Estimating oceanic heat content change using isotherms

This paper presents a new analysis of ocean heat content changes over the last 50 yr using isotherms by calculating the mean temperature above the 14°C isotherm and the depth of the 14°C isotherm as separate variables. A new quantity called the "relative heat content" ("RHC") is...

Full description

Bibliographic Details
Published in:Journal of Climate
Main Authors: Palmer, Matthew D., Haines, Keith
Format: Article in Journal/Newspaper
Language:English
Published: 2009
Subjects:
Online Access:https://hdl.handle.net/1983/aaa517a8-36f0-4cf3-9f26-1b10105ed84d
https://research-information.bris.ac.uk/en/publications/aaa517a8-36f0-4cf3-9f26-1b10105ed84d
https://doi.org/10.1175/2009JCLI2823.1
http://www.scopus.com/inward/record.url?scp=72149115882&partnerID=8YFLogxK
id ftubristolcris:oai:research-information.bris.ac.uk:publications/aaa517a8-36f0-4cf3-9f26-1b10105ed84d
record_format openpolar
spelling ftubristolcris:oai:research-information.bris.ac.uk:publications/aaa517a8-36f0-4cf3-9f26-1b10105ed84d 2024-02-04T10:02:29+01:00 Estimating oceanic heat content change using isotherms Palmer, Matthew D. Haines, Keith 2009-10 https://hdl.handle.net/1983/aaa517a8-36f0-4cf3-9f26-1b10105ed84d https://research-information.bris.ac.uk/en/publications/aaa517a8-36f0-4cf3-9f26-1b10105ed84d https://doi.org/10.1175/2009JCLI2823.1 http://www.scopus.com/inward/record.url?scp=72149115882&partnerID=8YFLogxK eng eng info:eu-repo/semantics/openAccess Palmer , M D & Haines , K 2009 , ' Estimating oceanic heat content change using isotherms ' , Journal of Climate , vol. 22 , no. 19 , pp. 4953-4969 . https://doi.org/10.1175/2009JCLI2823.1 article 2009 ftubristolcris https://doi.org/10.1175/2009JCLI2823.1 2024-01-11T23:49:12Z This paper presents a new analysis of ocean heat content changes over the last 50 yr using isotherms by calculating the mean temperature above the 14°C isotherm and the depth of the 14°C isotherm as separate variables. A new quantity called the "relative heat content" ("RHC") is introduced, which represents the minimum local heat content change over time, relative to a fixed isotherm. It is shown how mean temperature and isotherm depth changes make separable and additive contributions to changes in RHC. Maps of RHC change between 1970 and 2000 show similar spatial patterns to a traditional fixed-depth ocean heat content change to 220 m. However, the separate contributions to RHC suggest a more spatially uniform contribution from warming above the isotherm, while isotherm depth changes show wind-driven signals, of which some are identifiable as being related to the North Atlantic Oscillation. The time series show that the warming contribution to RHC dominates the global trend, while the depth contribution only dominates on the basin scale in the North Atlantic. The RHC shows minima associated with the major volcanic eruptions (particularly in the Indian Ocean), and these are entirely contributed by mean temperature changes rather than isotherm depth changes. The depth change contributions to RHC are strongly affected by the recently reported XBT fall-rate bias, whereas the mean temperature contributions are not. Therefore, only the isotherm depth change contributions toRHCwill need to be reassessed as fall-rate-corrected data become available. Article in Journal/Newspaper North Atlantic North Atlantic oscillation University of Bristol: Bristol Research Indian Journal of Climate 22 19 4953 4969
institution Open Polar
collection University of Bristol: Bristol Research
op_collection_id ftubristolcris
language English
description This paper presents a new analysis of ocean heat content changes over the last 50 yr using isotherms by calculating the mean temperature above the 14°C isotherm and the depth of the 14°C isotherm as separate variables. A new quantity called the "relative heat content" ("RHC") is introduced, which represents the minimum local heat content change over time, relative to a fixed isotherm. It is shown how mean temperature and isotherm depth changes make separable and additive contributions to changes in RHC. Maps of RHC change between 1970 and 2000 show similar spatial patterns to a traditional fixed-depth ocean heat content change to 220 m. However, the separate contributions to RHC suggest a more spatially uniform contribution from warming above the isotherm, while isotherm depth changes show wind-driven signals, of which some are identifiable as being related to the North Atlantic Oscillation. The time series show that the warming contribution to RHC dominates the global trend, while the depth contribution only dominates on the basin scale in the North Atlantic. The RHC shows minima associated with the major volcanic eruptions (particularly in the Indian Ocean), and these are entirely contributed by mean temperature changes rather than isotherm depth changes. The depth change contributions to RHC are strongly affected by the recently reported XBT fall-rate bias, whereas the mean temperature contributions are not. Therefore, only the isotherm depth change contributions toRHCwill need to be reassessed as fall-rate-corrected data become available.
format Article in Journal/Newspaper
author Palmer, Matthew D.
Haines, Keith
spellingShingle Palmer, Matthew D.
Haines, Keith
Estimating oceanic heat content change using isotherms
author_facet Palmer, Matthew D.
Haines, Keith
author_sort Palmer, Matthew D.
title Estimating oceanic heat content change using isotherms
title_short Estimating oceanic heat content change using isotherms
title_full Estimating oceanic heat content change using isotherms
title_fullStr Estimating oceanic heat content change using isotherms
title_full_unstemmed Estimating oceanic heat content change using isotherms
title_sort estimating oceanic heat content change using isotherms
publishDate 2009
url https://hdl.handle.net/1983/aaa517a8-36f0-4cf3-9f26-1b10105ed84d
https://research-information.bris.ac.uk/en/publications/aaa517a8-36f0-4cf3-9f26-1b10105ed84d
https://doi.org/10.1175/2009JCLI2823.1
http://www.scopus.com/inward/record.url?scp=72149115882&partnerID=8YFLogxK
geographic Indian
geographic_facet Indian
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Palmer , M D & Haines , K 2009 , ' Estimating oceanic heat content change using isotherms ' , Journal of Climate , vol. 22 , no. 19 , pp. 4953-4969 . https://doi.org/10.1175/2009JCLI2823.1
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1175/2009JCLI2823.1
container_title Journal of Climate
container_volume 22
container_issue 19
container_start_page 4953
op_container_end_page 4969
_version_ 1789969177157566464