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  • Books  (192)
  • 1960-1964  (192)
  • AWI Library  (192)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Canada : Directorate of Scientific Information Services
    Call number: AWI G9-84-1168
    Type of Medium: Monograph available for loan
    Pages: 2, iii S. : Ill., Kt.
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  • 2
    Series available for loan
    Series available for loan
    New York : IGY World Data Center A, Glaciology
    Associated volumes
    Call number: AWI G7-85-0723
    In: IGY Glaciological Report
    Type of Medium: Series available for loan
    Pages: xiv, 197 p. : Ill.
    Series Statement: IGY Glaciological Report 5
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  • 3
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    Unknown
    Oslo : Norsk Polarinstitutt
    Call number: K-13-0038
    Pages: 1 Kt. in 4 Bl. ; 86 x 251 cm., sheets 66 x 79 cm or smaller
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  • 4
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI G7-92-0551
    In: Gljaciologiceskie issledovanija v period MGG
    Type of Medium: Monograph available for loan
    Pages: 233 S. : Ill., Kt.
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  • 5
    Call number: AWI E2-13-0068-2
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 653 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 2
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Contents: Предисловие = Predislovie = Foreword. - Метеорология = Meteorologija = Meteorology. - Метеорологические наблюдения = Meteorologičeskie nabljudenija = Meteorological observations. - Таблицы = Tablicy = Tables. - Актинометрия = Aktinometrija = Actinometry. - Актинометрические наблюдения = Aktinometričeskie nabljudenija = Actinometric observations. - Некоторые результаты наблюдений = Nekotorye rezul'taty nabljudenij = Some results of observations. - Таблицы = Tablicy = Tables. - , In kyrillischer Schrift
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  • 6
    Call number: ZSP-594/C-1
    In: Japanese Antarctic Research Expedition
    Description / Table of Contents: The chemical compositions of constituent minerals of metamorphic rocks of the area around Lutzow-Holm Bay in Antarctica are described along with their optic properties. The mineralogy and paragenesis of metamorphic rocks are interpreted as that the metamorphic rocks in this terrane belong to the granulite facies.
    Type of Medium: Series available for loan
    Pages: 12 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Geology 1
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  • 7
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
    Associated volumes
    Call number: ZSP-594/E-15
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 10 S. : Ill., graph. Darst.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 15
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  • 8
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-20
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 10 S.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports : Series E, Biology 20
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  • 9
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
    Associated volumes
    Call number: ZSP-594/E-11
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 10 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 11
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  • 10
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-138-4,1 ; ZSP-138-4,2
    In: Antarktika
    Type of Medium: Series available for loan
    Pages: 174 S. : Ill., graph. Darst.
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  • 11
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken
    Associated volumes
    Call number: ZSP-594/E-17
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 6 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 17
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  • 12
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
    Associated volumes
    Call number: ZSP-594/E-12
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 20 S. : Ill., graph. Darst.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 12
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  • 13
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-594/E-18
    In: Variations on some pennate diatoms from Antarctica
    Type of Medium: Series available for loan
    Pages: 20 S. : Ill., graph. Darst.
    Series Statement: 18
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  • 14
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-21
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 16 S.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports Series E, Biology 21
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  • 15
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
    Associated volumes
    Call number: ZSP-594/E-10
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 176 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 10
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  • 16
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/A-1
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 82 S. : graph. Darst.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series A, Aeronomy 1
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  • 17
    Call number: ZSP-594/E-16
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 8 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 16
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  • 18
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
    Associated volumes
    Call number: ZSP-594/E-13
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 7 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 13
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  • 19
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/D-1
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 12 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series D, Oceanography 1
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  • 20
    Call number: ZSP-697/B
    Former Title: Vorg. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / 9 / Gljaciologija i sejsmologija]
    Subsequent Title: Forts. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / Gljaciologiceskie issledovanija]
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  • 21
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdat. Akad. Nauk SSSR
    Call number: AWI G3-12-0050
    Type of Medium: Monograph available for loan
    Pages: 487 S. : Ill., Kt. + 2 Kt.-Beil.
    Series Statement: Prirodnye uslovija i estestvennye resursy SSSR
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  • 22
    Call number: AWI G7-83-0193
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 209 S.
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  • 23
    Call number: AWI G7-84-0845
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 265 S.
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  • 24
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/F-1 ; ZSP-594/F-1(2. Ex.)
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 12 S. : Ill.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series F, Logistics 1
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  • 25
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-23
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 14 S. : Ill.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports Series E, Biology 23
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  • 26
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-19
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 41 S. : Ill.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports : Series E, Biology 19
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  • 27
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/C-2
    In: Japanese Antarctic Research Expedition
    Description / Table of Contents: The East Ongul Island on the coast of the Lutzow-Holm Bukt, East Antarctica, was investigated from the tectonical and petrographical points of view. The rocks exposed in the island are petrographically classified into the following seven types : 1) Metabasites, 2) Pyroxene gneisses, 3) Hornblende gneisses, 4) Garnet gneisses, 5) Granites, 6) Feldspathic rocks, and 7) Pegmatites. It is verified that the unique structural feature of the island is represented by the isoclinal fold recumbent to the west with the frontal zone in which many small anticlinal as well as synclinal folds occur. The inner core of the main anticline is generally composed of the garnet gneisses with the pyroxene gneisses forming the outer mantle. The hornblende gneisses, which are distributed in front of the recumbent anticline, occur in the same horizon as the pyroxene gneiss, so the former may have been converted from the latter. This is also confirmed by the geological and petrographical observations. Besides, the hornblende gneiss zone coincides with the zone of granite and subsequent microcline pegmatite emplacement. The lineation of the rocks, represented by the undulating foliation, is defined to be a b-lineation parallel to the fold axis, but another lineation with the same character but perpendicular to the fold axis is also found. The fracture systems indicated by the pegmatite and joint patterns were analyzed by tectonic dating. The pegmatite intruded at the earlier folding stage, whereas the joint pattern was formed at the later upwarping stage. The gneisses and granites are classified mainly by the characteristic mafic minerals, and their modes of occurrence as well as the optical mineralogy are described. The optical data of the constituent minerals revealed that there is a tendency that the Fe/Mg ratio of the mafic minerals such as pyroxene, hornblende, biotite and garnet, may increase with acidity of the rocks, from the matabasites to the granites. The anorthite content of plagioclase is restricted within a rather narrow range between 22% and 35% when feldspar coexists with potash-feldspar, although that of plagioclase in metabasite and basic enderbitic pyroxene gneiss free from potash-feldspar ranges widely from 42% to 93%. The triclinicity of the potash-feldspar may become higher in the granite than the gneisses judging from the data of their 2V values. It is probable that the gneisses were formed originally under the condition of a granulite facies in the regional metamorphism. At the same time, the widespread developement of hornblende and biotite in the metabasites and gneisses suggests subsequent changes in temperature and pressure or the presence of water as well as changes in chemical composition which facilitated the mobilization and plastic deformation of the rocks. It is considered that two phases of metamorphism may be detected in the area; the granulite facies at an earlier phase and the amphibolite facies at a later phase. This has been suggested by the investigations not only in other regions of the East Antarctica but also in other Precambrian shields of the world.
    Type of Medium: Series available for loan
    Pages: 24 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Geology 2
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  • 28
    Call number: ZSP-697/B
    Parallel Title: 2=2; 3=3; 10=5a von [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / 12 / Sejsmologiceskie issledovanija]
    Subsequent Title: Forts. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / Gljaciologija]
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  • 29
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI G7-92-0552
    In: Gljaciologiceskie issledovanija v period MGG
    Type of Medium: Monograph available for loan
    Pages: 208 S.
