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  • 1
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : MacMillan
    Call number: IASS 17.91057
    Type of Medium: Monograph available for loan
    Pages: IX, 125 S.
    ISBN: 0333152271
    Uniform Title: Les marchés d'eurodevises engl.
    Language: English
    Branch Library: IASS
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  • 2
    Call number: ZSP-980-84
    In: ZfI-Mitteilungen, Nr. 84
    Type of Medium: Series available for loan
    Pages: 432 Seiten
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 84
    Language: German
    Note: Inhalt Bd. 84 - Vorträge 1: On some problems of the geochronological investigation by use of the lead isotope method / B. G. Amov. - Bleiisotopenverhältnisse und Altersbestimmung von Feldspäten aus südbulgarischen Graniten / B. Amow ; Z. Baldjiewa ; V. Arnaudow ; M. Pawlowa. - Möglichkeiten des Nachweises superschwerer Elemente mit massenspektrometrischen Methoden / S. Becker ; H.-J. Dietze. - Methodische Untersuchungen zur δD-Bestimmung an Gesteinen und Mineralen / T. Böttger. - Methoden der chemischen Konzentrierung und Identifizierung bei der Suche von seltenen Radionukliden in der Natur / H. Bruchertseifer. - Die Anwendung der ultraempfindlichen Massenspektrometrie zur Isotopenanalytik / H.-J. Dietze ; S. Becker. - Die getrennte Messung von Rn-220 und Rn-222 in Bodenluft und ihre geowissenschaftlichen Aussagemöglichkeiten / H. Gast ; W. Stolz. - Die Kontrolle der Standardmeßbedingungen bei 14C-Datierungen / J. Görsdorf. - Isotope analysis on nano-mole gas samples / S. Halas. - Tritium im Niederschlag Antarktikas - Aussagen zur globalen Verteilung / D. Hebert. - Isotopic characteristic of the Tithonian reef Štramberk Limestone, Czechoslovakia, West Carpathians / J. Hladíková ; H. Eliášová ; M. Eliáš. - Stable isotope ratios in the natural gas components CH4 and N2 separated by gas chromatography / G. Hut ; H. R. Weerkamp ; T. Poelhekken. - Frakcionirovanie izotopov ugleroda metanobrazujuščimi bakterijami, rastuščimi na različnych substratach / M. V. Ivanov ; S. S. Beljaev ; A. M. Zjakun ; V. A. Bondar' ; K. S. Laurinavičus ; O. V. Šipin. - Isotope geochemistry of stratified water bodies on northern Ellesmere Island, Canadian Arctic / M. O. Jeffries ; H. R. Krouse. - Zur hydrogeologischen Interpretation von Isotopendaten im Zusammenhang mit Stofftransportprozessen / H. Jordan ; D. Hebert ; K. Fröhlich ; R.-P. Scholz ; R. Gellermann. - Spurenanalytische Untersuchungen an rezenten Mineralisationen mittels Messung der natürlichen Radioaktivität, der Anwendung der Instrumentellen Neutronenaktivierungsanalyse (INAA) und der Spektrometrie protoneninduzierter Gammastrahlung (PIGE) / G. Just ; G. Loos ; J. Vogt. - 40Ar/39Ar-Altersspektrum eines Biotits / G. Kaiser ; J. Pilot. - Kalium-Calcium-Isochrone für Sylvinite des Sibirischen Tafellandes / W. S. Lepin ; S. M. Samarajew ; S. B. Brandt. - Untersuchungen zur Fraktionierung der Schwefelisotope bei der chemischen und biochemischen Oxydation von Sulfid zu Sulfat / I. Maaß ; J. Heyer ; K. Wetzel ; G. Weise. - Isotopenanalyse leichter Elemente mit einem Restgasquadrupolmassenspektrometer? / G. Meier. - Experimental studies of natural processes with help of the radioisotopes of stable elements / A. G. Mironov. - Carbon-13 in atmospheric CO2 / W. G. Mook ; C. D. Keeling. - Isotopenhydrologische Untersuchungen - Arbeiten aus dem GSF-Institut für Radiohydrometrie / H. Moser. - Untersuchungen zur Isotopenfraktionierung des Stickstoffs in den Systemen Ammonium / Ammoniak und Nitrid / Stickstoff / H.-M. Nitzsche ; G. Stiehl. - Gewinnung von Einschlußkomponenten aus Mineralen für isotopen-geochemische Untersuchungen / H.-M. Nitzsche ; G. Strauch. - Raspredelenie izotopa 14C v različnych uglerodsoderžaščich materialach i frakcijach paleopočv v svjazi s geologičeskimi uslovijami zachoronenija / L. A. Orlova ; V. A. Panyčev ; I. V. Nikolaeva. - Rb-Sr-Datierungen von Metamorphiten / J. Pilot. - Light isotope variations in carbonate sediments and their palaeogeographical value / J.-M. Punning ; T. Martma ; R. Vaikmäe. - Die isotope Zusammensetzung des Kristallwassers von Carnalliten und ihrer Ausgangslösungen / H. D. Schmiedl ; K. Koch ; T. Böttger ; G. Stiehl ; J. Pilot ; H. Jordan. - Der 18O-Index - ein isotopengeochemisches Konzept / H. Schütze. - Intramolekulare Sauerstoffisotopengeothermometrie an Hydrosilicaten / H. Schütze. - Modellbetrachtungen zur Abschätzung des δ 13C-Wertes in Pflanzen / H. Schütze ; D. Mißbach. - Isotopic composition of carbonates and differences in deposition environment during the Miocene lacustrine sedimentation in the Krušné Hory graben / V. Šmejkal. - Deuterium and oxygen-18 in water vapour and precipitation: application to atmospheric water vapour transport and to paleoclimate / C. Sonntag ; H. Schoch-Fischer. - Komplexe Isotopenuntersuchungen an armenischen Mineralwässern / R. Trettin ; A. Hiller ; E. S. Chalatjan. - Die Verteilung des Strontium-90 und Cäsium-137 im Wasserkörper der Ostsee 1975 bis 1982 / D. Weiß und E. Ettenhuber. - Preparation of CO2 for 13C/12C analysis of hydrocarbons in natural gases / W. Wolacewicz ; S. Halas. - Investigation of isotopic fractionation effects in thermal ion source for mass spectrometer / J. M. Zinkiewicz.
    Location: AWI Archive
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  • 3
    Call number: SR 17.90400(1973,2)
    In: Abhandlungen der Mathematisch-Naturwissenschaftlichen Klasse
    Type of Medium: Series available for loan
    Pages: 23 S. , graph. Darst. , 24 cm
    Series Statement: Abhandlungen der Mathematisch-Naturwissenschaftlichen Klasse 1973, 2
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Ithaca [u.a.] : Cornell Univ. Press
    Call number: IASS 16.90576
    Type of Medium: Monograph available for loan
    Pages: XI, 226 S.
    ISBN: 0801488230 (pbk.) , 9780801488238 (pbk.) , 0801440904 (cloth)
    Language: English
    Branch Library: IASS
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  • 5
    Monograph available for loan
    Monograph available for loan
    Madrid : Secc
    Call number: PIK N 456-17-90913
    Type of Medium: Monograph available for loan
    Pages: 536 Seiten
    Series Statement: Ministerio de Transportes Turismo Y Comunicaciones : Publicación Serie A 114
    Parallel Title: 1,1=6; 2,1=13 von Publicaciones / D / Ministerio del Aire, Subsecretaria de Aviación Civil, Servicio Meteorológico Nacional
    Language: Spanish
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 6
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: IASS 17.91234
    Type of Medium: Monograph available for loan
    Pages: XI, 205 S. , graph. Darst.
    ISBN: 0521796873 (pbk) , 9780521796873 (pbk) , 0521792525 (hbk) , 9780521792523 (hbk)
    Language: English
    Branch Library: IASS
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  • 7
    Monograph available for loan
    Monograph available for loan
    London : Arnold
    Call number: AWI G7-17-90989
    Type of Medium: Monograph available for loan
    Pages: XV, 608 S. , Ill., graph. Darst., Kt.
    Edition: Repr.
    ISBN: 0713153776
    Language: English
    Note: Contents: Preface. - List of Plates. - Figures in the Text. - Introduction. - PART I. BASIC CONCEPTS OF GLACIATION AND GLACIER BEHAVIOUR. - Chapter 1 Ice Ages and World Glaciation. - Chapter 2 Glacier Régimes. - Chapter 3 The Physical Properties of Ice and Types of Glacier. - Chapter 4 Ice Motion. - Chapter 5 Some Indirect Effects of Pleistocene Glaciation. - PART II. GLACIAL AND FLUVIOGLACIAL EROSION. - Chapter 6 Small-scale Features of Glacial and Fluvioglacial Erosion. - Chapter 7 Glaciated Valleys. - Chapter 8 Cirques. - Chapter 9 Glacial Erosion in Areas of Low Relief. - Chapter 10 Glaciation in Coastal Environments. - Chapter 11 Quantitative Aspects of Glacial Erosion. - Chapter 12 Erosion by Glacial Meltwater, and Glacial Diversion of Drainage. - PART III. GLACIAL AND FLUVIOGLACIAL DEPOSITION. - Chapter 13 General Considerations of Glacial and Fluvioglacial Deposition. - Chapter 14 Drumlins. - Chapter 15 Moraines. - Chapter 16 Fluvioglacial Ice-Contact Features: Eskers and Kames. - Chapter 17 Ice Stagnation Features. - Chapter 18 Proglacial Features. - Chapter 19 Glacial Lakes and Lacustrine Deposits. - PART IV. PERIGLACIAL GEOMORPHOLOGY. - Chapter 20 The Periglacial Environment: An Introductory Survey. - Chapter 21 Frozen Ground Phenomena. - Chapter 22 Patterned Ground. - Chapter 23 Periglacial Mass Movements and Slope Deposits. - Chapter 24 Altiplanation, Tors, Blockfields, and Stone Streams. - Chapter 25 The Action of Snow. - Chapter 26 Periglacial Wind Action. - Index.
    Location: AWI Reading room
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  • 8
    Monograph available for loan
    Monograph available for loan
    Moskva : Nauka
    Call number: 12256
    Type of Medium: Monograph available for loan
    Pages: 191 S
    Language: Russian
    Note: In kyrill. Schr.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 9
    Call number: M 17.91145
    Type of Medium: Monograph available for loan
    Pages: 481 S.
    Language: German
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 10
    Monograph available for loan
    Monograph available for loan
    Wittenberg Lutherstadt : Ziemsen
    Associated volumes
    Call number: AWI Bio-18-91301
    In: Die neue Brehm-Bücherei, 202
    Description / Table of Contents: Die Pollenananlyse ist ein junger Zweig der Botanik, der viele Beziehungen zu den Nachbarwissenschaften hat. Wie man mit ihrer Hilfe die quartäre Vegetationsgeschichte auf Grund mühsamer Untersuchungen und scharfsinniger Überlegungen zu rekonstruieren versucht hat, schildert dieses Büchlein. Aus der Geschichte des Pflanzenkleides ergibt sich diejenige des Klimas. Daß die Pollenanalyse neben der noch viel jüngeren Radiokarbonmethode herangezogen wird, wenn wichtige vorgeschichtliche Funde und Ereignisse zu datieren sind, und daß beide Verfahren aus der Zusammenarbeit Nutzen ziehen können, wird an praktischen Beispielen erklärt. Es wird von der nacheiszeitlichen Ausbreitung unserer Waldbäume und ihren Wegen berichtet. Die Pollen- und Sporenanalyse wird auch in älteren Ablagerungen angewendet.
    Type of Medium: Monograph available for loan
    Pages: 109 S. , Ill., graph. Darst., Kt.
    Edition: 2., erw. und verb. Aufl.
    Series Statement: Die neue Brehm-Bücherei 202
    Language: German
    Note: Inhaltsübersicht: 1. Der Blütenstaub, sein Aussehen und Aufbau, seine Bildung und Funktion. Die Sporen. - 2. Vom Pollenregen und der Erhaltung des Blütenstaubs in den Mooren. - 3. Moore und Seen als Archive der Vegetationsgeschichte. - Gewinnung und Aufbereitung des Torfes oder der Mudde. - Zählung der Pollenkörner. - Das Pollendiagramm. - 4. Die Geschichte des Pflanzenkleides im Untereichsfeld und im Harz. - Vegetationsstufen des Harzes. - Das Pollendiagramm vom Luttersee und seine Pollenzonen. - Wie weit kann man die gefundenen Pollenkörner bestimmen?. - Wie verhält sich das Pollenspektrum zur Zusammensetzung der Vegetation?. - Was bedeuten die Nichtbaumpollenwerte und die Pollendichte? Die Vegetations- und Waldzeiten. - Die Klimageschichte. - Das Pollendiagramm aus dem Oberharz. - 5. Altersbestimmung mit Hilfe der Pollenanalyse. - 5.1. Das Alter von Vulkanausbrüchen. - Der Laacher See, Entstehung der Maare. - Das Schalkenmehrener Maar, sein Pollendiagramm. - Das Alter des Schalkenmehrener Maares. - 5.2. Das absolute Alter der Pollenzonen. - Die Bändertonchronologie. - Die Radiokarbonmethode (C 14). - Vorgeschichtliche Funde. - 5.3. Das Alter der bisher datierten vulkanischen Maararusbrüche. - Das Pflanzenkleid der Maarumgebung während und nach der vulkanischen Tätigkeit. - 5.4. Die Datierung vorgeschichtlicher Funde und Ereignisse mit Hilfe der Pollenanalyse. - Der Pflug von Walle. - Brandrodungen im Pollendiagramm. - Die Vorgeschichte der Eifel im Pollendiagramm. - 6. Die Wandlung des Pflanzenkleides von Mitteleuropa während und nach der letzten Eiszeit. - Hocheiszeit. - Späteiszeit (Allerödzeit, Jüngere Tundrenzeit). - Vorwärmezeit. - Frühe Wärmezeit. - Mittlere Wärmezeit. - Späte Wärmezeit. - Nachwärmezeit. - 7. Wanderungen und Wanderwege der Waldbäume und der Hasel in Mitteleuropa seit der letzten Eiszeit. - 7.1. Pollenniederschlagskarten und Diagrammketten. - 7.2. Die Birken. - 7.3. Die Kiefern. - 7.4. Die Hasel. - 7.5. Die Eichen. - 7.6. Die Ulmen. - 7.7. Die Linden. - 7.8. Die Esche. - 7.9. Weitere Bäume des Eichenmischwaldes. - 7.10. Die Erlen. - 7.11. Die Fichte 7.12. Die Tanne. - 7.13. Die Rotbuche. - 7.14. Die Hainbuche. - 7.15. Die Eibe. - 8. Pollenfunde einiger anderer spät- und nacheiszeitlicher Pflanzen. - 9. Die Vegetationsgeschichte in den Kalt- und Warmzeiten des Quartärs. - 10. Die Anwendung der Pollen- und Sporenanalyse in älteren Ablagerungen. - 11. Von anderen Zweigen der Pollenforschung. - 12. Hinweise auf einige wichtige Bücher und Aufsätze zur Erweiterung des Studiums sowie auf die Herkunft der Bilder.
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  • 11
    Monograph available for loan
    Monograph available for loan
    Kaiserslautern : Technische Universität Kaiserslautern
    Call number: M 18.91476
    Type of Medium: Monograph available for loan
    Pages: ii, 157 Seiten , Graphische Darstellungen
    Language: English
    Note: Kaiserslautern, Technische Universität, Dissertation, 2003 (Nicht für den Austausch)
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 12
    Call number: AWI Bio-18-91483
    Type of Medium: Monograph available for loan
    Pages: 639 Seiten , Illustrationen
    Edition: 12. Auflage
    Language: German
    Note: Inhalt: Vorwort. - Einleitung. - Der Bau der Pflanzen. - Wurzel. - Sproßachse. - Blatt. - Anhangsgebilde an Sproßachsen und Blättern. - Oberfläche von Sproßachsen, Blättern, Blütenhüllen, Früchten und Samen. - Blütenstand. - Blüte. - Frucht. - Samen. - Besondere Bezeichnungen bei Gefäß-Sporenpflanzen. - Die Biologie der Pflanzen. - Lebensdauer. - Lebensformen. - Bestäubung. - Verbreitung der Samen; Früchte und Sporen. - Die Geographie der Pflanzen. - Übersicht über die wichtigsten Gruppen der Pflanzengesellschaften. - Ordnung und Benennung der Pflanzen. - Geschützte Pflanzen. - Anleitung zum Bestimmen. - Tabellen zum Bestimmen. - Tabelle zum Bestimmen der Hauptgruppen. - Tabelle I Pflanzen ohne Blüten (Sporenpflanzen). - Tabelle II Nacktsamige Pflanzen. - Tabelle III Einkeimblättrige Pflanzen. - Tabelle IV Zweikeimblättrige Pflanzen mit einfacher oder fehlender Blütenhülle. - Tabelle V Zweikeimblättrige Pflanzen mit freien Kronblättern. - Tabelle VI Zweikeimblättrige Pflanzen mit verwachsenen Kronblättern. - Tabelle VII Bäume und Sträucher. - Tabelle VIII Tauch- und Schwimmpflanzen. - Tabelle IX Pflanzen zur Blütezeit ohne grüne Blätter. - Abteilung Gefäß-Sporenpflanzen - Pteridophyta. - Abteilung Samenpflanzen - Spermatophyta. - Anhang. - Autorenverzeichnis. - Übersicht über das System. - Register der deutschen Pflanzennamen. - Register der wissenschaftlichen Pflanzennamen. - Erklärung der Abkürzungen auf den Vorsatzblättern.
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  • 13
    Call number: AWI G6-18-91535
    Type of Medium: Dissertations
    Pages: Getr. Zählung: Ill., graph. Darst.
