Controls of topographic Rossby wave properties and downslope transport in dense overflows ...

<!--!introduction!--> Antarctic Bottom Water is primarily formed via overflows of dense shelf water (DSW) around the Antarctic continental margins. The dynamics of these overflows therefore influence the global abyssal stratification and circulation. Previous studies indicate that dense overfl...

Full description

Bibliographic Details
Main Authors: Han, Xianxian, Wang, Zhaomin
Format: Article in Journal/Newspaper
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-0330
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016134
id ftdatacite:10.57757/iugg23-0330
record_format openpolar
spelling ftdatacite:10.57757/iugg23-0330 2023-06-11T04:07:07+02:00 Controls of topographic Rossby wave properties and downslope transport in dense overflows ... Han, Xianxian Wang, Zhaomin 2023 https://dx.doi.org/10.57757/iugg23-0330 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016134 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Oral ConferencePaper Article 2023 ftdatacite https://doi.org/10.57757/iugg23-0330 2023-05-02T10:27:28Z <!--!introduction!--> Antarctic Bottom Water is primarily formed via overflows of dense shelf water (DSW) around the Antarctic continental margins. The dynamics of these overflows therefore influence the global abyssal stratification and circulation. Previous studies indicate that dense overflows can be unstable, energizing Topographic Rossby Waves (TRW) over the continental slope. However, it remains unclear how the wavelength and frequency of the TRWs are related to the properties of the overflowing DSW and other environmental conditions, and how the TRW properties influence the downslope transport of DSW. This study uses idealized high-resolution numerical simulations to investigate the dynamics of overflow-forced TRWs and the associated downslope transport of DSW. It is shown that the propagation of TRWs is constrained by the geostrophic along-slope flow speed of the DSW and by the dynamics of linear plane waves, allowing the wavelength and frequency of the waves to be predicted a priori . The rate ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Article in Journal/Newspaper Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> Antarctic Bottom Water is primarily formed via overflows of dense shelf water (DSW) around the Antarctic continental margins. The dynamics of these overflows therefore influence the global abyssal stratification and circulation. Previous studies indicate that dense overflows can be unstable, energizing Topographic Rossby Waves (TRW) over the continental slope. However, it remains unclear how the wavelength and frequency of the TRWs are related to the properties of the overflowing DSW and other environmental conditions, and how the TRW properties influence the downslope transport of DSW. This study uses idealized high-resolution numerical simulations to investigate the dynamics of overflow-forced TRWs and the associated downslope transport of DSW. It is shown that the propagation of TRWs is constrained by the geostrophic along-slope flow speed of the DSW and by the dynamics of linear plane waves, allowing the wavelength and frequency of the waves to be predicted a priori . The rate ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Article in Journal/Newspaper
author Han, Xianxian
Wang, Zhaomin
spellingShingle Han, Xianxian
Wang, Zhaomin
Controls of topographic Rossby wave properties and downslope transport in dense overflows ...
author_facet Han, Xianxian
Wang, Zhaomin
author_sort Han, Xianxian
title Controls of topographic Rossby wave properties and downslope transport in dense overflows ...
title_short Controls of topographic Rossby wave properties and downslope transport in dense overflows ...
title_full Controls of topographic Rossby wave properties and downslope transport in dense overflows ...
title_fullStr Controls of topographic Rossby wave properties and downslope transport in dense overflows ...
title_full_unstemmed Controls of topographic Rossby wave properties and downslope transport in dense overflows ...
title_sort controls of topographic rossby wave properties and downslope transport in dense overflows ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-0330
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016134
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-0330
_version_ 1768379781185798144