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Mark C. Serreze

Researcher at University of Colorado Boulder

Publications -  201
Citations -  28691

Mark C. Serreze is an academic researcher from University of Colorado Boulder. The author has contributed to research in topics: Arctic & Sea ice. The author has an hindex of 76, co-authored 198 publications receiving 26214 citations. Previous affiliations of Mark C. Serreze include Cooperative Institute for Research in Environmental Sciences & Columbia University.

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Observational evidence of recent change in the northern high-latitude environment

TL;DR: In this paper, the authors present asynthesis of these observations, and conclude that roughly half of the pronounced recent rise in Northern Hemispherewinter temperatures reflects shifts in atmosphericcirculation. But, such changes are not consistent with anthropogenic forcing and include generally positive phases of the North Atlantic and ArcticOscillations and extratropical responses to the El-NinoSouthern Oscillation.
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Processes and impacts of Arctic amplification: A research synthesis

TL;DR: The past decade has seen substantial advances in understanding Arctic amplification, that trends and variability in surface air temperature tend to be larger in the Arctic region than for the Northern Hemisphere or globe as a whole as discussed by the authors.
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Arctic sea ice decline: Faster than forecast

TL;DR: In this paper, a multi-model ensemble mean time series provides a true representation of forced change by greenhouse gas (GHG) loading, 33-38% of the observed September trend from 1953-2006 is externally forced, growing to 47-57% from 1979-2006.
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The Arctic’s rapidly shrinking sea ice cover: a research synthesis

TL;DR: The sequence of extreme September sea ice extent minima over the past decade suggests acceleration in the response of the Arctic sea ice cover to external forcing, hastening the ongoing transition towards a seasonally open Arctic Ocean.
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Role of Land-Surface Changes in Arctic Summer Warming

TL;DR: It is shown that terrestrial changes in summer albedo contribute substantially to recent high-latitude warming trends and the continuation of current trends in shrub and tree expansion could further amplify this atmospheric heating by two to seven times.