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  • Books  (2,341)
  • English  (1,512)
  • German  (833)
  • 1965-1969  (2,222)
  • 1935-1939  (122)
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  • 1
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-242
    In: Research report, 242
    Description / Table of Contents: The attenuation of visible light by falling snow was studied by making simultaneous attenuation measurements and snow concentration measurements. The attenuation coefficient was calculated from photometric measurements and from visual observations. Snow concentration in the air was evaluated by two methods: from Formvar replicas collected during the snowfall, and by mass accumulation of snow in collecting pans. The snowflakes were arbitrarily classified by crystal types according to their estimated fall velocity. It was found that the correlation between extinction coefficient (attenuation) and snow concentration was generally much higher by types than when all snowflakes were considered together regardless of crystal components and degree of riming. Two types, apparently improperly classified, displayed lower correlations than the overall group. When no fog is present during the snowfall, the experimental results coincide well with attenuation theory if a reasonable correction is applied to the values obtained in the measurement of snowflake diameters. Measurements of mass flux indicate that for a given intensity the attenuation caused by snow is an order of magnitude greater than that caused by the same mass flux of rain.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 242
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Initial theoretical considerations. - Light attenuation by particles. - Basis of attenuation meter measurements. - Contrast reduction and visual range. - Transmissometer theory, Pritchard photometric method. - Terminal velocity of snowflakes. - Methods of measurement: Light attenuation. - Duntley (Scripps Institution) attenuation meter. - "Meteorological range" observations. - Pritchard photometric method. - Methods of measurement: Atmospheric concentration of snowflakes. - Replication method. - Mass accumulation method. - Analysis of snow samples. - Terminal velocity of snowflakes. - Flux density and atmospheric concentration. - Mass accumulation rate. - Concurrent attenuation due to fog. - Discussion of results. - Computational methods. - Correlations: Attenuation coefficient vs area concentration. - Correlations: Attenuation coefficient vs are a flux. - Correlations: Attenuation coefficient vs mass concentration and mass flux. - Comparison of sampling methods for mass flux. - Attenuation of visible light by snow compared to rain. - Literature cited. - Appendix A.
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  • 2
    Dissertations
    Dissertations
    Zeulenroda : Sporn
    Call number: AWI Bio-15-0014
    Type of Medium: Dissertations
    Pages: 87 S. : Kt.
    Edition: Teildr.
    Language: German
    Note: Jena, Univ., Diss., 1935 , nhaltsverzeichnis: Vorwort. - Einleitender Teil: (als kurze Zusammenfassung gedruckt). - 1. Geschichte der pflanzengeographischen Erforschung der Taiga. - 2. Lage, Größe, Grenzen und Name der Taiga. - 3. Das Bild der Taiga und ihre wichtigsten Baumarten. - a. Die Lärche (Larix sibirica Ldb. et L. dahurica Turcz). - b Die sibirische Fichte (Picea obovata Ldb.). - c. Die Ajan-Fichte (Picea ajanensis Fisch). - d. Die sibirische Tanne oder Pichta (Abies sibirica Mayr.). - e. Die Kiefer (Pinus silvestris L.). - f. Die Arve oder sibirische Zeder (Pinus sibirica Mayr.). - g. Die Straucharve (Pinus pumila Rgl.). - h. Der Wacholder (Juniperus communis L.). - i. Die Birke (Betula sp. sp.). - j. Die Espe (Populus tremula L.). - k. Andere Laubhölzer. - Hauptteil: Die Gliederung der Taiga. - I. Bereits bestehende Gliederungen. - II. Westsibirien. - a. Das eigentliche Tiefland des Ob-Irtysch-Gebietes. - 1. Nördliche Fichten- und Lärchenwälder. - 2. Die dunkle Taiga - der Urman. - 3. Der Bor. - 4. Birkenwälder. - b. Das Übergangsgebiet zum sibirischen Mittelgebirge am Jenissei. - 1. Flechten-Wälder. - 2. Trockene Wälder. - c. Das Übergangsgebiet am Kusnezker Alatau. - 1. Birkenwälder. - 2. Lärchenwälder. - 3. Dunkle Bergtaiga. - III. Mittelsibirien. - a. Die Landschaft am Jenissei. - 1. Nördliche Lärchen- und Fichtenwälder. - 2. Südliche, trockene Nadelwälder. - b. Das Stromgebiet der Lena. - 1a. Nördliche Plateauwälder. - 1b. Südliche Plateauwälder. - 2. Talwälder. - IV. Die südlichen Gebirge. - a. Der Altai. - 1. Lärchenwälder. - 2. Der Schwarzwald - Tschernj. - 3. Fichtenwälder. - 4. Arvenwälder. - 5. Kiefernwälder. - b. Das Sajanische Gebirge. - 1. Lichte Lärchen- und Laubwälder. - 2. Dunkle Bergtaiga. - c. Transbaikalien. - 1. Höhenwälder. - 2. Baikal-See-Hangwälder. - 3. Daurische Hangwälder. - V. Ostsibirien. - a. Die nördlichen Gebirgslandschaften und das Gebiet der zum Eismeer fließenden Ströme. - 1. Wälder der Südhänge. - 2. Wälder der Nordseite. - b. Das Stanowoigebirge und das Ochotsker Küstenland. - c. Kamschatka. - 1. Zentrale Mischwälder. - 2. Periphere Laubwälder. - d. Das Amurland. - 1. Küstenwälder mit nördlichem Charakter. - 2. Begwälder. - 3. Nordmandschurische Übergangswälder. - 2. Sachalin. - 1. Talwälder. - 2. Höhenwälder. - Zusammenfassung.
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  • 3
    Monograph available for loan
    Monograph available for loan
    Leningrad : Hydrometeorologischer Verl.
    Associated volumes
    Call number: MOP 38306(2)
    In: Numerische Methoden der Wettervorhersage
    Type of Medium: Monograph available for loan
    Pages: 119 S.
    Series Statement: Numerische Methoden der Wettervorhersage 2
    Language: German
    Location: MOP - must be ordered
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  • 4
    facet.materialart.
    Unknown
    Delft ; 1.1969-76.2010
    Call number: S 90.0083
    ISSN: 0165-1706
    Language: English
    Branch Library: GFZ Library
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  • 5
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-254
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Description of the anemometer. - Temperature effects and their compensation. - Input-output relations. - Vibration isolation and compensation. - Wind tunnel tests. - Conclusions.
    Description / Table of Contents: A triaxial semiconductor strain-gage anemometer measuring wind velocities in three directions and thereby also determining the direction of the wind was designed and subjected to many crucial tests under various conditions. It was found that the measurements were affected by temperature and vibrations. Temperature compensation in two directions was made and wind tunnel tests on an almost vibration-free platform were performed. The results show that this type of instrument can be successfully used to measure large-scale turbulences. Throughout this report, emphasis is placed on the compensation necessary for temperature and vibration effects and the determination of input-output relationships. It is concluded that it is possible to design a practical triaxial strain-gage anemometer with high-frequency response and high sensitivity and to measure wind velocities accurately with this type of instrument when temperature and vibration compensations are properly made.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 254
    Language: English
    Branch Library: AWI Library
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  • 6
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-253
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical considerations. - Method of canopy evaluation. - Application to forest problems. - Forest blowdown. - Radioactivity gradient. - Phenology. - Forest types and structure. - Distribution of leaves and canopy gaps. - Light quality. - Discussion and summary. - Literature cited.
