Validation of NCEP and OAFlux air-sea heat fluxes using observations from a Black Pearl wave glider |
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Authors: | Huabin Mao Xiujun Sun Chunhua Qiu Yusen Zhou Hong Liang Hongqiang Sang Ying Zhou Ying Chen |
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Affiliation: | Ocean College,Zhejiang University,Zhoushan 316021,China;Key Laboratory of Science and Technology on Operational Oceanography,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301,China;Key Laboratory of Physical Oceanography,Ministry of Education,Qingdao 266100,China;Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266237,China;School of Marine Sciences,Sun Yat-sen University,Guangzhou 510275,China;School of Mechanical Engineering,Tiangong University,Tianjin 300387,China;Tianjin Key Laboratory of Advanced Mechatronic Equipment Technology,Tiangong University,Tianjin 300387,China;Institute for Advanced Ocean Study,Ocean University of China,Qingdao 266100,China;Ocean College,Zhejiang University,Zhoushan 316021,China |
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Abstract: | Latent and sensible heat fluxes based on observations from a Black Pearl wave glider were estimated along the main stream of the Kuroshio Current from the East China Sea to the east coast of Japan, from December 2018 to January 2019. It is found that the data obtained by the wave glider were comparable to the sea surface temperature data from the Operational Sea Surface Temperature and Sea Ice Analysis and the wind field data from WindSat. The Coupled Ocean Atmosphere Response Experiment 3.0 (COARE 3.0) algorithm was used to calculate the change in air-sea turbulent heat flux along the Kuroshio. The averaged latent heat flux (LHF) and sensible heat flux (SHF) were 235 W/m2 and 134 W/m2, respectively, and the values in the Kuroshio were significant larger than those in the East China Sea. The LHF and SHF obtained from Objectively Analyzed Air-Sea Fluxes for the Global Oceans (OAFlux) were closer to those measured by the wave glider than those obtained from National Centers for Environmental Prediction (NCEP) reanalysis products. The maximum deviation occurred in the East China Sea and the recirculation zone of the Kuroshio (deviation of SHF >200 W/m2; deviation of LHF >400 W/m2). This indicates that the NCEP and OAFlux products have large biases in areas with complex circulation. The wave glider has great potential to observe air-sea heat fluxes with a complex circulation structure. |
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Keywords: | wave glider air-sea heat flux Kuroshio observation |
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