crystals of high purity ice deformed by uniaxial compression on an Instron machine showed remarkable work-hardening after about 8% strain. By changing the strain rate during compression tests in the plastic region of the stress-strain curve, an apparent activation volume V* and a dislocation mobility exponent m were calculated from the strain rate sensitivity of flow stress. The large work-hardening and the rapid increase in the value of m beyond about 10% strain indicate that the plastic flow in this region is controlled by dislocation intersections and nonconservative motion of jogs.
    Type of Medium: Series available for loan
    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 342
    Language: English
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  • 45
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory,
    Associated volumes
    Call number: ZSP-202-329
    In: Research report
    Description / Table of Contents: CONTENTS: General Introduction. - Part I. Spatial and temporal variations in sea ice deformatfon. - Introduction. - Approach. - Site location and data collection procedures. - Data analysis. - Strain results. - Comparison of mesoscale deformation with macroscale deformation. - Nature of the ice pack rotation. - Conciusion. - Literature cited. - Part Il. Comparison of mesoscale strain measurements with linear drift theory predictions. - Introduction. - List of symbols. - Linear drift equations. - Ice drift solutions. - Comparison of theory with mesoscale measurements. - A more general linear constitutive law. - Conclusions. - Literature cited. - Appendix Relative magnitudes of differential drift forces. - Abstract.
    Description / Table of Contents: Measurements of mesoscale sea ice deformation over a region approximately 20 km in diameter were made over a five-week period in the spring of 1972 at the main AIDJEX camp in the Beaufort Sea. They have been analyzed to determine nonlinearities in the ice velocity field (due to the discrete small-scale nature of the ice pack), as well as a continuum mode of deformation represented by a least squares strain rate tensor and vorticity. The deformation rate time series between Julian day 88 and 113 exhibited net areal changes as large as 3% and deformation rates up to 0.16% per hour. In the principal axis coordinate system, the strain rate typically exhibited a much larger compression (or extension) along one axis than along the other. Persistent cycles at ~12-hour wavelengths were observed in the divergence rate. A comparison of the average residual error with the average strain rate magnitude indicated that strains measured on a scale of 10 km or greater can serve as a valid measure of the continuum motion of the sea ice. This conclusion is also substantiated by a comparison between the mesoscale deformation, and macroscale deformation measured over a ~100-km-diameter region. Vorticity calculations indicate that at low temporal frequencies ( 〈 0.04 hr^-1 ) the whole mesoscale array rotates essentially as an entity and consequently the low frequency vorticity can accurately be estimated from the rotation of a single floe. (Part I) A comparison of mesoscale strain measurements with the atmospheric pressure field and the wind velocity field indicated that the ice divergence rate and vorticity followed the local pressure and wind divergence with significant correlation. For low atmospheric pressures and converging winds, the divergence rate was negative with the vorticity being counterclockwise. The inverse behavior was observed for high pressures and diverging winds. This behavior agreed with predictions based upon the infinite boundary solution of a linearized drift theory in the absence of gradient current effects and using the constitutive law proposed by Glen for pack ice. The best least squares values of the constitutive law parameters [Eta] and [Zeta] were found to be given by ~10^12 kg sec^-1. Using typical divergence rates, these values yielded compressive stresses of the magnitude of 10^5 N m^-1, which are similar to values suggested by the Parmerter and Coon ridge model. In general, the infinite boundary solution of the linear drift equation indicates that in a low pressure region that is reasonably localized in space, the ice would be expected to converge for high compactness (winter) and diverge for low compactness (summer). Calculations were also carried out using a more general linear viscoelastic constitutive law that includes memory effects and that includes a generalized Hooke's law as well as the Glen law as special cases. A best fit of this more general calculation with strain measurements indicates, overall, a better agreement with viscous behavior than with elastic behavior, with the frequency behavior of the estimated "viscosities" similar to the Glen law behavior at temporal frequencies less than ~0.01 hr^-1 (Part II)
    Type of Medium: Series available for loan
    Pages: v, 37 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 329
    Language: English
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  • 46
    Series available for loan
    Series available for loan
    Hanover, N.H. : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-349
    In: Research report / Cold Regions Research and Engineering Laboratory, 349
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Test locations. - Post Pond. - Mascoma Lake. - Winter freeze-up. - Ice cover properties. - Stratigraphy. - Microstructure. - Porosity. - Impurity content. - Flexural strength. - Test sites. - Beam test procedure. - Beam dimensions. - Beam temperatures. - Beam strengths. - Results. - Post Pond, Site PB, 12 February 1974. - Post Pond, Site PC, 21 February 1974. - Mascoma Lake, Site MD, 25 February 1974. - Mascoma Lake, Site MD, 26 February 1974. - Mascoma Lake, Site MD, 1 March 1974. - Post Pond, Site PA, 4 March 1974. - Post Pond, Site PA, 7 March 1974. - Post Pond, Site PA, 8 March 1974. - Post Pond, Site PB, 12 March 1974. - Post Pond, Midway between Sites PB and PC, 15 March 1974. - Post Pond, Midway between Sites PA and PB, 26 March 1974. - Post Pond, Midway between Sites PA and PB, 29 March 1974. - Post Pond, Midway between Sites PA and PB, 3 April 1974. - Conclusions. - Literature cited.