    Description / Table of Contents: A technique for evaluating forest canopies was developed based on the use of a divergent lens system to obtain hemispherical photographs of tree crowns. The photography was processed from 35 mm film and enlarged as a silhouette, and the light transmission was measured with a specially fabricated macrodensitometer. It is concluded that the amount of forest canopy can be expressed as canopy closure index (CCI) at a precision of approximately 5%. It is shown by application to a variety of problems in diverse geographical areas that this technique can be used for measuring both temporal and spatial changes in the canopy, for estimating the shade light climate, and for specifying the probability of target detection through a canopy. Data are presented to analyze changes caused by explosions, radioactivity, growing season, and vegetation types. The geometry of gaps in tree crowns is discussed and the nature of shade light quality under forests is illustrated.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 253
    Language: English
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  • 7
    Call number: AWI A5-18-91979
    Type of Medium: Monograph available for loan
    Pages: 391 Seiten , 196 Abbildungen und 13 Tafeln
    Language: German
    Note: INHALT: 1. Allgemeine Meteorologie. - 1.1. Entwicklung der Meteorologie zur Wissenschaft. - 1.1.1. Geschichtliche Einführung. - 1.1.2. Moderne Meteorologie und ihre Teilgebiete. - 1.2. Atmosphäre. - 1.2.1. Begriff der Atmosphäre. - 1.2.2. Erforschung der Atmosphäre. - 1.2.2.1. Indirekte Methoden. - 1.2.2.2. Direkte Methoden. - 1.2.3. Zusammensetzung der Luft. - 1.2.4. Vertikaler Aufbau der Atmosphäre. - 1.2.4.1. Änderung der Zusammensetzung der Luft mit der Höhe. - 1.2.4.2. Abnahme der Dichte mit der Höhe und Grenze der Atmosphäre. - 1.2.4.3. Stockwerkgliederung der Atmosphäre. - 1.2.5. Luftelektrizität. - 1.2.6. Atmosphärische Optik. - 1.3. Meteorologische Grundelemente und ihre Meßmethoden. - 1.3.1. Luftdruck. - 1.3.2. Wind. - 1.3.3. Temperatur. - 1.3.4. Luftfeuchte. - 1.4. Wetterelemente in ihrem Zusammenwirken. - 1.4.1. Strahlung und Wärmehaushalt. - 1.4.2. Erwärmung der Luft. - 1.4.3. Temperaturänderungen unter dem Einfluß von Vertikalbewegungen (Thermodynamik). - 1.4.4. Durch Kondensation und Verdunstung bedingte vVettererscheinungen. - 1.4.4.1. Zuführung von Feuchte. - 1.4.4.2. Mischung. - 1.4.4.3. Abkühlung. - 1.4.5. Zusammenhang zwischen Temperatur, Luftdruck und Wind. - 1.5. Allgemeine Zirkulation. - 1.6. Wetter in den Luftdruck- und Windgürteln. - 1.7. Wetter in den gemäßigten Breiten. - 1.7.1. Luftmassen. - 1.7.2. Planetarische Frontalzone. - 1.7.3. Polarfront, Entstehung einer Zyklone. - 1.7.4. Wetter in der Zyklone. - 1.7.5. Rand- und Teiltiefbildungen, Kaltlufttropfen. - 1.7.6. Bewegung und Steuerung von Tiefdruckgebieten. - 1.7.7. Hochdruckgebiete. - 1.7.8. Zirkulationstypen und Großwetterlagen. - 2. Praktischer Wetterdienst. - 2.1. Wetterbeobachtung als Grundlage wetterdienstlicher Arbeit. - 2.1.1. Wetterbeobachtungsdienst. - 2.1.2. Verbreitung von Wettermeldungen. - 2.1.3. Eintragen der Meldungen in Karten. - 2.1.4. Arbeitsunterlagen der synoptischen Meteorologie. - 2.2. Wetterberatung. - 2.2.1. Analyse der synoptischen Unterlagen. - 2.2.2. Prognose des Wetters. - 2.2.3. Gütegrad der Wetterprognosen. - 2.3. Seewetterdienst. - 2.3.1. Aufgaben des Seewetterdienstes. - 2.3.1.1. Inhalt der Wetterberichte für die Schiffahrt. - 2.3.1.2. Wetterberichte für die allgemeine Schiffahrt. - 2.3.1.3. Wetterberichte für spezielle Zwecke. - 2.3.1.4. Beratungstätigkeit der Seewetterdienststelle Warnemünde. - 2.3.1.5. Verschlüsselte Seewetterberichte (MAFO H), Seewetterberichte über Bildfunk (Faksimile). - 2.3.2. Wind- und Sturmwarndienst an der Küste und auf See. - 2.3.3. Meteorologischer Hafendienst. - 2.3.4. Nebelvorkommen und Nebelwarnung. - 2.3.5. Eisdienst. - 2.3.6. Bordwetterwarten. - 2.3.7. Wetterbeobachtung an Bord von Schiffen, mit Hilfe von Wetterbojen, Flugzeugen und Satelliten. - 2.3.8. Methoden der Wetterbeobachtung auf See. - 2.3.8.1. Wolkenbeobachtung und Wetterbeobachtung. - 2.3.8.2. Sichtweitenbestimmung auf See. - 2.3.8.3. Seegangsbeobachtung. - 2.3.8.4. Bestimmung des Windes. - 2.3.8.5. Luftdruckmessung. - 2.3.8.6. Messung der Lufttemperatur. - 2.3.8.7. Messung der Luftfeuchte. - 2.3.8.8. Messung der Wassertemperatur. - 2.3.9. Zeichnen von Bordwetterkarten. - 2.4. Beurteilung von Wetterlage und Wettervorhersage an Bord von Schiffen. - 2.4.1. Auswertung meteorologischer Unterlagen für Zwecke der Navigation. - 2.4.1.1 Auswertung der Seewetterberichte. - 2.4.1.2. Auswertung von Bordwetterkarten. - 2.4.2. Wetterzeichen und Wetterregeln. - 2.5. Wirbelstürme. - 2.5.1. Luftwirbel mit vertikaler Achse. - 2.5.2. Größe dieser Wirbel. - 2.5.3. Tropische Wirbelstürme. - 2.5.3.1. Auftreten der tropischen Wirbelstürme. - 2.5.3.2. Häufigkeit des Auftretens von tropischen Wirbelstürmen. - 2.5.3.3. Aufbau und Eigenschaften eines tropischen Wirbelsturms. - 2.5.3.4. Anzeichen für das Herannahen eines tropischen Orkanes. - 2.5.3.5. Bestimmung der Lage des Orkanzentrums und seiner Bahn. - 2.6. Wetter und Klima auf unseren wichtigsten Schiffahrtswegen. - 2.6.1. Maritime Klimatologie. - 2.6.2. Typische Wetterlagen in Ostsee und Nordsee. - 2.6.2.1. Charakteristische Merkmale einzelner Wetterlagen in der Ostsee und deren Teilgebieten. - 2.6.2.2. Charakteristische Merkmale einzelner Weiterlagen in der Nordsee und deren Teilgebieten. - 2.6.3. Großwetterlagen im Nordatlantik. - 2.6.3.1. Wetter und Klima auf den Fangplätzen der Hochseefischerei im Nordatlantik. - 2.6.4. Wetter und Klima in den äquatorialen Gebieten des Atlantiks. - 2.6.5. Wetter und Klima im Südatlantik. - 2.6.6. Wetter und Klima im Mittelmeer. - 2.6.7. Wetter und Klima im Indischen Ozean. - 2.6.8. Wetter und Klima in den chinesischen Gewässern. - 2.7. Seegang. - 2.7.1. Windsee, Dünung, Brandung. - 2.7.2. Seegangsbeobachtungen. - 2.7.3. Wellenmessungen und Wellenbeobachtungen. - 2.7.4. Seegangsvorhersagen. - 3. Meteorologische Navigation. - 3.1 Aufgabe der meteorologischen Navigation. - 3.1.1. Klimatische Navigation. - 3.1.2. Witterungsnavigation. - 3.1.3. Wetternavigation. - 3.1.3.1. Wetternavigation in der Nähe tropischer Wirbelstürme. - 3.1.3.2. Wetternavigation im Einflußbereich eines tropischen Wirbelsturms 3.1.3.3. Wetternavigation im Einflußbereich der Polarfront. - 3.1.3.4. Wetternavigation zur Vermeidung lokaler Starkwindgebiete. - 3.1.3.5. Wetternavigation zur Vermeidung von Gebieten mit hohem Seegang. - 3.1.3.6. Wetternavigation zur Vermeidung von Gebieten mit Sichtbehinderung. - 4. Aufgabensammlung. - 4.1. Luftfeuchte. - 4.2. Übungen zum Wetterschlüssel. - 4.3. Zeichnen von Wetterkarten. - 4.3.1. Analysen mit Wirbelstürmen. - 4.3.2. Meteorologische Navigation in der Nähe eines tropischen Wirbelsturmes. - Anhang. - Tafel I Windstärkenskala nach Beaufort und Seegang. - Tafel II Beobachtungs-Hilfstafel (See). - Tafel III Wetterzustand . - Tafel IV i-x Diagramm für 760 Torr. - Tafel V Psychrometer- Nomogramm. - Tafel VI Windstärkenbestimmung aus der Bordwetterkarte. - Tafel VII Analysenschlüssel - Kurzform. - Tafel VIII Umrechnung des Luftdruckes von Torr in Millibar. - Tafel IX Reduktion des Luftdruckes auf den Meeresspiegel. - Tafel X Verschlüsselungsskizzen und Wolkentafel. - Sachwortverzeichnis. - Quellennachweis der Abbildungen. - Literaturhinweise.
