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  • 1
    Call number: 9/N 11.0331
    Description / Table of Contents: Contents: Ablation Depression.-Ablatometer.-Acidity of Glacier Ice.-Active Ice Wedge.-Adfreeze.-Aerial Photogrammetry for Glacial Monitoring.-Alaskan Glaciers.-Albedo.-Alps.-Altai-Sayan Glaciers.-Anabatic Winds: In Relation with Snow/Glacier Basin.-Anchor Ice.-Andean Glaciers.-Anisotropic Ice Flow.-Antarctica.-Anti-Icing.-Anti-Syngenetic Ice Wedge.-Appalachian Glacier Complex in Maritime Canada.-Arctic Hydroclimatology.-Artificial Ground Freezing.-Artificial Production of Snow.-Atmosphere-Snow/Ice Interactions.-Atmospheric Circulation and Glaciochemical Records.-Automated Glacier Mapping.-Basal Sediment Evacuation by Subglacial Drainage Systems.-Base Flow/Groundwater Flow.-Bed (Bottom) Topography.-Bed Forms (Fluvial).-Bed Roughness.-Bed Strength.-Benchmark Glacier.-Biogeochemistry of Sea Ice.-Blue Ice.-Bottom Melting or Undermelt (Ice Shelf).-Brash Ice.-Calving Glaciers.-Canadian Rockies and Coast Mountains of Canada.-Cascade Mountains, USA.-Cascade System.-Catastrophic Flooding.-Catastrophic Rock Slope Failures and Mountain Glaciers.-Catchment Glacier.-Caucasus Mountains.-Characteristics of Snow and Glacier Fed Rivers in Mountainous Regions with Special Reference to Himalayan Basins.-Chemical Composition of Snow, Ice, and Glaciers.-Chemical and Microbe Records in Snow and Ice.-Chemical Processes in Snow and Ice.-Circulation and Mixing in Ice-Covered Lakes.-Cirque Glaciers.-Temperature and Precipitation.-Cloudburst.-Cohesion.-Cold-Based Glaciers.-Condensation Nuclei.-Confluence of Rivers.-Congelation Ice.-Crack.-Creep.-Crevasses.-Critical Temperature.-Crush.-Crust.-Cryoconite.-Cryodessication.-Cryofront.-Cryogenesis.-Cryogenic Aquiclude.-Cryogenic Fabric.-Cryolithology.-Cryopeg.-Cryosol.-Cryostatic Pressure.-Cryostructure.-Cryoturbation.-Dating Glacial Landforms.-Dead Ice.-Debris.-Debris Thermal Properties and Impact on Ice Ablation.-Debris-Covered Glaciers.-Deglaciation.-Degree-Days.-Depletion of Snow Cover.-Deposition from Debris-Rich Ice.-Digital Elevation Model Generation over Glacierized Region.-Digital Image Information Extraction Techniques for Snow Cover Mapping from Remote Sensing Data.-Direct Surface Runoff.-Discharge/Streamflow.-Distributary Channels.-Diurnal Cycle of Runoff.-Diverging Ice Flow.-Drift Glacier/Ice/Snow.-Dry and Wet Snow Line/Zone.-Dry Snow.-Dye Tracer Investigations of Glacier Hydrology.-Dynamics of Glaciers.-Elongation Ratio.-Englacial Conduit.-Englacial Processes.-.Environmental Isotopes.-Epigenetic Ice.-Epiglacial Morphology.-Equilibrium-Line Altitude (ELA).-Erosion of Hard Rock Bed.-Erosion Rate.-Estimation of Glacier Volume and Volume Change by Scaling Methods.-Estuary Ice Cover.-Fast Ice.-Finger Rafting.-Firn.-Fjords.-Foliation.-Forbes Band.-Formation and Deformation of Basal Ice.-Frazil.-Freezing Bottom (Ice Shelf).-Freezing Meltwater.-Freezing and Thawing Index.-Frequency Analysis of Snow Storms.-Fresh Water Storage.-Frictional Melting.-Frost.-Frozen Soil Hydrology.-Frozen Toe (Outer Zone of Glacier Snout).-Gelisols.-Geochemistry of Snow and Ice.-Geocryology.-GIS in Glaciology.-Glacial Drainage Characteristics.-Glacial Ecosystems.-Glacial Erosion.-Glacial Erratic.-Glacial Geomorphology and Landforms Evolution.-Glacial Grooves.-Glacial Overdeepening.-Glacial Striations.-Glacial Trough.