    Description / Table of Contents: In-place cantilever beam tests on Post Pond and Mascoma Lake ice yielded a maximum flexural strength of 7.1 kg/cm^2. The minimum strength, unrelated to failure along pre-existing cracks in the ice, was 2.9 kg/cm^2. The majority of tests were performed in the push-down mode after it was discovered that beams tested in the pull-up mode, which places the bottom surface in tension, frequently broke prematurely along cracks in the bottom of the ice. Premature failures of this kind usually occurred at stresses of 2-3 kg/cm^2. Data further demonstrate that the intrinsic strength of lake ice decreases significantly as the surface air temperature goes to 0°C. Ice that has just become isothermal, but has not yet begun to candle, has a strength of about 4 kg/cm^2; ice that has been subjected to prolonged periods of above-freezing air temperatures generally fails at about 3 kg/cm^2. Tests also show that cold unrecrystallized snow-ice is as strong as the underlying lake ice. Tests of the effect of crystalline structure indicate that ice composed of crystals with their c-axes horizontal is measurably stronger than ice in which the crystals are oriented with their c-axes vertical.
    Type of Medium: Series available for loan
    Pages: v, 28 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 349
    Language: English
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  • 47
    Call number: ZSP-202-343
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental procedure. - Experimental and theoretical equations. - Results and discussion. - Conclusions. - Literature cited.
    Description / Table of Contents: Simultaneous laser extinction measurements were made in warm fog at wavelengths of 0.6238, 1.15 and 10.6 [Mu]. The warm fog was generated in a 4-m^3 environmental chamber. Particle sampling was carried out simultaneously with the laser measurements using an impactor. Using the same size distribution in each case the theoretical extinction coefficients were calculated and compared with the experimental coefficients. Results obtained during this experiment and aprevious one indicate that propagation at 1.15 [Mu] is adversely affected by the presence of atmospheric water vapor. Experimental data obtained simultaneously at 0.6328 and 10.6 [Mu] indicate that virtually no difference exists between the extinction coefficients at these two wavelengths for moderate particle concentrations while at much larger concentrations [Alpha]0.6328 increases indefinitely while [Alpha]10.6 levels off at 0.2.
    Type of Medium: Series available for loan
    Pages: iii, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 343
    Language: English
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  • 48
    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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  • 49
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-341
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Samples. - Collection. - Preparation. - Analytical methods. - Cations. - Lead, silicon and aluminum. - Sulfate. - Comparative analyses. - Results and discussion. - Sea salt and terrestrial dust. - Sulfate. - Lead. - Summary and conclusions. - Literature cited. - Appendix A. Concentrations of chemical constituents in Dye 3 snow and ice strata.
    Description / Table of Contents: Concentrations of sodium, potassium, magnesium, calcium, silicon, aluminum, lead and sulfate were measured in surface snow and in individual annual accumulation layers from a 373-m-deep ice core from Dye 3, Greenland, covering the time period from 1232 to 1971 A.D. Average background (pre-1840) concentrations in micrograms/liter are: Na, 12.9 ± 9.3; K, 2.2 ± 2.1; Mg, 1.5 ± 1.0; Ca, 4.8 ± 2.4; Si, 12 ± 6; Al, 3.3 ± 1.4; Pb, 0.07 ± 0.06; and SO4, 56 ± 22. Deviations are due mainly to the variability of the concentrations in the samples deposited over the stated time interval rather than analytical precision. Observed concentrations of sodium, potassium, magnesium, calcium, silicon and aluminum can be adequately explained by relative abundances of these elements in seawater andterrestrial dust. Late 19th century annual ice layers contain twice as much sulfate as pre-1840 deposits, reflecting the increased use of fossil fuels in the Northern Hemisphere. Lead concentrations in post-1955 snow deposits are more than an order of magnitude greater than pre-1840 baseline concentrations and are attributed to smelting and the increased use of lead alkyls in gasoline.
    Type of Medium: Series available for loan
    Pages: v, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 341
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  • 50
    Call number: ZSP-202-337
    In: Research report
    Description / Table of Contents: Contents: Introduction. - Surface ice observations. - Imagery interpretation. - Side-looking airborne radar. - Infrared. - Conclusions. - Literature cited.
    Description / Table of Contents: Ice conditions during mid-January 1974 in the Gulf of St. Lawrence and in the estuaty as far upstream as Rimouski are described utilitizing side-looking airborne radar, infrared and photographic imagery. The interpretations were verified by simultaneous surface observations on the ice by investigators operating from the CSS Dawson. The ice examined was undergoing rapid drift and deformation and showed a wide variety of thin ice (0-40 cm) features formed under the influence of strong winds and currents. These observations should serve as a guide in interpreting ice conditions in similar areas where ground truth data are not available.
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    Pages: 41 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 337
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  • 51
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45793 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 263 S. : Ill.
    Language: Russian
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  • 52
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    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(963-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 47-80 + 4 pl.
    Series Statement: U.S. Geological Survey bulletin; 963-B
    Language: English
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  • 53
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(970)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 74 S. + 7 pl.
    Series Statement: U.S. Geological Survey bulletin 970
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  • 54
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(965-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 281-353
    Series Statement: U.S. Geological Survey bulletin 965-C
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  • 55
    Call number: SR 90.0001(1839-A-D)
    In: U.S. Geological Survey bulletin
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    Pages: Getr. Zählung
    Series Statement: U.S. Geological Survey bulletin 1839-A-D
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  • 56
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(988-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: getr. Zählung
    Series Statement: U.S. Geological Survey bulletin 988-I
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  • 57
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(997)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 132 S. + 11 pl.