    Language: German
    Note: Karlsruhe, Univ., Diss., 1981 , INHALT: Zusammenfassung. - 1. Einleitung. - 1.1 Stand der Carbonatitforschung: experimentelle Untersuchungen und Bildungshypothesen. - 1.2 Mikrothermische Untersuchungen an fluiden Einschlüssen in Carbonatitmineralen. - 1.3 Der Carbonatit des Kaiserstuhls. - 1.4 Problemstellung, Methodisches. - 2. Das Probenmaterial. - 2.1 Proherrnahme und Aufbereitung. - 2.2 Probenpräparation für die Einschlußuntersuchungen. - 2.3 Optische Untersuchung, Phänomenologie. - 2.31 Anordnung, Verwachsungen und Habitus der Apatite. - 2.32 Die Einschlüsse der Apatite. - 2.321 Cavitätenformen, Füllungen, Dimensionen. - 2.322 Kriterien für primäre Einschlußbildung und sekundäre Veränderungen. - 2.323 Unterschiedliche Einschlußführung in Apatiten und anderen Mineralen. - 3. Apparaturen. - 3.1 Die mikrothermische Apparatur. - 3.11 Konzeption und Ausführung des Beiz-Kühltisches. - 3.12 Eichung des Beiz-Kühltisches. - 3.13 Präzision und Probleme im Meßbetrieb. - 3.2 Kühlplatte. - 3.3 Quetschtisch. - 4. Zur Theorie der Einschlußuntersuchungen. - 4.1 Geometrische Berechnungen. - 4.11 Berechnung des Cavitätenvolumens. - 4.12 Fehlerdiskussion. - 4.13 Grenzen der optischen Auflösung. - 4.2 Zur Theorie der Phasenverhältnisse. - 4.21 Einschlußbildung und Phasentrennung. - 4.22 Phasenverhältnisse in Einkomponentensystemen, Homogenisierungskurven. - 4.23 Phasenverhältnisse in Wasser-Salz-Systemen: H2O-NaCl; H2O-NaCl-KCl. - 4.24 Phasenverhältnisse in Wasser-Gas-Systemen: CO2-H2O. - 5. Konstruktion der Phasendiagramme. - 5.1 H2O. - 5.2 CO2. - 5.3 H2O-NaCl. - 5.4 CO2-H2O. - 5.5 Wasser-Salzsysteme mit kritischen Endpunkten (PQ-Systeme). - 5.6 Wasser-Salzsysteme bei stark positivem Temperaturkoeffizient der Löslichkeit der Salzkomponente: H2O-KCl, H2O-NaCl-KCl. - 5.7 System CO2-H2O-NaCl. - 6. Untersuchungsergebnisse. - 6.1 Experimentelle Untersuchungen an einzelnen Einschlüssen: Mikrothermometrie und destruktive Methoden. - 6.11 Einphasige Einschlüsse mit Gasfüllung. - 6.12 Calcit als Einphaseneinschluß im Apatit. - 6.13 Zweiphaseneinschlüsse L+V. - 6.14 Dreiphaseneinschlüsse LH2O + LCO2 +V. - 6.15 Einschlüsse mit übersättigten Lösungen (Multiphaseneinschlüsse). - 6.16 Fluide Einschlüsse im Calcit des Carbonatits. - 6.2 Analytische Untersuchungen. - 6.21 Kationen und Anionen in wäßrigen Extrakten des Apatitmahlgutes. - 6.22 Bitumenphasen in organischen Solventextrakten. - 6.23 Gasanalytische Messungen. - 7. Genetische Interpretation der Einschlußresultate. - 7.1 Das Subsystem H2O-Salzphasen. - 7.11 H2O-NaCl. - 7.12 H2O-NaCl-Na2SO4/Na2CO3. - 7.13 H2O-NaCl-KCl. - 7.2 Druckmodelle im seichten, subvulkanischen Niveau. - 7.21 Hydrostatische Bedingungen. - 7.22 Lithostatische Bedingungen. - 7.3 Das Subsystem CO2-H2O 7.4 Kombination der Teilsysteme, das System CO2-H2O-NaCl bei volumenkontrollierten Bedingungen. - 7.5 Zusammenfassung und Vergleich mit den Resultaten aus anderen Carbonatitlokalitäten. - 8. Petrogenetische Schlußfolgerungen. - 8.1 Magmatische Carbonatitintrusion und autometasomatische Folgeprozesse. - 8.2 Hydrothermaltransport des Calcits. - 8.3 Überlegungen zur Herkunft der Salzphasen. - 8.4 Künftige, weiterführende Untersuchungen. - 8.5 Zusammenfassung. - 9.0 Anhang I Abbildungen. - 10.0 Anhang II Originalmeßwerte.
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  • 14
    Call number: M 18.91591
    Type of Medium: Monograph available for loan
    Pages: XII, 441 Seiten
    ISBN: 9604318527
    Language: English
    Branch Library: GFZ Library
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  • 15
    Call number: MOP 46237
    Type of Medium: Monograph available for loan
    Pages: 138 S. , Kt.
    Language: German
    Location: MOP - must be ordered
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  • 16
    Call number: AWI G6-18-91903
    Type of Medium: Series available for loan
    Pages: 93 Seiten , Illustrationen
    Series Statement: Schriftenreihe Anwendung von Isotopen und Kernstrahlungen in Wissenschaft und Technik 5
    Language: German
    Note: Inhaltsverzeichnis: 1. Einleitung. - 2. Grundlagen der 15N-Tracertechnik. - 3. Versuchsplanung und -auswertung. - 3.1. Begriffe und Symbole. - 3.2. Formeln und Definitionen für die Berechnung der in der 15N-Tracertechnik benötigten Größen. - 3.2.1. Relative 15N-Häufigkeit. - 3.2.2. Molmasse. - 3.2.3. Stickstoffgehalt. - 3.2.4. N-Masse. - 3.2.5. Stoffmenge. - 3.2.6. N-Menge. - 3.2.7. 15N- bzw. 14N-Menge. - 3.2.8. 15N-Masse. - 3.2.9. 15N-Exzeßmasse. - 3.2.10. Titrimetrische Neutralisationsanalysen. - 3.2.11. Spektren-Auswertung der 15N-Messung. - 3.3. Untersuchung statischer Eigenschaften biologischer Systeme (statische Isotopenverdünnungsanalyse). - 3.4. Untersuchung des dynamischen Verhaltens biologischer Systeme. - 3.4.1. Modellierung von Tracerprozessen. - 3.4.2. Theoretische Grundlagen der mathematischen Modellierung. - 3.4.3. Modell des Stickstoff-Stoffwechsels im Ackerboden. - 3.5. Berechnungsbeispiele zu den Abschnitten 3.2. bis 3.4. - 3.5.1. Isotopenstöchiometrie. - 3.5.2. Titrimetrische Analyse einer 15N-markierten Substanz. - 3.5.3. Isotopenverdünnungsanalyse. - 3.5.4. Tracerkinetik. - 3.6. Literatur. - 4. Methodik der Probenaufbereitung und Isotopenanalytik. - 4.1. Aufarbeitung des Probenmaterials. - 4.2. Chemische Aufbereitung. - 4.3. Probenchemie. - 4.3.1. Dumas-Methode. - 4.3.2. Hypobromit-Methode. - 4.3.3. Sonstige Methoden. - 4.4. Isotopenanalytik. - 4.4.1. Emissionsspektrometrische 15N-Analytik. - 4.4.1.1. Isotopenanalytik mit dem 15N-Analysator NOI-5. - 4.4.1.2. Isotopenanalytik mit dem automatischen 15N-Analysator ISONITROMAT 5200. - 4.4.2. Massenspektrometrische 15N-Isotopenanalyse. - 4.4.3. Methodenvergleich. - 4.5. Fehlerquellen in der 15N-Analytik. - 4.6. Weitere Analysenmethoden in der 15N-Tracertechnik. - 4.6.1. NMR-Spektroskopie. - 4.6.2. Kombinierte Gaschromatographie-Massenspektroskopie und Hochdruck-Flüssigkeitschromatographie-Massenspektroskopie. - 4.7. Literatur. - 5. 15N-Anwendung in der Biochemie. - 5.1. Die biologische Stickstoff-Fixierung. - 5.2. Pflanzenphysiologie. - 5.3. Tierphysiologie. - 5.4. Literatur. - 6. 15N-Anwendung in der landwirtschaftlichen Forschung. - 6.1. Allgemeines. - 6.2. Die Anwendung 15N-markierter Düngemittel zum Studium des N-Umsatzes im Boden. - 6.2.1. Stickstoff-Festlegung. - 6.2.1.1. Ammoniumfixierung und Sorption an organischen Bodenbestandteilen. - 6.2.1.2. Stickstoff-Festlegung in organischen N-Verbindungen. - 6.2.2. Verfügbarkeit und Mobilisierung von Stickstoff. - 6.2.3. Stickstoff-Transformation und Dynamik des Stickstoff-Umsatzes. - 6.2.3.1. Mineralisierung und Immobilisierung. - 6.2.3 .2. Humifizierung. - 6.2.3.3. Nitritzersetzung im Boden. - 6.2.4. Ausnutzung des Düngemittel-Stickstoffs und Stickstoff-Verluste (N-Bilanz). - 6.2.5. Migration von Düngemittel-Stickstoff im Boden. - 6.2.6. Nachwirkungseffekt. - 6.2.7. Forstwirtschaftliche Untersuchungen mit 15N. - 6.3. Die Anwendung 15N-markierter Düngemittel zum Studium des Stickstoff-Umsatzes in der Pflanze. - 6.3.1. Die Aufnahme des Stickstoffs und ihre Beeinflussung durch N-Form, Applikationsart, Pflanzenart, Ernährungszustand, Spurenelementversorgung, Temperatur und Zusammensetzung des Nährsubstrates (Stickstoff-Fixierung). - 6.3.2. Die Ausnutzung des Düngemittel-Stickstoffs durch die Pflanze. - 6.3.3. Verteilung des Dünge-Stickstoffs in der Pflanze. - 6.3.4. Stoffwechsel des gedüngten Stickstoffs. - 6.4. Die Untersuchung des Stickstoff-Umsatzes im Tier mittels 15N. - 6.4.1. Eiweißstoffwechsel. - 6.4.1.1. Proteinverdaulichkeit, Stickstoff-Verweilzeitstudien und Aminosäure-Resorptionskinetik. - 6.4.1.2. Biosynthese von Eiproteinen. - 6.4.1.3. Metabolismus von NPN-Verbindungen bei Wiederkäuern. - 6.5. Literatur. - 7. 15N-Anwendung in der medizinischen Forschung. - 7.1. Besonderheiten der Anwendung stabiler Isotope in der Humanmedizin. - 7.2. Biochemie des Intermediärstoffwechsels. - 7.2.1. Anatomische Lokalisation von Stoffwechselprozessen. - 7.2.2. Aufklärung von Stoffwechselwegen durch Erfassung der Stoffwechselzwischen- oder Endprodukte. - 7.2.3. Bestimmung der mittleren Verweilzeit bzw. Lebensdauer von Verbindungen. - 7.2.4. Bestimmung der Größe von Stoffwechsel-Pools. - 7.3. Gastroenterologie. - 7.4. Pädiatrie. - 7.5. Ernährung. - 7.6. Beiträge zur Diagnostik und Ursachenforschung von Krankheiten und zu pharmakologischen Fragestellungen. - 7.7. Literatur.
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  • 17
    Series available for loan
    Series available for loan
    Leipzig : Akademie der Wissenschaften der DDR, Zentralinstitut für Isotopen- und Strahlenforschung
    Associated volumes
    Call number: ZSP-980-90
    In: ZfI-Mitteilungen, Nr. 90
    Type of Medium: Series available for loan
    Pages: 358 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 90
    Language: German
    Note: Inhaltsverzeichnis: 1. Wissenschaftliche Beiträge. - (01) Isotopen- und elementgeochemische sowie radiogeochronologische Untersuchungen an der Zinnlagerstätte Ehrenfriedersdorf (Beste wissenschaftliche Arbeit des ZfI 1983 / Autorenkollektiv. - (02) Einsatz ionisationsgasanalytischer Methoden an der Mikroelektronik (Beste wissenschaftlich-technische Arbeit des ZfI 1983) / Autorenkollektiv. - (03) Zur Geschichte der künstlichen Radioaktivität / H. Koch. - (04) 50 Jahre künstliche Radioaktivität / G. Vormum. - (05) Frédéric und Irène Joliot-Curie - Biographische Skizze / K.-P- Dostal. - 2. Institutskolloquien. - 3. Patente. - 4. Veröffentlichungen und Vorträge. - 5. Register. - 5.1. Namensregister. - 5.2. Deskriptorenregister. - 6. Verzeichnis aller bisher erschienenen Hefte der ZfI-Mitteilungen. - 6.1. Titel der bis 1982 erschienenen Hefte 1-61 und Sonder-Nr. 1. - 6.2. Inhaltsverzeichnisse der im Jahre 1983 erschienenen Hefte 62-82. - 6.3. 1984 bisher erschienene Hefte. - 7. Verzeichnis aller bisher erschienenen Preprints.
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  • 18
    Monograph available for loan
    Monograph available for loan
    Braunschweig : Vieweg
    Call number: IASS 18.91911
    Type of Medium: Monograph available for loan
    Pages: 241 S. , graph. Darst. , 23 cm
    ISBN: 3528073039 (gbd.) , 3528073144 (kart.) , 9783528073145
    Series Statement: Wissenschaftstheorie, Wissenschaft und Philosophie 4
    Uniform Title: Sémantique structurale 〈dt.〉
    Language: German
    Branch Library: IASS
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  • 19
    Call number: MOP Per 116(129)
    In: Prace geograficzne Instytut Geografii Uniwersytetu Jagiello´nskiego
    Type of Medium: Series available for loan
    Pages: 109 Seiten , Illustrationen, graphische Darstellungen, Karten
    Series Statement: Prace Geograficzne 129
    Language: Polish
    Note: Mit Zusammenfassung in englischer und russischer und Bildunterschrift in englischer Sprache.
    Location: MOP - must be ordered
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  • 20
    Monograph available for loan
    Monograph available for loan
    Bonn : Federal Republic of Germany, Press and Public Relations Department
    Call number: AWI P6-18-91970
    Type of Medium: Monograph available for loan
    Pages: iv, 169 Seiten
    Language: English
    Note: CONTENTS: Introduction. - International co-operation. - Intergovernmental co-operation. - Non-governmental co-operation. - I. Scientific Programme. - 1. Astronomy. - 2. Biological Sciences. - 2.1 The marine ecosystem and its living resources. - 2.1.1 Food resources, phytoplankton production and zooplankton. - 2.1.2 The role of the benthos. - 2.1.3 The role of micro-organisms. - 2.1.4 Distribution and incidence of seals in the pack-ice of the Weddell Sea. - 2.1.5 Distribution and life history of fishes. - 2.1.6 Large-scaie distribution and drift of krill. - 2.1.7 Composition and behaviour of krill shoals. - 2.1.8 Preservation and processing of krill. - 2.2 The adaptation of antarctic marine organisms to their environment. - 2.2.1 Experiments and marine studies on .the ecophysiology of krill. - 2.2.2 Temperature regulation and food requirements of warm-blooded antarctic animals. - 2.2.3 Growth, digestive system and food economy of antarctic fishes. - 2.2.4 Freezing resistance of sea animals. - 2.2.5 Taxonomy of antarctic marine organisms. - 2.3 Terrestrial biology in Antarctica. - 2.3.1 Temperature adjustments in the reproductive biology of antarctic birds. - 2.3.2 Biochemical bases of growth processes in poikilothermic organisms at very low temperatures. - 2.3.3 Nutritional biology of poikilothermic herbivora. - 2.3.4 Study of lichens, fungi and bacteria in Antarctica and on offshore islands. - 2.3.5 Photosynthesis and heterotrophic life cycle of plants at very low temperatures. - 2.4 Environmental protection in Antarctica. - 2.5 Human biology and medicine in polar regions. - 3. Geodesy, Cartography and Remote Sensing. - 3.1 Satellite geodesy. - 3.2 Doppler satellite positioning. - 3.3 Geodetic mapping of ice-free areas. - 3.4 Remote-sensing by satellite. - 4. Geology and Geophysics. - 4.1 Study of drift processes as a contribution to the geological history of Antarctica. - 4.1.1 Study of magnetic structures by means of aeromagnetic photography. - 4.1.2 Paleomagnetic studies of drift evolution. - 4.1.3 Micro-earthquakes as indicators of tectonic activity. - 4.1.4 Earth tides and natural oscillations of the earth. - 4.2 Studies of the structure of crust and mantle. - 4.2.1 Structure of the basement complex of the transantarctic mountain chain in the area east of the Filchner Ice Shelf. - 4.2.2 Structure of the basement of the Weddell Sea, the Filchner/Ronne Ice Shelf, and the peripheral area. - 4.2.3 Oldest and highly metamorphous rocks of the East Antarctic. - 4.3 Stratigraphy, tectonics and magmatism in the mobile areas. - 4.3.1 Mobile fringe areas of the East Antarctic. - 4.3.2 Paleozoic and mesozoic mountains(Beacon upper group) in the transantarctic mountains. - 4.3.3 Early paleozoic to cainozoic orogenes in the area around the Filchner/Ronne Ice Shelf. - 4.4 Study of exogenous processes under extremely cold conditions. - 4.4.1 Glacial geology and geomorphology. - 4.4.2 Weathering and detrital formation. - 4.5 Geoscientific marine research. - 5. Glaciology. - 5.1 Volume and dynamics of the Filchner/Ronne Ice Shelf. - 5.2 Determining the extent and thickness of the ice and its temporal variation in the Filchner/Ronne Ice Shelf sector and peripheral areas. - 5.3 Determining the composition and inner structure of the Filchner/Ronne Ice Shelf on the basis of geophysical surface measurements. - 5.4 Studies of the dynamics of the pack-ice in the Weddell Gyre. - 5.5 Physical characteristics of ocean ice. - 5.6 Glaciological drillings. - 5.7 Chemical composition and accumulation genesis of antarctic background aerosol; global transport of trace gases and aerosols. - 5.8 Study of the elastic and rheological characteristics of ice, its heat conductability and texture affected by deformation. - 6. Upper Atmosphere and Extraterrestrial Physics. - 6.1 Investigation of whistlers and VLF radio emissions (chorus, hiss, etc) at conjugated points. - 6.2 Study of terresterial magnetic pulsations at conjugated points. - 6.3 Study of atmospherics to obtain more precise data on worldwide thunderstorms. - 6.4 Measurements of the aero-electric field. - 6.5 Balloon-based study of the ionosphere in the light of Mg t resonance lines. - 6.6 Measurement of the vertical distribution of ozone, steam and aerosol up to an altitude of 30 km. - 6.7 Measurements of emission in the infrared 9.6 µ ozone band from the ground. - 6.8 Other projects which may be carried out simultaneously with the above or later. - 6.9 Proposed basic terrestrial magnetic equipment for the Antarctic Station. - 6.10 Meteorite search expedition. - 6.11 Study of micrometeorites and cosmic dust. - 7. Meteorology and Oceanography. - 7.1 Meteorology. - 7.1.1 Atmospheric boundary stratum. - 7.1.2 Study of stratospheric circulation. - 7.1.3 Measurement of trace gases over long periods. - 7.1.4 Other research projects. - 7.1.5 Weather service observations and consultations. - 7.1.6 Basic meteorological equipment for the Antarctic Station. - 7.2 Physical oceanography. - 7.2.1 Formation and extent of bottom water in the Atlantic sector of the circumantarctic ocean. - 7.2.2 Numeric simulation of the vertical flows of material, energy and impulses. - 7 2.3 Time scales of transportation in deep water with the aid of radioactive trace elements. - 7.2.4 Detection of heavy metals in the Antarctic Ocean. - 7.2.5 Fishery oceanography in circumantarctic waters. - 7.2.6 Other research projects. - 8. Engineering Sciences. - 8.1 Shipbuilding technology. - 8.1.1 Measuring and testing programme regarding the performance of vessels in ice and technical developments in the construction of ice-going vessels. - 8.2 Iceberg location and navigation. - 8.2.1 Iceberg location. - 8.2.2 Development of precision positioning systems (also for dynamic positioning) to ensure noninterference with signals transmitted through ice and water masses of different thicknesses. - 8.3 Construction techniques. - 8.4 Exploration techniques. - 8.5 Other topics. - The Antarctic Research Station. - The Polar Research and Supply Ship. - The Polar Research Institute. - Institutions contributing to the Programme.
