Submesoscale streamers exchange water on the north wall of the Gulf Stream
The Gulf Stream is a major conduit of warm surface water from the tropics to the subpolar North Atlantic. Here we observe and simulate a submesoscale (<20 km) mechanism by which the Gulf Stream exchanges water with subpolar water to the north. Along isopycnals, the front has a sharp compensated t...
Main Authors: | , , , , , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English unknown |
Published: |
John Wiley & Sons, Inc.
|
Subjects: | |
Online Access: | https://ir.library.oregonstate.edu/concern/articles/vh53x1362 |
id |
ftoregonstate:ir.library.oregonstate.edu:vh53x1362 |
---|---|
record_format |
openpolar |
spelling |
ftoregonstate:ir.library.oregonstate.edu:vh53x1362 2024-09-15T18:23:18+00:00 Submesoscale streamers exchange water on the north wall of the Gulf Stream Klymak, Jody M. Shearman, R. Kipp Gula, Jonathan Lee, Craig M. D'Asaro, Eric A. Thomas, Leif N. Harcourt, Ramsey R. Shcherbina, Andrey Y. Sundermeyer, Miles A. Molemaker, Jeroen McWilliams, James C. https://ir.library.oregonstate.edu/concern/articles/vh53x1362 English [eng] eng unknown John Wiley & Sons, Inc. https://ir.library.oregonstate.edu/concern/articles/vh53x1362 Attribution-NonCommercial-NoDerivs 3.0 United States Article ftoregonstate 2024-07-22T18:06:06Z The Gulf Stream is a major conduit of warm surface water from the tropics to the subpolar North Atlantic. Here we observe and simulate a submesoscale (<20 km) mechanism by which the Gulf Stream exchanges water with subpolar water to the north. Along isopycnals, the front has a sharp compensated temperature-salinity contrast, with distinct mixed water between the two water masses 2 and 4 km wide. This mixed water does not increase downstream despite substantial energy available for mixing. A series of streamers detrain this water at the crest of meanders. Subpolar water replaces the mixed water and resharpens the front. The water mass exchange accounts for a northward flux of salt of 0.5–2.5 psu m² s⁻¹, (large-scale diffusivity O (100 m² s⁻¹)). This is similar to bulk-scale flux estimates of 1.2 psu m² s⁻¹ and supplies fresher water to the Gulf Stream required for the production of 18° subtropical mode water. Keywords: ocean mixing, eddies, Gulf Stream, submesoscale mixing Article in Journal/Newspaper North Atlantic ScholarsArchive@OSU (Oregon State University) |
institution |
Open Polar |
collection |
ScholarsArchive@OSU (Oregon State University) |
op_collection_id |
ftoregonstate |
language |
English unknown |
description |
The Gulf Stream is a major conduit of warm surface water from the tropics to the subpolar North Atlantic. Here we observe and simulate a submesoscale (<20 km) mechanism by which the Gulf Stream exchanges water with subpolar water to the north. Along isopycnals, the front has a sharp compensated temperature-salinity contrast, with distinct mixed water between the two water masses 2 and 4 km wide. This mixed water does not increase downstream despite substantial energy available for mixing. A series of streamers detrain this water at the crest of meanders. Subpolar water replaces the mixed water and resharpens the front. The water mass exchange accounts for a northward flux of salt of 0.5–2.5 psu m² s⁻¹, (large-scale diffusivity O (100 m² s⁻¹)). This is similar to bulk-scale flux estimates of 1.2 psu m² s⁻¹ and supplies fresher water to the Gulf Stream required for the production of 18° subtropical mode water. Keywords: ocean mixing, eddies, Gulf Stream, submesoscale mixing |
format |
Article in Journal/Newspaper |
author |
Klymak, Jody M. Shearman, R. Kipp Gula, Jonathan Lee, Craig M. D'Asaro, Eric A. Thomas, Leif N. Harcourt, Ramsey R. Shcherbina, Andrey Y. Sundermeyer, Miles A. Molemaker, Jeroen McWilliams, James C. |
spellingShingle |
Klymak, Jody M. Shearman, R. Kipp Gula, Jonathan Lee, Craig M. D'Asaro, Eric A. Thomas, Leif N. Harcourt, Ramsey R. Shcherbina, Andrey Y. Sundermeyer, Miles A. Molemaker, Jeroen McWilliams, James C. Submesoscale streamers exchange water on the north wall of the Gulf Stream |
author_facet |
Klymak, Jody M. Shearman, R. Kipp Gula, Jonathan Lee, Craig M. D'Asaro, Eric A. Thomas, Leif N. Harcourt, Ramsey R. Shcherbina, Andrey Y. Sundermeyer, Miles A. Molemaker, Jeroen McWilliams, James C. |
author_sort |
Klymak, Jody M. |
title |
Submesoscale streamers exchange water on the north wall of the Gulf Stream |
title_short |
Submesoscale streamers exchange water on the north wall of the Gulf Stream |
title_full |
Submesoscale streamers exchange water on the north wall of the Gulf Stream |
title_fullStr |
Submesoscale streamers exchange water on the north wall of the Gulf Stream |
title_full_unstemmed |
Submesoscale streamers exchange water on the north wall of the Gulf Stream |
title_sort |
submesoscale streamers exchange water on the north wall of the gulf stream |
publisher |
John Wiley & Sons, Inc. |
url |
https://ir.library.oregonstate.edu/concern/articles/vh53x1362 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://ir.library.oregonstate.edu/concern/articles/vh53x1362 |
op_rights |
Attribution-NonCommercial-NoDerivs 3.0 United States |
_version_ |
1810463490688679936 |