    Series Statement: U.S. Geological Survey bulletin 997
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  • 58
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(989-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 63-218 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 989-D
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  • 59
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1001)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 65 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1001
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  • 60
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1010)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 111 S. + 30 pl.
    Series Statement: U.S. Geological Survey bulletin 1010
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  • 61
    Monograph available for loan
    Monograph available for loan
    Montreal [u.a.] : McGill-Queen's Univ. Press
    Call number: PIK N 630-11-0268 ; AWI Bio-17-17112
    Type of Medium: Monograph available for loan
    Pages: XVIII, 361 S. : Ill., graph. Darst., Kt.
    ISBN: 0773512411
    Language: English
    Note: Contents: Figures. - Tables. - Preface. - Illustrations. - 1. Introduction. - 1.1 Background. - 1.2 Scope of the text. - 1.3 World vegetation types. - 1.3.1 Vegetation formations and zones. - 1.3.2 Zonobiomes. - 1.3.3 Exoclimates. - 1.3.4 The Canadian vegetation classification system. - 1.3.5 Ecozones. - 1.3.6 Floristic realms. - 1.3.7 Plant species nomenclature. - 1.4 Soil classification and soil systems. - 1.5 Climatic parameters. - 1.5.1 The role of climate. - 1.5.2 Moisture indices. - 1.5.3 Climate diagrams. - 1.6 Plant strategies. - 1.6.1 Competition. - 1.6.2 Hydrature and moisture regulation. - 1.6.3 Life forms. - 1.6.4 Leaf morphology and adaptation. - 1.7 Biomass and net primary productivity. - 2. Tundra 2.1 Tundra distribution. - 2.2 Climate. - 2.3 Soils. - 2.4 Tundra in North America. - 2.4.1 Ecoclimatic sub-provinces and regions. - 2.4.2 High and mid-Arctic. - 2.4.3 Low Arctic. - 2.5 Tundra in other Northern Hemisphere locations. - 2.5.1 Arctic Tundra. - 2.5.2 Typical Tundra. - 2.5.3 Southern Tundra. - 2.5.4 Tundra on Arctic Islands. - 2.6 Tundea in the Southern Hemisphere. - 2.6.1 The Antarctic Subregion. - 2.6.2 The Sub-Antarctic Subregion. - 2.7 Alpine Tundra. - 2.7.1 Temperate-latitude alpine Tundra. - 2.7.2 Low-latitude (equatorial) alpine Tundra. - 2.8 Primary production and phytomass in Tundra. - 3. Forest-Tundra or Boreal-Tundra Ecotone. - 3.1 Definitions. - 3.2 Distribution. - 3.3 Climate. - 3.4 Soils. - 3.5 Forest-Tundra in Canada. - 3.5.1 Ecoclimatic sub-provinces. - 3.5.2 The shrub subzone (Northern Forest-Tundra). - 3.5.3 The forest subzone (Southern Forest Tundra). - 3.6 Eurasian Forest-Tundra. - 3.7 Primary production and phytomass in forest-Tundra. - 4. Boreal Forest (Taiga) and Mixed Forest Transition. - 4.1 Distribution. - 4.2 Climate. - 4.3 Soils. - 4.4 Boreal forest in North America. - 4.4.1 Open Lichen Woodland. - 4.4.2 Northern Coniferous Forest. - 4.4.3 Mixed-Forest (Boreal-Broadleaf ecotone). - 4.4.4 Mixed-Forest transition to grassland (Northern Mixedwoods). - 4.5 Eurasian Boreal. - 4.5.1 The European Boreal. - 4.5.2 The Siberian Boreal. - 4.5.3 Northwest Pacific Fringe Boreal. - 4.6 Primary production and phytomass in boreal forest. - 5. Prairie (Steppe). - 5.1 Distribution. - 5.2 Climate. - 5.2.1 North America. - 5.2.2 Climate in Eurasia and elsewhere. - 5.3 Soils. - 5.4 Prairie in North America. - 5.4.1 The Canadian Prairie. - 5.4.2 Prairie in the USA. - 5.5. Eurasian Steppe. - 5.6 Southern Hemisphere Grasslands. - 5.6.1 The High Veldt. - 5.6.2 The Pampas/Campos Grasslands. - 5.7 Primary production and biomass. - 6. Cordilleran Environments in Western North America. - 6.1 Canada's Cordilleran ecoclimatic provinces. - 6.1.1 Distribution. - 6.1.2 Climate. - 6.1.3 Soils. - 6.1.4 Pacific Coastal Mesothermal Forest. - 6.1.5 Pacific Coastal Subalpine Forest. - 6.1.6 Cordilleran Forest Region. - 6.1.7 Cordilleran Cold Steppe and Savanna Forst. - 6.1.8 Canadian Cordilleran Subalpine Forest. - 6.1.9 Alpine Tundra and Boreal Forest. - 6.2 The Cordilleran Region in the USA. - 6.2.1 Distribution. - 6.2.2 Northwest Coast Conifer-Hardwood Forests. - 6.2.3 Montane Pine Forests. - 6.2.4 Sagebrush and Grasslands. - 6.2.5 Interior Hemlock-Douglas-Fir-Larch. - 6.2.6 Subalpine Forest. - 6.3 Primary Production and Phytomass. - 7. Temperate Deciduous Forests. - 7.1 Distribution. - 7.2 Climate. - 7.3 Soils. - 7.4 Temperate Deciduous Forest in North America. - 7.4.1 Canada. - 7.4.2 United States of America. - 7.4.3 Southern Mexico and South America. - 7.5 Europe. - 7.5.1 Atlantic Deciduous Forest. - 7.5.2 Central European Deciduous Forest. - 7.5.3 East European Deciduous Forest. - 7.6 Asia. - 7.7 Southern Hemisphere. - 7.8 Primary Production and Phytomass. - 8. Wetlands. - 8.1 Introduction. - 8.2 Climate. - 8.3 Soils. - 8.4 Canadian Wetland Classification. - 8.4.1 Canadian Wetland Classification System. - 8.4.2 Wetland classes. - 8.4.3 Wetland forms and types. - 8.5 Canadian Wetlands. - 8.5.1 Arctic Wetlands. - 8.5.2 Subarctic Wetlands. - 8.5.3 Boreal Wetlands. - 8.5.4 Prairie Wetlands. - 8.5.5 Temperate Wetlands. - 8.5.6 Oceanic Wetlands. - 8.5.7 Mountain Wetlands. - 8.6 Wetlands in the USA. - 8.7 Eurasian Wetlands. - 8.7.1 European Wetlands. - 8.7.2 Asian Wetlands. - 8.8 Central and South American Wetlands. - 8.9 African Wetlands. - 8.10 Austromalesian and Pacific Wetlands. - 8.11 Phytomass and Primary Production. - 9. Conclusion. - Appendix: Biomials and their local names as used in the text. - Bibliography. - Index.
