Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data

International audience Surface turbulent exchanges play a key role on sea ice dynamics, on ocean and sea ice heat budgets and on the polar atmosphere. Uncertainties in parameterizations of surface turbulent fluxes are mostly held by the transfer coefficients and estimates of those transfer coefficie...

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Published in:Boundary-Layer Meteorology
Main Authors: Blein, Sébastien, Guemas, Virginie, Brooks, Ian, M, Elvidge, Andrew, D, Renfrew, Ian, A
Other Authors: Groupe de Météorologie de Grande Échelle et Climat (GMGEC), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), University of Leeds, University of East Anglia Norwich (UEA), ANR-17-MPGA-0003,ASET,Atmosphere - Sea ice Exchanges and Teleconections(2017), European Project: 101003826,CRiceS
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2024
Subjects:
Online Access:https://hal.science/hal-04554639
https://hal.science/hal-04554639/document
https://hal.science/hal-04554639/file/Blein_et_al_2024.pdf
https://doi.org/10.1007/s10546-023-00851-9
id ftutoulouse3hal:oai:HAL:hal-04554639v1
record_format openpolar
institution Open Polar
collection Université Toulouse III - Paul Sabatier: HAL-UPS
op_collection_id ftutoulouse3hal
language English
topic Bulk parameterizations
Polar regions
Turbulent surface fluxes
Transfer coefficient uncertainties
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
spellingShingle Bulk parameterizations
Polar regions
Turbulent surface fluxes
Transfer coefficient uncertainties
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
Blein, Sébastien
Guemas, Virginie
Brooks, Ian, M
Elvidge, Andrew, D
Renfrew, Ian, A
Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
topic_facet Bulk parameterizations
Polar regions
Turbulent surface fluxes
Transfer coefficient uncertainties
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
description International audience Surface turbulent exchanges play a key role on sea ice dynamics, on ocean and sea ice heat budgets and on the polar atmosphere. Uncertainties in parameterizations of surface turbulent fluxes are mostly held by the transfer coefficients and estimates of those transfer coefficients from field data are required for parameterization development. Measurement errors propagate through the computation of transfer coefficients and contribute to its total error together with the uncertainties in the empirical stability functions used to correct for stability effects. Here we propose a methodology to assess their contributions individually to each coefficient estimate as well as the total drag coefficient uncertainty and we apply this methodology on the example of the SHEBA campaign. We conclude that for most common drag coefficient values (between 1.0 × 10−3 and 2.5 × 10−3), the relative total uncertainty ranges from 25 and 50%. For stable or unstable conditions with a stability parameter |ζ| > 1 on average, the total uncertainty in the neutral drag coefficient exceeds the neutral drag coefficient value itself, while for |ζ| < 1 the total uncertainty is around 25% of the drag coefficient. For closer-to-neutral conditions, this uncertainty is dominated by measurement uncertainties in surface turbulent momentum fluxes which should therefore be the target of efforts in uncertainty reduction. We also propose an objective data-screening procedure for field data, which consists of retaining data for which the relative error on neutral drag coefficient does not exceed a given threshold. This method, in addition to the commonly used flux quality control procedure, allows for a reduction of the drag coefficient dispersion compared to other data-screening methods, which we take as an indication of better dataset quality.