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  • 8
    Call number: MOP 45564 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 50 Seiten
    Language: German
    Location: MOP - must be ordered
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  • 9
    Monograph available for loan
    Monograph available for loan
    Braunschweig : Westermann
    Call number: MOP 40017 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 163 Seiten , Illustrationen
    Series Statement: Das geographische Seminar
    Language: German
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  • 10
    Call number: PIK M 323-19-93070
    Type of Medium: Monograph available for loan
    Pages: XII, 216 Seiten , Diagramme
    Series Statement: Heidelberger Taschenbücher 36
    Language: German
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  • 11
    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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  • 12
    Call number: MOP 41158 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 122 Seiten , Illustrationen
    Language: English
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  • 13
    Monograph available for loan
    Monograph available for loan
    Berlin : Julius Springer
    Call number: MOP 41231 / Mitte
    Description / Table of Contents: Hochwasservoraussagen liefern heute noch vielfach unbefriedigende Ergeb­nisse. Das mag mit ein Grund sein dafür, daß außer einigen kürzeren Abhand­ lungen keine umfassendere Veröffentlichung auf diesem Gebiet bisher erschienen ist. Vorliegende "Hochwasservoraussage" versucht diese Lücke zu schließen und will gleichzeitig einen Beitrag zur Verbesserung der Voraussagen leisten. Der erste Teil des Werkchens bringt einen Überblick über den heutigen Stand der Voraussage aus der Wetterlage, aus den Niederschlägen und aus den Wasser­ ständen bzw. Wassermengen. Im zweiten Teil werden sodann alle Einflüsse unter­ sucht, die bei Bildung und Abfluß eines Hochwassers zusammenwirken, daraus allgemeingültige Gesichtspunkte für die Voraussage abgeleitet und diese in einem Verfahren zusammengefaßt. Mit Rücksicht auf die zu Beginn des Ausbaues einer Vorhersage meist nur wenigen vorhandenen Unterlagen beginnt dieses Verfahren als reines Wasserstandsverfahren, das dann bis zur Niederschlagsvoraussage mit Verwendung der Wassermengen ausgebaut werden kann, bei gleichzeitiger Stei­ gerung der Vorhersagegenauigkeit und Verlängerung der Vorhersagezeit. Die Betrachtung der Hochwasserverhältnisse zeigt verschiedene Ursachen für bis­ herige Mißerfolge und damit den Weg zur Verbesserung und den Ausbau be­ stehender Verfahren. Daneben konnten verschiedene Zusammenhänge über den Wasserabfluß und die Beziehungen zwischen Fluß-und Grundwasser aufgezeigt werden, die außer für die Hochwasservoraussage auch von allgemeinerem Inter­ esse sein werden, wie z. B. : Die Betrachtung über die Dichte des Flußschlauches, die Bestimmung der Größe der Versickerung pro Zeiteinheit für die verschiedenen Wasserstände, die erweiterte Schlüsselkurve, die Überlagerung von Vorauseilen und Retention bei Bildung der Fließzeit, ein Verfahren für die Ermittlung der Seeretention in der Voraussage, usw.
    Type of Medium: Monograph available for loan
    Pages: VII, 87 Seiten
    ISBN: 978-3-642-92374-6
    Language: German
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  • 14
    Monograph available for loan
    Monograph available for loan
    Amsterdam : Elsevier
    Call number: MOP 43353 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XII, 347 Seiten , Illustrationen , 2 Beilagen , 23 cm
    Language: English
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  • 15
    Monograph available for loan
    Monograph available for loan
    Toronto : Atmospheric Environment Service, Environment Canada
    Call number: MOP 42751 / Mitte
    Type of Medium: Monograph available for loan
    Pages: V, 60, 25 Seiten , Illustrationen
    Series Statement: Canadian meteorological memoirs 25
    Language: English
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  • 16
    Call number: MOP 41477 / Mitte
    Type of Medium: Dissertations
    Pages: 46 Seiten, [10] Blätter
    Language: German
    Note: Dissertation, Königsberg, Albertus-Universität zu Königsberg/Pr., 1935
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  • 17
    Call number: MOP 41085 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XIII, 144 Seiten , Illustrationen
    Language: English
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-96
    In: Research report / Cold Regions Research and Engineering Laboratory, 96
    Description / Table of Contents: Techniques were established by which quantitative data can be obtained from patterned ground features. The field work was carried out during the summers of 1954 and 1955 near Camp Tuto, Greenland. The investigation site is described, and extensive data are presented. The soil materials composing the patterned ground features were found to be of common mineralogy, grain size distribution, and plasticity. The chemical nature of the soils does not contribute to feature formation; it is the mechanical processes acting on these materials that are important. A sharp rise in the soil water content in the form of ice was consistently noted when passing through the base of the active layer into the present permafrost. A net heave occurred at both feature center and border locations, The magnitude of the heave is about 0.05 ft for the centers and 0.03 ft for the borders. Feature age was estimated to be about 150 yr. Vertical sorting occurs over the entire depth of the active layer but radial sorting is confined to the upper 2 ft. Groundwater flow occurs mostly through the feature borders, and incoming radiation has an important effect on the progression of the frost line. The progression of thaw is very rapid and, by the end of summer, the thaw penetration is greatest under the feature centers.
    Type of Medium: Series available for loan
    Pages: VI, 76 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 96
    Language: English
    Note: CONTENTS Preface Summary Introduction Site of investigation Selection of study area General information about site and vicinity Accumulation and initial evaluation of data Feature 1 - preliminary study (raised center feature) Feature 2 - bench mark excavation - preliminary soils study (depressed center feature) Feature 3 - cobble orientation study Feature 4 - precise movement survey Feature 5 - radial comparison studies Feature 6 - moisture content survey Feature 7 - temperature and heat flow study (depressed center feature) Feature 8 - temperature and heat flow study (raised center feature) Feature 9 - ground water table studies Features 10 and 11 - permafrost table survey (depressed and raised center features) Combined analysis of data Sharp rise in water content at frost table Estimate of heave since deposition Study of heave measurements Consideration of feature formation time Soil grain size distribution within features Conclusions Recommendations for future work in this or similar patterned ground study areas Heave and ground-ice accumulation Solifluction ground flow Incoming radiation and soil albedo References Appendix A: General. study of heat budget of the active layer
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  • 19
    Monograph available for loan
    Monograph available for loan
    Helsinki
    Call number: O 1354
    Type of Medium: Monograph available for loan
    Pages: 72 Seiten
    Series Statement: Sonderveröffentlichung / Baltische Geodätische Kommission 5
    Language: German
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  • 20
    Monograph available for loan
    Monograph available for loan
    Leningrad : Hydrometeorologischer Verl.
    Call number: MOP 38306
    Type of Medium: Monograph available for loan
    Pages: 2 Bd.
    Language: German
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  • 21
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    Monograph available for loan
    Berlin : Akad.-Verl.
    Associated volumes
    Call number: MOP 38726
    In: Mathematische Lehrbücher und Monographien
    Type of Medium: Monograph available for loan
    Pages: XI, 343 S. : Ill.
    Series Statement: Mathematische Lehrbücher und Monographien : Abteilung 2, Mathematische Monographien 23
    Uniform Title: Čislennaja realizacija variacionnich metodov
    Language: German
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  • 22
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    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 13.0083
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 471 S., Ill., graph. Darst., kt-.
    Series Statement: Developments in sedimentology 9A
    Language: English
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  • 23
    Monograph available for loan
    Monograph available for loan
    Berlin : VEB Dt. Verl. d. Wissenschaften
    Call number: MOP 33238
    Type of Medium: Monograph available for loan
    Pages: 301 S.
    Edition: Gekürzte Ausg.
    Uniform Title: Filosofskie problemy fiziki elementarnych častic
    Language: German
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  • 24
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    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-266
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Review of dielectric properties of soils and rocks. - Methods and measurements. - Introduction. - Dispersion. - Experimental procedures. - Introduction. - Apparatus. - Correction for stray fields. - Material. - Results. - The dielectric properties of Na-montmorillonite suspensions as a function of concentration. - The dielectric properties of K-montmorillonite water suspension. - Conclusions. - Outlook. - Literature cited.
