Zonal circulation in the NW Atlantic and Caribbean from a meridional WorldOcean Circulation Experiment hydrographic section at 66 degrees W

A World Ocean Circulation experiment Hydrographic Program section along 66 degreesW in the North Atlantic was made in 1997. In addition to the usual v ariables (hydrographic and tracer) measured in WOCE onetime sections, we ma de lowered acoustic doppler current profiler (LADCP) measurements at nearly all of the stations. The section closed off a portion of the western North Atlantic to the west of the line, making a closed volume for constraining the circulation. In addition, the deep portions of the Caribbean do not com municate with the rest of the basin. By combining mass, silica, and LADCP i nformation as constraints an inverse calculation obtained reveals a strong eastward transport in the Gulf Stream bounded by westward flowing water on either side. Within these energetic flows we see evidence for recently vent ilated Classical Labrador Sea Water, which has not reached the Deep Western Boundary Current north of Puerto Rico in any significant amounts. Within t he Caribbean our major new finding is a deep cyclonic circulation below sil l depth in excess of 100 times the inflow of deep Atlantic water through th e major deep sill: the Anegada-Jungfern Passage. The signature of the deep Atlantic source water is most prominent in CFCs and both a bottom and mid-d epth maximum are present in the Caribbean to the south of Puerto Rico. Off the coast of Venezuela, however, only the deeper CFC maximum is found. For the entire section the net overturning circulation, heat flux, and freshwat er fluxes are all consistent with expectations based on water mass formatio n and air-sea exchanges to the west of our section, but the annual mean air -sea fluxes of heat and freshwater from Comprehensive Ocean-Atmosphere Data Sets appear somewhat too small in comparison with our single-section resul t.