author2 Groupe de Météorologie de Grande Échelle et Climat (GMGEC)
Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
University of Leeds
University of East Anglia Norwich (UEA)
ANR-17-MPGA-0003,ASET,Atmosphere - Sea ice Exchanges and Teleconections(2017)
European Project: 101003826,CRiceS
format Article in Journal/Newspaper
author Blein, Sébastien
Guemas, Virginie
Brooks, Ian, M
Elvidge, Andrew, D
Renfrew, Ian, A
author_facet Blein, Sébastien
Guemas, Virginie
Brooks, Ian, M
Elvidge, Andrew, D
Renfrew, Ian, A
author_sort Blein, Sébastien
title Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
title_short Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
title_full Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
title_fullStr Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
title_full_unstemmed Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
title_sort uncertainties of drag coefficient estimates above sea ice from field data
publisher HAL CCSD
publishDate 2024
url https://hal.science/hal-04554639
https://hal.science/hal-04554639/document
https://hal.science/hal-04554639/file/Blein_et_al_2024.pdf
https://doi.org/10.1007/s10546-023-00851-9
genre Sea ice
genre_facet Sea ice
op_source ISSN: 0006-8314
EISSN: 1573-1472
Boundary-Layer Meteorology
https://hal.science/hal-04554639
Boundary-Layer Meteorology, 2024, 190, &#x27E8;10.1007/s10546-023-00851-9&#x27E9;
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s10546-023-00851-9
info:eu-repo/grantAgreement//101003826/EU/Climate Relevant interactions and feedbacks: the key role of sea ice and Snow in the polar and global climate system/CRiceS
hal-04554639
https://hal.science/hal-04554639
https://hal.science/hal-04554639/document
https://hal.science/hal-04554639/file/Blein_et_al_2024.pdf
doi:10.1007/s10546-023-00851-9
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1007/s10546-023-00851-9
container_title Boundary-Layer Meteorology
container_volume 190
container_issue 2
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spelling ftutoulouse3hal:oai:HAL:hal-04554639v1 2024-09-15T18:35:12+00:00 Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data Blein, Sébastien Guemas, Virginie Brooks, Ian, M Elvidge, Andrew, D Renfrew, Ian, A Groupe de Météorologie de Grande Échelle et Climat (GMGEC) Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) University of Leeds University of East Anglia Norwich (UEA) ANR-17-MPGA-0003,ASET,Atmosphere - Sea ice Exchanges and Teleconections(2017) European Project: 101003826,CRiceS 2024-02-14 https://hal.science/hal-04554639 https://hal.science/hal-04554639/document https://hal.science/hal-04554639/file/Blein_et_al_2024.pdf https://doi.org/10.1007/s10546-023-00851-9 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s10546-023-00851-9 info:eu-repo/grantAgreement//101003826/EU/Climate Relevant interactions and feedbacks: the key role of sea ice and Snow in the polar and global climate system/CRiceS hal-04554639 https://hal.science/hal-04554639 https://hal.science/hal-04554639/document https://hal.science/hal-04554639/file/Blein_et_al_2024.pdf doi:10.1007/s10546-023-00851-9 info:eu-repo/semantics/OpenAccess ISSN: 0006-8314 EISSN: 1573-1472 Boundary-Layer Meteorology https://hal.science/hal-04554639 Boundary-Layer Meteorology, 2024, 190, &#x27E8;10.1007/s10546-023-00851-9&#x27E9; Bulk parameterizations Polar regions Turbulent surface fluxes Transfer coefficient uncertainties [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology info:eu-repo/semantics/article Journal articles 2024 ftutoulouse3hal https://doi.org/10.1007/s10546-023-00851-9 2024-06-25T00:02:29Z International audience Surface turbulent exchanges play a key role on sea ice dynamics, on ocean and sea ice heat budgets and on the polar atmosphere. Uncertainties in parameterizations of surface turbulent fluxes are mostly held by the transfer coefficients and estimates of those transfer coefficients from field data are required for parameterization development. Measurement errors propagate through the computation of transfer coefficients and contribute to its total error together with the uncertainties in the empirical stability functions used to correct for stability effects. Here we propose a methodology to assess their contributions individually to each coefficient estimate as well as the total drag coefficient uncertainty and we apply this methodology on the example of the SHEBA campaign. We conclude that for most common drag coefficient values (between 1.0 × 10−3 and 2.5 × 10−3), the relative total uncertainty ranges from 25 and 50%. For stable or unstable conditions with a stability parameter |ζ| > 1 on average, the total uncertainty in the neutral drag coefficient exceeds the neutral drag coefficient value itself, while for |ζ| < 1 the total uncertainty is around 25% of the drag coefficient. For closer-to-neutral conditions, this uncertainty is dominated by measurement uncertainties in surface turbulent momentum fluxes which should therefore be the target of efforts in uncertainty reduction. We also propose an objective data-screening procedure for field data, which consists of retaining data for which the relative error on neutral drag coefficient does not exceed a given threshold. This method, in addition to the commonly used flux quality control procedure, allows for a reduction of the drag coefficient dispersion compared to other data-screening methods, which we take as an indication of better dataset quality. Article in Journal/Newspaper Sea ice Université Toulouse III - Paul Sabatier: HAL-UPS Boundary-Layer Meteorology 190 2