    Description / Table of Contents: The dielectric properties of Na- and K- montmorillonite suspensions with concentrations varying from 2.5% to 0.10% by weight were measured at 25°C in the frequency range of 50 Hz to 20 kHz. Effects of electrode polarization were minimized by using the same stainless steel electrodes at different interelectrode distances and a correction was applied to compensate for stray fields. This investigation establishes the fact that the high dielectric constants of clay suspensions at audio frequencies are real and not the result of electrode polarization. The polarization that determines the dispersion is an interfacial phenomenon between the ionic atmosphere and the negatively charged clay particle. The results of this study show that clay suspensions have the same dispersion as soil samples, indicating the probability that the dispersion of wet soils in the frequency range from 50 Hz to 20 kHz is similar for most soils. The actual value of the dielectric constant, however, cannot yet be predicted.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 266
    Language: English
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  • 25
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    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    Language: English
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  • 26
    Monograph available for loan
    Monograph available for loan
    Karl-Marx-Stadt : Institut für Fachschulwesen der Deutschen Demokratischen Republik
    Call number: AWI G4-18-92019
    Type of Medium: Monograph available for loan
    Pages: 64 Seiten , Tabellen
    Language: German
    Note: Inhaltsverzeichnis: 0. Einleitung. - 1. Pegelstellen. - 1.1 Allgemeine Erläuterungen. - 1.2 Anforderungen an Pegelstellen. - 1.3 Einrichtung von Pegelstellen. - 2. Pegelarten. - 2.1 Allgemeine Erläuterungen. - 2.2 Lattenpegel. - 2.3 Mechanische Schreibpegel. - 2.4 Druckluftpegel. - 2.5 Elektrische Fernpegelanlagen. - 2.6 Durchführung der Wasserstandsbeobachtung. - 3. Durchflußbestimmung. - 3.1 Allgemeine Erläuterungen. - 3.2 Behältermessung. - 3.3 Farbgeschwindigkeitsmessung. - 3.4 Schwimmermessung. - 3.5 Danaiden oder Maßdüsen. - 3.6 Staurohr. - 3.7 Wasserzähler. - 3.8 Radioaktive Isotope. - 3.9 Salzverdünnungsmessung. - 3.10 Maßwehre, Venturikanäle. - 4. Durchflußmessungen mit dem hydrometrischen Flügel. - 4.1 Meßgerät. - 4.2 Flügelarten. - 4.3 Auswahl und Einrichtung einer Durchflußmeßstelle. - 4.4 Durchführung der Durchflußmessung. - 4.5 Auswertung der Messungen. - 4.5.1 Rechnerische Auswertung der Messungen. - 4.5.2 Graphische Auswertung der Messungen. - 4.6 Ablaufmessungen. - 4.7 Auswertung bei wechselndem Wasserstand. - 5. Durchflußkurven. - 5.1 Konstruktion der Durchflußkurve. - 5.2 Durchflußtafel. - 6. Messungen und Auswertungen bei Eis und Verkrautung. - Literaturverzeichnis.
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  • 27
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    Series available for loan
    Potsdam : Zentralinstitut Physik der Erde
    Associated volumes
    Call number: 21/SR 90.0917(1)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 1
    Description / Table of Contents: Es werden geometrische Eigenschaften der räumlichen Bahnkurven der durch die 2 - 10s - Mikroseismik verursachten Bodenschwingungen untersucht. Dabei ergeben sich für Stationen im Inneren des Kontinents ebene, polarisierte Schwingungen, deren Polarisation von der Wetterlage über dem Nordatlantik abhängt. Davon ausgehend wird ein neues Verfahren zur Erhöhung des seismischen Signal-Rausch-Verhältnisses (SNR) entwickelt. Eine Übersicht über das Quellenproblem der Mikroseismik schließt sich an.
    Description / Table of Contents: The author has investigated geometrical quantities of the spatial particle orbits of 2 - 10s microseisms. For stations in the interior of the Continent these orbits are plane and polarized. The polarization depends on the weather situation over the Northern Atlantic. The paper presents a new method for signal-to-noise ratio augmentation, which is based on the found polarization phenomenon. A chapter follows on nature and sources of microseisms.
    Type of Medium: Series available for loan
    Pages: 190 Seiten , Illustrationen , 30 cm
    Edition: Als Manuskript gedruckt
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 1
    Language: German
    Note: Zugl.: Freiberg (Sachsen), Bergakad., Fak. für Mathematik und Naturwiss., Diss., 1969 , Inhaltsverzeichnis --- A Untersuchung der Polarisation und anderer Eigenschaften der langperiodischen Mikroseismik (Teil I, Text) --- 1. Einleitung --- 2. Die erste Aufbereitung der seismischen Registrierungen --- 3. Die Krümmungen als Unterscheidungsmerkmal --- 4. Die Polarisation der Mikroseismen --- 5. Vergleich Berggießhübel-Moxa --- 6. Die Einsatzsuchfunktion F --- 7. Besprechung der hinsichtlich ihrer Schwingungsebenenpolarisation untersuchten Stürme im Zusammenhang mit der Wetterlage --- 7.1 Der Sturm vom 28.1.1968 --- 7.2 Der Sturm vom 7.2.1967 --- 7.3 Der Sturm vom 6.2.1968 --- 7.4 Der Sturm vom 6.12.1966 --- 7.5 Der Sturm vom 15./16.12.1967 --- 7.6 Der Sturm vom 27./28.10.1967 --- 7.7 Weitere Stürme --- 8. Die Beziehung zwischen Amplitude und Periode der Mikroseismik der Stationen Berggießhübel und Moxa --- 9. Die Neigungswinkelverteilungen --- 10. Vergleich der Mikroseismik von Berggießhübel mit der von in Küstennähe gelegenen Stationen insbesondere Hamburg --- 10.1 Peilungen --- 10.2 Gestalt der Schwingungen --- 10.3 Polarisation der mikroseismischen Schwingungs-"Ebenen" und Polarisationsfilter --- 10.4 Schwingungstypen --- 10.5 Vergleich der Neigungswinkelverteilungen --- 10.6 Wellennatur --- 11. Deutung und Übersicht zum Quellenproblem --- 11.1 Theorien --- 11.2 Ozeanmikroseismen --- 11.3 Welche Quellen der Mikroseismik sind für Mitteleuropa maßgeblich? --- 11.4 Küstenmikroseismen --- 11.5 Mikroseismen, die in Nebenmeeren und Binnenseen entstehen --- 11.6 Lokale langperiodische Mikroseismen --- 12. Zusammenfassung --- Literatur --- B Polarization of Microseisms and Signal-to-Noise Ratio Enhancement --- A Untersuchung der Polarisation und anderen Eigenschaften der langperiodischen Mikroseismik (Teil II, Anlagen)
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  • 28
    Monograph available for loan
    Monograph available for loan
    Leipzig : VEB Bibliographisches Institut
    Call number: AWI A3-18-91938
    Type of Medium: Monograph available for loan
    Pages: 191 Seiten , Illustrationen
    Edition: 1.-6. Tausend
    Series Statement: Meyers Taschenlexikon
    Language: German
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  • 29
    Series available for loan
    Series available for loan
    Potsdam : Zentralinstitut Physik der Erde
    Associated volumes
    Call number: 21/SR 90.0917(3)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 3
    Description / Table of Contents: Es werden die Störungen im zeitlichen Ablauf der Amplituden und Phasen zweier auf elastischem Stativ schwingender Schwerependel untersucht. Betrag und Periode der Störungen werden in Abhängigkeit von den Anfangsbedingungen und dem Verhältnis [...] zwischen dem Parameter der elastischen Kopplung und der Verstimmung der beiden Pendel dargestellt. Es zeigt sich, daß die Amplituden und Phasendifferenzen bei [...] = 1 am stärksten gestört sind und mit wachsendem [...] zunehmend von den Anfangsbedingungen beeinflußt werden. Die Ergebnisse absoluter und relativer Pendelmessungen bestätigen den theoretischen Befund.
    Description / Table of Contents: Disturbances are investigated which are introduced by the sway effect into the time-functions of amplitudes and phases of two pendulums swinging on the same support. Rate and period of the disturbances are represented as functions of the initial conditions and the quotient [...] formed by the parameter of elastic coupling and the differences of the periods of the two pendulums. Hence it follows that the perturbations of the amplitudes and phase differences are biggest if [...] = 1. With increasing [...] the influence of the initial condi tions is growing up. The results of absolute and relative pendulum measurements confirm the theoretical statements.
