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海洋热浪背景下海气湍流热通量资料的评估OA北大核心CSTPCD

Evaluation of air-sea turbulent heat fluxes data under the background of marine heatwaves

中文摘要英文摘要

2019年夏季,东北太平洋地区经历了一次名为"Blob 2.0"的海洋热浪事件,对海洋生态系统造成了严重影响.利用美国国家数据浮标中心的浮标观测资料、全球客观分析通量产品OAFlux,以及大气再分析数据集ERA5、NCEP2和MERRA-2,综合分析了"Blob 2.0"事件期间海气湍流热通量的特征,并研究了其物理因素.浮标观测显示,在"Blob 2.0"事件期间,潜热通量呈现正增长趋势,而感热通量呈现负增长趋势,这一现象可归因于海气比湿度差呈正增长,而风速和海气温差呈负增长.评估结果表明:4种通量数据产品都低估了潜热通量的增长,ERA5的增长率与浮标最为接近.对于感热通量,MERRA-2和NCEP2产品的增长趋势与浮标观测相同,其中MERRA-2的增长率更接近;而OAFlux和ERA5产品的增长趋势与观测相反.

In the summer of 2019,the Northeastern on Pacific region experienced a marine heatwave event called"Blob 2.0",which had a significant impact on the marine ecosystem.This study conducted a comprehensive analysis of the characteristics of air-sea turbulent heat flux during this event using the buoy data from National Data Buoy Center,the global objective flux product OAFlux,and atmospheric reanalysis datasets ERA5,NCEP2 and MERRA-2.The study also investigated the physical factors influencing these fluxes.The buoy observation revealed that during the"Blob 2.0"event,there was a positive increasing trend in latent heat flux,while sensible heat flux exhibited a negative decreasing trend.This phenomenon can be attributed to the positive increase in the air-sea specific humidity difference and the negative decrease in wind speed and air-sea temperature difference.Evaluation results indicated that all four flux data products underestimated the growth of latent heat flux,with ERA5 showing the closest agreement with buoy observation.Regarding sensible heat flux,both MERRA-2 and NCEP2 products exhibited a similar increasing trend as observed by buoys,with MERRA-2 showing a closer growth rate.However,OAFlux and ERA5 products showed an opposite trend compared to the observations.

马婧;宋翔洲;闫运伟;王斌;陈陟

河海大学海洋学院,江苏南京 210024自然资源部国家海洋技术中心,天津 300112国家海洋环境预报中心,北京 100081

海洋学

海洋热浪湍流热通量异常浮标观测通量数据集

marine heatwavesturbulent heat flux anomaliesbuoy observationflux datasets

《海洋预报》 2024 (003)

1-11 / 11

国家自然科学基金项目(42122040、42076016).

10.11737/j.issn.1003-0239.2024.03.001

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