Operational Implementation of Sea Ice Concentration Estimates From the AMSR2 Sensor

被引:13
作者
Meier, Walter N. [1 ]
Stewart, J. Scott [2 ]
Liu, Yinghui [3 ]
Key, Jeffrey [4 ]
Miller, Jeffrey A. [1 ,5 ]
机构
[1] NASA, Goddard Space Flight Ctr, Cryospher Sci Lab, Greenbelt, MD 20771 USA
[2] Natl Snow & Ice Data Ctr, Boulder, CO 80309 USA
[3] Univ Wisconsin, Cooperat Inst Meteorol Satellite Studies, Madison, WI 53706 USA
[4] NOAA, Natl Environm Satellite Data & Informat Serv, Madison, WI 53706 USA
[5] ADNET Syst Inc, Bethesda, MD 20817 USA
基金
美国海洋和大气管理局;
关键词
AMSR2; Antarctic; Arctic; passive microwave; remote sensing; sea ice; PARAMETERS; RETRIEVAL;
D O I
10.1109/JSTARS.2017.2693120
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
An operation implementation of a passive microwave sea ice concentration algorithm to support NOAA's operational mission is presented. The NASA team 2 algorithm, previously developed for the NASA advanced microwave scanning radiometer for the Earth observing system (AMSR-E) product suite, is adapted for operational use with the JAXA AMSR2 sensor through several enhancements. First, the algorithm is modified to process individual swaths and provide concentration from the most recent swaths instead of a 24-hour average. A latency (time since observation) field and a 24-hour concentration range (maximum-minimum) are included to provide indications of data timeliness and variability. Concentration from the Bootstrap algorithm is a secondary field to provide complementary sea ice information. A quality flag is implemented to provide information on interpolation, filtering, and other quality control steps. The AMSR2 concentration fields are compared with a different AMSR2 passive microwave product, and then validated via comparison with sea ice concentration from the Suomi visible and infrared imaging radiometer suite. This validation indicates the AMSR2 concentrations have a bias of 3.9% and an RMSE of 11.0% in the Arctic, and a bias of 4.45% and RMSE of 8.8% in the Antarctic. In most cases, the NOAA operational requirements for accuracy are met. However, in low-concentration regimes, such as during melt and near the ice edge, errors are higher because of the limitations of passive microwave sensors and the algorithm retrieval.
引用
收藏
页码:3904 / 3911
页数:8
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