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  • Books  (2,786)
  • English  (1,906)
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  • 1975-1979  (2,786)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Gotha : VEB Hermann Haack
    Call number: MOP 42610 / Mitte ; AWI G4-18-14336
    Type of Medium: Monograph available for loan
    Pages: 224 Seiten , Illustrationen
    Edition: 2. Auflage
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - 1. Wasserkreislauf, Wassermengen und Eigenschaften des Wassers. - 1.1. Herkunft des Wassers auf dem Festlande. - 1.2. Wassermengen auf der Erde. - 1.3. Wichtige Eigenschaften des Wassers. - 2. Flüsse. - 2.1. Fluß und Flußsystem. - 2.1.1. Bildung von Flüssen. - 2.1.2. Wichtige Begriffe aus der Flußkunde. - 2.1.3. Wichtige flußmorphametrische Begriffe. - 2.2. Gewässersystemarten. - 2.2.1. Normaltyp. - 2.2.2. Jungmoränentyp. - 2.2.3. Fossiler Inlandeisrandtyp im nördlichen Mitteleuropa. - 2.2.4. Trockengebietstyp. - 2.2.5. Karsttyp. - 2.3. Fluß und Relief. - 2.3.1. Fluß- und Talanlage. - 2.3.2. Durchbruchstäler. - 2.3.2.1. Epigenetische Durchbruchstalstrecken. - 2.3.2.2. Antezedente Durchbruchstalstrecken. - 2.3.3. Flußanzapfungen und Überschüttung von Wasserscheiden. - 2.3.4. Gewässer und Relief im Jungmoränenland. - 2.3.4.1. Phasen der Flußentwicklung im Jungmoränengebiet. - 2.3.4.2. Phasen der Seenentwicklung im Jungmoränengebiet. - 2.3.4.3. Ineinandergreifen beider Entwicklungsreihen. - 2.4. Abfluß und Schwankungen des Abflusses. - 2.4.1. Erfassung des Wasserstandes und Abflusses. - 2.4.1.1. Wasserstandsmessung. - 2.4.1.2. Abflußmessung. - 2.4.1.3. Abflußkurve und Abflußtafel. - 2.4.1.4. Hydrologisches Jahr und hydrologische Hauptzahlen. - 2.4.2. Abfluß und Abflußschwankungen. - 2.4.2.1. Hochwasser. - 2.4.2.2. Niedrigwasser. - 2.4.3. Eisbildung in Flüssen. - 2.4.4. Materialtransport. - 2.5. Riesenströme und Abfluß von den Kontinenten. - 2.5.1. Ordnung der Stromriesen nach der Lauflänge. - 2.5.2. Rangordnung der Riesenströme nach ihrer Einzugsgebiets- bzw. ihrer Niederschlagsgebietsgröße. - 2.5.3. Mittlerer jährlicher Abfluß der größten Ströme. - 2.5.4. Abflußmäßig größte Flüsse Europas. - 2.5.5. Mittlerer jährlicher Abfluß (MQ) und weitere Abflußdaten (MHQ, MNQ, HHQ und NNQ) von Flüssen der DDR. - 2.5.6. Abfluß von den Kontinenten. - 2.6. Abflußregime. - 2.6.1. Abflußregime und Regimefaktoren. - 2.6.2. Abflußregime nach M. Parde. - 2.6.2.1. Grundlagen der Klassifizierung nach M. Parde. - 2.6.2.2. Übersicht über die Klassifikation der Abflußregime nach M. Parde. - 2.6.2.3. Einige Bemerkungen zur Klassifikation von M. Parde und weiterführende Versuche. - 3. Seen. - 3.1. Seenverbreitung. - 3.1.1. Seen in ehemaligen und heutigen Inlandeis und Gletschergebieten. - 3.1.2. Seen in Trockengebieten. - 3.1.3. Seen in Vulkangebieten und Bereichen junger Erdkrustenbewegungen. - 3.1.4. Seen in Karst- und Auslaugungsgebieten. - 3.1.5. Seen in breiten Flußebenen. - 3.1.6. Seen an Ausgleichsküsten. - 3.2. Seebeckenentstehung. - 3.2.1. Glazialbecken. - 3.2.1.1. Seebecken im Bereich heutiger Gebirgsvergletscherung oder Inlandeisbedeckung. - 3.2.1.2. Seebecken im Abtragungsbereich letzteiszeitlicher Vergletscherung und Inlandeisbedeckung. - 3.2.1.3. Seebecken im Aufschüttungsbereich letzteiszeitlicher Inlandeisbedeckung und Vergletscherung. - 3.2.2. Bergsturz- und Erdrutschbecken. - 3.2.3. Tektonisch und vulkanisch angelegte Becken. - 3.2.4. Windwirkungsbecken. - 3.2.5. Lösungs- und Auslaugungsbecken, Abdämmung durch Sinterbildung. - 3.2.6. Becken fluvialen Ursprungs. - 3.2.7. Becken an Küsten. - 3.2.8. Becken pflanzlichen und tierischen Ursprungs. - 3.2.9. Anthropogen (durch die menschliche Gesellschaft) geschaffene Becken. - 3.2.10. Meteoritenfallbecken. - 3.3. Gestaltung, Verlandung und Form der Seebecken. - 3.4. Wasserhaushalt von Seen. - 3.5. Dichtemaximum und temperaturabhängige Schichtung des Wassers. - 3.6. Zirkulation und Stagnation. - 3.7. Thermische Seetypen. - 3.8. Biologische Seetypen. - 4. Unterirdisches Wasser (von Josef Saratka). - 4.1. Arten des unterirdischen Wassers. - 4.2. Hydrogeologische Eigenschaften der Gesteine. - 4.3. Bildung des unterirdischen Wassers. - 4.4. Zehrung des unterirdischen Wassers. - 4.5. Einige wichtige geohydrologische Begriffe. - 4.6. Grundwasserbewegung. - 4.7. Grundwasserstandsschwankungen. - 4.8. Unterirdisches Wasser in Klüften und Spalten, auf Schichtflächen und in Karsthohlräumen. - 4.9. Quellen und Grundwasserblänken. - 4.10. Mineralwässer- Säuerlinge - Thermalwässer. - 5. Gletscher. - 5.1. Inlandeis- und Gletscherverbreitung sowie Mächtigkeiten. - 5.2. Gletscherbildung. - 5.2.1. Schneegrenzen und Firnlinie. - 5.2.2. Metamorphose (Umwandlung) des Schnees in Gletschereis. - 5.3. Gletschertypen. - 5.3.1. Geomorphologische Einteilung der Gletscher. - 5.3.2. Gletschertypen - im Sinne einer einheitlichen Terminologie (nach H.