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  • 21
    Call number: AWI G7-19-92029
    Type of Medium: Monograph available for loan
    Pages: 37 ungezählte Blätter
    Language: English
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  • 22
    Monograph available for loan
    Monograph available for loan
    Sosnowiec : Uniwersytet Śląski, Instytut Geografii
    Call number: AWI P9-83-1079
    Type of Medium: Monograph available for loan
    Pages: 248 Seiten , Illustrationen, Karten
    Language: Polish
    Note: Contents: A snow cover in the region of Fiord Hornsund on Spitsbergen / J. Pereyma. - Temperature rations in summer on the Waldemar Glacier and on the Waldemar sea lowland / G. Wójcik, K. Marciniak, R. Przybylak. - Precipitation and evaporation in Werenskiold Glacier district / A. Szczepankiewicz-Szmyrka. - Biometeorological conditions on the Werenskiold Glacier forefield in summer of 1980 / A. Szczepankiewicz-Szmyrka. - Some notes on wind directions in the West Spitsbergen in 1980 / K. Gerstmann. - Radar measurements of the thickness of the Werenskiold Glacier / R. Czajkowski - The analysis of movements of the Werenskiold Glacier based on dating of fossil moss / H. Chmal - Increase in the mass of the firn snow in the glacial amphiteatre of the Penck Glacier in the period 1934 to 1958 / C. Lipert - Some automatic systems to collect and transmission stored data using various radio-links / J. Molski. - Würm and Holocene glaciations of North-Western Sörkappland exemplified by the Slakli Valley, Spitsbergen / P. Kłysz, L. Lindner. - The marine origin of Lisbetdalen mezorelief SW Spitsbergen / W. Stankowski - Raised marine terraces of Kulmstranda North-Western Sörkappland / P. Kłysz, L. Lindner - The geomorphological sketch map of the Gåsdalen region, South Spitsbergen / J. Jania, Z. Lentowicz, T. Szczypek, J. Wach. - Last deglaciation of Treskelen Peninsula, Hornsund, Svalbard / L. Marks. - The recession of Vitkovski Glacier as recorded in its marginal zone / L. Andrzejewski, w. Stankowski. - Degradation processes on the end moraine of the Werenskiold Glacier / J. Cegła, J. Kida. - Studies of the dessication crack on the forefield of the Werenskiold Glacier / J. Cegła. - The beginning and evolution of the marginal outwash on the forefield of the Eliza Glacier / A. Olazewski. K. Sendobry. - Summer thawing of the ground in the Kaffiöyra, SW Spitsbergen / K. Marciniak, W. Szczepanik, R. Przybylak - Morphology and sedimentary environments of the Baszkara ·and Dzankuat Glaciers in the High Kaukas / A. Karczewski, A. Kostrzewski,P. W. Kowalew. - Stratigraphic position and remarks on sedimentation of the Brentskardhaugen Bed, Spitsbergen / A. Wierzbowski, G. Biernat, C. Kulicki. - Some remarks concerning the structure of groups of the bottom fauna of the Admiralty Bay - King George Island, South Shetland / P. Presler, K. Jażdżewski·, W. Jurasz, W. Kittel, J. Siciński. - Biological indexes of the hydrological conditions - observations from Hornsund region, Spitsbergen / J. M. Węsławski. - The habitability of the littoraly rocks in region Steinvika and Hyttevika Bays, Vestspitsbergen / O. Różycki, M. Gruszczynski. - Some aspects of the acoustical estimation of the krill abundance / M. Brzozowska. - Liberation of carbon dioxide from tundra soils / H. Dziadowiec. - Exploration in the Hornsundfiord region / J. Szupryczyński. - , In polnischer Sprache
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  • 23
    Monograph available for loan
    Monograph available for loan
    Berlin : Zentralinstitut für Physik der Erde
    Call number: AWI G2-19-92036
    Type of Medium: Monograph available for loan
    Pages: 78 Seiten , Illustrationen
    Language: German
    Note: Inhaltsverzeichnis: 1. Vorwort. - 2. Struktur und Entwicklung der Antarktischen Platte. - 2.1. Generelle Kennzeichnung der Antarktischen Platte. - 2.2. Tripelpunkte. - 2.2.1. Bouvet-Tripelpunkt. - 2.2.2. Indik-Tripelpunkt. - 2.2.3. Macquarie-Tripelpunkt. - 2.2.4. Osterinsel-Tripelpunkt. - 2.3. Plattengrenzen und Plattenfelder. - 2.3.1. Bouvet-Indik-Feld. - 2.3.1.1. Ausbildung der Plattengrenze. - 2.3.1.2. Anomale Entwicklung südlich der Agulhas-Bruchzone. - 2.3.1.3. Inseln und submarine Plateaus im südlichen Indik. - 2.3.2. Indik-Macquarie-Feld. - 2.3.3. Macquarie-Osterinsel-Feld. - 2.3.3.1. Ausbildung der Plattengrenze. - 2.3.3.2. Sandwich- und Scotia-Platte. - 2.3.4.3. Beziehungen zwischen Südamerika und Antarktika und das Problem der Antarktischen Halbinsel. - 2.3.4.4. Weddellbecken. - 2.3.4.5. "Drake-Platte". - 2.3.4.6. Plattentektonische Entwicklung des Südostpazifiks. - 2.4. Überblick über den Werdegang der südhemisphärischen Ozeangebiete und den Ablauf des Gondwanazerfalls. - 3. Zur Bedeutung der Krustenentwicklung für Paläoozeanlogie und Paläoklimatologie. - 3.1. Einige Kennzeichen der ozeanologischen Situation in den antarktischen Meeresgebieten. - 3.2. Kriterien für Veränderungen der paläoozeanologischen und paläoklimatologischen Verhältnisse im Hinblick auf die paläotektonische Interpretation. - 3.3. Abriß der paläoozeanologisch-paläoklimatologischen Entwicklung im Känozoikum und mögliche Zusammenhänge mit dem tektonischen Geschehen. - 4. Zusammenfassung. - 5. Literaturverzeichnis. - 6. Abbildungsverzeichnis. -
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  • 24
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: IASS 19.92037
    Type of Medium: Monograph available for loan
    Pages: XVI, 343 Seiten , 23cm
    ISBN: 0521816467 , 0521016711 (pbk.)
    Language: English
    Branch Library: IASS
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  • 25
    Call number: D 2044/4
    In: Forschungsaufgabe "Strukturentwicklung Mitteldeutsche Hauptabbrüche und Südrand NPS"
    Type of Medium: Monograph non-lending collection
    Pages: 19 Blätter , graphische Darstellungen
    Language: German
    Note: Inhaltsverzeichnis: 1. Grundlagen, einschl. Zielstellung. - 2. Geologisch-tektonischer Überblick. - 3. Ergebnisse. - 3.1 Harzaufrichtungszone. - 3.2 Huy. - 3.3 Hakel. - 3.4 Ascherslebener Sattel. - 3.5 Straßfurter Sattel. - 3.6 Weferlinger Triasplatte und Allertal-Störungszone. - 3.7 Östliches Subherzynes Becken. - 4. Vergleich der einzelnen Untersuchungsgebiete. - 5. Zusammenfassung und Schlußfolgerungen. - 6. Literatur. - Kurze Stellungnahme Bereichsleitung ZIPE III (Geologie).
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  • 26
    Monograph available for loan
    Monograph available for loan
    Copenhagen : [s.n.]
    Call number: AWI G7-19-92045
    Type of Medium: Monograph available for loan
    Pages: 137 Seiten , Illustrationen
    Language: English
    Note: Contents: Report on the 2001 activities of NGRIP Operations. - Objective. - Kangerlussuaq (Søndre Strømfjord). - Preparation of the field season. - Drilling equipment. - Start of the field season. - Starting the camp. - Communication. - Bailing. - Drilling. - Logging. - Last Drilling. - Summaries. - DML electronics. - Garbage handling. - Medivac. - Acknowledgement. - Graphs. - NGRIP 2001 sub programs. - Automatic weather stations. - Dust program. - GPS measurements. - Firn gas sampling. - 2001 Field season, Diary. - Communication. - Maintenance/Logistics after the season. - Bulk supplies. - List of participants. - Table of LC130 flights. - NGRIP documentation. - NGRIP camp load. - Sitreps. - Daily reports from NGRIP. - Special reports. - Schedule for camp close down. - List of NGRIP addresses.
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  • 27
    Call number: ZSP-SCAR-570-6
    In: Antarctic Research Report to SCAR, No. 6
    Type of Medium: Series available for loan
    Pages: 38 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 6
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 83-October 84. - II. Planned Activities, October 84-October 85. - References.
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  • 28
    Call number: ZSP-SCAR-570-5
    In: National Antarctic Research Report to SCAR, No. 5
    Type of Medium: Series available for loan
    Pages: 35 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 5
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 82-October 83. - II. Planned Activities, October 83-October 84. - References.
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  • 29
    Call number: ZSP-SCAR-570-4
    In: National Antarctic Research Report to SCAR, No. 4
    Type of Medium: Series available for loan
    Pages: 24 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 4
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 81-October 82. - II. Planned Activities, October 82-October 83. - References.
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  • 30
    Call number: ZSP-SCAR-570-3
    In: National Antarctic Research Report to SCAR, No. 3
    Type of Medium: Series available for loan
    Pages: 16 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 3
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 80-October 81. - II. Planned Activities, October 81-October 82. - References.
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  • 31
    Call number: ZSP-SCAR-570-2
    In: Report to SCAR on Antarctic research activities of Germany (FRG), 2
    Type of Medium: Series available for loan
    Pages: 16 Seiten
    ISSN: 0179-0072
    Series Statement: Report to SCAR on Antarctic research activities of Germany (FRG) 2
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research of the Federal Republic of Germany. - Introduction. - Station. - Antarctic Research Activities 1979-1980. - Planned Research Activities 1980-1981. - References.
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  • 32
    Call number: AWI G7-18-91974
    Type of Medium: Monograph available for loan
    Pages: 38 Seiten , 1 Beilage
    Language: English
    Note: Contents: Preface. - Abstracts (in the alphabetic order). - The natural environment and cryosphere of the Tatra Mountains by Bogdan Gądek. - IASC Working Group on Arctic Glaciology. - General programme.
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  • 33
    Series available for loan
    Series available for loan
    Washington : National Academy of Sciences
    Call number: AWI G7-18-91940
    Type of Medium: Series available for loan
    Pages: x, 66 Seiten , 23 cm
    Language: English
    Note: Contents: 1. PRIMARY OBJECTIVES. - 2. DYNAMICS OF THE ICE: FIELD STUDIES. - Major Regional Studies. - In Progress. - Newly Proposed. - Continentwide Measurements. - Surface and Bed Topography. - Mass Balance. - Complementary Field Studies. - Glacier and Local Ice-Cap Studies. - Related Studies outside Antarctica. - Development of New Observational Techniques and Instrumentation. - 3. ANALYSIS AND INTERPRETATION OF FIELD DATA. - Description of the Dynamic State of the Ice Sheet. - Physical Properties of the Ice. - Sea-Ice Modeling. - 4. GLACIAL HISTORY. - Glacial Geology. - Core Studies. - Numerical Modeling. - 5. ENVIRONMENTAL INTERACTION. - Meteorology. - Oceanography. - Geology and Geophysics. - Biology. - Application of New Techniques. - Satellites and Systems. - Automatic stations. - Oceanographic Instruments. - Global Numerical Modeling. - REFERENCES AND BIBLIOGRAPHY. - APPENDIX A. International Antarctic Glaciological Project. - APPENDIX B. The International Antarctic Glaciological Project Standardization Document. - APPENDIX C. Abstracts of Projects Considered by the Glaciology Panel during the Antarctic Planning Exercise, November 11-13, 1971. - Core Drilling and Analysis. - Ice-Thickness Mapping. - Ross Ice Shelf Project (RISP). - Glacial and Periglacial Studies. - Sea Ice. - Ice Streamline Cooperative Antarctic Project (ISCAP). - Sub-Ice-Surface Remote Sensing. - Alpine Outlet Glaciers. - Roosevelt Island. - APPENDIX D. Antarctic Sea Ice Programm. - Differences between the Arctic and Antarctic Ice Packs. - Importance of the Antarctic Pack. - Proposed programs. - Satellite Programs. - Airborne Remote Sensing. - Unmanned Drifting Stations. - Manned Drifting Stations. - Coastal Stations. - Timing. - Conclusion. - Bibliography. - APPENDIX E. Abbreviations and Terms Used in this Report.
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  • 34
    Monograph available for loan
    Monograph available for loan
    Moskva : Institut Geografii RAN
    Call number: AWI G6-18-92021
    Type of Medium: Monograph available for loan
    Pages: 167 Seiten , Illustrationen
    ISBN: 5-89658-024-X
    Language: Russian , English
    Note: Contents: Introduction / V. I. Nikolaev. - Oxygen isotope composition of the bone phosphate of reindeer: potential as a palaeoenvironmental recorder / Vladimir Nikolaev, Silvana Davanzo, Antonio Longinelli, Paola Iacumin. - Carbon isotope studies of mammoth's food and fossil remains / Vladimir Nikolaev, Silvana Davanzo, Ludmila Kuznetsova, Paola Iacumin. - A fresh approach to palaeogeography of northern regions of West Siberia in sartan time (Late Pleistocene) / Dimitri Bolshiyanov, Vladimir Nikolaev, Alexander Sosnovskiy. - Relief and sediments forming of the Eastern Khibiny Mountains in the end of Late Pleistocene and Holocene / F. A. Romanenko, A. A. Lukashov, E. D. Sheremetskaya, Yu. R. Belyaev, N. E. Zaretskaya, D. K. Kuznetsov, O. S. Olyunina, A. M. Tarbeeva. , In kyrillischer Schrift
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  • 35
    Journal available for loan
    Journal available for loan
    Oakland, California : EERI Earthquake Engineering Research Institute
    Call number: Z 91.0813
    Description / Table of Contents: On June 23, 2001, the region of southern Peru and northern Chile was shaken by a Mw 8.4 earthquake, arguably the largest worldwide since 1965. Approximately 80 people were killed and 70 missing and presumed dead. In all, the earthquake affected more than 200,000 people. It was the result of thrust faulting on the boundary between the Nazca and South American plates. Structural damage was concentrated on adobe houses and historical constructions, but a significant number of engineered structures were damaged, mostly attributable to short–column effects. There was widespread damage to the highway system, and a destructive tsunami caused significant damage. This issue is a product of the combined efforts of several reconnaissance teams. Other topics covered include seismicity, ground motion and site response, ground failure, geotechnical effects; lifelines, and societal impacts.
    Type of Medium: Journal available for loan
    Pages: XIV, 165 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 0943198062
    Series Statement: Earthquake spectra Vol. 19, Suppl. A
    Language: English
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  • 36
    Journal available for loan
    Journal available for loan
    Oakland, California : EERI Earthquake Engineering Research Institute
    Call number: Z 91.0813
    Description / Table of Contents: This 7.7 magnitude earthquake occurred in the state of Gujarat in western India. Approximately 14,000 lives were lost and over 167,000 persons injured. Damage was spread over a radius of 400 kilometers from the epicenter. The first major quake to hit an urban area of India in the last 50 years, it caused extensive liquefaction and slope failures but no primary surface fault rupture. The resulting net economic loss is estimated to be about US $5 billion. This volume is a joint report from the combined EERI-NSF team. It covers the seismotectonic setting; local geological and geotechnical effects; performance of buildings, lifelines, and other structures and facilities; and social and governmental response.
    Type of Medium: Journal available for loan
    Pages: XV, 398 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 0943198119
    Series Statement: Earthquake spectra Vol. 18, Suppl. A
    Language: English
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  • 37
    Call number: AWI E3-19-92148
    Description / Table of Contents: In this publication for the first time the scientific activities of the Russian researchers of Antarctica are reviewed and summarized, from the very first landing to the ice continent until the present time (1956-2004). Dozens of monographs and hundreds of articles regarding the climate of Antarctica, its geology, geophysics, biology, oceanology, glaciology, medicine, etc. disciplines are used and generalized. For use by the specialists working in the field of earth sciences and by the readers interested in polar research.