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  • 30
    Call number: AWI E2-13-0068-4
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 4
    Type of Medium: Monograph available for loan
    Pages: 607 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 4
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Contents: Предисловие = Predislovie = Foreword. - Геофизина = Geofizika = Geophysics. - Ионосферные наблюдения = Ionosfernye nabljudenija = Ionospheric observations. - Таблица. Ионосферные данные = Tablica. Ionosfernye dannye = Table. Ionospheric data. - Магнитные наблюдения = Magnitnye nabljudenija = Magnetic observations. - Таблица 1. Ежечасные значения магнитных элементов D, Н, Z = Tablica 1. Ežečasnye značenija magnitnych ėlementov D, H, Z = Table 1. Hourly values of the magnetic elements D, H, Z. - Таблица 2. Ежечасные значения амплитуд горизонтальной составляющей rγH = Tablica 2. Ežečasnye značenija amplitud gorizontal'noj sostavljajuščej rγH = Table 2. Hourly values of amplitudes of the horizontal component rγH. - Таблица 3. Наблюденные значения магнитных элементов D, Н, Z = Tablica 3. Nabljudennye značenija magnitnych ėlementov D, H, Z = Table 3. Observed values of the magnetic elements D, H, Z. , In kyrillischer Schrift
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  • 31
    Call number: AWI E2-13-0068-3
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 3
    Type of Medium: Monograph available for loan
    Pages: 670 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 3
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Table of Contents. - Предисловие = Predislovie = Foreword. - Аэрология = Aėrologija = Aerology. - Методика и результаты аэрологических наблюдений = Metodika i rezul'taty aėrologičeskich nabljudenij = Method and results of upper-air observations. - Таблица 1. Географические координаты станций = Tablica 1. Geografičeskie koordinaty stancij = Table 1. Geographical coordinates of stations. - Таблица 2. Среднее месячное давление = Tablica 2. Srednee Mesjačnoe davlenie = Table 2. Average monthly pressure. - Таблица 3. Средняя месячная высота и температура изобарических поверхностей = Tablica 3. Srednjaja mesjačnaja vysota i temperatura izobaričeskich poverchnostej = Table 3. Average monthly height and temperature of isobaric surfaces. - Таблица 4. Средняя месячная плотность воздуха = Tablica 4. Srednjaja mesjačnaja plotnost' vozducha = Table 4. Average monthly air density. - Таблица 5. Средняя месячная температура = Tablica 5. Srednjaja mesjačnaja temperatura = Table 5. Average monthly temperature. - Таблица 6. Максимальная температура = Tablica 6. Maksimal'naja temperatura = Table 6. Maximum temperature. - Таблица 7. Минимальная температура = Tablica 7. Minimal'naja temperatura = Table 7. The minimum temperature. - Таблица 8. Средняя высота изотермических поверхностей = Tablica 8. Srednjaja vysota izotermičeskich poverchnostej = Table 8. The average height of isothermal surfaces. - Таблица 9. Повторяемость высоты нижней границы инверсий и изотермий и числа дней с инверсиями и изотермиями = Tablica 9. Povtorjaemost' vysoty nižnej granicy inversij i izotermij i čisla s inversijami i izotermijami = Table 9. Repeatability of the height of the lower boundary of inversions and isotherms and the number of days with inversions and isotherms Таблица 10. Средняя мощность инверсий и изотермий = Tablica 10. Srednjaja moščnost' inversij i izotermij = Table 10. The average power of inversions and isotherms. - Таблица 11. Средняя интенсивность инверсий и изотермий = Tablica 11. Srednaja intensivnost' inversij i izotermij = Table 11. The average intensity of inversions and isotherms. - Таблица 12. Средняя высота и температура нижней границы тропопаузы = Tablica 12. Srednjaja vysota i temperatura nižnej granicy tropopauzy = Table 12. The average height and temperature of the lower border of the tropopause. - Таблица 13. Повторяемость высоты нижней границы тропопаузы = Tablica 13. Povtorjaemost' vysoty nižnej granicy tropopauzy = Table 13. Repeatability of the height of the lower tropopause border. - Таблица 14. Повторяемость температуры нижней границы тропопаузы = Tablica 14. Povtorjaemost' temperatury nižnej granicy tropopauzy =Table 14. Repeatability of temperature of the lower tropopause border. - Таблица 15. Средняя месячнан относительная влажность = Tablica 15. Srednjaja mesjačnan otnositel'naja vlažnost' = Table 15. Average monthly relative humidity. - Таблица 16. Средняя месячная удельная влажность = Tablica 16. Srednjaja mesjačnaja udel'naja vlažnost' = Table 16. Average monthly specific humidity. - Таблица 17. Средняя высота нижней границы облаков = Tablica 17. Srednaja vysota nižnej granicy oblakov = Table 17. The average height of the lower boundary of the clouds. - Таблица 18. Средняя месячная скорость ветра = Tablica 18. Srednjaja mesjačnaja skorost' vetra = Table 18. Average monthly wind speed. - Таблица 19. Максимальная скорость ветра = Tablica 19. Maksimal'naja skorost' vetra = Table 19. Maximum wind speed. - Таблица 20. Повторяемость направления ветра = Tablica 20. Povtorjaemost' napravlenija vetra = Table 20. Wind direction repeatability. - Таблица 21. Результаты температурно-ветрового зондирования атмосферы = Tablica 21. Rezul'taty temperaturno-vetrovogo zondirovanija atmosfery = Table 21. Results of temperature-wind sounding of the atmosphere. - , In kyrillischer Schrift
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  • 32
    Call number: AWI G2-13-0066
    In: Ergebnisse der Limnologie
    Type of Medium: Series available for loan
    Pages: 90 Seiten , Illustrationen
    Series Statement: Ergebnisse der Limnologie 1
    Language: German
    Note: Inhaltsübersicht: A. Die Problemstellungen. - B. Überblick über die geomorphologische Entwicklung des Ostseeraumes. - 1. Der Baltische Schild und die ihn flankierenden Depressionen. - 2. Die Entwicklung des Ostseebeckens im Quartär. - I. Die Faktoren, die entscheidend die Morphologie Nordeuropas mitgestalteten. - II. Der Anteil der Weichsel-(Würm-)Vereisung an der morphologischen Formung. - III. Interglaziale Meerestransgressionen im Ostseeraum; Entwicklungsphasen der Ostsee im Spät- und Postglazial. - C. Eisstauseen des eurasischen Vergletscherungsgebietes als wesentliche Elemente des Smmelzwasserstromnetzes vor der Front des pleistozänen Inlandeises. - 1. Die Eisstauseen. - a) Im Gebiete des nordwesteuropäischen Kontinentalschelfes; die Reliktvorkommen in Großbritannien und Irland. - b) Entwicklungsgeschichte und Charakter des Südbaltischen Eisstausees. - c) Weichselzeitliche Stauseebildungen im Bereiche des Baltischen Landrückens. - d) Der Eisstausee im oberen Onega-Tal. - e) Das Becken des Weißen Meeres und seine Randgebiete. - f) Eisstauseen im östlichen Eurasien. - 2. Die Bedeutung der Lage und Verbreitung der Eisstauseen für die Lösung des Problems. - 3. Die Wasserscheiden im Raume des einstigen Pommersehen Stadiums und seines Hinterlandes. - 4. Die Abflußverhältnisse vor der Front des Inlandeises. - 5. Die Bedeutung der Richtung der Rückzugsbewegung des nordeuropäischen Inlandeises auf die Eiszentren in Fennoskandia. - D. Einwanderungsmöglichkeiten von Faunenelementen des Nördlichen Eismeeres in den Südbaltischen Eisstausee und in Binnengewässer Mittel- und Nordeuropas. - 1. Übersicht. - 2. Einwanderungsmöglichkeiten auf westlichen Wegen. - I. Der südwestliche Weg zwischen Jütland und Südschweden. - II. Die West-Ost-Verbindung vom Skagerrak-Kattegat über die mittelschwedischen Seen zum Ostseebecken. - 3. Einwanderungsmöglichkeiten auf östlichen Wegen. - I. Der nordöstliche Weg vom Weißen Meer über den Onega- und Ladoga-See zum Finnischen Meerbusen. - lI. Der Weg von der Kandalakscha-Bucht des Weißen Meeres zum Finnischen Meerbusen. - III. Der nordöstliche Weg unter Benutzung von Eisstauseen im Bereiche des Baltischen Landrückens und in den Küstenbezirken des Weißen Meeres. - a) Die Bedeutung der Brackwasser-Transgression beim Vorrücken der Kola- und Nowaja-Semlja-Gletscher. - b) Die Bedeutung des Langelancl-Vorstoßes für die Bildung von Eisstauseen und für die Hochschleusung von Reliktpopulationen aus dem Südbaltischen Eisstausee. - IV. Der Weg durch das Europäische Nordmeer entlang der norwegischen Küste zur Nord- und Ostsee. - 4. Der Einwanderungsweg von Pallasea quadrispinosa G. O. SARS. - E. Eisstauseen auf dem nordamerikanischen Kontinent und ihre Bedeutung für die Verbreitung mariner Glazialrelikte. - F. Die Vorkommen mariner Glazialrelikte an der Ostküste Gränlands. - G. Die Lebensmöglichkeiten während der weichselzeitlichen Rückzugsphasen. - H. Anlagen: I. Die Hauptstadien der Weichsel-Vereisung (Waldai-Vereisung der sowjetisehen Autoren) in Mittel- und Osteuropa. - II. Das nordamerikanische Vergletscheru:ngsgebiet: die Laurentische Inlandeisdecke. - III. Übersicht über die Hauptgliederung des Pleistozäns in Eurasien und Nordamerika. - I. Zusammenfassung. - K. Résumé. - L. Summary. - M. Schriftenverzeichnis (Auswahl).
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/A-2
    In: Japanese Antarctic Research Expedition
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    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
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    Call number: ZSP-594/E-14
    In: Biological results of the Japanese Antarctic Research Expedition
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/E-22
    In: Japanese Antarctic research expedition
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    Hanover, NH
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    Call number: ZSP-204-106
    In: CRREL Technical Report
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    Call number: ZSP-553-159,10
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  • 40
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    Oslo : Univ. Press [in Komm.]
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    Call number: ZSP-597-114
    In: Skrifter
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    Oslo : Univ. Press [in Komm.]
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    Call number: ZSP-597-131
    In: Skrifter
    In: Scientific results
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    Call number: ZSP-204-78
    In: CRREL Technical Report
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    Hanover, NH
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    Call number: ZSP-204-100
    In: CRREL Technical Report
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    Mannheim : Bibliograph. Inst.
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    Call number: ZSP-553-163,5
    In: Meddelelser om Grønland
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    Call number: ZSP-553-164,5
    In: Meddelelser om Grønland
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    Call number: ZSP-553-159,9
    In: Meddelelser om Grønland
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    Call number: ZSP-553-170,2
    In: Meddelelser om Grønland
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    Call number: ZSP-204-69
    In: CRREL Technical Report
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    Call number: ZSP-204-85
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    Call number: ZSP-204-97
    In: CRREL Technical Report
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    Hanover, NH
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    Call number: ZSP-204-102
    In: CRREL Technical Report
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    Call number: ZSP-204-104
    In: CRREL Technical Report
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    Call number: ZSP-204-121
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    Call number: ZSP-553-163,6
    In: Meddelelser om Grønland
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    Call number: ZSP-553-170,1
    In: Meddelelser om Grønland
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    Call number: AWI P9-90-0343b
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    København : Reitzel
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    Call number: ZSP-553-171,1
    In: Meddelelser om Grønland
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    Call number: ZSP-553-164,6 ; AWI P8-88-0281
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    Oslo : Univ. Press [in Komm.]
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    Call number: ZSP-597-123
    In: Skrifter
    In: Scientific results
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    Call number: ZSP-597-128
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    Call number: ad ZSP-597-114
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    Call number: M 93.0087/2 ; AWI G2-96-0027
    In: The sea ; 2, Vol. 2
    Type of Medium: Monograph available for loan
    Pages: xv, 554 S. , Ill., graph. Darst.
