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  • 1
    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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  • 2
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/43
    In: CRREL Report, 82-43
    Description / Table of Contents: The radar signatures of ice wedges and wedge-like structures have been investigated for a variety of soil conditions. The radar used for this study emitted short sinusoidal pulses of about 10-ns duration with an approximate center frequency of 150 MHz. Most of the ice wedges existed at depths of about 1 m in a variety of silty and sandy soils with both frozen and thawed active layers. The position of the wedges was usually identified from corresponding surface features. An artificial ice wedge in coarse-grained alluvium was also profiled as well as wedge-like structures of fine silt in a coarse-grained glacial outwash. All wedges and wedge-like structures produced a hyperbolic reflection profile except when an active layer of thawed, saturated silt was present which eliminated returns from the wedges. The peaks of the hyper-bolas were sometimes masked by reflections from the permafrost table or other material interfaces, and multiple hyperbolas occurred at some sites. The dielectric constant of the host medium was often calculated from the linear portions of the hyperbolas and the results were verified by laboratory time domain reflectometry measurements per-formed on field samples. In some cases, hyperbolic profiles originated at several meters depth suggesting that deep ice wedges could be detected in areas of cold permafrost.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 82-43
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Objectives and procedures Equipment used Radar TDR Definitions Massive ice Results Artificial wedge: Norwich, Vermont Ice wedges in sand: Fish Creek, Alaska Ice wedges: Prudhoe Bay, Alaska Ice wedges under thawed fine-grained soils: North Slope, Alaska Wedge-like soil structures: Ft. Greely, Alaska TDR measurements Summary and concluding remarks Literature cited Appendix A: Brief discussion of dispersion
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  • 3
    Monograph available for loan
    Monograph available for loan
    London : Macmillan
    Call number: AWI G7-19-92303
    Type of Medium: Monograph available for loan
    Pages: XLIII, 296 Seiten , Illustrationen
    Language: English
    Note: CONTENTS: INTRODUCTION. - VARIATIONS IN CLIMATE. - LIVING GLACIERS AND THEIR MOTIONS. - HOW GLACIERS SCOUR THEIR VALLEYS. - STRIATED STONES AND BouLDER CLAY. - SEASONALLY BANDED CLAYS. - METAMORPHOSED GLACIAL DEPOSITS. - PART I THE PLEISTOCENE ICE AGE. - CHAPTER I PLEISTOCENE GLACIATION IN NORTH AMERICA. - GENERAL FEATURES. - THE DRIFT. - EXTENT OF PLEISTOCENE GLACIATION. - DIFFERENCES IN CLIMATE DURING THE ICE AGE. - THE CORDILLERAN ICE SHEET. - THE KEEWATIN ICE SHEET. - THE LABRADOREAN ICE SHEET. - CONDITIONS SOUTH OF THE MAIN ICE SHEETS. - INTERGLACIAL PERIODS IN AMERICA. - TORONTO AND MOOSE RIVER INTERGLACIAL FORMATIONS. - GLACIATION IN GREENLAND. - REFERENCES. - CHAPTER II THE ICE AGE IN OTHER REGIONS. - GLACIATION IN ICELAND AND SPITZBERGEN. - GLACIATION OF NORTHERN EUROPE. - THE ICE AGE IN THE ALPS. - THE ICE AGE IN ASIA. - THE ICE AGE IN TROPICAL AND SOUTH TEMPERATE LANDS. - GLACIATION IN ANTARCTICA. - THE SLOPE OF THE SURFACE AND THE THICKNESS OF ICE SHEETS. - REFERENCES. - CHAPTER Ill RESULTS OF PLEISTOCENE GLACIATION. - GENERAL CONCLUSIONS. - EFFECTS OF GLACIATION ON LIFE. - PLACES OF REFUGE. - LIFE ON NUNATAKS. - EFFECTS OF ICE SHEETS COMBINED WITH BARRIERS. - ICE SHEETS AND ISOSTASY. - DURATION OF THE PLEISTOCENE ICE AGE. - REFERENCES. - PART II PRE-PLEISTOCENE ICE AGES. - CHAPTER IV CENOZOIC AND MESOZOIC GLACIATION. - PROBABLE TILLITES IN EUROPE. - EOCENE GLACIATION IN NORTH AMERICA. - EOCENE GLACIATION IN ANTARCTICA. - EFFECTS ON LIFE OF THE EOCENE COOLING. - MESOZOIC GLACIATION IN CENTRAL AFRICA. - JURASSIC TILLITES IN NORTH AMERICA. - REFERENCES. - CHAPTER V LATE PALÆOZOIC GLACIATION. - INTRODUCTION. - PERMIAN AND CARBONIFEROUS GLACIATION IN EUROPE. - REFERENCES. - CHAPTER VI PERMO-CARBONIFEROUS GLACIATION IN INDIA. - THE TALCHIRS. - THE SALT RANGE TILLITES. - A VISIT TO THE TALCHlRS. - PERMO-CARBONIFEROUS DEPOSITS IN OTHER PARTS OF ASIA. - EXTENT AND CHARACTER OF THE ASIATIC GLACIATION. - EFFECTS ON LIFE OF THE INDIAN GLACIATION. - REFERENCES. - CHAPTER VII PERMO-CARBONIFEROUS GLACIATION IN AFRICA. - INTRODUCTION. - DWYKA TILLITE IN SOUTHERN CAPE COLONY. - THE DWYKA IN NATAL. - THE DWYKA IN TRANSVAAL. - GLACIAL FEATURES NEAR KIMBERLEY. - EXTENT OF SOUTH AFRICAN GLACIATION. - EFFECTS OF GLACIATION ON THE LIFE OF SOUTH AFRICA. - REFERENCES. - CHAPTER VIII LATE PALÆOZOIC GLACIATION IN AUSTRALIA. - GENERAL FEATURES. - A GLIMPSE OF THE AUSTRALIAN GLACIAL BEDS. - SPECIAL FEATURES OF THE LATE PALÆOZOIC GLACIATION IN AUSTRALIA. - EFFECTS OF THE GLACIATION ON THE FLORA AND FAUNA. - PERMO-CARBONIFEROUS GLACIATION IN NEW ZEALAND. - POSSIBLE GLACIATION IN THE MALAY STATES. - REFERENCES. - CHAPTER IX PERMO-CARBONIFEROUS GLACIATION IN SOUTH AMERICA. - INTRODUCTION. - GLACIAL BEDS IN SÃO PAULO, SOUTHERN BRAZIL. - TILLITES IN STATES SOUTHWEST OF SÃO PAULO. - SUGGESTION OF TILLITE IN URUGUAY. - GLACIATION IN SOUTHEASTERN ARGENTINA. - TILLITES NEAR SAN JUAN IN WESTERN ARGENTINA. - GLACIAL CONGLOMERATES IN BOLIVIA. - PERMO-CARBONIFEROUS GLACIATION IN THE FALKLAND ISLANDS. - AREA AND GENERAL FEATURES OF GLACIATION IN SOUTH AMERICA. - RELATIONS OF THE FLORA AND FAUNA TO GLACIATION. - REFERENCES. - CHAPTER X PERMIAN OR CARBONIFEROUS GLACIATION IN NORTH AMERICA. - BOULDER CONGLOMERATES IN NOVA SCOTIA. - A POSSIBLE PERMIAN MORAINE IN PRINCE EDWARD ISLAND. - THE SQUANTUM TILLITE. - ALASKAN PERMO-CARBONIFEROUS TILLITES. - OTHER POSSIBLE PERMIAN OR CARBONIFEROUS TILLITES. - CORRELATION OF THE LATE PALÆOZOIC GLACIAL DEPOSITS. - EFFECTS ON LIFE OF THE LATE PALÆOZOIC ICE AGE. - REFERENCES. - CHAPTER XI MIDDLE AND EARLY PALÆOZOIC GLACIATION. - DEVONIAN GLACIATION. - SILURIAN GLACIATION. - ORDOVICIAN GLACIATION IN EUROPE. - THE LIMESTONE CONGLOMERATE. - REFERENCES. - CHAPTER XII GLACIATION AT OR JUST BEFORE THE BEGINNING OF THE CAMBRIAN. - EARLY CAMBRIAN OR LATE PRE-CAMBRIAN TILLITES IN EUROFE. - EARLY CAMBRIAN OR LATE PRE-CAMBRIAN BOULDER CONGLOMERATES IN NORTH AMERICA. - EARLY CAMBRIAN GLACIATION IN ASIA. - EARLY CAMBRIAN OR LATE PRE-CAMBRIAN TILLITES IN SOUTH AFRICA. - EARLY CAMBRIAN OR LATE PRE-CAMBRIAN TILLITES IN AUSTRALIA. - REFERENCES. - CHAPTER XIII GLACIATION IN HURONIAN AND EARLIER TIMES. - HURONIAN TILLITES. - OTHER TILLITES WHICH MAY BE HURONIAN. - TIMISKAMIAN OR SUDBURIAN BOULDER CONGLOMERATES. - SEASONAL BANDING IN TIMISKAMIAN OR SUDBURIAN ROCKS. - THE DORÉ CONGLOMERATE. - THE DARWAR BOULDER CONGLOMERATE OF INDIA. - CONCLUSIONS. - REFERENCES. - PART Ill CAUSES OF GLACIATION. - INTRODUCTION. - FEATURES THAT HAVE TO BE ACCOUNTED FOR. - TYPES OF THEORIES PROPOSED TO ACCOUNT FOR ICE AGES. - CHAPTER XIV GEOLOGICAL THEORIES OF ICE AGES. - THE SUPPOSED COOLING OF THE EARTH. - THEORIES CONNECTED WITH CHANGES OF LEVEL. - THE EFFECTS OF DEPRESSION. - THE SUPPOSED DRIFT OF CONTINENTS. - CHANGES IN OCEAN CURRENTS. - REFERENCES. - CHAPTER XV ATMOSPHERIC AND ASTRONOMIC THEORIES. - ATMOSPHERIC CHANGES AS CAUSES OF GLACIATION. - EFFECTS OF CARBON DIOXIDE. - EFFECTS OF VOLCANIC DUST. - CROLL'S THEORY OF CHANGES OF EXCENTRICITY IN THE EARTH'S ORBIT. - DRAYSON'S THEORY OF CHANGES OF ANGLE OF THE EARTH'S TO THE ECLIPTIC. - SHIFTING OF THE EARTH'S AXIS. - CHANGES IN THE RADIATION OF THE SUN. - CHANGES IN THE TEMPERATURE OF SPACE. - CONCLUSIONS. - REFERENCES. - INDEX TO AUTHORS. - GENERAL INDEX.
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  • 4
    Call number: MOP 46647 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VIII, 162 Seiten
    Language: English
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  • 5
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/24
    In: CRREL Report, 82-24
    Description / Table of Contents: Velocity data derived from petroleum industry seismic records from Harrison Bay show that high-velocity material ( or = 2 km/s) interpreted to be ice-bonded permafrost is common. In the eastern part of the bay, the depth to high velocity material increases and velocity decreases in an orderly manner with increasing distance from shore until the layer is no longer apparent. The western part of the bay is less orderly, possibly reflecting a different geological and thermal history. This western part may be an inundated section of the low coastal plain characterized by the region north of Teshekpuk Lake, and could have contained deep thaw lakes, creating low velocity zones. Along some seismic lines, the high-velocity material extends approximately 25 km offshore. Two anomalies have been found which could be associated with rapidly degrading permafrost. One is strong attenuation, which was interpreted as an indication of gas in the shallow deposits. The other is the presence of considerable seismic noise, including identifiable small seismic events. The origin of this noise has not been positively established, and it is proposed that it may indicate that some movement is occurring in the sediments due to thaw.
    Type of Medium: Series available for loan
    Pages: 65 Seiten , Illustrationen
    Series Statement: CRREL Report 82-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods Reading records Refractions Reflections Rayleigh waves Spatial resolution Anomalies Results and discussion Seismic velocity distribution Attenuation Low-level natural seismicity Summary Literature cited Appendix A: Error estimates Appendix B: Velocity profiles Appendix C: Seismic cross sections
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  • 6
    Call number: ZSP-201-82/26
    In: CRREL Report, 82-26
    Description / Table of Contents: The Caribou-Poker Creeks Research Watershed is a small (101.5-sq km) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations within the watershed range from 210 to 826 m, and approximately 28% of its area is underlain by permafrost. Climatic differences between the watershed and Fairbanks are primarily due to the higher elevation of the watershed. Generally the watershed climatic sites are warmer in winter and cooler in summer than Fairbanks. Within the watershed the greatest temperature contrasts exist in winter, when the valley-bottom sites are beneath the regional air temperature inversion, and the higher sites are above it. From May through September the total precipitation averages 270 mm, 1.47 times that received at Fairbanks. The annual precipitation is about 1.7 times that of Fairbanks. The historical precipitation record at Fairbanks indicates that summer precipitation was below the long-term normal in eight of the eleven years of watershed measurements (1969-1980); no climatic extremes occurred during this period. An analysis of annual streamflow data showed an inconsistency of baseflow recessions from year to year. The runoff-rainfall ratio for individual summer storms averaged 0.35 for Caribou Creek. Comparisons of spot discharge measurements of predominantly permafrost and non-permafrost subwatersheds showed that permafrost-dominated watersheds have a much flashier response to precipitation than non-permafrost watersheds. A comparison of the annual flow distribution of the watershed indicated that Caribou Creek has lower summer and higher winter discharges per unit area than the Chena or Salcha Rivers.