    Type of Medium: Monograph available for loan
    Pages: 303 Seiten , Illustrationen
    ISBN: 5-9584-0108-4
    Language: Russian , English
    Note: CONTENTS: From the author. - Foreword (V. M. Kotlyakov, the academician of Russian Academy of Science). - Introduction. - 1. A legal status of research in Antarctic. - 2. The Russian (Soviet) Antarctic expeditions. - 3. The first stage of the Russian Antarctic research (1956-1965). - 3.1. General characteristic of the first stage. - 3.2. Types of observations and research at the first stage of Soviet Antarctic expedition (SAE). - 3.3. Main scientific results of the first stage of SAE operation. - 4. The second stage of the Russian Antarctic Research (1966-1973). - 4.1. General characteristic of the second stage of SAE operation. - 4.2. Types of observations and research at the second stage of SAE operation. - 4.3. Main scientific results of the second stage of SAE operation. - 5. The third stage of the Russian Antarctic Research (1974-1990). - 5.1. General characteristic of the third stage of SAE operation. - 5.2. Types of observations and research at the third stage of SAE operation. - 5.3. Main basic scientific results ofthe third stage of SAE operation. - 6. The fourth stage of the Russian Antarctic Research (1991-2005). - 6.1. General characteristic of the fourth stage of Russian Antarctic expedition (RAE) operation. - 6.2. Types of observations and research at the fourth stage of RAE operation. - 6.3. Main scientific results of the fourth stage of RAE operation. - Conclusion. - References. - Appendices (1-8): Appendix 1. Chronology of RAE (SAE) operation. - Appendix 2. Number of native publications on various disciplines. - Appendix 3. Members of the Russian Antarctic expeditions. - Appendix 4. Number of RAE (SAE) wintering stations. - Appendix 5. Number of vessels operated in RAE (SAE). - Appendix 6. Volume of the cargo delivered by RAE (SAE) vessels. - Appendix 7. Wintering RAE (SAE) members. - Appendix 8. Photo portraits of the Russian Antarctic researchers. , In kyrillischer Schrift , Zusammenfassung in englischer Sprache
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  • 38
    Call number: AWI A13-19-92152
    In: HIRLAM technical report, No. 60
    Type of Medium: Series available for loan
    Pages: 69 Seiten , Illustrationen
    Series Statement: HIRLAM technical report 60
    Language: English
    Note: Contents: 1 Background. - 2 Processing overview. - 2.1 AAPP. - 2.2 BUFR and CMA. - 2.3 Cloud mask and thinning in HIRLAM 3D-VAR. - 2.4 Radiative transfer calculations. - 2.5 Data selection. - 3 Bias correction and error statistics. - 3.1 The need for bias correction. - 3.2 Bias correction method. - 3.3 Background errors in observation space. - 3.4 Estimation of observation error covariance statistics. - 3.4.1 Rotated channels. - 3.4.2 Estimation from analysis departures (DNMI). - 3.4.3 Non-diagonal cost contributions. - 3.4.4 Approach using comparison with background error (SMHI). - 4 Impact studies. - 4.1 Overview. - 4.2 The May 2001 impact study at DNMI. - 4.3 December 1999 SMHI experiment. - 4.3.1 Data coverage and model area. - 4.3.2 Verification. - 4.3.3 Results. - 4.3.4 The "French storm". - 4.4 December 2001 NOAA 16 impact study at DMI. - 4.5 January 2002 NOAA 16 impact study at DMI. - 5 Ongoing and future work. - 5.1 Overview. - 5.2 Use of observations over ice. - 5.3 Moisture channels. - 5.4 Future sensors. - 6 Conclusions and outlook for the future. - Acknowledgment. - References.
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  • 39
    Series available for loan
    Series available for loan
    Norrköping : HIRLAM-6 Project, SMHI
    Associated volumes
    Call number: AWI A13-19-92154
    In: HIRLAM newsletter, No. 43
    Type of Medium: Series available for loan
    Pages: 207 Seiten , Illustrationen
    Series Statement: HIRLAM newsletter 43
    Language: English
    Note: CONTENTS: Introduction and general report from All Staff Meeting 2003 / Per Undén. - Operational HIRLAM at DMI - Status and plans for 2003 / Kristian Mogensen. - The operational HIRLAM at the Finnish Meteorological Institute / Kalle Eerola. - Operational NWP suites at Meteo-France / Dominique Giard. - HIRLAM operational activities in Met Éireann / Ray McGrath. - Operational HIRLAM at met.no / Ole Vignes. - HIRLAM at INM. News and plans / Jose Antonio Garcia-Moya. - SMHI operational HIRLAM system / Lars Meuller. - Modelisation of background error statistics in ALADIN and ARPEGE / Dominique Giard and Loïk Berre. - Optimum interpolation analysis method for snow depth / Alberto Cansado and Beatriz Navascués. - Radiation in high-resolution mesoscale models - what can be done? / Hannu Savijärvi. - Testing the modified HIRLAM radiation scheme / Laura Rontu and Simo Järvenoja. - Enhanced formulation of convective cloud cover / Bent Hansen Sass. - Ideas about the water vapour saturation pressure / Carl Fortelius. - Recent physics modifications and results with KFB / Eric Bazile et al. - Comparison of two algorithms to simulate the effect of soil moisture freezing and thawing on the energy balance / J.A. Parodi, Ernesto Rodriguez and Beatriz Navascués. - Characteristics of CBR and STRACO versions / Sander Tijm. - Representing subgrid scale mixing under stable conditions: Importance for overall model synoptic development / Colin Jones, Geert Lenderink and Karl-Ivar Ivarsson. - Sensitivity and robustness of transparent boundary conditions / Aidan McDonald. - Re-arranging the HIRLAM boundary relaxation treatment / Aidan McDonald. - Testing of the MC2 boundary treatment in HIRLAM / Simo Järvenoja. - Experiences from pre-operational HIRLAM 5.1.4 tests at FMI / Simo Järvenoja. - A recent study on the initialization procedure in HIRLAM / Xiaohua Yang and Xiang-Yu Huang. - MLAM- MARS HIRLAM / Simo Järvenoja. - Forecasting snow with HIRLAM 5.2 / Viel Ødegaard. - The flood of Feb 1, 1953 and HIRLAM / Toon Moene. - HIRLAM verification scores, 1st quarter 2003 / Per Undén. - Reference system status / Gerard Cats.
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  • 40
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/40
    In: CRREL Report, 82-40
    Description / Table of Contents: The use of explosives to break floating ice sheets is described, and test data are used to develop design curves that predict explosives effects as ice thickness, charge size, and charge depth vary. Application of the curves to practical problems is illustrated by numerical examples. The general features of underwater explosions are reviewed and related to ice blasting. Quasi-static plate theory is considered, and is judged to be inapplicable to explosive cratering of ice plates. The specific energy for optimized ice blasting is found to compare quite favorably with the specific energy of icebreaking ships. All available field data for ice blasting are tabulated in appendices, together with details of the re­gression analyses from which the design curves are generated.
    Type of Medium: Series available for loan
    Pages: iv, 68 Seiten , Illustrationen
    Series Statement: CRREL Report 82-40
    Language: English
    Note: CONTENTS Abstract Preface Introduction General behavior of underwater explosions Regression analysis for ice-blasting data General features of the regression curves Use of the regression curves as design curves for ice blasting Row charges and pattern charges Response of floating ice sheets to underwater explosions Specific energy and “powder factor” Summary and conclusions Literature cited Appendix A: Basic data on ice blasting Appendix B: Scaled input data Appendix C: Initial regression analysis using complete polynomial Appendix D: Regression analysis with two coefficients of the original poly­nomial deleted
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  • 41
    Call number: ZSP-201-83/21
    In: CRREL Report, 83-21
    Description / Table of Contents: The probability density function of the gouge depths into the sediment is represented by a simple negative exponential over four decades of gouge frequency. The exceedance probability function is, therefore, e to the -lambda d, where d is the gouge depth in meters and lambda is a constant. The value of lambda shows a general decrease with increasing water depth, from 9/m in shallow water to less than 3/m in water 30 to 35 m deep. The deepest gouge observed was 3.6 m, from a sample of 20,354 gouges that have depths greater than or equal to 0.2 m. The dominant gouge orientations are usually unimodal and reasonably clustered, with the most frequent alignments roughly parallel to the general trend to the coastline. The value of N(bar) sub 1, the mean number of gouges (deeper than 0.2 m) per kilometer measured normal to the trend of the gouges, varies from 0.2 for protected lagoons to 80 in water between 20 and 38 m deep in unprotected offshore regions. The distribution of the spacings between gouges as measured along a sampling track is a negative exponential. The form of the frequency distribution of N sub 1 varies with water depth and is exponential for lagoons and shallow offshore areas, previously skewed for 10 to 20 m depths off the barrier islands, and near-normal for deeper water. As a Poisson distribution gives a reasonable fit to the N sub 1 distributions for all water depths, it is suggested that gouging can be taken as approximating a Poisson process in both space and time. The distributions of the largest values per kilometer of gouge depths, gouge widths, and the heights of the lateral embankment of sediments plowed from the gouges are also investigated.
    Type of Medium: Series available for loan
    Pages: 40 Seiten , Illustrationen, 1 Karte
    Series Statement: CRREL Report 83-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background and environmental setting Data collection and terminology Data analysis Gouge depths Gouge orientation Gouge frequency Extreme value analysis Applications to offshore design Gouge depth Extreme value statistics Burial depths Conclusion Literature cited Appendix A: Detailed bathymetric map of the Alaskan portion of the Beaufort Sea
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  • 42
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/18
    In: CRREL Report, 83-18
    Description / Table of Contents: An evaluation of an impulse radar system for detecting cavities under concrete pavement is discussed, and field results are presented. It was found that a dual antenna mode of surveying was ideal for void detection. In this mode one antenna operated in a transceive mode and a second, offset from the first, operated in a receive-only mode. This arrangement allowed a refraction-type profile survey to be performed, which enabled subpavement voids to be easily detected. Field trails were held at Plattsburgh Air Force Base, where 28 cavities were detected and mapped. Drilling of holes verified that a cavity existed and allowed cavity depth to be measured. The cavities varied from 1.5 in. to 23 in, depth and were up to 20 ft. long.
    Type of Medium: Series available for loan
    Pages: 49 Seiten , Illustrationen
    Series Statement: CRREL Report 83-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Plattsburgh Air Force Base Radar sounding system Survey procedure Cavity inspection Radar cavity detection test Radar profile results Falling-weight deflectometer tests Discussion and conclusions Literature cited
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  • 43
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. : MIT Press
    Call number: PIK V 102-19-92226
    Type of Medium: Monograph available for loan
    Pages: viii, 477 Seiten , Illustrationen, Diagramme , 23 cm
    Edition: Third edition
    ISBN: 0262232375 (alk. paper) , 9780262232371 (alk. paper) , 0262731541 (pbk.) , 9780262731546 (pbk.)
    Language: English
    Location: A 18 - must be ordered
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  • 44
    Call number: ZSP-201-83/24
    In: CRREL Report, 83-24
    Description / Table of Contents: Secondary recovery of oil at Prudhoe Bay, Alaska, will involve transporting large quantities of seawater in elevated pipelines across tundra for injection into oil-bearing rock strata. The possibility of a pipeline rupture raises questions concerning the effects of seawater on tundra vegetation and soils. To evaluate the relative sensitivities of different plant communities to seawater, eight sites representing the range of vegetation types along the pipeline route were treated with single, saturating applications of seawater during the summer of 1980. Within a month of the treatment 30 of 37 taxa of shrubs and forbs in the experimental plots developed clear symptoms of stress, while none of the 14 graminoid taxa showed apparent adverse affects. Live vascular plant cover was thus reduced by 89 and 91% in the two dry sites and by 54, 74 and 83% in the three moist sites, respectively. Live(green) bryophyte cover was markedly reduced in the moist experimental sites in 1981. Bryophytes in all but one of the wet-site experimental plots were apparently unaffected by the seawater treatment. Two species of foliose lichens treated with seawater showed marked deterioration in 1981. All other lichen taxa were apparently unaffected by the seawater treatment. The absorption and retention of salts by the soil is inversely related to the soil moisture regime. In the wet sites, conductivities approached prespill levels within about 30 days. In such sites, spills at the experimental volumes are quickly diluted and the salts flushed from the soil. In the dry sites, on the other hand, salts are retained in the soil, apparently concentrating at or near the seasonal thaw line.
    Type of Medium: Series available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: CRREL Report 83-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods Site selection and preparation Prespill assessment Seawater application Postspill assessment Enzyme assay and analysis of soil flora Results and discussion Soil-solution conductivities Vascular plant response Cryptogam response Site factors and plant response Soil flora and extracellular soil enzymes Limitations of this study Summary and conclusions Literature cited Appendix: Plant taxa included in this study
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  • 45
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/19
    In: CRREL Report, 84-19
    Description / Table of Contents: In this study a method for making long-range forecasts of freeze-up dates in rivers is developed. The method requires the initial water temperature at an upstream station, the long-range air temperature forecast, the predicted mean flow velocity in the river reach, and water temperature response parameters. The water temperature response parameters can be either estimated from the surface heat exchange coefficient and the average flow depth or determined empirically from recorded air and water temperature data. The method is applied to the St. Lawrence River between Kingston, Ontario, and Massena, New York, and is shown to be capable of accurately forecasting freeze-up. Originator-supplied keywords include: Ice formation, and River ice.
    Type of Medium: Series available for loan
    Pages: iii, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 84-19
    Language: English
    Note: CONTENTS Abstract Preface Introduction Problem formulation Analytical treatment Application to the upper St. Lawrence River Summary Literature cited Appendix A: Basic program for St. Lawrence River freeze-up forecast
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  • 46
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/24
    In: CRREL Report, 84-24
    Description / Table of Contents: This report describes the growth characteristics and crystalline textures of urea ice sheets which are now used extensively in the Cold Regions Research and Engineering Lab. (CRREL) test basin for modeling sea ice. The aims of the report are to describe the different kinds of crystalline texture encountered in urea ice sheets and to show that even small variations in texture can drastically influence the mechanical behavior of urea ice sheets. Standard petrographic techniques for studying microstructure in thin sections were used on 24 urea ice sheets. These investigations entailed observations of the crystalline texture of the ice (including details of the subgrain structure), grain size measurements, and studies of the nature and extent of urea entrapment and drainage patterns in the ice. Increased knowledge of the factors controlling the crystalline characteristics of urea ice sheets has progressed to the point where test basin researchers at CRREL are now able to fabricate ice sheets with prescribed structures leading to predictable mechanical properties. Originators supplied keywords include: Sea ice, and Mechanical properties.
    Type of Medium: Series available for loan
    Pages: iv, 55 Seiten , Illustrationen
    Series Statement: CRREL Report 84-24
    Language: English
    Note: Contents: Abstract Preface Introduction Objectives Analytical techniques Procedures for growing urea ice sheets Analysis of the crystalline structure of urea ice Characteristics of urea ice Results and discussion Ice sheet no. 1 Ice sheet no. 2 Ice sheet no. 3 Ice sheet no. 4 Ice sheet no. 5 Ice sheet no. 6 Ice sheet no. 7 Ice sheet no. 8 Ice sheet no. 9 Ice sheet no. 10 Ice sheet no. 11 Ice sheet no. 12 Ice sheet no. 13 Ice sheet no. 14 Ice sheet no. 15 Ice sheet no. 16 Ice sheet no. 17 Ice sheet no. 18 Ice sheet no. 19 Ice sheet no. 20 Ice sheet no. 21 Ice sheet no. 22 Ice sheet no. 23 Ice sheet no. 24 Urea concentrations in test tank solution and ice Discussion and conclusions E/σf ratio Thickness of incubation layer Crystal properties Literature cited Appendix A: Thin sections of urea ice sheets
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  • 47
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/18
    In: CRREL Report, 84-18
    Description / Table of Contents: This report investigates the influences of turbulence and water temperature on frazil ice formation. The rate and thequantity of frazil ice formed in a specified volume of supercooled water increase with both increasing turbulence inten-sitv and decreasing water temperature. The influence of turbulence intensity on the rate of frazil ice formation, how-ever. is more pronounced for larger initial supercooling. The turbulence characteristics of a flow affect the rate offrazil ice formation by governing the temperature to which the flow can be supercooled, by influencing heat transferfrom the frazil ice to surrounding water, and by promoting collision nucleation, particle and floc rupture and increasingthe number of nucleation sites. larger frazil ice particles formed in water supercooled to lower temperatures. The par-ticles usually were disks, with diameters several orders greater than their thickness. Particle size generally decreased with increasing turbulence intensity. This report develops an analytical model, in which the rate of frazil ice formation isrelated to temperature rise of a turbulent volume of water from the release of latent heat of fusion of liquid water toice. Experiments conducted in a turbulence jar with a heated, vertically oscillating grid served both to guide and tocalibrate thanalytical'model as well as to afford insights into frazil ice formation. The formation of frazil ice wasstudied for Vemperatures of supercooled water ranging from -0.9° to -0.050°C.
    Type of Medium: Series available for loan
    Pages: vi, 50 Seiten , Illustrationen
    Series Statement: CRREL Report 84-18
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Background Scope of study Literature review Introduction Incipient formation of frazil ice Particle size and evolution of frazil ice Influences of turbulence and water temperature on the rate of frazil ice formation Conclusions Analytical model Introduction Elements of heat transfer Elements of turbulence Experimentation Experimental apparatus Experimental procedure Results Introduction Nucleation of frazil ice Influences of turbulence on frazil ice formation Water temperature Influences of water temperature and turbulence on the concentration of frazil ice Frazil ice particle shape and size Conclusions Literature cited Appendix A: Preliminary frazil ice experiments Flume experiments Couette-flow Appendix B: Listing of computer program for calculation of frazil ice formation Appendix C: Water temperature rise attributable to frazil ice formation as computed usingthe analytical model .
