Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean
Oceanic fronts play a pivotal role in controlling water mass transfer, although little is known about deep frontal structure on appropriate temporal and spatial scales. Here, we present a sequence of calibrated time-lapse images from a three-dimensional seismic survey that straddles the Brazil-Malvi...
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:4765 2023-05-15T18:21:10+02:00 Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean Gunn, Kathryn L. White, Nicholas J. Caulfield, Colm-cille P. 2020-06-15 text http://eprints.esc.cam.ac.uk/4765/ http://eprints.esc.cam.ac.uk/4765/1/gunn-et-al-2020-v8_revision_2_compressed.pdf en eng AGU http://eprints.esc.cam.ac.uk/4765/1/gunn-et-al-2020-v8_revision_2_compressed.pdf Gunn, Kathryn L. and White, Nicholas J. and Caulfield, Colm-cille P. (2020) Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean. Journal of Geophysical Research: Oceans. ISSN 2169-9291 (In Press) 02 - Geodynamics Geophysics and Tectonics Article PeerReviewed 2020 ftucambridgeesc 2020-12-17T23:15:55Z Oceanic fronts play a pivotal role in controlling water mass transfer, although little is known about deep frontal structure on appropriate temporal and spatial scales. Here, we present a sequence of calibrated time-lapse images from a three-dimensional seismic survey that straddles the Brazil-Malvinas Confluence— a significant feature of the merid- ional overturning circulation. Eight vertical transects reveal the evolution of a major front. It is manifest as a discrete planar surface that dips at less than 2 ◦ and is traceable to 1.5–2 km depth. Its shape and surface expression are consistent with sloping isopycnal surfaces of the calculated potential density field and with coeval sea surface tempera- ture measurements, respectively. Within the top ∼1 km, where cold fresh water subducts beneath warm salty water, a series of tilted lenses are banked up against the sharply de- fined front. The largest of these structures is centered at 700 m depth and is cored by cold fresh water. Time-lapse imagery demonstrates that this tilted lens grows and de- cays over nine days. It has a maximum diameter of < 34 ± 0.13 km and a maximum height of < 750±10 m. Beneath 1 km, where horizontal density gradients are negligi- ble, numerous deforming lenses and filaments on length scales of 10–100 km are being swept toward the advecting front. Article in Journal/Newspaper South Atlantic Ocean University of Cambridge, Department of Earth Sciences: ESC Publications |
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Open Polar |
collection |
University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
02 - Geodynamics Geophysics and Tectonics |
spellingShingle |
02 - Geodynamics Geophysics and Tectonics Gunn, Kathryn L. White, Nicholas J. Caulfield, Colm-cille P. Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean |
topic_facet |
02 - Geodynamics Geophysics and Tectonics |
description |
Oceanic fronts play a pivotal role in controlling water mass transfer, although little is known about deep frontal structure on appropriate temporal and spatial scales. Here, we present a sequence of calibrated time-lapse images from a three-dimensional seismic survey that straddles the Brazil-Malvinas Confluence— a significant feature of the merid- ional overturning circulation. Eight vertical transects reveal the evolution of a major front. It is manifest as a discrete planar surface that dips at less than 2 ◦ and is traceable to 1.5–2 km depth. Its shape and surface expression are consistent with sloping isopycnal surfaces of the calculated potential density field and with coeval sea surface tempera- ture measurements, respectively. Within the top ∼1 km, where cold fresh water subducts beneath warm salty water, a series of tilted lenses are banked up against the sharply de- fined front. The largest of these structures is centered at 700 m depth and is cored by cold fresh water. Time-lapse imagery demonstrates that this tilted lens grows and de- cays over nine days. It has a maximum diameter of < 34 ± 0.13 km and a maximum height of < 750±10 m. Beneath 1 km, where horizontal density gradients are negligi- ble, numerous deforming lenses and filaments on length scales of 10–100 km are being swept toward the advecting front. |
format |
Article in Journal/Newspaper |
author |
Gunn, Kathryn L. White, Nicholas J. Caulfield, Colm-cille P. |
author_facet |
Gunn, Kathryn L. White, Nicholas J. Caulfield, Colm-cille P. |
author_sort |
Gunn, Kathryn L. |
title |
Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean |
title_short |
Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean |
title_full |
Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean |
title_fullStr |
Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean |
title_full_unstemmed |
Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean |
title_sort |
time-lapse seismic imaging of oceanic fronts and transient lenses within south atlantic ocean |
publisher |
AGU |
publishDate |
2020 |
url |
http://eprints.esc.cam.ac.uk/4765/ http://eprints.esc.cam.ac.uk/4765/1/gunn-et-al-2020-v8_revision_2_compressed.pdf |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
http://eprints.esc.cam.ac.uk/4765/1/gunn-et-al-2020-v8_revision_2_compressed.pdf Gunn, Kathryn L. and White, Nicholas J. and Caulfield, Colm-cille P. (2020) Time-Lapse Seismic Imaging of Oceanic Fronts and Transient Lenses within South Atlantic Ocean. Journal of Geophysical Research: Oceans. ISSN 2169-9291 (In Press) |
_version_ |
1766200295047561216 |