A stochastic model for the turbulent ocean heat flux under Arctic sea ice

Heat flux from the upper ocean to the underside of sea ice provides a key contribution to the evolution of the Arctic sea ice cover. Here, we develop a model of the turbulent ice-ocean heat flux using coupled ordinary stochastic differential equations to model fluctuations in the vertical velocity a...

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Main Authors: Toppaladoddi, S, Wells, AJ
Format: Internet publication
Language:English
Published: 2021
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author Toppaladoddi, S
Wells, AJ
author_facet Toppaladoddi, S
Wells, AJ
author_sort Toppaladoddi, S
collection OXFORD
description Heat flux from the upper ocean to the underside of sea ice provides a key contribution to the evolution of the Arctic sea ice cover. Here, we develop a model of the turbulent ice-ocean heat flux using coupled ordinary stochastic differential equations to model fluctuations in the vertical velocity and temperature in the Arctic mixed layer. All the parameters in the model are determined from observational data. A detailed comparison between the model results and measurements made during the Surface Heat Budget of the Arctic Ocean (SHEBA) project reveals that the model is able to capture the probability density functions (PDFs) of velocity, temperature and heat flux fluctuations. Furthermore, we show that the temperature in the upper layer of the Arctic ocean can be treated as a passive scalar during the whole year of SHEBA measurements. The stochastic model developed here provides a computationally inexpensive way to compute observationally consistent PDF of this heat flux, and has implications for its parametrization in regional and global climate models.
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spelling oxford-uuid:d3dc9db6-7d50-4a92-8cd1-03a7422705ac2022-03-27T08:14:10ZA stochastic model for the turbulent ocean heat flux under Arctic sea iceInternet publicationhttp://purl.org/coar/resource_type/c_7ad9uuid:d3dc9db6-7d50-4a92-8cd1-03a7422705acEnglishSymplectic Elements2021Toppaladoddi, SWells, AJHeat flux from the upper ocean to the underside of sea ice provides a key contribution to the evolution of the Arctic sea ice cover. Here, we develop a model of the turbulent ice-ocean heat flux using coupled ordinary stochastic differential equations to model fluctuations in the vertical velocity and temperature in the Arctic mixed layer. All the parameters in the model are determined from observational data. A detailed comparison between the model results and measurements made during the Surface Heat Budget of the Arctic Ocean (SHEBA) project reveals that the model is able to capture the probability density functions (PDFs) of velocity, temperature and heat flux fluctuations. Furthermore, we show that the temperature in the upper layer of the Arctic ocean can be treated as a passive scalar during the whole year of SHEBA measurements. The stochastic model developed here provides a computationally inexpensive way to compute observationally consistent PDF of this heat flux, and has implications for its parametrization in regional and global climate models.
spellingShingle Toppaladoddi, S
Wells, AJ
A stochastic model for the turbulent ocean heat flux under Arctic sea ice
title A stochastic model for the turbulent ocean heat flux under Arctic sea ice
title_full A stochastic model for the turbulent ocean heat flux under Arctic sea ice
title_fullStr A stochastic model for the turbulent ocean heat flux under Arctic sea ice
title_full_unstemmed A stochastic model for the turbulent ocean heat flux under Arctic sea ice
title_short A stochastic model for the turbulent ocean heat flux under Arctic sea ice
title_sort stochastic model for the turbulent ocean heat flux under arctic sea ice
work_keys_str_mv AT toppaladoddis astochasticmodelfortheturbulentoceanheatfluxunderarcticseaice
AT wellsaj astochasticmodelfortheturbulentoceanheatfluxunderarcticseaice
AT toppaladoddis stochasticmodelfortheturbulentoceanheatfluxunderarcticseaice
AT wellsaj stochasticmodelfortheturbulentoceanheatfluxunderarcticseaice