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  • 48
    Call number: ZSP-201-84/16
    In: CRREL Report, 84-16
    Description / Table of Contents: Phase composition curves are presented for a typical saline silt from Lanzhou, P.R.C., and compared to some silts from Alaska. The unfrozen water content of the Chinese silt is much higher than that of the Alaskan silts due to the large amount of soluble salts present in the silts from China, which are not present in silt from interior Alaska. When the salt is removed, the unfrozen water content is then similar for both the Chinese and Alaskan silt. Here we introduce a technique for correcting the unfrozen water content of partially frozen soils due to high salt concentrations. We calculate the equivalent molality of the salts in the unfrozen water at various temperatures from a measurement of the electrical conductivity of the extract from saturated paste.
    Type of Medium: Series available for loan
    Pages: iii, 25 Seiten , Illustrationen
    Series Statement: CRREL Report 84-16
    Language: English
    Note: Contents Abstract Preface Introduction Background Materials Sample preparation Nuclear magnetic resonance Specific surface area Electrical conductivity Results and discussion Summary Literature cited Appendix A: Unfrozen water content vs temperature data for Lanzhou silt
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  • 49
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/12
    In: CRREL Report, 84-12
    Description / Table of Contents: Icing on stationary structures such as oil rigs is becoming an increasingly serious problem as offshore drilling operations in the subpolar regions become more common. Little information exists on this subject. Extensive observations have been made of icing on the upper structures of moving ships, but the complexity of this problem makes analysis of the results very difficult. Even the generation of water drops in this case involves many factors, such as windspeed, wave direction relative to the bearing of the ship, and size and free-board of the ship. On stationary structures, however, the problem is much simpler, since the major factor in drop generation is whitecaps produced by wind, and no motion of the structure is involved. In the present study, a theoretical calculation was made by combining the data available on the generation of drops by wind with data on the proportion of ice frozen from the collected water. The rate of ice accumulation on stationary structures was calculated using published data. The results were compared with icing measured on board ships. Although the general trend of this calculation indicated parallelism with the onboard measurements, the measured ice accumulation rate on ships needed a 5 to 8 m/s higher windspeed to correspond with the calculated rate for stationary structures.
    Type of Medium: Series available for loan
    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 84-12
    Language: English
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  • 50
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/11
    In: CRREL Report, 84-11
    Description / Table of Contents: Data obtained from two sets of data buoys either air-dropped or deployed by ship onto the Weddell Sea pack ice during the period from Dec 1978 to Nov 1980 are presented. The buoy data include position, pressure and temperature information and to date represent the most complete combined weather and pack ice drift records for the ice-covered Southern Ocean regions. The buoys tended to drift north initially and then to turn east generally between latitudes 62°S and 64°S. Buoy 1433 turned east farther south at approximately 67°S but at about the same time as buoy 0527, implying that the westerly wind belt was farther south than usual in 1979. The range of air pressures-from about 950 mb to about 1020 mb is typical of the circumpolar low pressure trough in the Southern Hemisphere. All buoys were equipped with an internal or compartment temperature sensor. The 1980 buoys also contained an external air temperature sensor in a ventilated, shielded can at 1-m height. Although differences of 10°C or more between recorded air and compartment temperatures are common, the correlation between the two measured temperatures is generally very good. The compartment temperatures are higher probably because the buoy is radiationally heated. We found that subtracting 3°C from the average daily compartment temperature yielded a good estimate of the average air temperature for any given day. This technique can be used to construct average daily air temperature records for the 1979 buoys which only contained the internal or compartment temperature sensor.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 84-11
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods and instrumentation Results Drift tracks Pressure data Temperature data Discussion Conclusions Literature cited
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  • 51
    Call number: ZSP-201-84/9
    In: CRREL Report, 84-9
    Description / Table of Contents: This report presents the results of the first phase of a test program designed to obtain a comprehensive understanding of the mechanical properties of multi-year sea ice from the Alaskan Beaufort Sea. In Phase I, 222 constant-strain-rate uni-axial compression tests were performed on ice samples from ten multi-year pressure ridges to examine the magnitude and variation of ice strength within and between pressure ridges. A limited number of constant-strain-rate compression and tension tests, constant-load compression tests, and conventional triaxial tests were also performed on ice samples from a multi-year floe to provide preliminary data for developing ice yield criteria and constitutive laws for multi-year sea ice. Data are presented on the strength, failure strain, and modulus of multi-year sea ice under different loading conditions. The statistical variation of ice strength within and between pressure ridges is examined, as well as the effects of ice temperature, porosity, structure, strain rate and confining pressure on the mechanical properties of multi-year sea ice.
    Type of Medium: Series available for loan
    Pages: v, 107 Seiten , Illustrationen
    Series Statement: CRREL Report 84-9
    Language: English
    Note: CONTENTS Abstract Preface Introduction Field Sampling Site selection and description Ice sampling procedures Shipping and storage of ice samples Testing Techniques Multi-year Pressure Ridge Tests Ice description Sampling scheme and test variables Uniaxial compressive strength Residual compressive strength Failure strains Initial tangent modulus Statistical Variations in Ice Strength Differences in strength above and below level ice Sources of the variation in strength Shape of the strength histograms Multi-year Floe Ice Tests Ice description Uniaxial compressive strength Constant-load compression tests Constant-strain-rate tension tests Triaxial tests Conclusions Literature Cited Appendix A: Structural profile of a multi-year pressure ridge core Appendix B: Ridge uniaxial compression test data Appendix C: Structural profile of the continuous multi-year floe core Appendix D: Multi-year floe test data
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  • 52
    Monograph available for loan
    Monograph available for loan
    Frankfurt am Main : Suhrkamp
    Associated volumes
    Call number: M 19.92568
    In: Sphären
    Type of Medium: Monograph available for loan
    Pages: 1013 Seiten , Illustrationen
    Edition: 9. Auflage
    ISBN: 9783518410547
    Series Statement: Sphären 2
    Language: German
    Location: Upper compact magazine
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  • 53
    Monograph available for loan
    Monograph available for loan
    Osnabrück : Naturwissenschaftliches Museum
    Call number: G 8547/2
    Type of Medium: Monograph available for loan
    Pages: 31 Blatt , Karten
    Language: German
    Location: Upper compact magazine
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  • 54
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: S 92.0083(1984)
    In: Erdbeben in der Bundesrepublik Deutschland
    Type of Medium: Series available for loan
    Pages: 57 Seiten
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  • 55
    Call number: MOP Per 800(301)
    In: WMO / World Meteorological Organization
    Type of Medium: Monograph available for loan
    Pages: 166 Seiten
    Series Statement: WMO / World Meteorological Organization 301
    Language: English
    Location: MOP - must be ordered
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  • 56
    facet.materialart.12
    facet.materialart.12
    Washington, D.C. : George Washington University
    Description / Table of Contents: This handbook is for any educator teaching a topic that includes data analysis or computation in order to support learning. It is not just for educators teaching courses in engineering or science, but also data journalism, business and quantitative economics, data-based decision sciences and policy, quantitative health sciences, and digital humanities. It aims to provide an entry point, and a broad overview of Jupyter in education. Whether you are already using Jupyter to teach, you have found learning materials built on Jupyter that piqued your curiosity, or have never heard of Jupyter, the material in this open book can empower you to use this technology in your teaching. Project Jupyter is a broad collaboration that develops open-source tools for interactive and exploratory computing. The tools include: over 100 computer languages (with a focus on Python), the Jupyter Notebook, JupyterHub, and an ecosystem of extensions contributed by a large community. The Jupyter Notebook has exploded in popularity since late 2014, fueled by its adoption as the favorite environment for doing data science. It has also grown as a platform to use in the classroom, to develop teaching materials, to share lessons and tutorials, and to create computational stories. Notebooks are documents containing text narratives with images and math, combined with executable code (many languages are supported) and the output of that code. This marriage of content and code makes for a powerful new form of data-based communication. Educators everywhere are adopting Jupyter for teaching. Educators newly adopting Jupyter can be overwhelmed by having to navigate the ecosystem of tools and content. They could study many examples, or consume a myriad of blog posts and videos of talks to distill the patterns of good practices and technical solutions to serve their students best. Several early adopters, having much experience to share, decided to begin collecting this know-how, and share open documentation about using Jupyter for teaching and learning. The result is this open book: a living document that captures the experiences of community members using Jupyter in education. The Jupyter Community Workshop in Washington, DC (November 2018) began that process, with a book sprint aimed at producing the first version of this handbook. The collaboratively written book consolidates explanations and examples covering key topics, including: what is Jupyter, how to try Jupyter, sharing notebooks with students, locally installing Jupyter, cloud offerings, finding example notebooks, writing lessons in Jupyter, making collections for a course, exporting to other formats with nbconvert, writing textbooks with Jupyter, using Binder and JupyterHub, making assignments and auto-grading, making online courses, teaching with Jupyter in the classroom, active learning and flipped learning pedagogies with Jupyter, and guiding learners to create their own content in Jupyter. This open handbook will grow to encompass all you need to know about Jupyter in teaching and learning.
    Type of Medium: 12
    Pages: Online-Ressource
    Language: English
    Note: 1 Introduction Acknowledgments 2 Why we use Jupyter notebooks 2.1 Why do we use Jupyter? 2.2 But first, what is Jupyter Notebook? 2.3 Course benefits & anecdotes 2.4 Student benefits 2.5 Instructor benefits 2.6 Conclusions 3 Notebooks in teaching and learning 3.1 Oh the places your notebooks will go! 3.2 Before You Begin… 4 A catalogue of pedagogical patterns 4.1 Introduction 4.2 Shift-Enter for the win 4.3 Fill in the blanks 4.4 Target Practice 4.5 Twiddle, tweak, and frob 4.6 Notebook as an app 4.7 Win-day-one 4.8 Top-down sequence 4.9 Two bites at every apple 4.10 Coding as translation 4.11 Symbolic math over pencil + paper 4.12 Replace analysis with numerical methods 4.13 The API is the lesson 4.14 Proof by example, disproof by counterexample 4.15 The world is your dataset 4.16 Now you try (with different data or process) 4.17 Connect to external audiences 4.18 There can be only one 4.19 Hello, world! 4.20 Test driven development 4.21 Code reviews 4.22 Bug hunt 4.23 Adversarial programming 5 Jupyter Notebook ecosystem 5.1 Language support: kernels 5.2 Using Jupyter notebooks 5.3 Authoring Jupyter notebooks 5.4 Tips and tricks 5.5 Gotchas 6 Getting your class going with Jupyter 6.1 Local installation on students’ or lab computers 6.2 Jupyter on remote servers 6.3 Distribution and collection of materials 6.4 Assessing student learning with Jupyter notebooks 6.5 How do you create Jupyter notebooks for reuse and sharing? 6.6 Jupyter: a 21st Century genre of Open Educational Resources and practices 7 Usage case studies 7.1 Jupyter notebooks in support of scaling for large enrollments 7.2 The “CFD Python” story: guiding learners at their own pace 7.3 Analyzing music with music21 7.4 Interactivity in computer science (high school and middle school) 7.5 Interactive geophysics with Jupyter 7.6 Investigating hurricanes 8 About the authors 8.1 Project lead 8.2 Authors at the sprint 9 Glossary References
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    Type of Medium: Non-book medium
    Pages: Online-Ressource
    Language: English
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  • 58
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/5
    In: CRREL Report, 83-5
    Description / Table of Contents: This report presents the results of dynamic ice-structure interaction model tests conducted at the CRREL Ice Engineering Facility. A flexible, single-pile, bottom-founded offshore structure was simulated by a test pile with about a one-to-ten scale ratio. Urea (instead of sodium chloride) was used as dopant to scale down the ice properties, resulting in good model ice properties. Six ice fields were frozen and 18 tests carried out. In all cases distinctive dynamic ice structure interaction vibrations appeared, from which abundant data were collected. In tests with linear ice velocity sweep, sawtooth-shaped ice force fluctuations occurred first. With increasing velocity the natural modes of the test pile were excited, and shifts from one mode to another occurred. The maximum ice force values appeared mostly with low loading rates, but high forces appeared random'y at high ice velocities. As a general trend, ice force maximums, averages and standard deviations decreased with increasing ice velocities. The aspect ratio effect of the ice force in continuous crushing follows the same dependence as in static loadings. The frequency of observed ice forces is strongly dominated by the natural modes of the structure. Dynamically unstable natural modes tend to make the developing ice force frequencies the same as the natural frequencies. Otherwise the resulting frequency depends directly on structural stiffness and ice velocity and inversely on the ice force range. During vibrations the displacement rates of the structure overcome the velocity of ice, making low loading rates and hence high ice forces possible. During crushing, ice induces both positive and negative damping.
    Type of Medium: Series available for loan
    Pages: iv, 53 Seiten , Illustrationen
    Series Statement: CRREL Report 83-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test arrangements Ice properties Crushing patterns Maximum ice force vs velocity Dynamic aspect ratio effect and crushing strength Measured ice force frequencies Calculated ice force frequencies Accelerations, velocities and displacements Damping Ice-induced negative damping Limit cycles Buckling load Conclusions Literature cited
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  • 59
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/4
    In: CRREL Report, 83-4
    Description / Table of Contents: Measurements and analysis of seasonal ice growth and decay on Post Pond, New Hampshire, for the period 1973-1982 are presented. Observations included ice thickness measurements, examination of the various ice types contributing to the ice cover, and measurements of meteorological parameters for correlation with and modeling of the ice growth process. The overall nature of ice growth and decay (ice loss) on the Post Pond has been ascertained, the seasonal variability in the timing of freeze-up and ice-out and the duration of the ice cover have been determined, and the relationship of ice growth to freezing-degree-day (deg C) records evaluated on the basis of a Stefan conduction equation modified to deal with ice sheets covered with or free of snow. Ice growth occurs predominantly by the direct freezing of lake water, but snow ice may compose as much as 50% of the ice cover in winters with higher than average snowfall. Freeze-up leading to the establishment of a stable ice cover occurs during the 4-week period from the end of November to the end of December. Maximum seasonal ice thicknesses were from 45 to 67 cm and are generally attained during the first two weeks of March; ice-out, marking the final disappearance of ice from Post Pond, usually occurs by the third week of April. The overall rate of the ice loss is three to four times that of ice growth, and is dominated initially by melting from the top. As much as 50% of the ice may be lost in this way before the onset of any bottom melting. Final dissipation of the ice cover is usually expedited by candling resulting from preferential melting and disintegration of the ice at crystal boundaries.