    Type of Medium: Series available for loan
    Pages: 42 Seiten , Illustrationen
    Series Statement: CRREL Report 82-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Setting Geology and soils Vegetation Climate Air temperature Precipitation Hydrology Annual and monthly runoff Individual storms Baseflow recessions Spatial flow variability Temporal flow variability Summary and conclusions Literature cited Appendix A: Station histories
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  • 7
    Monograph available for loan
    Monograph available for loan
    Leipzig : Academy of Sciences of the GDR, Central Institute for Isotope and Radiation Research
    Associated volumes
    Call number: AWI G6-19-93042-2
    In: Interregional Training Course on Radiochemistry, [Supplement]
    Type of Medium: Monograph available for loan
    Pages: 88 Seiten , Illustrationen
    Language: English
    Note: Contents Manual 2.2 The relative measurement of aktivity Lectures 1.3 Statistics / H. Baumbach 2.2 Sealed sources / K. Vormum 2.4 Energy dispersive x-ray fluorescence analysis / H.-K. Bothe 3.1 The use of carriers / H. Koch 4.3 Autoradiography / K. Freyer 6.1 Radiometric methods in environmental control / H.-J. Große
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  • 8
    Call number: MOP 46293/B / Mitte
    In: United States Antarctic Research Report to SCAR, No. 24
    Type of Medium: Series available for loan
    Series Statement: United States Antarctic Research Report to SCAR 24
    Language: English
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  • 9
    Call number: MOP 46270 / Mitte
    Type of Medium: Monograph available for loan
    Pages: viii, 545 Seiten , 28 cm
    Language: English
    Note: Prefatory material in French
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  • 10
    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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  • 11
    Call number: AWI A3-19-92361
    Type of Medium: Monograph available for loan
    Pages: IX, 423 Seiten , Illustrationen
    ISBN: 9972-50-015-2
    Language: Spanish , English
    Note: Contenido PREFACIO A LA MEMORIA DE MIA JEAN TEGNER PRESENTACIÓN DE APERTURA Reducción de la vulnerabilidad a episodios de El Niño como parte de la planificación en áreas del desarrollo / STEPHEN BENDER SECCIÓN I - ECOSISTEMA MARINO Aspectos oceanográficos de El Niño 1997-98 y su relación con los recursos pelágicos / OCTAVIO MORÓN Y MIGUEL SARMIENTO El fitoplancton frente a la costa peruana durante El Niño 1997-98 / ELCIRA DELGADO, SONIA SÁNCHEZ, FLOR CHANG, PATRICIA VILLANUEVA Y CÉSAR FERNÁNDEZ Variabilidad del fitoplancton en la bahía de Ancón, Lima- Perú, durante El Niño 1997-98 / NOEMÍ OCHOA Y GABRIELA RUILLÓN Efecto de El Niño en el fitoplancton de la bahía de llo, Moque gua / OLGA GÓMEZ Efectos del evento El Niño 1997-98 sobre la distribución y abundancia de anchoveta (Engraulis ringens) / MARIANO GUTIÉRREZ Fluctuaciones de la ictiofauna pelágica en la región norte-centro del litoral peruano de 1994 a 1998 / MARILÚ BOUCHON, SANDRA CAHUÍN Y MIGUEL ÑIQUEN Los peces como indicadores de El Niño en el ecosistema marino peruano desde 1972 a 1998 / ALBERTINA KAMEYA, MIGUEL LLEELLISH Y LUIS CACCHA El Niño 1997-98 y la reproducción de la merluza Merluccius gayi peruanus en el Perú / ANGEL PEREA, BETSY BUITRÓN Y ENRIQUE MECKLENBURG Tecnología espacial y pesca / ANIBAL DÍAZ Y GUILLERMO HASEMBANK A model for the negative effects of El Niño and La Niña oscillation on marine bivalves: Gari solida from Bahía Independencia, Perú / HANS-JÖRG URBAN Los índices de El Niño y del impacto sobre las comunidades bentónicas / JUAN TARAZONA, WOLF ARNTZ, SONIA VALLE Y TANIA PEÑA Estrategias de vigilancia biológica del evento El Niño / MARIO EDDING Y MARCELA BLANCO Biological impacts ofthe 1997-98 El Niño in the californias: kelp forests were devastated / MIA TEGNER Densidad de Stichaster striatus en la orilla rocosa de Ancón durante El Niño 1997-98 / LEONARDO ROMERO Evaluación poblacional del percebe Pollicipes elegans en las islas Lobos: 1996 y 1998 / MARTÍN QUEVEDO, MANUEL SAMAMÉ, JAVIER CASTRO, JAIME DE LA CRUZ Y JORGE FUPUY La pesca del langostino titíXiphopenaeus riveti en la caleta San José, Lambayeque, Perú / JAVIER CASTRO, MARTÍN QUEVEDO Y JAIME DE LA CRUZ Talla, densidad y distribución de Argopecten purpuratus durante 1998 en la bahía de San Lorenzo, Callao, Perú / JUAN ARGÜELLES Y GLADYS CASTILLO Bases para el estudio de las adaptaciones evolutivas de la biodiversidad frente a El Niño en la costa peruana / GONZALO CASTRO SECCIÓN II - ECOSISTEMA TERRESTRE El Niño y las inundaciones en el noreste argentino / ENRIQUE J. SCHNACK, UBALDO R. COLADO, FERNANDO O. DE FRANCESCO, LUIS C. GARCÍA LOZANO Y JUAN A. SCHNACK El Niño 1997-98 y los bosques secos de la costa norte del Perú, caso Sechura y Tambogrande en Piura / JUAN TORRES Productividad primaria neta durante El Niño 1997-98 en los bosques secos de Piura, Perú / CATERINA CÁRDENAS, JUAN TORRES Y JOEL RODAS Dinámica poolacional de los algarrobales (Prosopis pallida)y El Niño en la costa norte del Perú / SUSANA GUSHIKEN, TANIA ACUÑA Y JUAN TORRES La reforestación con algarrobo en zona desértica de Piura, Perú / JORGE VERA TUDELA, JOSEP TRÍAS, LUIS ALBÁN, GUILLERMO MORALES Y JOSÉ ROMERO Condiciones meteorológicas en los algarrobales del caserío Bella Esperanza (Piura, Perú) durante 1991-1998 / YONEL MENDOZA Y MARÍA VILA Impacto de El Niño sobre los cultivos vegetales y la productividad primaria en la sierra central de Piura / FIDEL TORRES, FLAVIO PEÑA, RAMIRO CRUZ Y EVARISTO GÓMEZ El Niño 1997-1998 y el cultivo de papa en la costa central del Perú / ROLANDO EGÚSQUIZA Y SATURNINO ATAUCUSI Flora vascular en las lomas de Ancón y Carabay llo Lima, Perú durante El Niño 1997-98 / ASUNCIÓN CANO, MÓNICA ARAKAKI, JOSÉ ROQUE, MARÍA l. LA TORRE, NANCY REFULIO Y CÉSAR ARANA Productividad primaria de las plantas anuales durante El Niño 1997-98 en las Lomas de Mejia (Islay, Arequipa-Perú) / CARMELO TALA VERA, PERCY JIMÉNEZ, ALDO ORTEGA, LUIS VILLEGAS Y FRANCISCO VILLASANTE Poblaciones de zancudos en la Provincia Constitucional del Callao durante y después del evento El Niño 1997-98 / ROCÍO MORENO, MARÍA REYES, JOSÉ CHAUCA Y JOSÉ IANNACONE SECCIÓN III - CONSECUENCIAS SOCIO-ECONÓMICA Las reacciones del sector pesquero chileno al evento El Niño 1997-98 / DANIEL SUMAN Impacto de El Niño 1997-98 en la actividad pesquera del departamento de Piura / WILLIAM LEÓN La construcción social de la deforestación en México: los incendios de 1998 en la selva tropical de los Chimalapas / DAVID BARKIN y MIGUEL ÁNGEL GARCÍA Comportamiento del período seco y lluvioso e impactos de El Niño en Panamá / CÉSAR CASTILLO Los múltiples avatares de El Niño / ANNE-MARIE HOCQUENGHEM, EVELYNE MESCLIER Y MARÍA TERESA ORÉ Carta de susceptibilidad al peligro de inundaciones: el caso de las lagunas de Sechura / CARLOS TAVARES, FERNÁN ALAYZA Y JAVIER RAMÍREZ Impacto de El Niño 1997-98 en Lambayeque, Perú / JORGE CHANAMÉ, VíCTOR ALVITRES, JORGE FUPUY Y MIGUEL CORTEZ Uso del SIG en la evaluación de daños en la Carretera Panamericana entre Tumbes y Chiclayo / MOISÉS CASTILLO Y ANTONIO RAMÍREZ Efecto de El Niño 1997-98 sobre la salud en la cuenca de Huaura, Sayán / NELSON PACHECO, DENNY RODRÍGUEZ Y LINO CÁCERES SECCIÓN IV - EL NIÑO EN EL PASADO Reconstrucción del registro histórico de eventos El Niño en el Perú: un estado de avance / LUC ORTLIEB Y ANNE-MARIE HOCQUENGHEM Eventos ENOS como pulso de los océanos datos de anillos de árboles de 7 000 AP y 6 000 AP / JAMES H.L. LAWLER TAMAs, ocurrencia episódica de moluscos tropicales en el norte de Chile y evento El Niño / NURY GUZMÁN AMANDA DÍAZ, LUC ORTLIEB Y MARCELA CLARKE ¿1544, un año de El Niño? / ENRIQUE ANGULO El diluvio de 1891 / HUMBERTO RODRÍGUEZ LISTA DE REVISORES ÍNDICE , In spanischer und englischer Sprache
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  • 12
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/23
    In: CRREL Report, 82-23
    Description / Table of Contents: A direct filtration, water treatment pilot plant was operated on the Kenai River at Soldotna, Alaska, during the summer of 1980. The purpose of the pilot plant operations was to determine the feasibility of the direct filtration process for removal of glacial silt. The major criterion used to determine feasibility was production of water containing less than 1.0 NTU of turbidity. For the range of raw water turbidities encountered (22-34 NTU), the pilot plant testing indicated that direct filtration was feasible and could be considered as an alternative to conventional waiter treatment plants containing sedimentation tanks.
    Type of Medium: Series available for loan
    Pages: 26 Seiten , Illustrationen
    Series Statement: CRREL Report 82-23
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric Introduction Glacial characteristics Water treatment Materials and methods Experimental design Pilot plant intake Hydrocyclone Chemical addition system Flocculation system Filtration system Pilot plant operations Coagulant chemical preparations Flow measurement Sampling Results and discussion Kenai River w ater quality Evaluation of pilot plant testing Performance of pilot plant elements Physical and chem ical variables Conclusions Recommendations Literature cited
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  • 13
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/13
    In: CRREL Report, 82-13
    Description / Table of Contents: Frost heave is analyzed for the common case in which some ice penetrates the soil. In this situation, heave is due to the accumulation of soil-free ice just within the frozen zone, behind a frozen fringe of finite thickness. Heat and mass transport within and across that fringe are crucial processes in the dynamics of heave. This analysis concentrates on activity within the fringe, also connecting that activity to heat and mass flows in the more frozen and unfrozen zones. Each component in a set of governing differential equations is developed from rational physics and thermodynamics, using previous experimental work. It is assumed that the soil ice grows through interconnected interstices; hence it constitutes and can move as a rigid body. When the assumption is translated into mathematical terms, it completes the governing equations. The model resulting from these considerations is a one-dimensional finite element computer program that solves the equations for arbitrary initial and boundary conditions. The model is used to simulate the heave history of a hypothetical soil column frozen unidirectionally and subjected to a surcharge. The results are gratifying in that they predict qualitatively the characteristics of numerous laboratory observations. Some questions about the completeness of the theory remain, and strict verification of the model awaits further experimentation and better parameter identification.
    Type of Medium: Series available for loan
    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 82-13
    Language: English
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  • 14
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/11
    In: CRREL Report, 82-11
    Description / Table of Contents: The purpose of this investigation was to provide data to be used in evaluating the effects of winter navigation on pro­cesses that cause bank erosion. The specific objectives were to document bank conditions and erosion sites along the rivers, to monitor and compare the amounts of winter and summer bank recession and change, and to estimate the amount of recession that occurred prior to winter navigation. Shoreline conditions and bank recession were documented during field surveys each spring and fall. Bank changes were evaluated by comparison to observations from a previous survey. Aerial photointerpretation was done to estimate the amount of bank recession that occurred prior to winter navigation. Three hundred forty-five miles of river shoreline were surveyed. Banks were eroding along 21.5 miles (6.2%). The common types of bank failures were soil falls (sloughing) and block sliding and slumping. The erosion along approxi­mately 15 miles (70%) of the 21.5 miles was occurring along reaches not bordering winter navigation channels.
    Type of Medium: Series available for loan
    Pages: v, 75 Seiten , Illustrationen
    Series Statement: CRREL Report 82-11
    Language: English
    Note: CONTENTS Abstract Preface Introduction Previous investigations Approach Shoreline conditions Bank changes Bank recession before winter navigation St. Marys River Bank changes Bank recession before winter navigation St. Clair River Bank changes Bank recession before winter navigation Detroit River Bank changes Bank recession before winter navigation St. Lawrence River Bank changes Historical bank recession Summary and conclusions Literature cited Appendix A: St. Marys River Appendix B: St. Clair River Appendix C: Detroit River Appendix D: St. Lawrence River
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  • 15
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    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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  • 16
  • 17
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Oxford Universty Press
    Call number: PIK B 130-20-93890
    Type of Medium: Monograph available for loan
    Pages: XV, 244 Seiten , Diagramme , 24 cm
    Edition: Reprinted
    ISBN: 0198296983 , 9780198296980
    Language: English
    Note: Contents: 1:Information, Equilibrium, Efficiency Concepts ; 2:No-Trade Theorems, Asset Pricing, Bubbles ; 3:Market Microstructure Models ; 4:Dynamic Models, Technical Analysis and Volume ; 5:Herding and Informational Cascades ; 6:Crashes, Investigative Herding, Bank Runs
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  • 18
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    Moscow : Academy of Sciences of the USSR, Soviet Committee on Antarctic Research
    Associated volumes
    Call number: MOP 46294 / Mitte
    In: USSR national report to SCAR, No. 24
    Type of Medium: Series available for loan
    Series Statement: USSR national report to SCAR 24
    Language: English
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  • 19
    Call number: MOP 46357 / Mitte
    In: Studies in geophysics
    Type of Medium: Monograph available for loan
    Pages: XIV, 106 Seiten , Illustrationen
    ISBN: 0309032849
    Series Statement: Studies in geophysics
    Language: English
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  • 20
    Monograph available for loan
    Monograph available for loan
    New York, NY : Penguin Books
    Call number: M 21.94577
    Type of Medium: Monograph available for loan
    Pages: XIV, 267 Seiten , Illustrationen
    ISBN: 0142000280 , 9780142000281 , 0670899240
    Language: English
    Location: Upper compact magazine
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  • 21
    Call number: 10.1144/GSL.SP.1982.010.01.01
    In: Special publications / the Geological Society, London, Volume 10
    Description / Table of Contents: This book is a collection of papers on an aspect of plate tectonics of which our understanding is at present limited. In the mid-1970s, prior to the recent phase of IPOD active margin drill- ing, few geologists would have anticipated that at the start of the 1980s so many new questions concerning the nature of tectonic and sedimentary processes in forearc regions would have come to light.