    Type of Medium: Series available for loan
    Pages: 26 Seiten , 8 Diagramme , 30 cm
    Edition: Als Manuskript gedruckt
    ISSN: 0514-8790
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 3
    Language: German
    Note: 1. Die Differentialgleichungen des Problems und ihre Lösungen 2. Amplituden- und Phasenverlauf bei gegeneinander schwingenden Pendeln 3. Diskussion der Lösungen 3.1. Verlauf der Amplitudenschwankungen 3.2. Verlauf der Phasenschwankungen 4. Zur Mitschwingreduktion der Schwingungszeiten 5. Praktische Anwendungen Literatur Abbildungen
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  • 30
    Monograph available for loan
    Monograph available for loan
    London : The National Society for Clean Air
    Associated volumes
    Call number: MOP 41127 / Mitte
    In: Proceedings of the International Clean Air Congress
    Type of Medium: Monograph available for loan
    Series Statement: Proceedings of the International Clean Air Congress Proceedings: part 2
    Language: English
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  • 31
    Monograph available for loan
    Monograph available for loan
    Paris : Organisation Européenne de Recherches Spatiales
    Call number: MOP 41394 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 55 Seiten , Illustrationen
    Series Statement: European Space Research Organization: Scientific note 54
    Language: English
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  • 32
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    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: PIK M 323-19-93071
    Type of Medium: Monograph available for loan
    Pages: X, 177 Seiten , Diagramme
    Series Statement: Heidelberger Taschenbücher 43
    Language: German
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  • 33
    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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  • 34
    Monograph available for loan
    Monograph available for loan
    London : The National Society for Clean Air
    Associated volumes
    Call number: MOP 41126 / Mitte
    In: Proceedings of the International Clean Air Congress
    Type of Medium: Monograph available for loan
    Series Statement: Proceedings of the International Clean Air Congress Proceedings: part 1
    Language: English
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  • 35
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-203-116
    In: Special report / Cold Regions Research and Engineering Laboratory, Corps of Engineers, US Army, 116
    Description / Table of Contents: Abstract: Pendulum steering, a new concept of attitude stabilization for thermal probes or coring drills in ice, eliminates instability. The center of support is placed above the center of gravity. A lower and upper hot point produce melt penetration. The ratio of their power levels is the basis for stabilization, which is provided by the automatic control of the heater in the upper hot point. This feature makes possible a single thermal probe design that is suitable for all ice cap temperatures and a wide range of penetration rates (i.e., applied power levels). The simplicity of a thermal probe with pendulum steering suggests availability at modest cost and versatility as a widely applicable tool.
    Type of Medium: Series available for loan
    Pages: iv, 4 Seiten , Illustrationen
    Series Statement: Special report / Cold Regions Research and Engineering Laboratory, Corps of Engineers, US Army 116
    Language: English
    Note: CONTENTS Preface Summary Introduction The principle of pendulum steering Analysis of the power requirements The upper heater control Laboratory tests Summary
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  • 36
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-109
    In: Research report / Cold Regions Research and Engineering Laboratory, 109
    Description / Table of Contents: Summary: The present paper contains a critical study of a number of foundation models suggested by various investigators, as well as a further development of some of the ideas involved. It is found that the model by Pasternak is the most natural extension of the Winkler foundation. It is also shown that the "non-solvability" of the problem of a finite bean or plate resting on a continuous foundation as posed by Wieghardt and further elaborated by Pflanz is not correct, and that problems of this type are solvable for any load distribution permissible in classical plate theory. The paper concludes with derivations of differential equations for plates resting on viscous and viscoelastic foundations, which may be used for solving problems involving compacted snow and permafrost bases.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 109
    Language: English
    Note: CONTENTS Preface Summary Introduction The Hetényi foundation The Filonenko-Borodich foundation The Pasternak foundation Plates on a Pasternak foundation Visco-elastic Pasternak foundation Plates on visco-elastic foundations References Appendix A: Notation
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  • 37
    Call number: ZSP-202-111,2
    In: Research report / Cold Regions Research and Engineering Laboratory, 111,2
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    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 111,2
    Language: English
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  • 38
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-116
    In: Research report / Cold Regions Research and Engineering Laboratory, 116
    Description / Table of Contents: Abstract: Specimens of snow from the South Pole were tested to investigate air permeability K (cm/sec), ultimate compressive strength σc (g/cm^2 ) and dynamic Young's modulus E (g/cm^2 ) as a function of density. Anisotropy in a single layer of snow (snow between two summer crusts) was found in all three properties. Comparison with data for snow from Site II, Greenland, showed an empirical relation for both areas: σc = 10.42 x 10^-4 E for 0.43 g/cm^3 〈 ρ 〈 0.51 g/cm^3. σc = 5.68 x 10^-4 E for 8.63 x 10^3 g/cm^2 for 0.51 g/cm^3 〈 ρ 〈 0.90 g/cm^3. Air permeabilities are different for the two sites because of time and meteorological effects.
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    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 116
    Language: English
    Note: CONTENTS Preface Summary Introduction Preparing the snow specimens Air permeability Experimental procedure Results and discussion Viscoelastic properties Principle Experimental method Results and discussion Creep tests Unconfined compressive strength Experimental procedure Results and discussion General discussion Literature cited Appendix A: Test result
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  • 39
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-77
    In: Research report / Cold Regions Research and Engineering Laboratory, 77
    Description / Table of Contents: Abstract: A deep rotary core drilling project in 1957 at Site 2 on the Greenland ice sheet (76°59'N, 56°04'W provided ice core to a depth of 411 m. The vertical variation in bulk density, macroscopic structure, oxygen isotope ratios, ionic constituents, and extraterrestrial dust (black spherules) were analyzed using both field and laboratory techniques . These data permit the direct estimate of annual accumulation layers in the core. Continuous stratigraphic measurements and observations were made over the upper 110 m of the profile and detailed physical and chemical analyses were made on continuous lo 3 to 3.9-m core increments at 100, 200, 300 and 411-m depths. The average total ionic concentration in the ice sheet ranges between 0.65 and 1.35 mg/liter. The annual global mass deposit of black spherules as calculated from these studies varies from 2.10 x 10^5 metric tons in 700 year old ice to 6.57 x 10^5 metric tons in 12 year old firn. The oxygen isotope ratio variation provides the best means of estimating accumulation at depth. Results of the investigations indicate rates of net snow accumulation of 42.3, 34.2, 37.4, 41.1 and 41.6 g/cm^2 -yr at the surface, A.D. c. 1773, c. 1513, c. 1233 and c. 934 respectively. Accumulation data and other physical and chemical evidence allow climatological inferences to be made over the 10-century profile. The ice core record shows that snow accumulation and temperature in A. D. 934 were similar to today, followed by a gradual decrease in accumulation to a minimum around the late 18th century and an increase in both accumulation and temperature from A. D. 1773 to 1957 and following.
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    Pages: vi, 130 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 77
    Language: English
    Note: CONTENTS Preface Summary 1. lntroduction General background Previous work The Greenland Ice sheet Present work Ice core studies ll. Field procedures General background Subsurface snow laboratory Core reference datum Core handling and processing Ill. Macroscopic stratigraphy General background Polar stratigraphy General observations and results Discussion of results and conclusions above 100 m IV. Detailed stratigraphic studies General background Macroscopic stratigraphy at 100 m Results of analysis and discussion Summary and conclusions V. Oxygen isotope studies General background Previous work Deep ice core 0-isotope stratigraphy Results of analyses Summary and conclusions Vl. Chemical composition studies General background Previous work Factors influencing the chemistry of glaciers Deep core stratigraphy using chemical variations Results of analyses and discussion Summary and interpretation of the 300 m results Geochemistry of the ice sheet Results of analyses and discussion Summary and conclusions Vll. Cosmic dust studies General background Previous work Origin of extraterrestrial dust Deep ice core and near surface studies Results of analyses Discussion of results Summary and conclusions VIII. Climatological implications General background Recent history of the inland ice Past history from the deep core Summary and conclusions- IX. Summary and conclusions Discussion Post Site l deep drilling programs Selected bibliography Appendix A. Sorge's law Appendix B. Thinning of layers Appendix C. Statistical terms Appendix D. Average density determinations for meter increments from the surface to 411.21 meters , Site 2, Greenland
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  • 40
    Call number: 10.1144/GSL.SP.1967.002.01.01 (e-book)
    In: Special publications / the Geological Society, London, Volume 2
    Type of Medium: 12
    Pages: 1 Online-Ressource (XI, 827 Seiten)
    Series Statement: Special publications / the Geological Society, London 2
    Language: English
