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基于卫星遥感海温数据的南海SST预报误差订正
引用本文:张培军,周水华,梁昌霞.基于卫星遥感海温数据的南海SST预报误差订正[J].热带海洋学报,2020,39(6):57-65.
作者姓名:张培军  周水华  梁昌霞
作者单位:1.国家海洋局南海预报中心, 广东 广州 5103102.自然资源部海洋环境探测技术与应用重点实验室, 广东 广州 510330
基金项目:国家重点研发计划重点专项(2017YFC1404700);广东省促进经济发展专项资金(海洋经济发展用途)项目(GDME-2018B001)
摘    要:尝试利用卫星遥感高分辨率海表温度资料GHRSST (Group for High Resolution Sea Surface Temperature) 与海表温度(sea surface temperature, SST)数值预报产品之间的误差, 建立一种南海SST模式预报订正方法。首先, 利用南海的Argo浮标上层海温数据对GHRSST 海温数据进行验证, 结果表明两者之间均方根误差约为0.3℃, 相关系数为0.98, GHRSST 海温数据可用于南海业务化数值预报SST的订正。预报订正后的SST与Argo浮标海温数据相比, 24h、48h和72h的均方根误差均由0.8℃左右下降到0.5℃以内。与GHRSST 海温数据相比, 南海北部海域(110°E—121°E, 13°N—23°N)订正后的24h、48h和72h的SST预报空间误差均显著减小, 在冷空气影响南海期间或中尺度涡存在的过程中, SST预报订正效果也较为显著。因此, 该方法可考虑在南海业务化SST数值预报系统中应用。

关 键 词:SST  数值预报  误差订正  GHRSST  Argo浮标  南海  
收稿时间:2019-12-09
修稿时间:2020-03-29

Study on the correction of SST prediction in South China Sea using remotely sensed SST
ZHANG Peijun,ZHOU Shuihua,LIANG Changxia.Study on the correction of SST prediction in South China Sea using remotely sensed SST[J].Journal of Tropical Oceanography,2020,39(6):57-65.
Authors:ZHANG Peijun  ZHOU Shuihua  LIANG Changxia
Institution:1. South China Sea Marine Prediction Center, State Oceanic Administration, Guangzhou, Guangdong 510310, China2. Key Laboratory of Marine Environment Survey Technology and Application, Ministry of Natural Resource, Guangzhou, Guangdong 510330, China
Abstract:A new error-correction forecast model for sea surface temperature (SST) is proposed in this paper, where the SST errors are derived from the Group for High Resolution Sea Surface Temperature (GHRSST) data and operational numerical prediction SST product. First of all, the reliability of the GHRSST data was validated with the upper temperature data of Argo floats in the South China Sea. The results showed that the Root Mean Square Error (RMSE) between the two sets of data was about 0.3℃ while the correlation coefficient was 0.98; the GHRSST data could be used for the correction of operational numerical forecast model on SST in the South China Sea. After being corrected, the RMSEs of 24-hr, 48-hr and 72-hr SST forecast results were dropped from 0.8 ℃ to 0.5 ℃ compared with the upper temperature data of Argo floats. Meanwhile, the 24-hr, 48-hr and 72-hr SST forecast errors between the GHRSST data and model results were significantly reduced after the correction in the northern South China Sea (110°E -121°E, 13°N -23°N). During the influence of the cold air or the mesoscale eddy in the South China Sea, the effect of SST forecast correction was also quite significant. Therefore, this method should be considered to apply in the operational numerical forecast system on SST in the South China Sea.
Keywords:SST  Operational numerical prediction  Error correction  GHRSST  Argo  South China Sea  
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