Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models
The performance of coupled climate models (CCMs) in simulating the hydrographic structure and variability of the northwestern North Atlantic Ocean, in particular the Labrador and Irminger Seas, has been assessed. This area plays an important role in the meridional overturning circulation. Hydrograph...
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ftsouthampton:oai:eprints.soton.ac.uk:348364 2023-07-30T04:05:20+02:00 Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models de Jong, M.F. Drijfhout, S.S. Hazeleger, W. van Aken, H.M. Severijns, C.A. 2009-04 https://eprints.soton.ac.uk/348364/ unknown de Jong, M.F., Drijfhout, S.S., Hazeleger, W., van Aken, H.M. and Severijns, C.A. (2009) Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models. Journal of Climate, 22 (7), 1767-1786. (doi:10.1175/2008JCLI2448.1 <http://dx.doi.org/10.1175/2008JCLI2448.1>). Article PeerReviewed 2009 ftsouthampton https://doi.org/10.1175/2008JCLI2448.1 2023-07-09T21:44:17Z The performance of coupled climate models (CCMs) in simulating the hydrographic structure and variability of the northwestern North Atlantic Ocean, in particular the Labrador and Irminger Seas, has been assessed. This area plays an important role in the meridional overturning circulation. Hydrographic properties of the preindustrial run of eight CCMs used in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) are compared with observations from the World Ocean Circulation Experiment Repeat section 7 (WOCE AR7). The mean and standard deviation of 20 yr of simulated data are compared in three layers, representing the surface waters, intermediate waters, and deep waters. Two models simulate an extremely cold, fresh surface layer with model biases down to ?1.7 psu and ?4.0°C, much larger than the observed ranges of variability. The intermediate and deep layers are generally too warm and saline, with biases up to 0.7 psu and 2.8°C. An analysis of the maximum mixed layer depth shows that the low surface salinity is related to a convective regime restricted to the upper 500 dbar. Thus, intermediate water formed by convection is partly replaced by warmer water from the south. Model biases seem to be caused by the coupling to the atmospheric component of the CCM. Model drift during long spinup periods allows the initially small biases in water mass characteristics to become significant. Biases that develop in the control run are carried over to the twentieth-century runs, which are initialized from the control runs. Article in Journal/Newspaper North Atlantic University of Southampton: e-Prints Soton Journal of Climate 22 7 1767 1786 |
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Open Polar |
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University of Southampton: e-Prints Soton |
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ftsouthampton |
language |
unknown |
description |
The performance of coupled climate models (CCMs) in simulating the hydrographic structure and variability of the northwestern North Atlantic Ocean, in particular the Labrador and Irminger Seas, has been assessed. This area plays an important role in the meridional overturning circulation. Hydrographic properties of the preindustrial run of eight CCMs used in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) are compared with observations from the World Ocean Circulation Experiment Repeat section 7 (WOCE AR7). The mean and standard deviation of 20 yr of simulated data are compared in three layers, representing the surface waters, intermediate waters, and deep waters. Two models simulate an extremely cold, fresh surface layer with model biases down to ?1.7 psu and ?4.0°C, much larger than the observed ranges of variability. The intermediate and deep layers are generally too warm and saline, with biases up to 0.7 psu and 2.8°C. An analysis of the maximum mixed layer depth shows that the low surface salinity is related to a convective regime restricted to the upper 500 dbar. Thus, intermediate water formed by convection is partly replaced by warmer water from the south. Model biases seem to be caused by the coupling to the atmospheric component of the CCM. Model drift during long spinup periods allows the initially small biases in water mass characteristics to become significant. Biases that develop in the control run are carried over to the twentieth-century runs, which are initialized from the control runs. |
format |
Article in Journal/Newspaper |
author |
de Jong, M.F. Drijfhout, S.S. Hazeleger, W. van Aken, H.M. Severijns, C.A. |
spellingShingle |
de Jong, M.F. Drijfhout, S.S. Hazeleger, W. van Aken, H.M. Severijns, C.A. Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models |
author_facet |
de Jong, M.F. Drijfhout, S.S. Hazeleger, W. van Aken, H.M. Severijns, C.A. |
author_sort |
de Jong, M.F. |
title |
Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models |
title_short |
Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models |
title_full |
Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models |
title_fullStr |
Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models |
title_full_unstemmed |
Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models |
title_sort |
simulations of hydrographic properties in the northwestern north atlantic ocean in coupled climate models |
publishDate |
2009 |
url |
https://eprints.soton.ac.uk/348364/ |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
de Jong, M.F., Drijfhout, S.S., Hazeleger, W., van Aken, H.M. and Severijns, C.A. (2009) Simulations of hydrographic properties in the northwestern North Atlantic Ocean in coupled climate models. Journal of Climate, 22 (7), 1767-1786. (doi:10.1175/2008JCLI2448.1 <http://dx.doi.org/10.1175/2008JCLI2448.1>). |
op_doi |
https://doi.org/10.1175/2008JCLI2448.1 |
container_title |
Journal of Climate |
container_volume |
22 |
container_issue |
7 |
container_start_page |
1767 |
op_container_end_page |
1786 |
_version_ |
1772817166789246976 |