-Glacial/Interglacial Cycles.-Glaciation During Times of Enhanced/Reduced Atmospheric Carbon Dioxide.-Glaciations and Groundwater Flow Systems.-Glacier.-Glacier Bird of the Andes.-Glacier Cave.-Glacier Field Studies: Important Things to Notice.-Glacier Hydrology.-Glacier Lake Outburst Floods.-Glacier Mass Balance.-Glacier Motion/Ice Velocity.-Glacier Pothole.-Glacier Sliding.-Glacier Surging.-Glacier System.-Glacier Toe.-Glaciers of the Karakoram Himalaya.-Glacieret.-Glacierization.-Glacioeustasy.-Glaciofluvial.-Glaciogenic Deposits.-Glaciohydraulic Supercooling.-Glacioisostasy.-Glaciolacustrine.-Glaciology.-Glaciomarine.-Glaciostatic Pressure/Stress.-Glaciotectonic Structures, Landforms, and Processes.-Global Climate Modeling in Cryospheric Assessment.-Global Outlook of Snowcover, Sea Ice, and Glaciers.-Global Warming and its Effect on Snow/Ice/Glaciers.-GPS in Glaciology, Applications.-GRACE in Glaciology.-Granulometry.-Gravel Sheet.-Gravitational Mass Movement Deposits.-Gravity Flow (Mass Flow).-Gray-White Ice.-Greenland Glaciers Outside the Ice Sheet.-Greenland Ice Sheet.-Ground Ice.-Ground Penetrating Radar Measurements over Glaciers.-Heat and Mass Transfer in Sea Ice.-High Elevation Glacio-Climatology.-Himalaya.-Himalayan Glaciers in 2010 and 2035.-Hindu Kush.-Holocene Glacier Fluctuations.-Horizontal Component of Ablation.-Horizontal Component of Velocity.-Hummocks (Peat).-Hydrochemical Characteristics of Snow, Ice, and Glaciers.-Hydrogen Isotopes.-Hydrographs.-Hydrologic Cycle and Snow.-Hydrological Response in Glacierized Basins.-Hydrology of Jökulhlaups.-Hydropower: Hydroelectric Power Generation from Alpine Glacier Melt.-Hypsometry.-Hysteresis.-Ice.-Ice Age.-Ice Age Cycles: Data, Models, and Uncertainties.-Ice Age Development Theory.-Ice Apron.-Ice Caps.-Ice Caves.-Ice Core.-Ice Covered Lakes.-Ice Dams.-Ice Sheet.-Ice Sheet Mass Balance.-Ice Shelf.-Ice-Cored Moraines.-Ice-Dammed Lakes.-Ice-Marginal Deposition.-Ice-Marginal Processes.-Ice-Volcano Interactions.-Icefall.-Iceland Glaciers.-ICESat Data in Glaciological Studies.-Icicle.-Icing.-Impacts of Snow and Glaciers on Runoff.-Interception of Snow.-Interflow.-International Polar Year 20072008.-Interstitial Ice.-Intrusive Ice.-Inventory of Glaciers.-Inverse Methods in Glaciology.-Inversion Layers.-Inverted Cup Depth Hoar Crystals.-Irreducible Water.-Isotope Analysis.-Isotopic Characteristics of Ice, Snow, and Glaciers.-Isotopic Fractionation of Freezing Water.-Isotopic Signatures.-Kame and Kettle Topography.-Katabatic Wind: In Relation with Snow and Glaciers.-Kilimanjaro.-Kunlun Mountains.-Lake Ellsworth.-Lake Ice.-Lake Vostok.-Laminated Sediments.-Landforms of Glacial Deposition.-Landforms of Glacial Erosion.-Landforms of Glacial Transportation.-Landscapes of Glacial Erosion.-Last Glacial Maximum Glaciation (LGM/LGP) in High Asia (Tibet and Surrounding Mountains).-Latent Heat of Condensation.-Latent Heat of Fusion/Freezing.-Latent Heat of Sublimation.-Latent Heat of Vaporization/Condensation.-Lateroglacial.-Lateroglacial Landform Systems.-Laurentide Ice Sheet.-Layering of Snow.-LIDAR in Glaciology.-Little Ice Age.-Lobe.-Mapping of Internal Glacial Layers.-Marginal Channel (Lateral Meltwater Channel).-Marginal Ice Zones.-Marine Glaciers.-Marine Ice Sheet.-Mechanical Weathering.-Median Elevation of Glaciers.-Mediterranean Glaciers and Glaciation.-Melt Runoff Modeling.-Melting Processes.