D
Douglas G. Martinson
Researcher at Lamont–Doherty Earth Observatory
Publications - 108
Citations - 16508
Douglas G. Martinson is an academic researcher from Lamont–Doherty Earth Observatory. The author has contributed to research in topics: Sea ice & Arctic ice pack. The author has an hindex of 50, co-authored 107 publications receiving 15540 citations. Previous affiliations of Douglas G. Martinson include Woods Hole Oceanographic Institution & Columbia University.
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Journal ArticleDOI
Sea ice in the western Antarctic Peninsula region : Spatio-temporal variability from ecological and climate change perspectives
Sharon Stammerjohn,Sharon Stammerjohn,Douglas G. Martinson,Douglas G. Martinson,Raymond C. Smith,Richard A. Iannuzzi +5 more
TL;DR: In this paper, a suite of ocean-atmosphere-ice interactions are described that are consistent with the amplified warming in late autumn, early winter, which in turn affect the timing of the sea-ice retreat and subsequent advance.
Journal ArticleDOI
Antarctic sea ice extent variability and its global connectivity
TL;DR: In this article, the temporal cross correlations between detrended Antarctic sea ice edge (SIE) anomaly and various climate indices are calculated, showing that up to 34% of the variance in SIE* is linearly related to ENSO.
Journal ArticleDOI
How Do Polar Marine Ecosystems Respond to Rapid Climate Change
Oscar Schofield,Hugh W. Ducklow,Douglas G. Martinson,Michael P. Meredith,Mark A. Moline,William R. Fraser +5 more
TL;DR: Robotic networks, satellites, ships, and instruments mounted on animals and ice will collect data needed to improve numerical models that can then be used to study the future of polar ecosystems as climate change progresses.
The orbital theory of Pleistocene climate: support from a revised chronology of the marine d18O record
John Imbrie,James D. Hays,Douglas G. Martinson,Andrew McIntyre,Alan C. Mix,Joseph J. Morley,Nicklas G Pisias,Warren L. Prell,Nicholas J Shackleton +8 more
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Interpretation of recent Antarctic sea ice variability
TL;DR: In this paper, the authors investigated the mechanisms responsible for the covariability between the ice and the (a) AAO and (b) ENSO and demonstrated that over the last 24 years, a positive AAO trend and a slightly negative e nino-nino-southern Oscillation trend produce a spatial pattern of ice changes similar to the regional ice trends.