    Type of Medium: 12
    Pages: 1 Online-Ressource (VII, 576 Seiten)
    ISBN: 0632007087
    Series Statement: Special publications / the Geological Society, London 10
    Language: English
    Note: Table of Contents Japan The Shimanto Belt of Japan: Cretaceous-lower Miocene active-margin sedimentation A. Taira, H. Okada,J. H. Whitaker, and A. J. Smith https://doi.org/10.1144/GSL.SP.1982.010.01.01 Sedimentation across the Japan Trench off northern Honshu Island Roland von Huene and Michael A. Arthur https://doi.org/10.1144/GSL.SP.1982.010.01.02 Tectonics of some forearc fold belts in and around the arc-arc crossing area in central Japan Yujiro Ogawa https://doi.org/10.1144/GSL.SP.1982.010.01.03 Forearc geological structure of the Japanese Islands Tsunemasa Shiki and Yoshibumi Misawa https://doi.org/10.1144/GSL.SP.1982.010.01.04 Central America Facies belts of the Middle America Trench and forearc region, southern Mexico: results from Leg 66 DSDP J. Casey Moore, Joel S. Watkins, Kenneth J. McMillen, Stephen B. Bachman, Jeremy K. Leggett, Neil Lundberg, Thomas H. Shipley, Jean-Francois Stephan, Floyd W. Beghtel, Arif Butt, Borys M. Didyk, Nobuaki Niitsuma, Les E. Shephard, and Herbert Stradner https://doi.org/10.1144/GSL.SP.1982.010.01.05 Tectonic processes along the Middle America Trench inner slope Thomas H. Shipley, John W. Ladd, Richard T. Buffler, and Joel S. Watkins https://doi.org/10.1144/GSL.SP.1982.010.01.06 Sedimentation in different tectonic environments of the Middle America Trench, southern Mexico and Guatemala Kenneth J. McMillen, Robert H. Enkeboll, J. Casey Moore, Thomas H. Shipley, and John W. Ladd https://doi.org/10.1144/GSL.SP.1982.010.01.07 A summary of Deep Sea Drilling Project Leg 67 shipboard results from the Mid-America Trench transect off Guatemala Roland von Huene, Jean Aubouin, Jacques Azema, Grant Blackinton, Jerry A. Carter, William T. Coulbourn, Darrel S. Cowan, Joseph A. Curiale, Carlos A. Dengo, Richard W. Faas, William Harrison, Reinhard Hesse, Donald M. Hussong, John W. Ladd, … View all authors https://doi.org/10.1144/GSL.SP.1982.010.01.08 Evolution of the slope landward of the Middle America Trench, Nicoya Peninsula, Costa Rica Neil Lundberg https://doi.org/10.1144/GSL.SP.1982.010.01.9 South America Cenozoic structure, stratigraphy and tectonics of the central Peru forearc L. D. Kulm, T. M. Thornburg, and H.-J. Schrader J. M. Resig https://doi.org/10.1144/GSL.SP.1982.010.01.10 Forearc and other basins, continental margin of northern and southern Peru and adjacent Ecuador and Chile R. Moberly, G. L. Shepherd, and W. T. Coulbourn https://doi.org/10.1144/GSL.SP.1982.010.01.11 The geology of the western part of the Borbón Basin, North-west Ecuador C. D. R. Evans and J. E. Whittaker https://doi.org/10.1144/GSL.SP.1982.010.01.12 Aleutians Ancient plate boundaries in the Bering Sea region M. S. Marlow, A. K. Cooper, D. W. Scholl, and H. McLean https://doi.org/10.1144/GSL.SP.1982.010.01.13 The Chugach Terrane, a Cretaceous trench-fill deposit, southern Alaska Tor H. Nilsen and Gian G. Zuffa https://doi.org/10.1144/GSL.SP.1982.010.01.14 Structural evolution of coherent terranes in the Ghost Rocks Formation, Kodiak Island, Alaska Tim Byrne https://doi.org/10.1144/GSL.SP.1982.010.01.15 Asia and Australasia Sedimentation in the Sunda Trench and forearc region Gregory F. Moore, Joseph R. Curray, and Frans J. Emmel https://doi.org/10.1144/GSL.SP.1982.010.01.16 Development of the North Island Subduction System, New Zealand Gerrit J. van der Lingen https://doi.org/10.1144/GSL.SP.1982.010.01.17 Atlantic The Barbados Ridge Complex: tectonics of a mature forearc system G. K. Westbrook https://doi.org/10.1144/GSL.SP.1982.010.01.18 Sedimentology and structure of the Scotland Group, Barbados C. J. Pudsey and H. G. Reading https://doi.org/10.1144/GSL.SP.1982.010.01.19 Subduction and tectonics on the continental margin off northern Spain: observations with the submersible Cyana Jacques-André Malod, Gilbert Boillot, Claude Lepvier, Georges Mascle, and Josette Taugourdeau-Lantz Raymond Capdevila, Pierre-Alain Dupeuble, and Carla Müller https://doi.org/10.1144/GSL.SP.1982.010.01.20 Mediterranean Subduction in the Hellenic Trench: probable role of a thick evaporitic layer based on Seabeam and submersible studies X. Le Pichon, P. Huchon, J. Angelier, N. Lybéris, J. Boulin, and D. Bureau J.P. Cadet, J. Dercourt, G. Glaçon, H. Got, D. Karig, J. Mascle, L.E. Ricou, and F. Thiebault https://doi.org/10.1144/GSL.SP.1982.010.01.21 Detailed tectonic trends on the central part of the Hellenic Outer Ridge and in the Hellenic Trench System N. H. Kenyon, R. H. Belderson, and A. H. Stride https://doi.org/10.1144/GSL.SP.1982.010.01.22 The structure of the Calabro-Sicilian Arc: result of a post-orogenic intra-plate deformation Forese Carlo Wezel https://doi.org/10.1144/GSL.SP.1982.010.01.23 Makran of Iran and Pakistan Deformation of the Makran accretionary sediment prism in the Gulf of Oman (north-west Indian Ocean) Robert S. White https://doi.org/10.1144/GSL.SP.1982.010.01.24 The Late Cretaceous-Cenozoic history of western Baluchistan Pakistan—the northern margin of the Makran subduction complex Russell S. Arthurton, Abul Farah, and Wahiduddin Ahmed https://doi.org/10.1144/GSL.SP.1982.010.01.25 The Makran, Southeastern Iran: the anatomy of a convergent plate margin active from Cretaceous to Present G. J. H. McCall and R. G. W. Kidd https://doi.org/10.1144/GSL.SP.1982.010.01.26 California The Coastal Belt of the Franciscan: youngest phase of northern California subduction Steven B. Bachman https://doi.org/10.1144/GSL.SP.1982.010.01.27 The Franciscan Complex of northernmost California: sedimentation and tectonics K. R. Aalto https://doi.org/10.1144/GSL.SP.1982.010.01.28 Sedimentation, metamorphism and tectonic accretion of the Franciscan assemblage of northern California M. C. Blake, Jr, A. S. Jayko, and D. G. Howell https://doi.org/10.1144/GSL.SP.1982.010.01.29 Deformation of partly dewatered and consolidated Franciscan sediments near Piedras Blancas Point, California Darrel S. Cowan https://doi.org/10.1144/GSL.SP.1982.010.01.30 Initiation and evolution of the Great Valley forearc basin of northern and central California, U.S.A. Raymond V. Ingersoll https://doi.org/10.1144/GSL.SP.1982.010.01.31 Forearc Terranes in Orogenic Belts Cretaceous-Palaeogene Flysch Zone of the East Alps and Carpathians: identification and plate-tectonic significance of ‘dormant’ and ‘active’ deep-sea trenches in the Alpine-Carpathian Arc Reinhard Hesse https://doi.org/10.1144/GSL.SP.1982.010.01.32 The anatomy of a Lower Palaeozoic accretionary forearc: the Southern Uplands of Scotland J. K. Leggett W. S. McKerrow and D. M. Casey https://doi.org/10.1144/GSL.SP.1982.010.01.33 Sedimentology, volcanism, structure and metamorphism of the northern margin of a Lower Palaeozoic accretionary complex; Bail Hill-Abington area of the Southern Uplands of Scotland Barry C. Hepworth, Grahame J. H. Oliver, and Michael J. McMurtry https://doi.org/10.1144/GSL.SP.1982.010.01.34 Facies, Petrology and Models Sedimentary facies associations within subduction complexes Michael B. Underwood and Steven B. Bachman https://doi.org/10.1144/GSL.SP.1982.010.01.35 Composition of modern deep-sea sands from arc-related basins J. Barry Maynard, Renzo Valloni, and Ho-Shing Yu https://doi.org/10.1144/GSL.SP.1982.010.01.36 Initiation of subduction zones: implications for arc evolution and ophiolite development D. E. Karig https://doi.org/10.1144/GSL.SP.1982.010.01.37
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  • 22
    Call number: AWI G8-23-95155
    Type of Medium: Monograph available for loan
    Pages: 59 Seiten , Illustrationen
    Language: English
    Note: Contents 1.0 PROGRAM GOALS AND OBJECTIVES 2.0 BACKGROUND 2.1 THE CANADIAN FOREST FIRE DANGER RATING SYSTEM'S FIRE WEATHER lNDEX 2.2 C-BAND SAR BACKSCATTER FROM BURNED BOREAL FORESTS 2.3 C-BAND SAR BACKSCATTER FROM UNBURNED BOREAL FORESTS 2.4 PREVIOUS FIRE-DANGER ANALYSIS USING ERS-SAR DATA 3.0 PROJECT SITE DESCRIPTIONS AND SAMPLING STRATEGY 3.1 STUDY AREA DESCRIPTIONS 3.2 EXPERIMENTAL APPROACH 4.0 RESULTS OF FIELD MEASUREMENTS 4.1 PERMANENT SITES 4.2 SURFACE MOISTURE MEASUREMENTS 5.0 RESULTS OF SAR VERSUS FIRE DANGER CODES 5.1 ANALYSIS OF DONNELLY FLATS SAR BACKSCATTER VERSUS FIRE CODES 5.2 ANALYSIS OF SAR BACKSCATTER FROM 1HE HAJDUKOVICH CREEK 94 BURN VERSUS FIRE DANGER 5.3 COMBINATION OF TOK, HAJDUKOVICH CREEK, AND DONNELLY FLATS BACKSCATTER FOR FIRE DANGER ASSESSMENT 6.0 SUMMARY AND CONCLUSIONS 6.0 OUTREACH ACTIVITIES REFERENCES Figures 1,3,4,5
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  • 23
    Series available for loan
    Series available for loan
    College, Alas. : Division of Geological and Geophysical Surveys
    Call number: AWI G3-23-95009
    Type of Medium: Series available for loan
    Pages: IX,109 Seiten , Illustrationen
    Series Statement: Special report / Division of Geological and Geophysical Surveys 15
    Language: English
    Note: CONTENTS Introduction Sources of information Acknowledgments Physical setting of the Fairbanks area Topography and geology Climate Selected references Frozen ground Seasonally frozen ground Definition The problem Cause of frost heaving Frost action in the Fairbanks area Frost action on pile construction Highway bridges The Alaska Railroad Trans-Alaska Pipeline System Other frost-heave problems Loss of bearing strength Solutions to the frost-action problem Permafrost Definition The problem Origin and thermal regime Distribution and thickness Permafrost in the Fairbanks area Permafrost of the flood plain Permafrost of alluvial fans, colluvial slopes, and silt lowlands Boundaries between permafrost and non permafrost areas Character of ground ice Principles of land use in permafrost areas Ground subsidence caused by thawing of ice-rich permafrost Preliminary statement Thermokarst phenomena General features Therrnokarst mounds Therrnokarst pits Effects on agricultural development Effects on railroads Effects on roads and highways Effects on airfields Effects on heated buildings Effects on natural-gas and oil pipelines General statement Gas pipelines Trans-Alaska Pipeline System Effects on buried utility lines Indicators of permafrost Recognition of the problem Vegetation Small landforms and natural surface patterns Selected references Ground water Preliminary statement Ground water in the Fairbanks area Preliminary statement Tanana and Chena River flood plains Upland hills Lower hillslopes and creek-valley bottoms Geologic hazards associated with ground-water movement in permafrost regions Preliminary statement Artesian wells Icings Seepage icings Stream icings Summary of icings Pingos Selected references Earthquakes Introduction Causes and locations of earthquakes Classification and terminology of earthquakes Earthquake hazards in the Fairbanks area Summary of the earthquake hazard Selected references Landslides Landslides in the Fairbanks area Selected references Hillside erosion in loess Preliminary statement Examples of loess erosion Selected references Flooding Introduction History of flooding in the Fairbanks area Frequency of flooding in the Fairbanks area Solution to the problem of flooding Introduction Structural measures Nonstructural measures Flood proofing Flood warning and evacuation Flood insurance Selected references , Englisch
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  • 24
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/38
    In: CRREL Report, 82-38
    Description / Table of Contents: Extreme cold causes heavy buildup of frost, ice and condensation on many windows. It also increases the incentive for improving the airtightness of windows against heat loss. Our study shows that tightening specifications for Alaskan windows to permit only 30% of the air leakage allowed by current American airtightness standards is economically attractive. We also recommend triple glazing in much of Alaska to avoid window icing in homes and barracks. We base our conclusions on a two-year field study of Alaskan military bases that included recording humidity and temperature data, observing moisture accumulation on windows and measuring airtightness with a fan pressurization device.
    Type of Medium: Series available for loan
    Pages: v, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 82-38
    Language: English
    Note: Contents Abstract Preface Nomenclature Introduction Previous work in cold weather window performance Investigation Data acquisition and analysis Modeling the window thermal regime Moisture and ice observations Airtightness testing and analysis Annual heat loss from air leakage Results and conclusions Moisture on windows Airtightness Airtightness economics Recommendations for windows in extreme cold Airtightness Multiple glazing Literature cited Appendix A: Moisture levels and airtightness Appendix B: Dewpoint data Appendix C: Sample observations of icing
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  • 25
    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.
    Type of Medium: Series available for loan
    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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  • 26
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-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.
    Type of Medium: Series available for loan
    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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  • 27
    Call number: MOP 45206 / Mitte
    In: Daily Global Analyses
    Type of Medium: Monograph available for loan
    Pages: 6, 371 Seiten , graphische Darstellungen
    Series Statement: Daily Global Analyses Part 4
    Language: English
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  • 28
    Monograph available for loan
    Monograph available for loan
    Geneva : United Nations Environment Programme
    Call number: MOP 45806 / Mitte
    Type of Medium: Monograph available for loan
    Pages: v, 86 Seiten , Illustrationen, Karten
    Series Statement: UNEP Regional Seas Reports and Studies 12
    Language: English
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  • 29
    Call number: AWI G6-19-92758
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Abstracts of papers
    Type of Medium: Monograph available for loan
    Pages: 167 Seiten
    Language: English
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  • 30
    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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  • 31
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/16
    In: CRREL Report, 82-16
    Description / Table of Contents: Abstract: A dynamic-thermodynamic sea ice model which employs a viscous-plastic constitutive law has been applied to the East Greenland area. The model is run on a 40-km spatial scale at 1/4-day time steps for a 60-day period with forcing data beginning on 1 October 1979. Results tend to verify that the model predicts reasonable thicknesses and velocities within the ice margin. Thermodynamic ice growth produces excessive ice extent, however, probably due to inadequate parameterization of oceanic heat flux. Ice velocities near the free ice edge are also not well simulated, and preliminary investigations attribute this to an improper wind field in this area. A simulation which neglects ice strength, effectively damping ice interaction with itself and allowing no resistance to deformation, produces excessive ice drift toward the coast and results in unrealistic nearshore thicknesses. A dynamics-only simulation produced reasonable results, including a more realistic ice extent, but the need for proper thermodynamics is also apparent. Other simulations verify that ice import from the Arctic Basin, and ice transport due to winds and currents, were also important components in the model studies.
    Type of Medium: Series available for loan
    Pages: v, 40 Seiten , Illustrationen , 29 cm
    Series Statement: CRREL Report 82-16
    Language: English
    Note: CONTENTS Abstract Preface Introduction Model description and application Results and discussion Wind and current fields Standard simulation Thermodynamic simulation Zero ice strength Zero ice import Zero currents Modified currents Zero winds Dynamics simulation Summary and concluding remarks Literature cite
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  • 32
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/14
    In: CRREL Report, 82-14
    Description / Table of Contents: A comparative study was made of design criteria and analytical methods for footings and pile foundations on perma­frost employed in U.S.S.R. Design Code SNiP II-18-76 (1977) and U.S. Army Cold Regions Research and Engineering Laboratory Special Report 80-34 developed in the early 1970's by the U.S. Army Corps of Engineers and published in 1980. The absence of adequate constitutive equations for frozen soils and of rigorous solutions of the boundary prob­lems has made it necessary to incorporate (explicitly or implicitly) various safety factors in the foundation analyses. From the review it is concluded that the principal difference between these practices is in the assessment and application of appropriate values of safety factors, which leads to a substantial discrepancy in the dimensions and cost of footings and pile foundations in permafrost.