-Meltwater Channels.-Meltwater Conduit.-Meltwater Erosion.-Meltwater Pressure.-Meltwater Storage.-Microorganisms Associated with Glaciers.-Monitoring and Warning Systems.-Monsoonal Records Observed from Snow/Ice/Glacier.-Moraine.-Moulins.-Mount Everest.-Mount Kenya.-Mountain Geomorphology.-Natural Hazards Associated with Glaciers and Permafrost.-Negative Temperature Gradient (in Ice).-Neoglaciation.-Network of Stakes.-New Zealand Glaciers.-Niche Glacier.-Normalized-Difference Snow Index (NDSI).-Nye (N) Channels.-Ogives.-Optical Remote Sensing of Alpine Glaciers.-Orographic Precipitation.-Outlet Glacier.-Overburden Pressure.-Oxygen Isotopes.-Palaeo Glaciofluvial Sediment Systems.-Palaeo-Channel.-Palaeo-Ice Stream.-Palaeoclimate and Past Glaciations.-Palaeohydrology.-Pamirs.-Pancake Ice.-Papua.-Paraglacial Landscape Transformations.-Patagonia.-Paternoster Lakes.-Peak Flood Glacier Discharge.-Percolation Zone.-Perennially Frozen Ground.-Periglacial.-Permacrete.-Permafrost.-Permafrost on Asteroids.-Permafrost and Climate Interactions.-Permafrost Modeling.-Permanent/Perpetual Snow Line.-Physical Properties of Snow.-Piedmont Glaciers.-Pingo.-Plastic Deformation.-Plastic Flow.-Pleistocene Epoch.-Plucking.-Polythermal Glaciers.-Precipitation.-Proglacial Lakes.-Quaternary Glaciation.-Radar Application in Snow, Ice, and Glaciers.-Radiative Transfer Modeling.-Radioactive Fallout.-Radioactive Isotopes.-Radioactivity.-Rain-Induced Snowmelt.-Ram Resistance.-Rating Curve.-Recession Coefficient.-Recession of Discharge.-Reconstruction of the Last Glaciations in the Whole of Asia.-Recrystallization of Ice.-Refreezing of Meltwater.-Regelation.-Remobilization (of Debris).-Resedimentation.-Retreat/Advance of Glaciers.-Rime Ice.-River Ice Hydrology.-Roche Moutonnees.-Rock Glaciers.-Rocky Mountains.-Röthlisberger (R)-Channels.-Runoff Coefficient.-Runoff Generation.-Runoff Observations.-Runout Distance.-Salinity.-Saltation.-Scandinavian Glaciers.-Sea Ice.-Sea-Level.-Seasonal Frost.-Seasonal Snow Cover.-Sediment Budgets.-Sediment Core and Glacial Environment Reconstruction.-Sediment Entrainment, Transport, and Deposition.-Sediment Flux Source-To-Sink.-Sediment Gravity Flow.-Sediment Routing.-Sediment Transfer Modeling.-Sediment Yield.-SEM Analysis of Glacial Sediments.-Septa of Englacial Debris.-Serac.-Siberia.-Slush and Sleet of Snow.-Snow.-Snow Bed/Snow Bed Vegetation.-Snow Course.-Snow Cover and Snowmelt in Forest Regions.-Snow Cover Changes in the Alps.-Snow Crystal Structure.-Snow Deformation.-Snow Density.-Snow Depth.-Snow Drift.-Snow Gauge.-Snow Grains.-Snow Hydrology.-Snow Layer.-Snow Load.-Snow Metamorphism.-Snow Microstructure.-Snow Pellet.-Snow Pillow.-Snow Pit.-Snow Ripening.-Snow Skating.-Snow Skiing.-Snow Storm.-Snow and Vegetation Interaction.-Snow Water Equivalent.-Snowboard.-Solifluction.-Solute in Glacial Meltwaters.-Solutes in Glacier Ice.-Specific Melt Rate.-Stable Isotopes.-Stage-Discharge Relationship.-Stationary Glacier.-Stratigraphy of Snowpacks.-Streamflow Trends in Mountainous Regions.-Structural Glaciology.-Subglacial Borehole Instrumentation.-Subglacial Drainage System.-Subglacial Lakes, Antarctic.-Subglacial Processes.-Subglacial Volcanism.-Subglacial Weathering.-Sublimation from Snow and Ice.-Summer Accumulation Type Glaciers.-Super Cooling Clouds.-Supercooled Water.-Supra-Glacial Debris Entrainments.-Surface Energy Balance.