Enhanced Arctic Sea Ice Drift Estimation Merging Radiometer and Scatterometer Data

Type Publication
Publication date 2012-07
Language English
Copyright 2012 IEEE
Author(s) Ardhuin FannyORCID1, Ezraty Robert1
Affiliation(s) 1 : Inst Francais Rech Exploitat Mer, Lab Oceanog Spatiale, F-29280 Plouzane, France.
Source Ieee Transactions On Geoscience And Remote Sensing (0196-2892) (Ieee-inst Electrical Electronics Engineers Inc), 2012-07 , Vol. 50 , N. 7 , P. 2639-2648
DOI 10.1109/TGRS.2012.2184124
WOS© Times Cited 20
Keyword(s) Arctic, Advanced Scatterometer (ASCAT), drift, merging, scatterometry, sea ice
Abstract Satellites enable daily and global coverage of the polar oceans and provide a unique monitoring capability of sea ice dynamics. Sea ice drift maps can be estimated in Arctic from several satellite sensors, particularly from scatterometers and radiometers. This study presents the benefits of combining single drift fields at the same resolution into a "merged" field, built at three-and six-day lags during winters with a 62.5-km resolution. It is shown that combining these drift fields not only increases the reliability of the displacement estimation and the number of estimated vectors to almost a full ice covered area but also expands the time period over which these estimations are reliable from freeze until the melt onset. The autumn-winter-spring sea ice drift fields presented here are systematically produced at Institut Francais de Recherche pour l'Exploitation de la Mer/Centre d'Exploitation et de Recherche Satellitaire, the sea ice drift 1992-2011 time series is available, and the processing is ongoing. These data are available for operational use and for the scientific community.
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