    Type of Medium: Series available for loan
    Pages: iv, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 83-4
    Language: English
    Note: CONTENTS Abstract Preface Introduction Location of study Study methods Ice thickness Ice-cover composition Surface air temperatures Freeze-up and ice-out characteristics Results and discussion Ice-growth record Freezing-degree-day records Ice-growth predictions Summary and conclusions Literature cited Appendix A: Ice-growth records Appendix B: Measured and computed ice-growth curves
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  • 60
    Call number: AWI G3-19-92380
    In: Permafrost in Switzerland, 2000/2001 and 2001/2002
    Type of Medium: Series available for loan
    Pages: 86 Seiten , Illustrationen
    Series Statement: Glaciological Report (Permafrost) / Permafrost Monitoring Switzerland 2/3
    Language: German
    Note: Contents Preface Published reports Summary 1 Introduction 1.1 From permafrost research to permafrost monitoring 1.2 PERMOS elements 2 Weather and climate 2.1 Introduction 2.2 Weather and climate in 2000/2001 2.3 Weather and climate in 2001/2002 2.4 Climate deviation in 2000/2001 and in 2001/2002 2.5 Duration of the snow cover 3 Borehole measurements 3.1 Introduction 3.2 Active layer thickness 3.3 Permafrost temperatures 3.4 Borehole deformation 3.5 Conclusions 4 Surface temperatures 4.1 Introduction 4.2 Surface temperature mesasurements in 2000/2001 and in 20001/2002 4.3 Surface temperature measurements in the forthcoming years 4.4 Conclusions 5 Air photos Conclusions Acknowledgements References Appendix A Boreholes B Instructions for temperature monitoring in mountain permafrost (PACE-manual)
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  • 61
    Series available for loan
    Series available for loan
    Zurich : Cryospheric Commission of the Swiss Academy of Sciences (SCNAT)
    Associated volumes
    Call number: AWI G3-19-92381
    In: Permafrost in Switzerland, 2004/2005 and 2005/2006
    Type of Medium: Series available for loan
    Pages: XIV, 100 Seiten , Illustrationen
    Series Statement: Glaciological Report (Permafrost) / Permafrost Monitoring Switzerland 6/7
    Language: English
    Note: Contents: Imprint Published Reports Preface Summary Zusammenfassung Résumé Riassunto Resumaziun 1 Introduction 2 Weather and Climate 2.1 Weather and Climate in 2004/2005 2.2 Weather and Climate in 2005/2006 2.3 Climate Deviation from the Mean Value 1961–1990 2.4 Duration of the Snow Cover 3 Borehole Measurements 3.1 Active Layer Thickness 3.2 Permafrost Temperatures 3.2 ERT Monitoring Network 3.4 Conclusions Boreholes 4 Surface Temperatures 4.1 Surface Temperatures in Unconsolidated Sediments 4.2 Rock Surface Temperatures 4.3 Conclusions Surface Temperatures 5 Air Photos 5.1 Air Photos in 2004/2005 and 2005/2006 6 Conclusion 7 Selected Aspects of Permafrost Monitoring 7.1 Short-term Variations in Rock Glacier Kinematics 7.2 Destabilized Rock Glaciers 7.3 Conclusions Rock Glacier Dynamics Acknowledgements References Appendix
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  • 62
    Monograph available for loan
    Monograph available for loan
    Mendoza : Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales
    Call number: AWI G1-19-92379
    Type of Medium: Monograph available for loan
    Pages: xii, 269 Seiten , Illustrationen
    ISBN: 978-43-4545-4
    Language: Spanish
    Note: ÍNDICE PRÓLOGO INTRODUCCIÓN ALGAS DIATOMEAS TOXIGÉNICAS PRESENTES EN LA COSTA ARGENTINA / Eugenia Sar y Martha Ferrario ARQUEOLOGÍA EL POBLAMIENTO TEMPRANO DEL CENTRO-NORTE DE MENDOZA Y SU RELACIÓN CON LAS CONDICIONES AMBIENTALES DEL PASADO / Alejandro García PROCESOS DE OCUPACIÓN PREHISTÓRICA Y CAMBIO AMBIENTAL EN LA PLANICIE NORESTE DE MENDOZA: PERSPECTIVAS DESDE LA ARQUEOLOGÍA / Horado Chiavazza CUADRO DE FÓSILES DE MENDOZA / Osvaldo Luis Bordonaro DENDROCRONOLOGÍA INFLUENCIAS CLIMÁTICAS EN LA DINÁMICA FORESTAL DEL ECOTONO BOSQUE-ESTEPA EN EL NORTE DE PATAGONIA / Ricardo Villalba APORTE DE LA XILOLOGÍA AL ESTUDIO DENDROCRONOLÓGICO DE NOTHOFAGUS EN LA ARGENTINA / Stella Maris Rivera VARIACIONES EN EL CAUDAL DEL RÍO ATUEL DESDE 1575 HASTA EL PRESENTE RECONSTRUIDAS CON SERIES DE ANILLOS DE ÁRBOLES Y SUS RELACIONES CON LA OSCILACIÓN DEL SUR / José Boninsegna y Silvia Delgado de Brun LA INFLUENCIA DE LA TEMPERATURA EN EL CRECIMIENTO DE DISCARJA TRINERVISEN LA CORDILLERA MENDOCINA / Andrea Schmelter REGISTROS DENDROCRONOLÓGICOS DE MADERAS DEL PLEISTOCENO TARDÍO-HOLOCENO EN AMÉRICA DEL SUR / Fidel A. Roig Juñent EVIDENCIAS HISTÓRICAS Y DENDROCRONOLÓGICAS DE LAS VARIACIONES CLIMÁTICAS EN LA PATAGONIA DURANTE LOS ÚLTIMOS 1000 AÑOS (PATAGON-1000) / Silvia Delgado, Mariano Masiokas, Ricardo Villalba, Dario Trombotto, Alberto Ripalta, José Hernández y Salvador Calí DENDROECOLOGÍA DE LOS ALGARROBALES DE LA ZONA ÁRIDA ARGENTINA / Pablo E. Villagra, Mariano S. Morales, Ricardo Villalba y José A. Boninsegna EPISTEMOLOGÍA EL ROL DE LAS CIENCIAS NATURALES Y LAS CIENCIAS SOCIALES EN EL ESTUDIO DEL AMBIENTE / Teresita Castrillejo GEOCRIOLOGÍA EL AMBIENTE CRJOGÉNICO ACTUAL Y EL PALEOPERMAFROST EN EL EXTREMO AUSTRAL DE AMÉRJCA DEL SUR / Dario Trombotto PERFORADORA A PERCUSIÓN PARA SUELOS DETRÍTICOS CRJOGÉNICOS / José M. Hernández HIDROLOGÍA DE AMBIENTES PERJGLACIALES. CUENCA MORENAS COLORADAS - VALLECITOS, CORDÓN DEL PLATA, CORDILLERA FRONTAL, MENDOZA / Enrique Buk ESTRUCTURAS SEDIMENTARJAS INTERNAS Y CONCENTRACIÓN DE MINERALES PESADOS EN LA CAPA ACTIVA / Ana-Lía Ahumada HIDROLOGÍA DEL PERMAFROST DE MONTAÑA Y SU RELACIÓN CON LA RADIACIÓN SOLAR. ESTUDIO DE UNA CUENCA COLECTORA EN AGUA NEGRA, ALTOS ANDES DE SAN JUAN, ARGENTINA / Lothar Schrott MAPEO GEOMORFOLÓGICO DEL PISO PERJGLACIAL EN LOS ANDES SEMIÁRJDOS / Karl-Heinz Scholl EFECTOS DEL CONGELAMIENTO DEL SUELO EN MENDOZA Y TERMINOLOGÍA / María Cecilia Regairaz GEODESIA DISEÑO, ANÁLISIS DE PRECISIÓN Y AJUSTE DE REDES TOPOGEODÉSICAS / María Virginia Mackern SISTEMA DE INFORMACIÓN GEOGRÁFICA PARA EL ORDENAMIENTO TERRITORIAL / Roberto Bruce, Ernesto Corvalán, Orlando Di Giuseppe, Luis Lenzano, Rosana Llorens, M. Virginia Mackern, Ana M. Robin y Rolando Sendra GEOFÍSICA CONTRIBUCIÓN AL CONOCIMIENTO GEOFÍSICO DE LA REGIÓN A LO LARGO DEL PARALELO 33°S EN ARGENTINA, MEDIANTE SONDEOS MTs Y MVs. SÍNTESIS PRELIMINAR / Enrique Borzotta, Manuel J. Mamaní y Hugo G. Fournier GEOLOGÍA DEL CUATERNARIO GLACIACIONES CUATERNARIAS EN EL VALLE DEL RÍO MENDOZA, ANDES ARGENTINOS / Lydia E. Espizúa LOS PALEOAMBIENTES DEL PLEISTOCENO-HOLOCENO EN LA CUENCA DEL ARROYO LA ESTACADA, MENDOZA / Marcelo A. Zárate y Marta M. Páez GEOLOGÍA REGIONAL LOS CARBONATOS CÁMBRJCOS Y ORDOVÍCICOS DE LA PRECORDILLERA ARGENTINA COMO ROCAS DE APLICACIÓN INDUSTRIAL / Osvaldo Luis Bordonaro CICLOS SEDIMENTARIOS ORDOVÍCICOS EN EL TERRANE DE PRECORDILLERA, OESTE DE ARGENTINA / Matilde Sylvia Beresi IDSTORIA AMBIENTAL EVIDENCIAS HISTÓRJCAS SOBRE ALGUNOS ASPECTOS DE VARIABILIDAD CLIMÁTICA EN ARGENTINA y BOLIVIA DURANTE LOS ÚLTIMOS CUATRO SIGLOS / María del R. Prieto y Roberto Herrera MANEJO ECOLÓGICO DE CUENCAS INTERRELACIÓN DEL PASTOREO CAPRJNO y LA VEGETACIÓN NATURAL: ALGUNAS PAUTAS PARA EL MANEJO DE AMBIENTES ÁRIDOS / Eduardo Guillermo Grünwaldt LA EDUCACIÓN AMBIENTAL EN EL CONTEXTO DEL MANEJO DE CUENCAS / Marcela S. Mansilla, Armando R. Pedrani y Ricardo Ojeda CARACTERJZACIÓN DEL PROCESO DE INFILTRACIÓN EN EL PIEDEMONTE MENDOCINO / Marcela Nave, Armando Pedrani, Alberto I.J. Vich y Adriana Mariani LA EROSIÓN HÍDRJCA EN EL PIEDEMONTE ÁRIDO DE MENDOZA / Alberto I.J. Vich y Armando Pedrani CORRECCIÓN DE CUENCAS CON TRAMPAS DE AGUA / Adriana Mariani, Armando Pedrani, Alberto Vich y Marcela Nave METEOROLOGÍA PROGRAMA REGIONAL DE METEOROLOGÍA, MENDOZA (ARGENTINA) / J. Cristaldo, H. Estrella, J. Ferraro, N. Heredia, R. Moltó, F. Norte, A. Palma, M. Silva y S. Simonelli NIVOGLACIOLOGÍA INVENTARlO DE GLACIARES DE MENDOZA Y SAN JUAN / Rafael Bottero FLUCTUACIONES GLACIARJAS EN LA CUENCA SUPERJOR DEL RÍO ATUEL, MENDOZA, ARGENTINA / Daniel Roberto Cobos CONSTRUCCIÓN DE LA SONDA N° 5 / Víctor Hugo Videla y Jorge Suarez AVANCES O RETROCESOS GLACIARIOS EN LOS ANDES CENTRALES ARGENTINOS / Rosana Elisabeth Llorens LA SITUACIÓN ACTUAL DE LOS GLACIARES ANDINOS / Juan Carlos Leiva MODELO DE CAPTURA DE PARTÍCULAS DE NIEVE Y DE POLVO AMBIENTAL POR EL VIENTO / Hugo Martínez PALEONTOLOGÍA DE INVERTEBRADOS ANÁLISIS BIOESTRATIGRÁFICO Y PALEOBIOGEOGRÁFICO DE LOS GRAPTOLITOS DEL PALEOZOICO INFERJOR DE LA CORDILLERA ORIENTAL, ARGENTINA / Blanca A. Toro PALEONTOLOGÍA DE VERTEBRADOS HALLAZGO DEL PRIMER HUEVO FÓSIL DE DINOSAURIO (?) EN MENDOZA / Elíseo Sepúlveda DINOSAURIOS Y AMBIENTES DEL CRETÁCICO DE LA PROVINCIA DE MENDOZA, ARGENTINA / Bernardo J. González Riga PALEOPAUNOLOGÍA ASPECTOS BIOGEOG~FICOS Y PALEOCLIMÁTICOS DE LAS SUCESIONES TRIÁSICAS DE ARGENTINA EN BASE A REGISTROS PALINOLOGICOS / Ana María Zavattieri BIOESTRATIGRAFÍA, PALEOGEOGRAFÍA Y PALEOAMBIENTES BASADOS EN PALINOMORFOS EN CUENCAS ORDOVÍCICAS SILURICAS Y DEVONICAS DE LA ARGENTINA / Claudia Viviana Rubinstein INFERENCIAS PALEOBIOGEOGRÁFICA Y PALEOAMBIENTAL DEL GÉNERO GRAPNELISPORA (STOVER & PARTRIDGE) DEL CRETACICO SUPERIOR DEL NORTE DE PATAGONIA / Oscar Hugo Papú ESTUDIO PALINOLÓGICO DEL CRETÁCICO INFERIOR DE LA CUENCA DE SAN LUIS / Mercedes B. Prámparo INFERENCIAS PALEOAMBIENTALES EN BASE A DINOFLAGELADOS MARINOS DEL CRETÁCICO INFERIOR DE LA CUENCA NEUQUINA / Patricia Peralta ALGUNAS OBSERVACIONES SOBRE UNA MICROFLORA EOCENA DE LA ISLA VICECOMODORO MARAMBIO ANTARTIDA ARGENTINA / Eliseo G. Sepúlveda PAUNOLOGÍA ESTUDIOS PALINOLÓGICOS EN LAS REGIONES ÁRIDAS MENDOCINAS / Mónica Cristina Wingenroth COLECTOR DE POLEN / Jorge A. Suarez y Víctor H. Videla PETROLOGÍA Y GEOQUÍMICA LAS PEGMATITAS MINERALIZADAS DE LAS SIERRAS PAMPEANAS / Miguel Ángel Galliski MINA CAPILLITAS, UN DEPÓSITO EPITERMAL DEL NOROESTE ARGENTINO / María Florencia Márquez Zavalía RIESGO GEOLÓGICO EL VOLCANISMO RECIENTE Y RIESGO ASOCIADO EN LA PROVINCIA DE MENDOZA / Patricia Sruoga EL CUATÉRNARIO DEL BLOQUE DE SAN RAFAEL. CARACTERÍSTICAS GEOMORFOLÓGICAS - ESTRUCTURALES Y RIESGO SISMICO ASOCIADO / Héctor Américo Cisneros TESTIGOS DE HIELO TESTIGOS DE HIELO (PENÍNSULA ANTÁRTICA- HIELO CONTINENTAL PATAGÓNICO) / Alberto José Aristarain
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  • 63
    Monograph available for loan
    Monograph available for loan
    Palisades : Lamont-Doherty Geological Observatory, Columbia University
    Call number: AWI G2-19-92382
    Type of Medium: Monograph available for loan
    Pages: 690 Seiten , Illustrationen, Karten
    Language: English
    Note: Table of Contents CHAPTER 1 INTERNAL CYCLING AND THROUGHPUT : Pathways from River Mouth to Sea Floor Depth Profiles of Sea Salt Composition Constituent Classification The Chemical Composition of Marine Organic Matter Composition of Particulate Matter Caught in Sediment Traps A Simple Model for Biologically Utilized CDnstituents The Distributions of Biointermediate Constituents Estimation of Input Rates Horizontal Segregation of CDnstituents in the Deep Sea Summary CHAPTER 2 THE SEDIMENTARY SINK Factors Influencing the Distribution of Sedimentary Constituents Introduction Sediment Types Distribution of Opal Production Opal Solution on the Sea Floor Distribution of Calcite in Marine Sediments Degree of Calcite Saturation Variation in the Carbonate Ion Content of Sea Water Spacial Variations in the CaC0 3 Saturation of Sea Water Factors Controlling the Rate of Calcite Solution Thickness and Shape of the Sublysocline Transition Zone Variation of Sediment Type with Time Manganese Nodules Summary CHAPTER 3 THE ATMOSPHERIC IMPRINT : The Cycles of Gases within the Sea Introduction Solubilities of Gases in Sea Water The Rate of Gas Exchange Stagnant Film Thickness Derived from Natural Radiocarbon Stagnant Film Thicknesses Determined by the Radon Method Oxygen Concentrations in Surface Ocean Water Oxygen Deficiencies in the Deep Sea The Marine N2O Cycle Excess Helium The Carbon Dioxide Content of Surface Ocean Water Origin of the Equatorial Pacific CO2 Anomaly Summary CHAPTER 4 REACTIVE METALS AND THE GREAT PARTICULATE SWEEP : The Cycle of Metals in the Sea Introduction Products of Uranium and Thorium Decay Thorium Isotopes in the Sea Protactinium-231 to Thorium-230 Activity Ratios The Distribution of Lead-210 The Distribution of Polonium-210 The Distribution of Radium-226 Anthropogenic Plutonium in the Sea Toward a Model of Metal Transport Distributions of Stable Metals in the Sea Stable Isotope Ratios in Reactive Metals Transport of Iron and Manganese in the Sea Lessons from Controlled Ecosystem Studies Distribution Coefficients Summary CHAPTER 5 HOW FAST DOES THE MILL GRIND? : Rates of Vertical Mixing and Sediment Accumulation Introduction Rate of Vertical Mixing Implication to the Distribution of Radium-226 Distribution of Radiocarbon in the Ocean Rate of Continental Runoff Sediment Accumulation Rates Radiocarbon Dating Uranium Series Dating Beryllium Dating Potassium-Argon Dating Agreement Among Dating Methods Comparison of Model and Observed Rates of CaC0 3 Solution Summary CHAPTER 6 WHAT KEEPS THE SYSTEM IN WHACK? : Control Mechanisms Operating in the Sea Introduction Phosphate Controls Silicate Controls Carbon Controls Interactions between the Phosphate and Carbon Controls Nitrate Controls Dissolved Oxygen Controls Major Anion Controls Major Cation Controls Possible Causes for Perturbations Recorders of Paleoocean Chemistry The Marine Geochemistry of Carbon-13 The Uranium Content of Coral Factors Influencing Nutrient Gradients in the Deep Sea Summary CBAPTER 7 FREIGHT TRAINS AND FICKIAN CONFUSION : The Movement of Water Through the Deep Sea Introduction Types of Motion One Dimensional Advection - Diffusion Model Tracers for Diapycnal and Isopycnal Mixing Mixing Rates Based on Radon-222 and Radium-228 The Distribution of Helium-3 in the Deep Pacific Sources of Deep Water Northern Component Water Conservative Properties of NCW Initial Radiocarbon to Carbon Ratio in NCW Feed for NCW Production Southern Component Water Ventilation of the Deep Atlantic Ocean Ventilation of the Deep Pacific and Indian Oceans The Grand Cycle of Radiocarbon in the Deep Ocean Biological Short-Circuiting Temporal Variations in Radiocarbon Production Argon-39 Summary CHAPTER 8 THE ANTHROPOGENIC INVASION : The Movement of Water Through the Oceanic Thermocline Introduction Input Functions Hydrology of the Main Thermocline Tritium Distribution within the Thermocline Temporal Trends in Tritium Tritium as a Guide to Deep Water Formation Supplementary Information from Strontium-90 Bomb Carbon-14 Distribution within the Thermocline Explanations for Low Equatorial Bomb Carbon-14 Inventories Implications of Equatorial Upwelling to the Tritium Budget An Upwelling Rate Based on the Equatorial CO2 Anomaly Helium-3 Distribution in the Main Oceanic Thermocline Purposeful Tracers Summary CHAPTER 9 ICE SHEETS AND OCEAN PHOSPHATE : Glacial to Interglacial Changes in Ocean Chemistry Introduction Temperature and Salinity Changes Formation and Destruction of Organic Materials Changes in CaCO3 Storage Evidence for an Early Post-Glacial Lysocline Change Changes in Phosphate Concentration The Combined Evidence from Deep Sea Cores Cause of the Oceanic Phosphate Change An Alternate Scenario Wrap Up of the CO2 Record The Oxygen Record Glacial to Interglacial Changes in Ocean Mixing Rate Glacial to Interglacial Lysocline Changes Changes in the Distribution of Nutrients in the Deep Sea Summary CHAPTER 10 CAN MAN OVERRIDE THE CONTROLS? : The Buildup of Fossil Fuel CO2 in the Atmosphere and Oceans Introduction CO2 Production in the Past CO2 Production in the Future Capacity of the Sea for Fossil Fuel CO2 Uptake Utilizable Capacity - Simplified Calculation Utilizable Capacity - Rigorous Calculation Kinetics of Fossil Fuel CO2 Uptake by the Sea Numerical Model crosschecks on the Validity of the Numerical Model Prediction of Future CO2 Levels Solution of Sea Floor Calcite Summary REFERENCES, CONSTANTS, DEFINITIONS, ABBREVIATIONS AND INDEX Introduction to the References Subject Outline for the References Annotated Reference List Frequently Used Constants Definitions of Isotope Notations Abbreviations Index Foldout Caption
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  • 64
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-82/29
    In: CRREL Report, 82-29
    Description / Table of Contents: Ice grains in a snow cover with a low temperature gradient assume a well-rounded equilibrium form. However, at temperature gradients of 0.1 to 0.2 C/cm (depending somewhat on temperature and snow density), the rounded grains recrystallize into a faceted kinetic growth form. The large temperature gradient must play a decisive role in moving the vapor fast enough to sustain the rapid growth rate associated with the kinetic growth form. Once the large temperature gradient is removed, the grains recrystallize back to the equilibrium form. the recrystallization occurs in either direction without a change in bulk density. The growth of faceted crystals begins at the warmer base of the snow cover where the excess vapor pressure is largest. A transition between the overlying rounded grains moves upward in time. Faceted crystals also grow just below crusts of reduced permeability, where the increased vapor accumulation can sustain the excess vapor pressure neded for kinetic growth. The heat and vapor flows are described using a model based on thermodynamic equilibrium. The temperature distribution is shown to be quasi-linear at steady state in homogeneous snow. The recrystallization of the snow is modeled using the rounded grains as sources and the faceted grains as sinks. In the future this model should be extended to account for different temperatures among the sources and sinks.
