Surface frontogenesis by surface heat fluxes in the upstream Kuroshio Extension region.

ABSTRACT: Western boundary currents bring warm tropical water poleward and eastward and are characterized by a sharp sea surface temperature (SST) front on the poleward edge of the current as it extends into the interior basin. One of the most prominent such front is associated with the Kuroshio Extension (KE) as it extends east of Japan ("upstream KE"). Large latent and sensible heat fluxes that warm the atmosphere and cool the ocean project this front into the atmosphere, thereby affecting weather and climate both locally and remotely. While one might assume that these larger surface heat fluxes on the equatorward side would tend to damp the SST front, here we present observational evidence that the surface heat loss actually strengthens the front during October-April in monthly climatology and ab

SUBMITTER: Tozuka T 

PROVIDER: S-EPMC5579054 | biostudies-literature | 2017 Aug

REPOSITORIES: biostudies-literature