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  • 1960-1964  (51)
  • 1964  (51)
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  • 1
    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
    Location: AWI Reading room
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  • 2
    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
    Location: AWI Reading room
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  • 3
    facet.materialart.
    Unknown
    Jena : G. Fischer
    Call number: Bio-05-0015
    Branch Library: AWI Library
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  • 4
    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]
    Location: AWI Reading room
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  • 5
    Call number: AWI G3-93-0257
    Type of Medium: Monograph available for loan
    Pages: 2 S.
    Branch Library: AWI Library
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  • 6
    Series available for loan
    Series available for loan
    Wiesbaden : Steiner
    Associated volumes
    Call number: ZSP-265-2
    In: Ergebnisse der Stauferland-Expedition 1959/60 [und 1967]
    Type of Medium: Series available for loan
    Pages: 53, [12] S. : Ill.
    Series Statement: Ergebnisse der Stauferland-Expedition 1959/60 [und 1967] 2
    Branch Library: AWI Library
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  • 7
    Call number: MOP Per 581(3/1) ; ZSP-319/C-1(2. Ex.) ; ZSP-319/C-1
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, 1
    Type of Medium: Series available for loan
    Pages: 188 Seiten , Illustrationen, Karten , 5 Kartenbeilagen
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 1
    Language: German
    Note: Kartenbeilage unter dem Titel: Fedtschenko-Gletscher : Südblatt 〈1 : 50 000〉 , Kartenbeilage unter dem Titel: Fedtschenko-Gletscher : Nordblatt 〈1 : 50 000〉 , Kartenbeilage unter dem Titel: Fedtschenko-Gletscher : Zungenkarte 〈1 : 25 000〉 , Kartenbeilage unter dem Titel: Fedtschenko-Gletscher : Unterer Zungenteil 〈1 : 10 000〉 , Kartenbeilage unter dem Titel: Fedtschenko-Gletscher : Tanymas-Lappen 〈1 : 10 000〉 , Inhaltsverzeichnis Vorwort Inhaltsverzeichnis 1. Die Aufgabenstellung und die Durchführung der Arbeiten 1.1. Einführung 1.2. Fragen der glaziologischen Forschung 1.3. Der Fedtschenkogletscher und seine Erforschung 1.4. Die Aufgaben der glaziologischen Expedition im Jahre 1958 1.5. Die Tätigkeit der geodätischen Arbeitsgruppe 1.5.1. Organisation und Ablauf der Arbeiten 1.5.2 Trigonometrische Arbeiten 1.5.2.1. Die verwendeten Instrumente 1.5.2.2. Die Anlage und Beobachtung des trigonometrischen Netzes 1.5.3. Photogrammetrische Aufnahmearbeiten 1.5.3.1. Instrumente und photographisches Material 1.5.3.2. Die Anlage der photogrammetrischen Standlinien und die Aufnahme der Meßbilder 1.5.3.3. Die Ermittlung der Oberflächengeschwindigkeit des Eises 2. Die Auswertung der geodätischen und photogrammetrischen Messungen 2.1. Vorbemerkungen 2.2 Die Berechnung des trigonometrischen Netzes 2.2.1. Grundzüge der Berechnungen 2.2.2. Netzberechnungen 2.2.2.1. Die Dreieckskette am Unterlauf des Fedtschenkogletschers 2.2.2.2. Die trigonometrischen Beobachtungen am Mittellauf des Fedtschenkogletschers 2.2.2.3. Die trigonometrischen Beobachtungen im Tal des Gletschers Kleiner Tanymas 2.2.3. Die Kontrolle des Maßstabes der Triangulationen durch Basismessungen 2.2.4. Die Ergebnisse der trigonometrischen Messungen 2.3. Bestimmung der Koordinaten und Höhen für die photogrammetrischen Aufnahmestandlinien 2.4. Die photogrammetrische Paßpunktverdichtung 2.4.1. Allgemeines zur Paßpunktverdichtung 2.4.2. Das Identifizieren von Paßpunkten 2.4.3. Die photogrammetrische Bestimmung von Paßpunkten 2.4.3.1. Bemerkungen zur Bestimmungsmethode 2.4.3.2. Die Bestimmung der Daten der inneren Orientierung 2.4.3.3. Die Bestimmung der Paßpunkte durch numerische Meßtischphotogrammetrie 2.4.3.4. Die Genauigkeit der photogrammetrischen Paßpunktbestimmung 2.5. Die Kartierung der terrestrisch-stereophotogrammetrischen Aufnahmen 2.5.1. Auswertegrundlagen und Kartierungsmethode 2.5.2. Inhalt und Genauigkeit der Kartierungen 2 5.2.1. Kartierung des Fedtschenkogletschers und Teile seiner Nebengletscher im Maßstab 1 : 25000 2.5.2.2. Die Kartierung des letzten Teiles der Zunge des Fedtschenkogletschers im Maßstab 1 : 10000 2.5.2.3. Die Kartierung des Tanymaslappens im Maßstab 1 : 10000 2.6 Kartographische Arbeiten 3. Die glaziologische Auswertung 3.1. Die Aufgabenstellung für die glaziologische Auswertung 3.2. Die Verfahren der glaziologischen Auswertung 3.2.1. Die Bestimmung der Gletscherveränderungen durch Kartenvergleich 3.2.2. Die Ermittlung der Oberflächengeschwindigkeit des Eises 3.2.2.1. Die Auswertung der Meßbilder 3.2.2.2. Die Genauigkeit der Bestimmung der Oberflächengeschwindigkeit 3.2.3. Berechnung der Eisdicke und der Durchflußmengen 3.3. Die Ergebnisse der glaziologischen Auswertung 3.3.1. Vergleich der topographischen Karten von 1928 und 1958 3.3.1.1. Vergleich der Gletscherstände 3.3.1.2. Ermittlung des Eisverlustes des Fedtschenkogletschers 3.3.1.3. Sonstige Veränderungen 3.3.2. Ermittlung der Oberflächengeschwindigkeit des Eises 3.3.3. Berechnung der Eisdicke und der Durchflußmengen 3.3.4. Zusammenfassung der Vergleichsergebnisse 4. Literaturangaben 5. Bildanhang
