Observational Assessment of Nonlocal Heat Flux Feedback in the North Atlantic by GEFA

Na Wen Key Laboratory of Meteorological Disaster, Ministry of Education, and College of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing, China

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Zhengyu Liu Center for Climate Research, University of Wisconsin—Madison, Madison, Wisconsin

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Qinyu Liu Physical Oceanography Laboratory and College of Physical and Environmental Oceanography, Ocean University of China, Qingdao, China

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Abstract

Most previous studies have proven the local negative heat flux feedback (the surface heat flux response to SST anomalies) in the midlatitude areas. However, it is uncertain whether a nonlocal heat flux feedback can be observed. In this paper, the generalized equilibrium feedback assessment (GEFA) method is employed to examine the full surface turbulent heat flux response to SST in the North Atlantic Ocean using NCEP–NCAR reanalysis data. The results not only confirm the dominant local negative feedback, but also indicate a robust nonlocal positive feedback of the Gulf Stream Extension (GSE) SST to the downstream heat flux in the subpolar region. This nonlocal feedback presents a strong seasonality, with response magnitudes of in winter and in summer. Further study indicates that the nonlocal effect is initiated by the adjustments of the downstream surface wind to the GSE SST anomalies.

Corresponding author address: Dr. Na Wen, College of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044, China. E-mail: wenna@nuist.edu.cn

Abstract

Most previous studies have proven the local negative heat flux feedback (the surface heat flux response to SST anomalies) in the midlatitude areas. However, it is uncertain whether a nonlocal heat flux feedback can be observed. In this paper, the generalized equilibrium feedback assessment (GEFA) method is employed to examine the full surface turbulent heat flux response to SST in the North Atlantic Ocean using NCEP–NCAR reanalysis data. The results not only confirm the dominant local negative feedback, but also indicate a robust nonlocal positive feedback of the Gulf Stream Extension (GSE) SST to the downstream heat flux in the subpolar region. This nonlocal feedback presents a strong seasonality, with response magnitudes of in winter and in summer. Further study indicates that the nonlocal effect is initiated by the adjustments of the downstream surface wind to the GSE SST anomalies.

Corresponding author address: Dr. Na Wen, College of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044, China. E-mail: wenna@nuist.edu.cn
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