    Language: English
    Note: CONTENTS: THE COMPOSITION OF SEA-WATER. - SECTION I. CHEMISTRY. - 1. THE OCEANS AS A CHEMICAL SYSTEM / BY E. D. GOLDBERG. - 1. The composition of sea-water. - 2. Reactivities of the elements. - 3. Chemical reaction in the oceans and the compositions of the end-products. - 4. Space and time distributions of the elements. - 2. THE INFLUENCE OF ORGANISMS ON THE COMPOSITION OF SEAWATER / BY A. C. REDFIELD, B. H. KETCHUM AND F. A. RICHARDS. - 1. Introduction. - 2. The biochemical cycle. - 3. The biochemical circulation. - 3. ARTIFICIAL RADIOACTIVITY IN THE SEA / BY Y. MIYAKE. - 1. Artificial radioactivity in oceanic waters. - 2. Enrichment of radioactive substances in marine products. - 3. Artificial radioactivity as a tracer of water movements in the ocean. - 4. Disposal of radioactive waste in the ocean. - 4. RADIOISOTOPES AND LARGE-SCALE OCEANIC MIXING / W. BROECKER. - 1. Introduction. - 2. Useful isotopes. - 3. Steady-state distribution of 14C. - 4. Ocean-atmosphere CO2 exchange rates. - 5. Oceanic mixing models. - 6. Industrial CO2 effect. - 7. 226Ra distribution. - 8. 90Sr distribution. - 9. Non-steady-state conditions. - 10. Conclusion. - 5. CHEMICAL INSTRUMENTATION / BY D. E. CARRITT. - 1. Introduction. - 2. Chlorinity, salinity, density and related properties. - 3. Water tagging and tracer techniques. - 4. Measurement of dissolved gases. - 6. WATER SAMPLING AND THERMOMETERS / BY H. F. P. HERDMAN. - 1. Sampling. - 2. Thermometry. - SECTION II. FERTILITY OF THE OCEANS. - 7. PRODUCTIVITY, DEFINITION AND MEASUREMENT / BY E. STEEMANN NIELSEN. - 1. Introduction. - 2. Definitions. - 3. Methods for measuring primary production. - 4. The relation between the rate of gross production and net production below a surface unit. - 5. Transparency of the water versus organic production. - 6. The significance of single individual measurements of primary production. - 7. The influence of weather conditions. - 8. ORGANIC REGULATION OF PHYTOPLANKTON FERTILITY / BY L. PROVASOLI. - 1. Introduction. - 2. Data from chemical analysis. - 3. Organic products of algae and bacteria. - 4. Nutritional requirements of marine algae. - 5. Crustacea and organic solutes. - 6. Data from biological analysis of sea-water. - 7. Prospects. - 8. Addendum. - 9. BIOASSAY OF TRACE SUBSTANCES / BY W. L. BELSER. - 1. Introduction. - 2. Vitamins. - 3. Amino acids. - 4. Purines and pyrimidines. - 5. Perspectives. - COMPARATIVE AND DESCRIPTIVE OCEANOGRAPHY. - SECTION III. CURRENTS. - 10. EQUATORIAL CURRENT SYSTEMS / BY J. A. KNAUSS. - 1. Methods of study of ocean currents. - 2. Gross circulation pattern. - 3. A two-layer ocean - the thermocline. - 4. Zonal fiow-geostrophic currents. - 5. Meridional flow-upwelling. - 6. Conclusions and speculations. - 11. EASTERN BOUNDARY CURRENTS / BY W. S. WOOSTER AND J. L. REID, JR. - 1. Introduction. - 2. Common features of eastern boundary currents. - 3. Coastal upwelling. -4. Poleward eastern boundary currents. - 5. Biological implications. - 12. THE SOUTHERN OCEAN / BY G. E. R. DEACON. - 1. Topography. - 2. Oceanographic data. - 3. Wind zones. - 4. The water-masses. - 5. Climatology and zoogeography. - 6. Nutrient salts. - 7. Future needs. - 13. DEEP-CURRENT MEASUREMENTS USING NEUTRALLY BUOYANT FLOATS / BY G. H. VOLKMANN. - 1. Introduction. - 2. The pinger. - 3. Measurements. - 14. DROGUES AND NEUTRAL-BUOYANT FLOATS / BY J. A. KNAUSS. - 15. ESTUARIES / BY W. M. CAMERON AND D. W. PRITCHARD. - 1. Definition of estuaries. - 2. General considerations. - 3. Estuarine circulation patterns. - 4. Some variations on the estuarine sequence. - 5. Flushing in estuaries. - 6. Dynamics of estuaries. - 7. Kinematic description of the distribution of properties in an estuary. - 16. APPLICATIONS OF THE GYROPENDULUM / BY W. S. VON ARX. - 1. Introduction. - 2. The gyropendulum. - 3. The problem of time variations. - SECTION IV. BIOLOGICAL OCEANOGRAPHY. - 17. GEOGRAPHIC VARIATIONS IN.PRODUCTIVITY / BY J. H. RYTHER. - 1. Introduction. - 2. Incident radiation. - 3. Transparency. - 4. Nutrients. - 5. Latitudinal variations in the stability of surface water. - 6. Productivity of the major oceanic regions. - 7. Hydrodynamic features which influence productivity. - 8. Plankton production in coastal and inshore waters. - 9. Production of benthic plant communities. - 18. BIOLOGICAL SPECIES, WATER-MASSES AND CRRRENTS / BY M. W. JOHNSON AND E. BRINTON. - 1. Introduction. - 2. Water-masses and biological species. - 3. Water currents and biological species. - 19. COMMUNITIES OF ORGANISMS / BY E. W. FAGER. - 1. Introduction. - 2. Definition of community. - 3. Identification of communities. - 4. Community structure. - 5. Community function. - 6. Community theory. - 20. THEORY OF FOOD-CHAIN RELATIONS IN THE OCEAN / BY G. A. RILEY. - 1. Introduction. - 2. Mathematical models of plankton populations. - 3. Complex versus simple models. - 4. Prognosis for mathematical models. - 5. Higher elements of the food chain. - 21. FISHERY DYNAMICS - THEIR ANALYSIS AND INTERPRETATION / BY M. B. SCHAEFER AND R. J. H. BEVERTON. - 1. Introduction. - 2. The Beverton-Holt approach. - 3. The Schaefer approach. - 4. Concluding remarks. - SECTION V. OCEANOGRAPHICAL MISCELLANEA. - 22. SEASONAL CHANGES IN SEA-LEVEL / BY JUNE G. PATTULLO. - 1. Introduction. - 2. The observed seasonal variations. - 3. Factors influencing variations in sea-level. - 4. Summary. - 5. Conclusions. - 23. BATHYSCAPHS AND OTHER DEEP SUBMERSIBLES FOR OCEANOGRAPHIC RESEARCH / BY R. S. DIETZ. - 1. Introduction. - 2. Diving chambers. - 3. Bathyscaphs. - 4. Diving saucer. - 5. Buoyant-hulled deep ships or bathynauts. - 6. Deep-research vessel (D.R.V.). - 7. Remote underwater manipulator (RUM). - 8. Concluding remarks. - 24. DEEP-SEA ANCHORING AND MOORING / BY JOHN D. ISAACS. - 1. Introduction. - 2. Historical background. - 3. Problems of taut-mooring. - 4. Remarks on components of moorings. - 5. Mooring cables. - 6. The anchors. - 7. Fittings. - 8. Performance. - AUTHOR INDEX. - SUBJECT INDEX.
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    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0087/1 ; AWI G2-96-0026 ; MOP 34194
    In: The sea ; 1, Vol. 1
    Type of Medium: Monograph available for loan
    Pages: xv, 864 S. , Ill., graph. Darst., Kt.
    Edition: 1. publ.
    Language: English
    Note: CONTENTS: PHYSICAL OCEANOGRAPHY. - SECTION I. FUNDAMENTALS. - 1. PHYSICAL PROPERTIES OF SEA-WATER / BY N. P. FOFONOFF. - 1. The equilibrium thermodynamic state. - 2. Equation of state for sea-water. - 3. Entropy. - 4. Chemical potential difference. - 5. The non-equilibrium state. - 6. Other physical properties of sea-water. - 2. THE EQUATIONS OF MOTION OF SEA-WATER / BY CARL ECKART. - 1. Introduction. - 2. Thermodynamics. - 3. Hydrodynamics. - 4. The irreversible processes. - 5. Transformation of the equation. - 6. The zeroth approximation. - 7. The first approximation. - 8. Definitions related to convective motion. - 9. The field equations. - SECTION II. INTERCHANGE OF PROPERTIES BETWEEN SEA AND AIR. - 3. SMALL-SCALE INTERACTIONS / BY E. L. DEACON AND E. K. WEBB. - 1. General considerations of transfer. - 2. Momentum transfer and the wind-profile. - 3. Drag coefficients of the sea surface. - 4. Transfer of heat and water vapour. - 4. LARGE-SCALE INTERACTIONS / BY JOANNE S. MALKUS. - 1. Introduction. - 2. How the whole system works. - 3. Determination of air-sea fluxes. - 4. Climatology of energy exchange and the global heat and water budgets. - 5. Heat and water exchange and its role in tropical circulations. - 6. Large-scale momentum relations. - 7. Exchange mechanisms and fluctuations. - 8. Exchange fluctuations in mid-latitudes and long-period interaction anomalies. - 9. Concluding remarks. - 5. INSOLUBLES / BY R. W. REX AND E. D. GOLDBERG. - 1. Meteorology of transport. - 2. Eolian materials in marine sediments. - 6. SOLUBLES / BY A. H. WOODCOCK. - 7. GASES / BY R. REVELLE AND H. E. SUESS. - 1. Introduction. - 2. Oxygen and nitrogen. - 3. Rare gases. - 4. Carbon dioxide. - SECTION III. DYNAMICS OF OCEAN CURRENTS / BY N. P. FOFONOFF. - 1. Conservation equations for momentum and mass. - 2. Separation into steady and time-dependent motion. - 3. Magnitude of forces. - 4. Steady-state circulation. - 5. Steady inertial circulation. - 6. Convective circulation. - 7. Time-dependent motion. - SECTION IV. TRANSMISSION OF ENERGY WITHIN THE SEA. - 8. LIGHT / BY J. E. TYLER AND R. W. PREISENDORFER. - 1. Physical constructs. - 2. Instrumentation for the measurement of the underwater light field and the determination of the optical properties of the sea. - 3. Radiance distribution. - 4. Attenuation coefficient. - 5. Volume scattering functions and total scattering coefficient. - 6. Irradiance. - 7. Diffuse attenuation function and reflectance function. - 8. Scalar irradiance (spherical irradiance). - 9. Absorption coefficient. - 10. Path function. - 11. Data. - 12. Applications. - 13. List of symbols. - 9. UNDERWATER VISIBILITY / BY S. Q. DUNTLEY. - 1. Image transmission. - 2. Inherent contrast. - 3. Sighting range. - 10. LIGHT AND ANIMAL LIFE / BY G. L. CLARKE AND E. J. DENTON. - 