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  • 62
    Monograph available for loan
    Monograph available for loan
    Moskva : Mosk. Otd. Gidrometeoizdata
    Associated volumes
    Call number: MOP Per 759(44)
    In: Trudy VNIIGMI MCD
    Type of Medium: Monograph available for loan
    Pages: 55 S.
    Series Statement: Trudy VNIIGMI MCD 44
    Language: Russian
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  • 63
    Series available for loan
    Series available for loan
    Moskva : Akad.
    Associated volumes
    Call number: ZSP-697-92-0615
    In: Rezul'taty issledovanij po meždunarodnym geofizičeskim proektam
    Type of Medium: Series available for loan
    Pages: 239 S. : Kt.
    Series Statement: Rezul'taty issledovanij po meždunarodnym geofizičeskim proektam
    Language: Russian
    Note: Contents: Preface. - Chapter 1. Glaciation of the earth and problems connected with it. - Chapter 2. Glaciation of the Urals. - Chapter 3. Glaciation of Scandinavia. - Chapter 4. Glaciation of the Pacific Arctic and Subarctic. - Chapter 5. Glaciation of the Arctic Islands: the Eurasian Arctic. - Chapter 6. Glaciation of the Arctic Islands: the Cannadian Arctic. - Chapter 7. Glaciation of Greenland. - Chapter 8. Arctic Ocean. - Chapter 9. Present-day glacio-climatic conditions in the North Polar area and their variations during historical time. - Chapter 10. History of Cenozoic glaciation. - Chapter 11. Causes of glaciation. - Conclusion. - Summary. - References. - Geographical Index. , In kyrill. Schr. - Zsfassung in engl. Sprache.
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  • 64
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A9-87-0348
    Type of Medium: Monograph available for loan
    Pages: 255 S. : Ill., graph. Darst.
    Language: Russian
    Note: In kyrill. Schr.
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  • 65
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: PIK N 630-13-0084 ; AWI Bio-22-20909
    Type of Medium: Monograph available for loan
    Pages: XII, 178 Seiten , Illustrationen
    ISBN: 0-521-30868-2 , 0-521-54409-2
    Language: English
    Note: Contents Preface Acknowledgements 1 Introduction Terms and abbreviations 2 The biogeographlcal setting Geology, physiography, and surface materials The structural framework Pleistocene geology Bioclimates Arctic and its three subzones Subarctic zone Boreal zone Eastern temperate zone Grassland zone Pacific and Cordilleran zones 3 Autecology and pollen representation Introduction Transcontinental, primarily boreal taxa Eastern, primarily temperate taxa Pacific-Cordilleran taxa Arctic taxa Modern regional pollen spectra The Western Interior The eastern plains transect The Pacific-Cordilleran transect General comments on the modern pollen spectra 4 Full-glacial refugla The southern refugia Pacific-Cordilleran refugia Interior plains and eastern region The Beringian refugia 5 Eastern Canada-fossil record and reconstruction Introduction The late glacial - 12,700 to 10,000 yr BP Southern Quebec and New Brunswick Maritime Canada The Great Lakes Basin Vegetation reconstruction The Holocene - 10,000 yr BP to the present Southern Quebec and New Brunswick The Maritimes, Labrador, and Northern Quebec The Great Lakes Vegetation reconstruction Boreal region 6 The Western Interior Sites near the forest-grassland transition Sites within the modern boreal forest Sites near the modern forest-tundra boundary 7 Pacific-Cordilleran region Southern Pacific zone Southern Cordilleran zone Northern Pacific zone Northern Cordilleran zone 8 Vegetation reconstruction and palaeoenvironments Introduction Origins and history Eastern temperate forests Boreal forest Grasslands and parklands Pacific-Cordilleran complex Tundra (arctic) Palaeoenvironmental controls Climate The Milankovitch model Full-glacial conditions Late-glacial and Holocene Fire Pathogens Paludification Problems for the future Climate disequilibrium Spatial resolution Pollen source area Concluding comments Appendix References Index
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  • 66
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gosudarstvennoe Izdatel'stvo Vodnogo Transporta
    Associated volumes
    Call number: AWI E2-13-0067-3
    In: Materialy nabljudenij naučno-issledovatel'skoj drejfujuščej stancii 1950/51 goda, Tom 3
    Type of Medium: Monograph available for loan
    Pages: 516 Seiten , Illustrationen
    Series Statement: Ėkz. 112
    Language: Russian
