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Elizabeth N. Cassano

Researcher at Cooperative Institute for Research in Environmental Sciences

Publications -  20
Citations -  739

Elizabeth N. Cassano is an academic researcher from Cooperative Institute for Research in Environmental Sciences. The author has contributed to research in topics: Sea ice & Arctic ice pack. The author has an hindex of 13, co-authored 19 publications receiving 616 citations.

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Predicted changes in synoptic forcing of net precipitation in large Arctic river basins during the 21st century

TL;DR: In this paper, the authors used self-organizing maps to create a synoptic climate of the Arctic and to assess predicted changes in net precipitation over the Arctic in the 21st century.
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Classification of synoptic patterns in the western Arctic associated with extreme events at Barrow, Alaska, USA

TL;DR: This article used the self-organizing map (SOM) algorithm, an unsu- pervised learning process that codifies large, multivariate datasets onto a 2-dimensional array, or map, to study large-scale circulation patterns associated with temperature and high wind extremes at Barrow.
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Self-organizing map analysis of widespread temperature extremes in Alaska and Canada

TL;DR: In this article, the authors used self-organizing maps (SOMs) to evaluate the synoptic circulation associated with widespread temperature extremes in four regions: 2 each in Alaska and in northern Canada during winter (December, January, and February) for 1989−2007.
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Modeled precipitation variability over the Greenland Ice Sheet

TL;DR: In this paper, an improved dynamic method was proposed to model the topographic effect of precipitation on the precipitation distribution in Greenland using the modern digital elevation data of Ekholm [1996].
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Atmospheric impacts of an Arctic sea ice minimum as seen in the Community Atmosphere Model

TL;DR: In this article, the authors explore the impact of 2007 ice conditions (the second lowest Arctic sea ice extent in the satellite era) on atmospheric circulation and surface temperatures and fluxes through a series of model experiments with the NCAR Community Atmospheric Model version 3.