11. OTHER ELECTROMAGNETIC RADIATION / BY L. N. LIEBERMANN. - 1. Introduction. - 2. Electromagnetic properties of sea-water. - 3. Propagation through sea-water. - 4. The effect of the sea-surface on electromagnetic propagation. - 5. Natural electromagnetic radiation or "noise" in the sea. - 12. SOUND IN THE SEA / BY P. VIGOUREUX and J. B. HERSEY. - 1. The nature of sound. - 2. Propagation of sound in water. - 3. Noise. - 4. Instruments and applications of sound to oceanography. - 13. SOUND SCATTERING BY MARINE ORGANISMS / BY J. B. HERSEY AND R. H. BACKUS. - 1. Introduction. - 2. Occurrence and description of scattering layers. - 3. Identification of sound scatterers. - 4. Sound-scattering theory. - 5. Sound-scattering observations. - 6. What is "the deep scattering layer"?. - 7. Ideas and miscellaneous observations. - 14. SOUND PRODUCTION BY MARINE ANIMALS / BY W. E. SCHEVILL, R. H. BACKUS, AND J. B. HERSEY. - 1. Introduction. - 2. History. - 3. Instrumentation. - 4. Identification of source. - 5. Purposeful and adventitious sounds. - 6. Sound-producing mechanisms. - 7. Spectra of sounds. - 8. Functions of sound. - 9. Hearing as related to sound production. - 10. Eliciting and suppressing marine animal sounds. - 11. Exploitation of marine animal sounds by the oceanographer. - SECTION V. WAVES. - 15. ANALYSIS AND STATISTICS / BY D. E. CARTWRIGHT. - 1. Introduction. - 2. Fundamental equations of wave motion. - 3. Statistical formulation. - 4. Properties of a wave system in terms of its directional energy spectrum. - 5. Estimating the directional energy spectrum. - 6. Waves recorded by a single detector. - 7. Spectral measurement. - 8. Second-order approximations to energy spectra. - 16. LONG-TERM VARIATIONS IN SEA-LEVEL / BY J. R. ROSSITER. - 1. Introduction. - 2. The determination of mean sea-level. - 3. Causes of variations in sea-level. - 4. The analysis of observations. - 5. Some geophysical implications of long-term variations in sea-level. - 6. Conclusion. - 17. SURGES / BY P. GROEN AND G. W. GROVES. - 1. Introduction. - 2. Description. - 3. Dynamics and forecasting. - 18. LONG OCEAN WAVES / BY W. H. MUNK. - 1. Introduction. - 2. The instruments. - 3. The spectrum. - 4. Surf beat. - 5. Shelf waves. - 6. Tsunamis. - 19. WIND WAVES / BY N. F. BARBER AND M. J. TUCKER. - 1. Kinematics of waves. - 2. The description of a complicated wave pattern: the wave spectrum. - 3. Theories of wave generation by wind. - 4. Wave prediction. - 5. Waves from distant storms. - 6. Waves approaching the shore. - 7. The surf zone. - 8. Ships and waves. - 9. Methods of observation and analysis-methods taking no account of direction of travel. - 10. Methods of observation and analysis - the directional power spectrum. - 20. MICROSEISMS / BY J. DARBYSHIRE. - 1. Relation between sea waves and microseisms. - 2. The nature of microseisms. - 3. Refraction of microseisms. - 4. Storm tracking and estimation of the direction of approach of microseisms. - 5. Estimation of direction from the nature of microseisms. - 6. Instruments. - 7. Other work. - 21. RIPPLES / BY C. S. COX. - 1. Spectrum and mean square slope. - 2. Effect of slicks. - 3. Shape of a rippled water surface. - 4. Growth of ripples. - 22. INTERNAL WAVES : Part I / BY E. C. LAFOND. - 1. Introduction. - 2. Measurements. - 3. Observed relations. - 22. INTERNAL WAVES : Part II / BY C. S. COX. - 4. Differential equations. - 5. Spectrum. - 6. Internal waves and turbulence. - 23. TIDES / BY W. HANSEN. - 1. Introduction. - 2. The hydrodynamic equations and their application to tidal problems. - 3. Tidal observation. - 4. Tidal charts. - 5. Classical theory. - 6. Numerical methods for ascef!.aining the tides and tidal currents. Boundary-value problems. - 7. The application of difference methods to initial-boundary problems. - 8. Numerical solutions of initial-boundary-value problems of tides in one and two dimensions. - 9. Internal tides. - SECTION VI. TURBULENCE / BY K. F. BOWDEN. - 1. General properties of turbulence. - 2. Turbulence in the sea. - 3. Turbulent fluctuations and turbulent transports. - 4. Vertical turbulence. - 5. Horizontal turbulence. - SECTION VII. THE PHYSICS OF SEA-ICE / BY E. R. POUNDER. - 1. Introduction. - 2. Mechanical properties. - 3. Thermal properties. - 4. Electrical properties. - 5. Growth and disintegration of an ice cover. - 6. Theory of sea-ice structure and properties. - AUTHOR INDEX. - SUBJECT INDEX.
    Location: Upper compact magazine
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  • 68
    Monograph non-lending collection
    Monograph non-lending collection
    Bruxelles
    Associated volumes
    Call number: AWI PY-5831
    In: Expédition Antarctique Belge 1957-1958 : Résultats Scientifiques ; Vol. 3, Fasc. 1, Vol. 3, Fasc. 1
    Type of Medium: Monograph non-lending collection
    Pages: 174 S , graph. Darst., Kt
    Series Statement: Expédition Antarctique Belge 1957-1958 : résultats sientifiques ; Vol. 3, Fasc. 1
    Language: French
    Note: Table des Matières: Liste des figures. - Avant propos. - Préambule. - Introduction. - 1. Programme du Géomagnétisme. - 2. Situation de la base Roi Baudouin et plans des installations. - 3. Installation de la station de Géomagnétisme. - Pavillon des mesures absolues. - Pavillon des enregistreurs. - Le géomagnétisme au bâtiment "Science". - Installations électriques. - 4. Les instruments. - Nomenclature et description. - Etablissement du méridien magnétique et orientation des aimants des variomètres. - Installation et réglage des instruments. - 5. Les températures. - Variations journalières pour chaque variomètre. - Moyennes et écarts max. - Humidité relative. - 6. Les temps. - Controle et correction du temps. - Temps vrai de la station. - 7. Les magnétogrammes. - Marquage et magnétogrammes disponibles. - Magnétogramme du 8/9/1958 et description de l'aurore. - 8. Méthodes d'observation. - Constantes, méthodes de mesure utilisées, calculs. - Valeurs d'echelle et parallaxes. - Valeurs tabulées des mesures absolues. - 9. Mesures magnétiques en campagne. - Etablissement des stations. - Températures, durée et nombre des mesures. - Azimuts et temps. - Valeurs tabulées des mesures. - 10. Difficultés rencontrées et propositions. - Choix du terrain et installation des pavillons. - Solutions proposées pour la stabilité des pilliers. - Résumé des caractéristiques principales de la station. - Bibliographie.
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  • 69
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Longmans
    Call number: AWI P7-17-90975
    Type of Medium: Monograph available for loan
    Pages: XVI, 328 S. , Ill., Kt., graph. Darst.
    Edition: 1st publ.
    Series Statement: Geographies for advanced study
    Language: English
    Note: Contents: Preface. - 1. Introduction. - 2. History of Arctic exploration. - 3. The meteorology and climate of the Arctic. - 4. Landforms of the Arctic. - 5. The Arctic Seas. - 6. Arctic flora and fauna. - 7. Native peoples. - 8. Transportation. - 9. Political geography of the Arctic. - 10. Regional description of the Canadian Arctic. - 11. Alaska. - 12. The Soviet Arctic. - 13. Svalbard. - 14. Greenland. - 15. The history of Antarctic exploration. - 16. The Antarctic continent. - 17. Meteorology and climate of the Antarctic. - 18. The Antarctic Seas. - 19. The sub-Antarctic islands. - Index.
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  • 70
    Monograph available for loan
    Monograph available for loan
    Leningrad : Izdatel'stvo Leningradskogo Universiteta
    Call number: AWI G1-19-92227
    Type of Medium: Monograph available for loan
    Pages: 445 Seiten , Illustrationen
    Series Statement: Zemnoj magnetizm / B.M. Janovskij 1
    Language: Russian
    Note: In kyrillischer Schrift
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  • 71
    Series available for loan
    Series available for loan
    Hanover, New Hampshire : U.S. Army Material Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-145
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 145
    Description / Table of Contents: An analysis is made of the time required to build up an ice-age ice sheet and of the time required to destroy such an ice sheet. The calculations are based on the approximation that the theory of perfect plasticity is valid. It is concluded that the time required to eliminate it. If it is assumed that the accumulation rate of an ice-age ice sheet lies of a large ic sheet is of the order of 15.000 to 30.00 years. Ablation rates of 1 to 2 meters/year lead to shrinkage times of the order of 2000 to 4000 years, provided ablation occurs over an appreciable area of the ice sheet.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 145
    Language: English
    Note: Contents: Preface. - Summary. - Introduction. - Basis of theory. - Basic equations. - Ice sheets with only accumulation or ablation. - Growing ice sheets which contain only an accumulation zone. - Shrinking ice sheets which contain only an ablation zone. - Comments. - Ice sheet with both accumulation and ablation zones. - Growing ice sheets. - Shrinking ice sheets. - Conclusions. - References.