    Note: Содержание = Soderžanie = Inhalt: Предисловие = Predislovie = Vorwort. - Аэрометеорология = Aėrometeorologija = Aerometeorologie. - Метеорологические наблюдения приложение (таблицы) = Meteorologičeskie nabljudenija priloženie (Tablicy) = Anwendung meteorologischer Beobachtungen (Tabellen) / К. И. Чуканин = K. I. Čukanin. - Аэрологические наблюдения приложение (таблицы) = Aėrologičeskie nabljudenija priloženie (Tablicy) = Anwendung für Beobachtungen aus der Luft (Tabellen) / В. Г. Канаки, В. Е. Благодаров = V. G. Kanaki, V. E. Blagodarov. - Наблюдения над ветром по демпферному флюгеру приложение (таблицы) = Nabljudenija nad vetrom po dempfernomu fljugeru priloženie (Tablicy) = Beobachtungen über den Wind bei Dämpfer-Windfahnen (Tabellen) / М. М. Никитин = M. M. Nikitin. , In kyrillischer Schrift
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  • 67
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A4-77-0560
    Description / Table of Contents: In the monograph the author sets forth some features of the Southern Hemisphere stratosphere in every year season. It is done on the grounds of the average monthly baric topography Southern Hemisphere charts for 30 mb and also on the grounds of the daily radiosonding by some polar stations. Some urgent problems are examined in this work, they are the possibilities and character of the origin stratospheric rising in temperature, vertical power of the cold polar invasions in the middle latitudes, the pecularities of the spring and autumn field temperature changes and the polar region geopotential, the velopause topography over the polar region and some other problems. Differences in the stratospheric field temperature structure and the geopotential in the polar region of the northern and southern hemisphere are presented in the conclusion. In the first place the monograph is of interest to specialists in meteorology dealing with the atmospheric general circulation, weather forecasters - practical workers, geographers, geophysicists and students-meteorologists. It can also be of interest to specialists concerning with the atmospheric earth structure.
    Type of Medium: Monograph available for loan
    Pages: 110 S. : Ill.
    Language: Russian
    Note: In kyrill. Schr.
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  • 68
    Call number: AWI A3-90-0313 ; AWI A3-90-0313(2. Ex.)
    Type of Medium: Monograph available for loan
    Pages: 97 S. : graph. Darst.
    Language: Russian
    Note: In kyrill. Schr.
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  • 69
    Call number: AWI A4-90-0154 ; AWI A4-17-20945
    Type of Medium: Monograph available for loan
    Pages: 295 S. , Ill , 23 cm
    Language: Russian
    Note: In kyrill. Schr.
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  • 70
    Call number: ZSP-202-344
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Approach and methods. - Results. - Lake morphology. - Elongation. - Orientation. - Percentage cover (density). - Lake classification. - L1 unit. - L2 unit. - L3 unit. - L4 unit. - L5 and Lu units. - Other units. - Lake basin depths. - Ice volume and basin genesis. - Geological implications. - Conclusions. - Selected bibliography.
    Description / Table of Contents: The lakes of the Arctic Coastal Plain of northern Alaska were classified, based on size, shape, orientation and distribution, into six lake units and three nonlake units. Regional slope and relief were demonstrated to control lake size, the largest lakes occurring on the flattest, northernmost segment of the Coastal Plain. Using ERTS-1 sequential imagery and existing photography and data, lakes were grouped according to three depth ranges, 〈 1 m, 1-2 m and 〉 2 m. Deepest lakes have the longest period of summer ice cover. Ice on shallow lakes melts the earliest. Maximum depths of lakes were computed based on ice volume content of the perennially frozen ground (permafrost) and these agreed with observed values and ranges. The lake classification and regional ERTS-1 coverage also appear to provide additional information on the limits of late-Pleistocene transgressions on the Coastal Plain.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 344
    Language: English
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  • 71
    Call number: ZSP-202-348
    In: Detecting structural heat losses with mobile infrared thermography, Part III
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 348
    Description / Table of Contents: During the winter of 1973 - 74 a mobile infrared thermography system was used to survey the USA CRREL building at Hanover, New Hampshire. This report provides a description of excessive heat losses at several locations around the building. This report also discusses the need to carefully monitor meteorological conditions before starting a survey of a building exterior to determine if solar radiation decay from the building surface might interfere with thermographic analysis by masking the heat emanating from within the building.
    Type of Medium: Series available for loan
    Pages: ii, 9 S. : Ill.
