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dc.contributor.authorChaudhuri, Ayan H.
dc.contributor.authorPonte, Rui M.
dc.date.accessioned2017-06-09T16:47:05Z
dc.date.available2017-06-09T16:47:05Z
dc.date.copyright2015/01/01
dc.date.issued2014
dc.identifier.otherams-74021.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216200
dc.description.abstracthe authors examine five recent reanalysis products [NCEP Climate Forecast System Reanalysis (CFSR), Modern-Era Retrospective Analysis for Research and Applications (MERRA), Japanese 25-year Reanalysis Project (JRA-25), Interim ECMWF Re-Analysis (ERA-Interim), and Arctic System Reanalysis (ASR)] for 1) trends in near-surface radiation fluxes, air temperature, and humidity, which are important indicators of changes within the Arctic Ocean and also influence sea ice and ocean conditions, and 2) fidelity of these atmospheric fields and effects for an extreme event: namely, the 2007 ice retreat. An analysis of trends over the Arctic for the past decade (2000?09) shows that reanalysis solutions have large spreads, particularly for downwelling shortwave radiation. In many cases, the differences in significant trends between the five reanalysis products are comparable to the estimated trend within a particular product. These discrepancies make it difficult to establish a consensus on likely changes occurring in the Arctic solely based on results from reanalyses fields. Regarding the 2007 ice retreat event, comparisons with remotely sensed estimates of downwelling radiation observations against these reanalysis products present an ambiguity. Remotely sensed observations from a study cited herewith suggest a large increase in downwelling summertime shortwave radiation and decrease in downwelling summertime longwave radiation from 2006 and 2007. On the contrary, the reanalysis products show only small gains in summertime shortwave radiation, if any; however, all the products show increases in downwelling longwave radiation. Thus, agreement within reanalysis fields needs to be further checked against observations to assess possible biases common to all products.
dc.publisherAmerican Meteorological Society
dc.titleAn Evaluation of Surface Atmospheric Changes over the Arctic Ocean for 2000–09 Using Recent Reanalyses
dc.typeJournal Paper
dc.journal.volume19
dc.journal.issue2
dc.journal.titleEarth Interactions
dc.identifier.doi10.1175/EI-D-14-0012.1
dc.journal.fristpage1
dc.journal.lastpage18
dc.treeEarth Interactions:;2014:;volume( 019 ):;issue: 002
dc.contenttypeFulltext


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