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Computing and Representing Sea Ice Trends: Toward a Community ConsensusEstimates of the recent decline in Arctic Ocean summer sea ice extent can vary due to differences in sea ice data sources, in the number of years used to compute the trend, and in the start and end years used in the trend computation. Compounding such differences, estimates of the relative decline in sea ice cover (given in percent change per decade) can further vary due to the choice of reference value (the initial point of the trend line, a climatological baseline, etc.). Further adding to the confusion, very often when relative trends are reported in research papers, the reference values used are not specified or made clear. This can lead to confusion when trend studies are cited in the press and public reports.
Document ID
20140005669
Acquisition Source
Goddard Space Flight Center
Document Type
Reprint (Version printed in journal)
Authors
Wohlleben, T.
(Meteorological Service of Canada Ottawa, Ontario, Canada)
Tivy, A.
(National Research Council of Canada Ottawa, Ontario, Canada)
Stroeve, J.
(National Snow and Ice Data Center (NSIDC) Boulder, CO, United States)
Meier, Walter N.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Fetterer, F.
(National Snow and Ice Data Center (NSIDC) Boulder, CO, United States)
Wang, J.
(National Oceanic and Atmospheric Administration Ann Arbor, MI, United States)
Assel, R.
(National Oceanic and Atmospheric Administration Ann Arbor, MI, United States)
Date Acquired
May 13, 2014
Publication Date
October 1, 2013
Publication Information
Publication: Eos
Publisher: AGU
Volume: 94
Issue: 40
Subject Category
Geosciences (General)
Report/Patent Number
GSFC-E-DAA-TN12603
Report Number: GSFC-E-DAA-TN12603
Distribution Limits
Public
Copyright
Public Use Permitted.
Keywords
trend
sea ice
computation
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