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Improvement of short-termforecasting in the northwest Pacific through assimilating Argo data into initial fields
作者姓名:FU Hongli  CHU Peter C  HAN Guijun  HE Zhongjie  LI Wei  ZHANG Xuefeng
作者单位:Key Laboratory of State Oceanic Adminstration forMarine Environmental Information Technology, NationalMarine Data and Information Service, State Oceanic Administration, Tianjin 300171, China;Naval Ocean Analysis and Prediction Laboratory, Naval Postgraduate School, Monterey, CA, USA;Key Laboratory of State Oceanic Adminstration forMarine Environmental Information Technology, NationalMarine Data and Information Service, State Oceanic Administration, Tianjin 300171, China;Key Laboratory of State Oceanic Adminstration forMarine Environmental Information Technology, NationalMarine Data and Information Service, State Oceanic Administration, Tianjin 300171, China;Key Laboratory of State Oceanic Adminstration forMarine Environmental Information Technology, NationalMarine Data and Information Service, State Oceanic Administration, Tianjin 300171, China;Key Laboratory of State Oceanic Adminstration forMarine Environmental Information Technology, NationalMarine Data and Information Service, State Oceanic Administration, Tianjin 300171, China
基金项目:The National Natural Science Foundation of China under contract Nos 41030854, 41106005, 41176003, and 41206178; the National Science and Technology Support Program of China under contract No. 2011BAC03B02-01-04.
摘    要:The impact of assimilating Argo data into an initial field on the short-term forecasting accuracy of temper- ature and salinity is quantitatively estimated by using a forecasting system of the western North Pacific, on the base of the Princeton ocean model with a generalized coordinate system (POMgcs). This system uses a sequential multigrid three-dimensional variational (3DVAR) analysis scheme to assimilate observation da- ta. Two numerical experiments were conducted with and without Argo temperature and salinity profile data besides conventional temperature and salinity profile data and sea surface height anomaly (SSHa) and sea surface temperature (SST) in the process of assimilating data into the initial fields. The forecast errors are estimated by using independent temperature and salinity profiles during the forecasting period, including the vertical distributions of the horizontally averaged root mean square errors (H-RMSEs) and the horizontal distributions of the vertically averaged mean errors (MEs) and the temporal variation of spatially averaged root mean square errors (S-RMSEs). Comparison between the two experiments shows that the assimila- tion of Argo data significantly improves the forecast accuracy, with 24% reduction of H-RMSE maximum for the temperature, and the salinity forecasts are improved more obviously, averagely dropping of 50% for H-RMSEs in depth shallower than 300 m. Such improvement is caused by relatively uniform sampling of both temperature and salinity from the Argo drifters in time and space.

关 键 词:Argo资料  短期预测  数据同化  西北太平洋  初始场  均方根误差  普林斯顿海洋模式  海表温度
收稿时间:2012/2/17 0:00:00
修稿时间:2012/11/13 0:00:00

Improvement of short-termforecasting in the northwest Pacific through assimilating Argo data into initial fields
FU Hongli,CHU Peter C,HAN Guijun,HE Zhongjie,LI Wei,ZHANG Xuefeng.Improvement of short-termforecasting in the northwest Pacific through assimilating Argo data into initial fields[J].Acta Oceanologica Sinica,2013,32(7):57-65.
Authors:FU Hongli  CHU Peter C  HAN Guijun  HE Zhongjie  LI Wei and ZHANG Xuefeng
Institution:1.Key Laboratory of State Oceanic Adminstration forMarine Environmental Information Technology, NationalMarine Data and Information Service, State Oceanic Administration, Tianjin 300171, China2.Naval Ocean Analysis and Prediction Laboratory, Naval Postgraduate School, Monterey, CA, USA
Abstract:The impact of assimilating Argo data into an initial field on the short-term forecasting accuracy of temperature and salinity is quantitatively estimated by using a forecasting system of the western North Pacific, on the base of the Princeton ocean model with a generalized coordinate system (POMgcs). This system uses a sequential multigrid three-dimensional variational (3DVAR) analysis scheme to assimilate observation data. Two numerical experiments were conducted with and without Argo temperature and salinity profile data besides conventional temperature and salinity profile data and sea surface height anomaly (SSHa) and sea surface temperature (SST) in the process of assimilating data into the initial fields. The forecast errors are estimated by using independent temperature and salinity profiles during the forecasting period, including the vertical distributions of the horizontally averaged root mean square errors (H-RMSEs) and the horizontal distributions of the vertically averaged mean errors (MEs) and the temporal variation of spatially averaged root mean square errors (S-RMSEs). Comparison between the two experiments shows that the assimilation of Argo data significantly improves the forecast accuracy, with 24% reduction of H-RMSE maximum for the temperature, and the salinity forecasts are improved more obviously, averagely dropping of 50% for H-RMSEs in depth shallower than 300 m. Such improvement is caused by relatively uniform sampling of both temperature and salinity from the Argo drifters in time and space.
Keywords:data assimilation  Argo data  western North Pacific  ocean prediction
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