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  • 72
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-117
    In: Research report / Cold Regions Research and Engineering Laboratory, 117
    Description / Table of Contents: Summary: An experiment was designed to investigate operator-variance in the determination of the plastic limit of cohesive soils, independent of sample preparation and hydration time. A standard sample was prepared by dry-mixing commercial clay, "Grundite", with a pure silt. After the sample was hydrated for 3 weeks, five random samples were taken and five replicates performed on each sample. Analysis of variance (AOV) shows that there is no reason to doubt that the sample is homogeneous at the 0.05 level of significance. Random samples were then distributed to five zones of operators, where a zone is defined as a group of operators with similar backgrounds and engineering interests. Two operators from each group performed five replicates. The AOV model used in the analysis is mixed with the upper level fixed and the two lower levels random. The estimated "within" and "between" operator variances are 0. 45 and 4. 18 respectively. The estimated "between zones" contribution to the total sum of squares is negative. No correlation was found between an operator's internal variance and his deviation from the grand mean. On the basis of this experiment, no reason-exists to doubt that an "untrained" operator can obtain results comparable to those of professional operators. The major factor contributing to the total sample variance is the inconsistency between the individual operators who, although able to duplicate their own determinations, do not call the same end point. To minimize between operator variance, a readily prepared standard sample is suggested with which any operator can calibrate his plastic limit determinations against the expected national average.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 117
    Language: English
    Note: CONTENTS Preface Summary ­Introduction Sample preparation Sample homogeneity Distribution of samples Analysis Conclusions and suggested standardization References
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  • 73
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-118
    In: Research report / Cold Regions Research and Engineering Laboratory, 118
    Description / Table of Contents: Summary: The observation that newly frozen ice sheets, resulting from pools of -water freezing over,- support more than would be predicted by ordinary theory is assessed. A solution is presented for a circular plate on an elastic, sealed foundation. Graphical results are shown for supports at the circumference of the plate. Graphs to obtain moments in a circular plate on an elastic bearing surface, using a sealed or unsealed foundation, are compiled for fixed and simple supports. In reality the foundation may not be completely sealed, calling for discretion in selecting the actual moment. The ability of the refrozen ice sheet to support the extra load is explained by the fact that the water has been sealed between the surface and main sheet of ice and the volume occupied by the water cannot change.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 118
    Language: English
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  • 74
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-62
    In: Research report / Cold Regions Research and Engineering Laboratory, 62
    Description / Table of Contents: Summary: Adhesive strength of ice for the systems ice/stainless steel and ice/optically flat fused quartz has been investigated as a function of surface roughness of steel surfaces and rates of shear for steel and quartz. The adhesive strength decreases with decreasing roughness of steel surfaces and the force vs time curves for smooth steel plates resemble those of two solids sliding over each other with a liquid layer sandwiched between them. This is particularly so in the case of quartz. The adhesive strength as a function of rate of shear is linear both for ice/stainless steel and ice/quartz; however, there are indications of yield values. The experimental results are in agreement with the assumption of a liquidlike layer on ice. Ratios of viscosity coefficient to the thickness of the layer have been evaluated for both systems and viscosity coefficients are estimated. The importance of interfacial free energy considerations is pointed out.
    Type of Medium: Series available for loan
    Pages: iii, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 62
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental Materials Apparatus Experimental results Ice/metal interface Ice/quartz interface Discussion References
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  • 75
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-67
    In: Research report / Cold Regions Research and Engineering Laboratory, 67
    Description / Table of Contents: Summary: The temperature distribution in snow subjected to gamma radiation from an operating nuclear reactor is analyzed mathematically, assuming that the effect of radiation is equivalent to a continuous heat source, the intensity of which is a function of the radial distance from the reactor. Steady-state solutions are derived for two cases: when the radial distance is 13 ft and when it is 19.1 ft. The results indicate that the temperature of the snow in certain regions in the several feet immediately below the foundation will exceed the design limit of 20°F. Increasing the shielding of the reactor will reduce the intensity of the radiation and snow temperature. Other possible ways to reduce the snow temperature include the use of refrigeration coils and the forcing of the atmospheric air through the snow.
    Type of Medium: Series available for loan
    Pages: iii, 4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 67
    Language: English
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  • 76
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-63
    In: Research report / Cold Regions Research and Engineering Laboratory, 63
    Description / Table of Contents: Summary: Experiments have been carried out on the plastic deformation of thick-walled snow-ice cylinders under hydrostatic pressure as a function of pressure and temperature. At constant circumferential stress and temperature the natural strain rate of closure is a constant. This constant varies with the circumferential stress according to a sine function and is exponentially dependent on temperature with an energy of activation of 14.1 kcal/mole at an average circumferential stress of 3.1 kg/cm^2. The mechanism of the plastic flow is in agreement with a mechanism proposed previously, that is, flow between grain boundaries takes place.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 63
    Language: English
    Note: CONTENTS Preface Summary Experimental Materials Apparatus Experimental results Deformation under constant hydrostatic pressure Deformation as a function of hydrostatic pressure Deformation as a function of temperature at constant pressure Discussion References
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  • 77
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-119
    In: Research report / Cold Regions Research and Engineering Laboratory, 119
    Description / Table of Contents: Summary: An experimental investigation of stress-wave propagation in snow and ice is described. Seven types of Greenland snow were investigated to determine the extent to which the variation in dynamic response of the snow is a function of snow types, and were compared with results of similar Michigan snow experiments. A low-density explosive charge was detonated, sending a steep-fronted shock wave through a metal transfer plate and into the snow sample, compressing the snow and setting it in motion. Measurements were made on shock waves with amplitudes of less than 200 atm. Density and pressure behind the wave fronts were determined by simultaneous measurement of wave-propagation and particle velocity as limited by the fast elastic wave and the slow plastic wave of the two-front structure. Values calculated by the Rankine-Hugoniot jump conditions determined the points at which the material behaves plastically or hydrodynamically. The maximum stable pressure-volume states that snow can reach under shock loading are also shown. Sources of scatter in the results from variations in snow type and errors in data reduction and geometry changes are pointed out.
    Type of Medium: Series available for loan
    Pages: v, 25, A11 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 119
    Language: English
    Note: CONTENTS Test area description Experimental techniques Explosive initiation system Grid lines on snow Grid lines on driving plates The streak camera Synchronization of camera and event Synchronization of flash bulb and event Timing-light generator High-speed framing camera
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  • 78
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-69
    In: Research report / Cold Regions Research and Engineering Laboratory, 69
    Description / Table of Contents: Summary: The relations between rate of snow accumulation, snow density, snow age, and depth below the surface are formulated in terms of a compactive viscosity factor, which is assumed to be a function of only density and temperature, with parameters which will vary with the snow-type sequences of different climatic areas of high polar glaciers. The theory could be useful in an analysis of the data obtained from the large number of snow pits in Greenland, Ellesmere Island,and Antarctica.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 69
    Language: English
    Note: CONTENTS Preface Summary Introduction The Sorge depth-density curve Generalization for time-variable rate of accumulation Path of a particle on the surface y=B(h,t) Effect of temperature Computational procedure Densification under high loads References
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  • 79
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI A19-98-0104
    In: The Scientific Papers of J. Willard Gibbs
    Type of Medium: Monograph available for loan
    Pages: XXVI, 434 S.
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  • 80
    Call number: AWI A19-98-0105
    In: The Scientific Papers of J. Willard Gibbs
    Type of Medium: Monograph available for loan
    Pages: VIII, 284 S.
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  • 81
    Call number: AWI E3-89-0395
    Description / Table of Contents: Sowjetische und amerikanische Antarktisforscher schüttelten sich Anfang 1959 am geographischen Südpol die Hände. Eine Kolonne sowjetischer Raupenschlepper hatte nach einem einzigartigen Marsch, der über Tausende von Kilometern hinweg durch bisher unerforschte Eiswüste führte, die amerikanische Station Amundsen-Scott erreicht. Und diese herzliche Begrüßung am Südpol ist charakteristisch für den Geist, in dem Vertreter von mehr als einem Dutzend Staaten seit Beginn des "Internationalen Geophysikalischen Jahres" in Antarktika zusammenarbeiten. Englische und französische, belgische, japanische, polnische WissenschaftIer und neuerdings auah solche aus der Deutschen Demokratischen Republik sind dabei, dem unter mächtigen Eismassen begrabenen sechsten Kontinent seine so lange gehüteten Geheimnisse zu entreißen. Überragenden Anteil daran, haben aber sowjetische Expeditionen, die ihre Stützpunkte am weitesten ins Innere des Kontinents vorschieben konnten. Höhen von 4000 Metern, unvorstellbar niedrige Temperaturen bis zu minus 88 Grad Celsius, die niedrigsten, die jemals an der Erdoberfläche gemessen wurden, ständig tobende Schneestürme, monatelange Polarnacht, die nur hin und wieder vom fahlen Licht des Südlichts erhellt wird - das sind die Bedingungen, unter denen die Besatzungen dieser Stationen arbeiten und überwintern müssen. Der Geograph Trjoschnikow leitet die Zweite Sowjetische Antarktisexpedition, deren Hauptaufgabe es ist, vom Küstenstützpunkt Mirny aus ins Innere des Erdteils vorzustoßen und dort weitere Stationen einzurichten. Mit vollem Bedacht wird gerade er für dieses schwierige Unternehmen ausgewählt: Schon viele Jahre hat Trjoschnikow in polaren Gebieten gearbeitet, so manche lange Polarnacht auf den driftenden Stationen in der Arktis zugebracht. Und er versteht es auch, den Leser die unerhörten Strapazen, die großen Erfolge miterleben zu lassen; er erzählt von den schweren Opfern an Menschen und Material, die trotz Einsatz modernster technischer Hilfsmittel auch jetzt noch gebracht werden müssen, berichtet vom Leben der amerikanischen Kollegen im USA-Hauptstützpunkt "Little America". - Ein Buch, das jeden packen wird, der sich über die Antarktis unterrichten will.