    Location: MOP - must be ordered
    Location: AWI Archive
    Location: AWI Archive
    Branch Library: GFZ Library
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 8
    Monograph available for loan
    Monograph available for loan
    Berlin : Akademie-Verlag
    Call number: 1.2/WE 43 ; AWI S5-98-0138
    Type of Medium: Monograph available for loan
    Pages: 424 S. :30 cm
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
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  • 9
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: AWI S1-97-0224
    In: Die Grundlehren der mathematischen Wissenschaften
    Type of Medium: Monograph available for loan
    Pages: XX, 536 S. : graph. Darst.
    Edition: 7. Aufl.
    Series Statement: Die Grundlehren der mathematischen Wissenschaften 4
    Branch Library: AWI Library
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  • 10
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-103
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 13 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 103
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  • 11
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-106
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 13 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 106
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-104
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 15 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 104
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  • 13
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-107
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 14 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 107
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  • 14
    Monograph available for loan
    Monograph available for loan
    København : Reitzel
    Associated volumes
    Call number: ZSP-553-159,11
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 74 S., XXI Taf. : zahlr. Ill.
    Series Statement: Meddelelser om Grønland 159,11
    Language: English
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  • 15
    Call number: ZSP-553-159,10
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 45 S. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 159,10
    Language: English
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  • 16
    Call number: ZSP-553-164,6 ; AWI P8-88-0281
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 105 S., 4 Taf. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 164,6
    Language: English
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  • 17
    Call number: ZSP-553-164,5
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 66 S., 7 Taf. : Ill., graph. Darst., Kt.
    Series Statement: Meddelelser om Grønland 164,5
    Language: English
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  • 18
    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
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  • 19
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    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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  • 20
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    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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  • 21
    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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  • 22
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    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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  • 23
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-110
    In: Research report / Cold Regions Research and Engineering Laboratory, 110
    Description / Table of Contents: Summary: Nafe's (1957) presentation of reflection and transmission coefficients at a solid-solid interface was used to compute tables for the case of ice in contact with another solid at a plane interface. Energy ratios of all the combinations of reflected and refracted plane P and S waves were computed for 30 different cases of the second solid. A compressional velocity of 3.6 km/sec, a density of 0.9 g/cm^3, and a value of 1/3 for Poisson's ratio were assumed for the ice. For the other solid, the velocity ranged from 1.2 to 6.0 km/sec, the density from 1.5 to 3.0 g/cm^3, and Poisson's ratio from 0 to 1/3. The computations were carried out with an electronic computer, and the results are presented graphically.