-J. Schneider). - 5.3.3. Geophysikalische Einteilung der Gletscher (nach H. W. Ahlmann und M. Lagally). - 5.3.4. Einteilung der Gletscher nach dem dynamischen Zustand (nach H. W. Ahlmann). - 5.4. Gletscherbewegung und -gefüge. - 5.4.1. Gletscherbewegung. - 5.4.2. Gletschergefüge. - 5.5. Gletscherhaushalt und Gletscherschwankungen. - 5.5.1. Gletscherhaushalt. - 5.5.2. Gletscherschwankungen. - 6. Wasserkreislauf und Wasserhaushaltsbilanz. - 6.1. Erforschung von Wasserkreislauf und Wasserhaushaltsbilanz. - 6.2. Wichtige Begriffe. - 6.3. Wasserhaushaltsgleichung für die Erde. - 6.4. Erfassung der Wasserhaushaltselemente. - 6.4.1. Niederschlag auf die Landflächen der Erde (N L). - 6.4.2. Abfluß von den Landflächen der Erde (AL). - 6.4.3. Verdunstung von den Landflächen (VL). - 6.4.4. Verdunstung von den Meeresflächen (VM). - 6.4.5. Niederschlag auf die Meeresflächen (NM). - 6.5. Wasserkreislauf und Wasserhaushaltsbilanz der Erde. - 6.5.1. Wasserhaushaltsbilanzen für die Erde. - 6.5.2. Wasserkreislauf und Wasserhaushaltsbilanz der Erde. - Literaturauswahl.
    Location: MOP - must be ordered
    Location: AWI Reading room
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 2
    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
    Branch Library: AWI Library
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  • 3
    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
    Branch Library: AWI Library
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  • 4
    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
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    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
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 6
    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.
    Type of Medium: Series available for loan
    Pages: vii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 346
    Language: English
    Location: AWI Archive
    Branch Library: AWI Library
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  • 7
    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
    Location: AWI Archive
    Branch Library: AWI Library
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  • 8
    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
    Location: AWI Archive
    Branch Library: AWI Library
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  • 9
    Call number: M 18.91936
    Type of Medium: Dissertations
    Pages: 124 Seiten , graphische Darstellungen
    Language: German
    Note: Dissertation,Technische Hochschule Aachen, Fakultät für Bergbau und Hüttenwesen,1979
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 10
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/26
    In: CRREL Report, 76-26
    Description / Table of Contents: Debris over a 44-mile stretch of the Chena River was studied. The study area extended from the first bridge on the Chena Hot Springs Road to the Chena River Flood Control damsite. The purpose of the study was to assess the potential danger to the Chena River Flood Control Dam outlet structure. Debris was catalogued, log jams were measured, and sources of debris were studied. The average size of logs was determined, as well as the number of logs present on the river. The authors concluded that a serious debris problem existed and would remain serious for the foreseeable future. Recommendations for debris handling were made.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 76-26
    Language: English
    Note: Contents Abstract Preface Summary Introduction Origin of debris Volume, magnitude Types of debris Hazards of the debris Recommended measures to counteract log jamming Conclusions and recommendations Future work Epilogue Selected bibliography Appendix: Additional photographs of Chena River debris
    Location: AWI Archive
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