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基于AHI观测的全天气条件海表温度反演
引用本文:王朋,诸葛小勇,陈宝君,陆一磊,肖宇昕,夏凡.基于AHI观测的全天气条件海表温度反演[J].气象科学,2020,40(2):249-256.
作者姓名:王朋  诸葛小勇  陈宝君  陆一磊  肖宇昕  夏凡
作者单位:南京大学 大气科学学院, 南京 210023;南京大学 大气科学学院, 南京 210023;南京市高淳区气象局, 南京 211300
基金项目:国家自然科学基金青年基金资助项目(41505086);南京大学大学生创新训练资助计划(X201610284006)
摘    要:基于搭载在日本新一代静止气象卫星Himawari-8上的先进葵花成像仪(Advanced Himawari Imager,AHI)观测资料,研究了高时空分辨率的、全天气条件的海表温度(Sea Surface Temperature,SST)反演算法。本算法包括两步:第一步,根据云检测算法划分晴空和云区,然后利用非线性SST(NLSST)方程由红外亮温估计晴空SST;第二步,在有云区,先由前5 d同一时刻的晴空SST进行初步补缺,然后再利用Barnes插值完善云区SST估计和进行异常点平滑。最终得到时间分辨率为10 min、空间分辨率为0.05°的全天气条件海温分布。利用移动浮标的观测SST验证,晴空区SST估计的均方根误差(Root Mean Square Error,RMSE)和平均误差(Mean Error,ME)分别为0.857 K和0.017 K。全天气条件SST估计的RMSE和ME分别为0.872 K和-0.005 K。

关 键 词:海表温度  反演  Himawari-8  全天气条件
收稿时间:2018/9/3 0:00:00
修稿时间:2018/11/24 0:00:00

Retrieval of sea surface temperature in all sky conditions based on AHI observations
WANG Peng,ZHUGE Xiaoyong,CHEN Baojun,LU Yilei,XIAO Yuxin,XIA Fan.Retrieval of sea surface temperature in all sky conditions based on AHI observations[J].Scientia Meteorologica Sinica,2020,40(2):249-256.
Authors:WANG Peng  ZHUGE Xiaoyong  CHEN Baojun  LU Yilei  XIAO Yuxin  XIA Fan
Institution:School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China;School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China;Gaochun District Meteorological Bureau of Nanjing, Nanjing 211300, China
Abstract:Based on the observations of Advanced Himawari Imager (AHI) carried by the Japanese new generation of geostationary meteorological satellite, Himawari-8, the Sea Surface Temperature (SST) retrieval algorithm with a high spatiotemporal resolution in all sky conditions was studied. The algorithm consists of two steps. Firstly, the clear sky and cloudy sky are separated using a cloud mask algorithm, and then the non-linear SST equation is used to estimate the clear-sky SST from the AHI infrared brightness temperature. Secondly, the clear-sky SST at the same time of previous five days are used as a first guess of the cloudy-sky SST, and then the Barnes Interpolation is employed to further conduct the cloudy-sky SST estimation and perform an anomalous point smoothing. Finally, the SST distributions in all sky conditions with 10 min temporal and 0.05° spatial resolutions are obtained. Validated with the buoy SST, the Root Mean Square Error (RMSE) and Mean Error (ME) for the clear-sky SSTs are 0.857 K and 0.017 K, respectively. The RMSE and ME for SSTs in all sky conditions algorithm are 0.872 K and -0.005 K, respectively.
Keywords:SST  retrieval  Himawari-8  all-sky
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