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 348
    Language: English
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  • 72
    Call number: ZSP-202-346
    In: Research report / Cold Regions Research and Engineering Laboratory, 346
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - USA CRREL project and personnel involvement. - Part I. Introduction. - Background. - Literature review. - Part II. CRREL investigations from 1970 - 1974. - Initial literature survey (1970). - Oil detection kit development. - Survey of Cape Simpson, Alaska, natural crude oil seepages (1970). - Haines-Fairbanks military pipeline investigations (1971-1973). - Barrow investigations (1970-1974). - Fairbanks and Fox investigations. - Germination studies. - Physiological studies. - Dispersant studies. - Microbiological investigations. - Field investigations of accidental petroleum losses. - Part III. Recent related literature. - Part IV. Conclusions and recommendations. - USA CRREL reports, publications and presentations on Alaska oil spill research. - Literature cited.
    Description / Table of Contents: Knowledge concerning the biological effects of oil pollution on arctic and subarctic terrestrial ecosystems is limited. USA CRREL research personnel conducted investigations from 1970 through 1974 to expand information in this field. Objectives were to: 1) define the ecosystems most sensitive to the presence of crude oil or its refined products, 2) quantify and understand the injury response, and 3) establish time frames for manifestation of damage and natural restorative processes in arctic and subarctic regions. This was accomplished through: 1) surveys of natural oil seepages and past accidential spills in the Arctic and Subarctic, 2) initiation of controlled oil spills and 3) detailed laboratory investigations. Results demonstrated that terrestrial oil spills will to some degree be detrimental to both arctic and subarctic plant communities. Degree and longevity of damage will be influenced primarily by the magnitude of the spill, season of occurrence and existing soil moisture content. Rapid recovery of plant communities subjected to spills will occur only if root systems remain relatively unaffected. Damage will be more extensive and long-term when root systems are saturated with oil. Effects of damage will be manifested gradually over several seasons being influenced by winter stresses. Variation does exist in plant species susceptibility. Carex aquatilis, a predominant sedge of the arctic, is markedly resistant to crude oil damage. In the taiga Picea mariana is very susceptible. Plant recovery can be enhanced through the application of fertilizer. Fertilization, in addition to its direct effect on plant nutrition, will stimulate microbial decomposition of crude oil.
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    Pages: vii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 346
    Language: English
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  • 73
    facet.materialart.
    Unknown
    Athens : Institute of Geology and Mineral Exploration
    Call number: K 94.0026
    Pages: 1 Kt. in 4 Teilen
    Language: English
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  • 74
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(971)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 134 S. + 8 pl.
    Series Statement: U.S. Geological Survey bulletin 971
    Language: English
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  • 75
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(988-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 29-43 + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 988-C
    Language: English
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  • 76
    Series available for loan
    Series available for loan
    Trieste : Osservatorio Geofisico Sperimentale
    Associated volumes
    In: Bollettino di Geofisica Teorica ed Applicata
    Type of Medium: Series available for loan
    ISSN: 0006-6729
    Series Statement: Bollettino di Geofisica Teorica ed Applicata
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  • 77
    Call number: AWI A4-89-0036-1 ; AWI A4-78-0791-1 ; MOP 45231/A / Mitte
    In: Spravočnik po klimatu Antarktidy / pod red. I. M. Dolgina, Tom 1
    Description / Table of Contents: Contents: Foreword. - Geographical description of the Antarctic stations. - Solar radiation measurements in Antarctica. - Sunshine observations in Antarctica. - References. - Explanations to tables. - SECTION 1. SOLAR RADIATION AND NET RADIATION. - 1. Time of sunrise and sunset on the day dated the 15th. - 2. Sun's altitude at noon and at midnight on the day dated the 15th. - 3. Maximum Sun's altitude. - 4. Dates of the commencement and ending of the polar day and night. - 5. Mean monthly values of radiation fluxes. - 6. Mean monthly values of radiation fluxes with clear sky. - 7. Mean monthly values of total radiation fluxes with continuous total cloudiness. - 8. Mean monthly values of total radiation fluxes with continuous low cloudiness. - 9. Mean monthly values of net radiation with continuous total cloudiness. - 10. Mean monthly values of net radiation with continuous low cloudiness. - 11. Maximum values of radiation fluxes. - 12. Minimum values of radiation fluxes. - 13. Hourly and daily values of direct solar radiation at normal incidence. - 14. Hourly and daily values of direct solar radiation on a horizontal surface. - 15. Hourly and daily values of diffuse radiation. - 16. Hourly and daily values of total solar radiation. - 17. Hourly and daily values of net radiation. - 18. Extreme daily values of direct solar radiation at normal incidence. - 19. Extreme daily values of direct solar radiation on a horizontal surface. - 20. Extreme daily values of diffuse radiation. - 21. Extreme daily values of total solar radiation. - 22. Extreme daily values of net radiation. - 23. Frequency of daily values of direct solar radiation on a horizontal surface in ranges. - 24. Frequency of daily values of total solar radiation in ranges. - 25. Frequency of daily values of net radiation in ranges. - 26. Ten-day values of direct solar radiation at normal incidence. - 27. Ten-day values of direct solar radiation on a horizontal surface. - 28. Ten-day values of diffuse radiation. - 29. Ten-day values of total solar radiation. - 30. Ten-day values of absorbed radiation. - 31. Ten-day values of net radiation. - 32. Monthly and annual values of solar radiation and mean values of the surface albedo. - 33. Monthly and annual values of solar radiation with clear