    Type of Medium: Series available for loan
    Pages: iv, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 82-14
    Language: English
    Note: CONTENTS Abstract Preface Introduction U.S.S.R. system of standards U.S.S.R. Design Code SNiP 11-18-76 (1977) subsoils and foundations on permafrost General regulations Classification of soils Basic regulations for foundation design Analysis of subsoils and foundations Design of foundations for special soil conditions, and appendices SR 80-34 (1980) design and construction of foundations in areas of deep seasonal frost and permafrost General information Foundation design Conclusions Literature cited
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  • 33
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/12
    In: CRREL Report, 82-12
    Description / Table of Contents: From a high-quality set of velocity, temperature, and humidity profiles collected upwind and downwind of a step change in surface roughness, temperature, and moisture, we have calculated upwind and downwind values of the heat fluxes and friction velocity. The surface change is from smooth to rough; upwind, the sensible heat flux is upward and the latent heat flux is zero; downwind, the surface is well-watered so that the latent heat flux is upward while the sensible heat flux is downward. The downwind latent heat flux in this fetch-limited flow obeys NL=0.08 Rx 0.76 where NL is the latent heat Nusselt number and Rx is the fetch Reynolds number, a parameter for characterizing fetch-limited flows. Because this relation is virtually the same as one found to describe the sensible heat and condensate fluxes over arctic leads, we conclude that the Nusselt numbers nondimensionalizing scalar fluxes are the same for a given fetch Reynolds number when boundary conditions are similar.
    Type of Medium: Series available for loan
    Pages: vii, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 82-12
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Upwind: flux gradient method Downwind: integral method ResulIts Energy budget Latent heat flux Surface stress Downwind humidity profiles Discussion Conclusions Literature cited
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  • 34
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/10
    In: CRREL Report, 82-10
    Description / Table of Contents: Dielectric measurements have been performed on silt and sand samples from permafrost areas using Time Domain Reflectometry. The sample temperatures were varied from +25 °C to -25 °C, and volumetric water content was varied between oven-dry and 0.55 gH2O/cm3. The data were processed for frequencies between 0.1 and 5.0 GHz. The results show a constant K' and a low K' for frequencies up to 1 GHz. A frequency dependence seen on the data above 2 GHz is probably the result of unfrozen, adsorbed water. At moisture levels near saturation at all temperatures, these soils have excellent propagation characteristics for ground-probing radar operating below 0.3 GHz. Massive ice should be easily detectable in permafrost within a few degrees of 0 °C.
    Type of Medium: Series available for loan
    Pages: 7 Seiten , Illustrationen
    Series Statement: CRREL Report 82-10
    Language: English
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  • 35
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/7
    In: CRREL Report, 82-7
    In: Charged dislocation in ice, II.
    Description / Table of Contents: The contribution of electrically charged dislocation motion to dielectric relaxation was studied theoretically. Experimentally obtained data on charge density, dislocation density, and segment length and distribution described in Part I of this series were used to calculate dielectric relaxation spectra. The results indicate that the charged dislocation process can produce the observed audio frequency dielectric relaxation as well as the distribution of spectra.
    Type of Medium: Series available for loan
    Pages: iii, 15 Seiten , Illustrationen
    Series Statement: CRREL Report 82-7
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theoretical development of dielectric relaxation due to charged dislocations Numerical calculations for distributed segment length Discussion Conclusions Literature cited Appendix A. Mosotti type catastrophe by charged dislocation processes
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  • 36
    Call number: MOP 45772/24 / Mitte
    In: South African Antarctic research report to SCAR, No. 24
    Type of Medium: Series available for loan
    Series Statement: South African Antarctic research report to SCAR 24
    Language: English
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  • 37
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/18
    In: CRREL Report, 82-18
    Description / Table of Contents: Snow and ice control on highways has come to rely heavily on the use of sodium chloride to maintain a trafficable surface for unimpeded movement. Empirical approaches have led to a wide range of application rates, some clearly excessive, but justified on the ground of safety and expediency. The combination of environmental degradation from the huge quantities of salt entering the environment, along with the increased cost of salt itself and the cost of its application have spurred the search for more precise knowledge of the proper amount of salt to apply to a pavement, considering a range of environmental, traffic and chemical parameters. Since controlled tests in the field are extremely difficult to make, a circular test track of three test pavements, dense-graded asphaltic concrete (DGA), open-graded asphaltic concrete (DGA) and portland cement concrete (PCC), was constructed in a coldroom. Natural snow and ice were applied to the pavements and an instrumented slipping wheel was driven over the surfaces to generate frictional forces. These forces were measured and then used to evaluate the response to salt application with time for three test temperatures. OGA had the lowest friction values at a temperature near the freezing point, but higher initial values or more rapidly increasing values than DGA and PCC following salt application at the two lower temperatures. Optimum application rate of salt on PCC and DGA lies between 100 and 300 lb/lane mile (LM), and a higher rate resulted in slight or no improvement in friction. DGA showed anomalous results: lower friction for 300 Ib/LM and higher friction for both 100 and 500 Ib/LM.
    Type of Medium: Series available for loan
    Pages: vi, 55 Seiten , Illustrationen
    Series Statement: CRREL Report 82-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Objectives Background Approach Influencing factors Field factors Laboratory Laboratory trafficking tests Force measurement and coefficient of friction Test tire slip Surface friction gauge Test procedure British portable tester Experimental results Conclusions Recommendations Literature cited Appendix A. Test pavements Appendix B. Pennsylvania State University field study Appendix C. Rochester Institute of Technology field study
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  • 38
    Call number: MOP 45579 / Mitte
    In: Topics in current physics, 28
    Type of Medium: Monograph available for loan
    Pages: IX, 152 Seiten , Illustrationen
    ISBN: 3540112294 , 0387112294
    Series Statement: Topics in current physics 28
    Language: English
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  • 39
    Monograph available for loan
    Monograph available for loan
    Minocqua, Wis. : Willow Creek Press
    Call number: AWI P3-20-93959
    Description / Table of Contents: Recent years have seen a phenomenal increase in bear attacks on humans. In Bear vs. Man, writer-photographer Brad Garfield chronicles many of these bear attacks, including dramatic photographs and stories told by victims who survived and companions of those who didn't. Along with these riveting stories, Garfield discusses bear behavior and instincts, and the various reasons for the increase in bear attacks. He instructs readers on the best advice and equipment that can protect a person. During an attack, offers tips on how to behave when traveling in bear country so as not to become a victim, and implores people to respect bears and their habitat. In the final chapter, the author imparts his knowledge of how to photograph bears in the wild while remaining safe and causing no harm to these awesome and powerful animals.
    Type of Medium: Monograph available for loan
    Pages: 192 Seiten , Illustrationen , 26 cm
    ISBN: 978-1-57223-396-6 , 1572233966
    Language: English
    Note: Contents Introduction Why Some Bears Attack Attack - Chris Widrig Warning Signs Attack - Michio Hishino How to Survive a Bear Attack Attack - Terry Everard When Traveling in Bear Country Attack - Mark Matheny Attacks: Are They Increasing? Attack - Glenda Ann Bradley Ned Rasmussen and Gene Moe Hattie Amitnaag and Moses Aliyak Photographing bears Bibliography
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  • 40
    Call number: AWI G3-22-95060
    Type of Medium: Monograph available for loan
    Pages: 676 Seiten , Illustrationen , 27 cm
    ISBN: 1566704618 (alk. paper)
    Series Statement: Advances in soil science
    Language: English
    Note: Contents Section I - Introduction Chapter 1 - Methods for Assessing Soil C Pools / J.M Kimble, R. Lal and R.F Follett Section II - Soil Sampling and Sample Preparation Chapter 2 - Methodology for Sampling and Preparation for Soil Carbon Determination / J.M Kimble, R.B. Grossman and S.E. Samson-Liebig Chapter 3 - Importance of Soil Bulk Density and Methods of Its Measurement / R. Lal and J.M Kimble Chapter 4 - The Effects of Terrain Position and Elevation on Soil C in the Southern Appalachians / P. V Bolstad and J.M Vose Chapter 5 - Approaching "Functional" Soil Organic Matter Pools through Particle-Size Fractionation: Examples for Tropical Soils / C. Feller, J. Balesdent, B. Nicolardot and C. Cerri Chapter 6 - Spatial Variability: Enhancing the Mean Estimate of Organic and Inorganic Carbon in a Sampling Unit / P. Wilding, L.R. Drees and L. C. Nordt Chapter 7 - Assessment of Soil Organic Carbon Using the U.S. Soil Survey / R.B. Grossman, D.S. Harms, D.F. Kingsbury, R.K Shaw and A.B. Jenkins Cbapter 8 - Organic Carbon Methods, Microbial Biomass, Root Biomass and Sampling Design under Development by NRCS / C.D. Franks, J.M Kimble, S.E. Samson-Liebig and TM Sobecki Section III - Assessment of Carbon Pools Chapter 9 - Characterization of Soil Organic Carbon Pools / HH Cheng and J.M Kimble Chapter 10 - Measuring and Comparing Soil Carbon Storage / B.H Ellert, HH Janzen andB. McConkey Chapter 11 - Estimating Total System C in Smallhold Farming Systems of the East African Highlands / P.L. Woomer, NK Karanja, and E.W. Murage Chapter 12 - Assessment and Significance of Labile Organic C Pools in Forest Soils / P.K Khanna, B. Ludwig, J. Bauhus and C. O'Hara Section IV - Assessment and Analytical Techniques Chapter 13 - Interlaboratory Carbon Isotope Measurements on Five Soils / R.F. Follett and E.G. Pruessner Chapter 14 - The Determination of Soil C Pool Sizes and Turnover Rates: Biophysical Fractionation and Tracers / E.A. Paul, SJ Morris and S. Bohm Chapter 15 - Ecozone and Soil Profile Screening for C-Residence Time, Rejuvenation, Bomb 14C Photosynthetic 613C Changes / H W. Scharpenseel, E.M Pfeiffer and P. Becker-Heidmann Chapter 16 - Use of 13C Isotopes to Determine Net Carbon Sequestration in Soil under Ambient and Elevated CO2 / W.R. Horwath, C: van Kessel, U Hartwig and D. Harris Chapter 17 - Methods Using Amino Sugars as Markers for Microbial Residues in Soil / W. Amelung Chapter 18 - Characterization of Soil Organic Matter / C.L. Ping, G.J. Michaelson, X Y Dai and R.J. Candler Chapter 19 - Fractionating Soil in Stable Aggregates Using a Rainfall Simulator / G.C. Starr, R. Lal and J.M Kimble Chapter 20 - Toward an Efficient Method for Measuring Total Organic Carbon Stocks in Forests / G.R. Smith Chapter 21 - Soil Organic Matter Evaluation / R.A. Rossell, J.C. Gasparoni and J.A. Galantini Chapter 22 - The Development of the KMnO4 Oxidation Technique to Determine Labile Carbon in Soil and Its Use in a Carbon Management Index / G. Blair, R. Lefray, A. Whitbread, N Blair and A. Conteh Chapter 23 - Effects of Soil Morphological and Physical Properties on Estimation of Carbon Storage in Arctic Soils / G.J. Michaelson, C.L. Ping and J.M Kimble Chapter 24 - Estimation of Particulate and Total Organic Matter by Weight Loss-on-Ignition / C.A. Camberdella, A.M Gajda, J. W. Doran, B.J. Wienhold and T.A. Kettler Chapter 25 - Use of Near Infrared Spectroscopy to Determine Inorganic and Organic Carbon Fractions in Soil and Litter / B. Ludwig and P.K Khanna Chapter 26 - Development of Rapid Instrumental Methods for Measuring Soil Organic Carbon / G. W. McCarty and J.B. Reeves III Chapter 27 - Soil Quality Evaluations of Alternative and Conventional Management Systems in the Great Plains / A.M Gajda, J. W. Doran, T.A. Kettler, B.J. Wienhold, J.L. Pikul, Jr. and C.A. Cambardella Section V - Soil Erosion and Sedimentation Chapter 28 - 137Cs for Measuring Soil Erosion and Redeposition: Application for Understanding Soil Carbon / J.C. Ritchie Chapter 29 - Assessing the Impact of Erosion on Soil Organic Car\:〉0n Pools and Fluxes / G. C. Starr, R. Lal, JM Kimble and L. Owens Chapter 30 - Assessing Water Erosion Impacts on Soil Carbon Pools and Fluxes / P.A. Jacinthe, R. Lal and JM Kimble Chapter 31 - Soil Organic Carbon Erosion Assessment by Cesium-137 / Y. Hao, R. Lal, L.B. Owens and RC. Izaurralde Section VI - Modeling and Scaling Procedures Chapter 32 - A Simple Model to Estimate Soil Carbon Dynamics at the BOREAS Northern Study Area, Manitoba, Canada / G. Rapalee Chapter 33 - Methods Used to .Create the North American Soil Organic Carbon Digital Database / R. Lacelle, S. Waltman, N Bliss and F. Orozco-Chavez Chapter 34 - Basic Principles for Soil Carbon Sequestration and Calculating Dynamic Country-Level Balances Including Future Scenarios / O. Andren and T Kiitterer Chapter 35 - Examining the Carbon Stocks of Boreal Forest Ecosystems at Stand and Regional Scales / JS. Bhatti, MJ Apps and lL Jiang Chapter 36 - Predicting Broadscale CStores of Woody Detritus from Plot Data / ME. Harmon, 0.N Krankina, M Yatskov and E. Matthews Chapter 37 - Soil C Dynamics: Measurement, Simulation and Site-to-Region Scale-Up / R.C. Izaurralde, Kll Haugen-Kozyra, D.C. Jans, WB. McGill, R.F. Grant and JC. Hiley . Chapter 38 - Some Factors Affecting the Distribution of Carbon in Soils of a Dry land Agricultural System in Southwestern Australia / R.J Harper and R.J. Gilkes Chapter 39 - A National Inventory of Changes in Soil Carbon from National Resources Inventory Data / MD. Eve, K. Paustian, R. Follett and E.T. Elliott Section VII - Economics and Policy Issues Chapter 40 - Assessing the Economics of Carbon Sequestration in Agriculture / L. Tweeten, B. Sohngen and J Hopkins Chapter 41 - Climate Change Policy and the Agricultural Sector / D. Zilberman and D. Sunding Chapter 42 - Approaches to Assessing Carbon Credits and Identifying Trading Mechanisms / A. Manale Section VIII - Synthesis Chapter 43 - Methodological Challenges: Toward Balancing Soil C Pools and Fluxes / R. Lal, JM Kimble and R.F. Follett Index
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  • 41
    Monograph available for loan
    Monograph available for loan
    Leipzig : Academy of Sciences of the GDR, Central Institute for Isotope and Radiation Research
    Associated volumes
    Call number: AWI G6-19-93042-1
    In: Interregional Training Course on Radiochemistry, [Hauptband]
    Type of Medium: Monograph available for loan
    Pages: 248 Seiten , Illustrationen
    Language: English
    Note: Contents Manual 1.1 Beta measurements 1.2 Measurement of the energy spectrum and range of α-radiation with semiconductor detectors 1.3 Error and statistical tests 1.4 Basic experiments of gamma spectroscopy 2.1 Determination of certain elements in sedimental atmospheric dust by x-ray fluorescence analysis 2.2 Calibration and efficiencies (see Supplement) 2.3 Thin-layer chromatographic separation and test of the purity of labelled compounds 2.4 Separation of Thorium-234 from Uranium-238 2.5 Separation of 137Ca/137mBa by precipitation and sorption 3.1 Determination of phosphate by simple isotope dilution analysis and determination of Zn in MgSO4 by substoichiometric isotope dilution analysis 3.2 The Szilard-Chalmers effect 3.3 Determination of the Ag content in slags by instrumental neutron activation analysis 4.1 Isotope exchange of Ethyl Iodide and Sodium Iodide 4.2 Liquid scintillation counting of Carbon-14 and Tritium 4.3 Autoradiography - Demonstration of Autoradiographic techniques Lectures 1.1 Fundamentals of radioactivity / G. K. Vormum 1.2 Interaction of nuclear radiation with matter / G. K. Vormum 1.4 Equations of radioactive decay / G. K. Vormum 1.5 Radiation detectors / M. Geisler 2.1 Radiation spectroscopy / M. Geisler 2.5 Handling of radioisotopes / G. K. Vormum 2.7 Behaviour of radionuclides in very low concentrations / H. Koch 3.6 Particle sources / J. W. Leonhardt 4.2 Tracers in chemical kinetics / J. Dermietzel 4.4 Liquid Scintillation Counting (LSC) / R. Trettin 5.1 Isotopic tracers in biology / H. Hübner 5.2 Low-level counting / R. Trettin 5.4 Basic concepts of radioimmunoassay (RIA) / G. K. Vormum 6.2 Radionuclide generators / R. Otto
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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-201-82/42
    In: CRREL Report, 82-42
    Description / Table of Contents: A high-resolution impulse radar profiling system was evaluated for 1) detecting the existence of sea ice which coring has revealed to exist on the bottom of the Ross Ice Shelf at Site J-9, 2) detecting the preferred horizontal c-axis azi-muthal direction of the sea ice crystals, using the voltage amplitude of the radar reflection from the sea ice bottom, and 3) determining the direction of the currents under an Antarctic ice shelf. A field program was conducted consisting of a surface radar survey on the Ross Ice Shelf at Site J-9 and surface and airborne radar profiling on the McMurdo Ice Shelf. The CRREL impulse radar system, operating at a center frequency of either 80 MHz or 20 MHz, was unable to detect the shelf bottom at Site J-9, which drilling revealed to be 416 m below the snow surface. The radar system was used to profile the McMurdo Ice Shelf both from the snow surface and from the air; a shelf thickness of about 275 m was easily detected. Theoretical considerations indicate that the bulk conductivity of the ice shelf at Site J1-9 was higher than originally anticipated, and this limited the radar sounding depth to about 405 m when operating at a frequency of 20 MHz.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 82-42
    Language: English
    Note: CONTENTS Abstract Introduction Profiling system Theoretical considerations Field program Discussion Literature cited
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  • 43
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/41
    In: CRREL Report, 82-41
    Description / Table of Contents: Many of the important factors influencing the choice of appropriate aquifer test procedures are presented. The concepts of bias, accuracy and spatial variabil­ity are explained. The definitions of a number of aquifer parameters are devel­oped from basic principles demonstrating the underlying assumptions and limita­tions. The parameters considered are: piezometric head, hydraulic conductiv­ity/intrinsic permeability, flow direction, specific discharge magnitude, transmissivity, volumetric flow rate, total porosity, effective porosity, aver­age linear velocity, storage coefficient, specific yield, dispersion coefficient-aquifer dispersivity. For each parameter several techniques are described, evaluated and ranked in terms of perceived potential accuracy, simplicity and value to contaminant transport studies. It must be stressed, however, that the evaluations are based principally upon theoretical grounds, and not upon actual conduct of the described procedures.