    Note: Table of Contents Introduction Geological Society, London, Special Publications, 2, 1-11, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.01 The symposium meeting Geological Society, London, Special Publications, 2, 13-14, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.02 Part I: Symposium Papers Introduction to Part I Geological Society, London, Special Publications, 2, 15-16, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.03 Life in Pre-Cambrian and early Cambrian times John Watson Cowie Geological Society, London, Special Publications, 2, 17-35, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.04 The significance of certain trace-fossil ranges Roland Goldring Geological Society, London, Special Publications, 2, 37-39, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.05 Fluctuations in the evolution of Palaeozoic intertebrates Michael Robert House Geological Society, London, Special Publications, 2, 41-54, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.06 The origins of some Silurian enteletacean brachiopods Victor Gordon Walmsley Geological Society, London, Special Publications, 2, 55-56, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.07 Permo-Triassic extinction Frank Harold Trevor Rhodes Geological Society, London, Special Publications, 2, 57-76, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.08 Changes in terrestrial vertebrate faunas during the Mesozoic C. B. Cox Geological Society, London, Special Publications, 2, 77-89, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.09 Some Cretaceous-Tertiary marine faunal changes John Michael Hancock Geological Society, London, Special Publications, 2, 91-104, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.10 Major features of the evolution of echinoids Graeme Maxwell Philip Geological Society, London, Special Publications, 2, 105-106, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.11 Plant-insect relationships in Palaeozoic and later time Norman Francis Hughes and John Smart Geological Society, London, Special Publications, 2, 107-117, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.12 Biochemical evolution and the fossil record Lambert Beverly Halstead Tarlo Geological Society, London, Special Publications, 2, 119-132, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.13 Fossil birds and their adaptive radiation James Fisher Geological Society, London, Special Publications, 2, 133-154, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.14 General Discussion Geological Society, London, Special Publications, 2, 155-156, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.15 Part II: Documentation of the Fossil Record Introduction to Part II Geological Society, London, Special Publications, 2, 158-159, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.16 Plantae Plantae N. F. H. Geological Society, London, Special Publications, 2, 162, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.17 Chapter 1 Thallophyta—1 H. P. Banks, K. I. M. Chesters, N. F. Hughes, G. A. L. Johnson, H. M. Johnson and L. R. Moore Geological Society, London, Special Publications, 2, 163-180, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.18 Chapter 2 Thallophyta—2 M. Black, C. Downie, R. Ross and W. A. S. Sarjeant Geological Society, London, Special Publications, 2, 181-209, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.19 Chapter 3 Bryophyta and Charophyta* L. J. Grambast and W. S. Lacey Geological Society, London, Special Publications, 2, 211-217, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.20 Chapter 4 Pteridophyta—1 H. P. Banks, W. G. Chaloner and W. S. Lacey Geological Society, London, Special Publications, 2, 219-231, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.21 Chapter 5 Pteridophyta—2 H. P. Banks, M. G. Collett, F. R. Gnauck and N. F. Hughes Geological Society, London, Special Publications, 2, 233-245, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.22 Chapter 6 Gymnospermophyta K.L. Alvin, P. D. W. Barnard, T.M. Harris, N. F. Hughes, R. H. Wagner and A. Wesley Geological Society, London, Special Publications, 2, 247-268, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.23 Chapter 7 Angiospermae K. I. M. Chesters, F. R. Gnauck and N. F. Hughes Geological Society, London, Special Publications, 2, 269-288, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.24 Invertebrata Invertebrata M. J. S. R. Geological Society, London, Special Publications, 2, 290, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.25 Chapter 8 Protozoa F. T. Banner, W. J. Clarke, J. L. Cutbill, F. E. Eames, A. J. Lloyd, W. R. Riedel and A. H. Smout Geological Society, London, Special Publications, 2, 291-332, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.26 Chapter 9 Porifera and Archaeocyatha R. M. Finks and D. Hill Geological Society, London, Special Publications, 2, 333-345, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.27 Chapter 10 Coelenterata G. A. L. Johnson, I. D. Sutton, F. M. Taylor and G. Thomas Geological Society, London, Special Publications, 2, 347-378, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.28 Chapter 11 Bryozoa G. P. Larwood, A. W. Medd, D. E. Owen and R. Tavener-Smith Geological Society, London, Special Publications, 2, 379-395, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.29 Chapter 12 Brachiopoda D. V. Ager, P. Copper, G. M. Dunlop, G. F. Elliott, F. A. Middlemiss, A. J. Rowell, A. Williams and A. D. Wright Geological Society, London, Special Publications, 2, 397-421, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.30 Chapter 13 Mollusca: Amphineura, Monoplacophora and Gastropoda D. Curry and N. J. Morris Geological Society, London, Special Publications, 2, 423-430, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.31 Chapter 14 Mollusca: Cephalopoda (Nautiloidea) C.H. Holland Geological Society, London, Special Publications, 2, 431-443, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.32 Chapter 15 Mollusca: Cephalopoda (Ammonoidea) D. T. Donovan, F. Hodson, M. K. Howarth, M. R. House, E. T. Tozer and C. W. Wright Geological Society, London, Special Publications, 2, 445-460, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.33 Chapter 16 Mollusca: Cephalopoda (Coleoidea) D. T. Donovan and J. M. Hancock Geological Society, London, Special Publications, 2, 461-467, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.34 Chapter 17 Mollusca: Scaphopoda and Bivalvia N. J. Morris Geological Society, London, Special Publications, 2, 469-477, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.35 Chapter 18 Arthropoda: Protarthropoda and Trilobitomorpha J. W. Cowie, W. T. Dean, R. Goldring, W. D. I. Rolfe, A. W. A. Rushton, J. T. Temple and R. P. Tripp Geological Society, London, Special Publications, 2, 479-497, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.36
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  • 41
    Call number: MOP 43905 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 135 Seiten , Illustrationen
    Language: German
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  • 42
    Monograph available for loan
    Monograph available for loan
    Gotha : Geographisch-Kartographische Anstalt
    Call number: MOP 42573 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 96 Seiten , Illustrationen, , 1 Karte
    Series Statement: Geographische Bausteine, Neue Reihe Heft 1
    Language: German
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  • 43
    Call number: MOP 43906 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 79 Seiten , Illustrationen
    Language: German
    Note: Dissertation zur Erlangung des Grades eines Doktors der Naturwissenschaften der Mathematisch-naturwissenschaftlichen Fakultät der Eberhard-Karls-Universität zu Tübingen vorgelegt von Friedrich Unz aus Schwarzenberg
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  • 44
    Call number: AWI G7-19-92221
    Type of Medium: Series available for loan
    Pages: Seiten 437 - 505 , Illustrationen
    Series Statement: Philosophical transactions of the Royal Society : Series A, Mathematical and physical sciences 265.1969,1166
    Language: English
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  • 45
    Call number: ZSP-319/C-9,2(2. Ex.) ; ZSP-319/C-9,2
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Heft 9
    In: Die wissenschaftlichen Ergebnisse der Deutschen Spitzbergenexpedition 1964-1965, Teil 2
    Type of Medium: Series available for loan
    Pages: 128 Seiten , Illustrationen, Karten , 1 Karte
    ISSN: 0435-6187
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 9,2
    Language: German
    Note: Kartenbeilage unter dem Titel: Periglaziallandschaft Irgensfjellet, Kingsbay-Westspitzbergen 〈1 : 1 500〉 , Inhalt: 4. Die Arbeiten zur Periglazialforschung 4.1. Vorwort zum Ergebnisbericht der Expeditionsgruppe Periglazialforschung 4.2. Untersuchungen zur Morphologie der periglazialen Auftauschicht im Kongsfjordgebiet (K. Herz; G. Andreas) 4.3. Untersuchungen zur Ökologie der periglazialen Auftauschicht im Kongsjfordgebiet (K. Herz; G. Andreas) 4.4. Geoelektrische Sondierungen zum Nachweis der sommerlichen Auftautiefe in der Arktis (G. Andreas) 5. Die geomagnetischen Arbeiten 5.1. Geomagnetische Tiefensondierungen am Süd- bzw. Nordufer des Kongsfjordes in Spitzbergen (V. Auster, K. Legning) 5.2. Ergebnisse der geomagnetischen Messungen der Spitzbergen-Expedition im Sommer 1964 (V. Auster, K. Legning, H. Zander) 5.3. Messungen des Erdpotentialgradienten an Land und auf See in Ny-Ålesund (K. Legning) 5.4. Messung der geomagnetischen Horizontalintensität sowie der Deklination auf einem eisernen Schiff (V. Auster, K. Legning)
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  • 46
    Call number: MOP 41371 / Mitte
    In: WMO / World Meteorological Organization
    Type of Medium: Series available for loan
    Pages: X, 145 Seiten , Illustrationen
    Language: English
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  • 47
    Call number: MOP 40138 / Mitte
    Type of Medium: Monograph available for loan
    Pages: II, 24 Seiten, IV Seiten Anhang
    Series Statement: Forschungsgesellschaft für den Wohnungsbau im ÖIAV Arbeitsunterlage A-662
    Language: German
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  • 48
    Call number: MOP 40130 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 330 Seiten , Illustrationen
    Series Statement: Umschau in Wissenschaft und Technik
    Language: German
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  • 49
    Monograph available for loan
    Monograph available for loan
    Frankfurt am Main : Umschau Verlag
    Call number: MOP 41272 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 192 Seiten , Illustrationen
    Series Statement: Wege zum Wissen
    Language: German
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  • 50
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 43365 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 338 Seiten , Illustrationen , 3 Karten , 27 cm
    Series Statement: Meždunarodnoe Gidrologičeskoe Desjatiletie / AN SSSR. Institut Geografii
    Language: Russian , English
    Note: In kyrillischer Schrift , Mit Zusammenfassung und Inhaltsverzeichnis in englischer Sprache
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  • 51
    Monograph available for loan
    Monograph available for loan
    Boston : American Meteorological Society
    Call number: MOP 40509 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 347 Seiten , Illustrationen
    Language: English
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  • 52
    Dissertations
    Dissertations
    [Münster] : [Westfälische Wilhelms-Universität]
    Call number: AWI P9-20-93557
    Type of Medium: Dissertations
    Pages: 112 Seiten , Illustrationen
    Language: German
    Note: Dissertation, Münster, Westfälische Wilhelms-Universität, 1939 , Inhaltsübersicht Vorbemerkung A. Allgemeine Einführung I. Bisherige Kenntnis und Problemstellung II. Kurze Orientierung über die topographischen Verhältnisse III. Die geologischen Verhältnisse IV. Die klimatischen Verhältnisse B. Morphologische Untersuchungen I. Das Vorland als Ganzes Beschreibung; formende Kräfte; Flächenspülung, Wind, Frostsprengung, Meereis und Schuttkriechen; Entstehung des Vorlandes II. Einzelformen des Vorlandes 1. Die polare Wanderschuttküste 2. Toteiswannen 3. Die Täler Gletschertäler, Trockentäler, Schuttquellen, Schmelzwasserrisse; Zusammenfassung III. Die Hangzone 1. Die Terrassen 2. Runsen und Schuttkegel Anhang: Hangschuttprofile IV. Das Plateaugebiet 1. Der Plateaurest im Norden 2. Das zertalte Plateau V. Ergebnisse Anhang I. Quellen und Literatur II. Karten 1. Die Arbeitsgebiete 2. Topographische Karte des nördlichen Andréelandes nach eigenen Aufnahmen im Maßstabe von 1:150 000
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  • 53
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 54
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-120
    In: Research report / Cold Regions Research and Engineering Laboratory, 120
    Description / Table of Contents: Abstract: The report is divided into four parts: Parts I and II cover investigations of the reliability of shear stress measurements in soils subjected to vibratory loads for biaxial and triaxial systems, respectively. Part I is a summary only (see USA CRREL Technical Report 90 for detailed treatment). Part III is a study of three-dimensional "principal" stress patterns produced in soil subjected to vibratory loads. Part IV is a theoretical analysis of some aspects of soil wave propagation in stratified soil. From the measurements of five shear stresses and one normal stress, the stress distribution of a triaxial system can be determined. In noncohesive soils triaxial stress fields due to vibratory loads can be determined by recording six independent stress components. Sinusoidal force excitation and impact excitation yield time-distance graphs which can be used to determine reflection and refraction techniques in stratified soils.