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    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 110
    Language: English
    Note: CONTENTS Preface Summary Introduction Definitions Computation Results
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  • 24
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    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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  • 25
    Call number: ZSP-202-111,1
    In: Research report / Cold Regions Research and Engineering Laboratory, 111,1
    Description / Table of Contents: Summary: Optical scintillation, visual resolution, and wind and temperature profiles were measured over snow, ice and frozen ground. The data were analyzed to determine relationships between (1) scintillation and visual resolution and (2) scintillation and meteorological and surface conditions. The experimental results included (1) estimates of the limit of visual resolution, (2) telephotometer measurements of the apparent fluctuations in brightness (scintillation) of an artificial light source, and (3) measurements of wind direction and of the vertical distributions of wind speed and temperature. The optical path was 543 m long and 1.5 m above uniform horizontal surfaces. All scintillation and meteorological data are given in an appendix. The principal results of the analysis showed that for turbulent flow in stable stratification over snow (1) visual resolution deteriorated systematically as scintillation increased in intensity and (2) scintilliation intensity increased with increase in vertical temperature gradient. Scintilliation was at a minimum in the absence of thermal stratification and at a maximum (in very stable thermal stratification) during the sudden transition from laminar to turbulent flow. For a given temperature gradient, scintilliation increased with increase in wind speed. When wind and temperature gradients were combined in terms of the Richardson number and related to scintilliation, the data obtained over snow indicated a critical Richardson number of about 0.35. Scintilliation power spectra for eight periods revealed characteristics that could be related to visual resolution, the Richardson number and the mean wind speed component normal to the optical path. NOTE: This file is large. Allow your browser several minutes to download the file.
    Type of Medium: Series available for loan
    Pages: iii, 32, A17, B44 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 111,1
    Language: English
    Note: CONTENTS Preface Page Summary Introduction The problem Previous work Plan of the investigation Conclusions Visual resolution and scintillation Visual resolution and wind, temperature, and surface conditions Visual resolution and height and length of optical path Results Measurements Analysis and discussion Visual resolution and scintillation relationships Scintillation and micrometeorological parameters Index of refraction fluctuations Scintillation and the temperature profile Scintillation and average wind speed Combined effects of wind speed and temperature gradient Scintillation and surface roughness Scintillation power spectra Scintillation and path length References Appendix A: Equipment and procedures Appendix B: Micrometeorological and scintillation data
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  • 26
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    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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  • 27
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    Series available for loan
    London : British Antarctic Survey
    Associated volumes
    Call number: ZSP-164-41
    In: Scientific reports
    Description / Table of Contents: The petrology of the Argentine Islands is described in detail. The oldest rocks are lavas and pyroclastic members of the Upper Jurassic Volcanic Group which have been intruded by pre-Andean dykes and sills. The Andean Intrusive Suite has metamorphosed and metasomatized the volcanic and hypabyssal rocks. There is a later dyke phase which cuts both the volcanic and plutonic rocks; finally, there are a few late comparatively unaltered Tertiary dykes. Eight new analyses of hypabysaal rocks are included, but the composition range is too small to show conclusive trends.
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    Pages: 31 S. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / British Antarctic Survey 41
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  • 28
    Call number: ZSP-597-131
    In: Skrifter
    In: Scientific results
    Type of Medium: Series available for loan
    Pages: 63 S. : Ill.
    Series Statement: Skrifter / Norsk Polarinstitutt 131
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  • 29
    Call number: ZSP-164-46
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 43 S.
    Series Statement: Scientific reports / British Antarctic Survey 46
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  • 30
    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
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  • 31
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    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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  • 32
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    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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  • 33
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    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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  • 34
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    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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  • 35
    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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  • 36
    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.
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    Pages: 12 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Geology 1
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  • 37
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    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.
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    Pages: 24 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Geology 2
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    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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  • 39
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    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-22
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 20 S. : Ill.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports : Series E, Biology 22
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  • 40
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    Series available for loan
    Tokyo : Polar Section, National Science Museum
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    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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  • 41
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    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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    Monograph available for loan
    Moskva : Gidrometeoizdat Otd.
    Call number: AWI A8-92-0542
    Type of Medium: Monograph available for loan
    Pages: 303 S. : Ill., graph. Darst., Kt.
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    Monograph available for loan
    Warszawa : Wydawnictwa Geologiczne
    Associated volumes
    Call number: AWI P9-89-0516
    In: Studia geologica polonica
    Type of Medium: Monograph available for loan
    Pages: 220 S. : Ill., graph. Darst., Kt.
    Series Statement: Studia geologica polonica 11
    Language: English
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  • 44
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    Monograph available for loan
    Oslo [u. a.] : Universitetsforlaget
    Call number: AWI Bio-95-0209
    Description / Table of Contents: Contents: Preface. - 1. Abstract. - 2. Introduction. - 3. The climatic conditions of Spitsbergen. - 4. Diatom material and localities. - 5. Taxonomic section. - 6. Summary. - 7. Literature. - 8. Plates
    Type of Medium: Monograph available for loan
    Pages: 204 S. : Ill., graph. Darst., Kt.
    Series Statement: Tromsö Museums Skrifter 11
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  • 45
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    Monograph available for loan
    Cambridge, USA : Wiley
    Call number: AWI A19-96-0032
    Type of Medium: Monograph available for loan
    Pages: XX, 752 S.