    Type of Medium: Series available for loan
    Pages: iv, 111 Seiten , Illustrationen
    Series Statement: CRREL Report 82-41
    Language: English
    Note: CONTENTS Abstrac Preface Introduction Purpose Scope Concept of accuracy Test selection Definition of parameters Piezometric head Use of piezometers Hydraulic conductivity Flow direction Specific discharge magnitude Transmissivity Volumetric flow rate Porosity Average linear velocity Storage coefficient-specific yield Aquifer dispersivity Parameter estimation techniques Piezometric head Hydraulic conductivity Direction and magnitude of specific discharge vector Transmissivity Volumetric flow rate Total porosity Average linear velocity Storage coefficient Specific yield Effective porosity Aquifer dispersivity-dispersion coefficients Conclusions Literature cited
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  • 44
    Call number: MOP 46633 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VII, 221 Seiten
    Language: English
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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-201-82/27
    In: CRREL Report, 82-27
    Description / Table of Contents: Recommendations for economical thicknesses for building insulation result from a study of fuel and construction costs of 12 military installations in Alaska. A comparison between the insulation thickness that a building owner might choose today and what he might choose in 20 years indicates a trend for much thicker insulation in the future. An analysis of how much more expensive a building built today with the thickness that would be appropriate 20 years hence indicates only a small penalty in life-cycle costs for the additional insulation. Therefore, a minimum of R-32 walls and R-62 attics is recommended for most of Alaska.
    Type of Medium: Series available for loan
    Pages: 54 Seiten , Illustrationen
    Series Statement: CRREL Report 82-27
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Summary Introduction Determining economic thicknesses for insulation Background Analysis method for new construction Analysis method for reinsulating existing construction Sensitivity and longevity of the results Sensitivity Longevity Recommendations Saving money vs. saving energy Energy economics conservation Building energy performance standards Conclusion Literature cited Appendix A: Heating system costs Appendix B: Present worth factors Appendix C: Base case and incremental thermal properties Appendix D: LCC comparison graphs for wall and roof systems Appendix E: Cost penalties for energy conservatism Appendix F: Graphic aid for figuring energy savings thermal improvements
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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-201-82/29
    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.
    Type of Medium: Series available for loan
    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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  • 47
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/30
    In: CRREL Report, 82-30
    Description / Table of Contents: Equations are developed that can be used to determine the amount of gas present in sea ice from measurements of the bulk ice density, salinity and temperature in the temperature range o f-2 to -30°C. Conversely these relationships can be used to give the density of sea ice as a function of its temperature and salinity, considering both the presence of gas and of solid salts in the ice. Equations are also given that allow the calculation of the gas and brine volumes in the ice at temperatures other than that at which the bulk density was determined.
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    Pages: 13 Seiten , Illustrationen
    Series Statement: CRREL Report 82-30
    Language: English
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  • 48
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/31
    In: CRREL Report, 82-31
    Description / Table of Contents: Information on sea ice conditions in the Bering Strait and the icefoot formation around Fairway Rock, located in the strait, is presented. Cross-sectional profiles of Fairway Rock and the relief of the icefoot are given along with theoretical analyses of the possible forces active during icefoot formation. It is shown that the ice cover most likely fails in flexure as opposed to crushing or buckling, as the former requires less force. Field observations reveal that the Fairway Rock icefoot is massive, with ridges up to 15 m high, a seaward face only 20 degrees from vertical, and interior ridge slopes averaging 33 degrees. The icefoot is believed to be grounded and its width ranges from less than 10 to over 100 m.
    Type of Medium: Series available for loan
    Pages: 44 Seiten , Illustrationen
    Series Statement: CRREL Report 82-31
    Language: English
    Note: CONTENTS Abstract Preface Introduction Bering Strait Field reconnaissance Estimation of ice forces on Fairway Rock 1. Creep deformation 2. Crushing failure 3. Flexural failure 4. Forces required to form floating or grounded pressure ridges along therock or to pile ice on the beaches 5. Buckling failure Driving forces Angle of internal friction of sea ice Summary Literature cited Appendix A: April 1982 field observations at Fairway Rock
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  • 49
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/33
    In: CRREL Report, 82-33
    Description / Table of Contents: Arctic sea ice is freckled with melt ponds during the ablation season; Antarctic sea ice has few, if any. On the basis of a simple surface heat budget, we investigate the meteorological conditions necessary for the onset of surface melting in an attempt to explain these observations. The low relative humidity associated with the relatively dry winds off the continent and an effective radiation parameter smaller than that characteristic of the Arctic are primarily responsible for the absence of melt features in the Antarctic. Together these require a surface-layer air temperature above 0 C before Antarctic sea ice can melt. A ratio of the bulk transfer coefficients C sub H/C sub E less than 1 also contributes to the dissimilarity in Arctic and Antarctic ablation seasons. The effects of wind speed and of the sea-ice roughness on the absolute values of C sub H and C sub E seem to moderate regional differences, but final assessment of this hypothesis awaits better data, especially from the Antarctic.
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    Pages: 16 Seiten , Illustrationen
    Series Statement: CRREL Report 82-33
    Language: English
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  • 50
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    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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  • 51
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/34
    In: CRREL Report, 82-34
    Description / Table of Contents: The ice discharge through an opening in an ice control structure was documented to be a function of the floe size, ice type, ice floe conditions and vessel direction. The model data for the average ice discharge per vessel transit scaled to prototype values compared favorably with data taken at the St. Marys River ice control structure (ICS). The model results of the force measurements were also consistent with data taken at the St. Marys ICS. The dynamic loading conditions were independent of vessel direction. The dynamic loading to the structure using 3 types of ice (plastic, natural and urea-doped) showed a considerable difference in their means and standard deviations. The urea-doped ice was evaluated for dynamic loading conditions, and reasonable peak values of 3 to 5 times the mean load at each measuring position were recorded, independent of vessel direction. It appears that synthetic random ice floes may be used in model studies where ice discharge through an opening in a structure needs to be documented. This study shows the synthetic random ice floe discharge to fall reasonably within the values obtained for natural ice discharge for both rafted and non-rafted ice fields above the ICS. However, the question of whether synthetic ice can be used for analyzing force distributions and dynamic force loading criteria cannot be fully answered at this time because the load distributions of the synthetic and natural floes appear to differ.
    Type of Medium: Series available for loan
    Pages: 68 Seiten , Illustrationen
    Series Statement: CRREL Report 82-34
    Language: English
    Note: CONTENTS Abstract Preface Introduction Scope of work Ice discharge from Lake Huron into St. Clair River Water velocity profiles at Port Huron Ice conditions Physical model Basis for selection Description Instrumentation Model ice control structure Open water calibration Open water tests Experimental procedures and techniques Ice cover calibration Ice control structure orientation Analysis of ice discharge due to ship transits Natural ice Synthetic ice Forces on the ice control structure Static measurements Dynamic force measurements Potential additional shear stresses Anticipated ice conditions with ICS Conclusions Literature cited Appendix A. Application of model results Appendix B. Suggested additional studies Appendix C. Derivation of ice discharge
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  • 52
    Call number: ZSP-201-82/19
    In: CRREL Report, 82-19
    Description / Table of Contents: Under proper design and management, a forest ecosystem in the central United States should renovate municipal wastewater as long or longer than conventional agricultural systems, especially when design limitations are hydraulic loading rate, heavy metals, P and N. Forest systems require smaller buffer zones than agricultural systems and lower sprinkler pressures. Immature forests are better wastewater renovators than mature forests.
    Type of Medium: Series available for loan
    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 82-19
    Language: English
    Note: CONTENTS Abstract Preface Introduction Forest systems design Pretreatment Distribution systems Public health considerations Buffer zone requirements Toxic effects Public access Hydraulic loading Nutrient uptake and loading Introduction Nitrogen Phosphorus Trace metals Design considerations Hydraulic loading rates Nitrogen loading rates Forest management options Reforestation Existing forest ecosystems Short term rotation plantations Potential long term effects on forest ecosystems Longevity of forest systems Consequences of overloading Soil chemical, physical and hydrologic properties Productivity Summary Literature cited
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  • 53
    Call number: ZSP-201-82/15
    In: CRREL Report, 82-15
    Description / Table of Contents: An experiment is described that demonstrates the balance between the ice and the unfrozen water in a frozen soil as water is removed. Nuclear magnetic resonance (NMR) is used to monitor the unfrozen water content as the soil is dehydrated by a molecular sieve material. Our results show that the unfrozen water content of a Morin clay soil remains constant until the total water content has been reduced to the point where no ice remains in the system. Once the ice is depleted, the unfrozen water content determined by NMR corresponds to the total water content of the soil determined by the weight of water removed by the molecular sieve material. Thus the validity of utilizing NMR in determining unfrozen water contents vs temperature is established.
    Type of Medium: Series available for loan
    Pages: 8 Seiten , Illustrationen
    Series Statement: CRREL Report 82-15
    Language: English
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  • 54
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/9
    In: CRREL Report, 82-9
    Description / Table of Contents: This study deals with the distribution of forces along the converging boundaries of the Port Huron, Michigan, region where unconsolidated ice in Lake Huron is held against wind and water stresses. An experimental basin was built to induce uniform shear stress on the model ice cover by flowing water beneath the ice. The boundary segments, which held the ice cover in the region, were instrumented to measure force in the normal and tangential directions. The distribution of normal forces along the boundary was compared with as distribution derived by using a theoretical model. An ice control structure (ICS) was installed in the basin and experiments were conducted to measure the forces on the ICS and the ice release through the opening in the ICS during simulated ship passages. The experimental results are presented in a nondimensional form. In addition, the force per unit length on the ICS and the area of ice released through its opening were estimated for the expected wind conditions at the Port Huron site.
    Type of Medium: Series available for loan
    Pages: v, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 82-9
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Theoretical models Case 1 Case 2 Case 3 Experimental program Experimental facility Scaling factors Experimental results Analysis of wind data for lower Lake Huron Summary and conclusions Release of ice through the opening of an ICS Ice forces on the ice control structure Ice forces on ice control structure from a large unconsolidated ice cover Literature cited Appendix A. Equation for the stress resultants and velocities of the ice cover Appendix B. Monthly summary of wind data at Port Huron
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  • 55
    Call number: ZSP-201-82/37
    In: CRREL Report, 82-37
    Description / Table of Contents: This report presents a Landsat-derived land cover map of the northwest portion of the Arctic National Wildlife Refuge, Alaska. The report is divided into two parts. The first is devoted to the land cover map with detailed descriptions of the mapping methods and legend. The second part is a description of the study area. The classification system used for the maps is an improvement over existing methods of describing tundra vegetation. It is a comprehensive method of nomenclature that consistently applies the same criteria for all vegetation units. It is applicable for large- and small-scale mapping and is suitable for describing vegetation complexes, which are common in the patterned-ground terrain of the Alaskan Arctic. The system is applicable to Landsat-derived land cover classifications. The description of the study area focuses on five primary terrain types: flat thaw-lake plains, hilly coastal plains, foothills, mountainous terrain, and river flood plains. Topography, landforms, soils and vegetation are described for each terrain type. The report also contains area summaries for the Landsat-derived map categories. The area summaries are generated for the five terrain types and for the 89 townships within the study areas. Two land cover maps at 1:250,000 are included.
    Type of Medium: Series available for loan
    Pages: 68 Seiten , Illustrationen, 2 Karten
    Series Statement: CRREL Report 82-37
    Language: English
    Note: CONTENTS Abstract Preface Foreword Introduction A land cover map of the ANWR study area Legend development Mapping method Results Discussion Description of the ANWR study area General description Description of specific terrain types Conclusions Literature cited Appendix A: Descriptions of Landsat land cover categories for ANWR Appendix B: Area summaries Appendix C: Aproximate equivalent units in several systems of land cover, wetland and vegetation classifications used in northern Alaska Appendix D: Soil taxonomy Appendix E: Summary of principal Landsat land cover categories within the terrain types of the ANWR study area
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  • 56
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Oxford University Press
    Call number: PIK B 190-19-93065
    Description / Table of Contents: In Development as Freedom Amartya Sen explains how in a world of unprecedented increase in overall opulence millions of people living in the Third World are still unfree. Even if they are not technically slaves, they are denied elementary freedoms and remain imprisoned in one way or another by economic poverty, social deprivation, political tyranny or cultural authoritarianism. The main purpose of development is to spread freedom and its `thousand charms` to the unfree citizens. Freedom, Sen persuasively argues, is at once the ultimate goal of social and economic arrangements and the most efficient means of realizing general welfare. Social institutions like markets, political parties, legislatures, the judiciary, and the media contribute to development by enhancing individual freedom and are in turn sustained by social values. Values, institutions, development, and freedom are all closely interrelated, and Sen links them together in an elegant analytical framework. By asking `What is the relation between our collective economic wealth and our individual ability to live as we would like?` and by incorporating individual freedom as a social commitment into his analysis Sen allows economics once again, as it did in the time of Adam Smith, to address the social basis of individual well-being and freedom.
