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James L. Fastook, Professor of Computer ScienceIS MWP 1A REAL AND COULD IT HAVE...
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Greenland surface mass balance derived from climate reanalysis models, 1979-2017
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Greenland surface mass balance derived from climate reanalysis models, 1979-2017
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Climate Investigations Using Ice Sheet and Mass Balance Models with Emphasis on...
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Is MWP 1A Real and Could It have Originated in the Northern Hemisphere in Respon...
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Sustainably Harvesting a Large Carnivore? Development of Eurasian Lynx Populatio...
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Analysis of Historical and Projected Future Climate of Mali, West African Sahel
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Modelling storage-driven connectivity between landscapes and riverscapes : towar...
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Modelling storage‐driven connectivity between landscapes and riverscapes: toward...
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ASSESSING THE CUMULATIVE IMPACTS OF HYDROPOWER REGULATION ON THE FLOW CHARACTERI...
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2005b) Prey density, environmental productivity and home-range size in the Euras...
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2005b) Prey density, environmental productivity and home-range size in the Euras...
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Quantifying the relative importance of stock level, river temperature and discha...
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Evaluation of Reanalysis Temperature and Precipitation for the Andean Altiplano...
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Holocene warming marked by abrupt onset of longer summers and reduced storm freq...
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Plausible Future Climate Scenarios and Implications for the Arctic ...
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Storm Track Influences on West Greenland Snow Accumulation ...
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Framework for an Arctic Nation/Community Risk Assessment in the Context of Futur...
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Association between recent U.S. northeast precipitation trends and Greenland blo...
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NOAA/WDS Paleoclimatology - Mt. Hunter, Alaska 1,200 Year Ice Core Accumulation...
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Southern Hemisphere
Earth Sciences
Ecology, Evolution, Behavior and Systematics
Environmental sciences
GE1-350
Geology
Global and Planetary Change
Paleoclimatology
climate change
climate reanalysis
ice cores
reanalysis
Antarctica
Archeology
Atmosphere
Atmospheric circulation--Models
Climate
Climate change
Climatic changes
Continents
Dust
Earth-Surface Processes
Eurasian lynx
Geodynamics
Glaciers
Glaciology
Greenland Ice Sheet
Hydrology
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Last Glacial Maximum
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