    Type of Medium: Monograph available for loan
    Pages: 287 Seiten , Illustrationen, Karten
    Uniform Title: Zakovannyj v led 〈dt.〉
    Language: German
    Note: Inhaltsverzeichnis: Der erste Tag in Antarktika. - Hochsommer. - Die Traktoristen bestehen ihr Examen. - In der Luft und auf dem Eis. - Ins Innere des Kontinents. - 24 Uhr Moskauer Zeit. - Bei Kilometer 100. - Aus meinem Tagebuch. - Pionerskaja. - Was lehrte und der Marsch ins Innere?. - Der Speicher im Eis. - Wo soll die Ladung gelöscht werden?. - Katastrophe aud der Eisbarriere. - Die Flagge wird gehißt. - In Mirny brennt es!. - Der Schlittenzug auf dem Marsch. - Ein ungewöhnlicher Vorfall. - Flug nach Komsomolskaja. - Wostok 1 entsteht. - Wir müssen vorübergehend zurückweichen. - Erfolge der Geologen und Biologen. - Pinguine und Sturmvögel. - Beginn der Überwinterung. - So vergeht Tag um Tag. - Wütend heult der Sturm. - Im Labyrinth der Gletscherspalten verirrt. - Festtage in Mirny. - Unsere Nachbarn. - Alltag in Antarktika. - Winterflüge. - Die Flieger helfen uns aus der Klemme. - Dem Frühling entgegen. - Bei den "Eingeborenen" von Antarktika. - Little America - "Klein-Amerika". - Orkan. - "Brigade Uch!". - Die Amerikaner auf dem sechsten Kontinent. - Nachricht vom Nachbar. - So war das Wetter im August. - Australische Gäste in Mirny. - Luftaufklärung. - In der Bunger-Oase. - Neues vom amerikanischen Hauptstützpunkt. - Probe für den großen Marsch. - Kurs Süd. - In der Zone der "Drachenzähne". - Siedlung auf Schlitten. - Und weiter geht der Marsch. - Die Leute von Wostok 1. - Minus 74° Celsius!. - Komsomolskaja ersteht von neuem. - "Frühling" im Schnee. - Die Ablösung trifft ein. - Alle Mann an die Arbeit!. - Der Vormarsch wird fortgesetzt. - Am geomagnetischen Südpol. - Flug zum Pol der relativen Unzugänglichkeit. - Abschied von Antarktika. - Der Heimat entgegen!. - Anmerkungen. - Tabelle: Höhe der Gletscheroberfläche über dem Meeresspiegel.
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  • 82
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-70
    In: Research report / Cold Regions Research and Engineering Laboratory, 70
    Type of Medium: Series available for loan
    Pages: 93 Seiten , Karten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 70
    Language: English
    Note: CONTENTS: Preface. - Summary. - Chapter I. Introduction. - Operations and logistics. - Chapter II. Methods of investigation. - Region of investigation. - Pit studies. - Elevation measurements. - Chapter Ill. Stratigraphy and accumulation. - Introduction. - Diagenesis without melt. - Diagenesis with melt. - Diagenetic facies defined on glaciers. - Grain size. - Description of three stratigraphic features. - Principles of stratigraphic interpretation. - Selection of a reference datum in the annual stratigraphic sequence. - Stratigraphic correlation. - Distribution of annual accumulation. - Independent checks on the stratigraphic interpretations. - Chapter IV. Temperature distribution. - Seasonal temperature variation on the snow surface. - Seasonal temperature variation below the snow surface. - Distribution of mean annual temperature on the ice sheet. - Chapter V. Diagenetic facies- a classification of glaciers. - Temperature. - Hardness. - Density. - Glacier facies - a classification of glaciers. - Chapter VI. Densification of snow and firn. - Load-volume relationship. - Depth-density relationship. - Chapter VII. Climatological implications. - Introduction. - Katabatic winds and accumulation. - Annual heat exchange. - The balance of the Greenland Ice Sheet. - References. - Appendix A: Stratigraphy, meteorology and glaciology. - Appendix B: Mean annual temperature. - Appendix C: The data sheets.
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  • 83
    Call number: AWI A3-20-93434-2
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 2
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,2
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 84
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    Call number: ZSP-202-112
    In: Research report / Cold Regions Research and Engineering Laboratory, 112
    Description / Table of Contents: Summary: The age hardening of artificially and naturally compacted snow has been investigated at the South Pole. Results show that the age-hardening process is greatly retarded at low temperatures. Artificially compacted samples of density 0.55 g/cm^3 attained a compressive strength of less than 3.0 kg/cm^2 after one year's aging at -49°C. Exposure to solar radiation accelerated the age hardening. Irradiated samples attained a strength of 6.0 kg/cm^2 after 100 hr, increasing to a virtual maximum of 8.0 kg/cm^2 at 600 hr. Compressive strengths increased witha decrease in snow-particle size and with an increasing angularity of the particles. Below 3 m the strength of naturally compacted snow was found to increase rapidly with an increase in density. Naturally compacted snow of density 0.55 g/cm^3 possessed considerably greater strength than any of the age-hardened samples of artificially compacted snow of the same density. Thin-section studies show that age hardening can be correlated with the formation and growth of intergranular bonds, and that bond growth falls off rapidly with decreasing temperature. In view of the low strength found in both naturally and artificially compacted snow at the South Pole, "cut-and-cover" undersnow camp construction may not prove practical at the South Pole.
    Type of Medium: Series available for loan
    Pages: v, 19, A6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 112
    Language: English
    Note: CONTENTS Preface Summary Introduction Previous work Experimental methods Experimental results Series A Series B Series C Series D Series E Discussion Conclusions References Appendix A
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  • 85
    Call number: AWI A3-20-93434
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 1
    Type of Medium: Series available for loan
    Pages: 121 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,1
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 86
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-115
    In: Research report / Cold Regions Research and Engineering Laboratory, 115
    Description / Table of Contents: SUMMARY Between 1 July and 7 August 1960, the U.S. Army Snow Ice and Permafrost Research Establishment, Corps of Engineers, supported a £our-man glaciological expedition on the southern dome of the Greenland ice sheet. Measurements of snow temperature, density, ram hardness, and grain size were made at seven pit ~tudies along 191 mileS of over-snow traverse. In addition to the pit studies, 38 Rammsonde profiles were measured and 166 shallow pits were dug to measure temperature in the first meter of snow. The annual accumulation of snow was found to decrease westward, from 97 em water equivalent 50 miles from tP.e east coast, to 40 em 80 miles from the western margin. A possible precipitation shadow was encountered immediately west of the crest line of the ice sheet. The precipitation shadow and the decrease in accumulation westward indicate that the source area for the precipitation lies to the east of the southern dome, in the. Greenland Sea. Temperature profiles in the firn indicated that summer warming was still in progress. During August, melting at an elevation of 2000 m above se~ level was intense (OC in the top 75 em} •. According to the facies classification of glaciers (Benson, 1959, 1960}, most of the study area is in tfie percolation facies, with the possible exception of the westernmost· s.tation (mile l-138) which is at or near the saturation line. The daily heat exchange in the first meter of snow, near the time of maximum melt conditions, is between 20 and '35 cal/cinZ. This is approxi-mately 25o/o of the heat necessary to raise the temperature of a column of firn of unit cross Section and 1 m deep to the melting point. Effective values of thermal conductivity and diffusivity as determined from the temperature curves with no attempt made to isolate radiation and con-vection are, respectively, 4-6 x 10-3 cgs and 20-30 x 10-3 cgs. Radiation and convection in the first meter of firn cause "effective conductivity" values to be 4 to 7 times greater than the value k = 0. 0068pZ given by Abel's (1892), which is the conductivity at greater depths.
    Type of Medium: Series available for loan
    Pages: v, 22, A4, B1 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 115
    Language: English
    Note: CONTENTS Preface Summary Introduction Method of investigation Location Pit studies Temperature Hardness Density Stratigraphic measurements Thermal studies Stratigraphic features Grain size Grain shape Crusts Discussion of results Temperature Altitude gradient Latitude gradient Depth-density relationship Depth-load relationship Densification Stratigraphic analysis Facies relationship Climatological aspects 1960 meteorological observations Temperature Wind Barometric pressure Radiation Cloudiness Visibility Thermal studies Summary and conclusions References Appendix A Appendix B
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  • 87
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-60
    In: Research report / Cold Regions Research and Engineering Laboratory, 60
    Description / Table of Contents: Summary: This report presents numerical results on the feasibility study of the use of in-ice cooling for a power plant. As a result of this type of arrangement, a water pond under ice is formed. The pond size as a function of time for various operating conditions has been computed. The associated problems such as water temperature, power consumption, etc., are also studied.
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    Pages: iv, 17, A6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 60
    Language: English
    Note: CONTENTS Preface Summary Introduction Open-loop system Method of analysis Time dependence of pond size Temperature of water in the pond Effect of inlet water temperature Effect of convection duct Power consumption for circulation of cooling water Condlusions Closed-loop system Method of analysis Time dependence of pond size Flow conditions of glycol solutions inside coil Discussion and conclusions References Appendix: Examples of calculations
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  • 88
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-71
    In: Research report / Cold Regions Research and Engineering Laboratory, 71
    Description / Table of Contents: Summary: The depth-density relationship of the surface snow to 30-ft depth at three locations on the Greenland Ice Cap east of Thule is presented. Rates of accumulation and densification deduced from the pit studies are used in elementary mathematical expressions developed in this report. These expressions describe a densification process applicable to continuously accumulating polar snow, between the depths of 10 and 40 ft. Loads, densities, and rates of densification are presented in relation to depth and time and applied to problems of undersnow military construction.
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    Pages: iv, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 71
    Language: English
    Note: CONTENTS Preface Summary Introduction Field investigations Application of profile data Densification theory Engineering applications References
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  • 89
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-78
    In: Research report / Cold Regions Research and Engineering Laboratory, 78
    Description / Table of Contents: Summary: This climatological study makes use of the temperature, wind, and precipitation records from 12 stations on the Greenland Ice Sheet. Many of these stations were not in operation for concurrent periods and records for a year or more were available from only a few of them. The mean, mean maximum, mean minimum, absolute maximum, and absolute minimum temperatures were computed from the records. The highest absolute maximum temperature reported was 44°F at Mint Julep in southwestern Greenland. The lowest absolute minimum was -94°F at Northice in northern Greenland. This study shows that the prevailing wind usually was from the direction of the high central area of the ice sheet. Stations on the west slope had prevailing winds with an easterly component whereas stations on the east slope had prevailing winds with a westerly component. The wind speed varied from 0 to approximately 60 kt, but was predominantly in the 0 to 20 kt range. At some of the stations on the ice sheet, precipitation was measured in precipitation gages, at others it was measured as surface accumulation. At many locations the annual accumulation was determined from stratigraphic studies of the snow profile. The number of days on which snow occurred, expressed as percent of total days of observation, was used as an index to the amount of snowfall. The mean annual accumulation shows precipitation to be heavier on the west slope of the ice sheet than in other areas. The precipitation records at Northice indicate that the annual precipitation in that part of northern Greenland may be very light. The means for the various climatological parameters covered in this study are presented in tables and on a climatological map which presents a cartographic picture of the overall climatology of the Greenland Ice Sheet.