    Type of Medium: Monograph available for loan
    Pages: XVI, 366 Seiten , Diagramme , 20 cm
    ISBN: 0192893300 , 9780192893307
    Series Statement: Oxford University Press paperback
    Language: English
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  • 57
    Call number: MOP 46080 / Mitte
    In: 82-16, Research reports / International Institute for Applied Systems Analysis
    Type of Medium: Series available for loan
    Pages: 59 Seiten , Illustrationen
    ISBN: 3704500364
    Series Statement: Research reports / International Institute for Applied Systems Analysis 82-16
    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-201-82/17
    In: CRREL Report, 82-17
    Description / Table of Contents: Seismic P and SH wave refraction experiments at the NATO RSG-11 test site in Munster Nord, Federal Republic of Germany, reveal the presence of a nearly horizontal, three-layer velocity structure. The upper layer, composed of un­consolidated glacial till, is 1 m thick and has P (compressional) and SH (shear-horizontal) wave velocities of 240 and 165 m s-1. The second layer, made up of similar, more compacted material, is 9.5 m thick, with a P wave velocity of 470 m s-1 and an SH wave velocity of 275 m s-1. The third layer, interpreted as the groundwater table, is located at a depth of 10.5 m and has a P wave velocity of 1590 m s-1. The SH wave velocity of this layer is controlled by the matrix material and is the same as that of the second layer. A single, unreversed observation indicated a fourth layer at a depth of about 20 m, but the existence of this layer remains unconfirmed. The observed fundamental mode Love wave dispersion is in agreement with the theoretical dispersion predicted by the refraction velocities. Computed partial derivatives of phase velocity with respect to shear wave velocity show, for the frequencies observed, that the dispersion confirms the thicknesses and velocities of the two upper layers and is not affected by the deeper structure.
    Type of Medium: Series available for loan
    Pages: iv, 33 Seiten , Illustrationen
    Series Statement: CRREL Report 82-17
    Language: English
    Note: CONTENTS Abstract Preface Introduction Refraction experiments Procedure Equipment Results P waves Low velocity zone SH waves Surface wave experiments Summary and discussion Literature cited Appendix A: P wave refraction data Appendix B: SH wave refraction data. Appendix C: Surface wave dispersion calculations
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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-201-82/8
    In: CRREL Report, 82-8
    Description / Table of Contents: A detailed analysis of methods for calculating the thermal conductivity of soils is presented, and trends in the predic­tions of these methods are compared. The influence of changes in the moisture content on the calculated thermal con­ductivity of a soil (at constant dry density) is shown, as is the sensitivity of this calculated value to changes in dry den­sity or in the soil solids’ thermal conductivity. The methods are evaluated to determine the extent of agreement of their predictions with measured values obtained on soils of known composition and properties. The deviations of the predicted values are determined for soils that are unfrozen or frozen, coarse or fine, unsaturated, saturated or dry. The applicability of each of the methods under various conditions is determined and recommendations are made as to the best method for each condition.
    Type of Medium: Series available for loan
    Pages: vi, 90 Seiten , Illustrationen
    Series Statement: CRREL Report 82-8
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Analysis of methods for calculating thermal conductivity Introduction Influence of moisture content on thermal conductivity Influence of dry density on thermal conductivity Influence of soil solids’ thermal conductivity Comparison of the various methods Evaluation of methods for calculating thermal conductivity Soils data used for evaluation Computer program Applicability of the methods Discussion and conclusions Applicability to unfrozen soils Applicability to frozen soils Applicability to saturated soils Effect of soil mineral composition Applicability to dry soils Summary of applicability of methods Literature cited Appendix A: Properties of some test soils Appendix B: Comparison of thermal conductivity values computed by the various methods and of their deviations from the values measured
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  • 60
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/21
    In: CRREL Report, 82-21
    Description / Table of Contents: The acoustic emission response from fine-grained polycrystalline ice subjected to constant compressive loads was examined. A number of tests were conducted with the nominal stress ranging from 0.8 to 3.67 MPa at a temperature of -5 C. The acoustic emission response was recorded and the data are presented with respect to time and strain. The source of acoustic emissions in ice is considered in terms of the formation of both microfractures and visible fractures that develop without catastrophic failure of the ice. A model to describe the acoustic emission response is developed.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: CRREL Report 82-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Experimental procedures Ice specimens Mechanical test equipment Acoustic emission equipment Data recording Acoustic emission sources in ice Acoustic events and visible fracturing Source mechanisms Tests on ice single crystals General acoustic emission response Analysis of data Transient response Steady-state response Amplitude distribution Combined transient and steady-state response in the time domain Discussion Summary Literature cited
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  • 61
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/1
    In: CRREL Report, 82-1
    Description / Table of Contents: On 27 March 1964 a major earthquake struck Southern Alaska. The city of Anchorage, which contained a large part of Alaska's population, suffered loss of life and destruction of property. The time of the day, the season, and ground conditions were such that loss of life and property was minimized. The frozen ground and the ice on fresh waster bodies responded to the earthquake shocks in a seldom-observable pattern, which was noted and recorded. Changes of sea level and slides into the sea were responsible for waterfront destruction. It is concluded that the main factor that limited structural damage was the frozen state of the ground.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 82-1
    Language: English
    Note: CONTENTS Abstract Preface Abstract of events Earthquakes and frozen ground The response of freshwater ice sheets to earthquake shock The earthquake disturbance in glaciated mountains Disturbed wildlife Tidal waves Summary Literature cited
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  • 62
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/3
    In: CRREL Report, 82-3
    Description / Table of Contents: The conditions that lead to initial breakup of a solid ice on a river due to rapid water level variations are analyzed. The analysis is based on the theory of beams on an elastic foundation. First cracking is assumed to occur when the bending moment induced in the ice cover by the wave exceeds the flexural strength of the ice cover.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 82-3
    Language: English
    Note: CONTENTS Abstract Preface Symbols Introduction Purpose of the study Stating the problem Fracturing of the ice cover due to the passage of surge waves Basic assumptions Derivation of the bending moments Determination of the wave characteristics Deflection of the ice Discussion and field observations Summary Literature cited
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  • 63
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/4
    In: CRREL Report, 82-4
    Description / Table of Contents: Several proposed methods for treating the momentum flux between drifting sea ice and the underlying ocean are interpreted in terms of simple planetary-boundary-layer (PBL) turbulence theory. The classical two-layer approach, in which the solution for a thin surface layer is matched to an Ekman solution for the outer layer, is used to derive several forms of the drag law. These forms range from linear (where stress is proportional to relative speed), through quadratic (where stress is proportional to relative speed squared), to a Rossby-similarity law like that used to express frictional drag on geostrophic wind in the atmosphere. Only formulations which conform with Rossby-similarity scaling are consistent with free-drift data from the 1975 AIDJEX drift station experiment.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 82-4
    Language: English
    Note: CONTENTS Abstract Preface Background Hierarchy of drag laws and simple models The momentum equation for the planetary boundary layer Linear eddy viscosity - the constant stress layer Two-layer eddy viscosity PBL scaling A dimensionless two-layer system A dimensionless two-layer system with modified stress Evaluating the drag laws Rossby similarity parameters and buoyancy effects Discussion Literature cited
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  • 64
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/5
    In: CRREL Report, 82-5
    Description / Table of Contents: The problem of simultaneous heat and mass transfer in a homogeneous snow layer, with one side kept at its initial temperature and the other side with a step temperature increase, was solved for the case of constant through-flow conditions. An experimentally determined effective thermal conductivity function, i.e. Ke = 0.0014 + 0.58 G (where G is dry mass flow rate of air in g/sq cm-s), was employed in the solution. The computed nondimensional temperature distribution agreed quite well with experimental data taken under pseudo-steady state conditions with the exception of the temperature for the lowest flow rate used in the experiment. The pronounced nonlinearity of the temperature distribution was found to be a strong function of the flow rate. For sinusoidal variation of atmospheric pressure, the responding flow in the snow medium was also found to be sinusoidal. In conjunction with the diurnal temperature change, this variation facilitated the process of repeated sublimation and condensation in alternate directions and thereby produced a surface layer of approximately constant snow density.
    Type of Medium: Series available for loan
    Pages: v, 10 Seiten , Illustrationen
    Series Statement: CRREL Report 82-5
    Language: English
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  • 65
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/6
    In: CRREL Report, 82-6
    Description / Table of Contents: The interpretation of continuous radar profiles requires an alternative geophysical means of obtaining ground dielectric information. Ground dielectric properties were measured using wide-angle reflection and refraction (WARR) soundings with a ground-probing radar set that transmits pulses f a few nanoseconds duration. The investigations, carried out over sandy gravel in interior Alaska, provided dielectric data to about a 5-m depth. The WARR soundings were displayed as individual traces allowing interference between separate events and dispersion to be observed, and the soundings were compared with continuous radar and resistivity profiles conducted concurrently to extract the maximum amount of dielectric information. The dielectric constants, derived mainly from the direct ground waves propagating along the surface, ranged from 2.9 to 7.4. Dielectric values interpreted for one site predicted the possibility of a refracted event which may have occurred during one of the soundings.
    Type of Medium: Series available for loan
    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 82-6
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theory of ground wave propagation from a horizontal electric dipole Equipment and methods Results Site 1 Site 2 Site 3 Summary and concluding remarks Literature cited
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  • 66
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: IASS 21.94542
    Type of Medium: Monograph available for loan
    Pages: XI, 370 S , graph. Darst
    Edition: Transferred to digital print.
    ISBN: 0521640830 , 0521646871 , 0521640830
    Language: English
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  • 67
    Call number: MOP 45650 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 49 Seiten
    Language: English
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  • 68
    Call number: 14592
    In: Modern crystallography / Boris K. Vainshtein (ed.-in-chief) ; Vol. 2
    In: Springer series in solid-state sciences ; 21
    Type of Medium: Monograph available for loan
    Pages: XVII, 433 S. , Ill., graph. Darst.
    ISBN: 3540105174 , 0387105174
    Series Statement: Modern crystallography / Boris K. Vainshtein (ed.-in-chief) ; Vol. 2 21
    Language: English
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  • 69
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 70
    Monograph available for loan
    Monograph available for loan
    London u.a. : Allen & Unwin
    Call number: MR 22.94921
    Type of Medium: Monograph available for loan
    Pages: 128 Seiten , zahlreiche Illustrationen
    ISBN: 0-04-551051-2 , 0-04-551052-0
    Language: English
    Note: Preface Acknowledgements 1 Introduction 2 Stress and strain 3 Structural symmetry 4 Structure and stratigraphical succession 5 Structures in brittle rocks: tension fractures and shear zones 6 Rock cleavage and schistosity: generalities 7 Fracture cleavage and strain-slip cleavage 8 Flow cleavage, schistosity and lineation 9 Boudinage 10 Drag-folds and parasitic folds 11 Mullion and rodding structures 12 Superposed minor structures 13 Minor structures and large-scale tectonics 14 Conclusions Bibliography Index
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  • 71
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell Scientific Publications
    Call number: MR 22.94942
    Type of Medium: Monograph available for loan
    Pages: X, 390 Seiten , 1 gefaltetes sheet , Illustrationen, graphische Darstellungen, Karten
    Edition: 3. edition
    ISBN: 0-632-02953-6
    Series Statement: Geoscience texts
    Language: English
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  • 72
    Monograph available for loan
    Monograph available for loan
    Enfield, NH [u.a.] : Science Publishers
    Associated volumes
    Call number: AWI Bio-07-0058
    In: Flora of Siberia / ser. ed.: I. M. Krasnoborov, Vol. 2
    Type of Medium: Monograph available for loan
    Pages: X, 362 S. : Ill., Kt.
    ISBN: 1578081017
    Uniform Title: Flora Sibiri 〈engl.〉
    Language: English
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  • 73
    facet.materialart.
    Unknown
    o.O. : Società Italiana di Mineralogia e Petrologia
    Call number: 93.0020
    Pages: 32 S.
    Language: English
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  • 74
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Longman
    Associated volumes
    Call number: 11/M 94.0299 ; M 93.0253
    In: Rock-forming minerals
    Type of Medium: Monograph available for loan
    Pages: 919 S.
    Edition: 2nd ed
    ISBN: 0582465265
    Classification:
    Mineralogy
    Language: English
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  • 75
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-8
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 20 S. : graph. Darst.
    Series Statement: Berichte zur Polarforschung 8
    Language: English
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  • 76
    Call number: AWI G9-89-0476
    In: International Union of Geological Sciences : Series B, Number 4
    Description / Table of Contents: Antarctic Geoscience is the proceedings volume of the Third Symposium on Antarctic Geology and Geophysics, held in Madison, Wisconsin. The 151 chapters in the book, which include both review papers and original contributions, range over all major fields of geoscience. At a time when interest in Antarctica, its geologic history, and its mineral resource potential is increasing, this book provides the most current and comprehensive overview of the subject. These papers, representing the recent work of many scientists from fifteen nations, offer a balanced assessment of current thought and knowledge concerning the geology and geoscience of Antarctica and the surrounding oceanic regions. Together, they constitute the most up-to-date reference work on Antarctic earth sciences. The book is divided into twelce sections: Gondwanaland (11 chapters), Scotia Arc Region (39, East Antarctica Shield (14), Upper Precambrian-Paleozoic Rocks (11), Paleontology (8), Igneous Rocks (14), Structural Geology and Tectonics (9), Mineral Deposits (4), Crustal Structure (13), Subglacial Morphology (4), Marine Geology (8), and Cenozoic History (16). The volume is generously illustrated with photographs and line drawings and includes a large color geologic map of the continent.
    Type of Medium: Monograph available for loan
    Pages: 1172 Seiten , Illustrationen , 29 cm
    Edition: First printing
    ISBN: 0299084108 , 0-299-08410-8
    Series Statement: International Union of Geological Sciences : Series B Number 4
    Language: English
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  • 77
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley & Sons
    Call number: M 95.0288
    Type of Medium: Monograph available for loan
    Pages: 450 S.
    ISBN: 0471060186
    Classification:
    Geodynamics
    Language: English
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  • 78
    Monograph available for loan
    Monograph available for loan
    New York : Wiley-Interscience
    Call number: M 94.0527
    Type of Medium: Monograph available for loan
    Pages: 450 S.