    Series Statement: University of California / Engineering and physical sciences extension series
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  • 46
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    Monograph available for loan
    Washington : American Geophysical Union
    Associated volumes
    Call number: AWI G7-96-0035
    In: Antarctic research series
    Type of Medium: Monograph available for loan
    Pages: X, 277 S. : Abb. ; 27 cm
    Series Statement: Antarctic research series 2
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    Monograph available for loan
    Jerusalem : Israel Program for Scientific Translations
    Call number: AWI A7-98-0092 ; PIK N 456-99-0205 ; MOP 35101
    Type of Medium: Monograph available for loan
    Pages: 200 S. : graph. Darst.
    Series Statement: IPST 1031
    Uniform Title: Fizika pogranichonogo sloya atmosfery 〈engl.〉
    Language: English
    Note: Contents: Preface. - Introduction. - I. THE EQUATIONS OF HYDROTHERMODYNAMICS OF THE BOUNDARY LAYERS; ANALYSIS OF THESE EQUATIONS. - § 1. Derivation of the Equations for the Averaged Quantities. - § 2. The Relation Between Fluctuations of the Meteorological Elements and the Averaged Characteristics. Currents of Various Substances Due to Turbulence. - § 3. Some Problems of Turbulence Dynamics. The Reynolds Number. The Richardson Number § 4. Classification of Motions. Estimation of the Thickness of the Planetary Boundary Layer. The Surface Sublayer. - II. THE BOUNDARY LAYER OF THE ATMOSPHERE IN STATIONARY CONDITIONS. - § 1. Some Information on the Distribution of the Meteorological Elements in the Boundary Layer. - § 2. External Factors Determining the Structure of the Boundary Layer of the Atmosphere. - § 3. A Boundary Layer Model with Height-Independent Turbulence Coefficient (One-Parameter Model). - § 4. The Structure of the Surface Sublayer. - § 5. Calculation of the Basic Characteristics of the Surface Sublayer. - § 6. Two-Parameter Model of the Boundary Layer of the Atmosphere. - § 7. Some Information on the Processes at the Active Surface and in the Upper Layers of the Ground Influencing the Boundary Layer. - III. DAILY VARIATION OF THE METEOROLOGICAL ELEMENTS. - § 1. The Simplest Model for the Daily Temperature Variation. Features of the Daily Temperature Variation Over Water. - § 2. Daily Temperature Variations for Turbulent Mixing Intensity Growing with Height. - § 3. An Account of the Time Variations of the Eddy Exchange in the Theory of the Daily Temperature Variations. - § 4. The Influence of the Radiative Heat Influx on the Daily Temperature Variation. - § 5. Nocturnal Lowering of the Temperature. Forecasting of Radiation Frosts. - § 6. Daily Humidity Variations. Radiation Fogs. - § 7. Daily Variations of Wind Velocity. - IV. VARIATIONS OF METEOROLOGICAL FIELDS DUE TO THE INHOMOGENEITY OF THE ACTIVE SURFACE. - § 1. Qualitative Analysis of the Transformation Process. - § 2. Variations of the Temperature and Humidity Fields Over an Inhomogeneous Underlying Surface. - § 3. Formation of Advection Fogs. - § 4. Variations of the Micrometeorological Regime in Irrigation, Irrigation Standards for Various Meteorological Conditions. - § 5. Influence of Small Reservoirs on the Structure of the Lower Layers of the Atmosphere. - § 6. Nonstationary Processes Over An Inhomogeneous Underlying Surface. - § 7. Local Winds. - V. PHENOMENA AND PROCESSES OF A SPECIAL NATURE RELATED TO THE METEOROLOGICAL REGIME OF THE BOUNDARY LAYER. - §1. Wind Drift of Ice Floes. - § 2. Applications of the Laws of the Boundary Layer of the Atmosphere to Problems of Construction and Power Engineering. - § 3. Freezing of the Upper Layer of the Ground. - § 4. Pollution of the Lower Layers of the Atmosphere by Smoke From Factory Chimneys. - § 5. Some Features of the Electrostatic Field in the Surface Layer of the Atmosphere. , Transl. from Russian
    Location: A 18 - must be ordered
    Location: MOP - must be ordered
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  • 48
    Monograph available for loan
    Monograph available for loan
    Leipzig : Brockhaus
    Call number: AWI E3-84-0762
    Type of Medium: Monograph available for loan
    Pages: 326 S. : Taf. , 1 Kte. ; 24 cm
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  • 49
    Call number: AWI G2-98-0195
    Type of Medium: Monograph available for loan
    Pages: 114 S. : graph. Darst.
    Series Statement: Archiv für Hydrobiologie : Beihefte 2
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  • 50
    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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  • 51
    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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