Inter-Comparison of SST Products from iQuam, AMSR2/GCOM-W1, and MWRI/FY-3D

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Publicado en:Remote Sensing vol. 16, no. 11 (2024), p. 2034
Autor principal: Zhao, Yili
Otros Autores: Liu, Ping, Wu, Zhou
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MDPI AG
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022 |a 2072-4292 
024 7 |a 10.3390/rs16112034  |2 doi 
035 |a 3067436130 
045 2 |b d20240101  |b d20241231 
084 |a 231556  |2 nlm 
100 1 |a Zhao, Yili  |u School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, China; <email>lp@jou.edu.cn</email> 
245 1 |a Inter-Comparison of SST Products from iQuam, AMSR2/GCOM-W1, and MWRI/FY-3D 
260 |b MDPI AG  |c 2024 
513 |a Journal Article 
520 3 |a Evaluating sea surface temperature (SST) products is essential before their application in marine environmental monitoring and related studies. SSTs from the in situ SST Quality Monitor (iQuam) system, Advanced Microwave Scanning Radiometer 2 (AMSR2) aboard the Global Change Observation Mission 1st-Water, and the Microwave Radiation Imager (MWRI) aboard the Chinese Fengyun-3D satellite are intercompared utilizing extended triple collocation (ETC) and direct comparison methods. Additionally, error characteristic variations with respect to time, latitude, SST, sea surface wind speed, columnar water vapor, and columnar cloud liquid water are analyzed comprehensively. In contrast to the prevailing focus on SST validation accuracy, the random errors and the capability to detect SST variations are also evaluated in this study. The result of ETC analysis indicates that iQuam SST from ships exhibits the highest random error, above 0.83 °C, whereas tropical mooring SST displays the lowest random error, below 0.28 °C. SST measurements from drifters, tropical moorings, Argo floats, and high-resolution drifters, which possess random errors of less than 0.35 °C, are recommended for validating remotely sensed SST. The ability of iQuam, AMSR2, and MWRI to detect SST variations diminishes significantly in ocean areas between 0°N and 20°N latitude and latitudes greater than 50°N and 50°S. AMSR2 and iQuam demonstrate similar random errors and capabilities for detecting SST variations, whereas MWRI shows a high random error and weak capability. In comparison to iQuam SST, AMSR2 exhibits a root-mean-square error (RMSE) of about 0.51 °C with a bias of −0.05 °C, while MWRI shows an RMSE of about 1.26 °C with a bias of −0.14 °C. 
610 4 |a National Oceanic & Atmospheric Administration--NOAA 
653 |a Latitude 
653 |a Microwave radiation 
653 |a Environmental monitoring 
653 |a Marine environment 
653 |a Accuracy 
653 |a Bias 
653 |a Sea surface temperature 
653 |a Radiometers 
653 |a Wind speed 
653 |a Calibration 
653 |a Water 
653 |a Quality control 
653 |a Remote sensing 
653 |a Microwaves 
653 |a Error analysis 
653 |a Mooring 
653 |a Water vapor 
653 |a Random errors 
653 |a Precipitation 
653 |a Meteorological satellites 
653 |a Variation 
653 |a Root-mean-square errors 
653 |a Sensors 
653 |a Remote sensing systems 
653 |a Floats 
653 |a Rain 
653 |a Surface wind 
700 1 |a Liu, Ping  |u School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, China; <email>lp@jou.edu.cn</email> 
700 1 |a Wu, Zhou  |u National Satellite Ocean Application Service, Beijing 100081, China; <email>zhouwu@mail.nsoas.org.cn</email> 
773 0 |t Remote Sensing  |g vol. 16, no. 11 (2024), p. 2034 
786 0 |d ProQuest  |t Advanced Technologies & Aerospace Database 
856 4 1 |3 Citation/Abstract  |u https://www.proquest.com/docview/3067436130/abstract/embedded/7BTGNMKEMPT1V9Z2?source=fedsrch 
856 4 0 |3 Full Text + Graphics  |u https://www.proquest.com/docview/3067436130/fulltextwithgraphics/embedded/7BTGNMKEMPT1V9Z2?source=fedsrch 
856 4 0 |3 Full Text - PDF  |u https://www.proquest.com/docview/3067436130/fulltextPDF/embedded/7BTGNMKEMPT1V9Z2?source=fedsrch