    ISBN: 0471060186
    Classification:
    Geodynamics
    Language: English
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  • 79
    Call number: AWI A3-02-0061
    In: Advances in global change research, Volume 7
    Type of Medium: Monograph available for loan
    Pages: IX, 343 Seiten , Illustrationen
    ISBN: 0792368010
    Series Statement: Advances in global change research 7
    Language: English
    Note: Table of contents List of contributors Preface A global vegetation index for SeaWiFS: Design and applications / N. Gobron, F, Melin, B. Pinty, M. M. Verstraete, J.-L. Widlowski and G. Bucini Modeling sensible heat flux using estimates of soil and vegetation temperatures: the HEIFE and IMGRASS experiments / Li Jia, Massimo Menenti, Zhongbo Su, Zhao-Liang Li, Vera Djepa and Jiemin Wang Exploitation of Surface Albedo Derived from the Meteosat Data to Characterize Land Surface Changes / Bernard Pinty, Michel M. Verstraete, Nadine Gobron, Fausto Roveda, Yves Govaerts, John V. Martonchik,David J. Diner and Ralph A. Kahn Towards a Climatology of Australian Land Surface Albedo for use in Climate Models / Ian F. Grant Collocated surface and satellite observations as constraints for Earth radiation budget simulations with global climate models / Martin Wild How well do aerosol retrievals from satellites and representation in global circulation models match ground-based AERONET aerosol statistics? / S. Kinne, B. Holben, T. Eck, A. Smirnov, O. Dubovik, I. Slutsker, D. Tanre, G. Zibozdi, U. Lohmann, S. Ghan, R. Easter, M. Chin, P. Ginoux, T. Takemura, I, Tegen, D. Koch, R. Kahn, E. Vermote, L. Stowe, O. Torres, M. Mishchenko, I. Geogdzhayev and A. Hiragushi Remote Sensing of Snow and Characterization of Snow Albedo for Climate Simulations / Anne W. Nolin and Allan Frei Using the Special Sensor Microwave Imager to Monitor Surface Wetness and Temperature / Alan Basist and Claude Williams Snow Cover Fraction in a General Circulation Model / A. Roesch, M. Wild and A. Ohmura Boreal Forest Fire Regimes and Climate Change / B.J. Stocks, B.M. Wotton, M.D. Flannigan, M.A. Fosberg, D.R. Cahoon and J.G. Goldammer Specification of surface characteristics for use in a high resolution regional climate model: on the role of glaciers in the Swiss alps / Stéphane Goyette, Claude Collet and Martin Beniston Using Satellite Data Assimilation to Infer Global Soil Moisture Status and Vegetation Feedback to Climate / Wolfgang Knorr and Jan-Peter Schulz The Use of Remotely-sensed Data for the Estimation of Energy Balance Components in a Mountainous Catchment Area / P.A. Brivio, R. Colombo and M. Meroni Integration of operationally available remote sensing and synoptic data for surface energy balance modelling and environmental applications on the regional scale / Stefan Niemeyer and Jürgen Vogt
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  • 80
    Monograph available for loan
    Monograph available for loan
    Upper Saddle River, NJ : Prentice Hall
    Call number: AWI A5-02-0029
    Type of Medium: Monograph available for loan
    Pages: XII, 484 S. , Ill., graph. Darst., Kt.
    Edition: 8. ed.
    ISBN: 0130879576
    Language: English
    Note: Contents: Preface. - 1 Introduction to the atmosphere. - Weather and climate. - Atmospheric hazards: assault by the elements. - The atmosphere: a part of the earth system. - Earth's four spheres. - Earth's spheres interact. - The carbon cycle. - Composition of the atmosphere. - Major components. - Carbon dioxide. - Variable components. - Ozone depletion - a global issue. - The ozone hole. - Effects of ozone depletion. - Montreal Protocol. - Probing the atmosphere. - Height and structure of the atmosphere. - Pressure changes. - Temperature changes. - Vertical variations in composition. - The ionosphere. - 2 Heating Earth's Surface and Atmosphere. - Earth-Sun Relationships. - Earth's Motions. - The Seasons. - Earth's Orientation. - Solstices and Equinoxes. - Energy, Heat, and Temperature. - Types of Energy. - Heat Energy Versus Temperature. - Mechanisms of Energy Transfer. - Conduction. - Convection. - Radiation. - Laws of Radiation. - The Fate of Incoming Solar Radiation. - Reflection and Scattering. - Absorption by Earth's Surface and Atmosphere. - Radiation Emitted by Earth. - Heating the Atmosphere. - The "Greenhouse Effect". - Role of Clouds in Heating Earth. - Heat Budget. - Latitudinal Heat Balance. - 3 Temperature. - For the Record: Air Temperature Data. - Why Temperatures Vary: The Controls of Temperature. - Land and Water. - Ocean Currents. - Altitude. - Geographic Position. - Cloud Cover and Albedo. - World Distribution of Temperatures. - Cycles of Air Temperature. - Daily Temperature Variations. - Magnitude of Daily Temperature Changes. - Annual Temperature Variations. - Temperature Measurement. - Mechanical Thermometers. - Electrical Thermometers. - Instrument Shelters. - Temperature Scales. - Applications of Temperature Data. - Heating Degree-Days. - Cooling Degree-Days. - Growing Degree-Days. - Temperature and Comfort. - 4 Moisture and Atmospheric Stability. - Movement of Water Through the Atmosphere. - Water's Changes of State. - Water in the Atmosphere. - Vapor Pressure and Saturation. - Relative Humidity. - How Relative Humidity Changes. - Natural Change in Relative Humidity. - Dew Point Temperature. - Humidity Measurement. - Adiabatic Temperature Changes. - Adiabatic Cooling and Condensation. - Lifting Processes. - Orographic Lifting. - Frontal Wedging. - Convergence. - Localized Convective Lifting. - Contents. - The Critical Weathermaker: Atmospheric Stability. - Types of Stability. - Stability and Daily Weather. - How Stability Changes. - Temperature Changes and Stability. - Vertical Air Movement and Stability. - 5 Forms of Condensation and Precipitation. - Condensation. - Condensation Aloft and Cloud Formation. - Clouds. - Cloud Classification. - Cloud Descriptions. - Fog. - Fogs Formed by Cooling. - Fogs Formed by Evaporation. - Dew and Frost. - How Precipitation Forms. - Precipitation from Cold Clouds: The Bergeron Process. - Precipitation from Warm Clouds: The Collision-Coalescence Process. - Forms of Precipitation. - Rain. - Snow. - Sleet and Glaze. - Hail. - Rime. - Precipitation Measurement. - Standard Instruments. - Measuring Snowfall. - Measurement Errors. - Precipitation Measurement by Weather Radar. - Intentional Weather Modification. - Cloud Seeding. - Fog and Cloud Dispersal. - Hail Suppression. - Frost Prevention. - Inadvertent Weather Modification: Urban-Induced Precipitation. - 6 Air Pressure and Winds. - Understanding Air Pressure. - Measuring Air Pressure. - Factors Affecting Air Pressure. - Pressure Changes With Altitude. - Factors Affecting Wind. - Pressure-Gradient Force. - Coriolis Force. - Friction. - Winds Aloft and Geostrophic Flow. - Curved Flow and the Gradient Wind. - Surface Winds. - How Winds Generate Vettical Air Motion. - Vertical Airflow Associated with Cyclones and Anticyclones. - Factors That Promote Vertical Airflow. - Wind Measurement. - 7 Circulation of the Atmosphere. - Scales of Atmospheric Motion. - Large- and Small-Scale Circulation. - Structure of Wind Patterns. - Local Winds. - Land and Sea Breezes. - Mountain and Valley Breezes. - Chinook (Foehn) Winds. - Katabatic (Fall) Winds. - Country Breeze. - Global Circulation. - Single-Cell Circulation Model. - Three-Cell Circulation Model. - Observed Distribution of Pressure and Winds. - Idealized Zonal Pressure Belts. - Semipermanent Pressure Systems: The Real World. - Monsoons. - The Asian Monsoon. - The North American Monsoon. - The Westerlies. - Why Westerlies?. - Jet Streams. - Origin of the Midlatitude Jet Stream. - Subtropical Jet Stream. - Waves in the Westerlies. - Westerlies and Earth's Heat Budget. - Global Winds and Ocean Currents. - The Importance of Ocean Currents. - Ocean Currents and Upwelling. - El Niño and La Niña. - Global Distribution of Precipitation. - Zonal Distribution of Precipitation. - Distribution of Precipitation Over the Continents. - Precipitation Regimes on a Hypothetical Continent. - 8 Air Masses. - What Is an Air Mass?. - Source Regions. - Classifying Air Masses. - Air-Mass Modification. - Properties of North American Air Masses. - Continental Polar (cP) and Continental Arctic (cA) Air Masses. - Lake-Effect Snow: Cold Air Over Warm Water. - Maritime Polar (mP) Air Masses. - Maritime Tropical (mT) Air Masses. - Continental Tropical (eT) Air Masses. - 9 Weather Patterns. - Polar-Front Theory. - Fronts. - Warm Fronts. - Cold Fronts. - Stationary Fronts. - Occluded Fronts. - Drylines. - Life Cycle of a Midlatitude Cyclone. - Formation: The Clash of Two Air Masses. - Development of Cyclonic Flow. - Occlusion: The Beginning of the End. - Idealized Weather of a Midlatitude Cyclone. - Cyclogenesis. - Cyclonic and Anticyclonic Circulation. - Divergence and Convergence Aloft. - Traveling Cyclones. - Patterns of Movement. - Anticyclonic Weather and Blocking Highs. - Case Study of a Midlatitude Cyclone. - Violent Spring Weather. - Weather in Peoria. - 10 Thunderstorms and Tornadoes. - What's in a Name?. - Thunderstorms. - Air-Mass Thunderstorms. - Stages of Development. - Occurrence. - Severe Thunderstorms. - Supercell Thunderstorms. - Squall Lines and Mesoscale Convective Complexes. - Lightning and Thunder. - What Causes Lightning?. - The Lightning Stroke. - Thunder. - Tornadoes. - The Development and Occurrence of Tornadoes. - Tornado Development. - Tornado Climatology. - Profile of a Tornado. - Tornado Destruction. - Tornado Forecasting. - Tornado Watches and Warnings. - Doppler Radar. - 11 Hurricanes. - Profile of a Hurricane. - Hurricane Formation and Decay. - Hurricane Formation. - Hurricane Decay. - Hurricane Destruction . - Storm Surge. - Wind Damage. - Inland Flooding. - Detecting and Tracking Hurricanes. - The Role of Satellites. - Aircraft Reconnaissance. - Radar and Data Buoys. - Hurricane Watches and Warnings. - 12 Weather Analysis and Forecasting. - The Weather Business: A Brief Overview. - Weather Analysis. - Gathering Data. - Weather Maps: Pictures of the Atmosphere. - Weather Forecasting. - Synoptic Weather Forecasting. - Numerical Weather Prediction. - Statistical Methods. - Techniques Used in Short-Range Forecasting. - Long-Range Forecasts. - Forecast Accuracy. - Tools in Weather Forecasting. - Satellites in Weather Forecasting. - What Weather Satellites Reveal. - Measurement by Satellite. - Weather Forecasting and Upper-Level Flow. - The Winter of 1977. - 13 Air Pollution. - A Brief Historical Perspective. - Air Pollution: Not a new Problem. - Some Historic Episodes. - Sources and Types of Air Pollution. - Primary Pollutants. - Secondary Pollutants. - Trends in Air Quality. - Meteorological Factors Affecting Air Pollution. - Wind as a Factor. - The Role of Atmospheric Stability. - Acid Precipitation. - Extent and Potency of Acid Precip
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  • 81
    Call number: PIK N 071-02-0097 ; AWI A3-02-0084
    Type of Medium: Monograph available for loan
    Pages: X, 397 Seiten , Illustrationen , 28 cm
    ISBN: 0521015073
    Language: English
    Note: Contents Foreword Preface Summary for Policymakers Synthesis Report Question 1 Question 2 Question 3 Question 4 Question 5 Question 6 Question 7 Question 8 Question 9 Working Group Summaries Working Group I: The Scientific Basis Working Group II: Impacts, Adaptation, and Vulnerability Working Group III: Mitigation Annexes A. Authors and Expert Reviewers B. Glossary of Terms C. Acronyms, Abbreviations, and Units D. Scientific, Technical, and Socio-Economic Questions Selected by the Panel E. List of Major IPCC Reports
    Location: A 18 - must be ordered
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  • 82
    Call number: AWI A7-92-0314
    Type of Medium: Monograph available for loan
    Pages: IX, 560 S. , graph. Darst., Kt.
    Edition: 1st publ.
    ISBN: 0521252229
    Language: English
    Note: CONTENTS: Foreword. - Introduction. - SESSION I - ATMOSPHERIC GENERAL CIRCULATION MODELS AND CLIMATE SIMULATIONS. - Large-scale climate modelling and small-scale physical processes / J. Smagorinsky. - Simulation of climate by general circulation models with hydrologic cycles / S. Manabe. - Current parameterizations of land-surface processes in atmospheric general circulation models / D. J. Carson. - The sensitivity of numerically simulated climates to land surface conditions / Y. Mintz. - SESSION II - THE MICROPHYSICAL PROCESSES OF MOMENTUM, HEAT AND WATER TRANSFERS ACROSS AND NEAR THE SURFACE OF THE LAND. - Vertical flux of moisture and heat at a bare soil surface / W. H. Brutsaert. - The vertical fluxes of heat and moisture at a vegetated land surface / L. J. Fritschen. - Vertical flux of heat and moisture in snow and ice / M. Kuhn. - SESSION III - MESOSCALE PARAMETERIZATIONS OF THE TRANSFER PROCESSES. - Parameterization of hydrologic processes / J. C. I. Dooge. - Dynamic hydro-thermal balances at macroscale / P. S. Eagleson. - SESSION IV - LAND SURFACE GLOBAL DATA SETS. - Use of regional and global soils data for climate modelling/ M. J. Gardiner. - Land surface processes: Vegetation / A. Perrier. - Data on snow cover and glaciers for the global climatic models / V. M. Kotliakov and A. N. Krenke. - The shortwave albedo and the surface emissivity / K. Ya. Kondratyev, V. I. Korzov, V. V. Mukhenberg and L. N. Dyachenko. - Water balance / A. Baumgartner. - SESSION V - ACQUISITION OF LAND SURFACE DATA. - Possibilities for remote sensing of surface characteristics / K. I. Itten.
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  • 83
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-5
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 39 S. : graph. Darst.
    Series Statement: Berichte zur Polarforschung 5
    Language: English
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  • 84
    Call number: ZSP-180-B41
    In: Berichte aus dem Zentrum für Meeres- und Klimaforschung
    Type of Medium: Monograph available for loan
    Pages: 68 S. : Abb. ; 30 cm
    ISSN: 0947-7136
    Series Statement: Berichte aus dem Zentrum für Meeres- und Klimaforschung : Reihe B, Ozeanographie 41
    Language: English
    Branch Library: GFZ Library
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  • 85
    Call number: ZSP-180-B39
    In: Berichte aus dem Zentrum für Meeres- und Klimaforschung
    Type of Medium: Monograph available for loan
    Pages: 72 S. : Abb. ; 30 cm
    ISSN: 0947-7136
    Series Statement: Berichte aus dem Zentrum für Meeres- und Klimaforschung : Reihe B, Ozeanographie 39
    Language: English
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  • 86
    facet.materialart.
    Unknown
    Berlin : Akad.-Verl. ; Moscow : Publishing house "Nauka"
    Call number: 95.0712
    Pages: Losebl.-ausg.
    Classification:
    Photogrammetry, Remote Sensing
    Language: English
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  • 87
    Call number: ILP/M 06.0270
    In: Publication of the International Lithosphere Programme
    Type of Medium: Monograph available for loan
    Pages: 32 S. : graph. Darst.