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    Pages: 27 Seiten , Illustrationen
    Series Statement: CRREL Report 82-29
    Language: English
    Note: Contents: Abstract Preface Introduction Vapor flow Temperature profile Crystal growth rates Equilibirum versus kinetic growth forms of snow crystals Discussion Summary Literature cited
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  • 65
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    Call number: ZSP-201-82/32
    In: CRREL Report, 82-32
    Description / Table of Contents: Low-frequency (10 Hz) volcanic earthquakes originate at a wide range of depths and occur before, during, and after magmatic eruptions. The characteristics of these earthquakes suggest that they are not typical tectonic events. Physically analogous processes occur in hydraulic fracturing of rock formations, low-frequency icequakes in temperate glaciers, and autoresonance in hydroelectric power stations. We propose that unsteady fluid flow in volcanic conduits is the common source mechanism of low-frequency volcanic earthquakes (tremor). The fluid dynamic source mechanism explains low-frequency earthquakes of arbitrary duration, magnitude, and depth of origin, as unsteady flow is independent of physical properties of the fluid and conduit. Fluid transients occur in both low-viscosity gases and high-viscosity liquids. A fluid transient analysis can be formulated as generally as is warranted by knowledge of the composition and physical properties of the fluid, material properties, geometry and roughness of the conduit, and boundary conditions. To demonstrate the analytical potential of the fluid dynamic theory, we consider a single-phase fluid, a melt of Mount Hood andeside at 1250 deg C, in which significant pressure and velocity variations occur only in the longitudinal direction.
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    Pages: 15 Seiten , Illustrationen
    Series Statement: CRREL Report 82-32
    Language: English
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  • 66
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    Call number: ZSP-201-83/2
    In: CRREL Report, 83-2
    Description / Table of Contents: A numerical model of rime ice accretion on an arbitrary two-dimensional airfoil is presented. The physics of the model are described and results are presented that demonstrate, by comparison with other theoretical data and experimental data, that the model predictions are believable. Results are also presented that illustrate the capability of the model to handle time-dependent rime ice accretion, taking into account the feedback between the ice accretion and the airflow and droplet trajectory fields.
    Type of Medium: Series available for loan
    Pages: vi, 81 Seiten , Illustrationen
    Series Statement: CRREL Report 83-2
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Methodology Potential flow around an arbitrary airfoil Incompressible velocity field Droplet trajectory equation Computational procedure for trajectories Determining the point of impact Calculation of collision efficiencies Accreting an ice layer Determining the accuracy of the flow field Determining the accuracy of the trajectories Results and discussion Comparing results with and without the history term Collision efficiency of NACA 0015 airfoil at 8° attack angle Time-dependent accretion on NACA 0015 airfoil at 8° attack angle Time-dependent accretion on NACA 0015 airfoil at 0° attack angle Conclusions and recommendations Literature cited Appendix A : Sample input Appendix B: Sample output Appendix C : Program listing
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  • 67
    Call number: ZSP-980-70
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Part 2, 50 to 97
    In: ZfI-Mitteilungen, Nr. 70
    Type of Medium: Series available for loan
    Pages: 355 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 70
    Language: English
    Note: Contents of Part 2 Hecht, K. Gerber, R. Otto: Studies on the drying of paints by means of 14C-labelled compounds K. Wagner, F. Brutschin, I. Ritter, T. Gritsch, H. Zimmermann, H. Borchert: Investigations by the aid of radioisotope methods on the technology of the production of carbon and silicon carbide materials K. Gloe, P. Mühl: Determination of metal extraction process parameters using tracer technique W. Migdał, W. Łada, K. Malec-Czechowska: Studies on liquid-liquid extraction of noble metals using radiotracers L. Petryka, K. Przewłocki: Radiotracer investigations of benefication copper ore in the industrial flotation process Z. Bazaniak, J. Palige: Determination of Cu recovery degree from slags in shaft process by means of radiotracers R. Burek, J .K. Zurawicz: On the optimization of concentration measurements in heterogeneous materials based on β-backscatter measurements B. Heinrich: Analysis of carbon content in crude brown coal by inelastic scattering of neutrons and the method of time correlated associated particles P. Urbańaki, D. Wagner, M. Jankowska, E. Kowalska: Determination of calcium and iron and measurements of ash content in the brown coal H.-W. Thümmel: Some considerations relating to the prediction of the efficiency of radiometric methods for the continuous ash content determination of coal L. Wawrzonek: Monitor of ash content of coal with X-ray source I. Pavlicsek, V. Stenger, A. Veres: Apparatus for gamma activation analysis I. Végvári, I. Juhász: Determination of PbO content of lead-glass samples on the ground of gamma-absorption E. Schöntube, H.-J. Große: Aerosol ionization gas analysis as a monitoring for waste halothane in the atmosphere of operating theatre S. Mothes, P. Popp, G. Oppermann, W.-D. Herberg: Measurement of fluorocarbons with the ECD P. Popp, E. Schöntube, G. Oppermann: The usability of radiation ionization detectors for the determination of N2O concentrations in the air of operating theatres P. Popp, G. Arnold, G. Oppermann: A hydrocarbon-sensitized argon ionization detector for the detection of inorganic compounds R. Szepke, W. Lisieski, J. Harasimczuk: Automatic dust monitor AMIZ G. Vormum: Sealed sources - problems of design, measurement and quality control L. Gąsiorowski: New trends in developments of ratioisotope gauges in Poland G. Brunner: Direct chemical information from special radio tracers as well as from outer X-ray excitation J. Hirling: Experience and future trend in industrial application of nuclear methods in Hungary I. N. Ivanov, O. K. Nikolaenko, Yu. V. Phecktistov, V. L. Chulkin: Use of short-lived nuclides in activation analysis Kl.-P. Rudolph, J. Flachowsky, A. Lange: Trace element determination in semiconducter selenium by neutron activation analysis (NAA) W. Lisieski, J. Mirowicz: Some industrial applications of instruments with neutron sources R. Dybczyński, H. Maleszewaka, S. Sterliński, Z. Szopa, M. Wasek: Some problems in neutron activation determination of gold and silver in ores and concentrates of copper industry L. Jankowski: Cost-benefit aspects of radioisotope application in industry B. Manouchev, T. Boschkova, L. Tsankov, V. Gurev, I. Kojucharov, G. Grozev: On the possibilities of the direct gamma-spectremetry in natural waters P. Morgenstern, D. Müller, W. Riedel: A parallel grid proportional scintillation counter for the X-ray region from 3 to 20 keV with regard to high count rates N. A. Anders, V. S. Isaev, V. I. Filatov, B. E. Kolesnikov, D. Müller, P. Morgenstern, W. Riedel, V. P. Varvaritsa: X-ray fluroescence analyzer of light elements with proportional scintillation counter D. Müller, P. Morgenstern, W. Riedel, W. Warwariza, B. E. Kolesnikow, N. A. Anders, W. J. Filatov: General considerations concerning the use of the X-ray analyzer "RALE" in industry
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  • 68
    Call number: ZSP-201-82/39
    In: CRREL Report, 82-39
    Description / Table of Contents: Observations of a 4.4-m-high brine step in the McMurdo Ice Shelf, Antarctica, show that it has migrated about 1.2 km in 4 years. The present brine wave is overriding an older brine-soaked layer. This migration is proof of the dynamic nature of the step, which is the leading edge of a brine wave that originated at the shelf edge after a major break-out of the McMurdo Ice Shelf. The inland boundary of brine penetration is characterized by a series of descending steps that are believed to represent terminal positions of separate intrusions of brine of similar origin. The inland boundary of brine percolation is probably controlled largely by the depth at which brine encounters the firn/ ice transition (43 m). However, this boundary is not fixed by permeability considerations alone, since measurable movement of brine is still occurring at the inland boundary. Freeze-fractionation of the seawater as it migrates throught the ice shelf preferentially precipitates virtually all sodium sulfate, and concomitant removal of water by freezing in the pore spaces of the infiltrated firm produces residual brines approximately six times more concentrated than the original seawater.
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    Pages: v, 35 Seiten , Illustrationen
    Series Statement: CRREL Report 82-39
    Language: English
    Note: CONTENTS Abstract Preface Introduction Objectives Analytical techniques Radio echo profiling Core drilling Results and discussion Brine infiltration survey Brine layer steps Brine infiltration characteristics Brine infiltration mechanisms at inland boundary Confirmation of brine depths by drilling Density and temperature profiles Ice shelf freeboard Brine upwelling Brine chemistry Conclusions Literature cited
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  • 69
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-82/36
    In: CRREL Report, 82-36
    Description / Table of Contents: Camp construction and drilling activities in 1950 at the East Oumalik drill site in northern Alaska caused extensive degradation of ice-rich, perennially frozen silt and irreversible modification of the upland terrain. In a study of the long-term degradational effects at this site, the near-surface geology was defined by drilling and coring 76 holes (maximum depth of 34 m) in disturbed and undisturbed areas and by laboratory analyses of these cores. Terrain disturbances, including bulldozed roads and excavations, camp structures and off-road vehicle trails, were found to have severely disrupted the site's thermal regime. This led to a thickening of the active layer, melting of the ground ice, thaw subsidence and thaw consolidation of the sediments. Slumps, sediment gravity flows and collapse of materials on slopes bounding thaw depressions expanded the degradation laterally, with thermal and hydraulic erosion removing materials as the depressions widened and deepened with time. Degradational processes became less active after thawed sediments thickened sufficiently to slow the increase in the depth of thaw and permit slope stabilization. The site's terrain is now irregular and hummocky with numerous depressions. Seasonal thaw depths are deeper in disturbed areas than in undisturbed areas and reflect the new moisture conditions and morphology. The severity of disturbance is much greater at East Oumalik than at another old drill site, Fish Creek. The difference results primarily from differences in the physical properties of the sediments, including the quantity and distribution of ground ice.
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    Pages: 42 Seiten , Illustrationen
    Series Statement: CRREL Report 82-36
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Methodology Geologic setting Camp construction and occupation Types of disturbance Degradational processes and the effective area of impact Areal effects of disturbance Topography Groundwater, surface water and drainage Sediment properties and near-surface stratigraphy Surficial processes Depth of thaw Comparison to Fish Creek Discussion and conclusions Literature cited
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  • 70
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    Call number: ZSP-201-83/19
    In: CRREL Report, 83-19
    Description / Table of Contents: Small-scale laboratory experiments were conducted on model bridge piers in the CRREL test basin. The experiments were performed by pushing model ice sheets against structures and monitoring the ice forces during the ice/structure interaction. The parameters, varied during the test program, were the geometry of the bridge piers and the velocity, thickness, and flexural strength of the ice. The results are presented in the form of ice forces on sloping and vertical structures with different geometries. During ice action on sloping structures, a phenomenon of transition of failure mode from bending to crushing was observed as the ice velocity was steadily increased.
    Type of Medium: Series available for loan
    Pages: 17 Seiten , Illustrationen
    Series Statement: CRREL Report 83-19
    Language: English
    Note: CONTENTS Abstract Preface Introduction Tests Results Ice forces on inclined structures Transition of ice action due to velocity increase Aspect ratio Bridge pier nose geometry Conclusions Literature cited
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  • 71
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-83/12
    In: CRREL Report, 83-12
    Description / Table of Contents: This paper documents the development and verification of two finite difference models that solve the general two-dimensional form of the heat conduction equation, using the alternative-direction implicit method. Both can handle convective, constant flux, specified temperature and semi-infinite boundaries. The conducting medium may be composed of many materials. The first program, ADI, solves for the case where no change of state occurs. ADIPC solves for case where a freeze/thaw change of phase may occur, using the apparent heat capacity method. Both models are verified by comparison to analytical results.
    Type of Medium: Series available for loan
    Pages: 74 Seiten , Illustrationen
    Series Statement: CRREL Report 83-12
    Language: English
    Note: CONTENTS Abstract Preface Introduction Finite differences applied to heat transfer Heat conduction equation Boundary conditions Phase change Computer program ADDATA, the data subroutine TRIDIG, the matrix solver ISOTHM, the isotherm finider ADI, main program ADEPC, main program Verification of ADI Comparison of ADI with analytical results Comparison of ADI with experimental results Verification of ADIPC Comparison of ADIPC with analytical results-the Neumann solution Comparison of ADIPC with analytical results-two-dimensional phase change verification User instruction for ADI User instruction for ADIPC Conclusions Literature cited Appendix A. Program INFSUM and sample input and output for program ADI Appendix B. Program ADIPC and sample input and output
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  • 72
    Call number: ZSP-201-83/14
    In: CRREL Report, 83-14
    Description / Table of Contents: An analysis of ice fracture that incorporates dislocation mechanics and linear elastic fracture mechanics is discussed. The derived relationships predict a brittle to ductile transition in polycrystalline ice under tension with a Hall-Petch type dependence of brittle fracture strength on grain size. A uniaxial tensile testing technique, including specimen preparation and loading system design was developed and employed to verify the model. The tensile strength of ice in purely brittle fracture was found to vary with the square root of the reciprocal of grain size, supporting the relationship that the theory suggests. The inherent strength of the ice lattice and the Hall-Petch slope are evaluated and findings discussed in relation to previous results. Monitoring of acoustic emissions was incorporated in the tests, providing insights into the process of microfracture during ice deformation.
    Type of Medium: Series available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: CRREL Report 83-14
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Development of testing technique Test specimens Tensile testing Compression testing Experimental results Tensile tests Compression tests Discussion Conclusions Suggestions for further work Literature cited Appendix A: Additional information on seed grains Appendix B: Thin-sectioning procedure Appendix C: Displacement transducer calibration
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  • 73
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    Call number: ZSP-201-83/16
    In: CRREL Report, 83-16
    Description / Table of Contents: The presence of snow on the ground can impose limitations on the mobility of wheeled and tracked vehicles. Snow depth and density are the two most easily measured snow properties that can be related to mobility over snow. Existing models of snowpack accumulation and ablation processes and models of internal snowpack structure were examined to determine if a model of the snowpack can be developed for use in predicting the snow parameters that affect mobility. Simple models, such as temperature index models, do not provide sufficient snowpack details, and the more detailed models require too many measured inputs. Components of the various models were selected from a basis of a snowpack model for predicting snow properties related to mobility over snow. Methods of obtaining the input data from some components are suggested, and areas where more development is needed are described.
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    Pages: 34 Seiten , Illustrationen
    Series Statement: CRREL Report 83-16
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Conversion of metric units Introduction Review of existing models Accumulation models Ablation models Using existing models for studying mobility Proposed snowpack model for mobility studies Model components Implementation of the model Developing input data Conclusions Literature cited
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  • 74
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    Call number: ZSP-201-83/17
    In: CRREL Report, 83-17
    Description / Table of Contents: A sea ice model was applied to the East Greenland Sea to examine a 60-day ice advance period beginning 1 October 1979. This investigation compares model results using driving geostrophic wind fields derived from three sources. Winds calculated from sea-level pressures obtained from the National Weather Service's operational analysis system resulted in strong velocities concentrated in a narrow band adjacent to the Greenland coast, with moderate velocities elsewhere. The model showed excessive ice transport and thickness build-ups in the coastal region. The extreme pressure gradient parallel to the coast resulted partially from a pressure reduction procedure that was applied to the terrain-following sigma coordinate system to obtain sea-level pressures. Additional sea-level pressure fields were obtained from an independent optimal interpolation analysis that merged FGGE buoys drifting in the Arctic basin with high latitude land stations and from manual digitization of the NWS hand-analyzed Northern Hemisphere Surface Charts. Modeling results using winds from both of these fields agreed favorably.
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    Pages: 19 Seiten , Illustrationen
    Series Statement: CRREL Report 83-17
    Language: English
    Note: CONTENTS Abstract Preface Introduction Description of study Model results The problem Conclusions Literature cited
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  • 75
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    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 42351 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 206 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
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  • 76
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-84/2
    In: CRREL Report, 84-2
    Description / Table of Contents: Investigations of the in situ complex dielectric constant of sea ice were made using time-domain spectroscopy. It was found that (1) for sea ice with a preferred horizontal crystal c-axis alignment, the anisotropy of polarizing properties of the ice increased with depth, (2) brine inclusion conductivity increased with decreasing temperature down to about -8 C, at which point the conductivity decreased with decreasing temperature, (3) the DC conductivity of sea ice increased with increasing brine volume, (4) the real part of the complex dielectric constant is strongly dependent upon brine volume but less dependent upon the brine inclusion orientation, (5) the imaginary part of the complex dielectric constant was strongly dependent upon brine inclusion orientation but much less dependent upon brine volume. Because the electromagnetic (EM) properties of sea ice are dependent upon the physical state of the ice, which is continually changing, it appears that only trends in the relationships between the EM properties of natural sea ice and its brine volume and brine inclusion microstructure can be established.
