Validation of ADEOS-II GLI ocean color products using in-situ observations

被引:0
|
作者
Hiroshi Murakami
Kosei Sasaoka
Kohtaro Hosoda
Hajime Fukushima
Mitsuhiro Toratani
Robert Frouin
B. Greg Mitchell
Mati Kahru
Pierre-Yves Deschamps
Dennis Clark
Stephanie Flora
Motoaki Kishino
Sei-Ichi Saitoh
Ichio Asanuma
Akihiko Tanaka
Hiroaki Sasaki
Katsumi Yokouchi
Yoko Kiyomoto
Hiroaki Saito
Cécile Dupouy
Absornsuda Siripong
Satsuki Matsumura
Joji Ishizaka
机构
[1] JAXA,Earth Observation Research and Application Center
[2] JAMSTEC,Frontier Research Center for Global Change
[3] Tokai University,School of High
[4] UCSD,Technology for Human Welfare
[5] Université des Sciences et Technologies de Lille,Scripps Institution of Oceanography
[6] National Environmental Satellite Service,Laboratoire d’Optique Atmosphérique
[7] Moss Landing Marine Labs,National Oceanic and Atmospheric Administration
[8] Tokyo University of Marine Science and Technology,Marine Science
[9] Hokkaido University,Fisheries Sciences and Faculty of Fisheries
[10] Tokyo University of Information Sciences,Seikai National Fisheries Research Institute
[11] Nagasaki Industrial Promotion Foundation,Tohoku National Fisheries Research Institute
[12] Fisheries Agency,Marine Science Department Faculty of Science
[13] Fisheries Research Agency,Faculty of Fisheries
[14] Fisheries Research Agency,undefined
[15] IRD UR103 CAMELIA,undefined
[16] Centre d’Océanologie de Marseille,undefined
[17] Chulalongkorn University,undefined
[18] Nagasaki University,undefined
来源
Journal of Oceanography | 2006年 / 62卷
关键词
Remote sensing; validation; ocean color; atmospheric correction; chlorophyll; ADEOS-2; GLI; match-up;
D O I
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中图分类号
学科分类号
摘要
The Global Imager (GLI) aboard the Advanced Earth Observing Satellite-II (ADEOS-II) made global observations from 2 April 2003 to 24 October 2003. In cooperation with several institutes and scientists, we obtained quality controlled match-ups between GLI products and in-situ data, 116 for chlorophyll-a concentration (CHLA), 249 for normalized water-leaving radiance (nLw) at 443 nm, and 201 for aerosol optical thickness at 865 nm (Tau_865) and Angstrom exponent between 520 and 865 nm (Angstrom). We evaluated the GLI ocean color products and investigated the causes of errors using the match-ups. The median absolute percentage differences (MedPD) between GLI and in-situ data were 14.1–35.7% for nLws at 380–565 nm, 52.5–74.8% nLws at 625–680 nm, 47.6% for Tau_865, 46.2% for Angstrom, and 46.6% for CHLA, values that are comparable to the ocean-color products of other sensors. We found that some errors in GLI products are correlated with observational conditions; nLw values were underestimated when nLw at 680 nm was high, CHLA was underestimated in absorptive aerosol conditions, and Tau_865 was overestimated in sunglint regions. The error correlations indicate that we need to improve the retrievals of the optical properties of absorptive aerosols and seawater and sea surface reflection for further applications, including coastal monitoring and the combined use of products from multiple sensors.
引用
收藏
页码:373 / 393
页数:20
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