- Home
- Search Results
- Page 1 of 1
Search for: All records
-
Total Resources4
- Resource Type
-
00000040000
- More
- Availability
-
40
- Author / Contributor
- Filter by Author / Creator
-
-
Galbraith, Eric D. (4)
-
Key, Robert M. (2)
-
Toggweiler, J. R. (2)
-
Bostock, Helen C. (1)
-
Cartapanis, Olivier (1)
-
Curry, William B. (1)
-
DeVries, Tim (1)
-
Druffel, Ellen R. (1)
-
Druffel, Ellen R. M. (1)
-
Filipsson, Helena L. (1)
-
Gottschalk, Julia (1)
-
Herguera, Juan Carlos (1)
-
Hoogakker, Babette (1)
-
Hwang, Jeomshik (1)
-
Jaccard, Samuel L. (1)
-
Kim, Guebuem (1)
-
Kwon, Eun Young (1)
-
Lisiecki, Lorraine E. (1)
-
Lund, David C. (1)
-
Lynch-Stieglitz, Jean (1)
-
- Filter by Editor
-
-
null (1)
-
& Spizer, S. M. (0)
-
& . Spizer, S. (0)
-
& Ahn, J. (0)
-
& Bateiha, S. (0)
-
& Bosch, N. (0)
-
& Brennan K. (0)
-
& Brennan, K. (0)
-
& Chen, B. (0)
-
& Chen, Bodong (0)
-
& Drown, S. (0)
-
& Ferretti, F. (0)
-
& Higgins, A. (0)
-
& J. Peters (0)
-
& Kali, Y. (0)
-
& Ruiz-Arias, P.M. (0)
-
& S. Spitzer (0)
-
& Sahin. I. (0)
-
& Spitzer, S. (0)
-
& Spitzer, S.M. (0)
-
-
Have feedback or suggestions for a way to improve these results?
!
Note: When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher.
Some full text articles may not yet be available without a charge during the embargo (administrative interval).
What is a DOI Number?
Some links on this page may take you to non-federal websites. Their policies may differ from this site.
-
Toggweiler, J. R. ; Druffel, Ellen R. ; Key, Robert M. ; Galbraith, Eric D. ( , Journal of Geophysical Research: Oceans)
-
Toggweiler, J. R. ; Druffel, Ellen R. M. ; Key, Robert M. ; Galbraith, Eric D. ( , Journal of Geophysical Research: Oceans)
Abstract Large volumes of cool water are drawn up to the surface in the tropical oceans. A companion paper shows that the cool water reaches the surface in or near the upwelling zones off northern and southern Africa and Peru. The cool water has a subantarctic origin and spreads extensively across the Atlantic and Pacific basins after it reaches the surface. Here, we look at the spreading in two low‐resolution ocean general circulation models and find that the spreading in the models is much less extensive than observed. The problem seems to be the way the upwelling and the spreading are connected (or not connected) to the ocean's large‐scale overturning. As proposed here, the cool upwelling develops when warm buoyant water in the western tropics is drawn away to become deep water in the North Atlantic. The “drawing away” shoals the tropical thermocline in a way that allows cool subantarctic water to be drawn up to the surface along the eastern margins. The amounts of upwelling produced this way exceed the amounts generated by the winds in the upwelling zones by as much as 4 times. Flow restrictions make it difficult for the warm buoyant water in our models to be drawn away.
-
Schmittner, Andreas ; Bostock, Helen C. ; Cartapanis, Olivier ; Curry, William B. ; Filipsson, Helena L. ; Galbraith, Eric D. ; Gottschalk, Julia ; Herguera, Juan Carlos ; Hoogakker, Babette ; Jaccard, Samuel L. ; et al ( , Paleoceanography)