Fig. 2
From: Oceanic eddy with submesoscale edge drives intense air-sea exchanges and beyond
Air-sea interaction differences between two experiments. Horizontal distribution of (a) surface heat flux (SHF), (b) surface moisture flux (SMF), and (c) air-sea transfer coefficient (Ch) in SubMesoE experiment. (d–f) are same as (a–c) but for MesoE experiment. (g–i) show their differences (SubMesoE-MesoE). Gray stripes denote significant values at 95% confidence level based on the Student’s t test. The freedom is calculated based on Satterthwaite’s approximation33. Submesoscale edge induces the stronger air-sea interaction above the eddy.