-Surface Temperature of Snow and Ice.-Suspended Sediment Concentration.-Suspended Sediment Dynamics.-Suspended Sediment Load.-Synthetic Aperture Radar (SAR) Interferometry for Glacier Movement Studies.-Talik.-Tarn.-Temperate Glaciers.-Temperature Lapse Rates in Glacierized Basins.-Temperature Profile of Snowpack.-Terminus.-Terraces.-Thaw Weakening.-Thermal Infrared Sensors.-Thermal Regime of Ice-Covered Lakes.-Thermokarst.-Thinning of Arctic Sea Ice.-Thinning of Glaciers.-Tibetan Plateau.-Tidewater Glaciers.-Tien Shan Glaciers.-Till.-Topographic Normalization of Multispectral Satellite Imagery.-Transformations of Snow at the Earths Surface and its Climatic and Environmental Consequences.-Transient Snowline.-Tree-Ring Indicators of Glacier Fluctuations.-Tributary Glaciers.-Urban Snow.-U-Shape Valley.-Vein Ice.-V-Shaped Valley.-Water Balance in the Glacierized Region.-Westerlies and their Effects on Maritime Ice Caps and Glaciers.-WGMS (World Glacier Monitoring Service).-Winter Accumulation Glacier.-Year-Round Ablation Pattern.-Younger Dryas
    Type of Medium: Monograph available for loan
    Pages: XLII, 1253 S. , zahlr. Ill., graph. Darst., Kt.
    ISBN: 9789048126439
    Series Statement: Encyclopedia of earth sciences series
    Classification:
    Geology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Keywords: distribution of snow, ice and glaciers ; glaciation ; ice ages ; glacier dynamics ; mass balance ; snowfall and snow cover
    Description / Table of Contents: The earth’s cryosphere, which includes snow, glaciers and ice caps, ice sheets, ice shelves, sea ice, river and lake ice, and frozen ground, contains about 75% of the earth’s fresh water. It exists at almost all latitudes, from the tropics to the poles, and plays a vital role in controlling the global climate system. It also provides direct visible evidence of the effect of climate change, and, therefore, requires proper understanding of the complex dynamics. This encyclopedia mainly focuses on the various aspects of snow, ice and glaciers, but also covers other cryospheric branches, and provides an up-to-date information and basic concepts on relevant topics. It includes alphabetically arranged and professionally written, comprehensive and authoritative academic articles by well-known international experts in individual fields. The encyclopedia contains a broad spectrum of topics, ranging from the atmospheric processes responsible for snow formation; transformation of snow to ice and changes in their properties; classification of ice and glaciers and their worldwide distribution; glaciation and ice ages; glacier dynamics; glacier surface and subsurface characteristics; geomorphic processes and landscape formation; hydrology and sedimentary systems; permafrost degradation; hazards caused by cryospheric changes; and trends of glacier retreat on the global scale along with the impact of climate change. This book can serve as a source of reference at the undergraduate and graduate level and help better understand snow, ice and glaciers. This will also be an indispensable tool containing specialized literature for geologists, geographers, climatologists, hydrologists, and water resources engineers; as well as to those who are engaged in the practice of agricultural and civil engineering, earth sciences, environmental sciences and engineering, ecosystem management, and other relevant subjects.
