High frequency fluctuations in the heat content of an ocean general circulation model

The transport and storage of heat by the ocean is of crucial importance because of its effect on ocean dynamics and its impact on the atmosphere, climate and climate change. Unfortunately, limits to the amount of data that can be collected and stored mean that many experimental and modelling studies...

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Main Authors: A. M. Huerta-Casas, D. J. Webb
Format: Article
Language:English
Published: Copernicus Publications 2012-09-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/8/813/2012/os-8-813-2012.pdf
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spelling doaj-f487f51285264ecc9d93a0375e3a983c2020-11-24T22:08:53ZengCopernicus PublicationsOcean Science1812-07841812-07922012-09-018581382510.5194/os-8-813-2012High frequency fluctuations in the heat content of an ocean general circulation modelA. M. Huerta-CasasD. J. WebbThe transport and storage of heat by the ocean is of crucial importance because of its effect on ocean dynamics and its impact on the atmosphere, climate and climate change. Unfortunately, limits to the amount of data that can be collected and stored mean that many experimental and modelling studies of the heat budget have to make use of mean datasets where the effects of short term fluctuations are lost. <br><br> In this paper we investigate the magnitude of the resulting errors by making use of data from OCCAM, a high resolution global ocean model. The model carries out a proper heat balance every time step so any imbalances that are found in the analysis must result from the use of mean fields. <br><br> The study concentrates on two areas of the ocean affecting the El Nino. The first is the region of tropical instability waves north of the Equator. The second is in the upwelling region along the Equator. <br><br> It is shown that in both cases, processes with a period of less than five days can have a significant impact on the heat budget. Thus, analyses using data averaged over five days or more are likely to have significant errors. It is also shown that if a series of instantaneous values is available, reasonable estimates can be made of the size of the errors. In model studies, such values are available in the form of the datasets used to restart the model. In experimental studies they may be in the form of individual unaveraged observations.http://www.ocean-sci.net/8/813/2012/os-8-813-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. M. Huerta-Casas
D. J. Webb
spellingShingle A. M. Huerta-Casas
D. J. Webb
High frequency fluctuations in the heat content of an ocean general circulation model
Ocean Science
author_facet A. M. Huerta-Casas
D. J. Webb
author_sort A. M. Huerta-Casas
title High frequency fluctuations in the heat content of an ocean general circulation model
title_short High frequency fluctuations in the heat content of an ocean general circulation model
title_full High frequency fluctuations in the heat content of an ocean general circulation model
title_fullStr High frequency fluctuations in the heat content of an ocean general circulation model
title_full_unstemmed High frequency fluctuations in the heat content of an ocean general circulation model
title_sort high frequency fluctuations in the heat content of an ocean general circulation model
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2012-09-01
description The transport and storage of heat by the ocean is of crucial importance because of its effect on ocean dynamics and its impact on the atmosphere, climate and climate change. Unfortunately, limits to the amount of data that can be collected and stored mean that many experimental and modelling studies of the heat budget have to make use of mean datasets where the effects of short term fluctuations are lost. <br><br> In this paper we investigate the magnitude of the resulting errors by making use of data from OCCAM, a high resolution global ocean model. The model carries out a proper heat balance every time step so any imbalances that are found in the analysis must result from the use of mean fields. <br><br> The study concentrates on two areas of the ocean affecting the El Nino. The first is the region of tropical instability waves north of the Equator. The second is in the upwelling region along the Equator. <br><br> It is shown that in both cases, processes with a period of less than five days can have a significant impact on the heat budget. Thus, analyses using data averaged over five days or more are likely to have significant errors. It is also shown that if a series of instantaneous values is available, reasonable estimates can be made of the size of the errors. In model studies, such values are available in the form of the datasets used to restart the model. In experimental studies they may be in the form of individual unaveraged observations.
url http://www.ocean-sci.net/8/813/2012/os-8-813-2012.pdf
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