![]() ![]() Alpine icefield landsystem of upland Britain. ![]() Subpolar landsystems of James Ross Island.Cirque glaciation landsystem of upland Britain.Introduction to glaciated valley landsystems. ![]() Introduction to Glaciofluvial Landforms.The role of debris cover on glacier ablation.An introduction to Glacier Mass Balance.Differences between Arctic and Antarctic sea ice.A introduction to the hierarchy of ice-sheet models.Degree day models: Modelling glacier melt.Dealing with uncertainty: predicting future sea level rise.Plateau Icefields: Glacial geomorphology of Juneau Icefield.Glacier disconnections, Juneau Icefield.Structural Glaciology of Juneau Icefield.Supraglacial hydrology of the Greenland Ice Sheet.Glacier recession around the Greenland Ice Sheet.An introduction to the Greenland Ice Sheet.Antarctic supraglacial lakes and ice-shelf collapse.Calculating glacier ice volumes and sea level equivalents.What is the global volume of land ice and how is it changing?.James Ross Island fieldwork photographs.Not so humbly Humboldt: the queer relationships of a German explorer.An introduction to the Physical Geography of Antarctica StoryMap.Deplete and Retreat Publications and Outputs.Deplete and Retreat: Andes Water Towers.NSIDC also provides information on more than 130,000 glaciers through the World Glacier Inventory. The Randolph Glacier inventory is not currently accessible through NSIDC but is available from the GLIMS project website. It includes detailed outlines of the extent of each glacier, with images in the inventory spanning from 1999 to 2010. The Randolph Glacier Inventory, which is a global catalogue of glacier outlines, supplements GLIMS Glacier Database. The GLIMS Glacier Database enables scientists to map how glaciers have changed over time, allowing them to better understand the impacts these changes will have on water resources, downstream hazards, ecosystem changes, and global sea level rise. Since its inception, over 60 institutions in 28 nations worldwide have contributed to the GLIMS Glacier Database.īecause glaciers advance and retreat in response to environmental cues, including changes in temperature and precipitation, they are strong indicators of climate change. It is a collection of worldwide cooperative networks (Regional Centers) that map and analyze glacier fluctuations in their geographic region of expertise. The GLIMS initiative was established in 1999 by the joint U.S./Japan ASTER Science Team. These additional sources include other satellite observations, such as observations from Satellite Pour l’Observation de la Terre (SPOT) and EMI+, as well as maps, aerial photographs, and historical observations dating back to 1850.Ī sample image of Alaskan glaciers from the GLIMS glacier viewer application. Data are primarily derived from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument aboard the Terra satellite and the Landsat Enhanced Thematic Mapper Plus (ETM+), but other sources are also used. The collection includes data from approximately 70 percent of the world's 200,000 glaciers, and new glaciers are continually added. The glacier database includes measurements of glacier geometry, glacier area, snowlines, supraglacial lakes and rock debris, and other glacial attributes, as well as browse images. ![]() This data collection’s primary data product is the GLIMS Glacier Database. GLIMS is an international project to inventory the world’s glaciers and to create a comprehensive, global database of land ice through repeat surveys. The NSIDC DAAC GLIMS data collection includes data from the Global Land Ice Measurements from Space (GLIMS) initiative.
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