    Type of Medium: Series available for loan
    Pages: v, 52 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 120
    Language: English
    Note: CONTENTS Preface Summary Part I. Two-dimensional shear stress measurements Part II. Three-dimensional shear stress measurements Introduction Measurements Experimental results Evaluation Compatibility checks Comparison between shear stresses under static and dynamic loads Conclusions Part III. Three-dimensional normal stress measurements Introduction Experimental setup Results Analysis Conclusions Part IV. Soil wave propagation in stratified soil Introduttion Distance-time graphs Results Sinusoidal force excitation Refraction Impact force excitation Selected bibliography Appendix A. Equations for computing stress components in Part II Appendix B. Equations for computer program in Part III
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  • 55
    facet.materialart.12
    facet.materialart.12
    London : Geological Society of London
    Call number: 10.1144/GSL.SP.1969.003.01.01
    Type of Medium: 12
    Pages: 1 Online-Ressource (VIII, 311 Seiten)
    Series Statement: Special publications / the Geological Society, London 3
    Language: English
    Note: Table of Contents Introductory Remarks Displacement within continents Introductory remarks R. M. Shackleton Geological Society, London, Special Publications, 3, 1-7, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.01 Structural Analysis of Orogenic Belts Problems of the relationship between surface structure and deep displacements illustrated by the Zagros Range N. L. Falcon Geological Society, London, Special Publications, 3, 9-21, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.02 Some principles governing interpretation of structure in the Rocky Mountain orogenic belt F. G. Fox Geological Society, London, Special Publications, 3, 23-41, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.03 The measurement of strain and displacement in orogenic belts J. G. Ramsay Geological Society, London, Special Publications, 3, 43-79, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.04 The construction of sections in areas of highly deformed rocks W. E. A. Phillips and J. G. Byrne Geological Society, London, Special Publications, 3, 81-93, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.05 The palaeomagnetic evidence of displacements within continents D. H. Tarling Geological Society, London, Special Publications, 3, 95-113, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.06 Historical Analysis of Orogenic Belts Interpretation of stratigraphical ages in orogenic belts W. B. Harland Geological Society, London, Special Publications, 3, 115-135, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.07 Interpretation of isotopic ages in orogenic belts P. E. Brown and J. A. Miller Geological Society, London, Special Publications, 3, 137-155, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.08 A new approach to radio-isotopic dating in orogenic belts F. J. Fitch, J. A. Miller and J. G. Mitchell Geological Society, London, Special Publications, 3, 157-195, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.09 Other Analyses Orogenic belts and their parts N. Rast Geological Society, London, Special Publications, 3, 197-213, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.10 Sedimentary thicknesses in orogenic belts R. Stoneley Geological Society, London, Special Publications, 3, 215-238, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.11 Rates of change within orogenic belts J. Sutton Geological Society, London, Special Publications, 3, 239-250, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.12 The deep structure of orogenic belts—the root problem E. R. Oxburgh Geological Society, London, Special Publications, 3, 251-273, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.13 Orogeny in relation to crust and upper mantle M. H. P. Bott Geological Society, London, Special Publications, 3, 275-283, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.14 Internal features of some orogenic belts of Africa T. N. Clifford Geological Society, London, Special Publications, 3, 285-287, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.15 Closing Remarks Displacement within continents Kingsley Charles Dunham Geological Society, London, Special Publications, 3, 289-290, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.16 Discussion Geological Society, London, Special Publications, 3, 291-308, 1 January 1969, https://doi.org/10.1144/GSL.SP.1969.003.01.17
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  • 56
    Series available for loan
    Series available for loan
    Berlin : VEB Deutscher Verlag der Wissenschaften
    Associated volumes
    Call number: 7120
    In: Mathematische Forschungsberichte, 23
    Type of Medium: Series available for loan
    Pages: 98 Seiten , Illustrationen
    Series Statement: Mathematische Forschungsberichte 23
    Language: English
    Note: TABLE OF CONTENTS Abstract Introduction Chapter I. The algebras H and L 1. Notation. General conventions 2. Fundamental notions and definitions 3. Geometrical interpretation 4. Summary Chapter II. Monogenic functions 1. Functions which have hypercomplex values 2. Monogenic functions 3. Representatives of monogenic functions in the Banach algebra Lγ 4. Analyticity of monogenic functions Chapter III. Some elementary monogenic functions I. Introduction 2. The inverse function ζ-1 3. The exponential function 4. The components of a power series with real coefficients 5. Trigonometric and hyperbolic functions 6. The logarithmic function 7. The inverse function ζ*-1 8. The singular manifold of (ζ-α*)-1 Chapter IV. Hypercomplex integrals and theorems of Cauchy's type 1. Introduction. Integrals of hypercomplex-valued functions 2. Integrals of monogenic functions over closed curves and surfaces 3. Cauchy's second theorem for monogenic functions of ζ 4. An application of Cauchy's second theorem Chapter V. On some results of Marcel N. Roşuleţ 1. Introduction 2. An algebra associated with Laplace's equation 3. Summary of analysis 4. On the relation between the algebras U and L Appendix. The product of two algebra elements Bibliography
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  • 57
    Monograph available for loan
    Monograph available for loan
    Düsseldorf : Econ-Verlag
    Call number: AWI E2-23-95526