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    Pages: iv, 13, A5, B4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 78
    Language: English
    Note: CONTENTS Preface Summary Introduction Air temperature Wind direction and speed Precipitation and accumulation Climatological map for the Greenland Ice Sheet Appendix A: Temperature data Appendix B: Precipitation data
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  • 90
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-80
    In: Research report / Cold Regions Research and Engineering Laboratory, 80
    Description / Table of Contents: From the Introduction: During the last few years, there has been an increased interest in developing a rational explanation for the rather considerable variation in such bulk properties of sea ice as its strength, density, thermal conductivity, latent heat of melting, and coefficient of thermal expansion. Of these properties, sea-ice strength has received by far the most attention for practical reasons.
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    Pages: iv, 30, A6, B10, C2, D5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 80
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimentation Method of growing salt ice Strength test procedures Bulk properties of salt ice Phase relations Density and air content Strength results Strength of fresh-water ice Strength of NaCl ice as a function of brine volume Strength of NaCl· 2H2O ice as a function of the relative volume of solid salt Effect of thermal history on salt-ice strength Phase hysteresis Geometric hysteresis Effect of short-term cooling on the strength of fresh-water and NaCl·2H2O ice Effect of the volume of inclosed air on the strength of salt ice Conclusions NaCl ice Sea ice References Appendix A: Volume of brine and NaCl· 2H2O in NaCl ice as a function of salinity and temperature Appendix B: Ring test results Normal test sequences Appendix C: Ring test results Hysteresis test sequences Appendix .b: Ring test results Thermal history test sequences
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  • 91
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-85,1
    In: Research report / Cold Regions Research and Engineering Laboratory, 85,1
    In: The frost behavior of soils : laboratory and field data for a new concept, Part I
    Description / Table of Contents: Partial summary: Laboratory experiments have been performed with special cabinets in which soil samples, under complete saturation and without surcharges, were subjected to alternate freezing and thawing cycles. Tests included series with both freezing and thawing from the top and with freezing from the bottom and thawing from the top. The soil materials used were well-graded, sandy gravels, the finest one with 14% finer than no. 200 mesh (0. 074 mm).
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    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 85,1
    Language: English
    Note: CONTENTS Preface Summary Introduction to the problem Laboratory data Preliminary experiments Vertical sorting and volume changes produced by cyclic freeze -thaw Volume increase by sorting in straight graded samples without freezing and thawing Field data Vertical sorting of the active layer Correlation between laboratory and field data Conclusion and recommendations References
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  • 92
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    Call number: ZSP-202-85,2
    In: Research report / Cold Regions Research and Engineering Laboratory, 85,2
    In: The frost behavior of soils : laboratory and field data for a new concept, Part II
    Description / Table of Contents: Laboratory experiments were performed with a specil closed-system side-freezing cabinet in which completely saturated soil samples were subjected to alternate freeze-thaw cycles without surcharge. A vertical or nearly vertical freezethaw plane was obtained in the side-freezing cabinet. The soil used was a straight graded noncohesive material with 14 finer than the No. 200 0.074 mm mesh sieve. According to frost criterion based only on gradation, the soil would be classified as a never frost-heaving moraine soil or non-frost-susceptible. All experiments were run for 20 and 22 cycles. Freezing rates used were as follows 30.0 mmhr 33.0 mmhr and 4 .0 mmhr. The initial dry density was approximately constant for each test at 1.8 gcm3 or 112.4 lbft3, and complete saturation was maintained in the tests.
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    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 85,2
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  • 93
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-90
    In: Research report / Cold Regions Research and Engineering Laboratory, 90
    Description / Table of Contents: Summary: A new method is presented for extracting more meaningful information from snow profile data which will simplify the study of the permeability of snow. Earlier analyses normally employed statistical methods to determine property variations with depth, with the line of mean values established by the method of least squares. The mean curves derived in this manner may not represent properly the true nature of the snow pack, or aid in understanding the dynamic processes which are in action. The new graphical methods described distinguish the separate effects of densification and thermal metamorphism on permeability, permitting future advances in the analysis. Profile data obtained in 1954 and 1960 are reanalyzed using the new techniques. For a natural polar pack under conditions when no melting occurs and the accumulation is assumed continuous, the following conclusions may be made: permeability for a given density of snow increases with depth and time except possibly near the surface or at depths below 30 m; the rate of permeability change with depth for given densities decreases in a calculable way relative to the density; and, mean permeability changes with depth in a complex manner.
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    Pages: iv, 14, A3, B2, C2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 90
    Language: English
    Note: CONTENTS Preface Summary Introduction Standard methods of data presentation- A class interval method of data presentation Interpretation of the numerical data Interpretation of thin sections Conclusions References Appendix A Appendix B Appendix C
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  • 94
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-53
    In: Research report / Cold Regions Research and Engineering Laboratory, 53
    Description / Table of Contents: Summary: The results of investigations on the structural changes of Greenland snow during age-hardening in the first 49 hr after ejection by a Peter snow miller from a trench 4.7 ft deep are reported, and the method of study is described. The samples of snow were taken at various distances from the trench 1, 3, 14, 25, and 49 hr after deposition, and their changes were studied as a function of time and distance from the trench. The porosity remained constant at an average of 50 ± 3%. The number of grains/cm^2 decreased with time and increased with distance from the trench because of the different speeds of sedimentation and wind sifting. The mean grain cross-section showed a similar dependence. The relative length of grain boundaries increased with time and slightly with distance from the trench, while the mean length of new grain-to-grain boundaries increased with age and decreased with distance from the trench. The mean number of adjacent grains per grain vs. relative length of grain boundaries showed a linear relation. A slight increase of new boundaries with increasing number of neighbors was also observed. Suggestions for a precise study of the age-hardening process of snow are made.
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    Pages: v, 15, A5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 53
    Language: English
    Note: CONTENTS Preface Summary Methods of testing Sampling Preparation of samples Preparation of structure pictures Results Influence of time and place Porosity Number of grains/cm2 Mean grain cross section Relative length of grain boundaries (KM ratio) Mean number of adjacent grains per grain Number of new boundaries/cm 2 Mean length of new grain-to-grain boundaries Some interrelations of the structure data Structure of a 1-yr old Peter snow Suggestions for an exact study of the age-hardening process of snow References Appendix: Structure pictures
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  • 95
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-61
    In: Research report / Cold Regions Research and Engineering Laboratory, 61
    Description / Table of Contents: Summary: The results of experiments on the bonding of polished and microtomed surfaces of bubble-free ice samples at -5°C with various loads are reported. Only a small part of the available surface area appeared to be bonded, this area increasing with the bonding load. Surfaces apposed immediately after preparation showed an appreciably higher force of separation than those joined after a time interval. The force of separation for surfaces placed together at 0% relative humidity was higher than that at 100% relative humidity. A simplified theory of bonding of irregular ice surfaces is formulated in the appendix. The calculations are based on the assumption of a distribution of small ice cylinders of equal cross sections but different heights located on a non-deformable plate. The cylinders are deformed by a constant force which is applied by another completely non-deformable flat plate. The deformation as a function of force and time and the force of separation as a function of load are derived, assuming that the distribution of heights is given by a box distribution (i.e., frequency of heights is constant).
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    Pages: iv, 6, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 61
    Language: English
    Note: CONTENTS Preface Summary Introduction Materials Apparatus and procedure Results Discussion References Appendix: Compression of an assembly of cylinders
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  • 96
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-64
    In: Research report / Cold Regions Research and Engineering Laboratory, 64
    Description / Table of Contents: Summary: The distribution of temperature throughout an idealized ice cap is studied. The idealized ice cap is considered as one with a constant growth rate, without internal movement, subject to a linear climatic change and to a constant geothermal influx. The problem is treated as a Stefan-type problem and the solution is obtained by the principle of superposition. The results indicate that the temperature at the base of the ice cap rises with time and eventually would reach the melting point of the ice. Under such conditions, it is concluded that the ice cap is not resting on a permafrost base as suggested by previous investigation.
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    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 64
    Language: English
    Note: CONTENTS Preface Summary Introduction Mathematical development Method of solution Discussion of results Base temperature Minimum temperature Effect of rate of growth Effect of geothermal influx Comparison with observed results References
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  • 97
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-66
    In: Research report / Cold Regions Research and Engineering Laboratory, 66
    Description / Table of Contents: Summary: A simple theory is proposed for crack formation and development by soil desiccation on the basis of laboratory experiments utilizing soil samples (Bloomington till) with max particle size of 1 mm diam. held in flat wooden containers. The crack pattern is more dependent on the thickness of the soil sample than on temperature or humidity. Some effect is caused also by differences in the bottom material of the containers. The area of cells made by crack patterns has a log normal size distribution. Total length of cracks decreases with increase in sample thickness. The number of sides of cells also depends on the thickness. Cracking was found to begin from the center of the soil layer and to propagate to the surface or bottom with non-uniform speed.
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    Pages: vi, 48, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 66
    Language: English
    Note: CONTENTS Preface Summary Introduction Soil material Soil Preparation of the soil material Containers Temperature and humidity of the air Moisture content and dry density of the soil Experimental procedures and results General procedures Definition of the characteristics of cracking of soil Cracking moisture content Size of cells made by cracking of the soil Length of cracks Number of sides of cells Development of cracks Additional experiments Interfacial fracture markings Method of auxilliary tests on physical properties of the soil Elastic constants of the soil Shrinkage of soil due to desiccation Tests of the adhesion between the soil and the bottom material Results of auxiliary tests Elastic constants of the soil Free shrinkage process of the soil due to desiccation Adhesion between the soil and glass or wood Mechanism of crack formation due to the desiccation of soil Geometric interpretation Mechanical interpretation Conclusions References Appendix: Table of experiments
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  • 98
    Call number: AWI G3-24-95691
    Description / Table of Contents: В 1960 г. в Канаде состоялся Первый международный симпозиум по геологии Арктики, в котором привяли участие советские, канадские, американские, английские, датские и норвежские ученые. Итогом работ симпозиума явился настоящий сборник, в котором сведены новейшие материалы по геологии, океанологии, гляциологии и климатологии северных полярных областей земного шара. Эти работы дают отчетливое представление о геологическом строении огромных территорий Канады и Аляски, о рельефе и характере осадков два Северного Ледовитого океана, о ледовом режиме Арктики. Необходимо отметить, что до недавнего времени многие области зарубежной Арктики были белыми пятнами на геологических картах; первые сведения о них содержатся в статьях этого сборника. Новые материалы сборника дают ценнейшие сведения для сравнительных оценок геологических условий и обстановки оруденения северных областей советской и зарубежной Арктики.
