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Role of Gulf Stream frontal eddies in forming phytoplankton patches on the outer southeastern shelf

Journal Article · · Limnol. Oceanogr.; (United States)

Continuous surface mapping of temperature, salinity, and chlorophyll along a 300-km segment of the Gulf Stream cyclonic front defined the spatial scales of a large diatom patch that persisted throughout a 10-day study. The patch was localized in the upwelled cold core of a Gulf Stream frontal eddy centered over the 200-m isobath off Jacksonville, Florida, in April 1979. The 2 ..mu..g.liter/sup -1/ surface chlorophyll isopleth enclosed in area >1,000 km/sup 2/ with an alongshore dimension of 130 km. Surface chlorophyll exceeded 5 ..mu..g.liter/sup -1/ within the upwelled cold core of the eddy, 10-100x higher than concentrations in Gulf Stream or resident shelf surface water. Diatoms dominated the patch with the maximum observed abundance >10/sup 6/ cells.liter/sup -1/. Several days after the initial shipboard mapping, the size, location, and strong chlorophyll gradients of the patch were confirmed with a surface chlorophyll image generated from an ocean color scanner (OCS) flown aboard a NASA U-2 aircraft. We show that the upwelling associated with eddies forming along the Gulf Stream cyclonic front results in localized zones of high near-surface production and plant biomass that lie adjacent to oligotrophic surface waters of the Gulf Stream.

OSTI ID:
5626528
Journal Information:
Limnol. Oceanogr.; (United States), Journal Name: Limnol. Oceanogr.; (United States) Vol. 26:6; ISSN LIOCA
Country of Publication:
United States
Language:
English