    Pages: Online-Ressource (XLVI, 1253 Seiten)
    ISBN: 9789048126422
    Language: English
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  • 3
    Publication Date: 2012-09-10
    Print ISSN: 0143-1161
    Electronic ISSN: 1366-5901
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Taylor & Francis
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    Publication Date: 2006-01-01
    Description: The Bhagirathi River, a proglacial melt water stream of the Gangotri Glacier, is the principal source of the Ganges river system. The upper part of the basin lies in the high altitude region of the Garhwal Himalayas and is extensively covered by glaciers. We provide hydro-meteorological insight into a severe storm that produced unusual high rains in June 2000 in the uppermost part of the Bhagirathi River. This storm was concentrated upstream of Gangotri town and triggered landslides/rockslides, at several locations between the glacier snout and Gangotri town. One of the major rockslides blocked the Bhagirathi River at Bhujbas, about 3 km downstream of the Gangotri Glacier snout, creating an artificial lake at this location. High stream flow in the river, generated by rapid runoff response from mountain slopes along with melt runoff from the glacier, quickly increased the level of water stored in the artificial lake. Daily rainfall in this region rarely exceeds 10 mm, while total rainfall during this 6-day storm was 131.5 mm. This unusual rain event occurred during the tourist season in June, consequently trapping a large number of tourists and vendors in this area. Sudden release of stored water generated floods that created havoc downstream of the artificially created lake. This paper presents the hydrological and meteorological information related to such an unusual and devastating event observed in the high altitude region of the Himalayas. Copyright © 2006 John Wiley & Sons, Ltd.
    Print ISSN: 0885-6087
    Electronic ISSN: 1099-1085
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Wiley
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  • 6
    Publication Date: 2005-01-01
    Description: Diurnal variations in discharge and suspended sediment concentration (SSC), including runoff delaying characteristics, have been studied for the Gangotri Glacier, the largest glacier in the Garhwal Himalayas (glacierized area 286 km2; drainage area 556 km2). Hourly discharge and SSC data were collected near the snout of the glacier (∼4000 m) at an interval of about 15 days for an entire ablation period (May-October 2001). Diurnal variability in SSC was found to be much higher than the discharge. Hysteresis trends between discharge and SSC were established. Results indicate that, for the study glacier, clockwise hysteresis dominated for the entire melt season, indicating that most of the time the SSC led the discharge. During the peak melt period, anticlockwise hysteresis was also observed for a few hours. Assessment of runoff-delaying characteristics was made by estimating the time lag between the occurrence of melting and its appearance as runoff along with estimation of time to peak. A comparison of runoff-delaying parameters with discharge ratio clearly indicated that changes in time lag and time to peak are inversely correlated with variations in discharge. Attempts have also been made to establish the relationship between discharge and SSC using short-interval data. Copyright © 2004 John Wiley & Sons, Ltd.
    Print ISSN: 0885-6087
    Electronic ISSN: 1099-1085
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Wiley
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  • 7
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    Publication Date: 2017-10-24
    Description: Despite recent research identifying a clear anthropogenic impact on glacier recession, the effect of recent climate change on glacier-related hazards is at present unclear. Here we present the first global spatio-temporal assessment of glacial lake outburst floods (GLOFs) focusing explicitly on lake drainage following moraine dam failure. These floods occur as mountain glaciers recede and downwaste and many have an enormous impact on downstream communities and infrastructure. Our assessment of GLOFs associated with the collapse of moraine-dammed lakes provides insights into the historical trends of GLOFs and their distributions under current and future global climate change. We observe a clear global increase in GLOF frequency and their regularity around 1930, which likely represents a lagged response to post-Little Ice Age warming. Notably, we also show that GLOF frequency and their regularity – rather unexpectedly – has declined in recent decades even during a time of rapid glacier recession. Although previous studies have suggested that GLOFs will increase in response to climate warming and glacier recession, our global results demonstrate that this has not yet clearly happened. From assessment of the timing of climate forcing, lag times in glacier recession, lake formation and moraine dam failure, we predict increased GLOF frequencies during the next decades and into the 22nd century.
    Print ISSN: 1994-0432
    Electronic ISSN: 1994-0440
    Topics: Geography , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 9
    Publication Date: 2020-01-08
    Electronic ISSN: 2296-6463
    Topics: Geosciences
    Published by Frontiers Media
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  • 10
    Publication Date: 2004-02-01
    Print ISSN: 0029-1277
    Electronic ISSN: 2224-7955
    Topics: Architecture, Civil Engineering, Surveying
    Published by IWA Publishing
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