    Description / Table of Contents: Translation of abstract: In 1960, the First International Symposium on Arctic Geology was held in Canada, in which Soviet, Canadian, American, English, Danish and Norwegian scientists took part. The result of the symposium was this collection, which brings together the latest materials on geology, oceanology, glaciology and climatology of the northern polar regions of the globe. These works give a clear idea of the geological structure of the vast territories of Canada and Alaska, the relief and nature of precipitation in the two Arctic Oceans, and the ice regime of the Arctic. It should be noted that before recently, many areas of the foreign Arctic were blank spots on geological maps; the first information about them is contained in the articles in this collection. New materials in the collection provide valuable information for comparative assessments of geological conditions and mineralization conditions in the northern regions of the Soviet and foreign Arctic.
    Type of Medium: Monograph available for loan
    Pages: 515 Seiten , Illustrationen
    Uniform Title: Geology of the Arctic proceedings of the first International Symposium on Arctic Geology
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Предисловие к английскому изданию Введение ШПИЦБЕРГЕН Схема структурной истории Шпицбергена / В. Б. Харланд ГРЕНЛАНДИЯ Обзор геологии северной и восточной Гренландии Докембрийские и нижнепалеозойские структурные элементы и осадконакопление в северной и восточной Гренландии / Л. Кох Каролиниды: орогенический пояс позднедокембрийского возраста в северо-восточной Гренландии / Дж. Халлер Нижний палеозой Гренландии / Дж. Коуи Значение каледонской орогении в Гренландии / Дж. Халлер Девонские отложения центральной части восточной Гренландии / Х. Бютлер Континентальные иаменноугольные и нижнепермские отложения центральной части восточной Гренландии / Х. Бютлер Пермь Гренландии / В. Майнц Триас восточной Гренландии / Р. Трюмпи Юрские отложения восточной Гренландии / Дж. Х. Калломон Меловые отложения восточной Гренландии / Д. Т. Донован Третичные отложения Гренландии / Э. Венк Стратиграфия позднего докембрия восточной Гренландии / Х. Р. Кац О хронологии докембрия западной Гренландии / А. Бертельсен КАНАДА Структурная истории Канадского арктического архипелага с докембрийского времени / Р. Topcтeйнccoн, Е. T. Тозер Общий обзор геологии докембрии арктической части Канады / Р. Г. Блакадар, Дж. А. Фрейзер Стратиграфия нижнего палеозоя Канадского арктического архипелага / Р. Торетейнссон Общий очерк стратиграфии мезозойских и третичных отложений Канадского арктического архипелага / Е. T. Тозер Соотношение дислокаций складчатого пояса островов Парри и корнуоллисских складчатых структур на востоке острова Батерст Канадского арктического архипелага / Э. Н. Мак-Нейр Геологическая интерпретация аэромагнитных профилей, проведенных через Канадский арктический архипелаг / А. Ф. Грегори, М. Е. Бауэр, Л. В. Морлей Тектоническое строение северной Канады / Л. Дж. Мартин Каледонские или акадийские граниты северной части территории Юкон / Х. Бадегард, Р. И. Фолинеби, Дж. Липсон Стратиграфия девона района среднего течения реки Макензи, Северо-Западные территории, Канада / Х. Г. Бacceт Стратиграфия девонских отложений района Нориан-Уэлс / Т. Cтopu АЛЯСКА Изучение тектоники Аляски / Г. Грик Корреляция палеозойских пород Аляски / Дж. Т. Дутромл Новые данные о распространении верхнетретичных континентальных отложений на Аляске и в северо-западной Канаде / В. С. Бениннгхоф, Г. В. Холмс, Д. М. Гопкинс АРКТИЧЕСКИЙ БАССЕЙН Истории геологических знаний о происхождении Арктинеского бассейна / А. Дж. Ирдли Срединно-океанический хребет и его продолжение через Арктический бассейн / Б. К. Хейзен, М. Юииг Продолжение горных цепей в Арктике в прошлом / Дж. T. Вилъсон Сейсмическое исследование дна Арктического океана / К. Ханкинс Гальки, поднятые при драгировании в центральной части Северного Ледовитого океана / В. Шварцахер, К. Ханкинс Батиметрия моря Бофорта / А. Дж. Kapcoла, Р. Л. Фишер, К. Дж. Шипек, Г. Шамвей Предварительные результаты исследований арктической дрейфующей станции Чарли / В. Дж. Кроми Геофизические исследования на дрейфующей станции МГГ Браво, Т-3, 1958-1959 гr. / Д. Плоуфф, Г. В. Келлер, Ф. Ц, Фришкнехт, Р. Р. Уол Морские геологические наблюдения в Баренцовом море / Х. Игнатиус Морская геология и батиметрия шельфа Чукотского моря в районе Оготорук-Крик, северо-западная Аляска / Д. В. Схолл, К. Л. Сайнсбери Геоморфология Арктического бассейна / Р. Дитц, Дж. Шамвей Предметный указатель Указатель географических названий , Translation of Content Preface Preface to the English edition Introduction SPITSBERGEN Scheme of the structural history of Spitsbergen / W. B. Harland GREENLAND Review of the geology of northern and eastern Greenland Precambrian and Lower Paleozoic structural elements and sedimentation in northern and eastern Greenland / L. Koch Carolinids: Late Precambrian orogenic belt in northeastern Greenland / J. Haller Lower Paleozoic of Greenland / J. Cowie The significance of the Caledonian orogeny in Greenland / J. Haller Devonian deposits of the central part of eastern Greenland / H. Bütler Continental Carboniferous and Lower Permian deposits of the central part of eastern Greenland / H. Bütler Perm Greenland / V. Mainz Triassic of eastern Greenland / R. Trumpy Jurassic deposits of eastern Greenland / J. H. Callomon Cretaceous deposits of eastern Greenland / D. T. Donovan Tertiary deposits of Greenland / E. Wenk Late Precambrian stratigraphy of eastern Greenland / H. R. Katz On the chronology of the Precambrian of western Greenland / A. Bertelsen CANADA Structural history of the Canadian Arctic archipelago since Precambrian time / R. Topsteinson, E. T. Tozer General overview of the Precambrian geology of the Canadian Arctic / R. G. Blakadar, J. A. Fraser Stratigraphy of the Lower Paleozoic of the Canadian Arctic Archipelago / R. Thoreteinsson General outline of the stratigraphy of Mesozoic and Tertiary deposits of the Canadian Arctic Archipelago / E. T. Tozer The relationship between the dislocations of the Parry Islands fold belt and the Cornwallis fold structures in the east of Bathurst Island in the Canadian Arctic Archipelago / E. N. McNair Geological interpretation of aeromagnetic profiles drawn through the Canadian Arctic Archipelago / A. F. Gregory, M. E. Bauer, L. V. Morley Tectonic structure of northern Canada / L. J. Martin Caledonian or Acadian granites of the northern Yukon Territory / H. Badegard, R. I. Folineby, J. Lipson Devonian stratigraphy of the middle Mackenzie River region, Northwest Territories, Canada / H. G. Basset Stratigraphy of Devonian deposits of the Norian-Wells region / T. Stopu ALASKA Study of Alaska tectonics / G. Grik Correlation of Paleozoic Rocks of Alaska / J. T. Dutroml New data on the distribution of Upper Tertiary continental sediments in Alaska and northwestern Canada / V. S. Beninghof, G. W. Holmes, D. M. Hopkins ARCTIC POOL Stories of geological knowledge about the origin of the Arctic Basin / A. J. Eardley Mid-ocean ridge and its continuation through the Arctic basin / B. K. Hazen, M. Huig The continuation of mountain ranges in the Arctic in the past / J. T. Wilson Seismic exploration of the Arctic ocean floor / K. Hankins Pebbles raised during dredging in the central part of the Arctic Ocean / V. Schwarzacher, K. Hankins Bathymetry of the Beaufort Sea / A. J. Kapcola, R. L. Fisher, K. J. Shipek, G. Shumway Preliminary results of studies of the Arctic drifting station Charlie / W. J. Cromie Geophysical research at the drifting station MGG Bravo, T-3, 1958-1959. / D. Plouffe, G. W. Keller, F. Z, Frischknecht, R. R. Wahl Marine geological observations in the Barents Sea / H. Ignatius Marine geology and bathymetry of the Chukchi Sea shelf in the Ogotoruk Creek area, northwestern Alaska / D. W. Scholl, K. L. Sainsbury Geomorphology of the Arctic Basin / R. Dietz, J. Shumway Subject index Index of geographical names , In kyrillischer Schrift
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 99
    Series available for loan
    Series available for loan
    London : H.M.Stat.Off.
    Associated volumes
    Call number: ZSP-164-24
    In: Scientific reports
    Description / Table of Contents: Recent collections of decapod crustaceans and serpulid worms from the Upper Cretaceous of James Ross Island have facilitated the re-description of three species previously recorded from the area and have contributed four new species. The decapods include Hoploparia stokesi (Weller), Meyeria crofti sp. nov. and Callianassa meridionalis sp. nov., and the serpluids Rotularia callosa (Stoliczka), Rotularia shackletoni (Wilckens), Rotularia dorsolaevis sp. nov. and Ditrupa varicosa sp. nov. The diagnosis of the subfamily Homarinae Mertin, 1941 is amended and observations are made on the taxonomic position and stratigraphical range of the genus Meyeria. In addition, the structure of the tube-wall of the genera Rotularia Defrance, 1827 and Ditrupa Berkeley, 1832-34, and their stratigraphical range are discussed. The age of the fauna is shown by associated ammonites to be of Lower to Middle Campanian age.
    Type of Medium: Series available for loan
    Pages: 30 S., 7 Bl. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / Falkland Islands Dependencies Survey 24
    Branch Library: AWI Library
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  • 100
    Call number: ZSP-164-42
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 45 S. : Ill.
    Series Statement: Scientific reports / British Antarctic Survey 42
    Branch Library: AWI Library
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