sky. - 34. Extreme monthly and annual values of direct solar radiation at normal incidence. - 35. Extreme monthly and annual values of direct solar radiation on a horizontal surface. - 36. Extreme monthly and annual values of diffuse radiation. - 37. Extreme monthly and annual values of total solar radiation. - 38. Extreme mean monthly and annual values of the surface albedo. - 39. Extreme values of the surface albedo. - 40. Extreme monthly and annual values of absorbed radiation. - 41. Extreme monthly and annual values of net radiation. - 42. Mean monthly values of radiation fluxes for the stations with short-period measurements. - 43.Mean monthly values of radiation fluxes for the period of anomalous decrease of the atmosphere transparency. - 44. Monthly and annual values of direct solar radiation at normal incidence. - 45. Monthly and annual values of direct solar radiation on a horizontal surface. - 46. Monthly and annual values of diffuse radiation. - 47. Monthly and annual values of total solar radiation. - 48. Mean monthly and annual values of the surface albedo. - 49. Monthly and annual values of absorbed radiation. - 50. Monthly and annual values of net radiation. - SECTION 2. SUNSHINE. - 51. Duration of sunshine. - 52. Mean duration of sunshine for the day with sunshine. - 53. Relative duration of sunshine. - 54. Number of days without sunshine. - 55. Diurnal variation of the duration of sunshine. - 56. Duration of sunshine: data for individual years. - 57. Mean sunshine duration for the day with sunshine: data for the individual years. - 58. Relative duration of sunshine: data for individual years. - 59. Number of days without sunshine: data for individual years. - Alphabetic index of stations (with the indication of the used period of observation). - List of meteorological stations ( in order of the mentioned data). - Meteorological stations location map.
    Type of Medium: Monograph available for loan
    Pages: 211 Seiten , Illustrationen
    Series Statement: Spravočnik po klimatu Antarktidy / pod red. I. M. Dolgina 1
    Language: Russian
    Note: In kyrillischer Schrift , Inhaltsverzeichnis in englischer Sprache (Seite 5-6)
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  • 78
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 40341 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 238 Seiten , Illustrationen
    Language: Russian
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  • 79
    Call number: MOP 47041 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 28 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
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  • 80
    Call number: MOP 44329 / Mitt
    Type of Medium: Monograph available for loan
    Pages: 295 S.
    Language: Russian
    Note: In kyrill. Schr.
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  • 81
    Monograph available for loan
    Monograph available for loan
    Moskva [u.a.] : Izdat. Akad. Nauk SSSR
    Call number: MOP 18582
    Type of Medium: Monograph available for loan
    Pages: 117 S.
    Language: Russian
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  • 82
    Call number: ZSP-202-347
    In: Research report / Cold Regions Research and Engineering Laboratory, 347
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental. - Results and discussion. - Applications. - Literature cited.
    Description / Table of Contents: Chemical analysis of century-old ice from continuous 5 to 7 year intervals of three ice cores from south and central Greenland (Dye 3, Milcent and Crete) show maximum concentrations of Na, Mg,Ca, K, and Al during early spring and minimum concentrations during late summer and early fall. Peak spring values are as much as 10 times greater than fall values. Because of the large seasonal chemical variations, samples used for depth-age or annual deposition rate studies must represent accumulation from exactly one year or whole multiples of a year. The seasonal chemical variations seem promising as a new method of defining annual layers and thus dating old ice cores.
    Type of Medium: Series available for loan
    Pages: iii, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 347
    Language: English
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  • 83
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-340
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Nomenclature. - Introduction. - Theory. - Application. - Literature cited. - Appendix.
    Description / Table of Contents: The equations describing water movement in a dry snow cover are derived and examples of flow through ripe, refrozen and fresh snows are given. The grain size of snow has a large effect on the timing of water discharge. Water is retained by dry snow to raise its temperature and satisfy the irreducible water saturation. These requirements delay and reduce runoff following rain on dry snow.
    Type of Medium: Series available for loan
    Pages: iv, 13 S. : graph. Darst.
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 340
    Language: English
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  • 84
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-336
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Nomenclature. - Introduction. - Description of study. - Sample preparation. - Test equipment and procedure. - Discussion of results. - Stress-density relationship. - Effect of rate of deformation. - Effect of temperature. - Effect of initial snow density. - Stress-deformation relationship. - Summary and conclusions. - Microstructural analysis. - Introduction. - Analytical methods. - Results and discussion. - Conclusion. - Literature cited. - Anpendix: Test data.
    Description / Table of Contents: The effects of snow temperature, rate of deformation, and initial density on the stress vs density and stress vs deformation relationships were investigated in the pressure range of 0.1 to 75 bars. The rate of deformation in the range of 0.027 to 27 cm sec^-1 does not have a significant effect. A decrease in temperature in the range of 0° to -40°C increases the resistance to stress and deformation, the temperature effect increasing with applied pressure and initial density. The effect of initial density is significant. For any stress, an increase in the initial density results in an increase in the resulting density, particularly at low stress levels and at temperatures near 0°C. The texture of artificially compacted snow is significantly different from that of naturally compacted snow of the same density because of the very short recrystallization time period.
