Half a century of satellite remote sensing of sea-surface temperature

被引:163
|
作者
Minnett, P. J. [1 ]
Alvera-Azcarate, A. [2 ]
Chin, T. M. [3 ]
Corlett, G. K. [4 ]
Gentemann, C. L. [5 ]
Karagali, I. [6 ]
Li, X. [7 ]
Marsouin, A. [8 ]
Marullo, S. [9 ]
Maturi, E. [10 ]
Santoleri, R. [11 ]
Picart, S. Saux [8 ]
Steele, M. [12 ]
Vazquez-Cuervo, J. [3 ]
机构
[1] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA
[2] Univ Liege, AGO, GHER, MARE, Allee Six Aout 17, B-4000 Liege, Belgium
[3] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA
[4] EUMETSAT, Eumetsat Allee 1, D-64295 Darmstadt, Germany
[5] Earth & Space Res, 2101 4th Ave 1310, Seattle, WA 98121 USA
[6] Tech Univ Denmark, DTU Wind Energy, Riso Campus,Frederiksborgvej 399, DK-4000 Roskilde, Denmark
[7] NOAA, IMSG Environm Modeling Ctr, Natl Ctr Environm Predict, 5830 Univ Res Court, College Pk, MD 20740 USA
[8] Univ Toulouse, Meteo France, CNRM, CNRS, Lannion, France
[9] Italian Natl Agcy New Technol Energy & Sustainabl, ENEA, Div Models & Technol Risk Reduct, Lab Climate Modelling,Ctr Ric Frascati, Frascati, Italy
[10] NOAA, Ctr Weather & Climate Predict NCWCP, NESDIS, STAR, 5830 Univ Res Court,Rm 3711, College Pk, MD 20740 USA
[11] CNR, Inst Marine Sci ISMAR, Venice, Italy
[12] Univ Washington, Appl Phys Lab, Polar Sci Ctr, 1013 NE 40th St, Seattle, WA 98105 USA
基金
美国国家航空航天局;
关键词
Sea surface temperature; Fifty year review; INFRARED RADIOMETER CALIBRATION; TRACK SCANNING RADIOMETERS; GULF-STREAM SEPARATION; IN-SITU; GLOBAL OCEAN; MEDITERRANEAN-SEA; DATA ASSIMILATION; DIURNAL CYCLE; SKIN TEMPERATURE; CLIMATE-CHANGE;
D O I
10.1016/j.rse.2019.111366
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Sea-surface temperature (SST) was one of the first ocean variables to be studied from earth observation satellites. Pioneering images from infrared scanning radiometers revealed the complexity of the surface temperature fields, but these were derived from radiance measurements at orbital heights and included the effects of the intervening atmosphere. Corrections for the effects of the atmosphere to make quantitative estimates of the SST became possible when radiometers with multiple infrared channels were deployed in 1979. At the same time, imaging microwave radiometers with SST capabilities were also flown. Since then, SST has been derived from infrared and microwave radiometers on polar orbiting satellites and from infrared radiometers on geostationary spacecraft. As the performances of satellite radiometers and SST retrieval algorithms improved, accurate, global, high resolution, frequently sampled SST fields became fundamental to many research and operational activities. Here we provide an overview of the physics of the derivation of SST and the history of the development of satellite instruments over half a century. As demonstrated accuracies increased, they stimulated scientific research into the oceans, the coupled ocean-atmosphere system and the climate. We provide brief overviews of the development of some applications, including the feasibility of generating Climate Data Records. We summarize the important role of the Group for High Resolution SST (GHRSST) in providing a forum for scientists and operational practitioners to discuss problems and results, and to help coordinate activities world-wide, including alignment of data formatting and protocols and research. The challenges of burgeoning data volumes, data distribution and analysis have benefited from simultaneous progress in computing power, high capacity storage, and communications over the Internet, so we summarize the development and current capabilities of data archives. We conclude with an outlook of developments anticipated in the next decade or so.
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页数:49
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