    Series Statement: Publication of the International Lithosphere Programme 105
    Language: English
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  • 88
    Call number: PIK W 510-16-89942
    Type of Medium: Monograph available for loan
    Pages: 277 S. , graph. Darst
    Series Statement: EFI proceedings 38
    Language: English
    Branch Library: PIK Library
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  • 89
    Monograph available for loan
    Monograph available for loan
    Joensuu : European Forest Institute
    Call number: PIK W 510-16-89943
    Type of Medium: Monograph available for loan
    Pages: 171 S. , graph. Darst.
    Series Statement: EFI proceedings 39
    Language: English
    Branch Library: PIK Library
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  • 90
    Call number: PIK N 456-16-90137
    Type of Medium: Monograph available for loan
    Pages: getr. Zählung , ill. (some col.) , 24 cm
    Language: English
    Note: Enth.: Introduction -- Pt. 2. Union of South Africa from Olifants River to Mossel Bay. With an appendix on conditions at Saldanha Bay, Cape Town and Simonstown -- Pt. 3. Union of South Africa from Mossel Bay to East London.With an appendix on conditions oat Mossel Bay and Port Elizabeth -- Pt. 4. Union of South Africa from East London to Kosi Bay.With an appendix on conditions at East London and Durban -- Pt. 5. Portuguese East Africa (Mocambique) and Mocambique Channel -- Pt. 5a. Madagascar. With an appendix on conditions at Mayotte, Diégo Suarez, Nossi Bé and Tamatave
    Location: A 18 - must be ordered
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  • 91
    Call number: MOP Per 492(1925) / DG
    In: Bericht über die Tätigkeit des Königlich Preußischen Meteorologischen Instituts ; 1925, 1925
    In: Veröffentlichungen des Preußischen Meteorologischen Instituts ; 335, Nr. 335
    Type of Medium: Monograph non-lending collection
    Pages: 111 S. , Ill.
    Series Statement: Veröffentlichungen des Preußischen Meteorologischen Instituts 335
    Language: English
    Note: Inhaltsverzeichnis: 1. Einleitung. - 2. Personalien. - 3. Das Stationsnetz. - Stationen I., II. und III. Ordnung und Stationen, die nur Sonnenschein beobachten. - Regenstationen. - Gewitterstationen. - 4. Wetterdienst. - 5. Stationsinstrumente und Sammlungen des Zentralinstituts. Instrumente. Bücherei. - 6. Besondere Arbeiten im Zentralinstitut. - 7. Das Meteorologisch-Magnetische Observatorium bei Potsdam. - Allgemeines. - Meteorologische Beobachungen und Arbeiten. - Magnetische Arbeiten. - 8. Dienstreisen. - 9. Veröffentlichungen. - Veröffentlichungen des Instituts. - Fachwissenschaftliche Veröffentlichungen der Beamten. - Eine photographische Registriereinrichtung mit weiter Zeitskala bei sparsamem Papierverbrauch / Ad. Schmidt. - Vertikale Temperaturgradienten im Gebirge / H. v. Ficker. - Ein Beitrag zur Kenntnis der Regenböen im atlantischen Passatgebiet / K. Knoch. - Ungewöhnlicher Luftdruckanstieg am 22. Dezember 1925 / W. König. - Ueber Niederschlag und gleichzeitigen Luftdruckgang / W. König. - Die Häufigkeit zu nasser und zu trockener Sommermonate (Regenklemmen) in Ostpreußen / G. Wussow. - Das Schwerefeld eines magnetischen Moleküls / O. Venske. - Jährlicher und täglicher Gang der Verdunstung in Potsdam / R. Süring. - Temperatur, Niederschlag und Sonnenschein im Jahre 1925 nach den Beobachtungen der im deutschen Witterungsbericht erscheinenden Stationen.
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  • 92
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: IASS 16.90379
    Type of Medium: Monograph available for loan
    Pages: XII, 239 S. : , Illustrationen, Karten
    Edition: 1. publ.
    ISBN: 0521804434 , 0521010578
    Series Statement: Cambridge studies in international relations ; 78
    Language: English
    Branch Library: RIFS Library
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  • 93
    Call number: AWI A4-17-91119
    Type of Medium: Monograph available for loan
    Pages: xv, 269 pages , illustrations, maps, portraits , 30 cm
    Language: English
    Note: Table of Contents: SESSION 1: EVIDENCE OF CLIMATE CHANGE. - Simulation of the Arctic in Global Climate Models / John E. Walsh. - Model assessment of observed contemporary trends in Arctic Climate / Konstantin Y. Vinnikov, Alan Robock, David A. Robinson, Richard L. Armstrong, Ronald J. Stouffer, Thomas L. Delworth, Anthony J. Broccoli, Keith W. Dixon. - Sea ice motion in response to the Arctic Oscillation / Ignatius G. Rigor, John M. Wallace, Roger L. Colony. - Arctic temperature change from long instrumental and paleoclimatic records / P. D. Jones. - Sea ice thinning in the Nansen basin and Greenland Sea / Peter Wadhams. - How anaomalous is the current state of the Arctic? / Ernst Augstein and Rüdiger Gerdes. - Warming of the Arctic in 1920s-1930s and 1980s-1990s / Genrikh V. Alekseev, Victor F. Zakharov, Roger L. Colony, Mark A. Johnson. - Variations in surface air temperature over the Arctic Ocean / Ignatius G. Rigor, Roger L. Colony, John M. Wallace and Seelye Martin. - Seasonal and regional perspectives of Arctic Sea Ice Oscillation: wavelet analysis / Jia Wang and Moto Ikeda. - Observations of ice sheet mass balance and climate change / J. Jay Zwally. - European contributions for Summit Greenland Environment Observatory / Atsumu Ohmura. - Features of seasonal and interannual variability of the water circulation and sea level of the Arctic Ocean / Vladimir K. Pavlov. - SESSION 2: PALEOCLIMATIC RECONSTRUCTIONS. - Climate surprises: lessons from tropical ice cores / Lonnie G. Thompson. - Temporal and spatial nature of change in the circum-polar Arctic / Roy M. Koerner, Bea T. Alt. - Greenland ice core contributions to PARCA (Program for Arctic Regional Climate Assessment) with emphasis on reconstructing annual accumulation histories / Ellen Mosley-Thompson and PARCA Collaborators. - Climatic and environmental histories for the last two centuries from Arctic ice cores / Kumiko Goto-Azuma, Roy M. Koerner, David A. Fisher, Okitsugu Watanabe. - A coupled atmosphere-ocean GCM experiment for 6 kyr BP and 21 kyr BP / Akio Kitoh, Shigenori Murakami. - Concentration variations of atmospheric methane over the past 340 kyrs deduced from Dome Fuji ice core / T. Nakazawa, S. Aoki, K. Kawamura and O. Watanabe. - Physical properties of Dome Fuji ice cores and paleoenvironmental reconstruction / T. Hondoh, H. Narita, A. Hori, T. Ikeda-Fukazawa, S. Mae, S. Fujita, H. Fukazawa, T. Fukumura, H. Shoji, T. Kameda, A. Miyamoto, N. Azuma, Y. Wong, K. Kawada, O. Watanabe, H. Motoyama. - Variations in the oceanographic environment during last 120 kyr in the Sea of Okhotsk / Takeshi Nakatsuka & the Okhotsk Sediment Core Analyses Group. - SESSION 3: PROCESSES, INTERACTIONS AND FEEDBACKS. - Sea surface temperatures off the East coast of Japan at the last glacial maximum inferred from oxygen isotope of foraminiferal tests / T. Oba. - Hydrologic response and feedbacks to a warmer climate in Arctic regions / Larry D. Hinzman, Kenji Yoshikawa, Douglas L. Kane. - Variability and trends in the hydro-climatology of the major Eurasian Arctic drainages / Mark C. Serreze, Martyn P. Clark, Andrew J. Etringer, David H. Bromwich. - Factors that determine when the seasonal snowmelt occurs in Northern Alaska / Robert S. Stone. - On the role of Siberia in global change / Kunihiko Kodera. - A study of Arctic oscillation induced by a positive feedback between the polar vortex and baroclinic instability / H. L. Tanaka and Hiroki Tokinaga. - A climatology of small-scale disturbances in the polar stratosphere / Kaoru Sato, Motoyoshi Yoshiki and Masaaki Takahashi. - Impacts of winter warming event on the cryosphere in the polar regions / Hiroyuki Enomoto. - Climatic impact of the Arctic aerosols ased on ASTAR 2000 (Arctic study of Tropospheric Aerosol and Radiation) field campaign / Takashi Yamanouchi and Andreas Herber. - Preliminary observational results of international Okhotsk Sea study / Masaaki Wakatsuchi. - Ice albedo feedback effect on sea ice / ocean coupled system in the Antarctic / Kay I. Ohshima and Sohey Nihashi. - Land surface processes in the tundra region of Eastern Siberia / Tetsuo Ohata, Yuji Kodama and Yoshiyuki Ishii. - Influence of the Aleutian/Icelandic low seesaw upon the seasonality of the variability in the Northern Hemisphere / Hisashi Nakamura and Meiji Honda. - SESSION 4: CLIMATE MODELING. - Arctic climate variability in the 20th century / Andrey Proshutinsky. - A sensitivity study of the Arctic climate on the basis of regional and global climate model simulations / K. Dethloff, A. Rinke, T. Kandlbinder, W. Dorn, M. Fortmann, D. Handorf, A. Weisheimer, A. H. Lynch, J. H. Christensen, M. Botzet. - Simulation of climate change in the 20th century / Thomas L. Delworth and Thomas R. Knutson. - GCM Simulations of polar climate variability and change / Vladimir M. Kattsov. - Arctic Alaska climate simulations using the regional atmospheric modeling system / Glen E. Liston, Joseph P. McFadden, Roger A. Pielke, Sr. - Role of North Pacific sea ice in climate variability of the NCAR climate model / Uma S. Bhatt, Srpa Häkkinen, Jack S. Miller. - Intercomparison study of Arctic oscillation (AO) and AO-like climate change simulated by various coupled general circulation models / Akira Noda, Kazuki Yamaguchi. - SESSION 5: CONSEQUENCES AND IMPACTS OF CHANGE. - Impacts of climate change in the Arctic / Gunter Weller. - The changes of permafrost induced by greenhouse warming: a numerical study applying multiple-layer ground model / Kazuki Yamaguchi, Akira Noda, Akio Kitoh. - The Northern Sea route and the perspective / H. Kitagawa. - POSTER SESSION. - Evolution of glaciation on the Novaya Zemlya archipelago during global warmings / M. D. Ananicheva, N. V. Davidovich. - Radar echo characteristics at Ny-Ålesund, Spitsbergen Island and Arctic storms over the Norwegian Sea / Yoshio Asuma, Nao Ogitani, Makoto Wada. - Projections of the anthropogenic air surface temperature variations onto the modes of internal climate variability / Roman V. Bekryaev. - Under-ice melt pools as an acceleration factor of Arctic sea ice melting / Pyotr V. Bogorodsky. - The coastal erosion as a significant source of the particulate matter into the Arctic shelf / Oleg V. Dudarev, Igor P. Semiletov, Anatoly I. Botsul, Igor V. Utkin, Vladimir V. Anikiev, Georgy M. Kolesov, Dmitry Yu. Sapozhnikov. - Relationships between Arctic circulation anomaly and mid-latitude transient eddy activity during NH Winter / Masamitsu Hayasaki, H. L. Tanaka. - Abrupt changes in meteorological conditions observed at an inland Antarctic Station in association with wintertime blocking / Naohiko Hirasawa, Hisashi Nakamura, Takashi Yamanouchi. - Seasonal dependence and life cycle of the interannual seesaw between the Aleutian and Icelandic lows / Meiji Honda, Hisashi Nakamura, Jinro Ukita. - Atmospheric control over the interannual variability of the Eurasian continent surface conditions / Masatake E. Hori, Tetsuzo Yasunari. - Hydrological simulation of the Lena River basin, Siberia / Xieyao Ma, Yoshihiro Fukushima, Tetsuo Ohata. - Measurements of carbon dioxide and methane fluxes over an Arctic coastal Tundra ecosystem in 2000 growing season / M. Mano, Y. Harazono, A. Miyata, R. C. Zulueta, W. C. Oechel. - Acoustic measure of climate change in the Arctic Ocean / Peter N. Mikhalevsky, Alexander N. Gavrilov. - Variability of water properties along the Barrow Canyon and the shelf-break of the Beaufort Sea observed from the R/V Mirai MR99-K05 and MR00-K06 cruises / Shigeto Nishino, Chikashi Kobayashi, Takashi Kikuchi, Koji Shimada, Takatoshi Takizawa. - Estimate of the predictability of the atmosphere in the Arctic / Daisuke Nohara, H. L. Tanaka. - Does the fresh water supply from the Amur River flowing into the Sea of Okhotsk affect sea ice formation? / Masayo Ogi, Yoshihiro Tachibana, Michael A. Danchenkov, Koji Yamazaki, Kensuke Takeuchi. - On the role of internal ice stress in mo
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  • 94
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Institut für atmosphärische Umweltforschung der Fraunhofer- Gesellschaft
    Call number: MOP 44829 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 25 S. , graph. Darst.
    Language: English
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  • 95
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: PIK M 370-16-89711
    Type of Medium: Monograph available for loan
    Pages: XX, 393 Seiten , graph. Darst. , 26 cm
    Edition: 7. print. 1. published 2001
    ISBN: 0521773202 , 9780521773201
    Language: English
    Note: Contents: Part I. Introduction: 1. Probabilistic risk analysis ; Part II. Theoretical Issues and Background: 2. What is uncertainty? ; 3. Probabilistic methods ; 4. Statistical inference ; 5. Weibull analysis ; Part II. System Analysis and Quantification: 6. Fault and event trees ; 7. Fault trees - analysis ; 8. Dependent failures ; 9. Reliability data bases ; 10. Expert opinion ; 11. Human reliability ; 12. Software reliability ; Part IV. Uncertainty Modeling and Risk Measurement: 13. Decision theory ; 14. Influence diagrams and belief nets ; 15. Project risk management ; 16. Probabilistic inversion ; 17. Uncertainty analysis ; 18. Risk measurement and regulation ; Bibliography ; Index.
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  • 96
    Call number: 19/M 17.90698
    Type of Medium: Monograph available for loan
    Pages: XII, 305 Seiten , Ill., graph. Darst.
    ISBN: 1584881941
    Series Statement: Monographs on statistics and applied probability 90
    Classification:
    Mathematics
    Language: English
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  • 97
    Monograph available for loan
    Monograph available for loan
    London : Imperial College Press
    Call number: M 17.91136
    Type of Medium: Monograph available for loan
    Pages: X, 381 S , zahlr. graph. Darst , 23 cm
    Edition: Reprinted
    ISBN: 1860940269
    Language: English
    Location: Upper compact magazine
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  • 98
    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
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  • 99
    Call number: NBM 06.0076
    In: Bulletin of the Seismological Society of America
    Type of Medium: Non-book medium
    Pages: 1 CD-ROM
    Series Statement: Bulletin of the Seismological Society of America Vol. 91, No. 5
    Language: English
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  • 100
    Call number: AWI G3-15-89067
    Type of Medium: Monograph available for loan
    Pages: XIX, 636 S. , Ill., graph. Darst , 25 cm
    ISBN: 0792367839 , 0792367847
    Series Statement: NATO science series 2, Environmental security 76
    Language: English
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