Diathermal heat transport in a global ocean Model
The rate at which the ocean moves heat from the tropics toward the poles, and from the surface into the interior, depends on diabatic surface forcing and diffusive mixing. These diabatic processes can be isolated by analyzing heat transport in a temperature coordinate (the diathermal heat transport)...
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ftunswworks:oai:unsworks.library.unsw.edu.au:1959.4/unsworks_73548 2024-05-12T08:10:56+00:00 Diathermal heat transport in a global ocean Model Holmes, RM Zika, JD England, MH 2019-01-01 http://hdl.handle.net/1959.4/unsworks_73548 https://doi.org/10.1175/JPO-D-18-0098.1 unknown American Meteorological Society http://purl.org/au-research/grants/arc/DP160103130 http://purl.org/au-research/grants/arc/DP190101173 http://hdl.handle.net/1959.4/unsworks_73548 https://doi.org/10.1175/JPO-D-18-0098.1 metadata only access http://purl.org/coar/access_right/c_14cb CC-BY-NC-ND https://creativecommons.org/licenses/by-nc-nd/4.0/ urn:ISSN:0022-3670 urn:ISSN:1520-0485 Journal of Physical Oceanography, 49, 1, 141-161 14 Life Below Water anzsrc-for: 0405 Oceanography anzsrc-for: 0911 Maritime Engineering journal article http://purl.org/coar/resource_type/c_6501 2019 ftunswworks https://doi.org/10.1175/JPO-D-18-0098.1 2024-04-17T15:36:36Z The rate at which the ocean moves heat from the tropics toward the poles, and from the surface into the interior, depends on diabatic surface forcing and diffusive mixing. These diabatic processes can be isolated by analyzing heat transport in a temperature coordinate (the diathermal heat transport). This framework is applied to a global ocean sea ice model at two horizontal resolutions (1/48 and 1/108) to evaluate the partioning of the diathermal heat transport between different mixing processes and their spatial and seasonal structure. The diathermal heat transport peaks around 228C at 1.6 PW, similar to the peak meridional heat transport. Diffusive mixing transfers this heat from waters above 228C, where surface forcing warms the tropical ocean, to temperatures below 228C where midlatitude waters are cooled. In the control 1/48 simulation, half of the parameterized vertical mixing is achieved by background diffusion, to which sensitivity is explored. The remainder is associated with parameterizations for surface boundary layer, shear instability, and tidal mixing. Nearly half of the seasonal cycle in the peak vertical mixing heat flux is associated with shear instability in the tropical Pacific cold tongue, highlighting this region's global importance. The framework presented also allows for quantification of numerical mixing associated with the model's advection scheme. Numerical mixing has a substantial seasonal cycle and increases to compensate for reduced explicit vertical mixing. Finally, applied to Argo observations the diathermal framework reveals a heat content seasonal cycle consistent with the simulations. These results highlight the utility of the diathermal framework for understanding the role of diabatic processes in ocean circulation and climate. Article in Journal/Newspaper Sea ice UNSW Sydney (The University of New South Wales): UNSWorks Pacific Journal of Physical Oceanography 49 1 141 161 |
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UNSW Sydney (The University of New South Wales): UNSWorks |
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ftunswworks |
language |
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topic |
14 Life Below Water anzsrc-for: 0405 Oceanography anzsrc-for: 0911 Maritime Engineering |
spellingShingle |
14 Life Below Water anzsrc-for: 0405 Oceanography anzsrc-for: 0911 Maritime Engineering Holmes, RM Zika, JD England, MH Diathermal heat transport in a global ocean Model |
topic_facet |
14 Life Below Water anzsrc-for: 0405 Oceanography anzsrc-for: 0911 Maritime Engineering |
description |
The rate at which the ocean moves heat from the tropics toward the poles, and from the surface into the interior, depends on diabatic surface forcing and diffusive mixing. These diabatic processes can be isolated by analyzing heat transport in a temperature coordinate (the diathermal heat transport). This framework is applied to a global ocean sea ice model at two horizontal resolutions (1/48 and 1/108) to evaluate the partioning of the diathermal heat transport between different mixing processes and their spatial and seasonal structure. The diathermal heat transport peaks around 228C at 1.6 PW, similar to the peak meridional heat transport. Diffusive mixing transfers this heat from waters above 228C, where surface forcing warms the tropical ocean, to temperatures below 228C where midlatitude waters are cooled. In the control 1/48 simulation, half of the parameterized vertical mixing is achieved by background diffusion, to which sensitivity is explored. The remainder is associated with parameterizations for surface boundary layer, shear instability, and tidal mixing. Nearly half of the seasonal cycle in the peak vertical mixing heat flux is associated with shear instability in the tropical Pacific cold tongue, highlighting this region's global importance. The framework presented also allows for quantification of numerical mixing associated with the model's advection scheme. Numerical mixing has a substantial seasonal cycle and increases to compensate for reduced explicit vertical mixing. Finally, applied to Argo observations the diathermal framework reveals a heat content seasonal cycle consistent with the simulations. These results highlight the utility of the diathermal framework for understanding the role of diabatic processes in ocean circulation and climate. |
format |
Article in Journal/Newspaper |
author |
Holmes, RM Zika, JD England, MH |
author_facet |
Holmes, RM Zika, JD England, MH |
author_sort |
Holmes, RM |
title |
Diathermal heat transport in a global ocean Model |
title_short |
Diathermal heat transport in a global ocean Model |
title_full |
Diathermal heat transport in a global ocean Model |
title_fullStr |
Diathermal heat transport in a global ocean Model |
title_full_unstemmed |
Diathermal heat transport in a global ocean Model |
title_sort |
diathermal heat transport in a global ocean model |
publisher |
American Meteorological Society |
publishDate |
2019 |
url |
http://hdl.handle.net/1959.4/unsworks_73548 https://doi.org/10.1175/JPO-D-18-0098.1 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
urn:ISSN:0022-3670 urn:ISSN:1520-0485 Journal of Physical Oceanography, 49, 1, 141-161 |
op_relation |
http://purl.org/au-research/grants/arc/DP160103130 http://purl.org/au-research/grants/arc/DP190101173 http://hdl.handle.net/1959.4/unsworks_73548 https://doi.org/10.1175/JPO-D-18-0098.1 |
op_rights |
metadata only access http://purl.org/coar/access_right/c_14cb CC-BY-NC-ND https://creativecommons.org/licenses/by-nc-nd/4.0/ |
op_doi |
https://doi.org/10.1175/JPO-D-18-0098.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
49 |
container_issue |
1 |
container_start_page |
141 |
op_container_end_page |
161 |
_version_ |
1798854483837452288 |