Atmospheric Response to the Gulf Stream Seasonal Variations

• Published in: Journal of climate Vol. 23; no. 13; pp. 3699 - 3719
• Main Authors: Minobe, Shoshiro, Miyashita, Masato, Kuwano-Yoshida, Akira, Tokinaga, Hiroki, Xie, Shang-Ping
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01.07.2010
• Subjects: Atmosphere; Atmospherics; Clouds; Earth, ocean, space; Exact sciences and technology; External geophysics; Gulfs; Marine; Meteorology; Ocean circulation; Ocean currents; Oceans; Precipitation; Seasons; SPECIAL U.S. CLIVAR Western Boundary Currents COLLECTION; Studies; Summer; Wind; Wind velocity; Winter; North Carolina; Cape Hatteras; United States; Atlantic Ocean; Florida Current; North Atlantic; Dare County North Carolina; Gulf Stream; AN, North Atlantic; ANW, USA, North Carolina, Cape Hatteras; ASW, Atlantic, Florida Current; A, Atlantic, Gulf Stream; INW, Japan; ocean currents; Marine atmosphere; Deep convection; Humidity transfer; Summer; clouds; subtropical zone; North America; Convergence; Winter; Reanalysis; high resolution; atmospheric precipitation; Space remote sensing; Satellite observation; Sea surface temperature; atmospheric pressure; Spatial distribution; water vapor; Lightning; warming; evaporation; seasonal variations; Surface wind; Atmospheric electricity
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/2010jcli3359.1

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, ashallow-heating modedominates the Gulf Stream proper, with strong sensible heating in the marine atmospheric boundary layer and latent heating in the lower troposphere. In summer, adeep-heating modeis 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.