    Description / Table of Contents: Pavel Gordijenko hat sein Leben der Polarforschung gewidmet. Er machte auf Eisbrechern Expeditionen mit, überwinterte auf Polarstationen, führte Eisdriftfahrten, Eiserkundungsflüge und Kreuzfahrten vor den arktischen Küsten durch. Er gibt in diesem Buch weitreichende Einblicke, warum, wie und mit welchen Ergebnissen die sowjetischen Forscher die Geheimnisse des Nordpols und des riesigen Meeres, das diesen bemerkenswerten Punkt umgibt, ergründen konnten. In dem Vorwort zu diesem zuerst in deutscher Sprache erschienenen Werk vermerkt der sowjetische Wissenschaftler: »Ich habe mich entschlossen, in diesem Buch die Hauptergebnisse der wissenschaftlichen Forschungsarbeiten sowjetischer Polarforscher in der Zentralarktis allgemein verständlich darzustellen. Um dieser schwierigen Aufgabe gerecht zu werden, habe ich mich entschieden, nur die Forschungsarbeiten der letzten 25 Jahre zu behandeln. Ich würde jedoch meine Aufgabe als nur teilweise gelöst empfinden, wenn ich mich auf eine trockene Darlegung der wissenschaftlichen Forschungsergebnisse beschränken und nichts davon berichten würde, wie Menschen der verschiedensten Berufe in der Arktis leben und arbeiten, unter welchen Bedingungen und unter welchen Mühen sie hier ihre Kenntnisse sammeln, mit welchen Gefahren und Entbehrungen ihre Arbeit manchmal verbunden ist. Ich werde deshalb in meinem Buch auch einige Episoden erzählen, die teils ungewöhnliche und bedeutungsvolle Ereignisse und Vorkommnisse beinhalten, teils jedoch auch Dinge, die für einen Polarforscher nichts Ungewöhnliches sind. Ich schreibe hier einerseits als Augenzeuge, andererseits als Beteiligter.« So ist ein Buch entstanden, das eine Reihe der faszinierenden Phänomene der Arktis verständlich macht, etwa die Entstehung des Nordlichts, die Bewegung des Eises und die gewaltigen, Auswirkungen der Meeresströmungen, ein Buch, das zudem Einblicke gibt, wie die verschiedenen .Forschergruppen - Hydrologen, Aerologen, Meteorologen,Geographen,Geologen, Ozeanographen, Physiker u. a. mehr - zusammenarbeiten, um die Arktis als Lebensraum für den Menschen zu erschließen, neue Verkehrswege zu finden, die Wettervorhersage zu vervollkommnen, vielleicht sogar das Klima zu beeinflussen. Polarforschung ist trotz aller technischen Vervollkommnung noch immer eines der großen Abenteuer unseres Jahrhunderts. Es bezieht seine Faszination aus dem Kampf des Menschen mit »ihrer Majestät - der arktischen Natur«, in der es Siege und Niederlagen gibt, von dem wir aber wissen, »daß die rauhe Natur dem Menschen allmählich untertan wird und ihre Kräfte ihm schon zu dienen beginnen«,
    Type of Medium: Monograph available for loan
    Pages: 350 Seiten , Illustrationen , 1 Beilage
    Edition: 1. Auflage
    Language: German
    Note: INHALTSVERZEICHNIS Vorwort 1. Kapitel DER KLEINSTE UND RAUHESTE OZEAN Das Nördliche Eismeer und der Nordpol Was ist die Arktis? Und dieser Ozean ist voller Leben Gutes oder »schlechtes« Wetter Die Rauheit des Wetters und Möglichkeiten der menschlichen Tätigkeit Die Polarländer - Antipoden 2. Kapitel VON DER LEGENDE ZUR WISSENSCHAFTLICHEN ERKENNTNIS In alten Zeiten Die Idee der Nordost-Passage Spitzbergen und Nowaja Semlja Erforschung der asiatischen Küsten des Nördlichen Eismeeres Die Große Nordexpedition Der Begründer der Polarozeanographie Der erste Versuch einer Fahrt zum Pol Die geheimnisvolle Insel Russen in Amerika Transarktisfahrten zum Nordpol Die neue Technik im Dienst der arktischen Wissenschaft Die Entdeckung von Sewernaja Semlja Die Hauptergebnisse der russischen Polarforschung bis zur Oktoberrevolution 3. Kapitel IN DER ARKTIS HEUTE Die ersten Etappen sowjetischer Arktisforscher Die »Sibirjakow« und die Entwicklung des Nördlichen Seeweges Die weitere Forschung Die weißen Flecke von der Landkarte der Zentralarktis verschwinden Polarstationen - ständige Vorposten der arktischen Wissenschaft Die Arktis ist unerbittlich Dem Tod um Haaresbreite entgangen Ein »bedingter Reflex« führt zu einer mißlichen Lage Vorbereitungen für eine Bergbesteigung Aus dem Bergsteiger-Tagebuch Der Gipfel ist bezwungen Von der Küste ins offene Meer Die Expeditionen »Sewer« in hohen nördlichen Breiten Eine »Springgruppe« am Pol 4. Kapitel MEHR ALS ZWANZIG JAHRE DRIFT AM POL Kampf mit den Elementen Alte und neue wissenschaftliche Probleme Zeit, Trajektorien, Kilometer Neue Geräte und Ausrüstungen Die Menschen auf den »Nordpol«-Stationen und ihre Arbeit Unvergeßliche Tage auf der Drift Die Polarnacht Entdeckungen im Meer 5. Kapitel NEUE ZÜGE DER ERDOBERFLÄCHE UNTER WASSER Entdeckungen auf dem Meeresboden Die geologische Geschichte des Meeresbodens 6. Kapitel DIE DRIFT DES EISES IM ARKTISCHEN BECKEN Systematische Beobachtungen Kreisförmige Drift oder direkter Abfluß in den Atlantik? Gewundene Driftlinien der Eisfelder Schleifenkurven in der Eisdrift Drehbewegungen der Eisfelder 7. Kapitel IN DEN TIEFEN DES MEERES UND IN DER FREIEN ATMOSPHÄRE Einige Worte über Wise und Subow. Die Wassermassen und ihre Zirkulation Die Zirkulation der Atmosphäre Durch Atmosphärenforschung zur Wettervorhersage 8. Kapitel ZU KOSMISCHEN HÖHEN Geophysikalische Untersuchungen Magnetische Störungen In den ionisierenden Schichten der Erdatmosphäre »Nordlichter« 9. Kapitel DAS ZIEL IST GREIFBAR, DOCH UNGEWISS Umgestaltung der arktischen Natur Budykos Projekt Andere Pläne zur Änderung des Klimas 10. Kapitel GEBURT EINES NEUEN BERUFES Aufklärungsflüge in der Arktis Das Kartieren der Eisverhältnisse, die Einführung von Isograden und Isolinien Beobachtungen über Unebenheiten der Eisdecke 11. Kapitel VORHERSAGEN - HÖHEPUNKT DER ARKTISFORSCHUNG (Anstelle eines Schlußwortes) Anhang Anmerkungen Tabellen Stichwortverzeichnis
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    Call number: M 93.0078/2 ; M 93.0079/2
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    Berlin [u.a.] : Springer
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    London : Heinemann
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    New Brunswick [u.a.] : Rutgers Univ.
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    Bergen : Grieg
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    Jerusalem : Israel Program for Scientific Transl.
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    København : Reitzel
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    New York [u.a.] : McGraw-Hill
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    New York [u.a.] : Acad. Press
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    Leipzig : Teubner
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    Washington, DC : American Geophysical Union
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    Call number: MOP 36871 / DG
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    Pages: 59 S. , Ill., graph. Darst.
    Language: German
    Note: Inhaltsverzeichnis: 1. Einleitung. - 2. Codierer. - 2.1 Generator (Wienbrückengenerator). - 2.2 Schmitt-Trigger. - 2.3 Flip-Flop-Kette. - 2.4 Dioden-Matrix. - 2.5 Realisierung eines Ausgangswiderstandes von 600 Ohm. - 3. Decodierer. - 3.1 RC-Verstärker. - 3.2 Synchronisiereinrichtung. - 3.2.1 Impedanzstufe. - 3.2.2 Integrierglied. - 3.2.3 Schmitt-Trigger. - 3.2.4 Differenzschaltung. - 3.3 Torschaltung. - 3.4 Generator (astabiler Multivibrator). - 3.5 Zählstufe (bitertiärer Teiler). - 3.5.1 Berechnung des Binärteilers. - 3.5.2 Berechnung des Tertiärteilers. - 4. Informationsgewinnung. - 4.1 Vergleichsimpulse. - 4.2 Auswertegruppen. - 4.2.1 Koinzidenzgatter. - 4.2.2 Impedanzstufe. - 4.2.3 Gleichrichterschaltung. - 4.2.4 Schmitt-Trigger. - 5. Allgemeine Betrachtungen. - 5.1 Sicherheitsvorkehrungen. - 5.2. Betriebsspannungspolung. - 5.3 Betriebsbedingungen. - 5.3.1 Codierer. - 5.3.2 Decodierer. - 6. Technische Daten der Anlage. - 6.1 Codierer. - 6.2 Decodierer. - 7. Anhang. - 7.1 Berechnung der bistabilen Multivirat. - 7.1.1 gesperrter Zustand für T2. - 7.1.2 leitender Zustand für T1. - 7.1.3 dynamisches Verhalten. - 7.2 Berechnung von Ringteilern. - 7.2.1 gesperrter Zustand für T3. - 7.2.2 leitender Zustand für T1. - 7.3 Senderausfallentscheidung. - 8. Literaturverzeichnis. - 9. Schaltzeichnung für Codierer und Decodierer.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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