    Type of Medium: Series available for loan
    Pages: iv, 57 Seiten , Illustrations
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 336
    Language: English
    Branch Library: AWI Library
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  • 85
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-333
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Analogy method. - Method based on the bending theory of elastic plates and the criterion [Sigma]max = [Sigma]f. - Methods based on viscoelastic theories. - Methods based on the yield line theory or limit analysis. - Comparison of analytical and test results. - General remarks. - Effect of bending and shearing forces on deflection of an ice cover. - Determination of Pf(O). - Determination of Pf(t). - Determination of [Sigma]f. - Summary and recommendations. - Literature cited.
    Description / Table of Contents: This report contains a critical survey of the literature on the bearing capacity of floating ice plates. It consists of a discussion of general questions, a critical survey of analytical attempts to determine the bearing capacity of floating ice plates, and a survey of field and laboratory tests on floating ice plates and their relation to the analytical results. The paper concludes with a systematic summary of the results, a discussion of observed shortcomings, and suggestions for needed investigations.
    Type of Medium: Series available for loan
    Pages: iv, 43 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 333
    Language: English
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  • 86
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-334
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols and associated dimensions. - Introduction and purpose. - Site characteristics. - Outline of study scheme. - Analysis. - Heat conduction to the drill hole. - Heat transfer between conduit wall and coolant. - Heat transfer between surface pipe and air. - Total heat extraction process. - Example calculations. - Estimate of basal water thickness and flow rates. - Summary of investigations of multiple-hole. - Literature cited.
    Description / Table of Contents: A scheme for cooling the lower portion of the edge of the Greenland ice sheet, which abuts a potential mining operation, is examined. The magnitude of cooling which may be accomplished by drilling a series of holes about the periphery of the mine site is determined as a function of hole size, spacing and time. Refrigeration is accomplished by pumping a coolant downhole in a central pipe, then uphole in an annulus between the pipe and hole wall, and then through a thin-walled pipe exposed to the surface climate above the ice sheet. It was found possible to achieve a temperature change in the ice of the order of -1°C with hole spacings and pumping requirements which are considered reasonable. Other effects are briefly examined and include an estimate of the basal water thickness and flow rates.
    Type of Medium: Series available for loan
    Pages: vii, 19 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 334
    Language: English
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  • 87
    Monograph available for loan
    Monograph available for loan
    St-Rémy-lès-Chevreuse : Association Francaise du Genie Parasismique
    Call number: M 15.0048
    Type of Medium: Monograph available for loan
    Pages: Getr. Zähl. : graph. Darst, Kt.
    Uniform Title: Guide méthodologique pour la réalisation d'études de microzonage sismique
    Language: English
    Location: Upper compact magazine
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    facet.materialart.
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    Roma : Consiglio Nazionale delle Ricerche Progetto Finalizzato Geodinamic
    Call number: K 95.0025
    Language: English
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  • 89
    Monograph available for loan
    Monograph available for loan
    Boston [u.a.] : Artech House
    Associated volumes
    Call number: M 92.1079/1
    In: Optical fiber sensors
    Type of Medium: Monograph available for loan
    Pages: XVI, 327 S.
    ISBN: 0890063176
    Classification:
    C.5.1.
    Language: English
    Location: Upper compact magazine
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  • 90
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(978-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 27-67 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 978-B
    Language: English
    Location: Lower compact magazine
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  • 91
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(976)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: S. 267-301, III S.
    Series Statement: U.S. Geological Survey bulletin 976
    Language: English
    Location: Lower compact magazine
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  • 92
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(982-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 95-119
    Series Statement: U.S. Geological Survey bulletin 982-D
    Language: English
    Location: Lower compact magazine
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  • 93
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(982-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI S., S. 153-244 + 5 pl.
    Series Statement: U.S. Geological Survey bulletin 982-F
    Language: English
    Location: Lower compact magazine
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  • 94
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(991-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 145-194
    Series Statement: U.S. Geological Survey bulletin 991-C
    Language: English
    Location: Lower compact magazine
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    Monograph available for loan
    Monograph available for loan
    Washington, DC : United State Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(988-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Monograph available for loan
    Pages: III S., S. 15-27
    Series Statement: U.S. Geological Survey bulletin 988-B
    Language: English
    Location: Lower compact magazine
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  • 96
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(988-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 69-122 + 10 pl.
    Series Statement: U.S. Geological Survey bulletin 988-E
    Language: English
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  • 97
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1000-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 50 S.
    Series Statement: U.S. Geological Survey bulletin 1000-A
    Language: English
    Location: Lower compact magazine
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    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Oxford Univ. Press
    Call number: M 97.0138
    Type of Medium: Monograph available for loan
    Pages: 343 S.
    ISBN: 0195085418
    Classification:
    Historical Geology
    Language: English
    Location: Upper compact magazine
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  • 99
    Call number: M 97.0217
    In: Mintrop-Seminar
    Type of Medium: Monograph available for loan
    Pages: 237 S.
    Series Statement: Mintrop-Seminar 17
    Classification:
    A.0.8.
    Language: English
    Location: Upper compact magazine
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  • 100
    GFZ publications
    GFZ publications
    Potsdam : GeoForschungsZentrum
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    Call number: 21/STR 97/08
    In: Scientific technical report
    Type of Medium: GFZ publications
    Series Statement: Scientific Technical Report / Geoforschungszentrum Potsdam 97/08
    Classification:
    Geodynamics
    Language: English
    Location: Reading room
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