Along-shelf transports across three cross-shelf lines on the continental shelf near Cape Hatteras have been calculated from moored current meter data over a continuous 24 month period in 1992-1994. The along-shelf convergence has been used to infer off-shelf export. Transport and transport convergence have been related to wind and Gulf Stream forcing and to variability in sea level at the coast. The along-shelf transport variability is primarily wind-driven and highly correlated with sea level fluctuations at the coast. Both winds and along-shelf transport exhibit a near-annual period variability. Along-shelf transport is not well correlated with Gulf Stream offshore position. Along-shelf transport convergence is highly correlated with Gulf...
Author Posting. © Sears Foundation for Marine Research, 2008. This article is posted here by permis...
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of Am...
The convergence of different water masses on the shelf and along the shelfbreak, and cross-isobath s...
Along-shelf transports across three cross-shelf lines on the continental shelf near Cape Hatteras ha...
Along-shelf transports across three cross-shelf lines on the continental shelf near Cape Hatteras ha...
The continental shelf circulation north of Cape Hatteras is strongly affected by the proximity of th...
[1] Cross-isobath flow on continental shelves is of interest for a variety of reasons. Near Cape Hat...
Low‐frequency longshore current fluctuations on the continental shelf off Georgia and their relation...
Low‐frequency longshore current fluctuations on the continental shelf off Georgia and their relation...
[1] Cross-isobath flow on continental shelves is of interest for a variety of reasons. Near Cape Hat...
[1] Cross-isobath flow on continental shelves is of interest for a variety of reasons. Near Cape Hat...
The circulation north of Cape Hatteras is complicated by the proximity of the shelfbreak front, the ...
Low‐frequency current and temperature time series from the outer shelf between Cape Canaveral, Flori...
Low‐frequency current and temperature time series from the outer shelf between Cape Canaveral, Flori...
Low‐frequency current and temperature time series from the outer shelf between Cape Canaveral, Flori...
Author Posting. © Sears Foundation for Marine Research, 2008. This article is posted here by permis...
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of Am...
The convergence of different water masses on the shelf and along the shelfbreak, and cross-isobath s...
Along-shelf transports across three cross-shelf lines on the continental shelf near Cape Hatteras ha...
Along-shelf transports across three cross-shelf lines on the continental shelf near Cape Hatteras ha...
The continental shelf circulation north of Cape Hatteras is strongly affected by the proximity of th...
[1] Cross-isobath flow on continental shelves is of interest for a variety of reasons. Near Cape Hat...
Low‐frequency longshore current fluctuations on the continental shelf off Georgia and their relation...
Low‐frequency longshore current fluctuations on the continental shelf off Georgia and their relation...
[1] Cross-isobath flow on continental shelves is of interest for a variety of reasons. Near Cape Hat...
[1] Cross-isobath flow on continental shelves is of interest for a variety of reasons. Near Cape Hat...
The circulation north of Cape Hatteras is complicated by the proximity of the shelfbreak front, the ...
Low‐frequency current and temperature time series from the outer shelf between Cape Canaveral, Flori...
Low‐frequency current and temperature time series from the outer shelf between Cape Canaveral, Flori...
Low‐frequency current and temperature time series from the outer shelf between Cape Canaveral, Flori...
Author Posting. © Sears Foundation for Marine Research, 2008. This article is posted here by permis...
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of Am...
The convergence of different water masses on the shelf and along the shelfbreak, and cross-isobath s...