Atmospheric Response to the Gulf Stream: Seasonal Variations*

Journal of Climate - Tập 23 Số 13 - Trang 3699-3719 - 2010
Shoshiro Minobe1, Masato Miyashita1, Akira Kuwano‐Yoshida2, Hiroki Tokinaga3, Shang‐Ping Xie3
1Department of Natural History Sciences, Graduate School of Science, Hokkaido University, Sapporo, Japan
2Earth Simulator Center, Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
3International Pacific Research Center and Department of Meteorology, University of Hawaii at Manoa, Honolulu, Hawaii

Tóm tắt

Abstract The atmospheric response to the Gulf Stream front in sea surface temperature is investigated using high-resolution data from satellite observations and operational analysis and forecast. Two types of atmospheric response are observed with different seasonality and spatial distribution. In winter, surface wind convergence is strong over the Gulf Stream proper between Cape Hatteras and the Great Banks, consistent with atmospheric pressure adjustments to sea surface temperature gradients. The surface convergence is accompanied by enhanced precipitation and the frequent occurrence of midlevel clouds. Local evaporation and precipitation are roughly in balance over the Florida Current and the western Gulf Stream proper. In summer, strong precipitation, enhanced high clouds, and increased lightning flash rate are observed over the Florida Current and the western Gulf Stream proper, without seasonal surface convergence enhancement. For the precipitation maximum over the Florida Current, local evaporation supplies about half of the water vapor, and additional moisture is transported from the south on the west flank of the North Atlantic subtropical high. Atmospheric heating estimated by a Japanese reanalysis reveals distinct seasonal variations. In winter, a shallow-heating mode dominates the Gulf Stream proper, with strong sensible heating in the marine atmospheric boundary layer and latent heating in the lower troposphere. In summer, a deep-heating mode is pronounced over the Florida Current and the western Gulf Stream proper, characterized by latent heating in the middle and upper troposphere due to deep convection. Possible occurrences of these heating modes in other regions are discussed.

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