    Type of Medium: Series available for loan
    Pages: vi, 38 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 84-2
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Dielectric properties of sea ice Time-domain spectroscopy measurement Laboratory measurements Field measurements Analysis of ladder data Conductivity of brine and sea ice Complex dielectric constant of brine and sea ice Discussion and conclusions Literature cited
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  • 77
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    Call number: ZSP-201-84/3
    In: CRREL Report, 84-3
    Description / Table of Contents: The results of resistance tests in level ice and broken ice channels are presented for two models of the WTGB 140-fticebreaker at scales of 1:10 and 1:24, respectively. No scale effect on the resistance in level ice could be detected between the two models. From the test results an empirical predictor equation for the full scale ice resistance is derived. Predicted resistance is compared against, and found to be 25 to 40% larger than, available full-scale values estimated from thrust measurements during full-scale trials of the Great Lakes icebreaker Katmai Bay.
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    Pages: v, 25 Seiten , Illustrationen
    Series Statement: CRREL Report 84-3
    Language: English
    Note: COTENTS Abstract Preface Nomenclature Introduction Model characteristics and test conditions Ice-hull coefficient of friction Measurements of ice properties Experimental procedures Data acquisition system Test program and procedures for 1:10 model Test program and procedures for 1:24 model Analysis of test results Comparison of test results between 1:10 and 1:24 models Analysis of tests in broken or brash-filled ice channels Analysis of tests in level ice Full-scale prediction of level ice resistance Conclusions Literature cited
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  • 78
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    Call number: ZSP-201-84/4
    In: CRREL Report, 84-4
    Description / Table of Contents: Ice problems developed in the Sault Ste. Marie, Michigan, portion of the St. Marys River because of winter navigation. Passing ships and natural influences moved ice from Soo Harbor into Little Rapids Cut in sufficient quantities to jam, cause high water in the harbor, and prevent further ship passage. After physical model and engineering studies, two ice booms with a total span of 1375 ft (419 m) with a 250-ft (76-m) navigation opening between were installed at the head of Little Rapids Cut in 1975. A modest field study program on the booms was conducted for the ensuring four winters to determine ice and boom interaction and the effects of ship passages on the system. Forces on some anchors were recorded and supplemental data were taken by local personnel. Several reports have been written about the booms' early operations. This paper presents four-year summary of the main effects of the booms on ice and ship interaction and vice versa. Throughout the four winter seasons, the small quantities of ice lost over and between the booms were manageable. Ships usually passed through the boom without influencing the boom force levels, but at time they brought about large changes. One boom needed strengthening, and artificial islands were added for upstream ice stability. Coast Guard icebreakers were also a necessary part of winter navigation in this area.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 84-4
    Language: English
    Note: CONTENTS Abstract Preface Introduction St. Marys River Ice problems Remedial measures Field studies Highlights, trends, and major findings Modifications to boom Maximum forces Ship traffic Characteristics Effect of boom forces Effect on ice Conclusion Literature cited Appendix A: Ice boom forces
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  • 79
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-84/6
    In: CRREL Report, 84-6
    Description / Table of Contents: An expression relating aerosol growth to cold environmental conditions was developed. This was accomplished by solving the diffusion equation with the method of Laplace transformation. The series solution was expressed in terms of the dimensionless parameters K (ratio of vapor density over droplet surface to droplet density), ω (ratio of environmental vapor density at time zero to vapor density over droplet surface), and dimensionless time τ (ratio of product of diffusion coefficient D and time t to square of initial radius of condensation nucleus). To take into account the variation of the vapor density over the surface of an acidic condensation nucleus due to the continuous dilution of the droplet, the solution was obtained by assuming various levels of constant vapor concentration. The final expression [R/R sub o - 1 = 2.4917 x 10 to the minus 18th power) exp(0.0737 θ) (P sub RHS/25) x (100-P sub RHS) τ to the 0.9890 powder] can be used to compute the value of R once the values of initial radius R sub o, relative humidity P sub RH, percent of relative humidity at the droplet surface P sub RHS, and environmental temperature θ are given.
    Type of Medium: Series available for loan
    Pages: vi, 28 Seiten , Illustrationen
    Series Statement: CRREL Report 84-6
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature General background The problem Method of solution Results and discussion Conclusions Literature cited Appendix: Evaluation of rn's in equation 25
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  • 80
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/7
    In: CRREL Report, 84-7
    Description / Table of Contents: Experiments were conducted in CRREL's refrigerated flume facility to examine the two-dimensional force distribution of a floating, fragmented ice cover restrained by a boom in a simulated river channel. To determine the force distribution, a vertically walled channel, instrumented for measuring normal and tangential forces, and an instrumented restraining boom were installed in a 40.0- by 1.3-m flume. Two sizes of polyethylene blocks and two similar sizes of fresh-water ice blocks were tested using water velocities ranging from 10 to 30 cm/s. The forces measured at the instrumented boom leveled off with increasing cover length. The contribution of the increasing shear forces developed along theshorelines to this leveling off in the data was clearly evident. The shear coefficients of the polyethylene blocks averaged 0.43, and the freshwater ice averaged 0.044. The normal force measured along the instrumented shoreline could not be related simply by a K coefficient to the longitudinal force; another expression was required, with a term being a function of the cover thickness and independent of the undercover shear stress or cover length. By adding this term, good agreement was then found between the measured and predicted values of the boom forces and the shoreline normal and shear forces
    Type of Medium: Series available for loan
    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 84-7
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experiments Test flume facility Experimental apparatus Experimental procedure Results Plastic versus freshwater ice Shoreline forces Boom forces Average shear stress under ice cover Internal forces Discussion Data scatter Summary and conclusions Literature cited Appendix A: Experimental results
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  • 81
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/8
    In: CRREL Report, 84-8
    Description / Table of Contents: This report describes the equipment and procedures that were used for acquiring, preparing and testing samples of multi-year sea ice. Techniques and procedures are discussed for testing ice samples in compression and tension at constant strain rates and constant loads, as well as in a conventional triaxial cell. A detailed account is given of the application and measurement of forces and dispiacements on the ice test specimens under these different loading conditions.
    Type of Medium: Series available for loan
    Pages: iv, 43 Seiten , Illustrationen
    Series Statement: CRREL Report 84-8
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test material and test specimens Test material Required dimensions for test specimens Acquisition and preparation of specimens Field core sampling Specimen preparation in the laboratory Application of forces and displacements to uniaxial specimens Compression Tension Squareness imperfections Loading devices Universal testing machine Gas actuator for constant load Weight-and-pulley system for constant tension Equipment for triaxial tests Measurement of force and displacement Force Displacement Readouts and recorders Literature cited Appendix A: Phenolic-resin end caps Appendix B: Compliant platens Appendix C: Theoretical factor for converting overall strain to gauge-length strain indumbbell specimens Appci dix D: Items developed but not used in Phase I Appendix E: Use of the Brazil test
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  • 82
    Monograph available for loan
    Monograph available for loan
    Silver Spring : Central Pacific Hurricane Center
    Call number: MOP 45480
    Type of Medium: Monograph available for loan
    Pages: V, 137 Seiten
    Language: English
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  • 83
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : National Advisory Committee on Oceans and Atmosphere
    Call number: MOP 45479 / Mitte
    Type of Medium: Monograph available for loan
    Pages: II, 28 Seiten
    Language: English
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  • 84
    Call number: MOP 45321 / Mitte
    In: Antarctic research activities of the German Democratic Republic
    Type of Medium: Monograph available for loan
    Pages: 15 Seiten
    Series Statement: Antarctic research activities of the German Democratic Republic : report to SCAR No 2
    Language: English
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  • 85
    Call number: MOP 45321 / Mitte
    In: Antarctic research activities of the German Democratic Republic
    Type of Medium: Monograph available for loan
    Pages: 13 Seiten
    Series Statement: Antarctic research activities of the German Democratic Republic : report to SCAR No 3
    Language: English
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  • 86
    Call number: MOP 45321 / Mitte
    In: Antarctic research activities of the German Democratic Republic
    Type of Medium: Monograph available for loan
    Series Statement: Antarctic research activities of the German Democratic Republic : report to SCAR No 4
    Language: English
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  • 87
    Call number: MOP 45321 / Mitte
    In: Antarctic research activities of the German Democratic Republic
    Type of Medium: Monograph available for loan
    Series Statement: Antarctic research activities of the German Democratic Republic : report to SCAR No 5
    Language: English
    Location: MOP - must be ordered
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  • 88
    Call number: ZSP-980-71
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Part 3, 98 to 155
    In: ZfI-Mitteilungen, Nr. 71
    Type of Medium: Series available for loan
    Pages: 368 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 71
    Language: English
    Note: Contents of Part 3 P. Popp, J. Leonhardt: Characterization of coulometric and hypercoulometric ECD mode of operation D. Hinneburg, H.-J. Grosse, J. Leonhardt, P. Popp: Calculation of current-voltage characteristics of electron-capture detectors A.G. Rozno, V.V. Gromov: Study of volume electric charge in radioactive dielectrics by the method of "acoustic sounding" Iv. N. Pandev, M.G. Christova, St.D. Stefanov, N.V. Gentchev, St.T. Bakardjiev, D.T. Genov, Ch.D. Christov: Portable gamma-irradiator - modified model P. Hargittai, V. Stenger: Planning of dose-rate distribution of radiation fields by computer M. Remer: DOSKMF2 - A contribution to the computer-aided design of dose rate distributions A. Heger, H. Dorschner, W. Schumann, D. Pleul: Characterization of the radiation field and control of the optimal electron beam accelerator operation for industrial processes V. Prenerov, K. Shivarov, P. Ivanov: Programme for radiation protection by using portable defectoscopes in industrial building T. Geßner, K. Irmer: Nuclear radiation detectors using high resistivity neutron transmutation doped silicon H.-G. Könnecke, D. Luther: The influence of airing systems on the residence time in biological clarification plants J. Dermietzel, C. Wienhold, H. Grundmann, A. Staschok, J. Koch, E. Bordes: Tracer studies on carbon monoxide and carbon dioxide formation in liquid phase oxidation of p-xylene W. Smułek: Use of technical mixtures of carboxylic acids to the extraction of silver H. Förster: Determination of oxide film thickness on aluminium using 14-MeV neutron activation and BET method H. Jaskólska, L. Waliś, C. Janusz: Investigations of the monocrystallization process of neodymium doped YAG using radiotracers H. Wagler: Substoichiometric determination of Pd-II-traces with dithizone and problems of determination P. Tábor, L. Molnár, D. Nagymihá!yi: Radioisotope gauge for automatic control of cottonwool package H.-W. Thummel, G. Körner, D. Fritzsche: Compensation for thickness variations in determining the bulk material composition on conveyor belts using combined scatter-transmission and thickness measuring methods D. Fritzsche, W. Dolak: Radiometric determination of ash content of raw lignites M. Braune: A simplified mathematical model for scattered transmission of X-rays in raw brown coal P. S. Kamenov, E. I. Vapirev, S. I. Ormandjiev: A new type of nuclear weighing device for transporter belts W. Smulek, M. Borkowski: Separation of reduced molybdenum from fission products. The Mo - HN03 - HDEHP system J. Komosiński, M. Radwan: Selected problems of radioisotope technique for wear investigation of precise elements Dr. A. Várkonyi: The thin layer activation for industry G. Hartmann, P. Kulicke: Wear testing in power stations J. Kraś, Z. Banasik: The radioisotopes in wear investigation of combustion engines H.-D. Grohmann: Short-time measurements of wear on surface activated rails G.M. Ter-Akopian, E.A. Sokol, Fam Ngok Chyong, M.P. Ivanov, L.P. Chelnokov, V.I. Smirnov, V.A. Gorshkov: Neutron multiplicity detector for the study of rare nuclear decay events L. Gąsiorowski, P. Mroziński, K. Sobkowicz, F. Zrudelny: Implementation of Intel 8080 - based microcomputer system in the radioisotope measurements control instrumentation W. Birkholz, M. Steinert: Evaluation of autoradiograms using a microcomputer F. Myšák, M. Krejči, J. Hakl, E. Smrkovský: Study of boron diffusion in high temperature Ni-base alloys by means of solid state track detectors W. Birkholz, H.-Ch. Treutler, K. Freyer, M. Geisler, J. Dubnack: Autoradiography of gallium in silicon H.C. Treutler, K. Freyer: On quantitative autoradiography of semiconductor basic material A.S. Shtan': Radiation evaluation techniques and facilities used for quality assurance of fuel elements and fuel assemblies for nuclear power plants D. Babić, A. Šafranj, V. Marković: Radiation degradation of poly-propylene-molecular weight and melt viscosity change A. Ciszek: Modern irradiation processes equipment-accelerators and their applications G. Kummer: Identification of signals by means of the decision theory N.S. Batchvarov, I.D. Vankov, L.P. Dimitrov, Ch.D. Shukov, P.A. Pavlov: Betareflektometer SR-77
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  • 89
    Call number: AWI G7-19-92930
    In: Glacier mass balance bulletin, No. 7
    Type of Medium: Series available for loan
    Pages: 87 Seiten , Illustrationen
    Series Statement: Glacier mass balance bulletin 7
    Language: English
    Note: CONTENTS 1. INTRODUCTION 2. SUMMARY DATA 2.1 SUMMARY TABLE (NET BALANCE, ELA, ELA0, AAR, AAR0) 2.2 CUMULATIVE SPECIFIC NET BALANCE GRAPHS 3. EXTENSIVE INFORMATION 3.1 WHITE (CANADA) 3.1.1 Topography and observational network 3.1.2 Net balance maps 1999/2000 and 2000/2001 3.1.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.1.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.2 PEYTO (CANADA) 3.2.1 Topography and observational network 3.2.2 Net balance maps 1999/2000 and 2000/2001 3.2.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.2.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.3 ZONGO (BOLIVIA) 3.3.1 Topography and observational network 3.3.2 Net balance maps 1999/2000 and 2000/2001 3.3.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.3.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.4 WALDEMARBREEN (NORWAY/SVALBARD) 3.4.1 Topography and observational network 3.4.2 Net balance maps 1999/2000 and 2000/2001 3.4.3 Net balance altitude (1999/2000 and 2000/2001) 3.4.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.5 NIGARDSBREEN (NORWAY) 3.5.1 Topography and observational network 3.5.2 Net balance maps 1999/2000 and 2000/2001 3.5.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.5.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.6 STORGLACIÄREN (SWEDEN) 3.6.1 Topography and observational network 3.6.2 Net balance maps 1999/2000 and 2000/2001 3.6.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.6.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.7 VERNAGTFERNER (AUSTRIA) 3.7.1 Topography and observational network 3.7.2 Net balance maps 1999/2000 and 2000/2001 3.7.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.7.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.8 DJANKUAT (RUSSIA) 57 3.8.1 Topography and observational network 3.8.2 Net balance map 2000/2001 3.8.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.8.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.9 TSENTRALNIY TUYUKSUYSKIY (KAZAKHSTAN) 3.9.1 Topography and observational network 3.9.2 Net balance maps 1999/2000 and 2000/2001 3.9.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.9.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.10 MALIYAKTRU (RUSSIA) 3.10.1 Topography and observational network 3.10.2 Net balance maps 1999/2000 and 2000/2001 3.10.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.10.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.11 URUMQIHE S. NO. 1 (CHINA) 3.11.1 Topography and observational network 3.11.2 Net balance maps 1999/2000 and 2000/2001 3.11.3 Net balance versus altitude (1999/2000 and 2000/2001) 3.11.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 4. FINAL REMARKS AND ACKNOWLEDGEMENTS 5. PRINCIPAL INVESTIGATORS AND NATIONAL CORRESPONDENTS 5.1 PRINCIPAL INVESTIGATORS 5.2 NATIONAL CORRESPONDENTS OF WGMS
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  • 90
    Call number: M 19.92943
    Type of Medium: Dissertations
    Pages: ix, 192 Seiten , Illustrationen
    ISBN: 90-9018106-7
    Language: English
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  • 91
    Monograph available for loan
    Monograph available for loan
    Hamburg : Deutscher Wetterdienst
    Associated volumes
    Call number: MOP 47414(14) / Mitte ; MOP 47414(14) / Mitte
    In: Wetterkundliche Lehrmittel, 14
    Type of Medium: Monograph available for loan
    Pages: 20 Seiten , Illustrationen
    Series Statement: Wetterkundliche Lehrmittel Nr. 14
    Language: German
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 92
    Call number: MOP 42437 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VII, 100 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 93
    Call number: MOP 42148/4 / Mitte
    In: Trudy V Vsesojuznogo meteorologičeskogo s''ezda, Tom IV
    Type of Medium: Monograph available for loan
    Pages: 204 Seiten , Illustrationen
    Series Statement: Trudy V Vsesojuznogo meteorologičeskogo s''ezda 4
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 94
    Call number: MOP 43670 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 112 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 95
    Call number: MOP 40486
    In: Flugklimatologische Übersichten
    Type of Medium: Monograph available for loan
    Edition: 4 Ordner
    Series Statement: Flugklimatologische Übersichten Teil 1-7
    Language: German
    Location: MOP - must be ordered
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  • 96
    Call number: MOP 40486/1-2
    In: Flugklimatologische Übersichten
    Type of Medium: Monograph available for loan
    Edition: 1 Ordner
    Series Statement: Flugklimatologische Übersichten Teil 1-2
    Language: German
    Location: MOP - must be ordered
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  • 97
    Call number: MOP 40486/3-4
    In: Flugklimatologische Übersichten
    Type of Medium: Monograph available for loan
    Edition: 1 Ordner
    Series Statement: Flugklimatologische Übersichten Teil 3-4
    Language: German
    Location: MOP - must be ordered
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  • 98
    Call number: MOP 46138 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 196 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 99
    Monograph available for loan
    Monograph available for loan
    Alma-Ata : Izdatel'stvo "Nauka" Kazachskoj SSR
    Call number: MOP 46038 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 174 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 100
    Call number: MOP 42165 / Mitte
    Type of Medium: Dissertations
    Pages: II, 42 Seiten , graphische Darstellungen
    Language: German
    Note: Inaugural-Dissertation zur Erlangung der Doktorwürde der Hohen Naturwissenschaftlichen Fakultät der Ludwig-Maximilians Universität zu München vorgelegt von Dieter Rühland aus München
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