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Air-sea fluxes with a focus on heat and momentum

Air-sea fluxes with a focus on heat and momentum
Air-sea fluxes with a focus on heat and momentum
Turbulent and radiative exchanges of heat between the ocean and atmosphere (hereafter heat fluxes), ocean surface wind stress, and state variables used to estimate them, are Essential Ocean Variables (EOVs) and Essential Climate Variables (ECVs) influencing weather and climate. This paper describes an observational strategy for producing 3-hourly, 25-km (and an aspirational goal of hourly at 10-km) heat flux and wind stress fields over the global, ice-free ocean with breakthrough 1-day random uncertainty of 15 W m–2 and a bias of less than 5 W m–2. At present this accuracy target is met only for OceanSITES reference station moorings and research vessels (RVs) that follow best practices. To meet these targets globally, in the next decade, satellite-based observations must be optimized for boundary layer measurements of air temperature, humidity, sea surface temperature, and ocean wind stress. In order to tune and validate these satellite measurements, a complementary global in situ flux array, built around an expanded OceanSITES network of time series reference station moorings, is also needed. The array would include 500–1000 measurement platforms, including autonomous surface vehicles, moored and drifting buoys, RVs, the existing OceanSITES network of 22 flux sites, and new OceanSITES expanded in 19 key regions. This array would be globally distributed, with 1–3 measurement platforms in each nominal 10° by 10° box. These improved moisture and temperature profiles and surface data, if assimilated into Numerical Weather Prediction (NWP) models, would lead to better representation of cloud formation processes, improving state variables and surface radiative and turbulent fluxes from these models. The in situ flux array provides globally distributed measurements and metrics for satellite algorithm development, product validation, and for improving satellite-based, NWP and blended flux products. In addition, some of these flux platforms will also measure direct turbulent fluxes, which can be used to improve algorithms for computation of air-sea exchange of heat and momentum in flux products and models. With these improved air-sea fluxes, the ocean’s influence on the atmosphere will be better quantified and lead to improved long-term weather forecasts, seasonal-interannual-decadal climate predictions, and regional climate projections.
2296-7745
Cronin, Meghan F.
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Gentemann, Chelle L.
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Edson, James
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Ueki, Iwao
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Bourassa, Mark
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Brown, Shannon
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Clayson, Carol Anne
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Fairall, Chris W.
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Farrar, J. Thomas
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Gille, Sarah T.
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Gulev, Sergey
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Josey, Simon A.
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Kato, Seiji
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Katsumata, Masaki
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Kent, Elizabeth
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Krug, Marjolaine
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Minnett, Peter J.
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Parfitt, Rhys
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Stackhouse, Paul W.
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Swart, Sebastiaan
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Tomita, Hiroyuki
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Weller, A. Robert
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Yoneyama, Kunio
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Yu, Lisan
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Zhang, Dongxiao
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Cronin, Meghan F.
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Gentemann, Chelle L.
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Edson, James
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Ueki, Iwao
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Bourassa, Mark
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Brown, Shannon
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Clayson, Carol Anne
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Fairall, Chris W.
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Farrar, J. Thomas
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Gille, Sarah T.
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Gulev, Sergey
a3e41450-397a-4cf2-b06d-157b4b7e06ba
Josey, Simon A.
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Kato, Seiji
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Katsumata, Masaki
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Kent, Elizabeth
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Krug, Marjolaine
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Minnett, Peter J.
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Parfitt, Rhys
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Pinker, Rachel T.
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Stackhouse, Paul W.
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Swart, Sebastiaan
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Tomita, Hiroyuki
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Vandemark, Douglas
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Weller, A. Robert
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Yoneyama, Kunio
fa119e5d-dc70-4fb4-acb7-9fcbedcd39a5
Yu, Lisan
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Zhang, Dongxiao
7b055a82-004f-4a9b-8e1d-c83809dbf235

Cronin, Meghan F., Gentemann, Chelle L., Edson, James, Ueki, Iwao, Bourassa, Mark, Brown, Shannon, Clayson, Carol Anne, Fairall, Chris W., Farrar, J. Thomas, Gille, Sarah T., Gulev, Sergey, Josey, Simon A., Kato, Seiji, Katsumata, Masaki, Kent, Elizabeth, Krug, Marjolaine, Minnett, Peter J., Parfitt, Rhys, Pinker, Rachel T., Stackhouse, Paul W., Swart, Sebastiaan, Tomita, Hiroyuki, Vandemark, Douglas, Weller, A. Robert, Yoneyama, Kunio, Yu, Lisan and Zhang, Dongxiao (2019) Air-sea fluxes with a focus on heat and momentum. Frontiers in Marine Science, 6. (doi:10.3389/fmars.2019.00430).

Record type: Article

Abstract

Turbulent and radiative exchanges of heat between the ocean and atmosphere (hereafter heat fluxes), ocean surface wind stress, and state variables used to estimate them, are Essential Ocean Variables (EOVs) and Essential Climate Variables (ECVs) influencing weather and climate. This paper describes an observational strategy for producing 3-hourly, 25-km (and an aspirational goal of hourly at 10-km) heat flux and wind stress fields over the global, ice-free ocean with breakthrough 1-day random uncertainty of 15 W m–2 and a bias of less than 5 W m–2. At present this accuracy target is met only for OceanSITES reference station moorings and research vessels (RVs) that follow best practices. To meet these targets globally, in the next decade, satellite-based observations must be optimized for boundary layer measurements of air temperature, humidity, sea surface temperature, and ocean wind stress. In order to tune and validate these satellite measurements, a complementary global in situ flux array, built around an expanded OceanSITES network of time series reference station moorings, is also needed. The array would include 500–1000 measurement platforms, including autonomous surface vehicles, moored and drifting buoys, RVs, the existing OceanSITES network of 22 flux sites, and new OceanSITES expanded in 19 key regions. This array would be globally distributed, with 1–3 measurement platforms in each nominal 10° by 10° box. These improved moisture and temperature profiles and surface data, if assimilated into Numerical Weather Prediction (NWP) models, would lead to better representation of cloud formation processes, improving state variables and surface radiative and turbulent fluxes from these models. The in situ flux array provides globally distributed measurements and metrics for satellite algorithm development, product validation, and for improving satellite-based, NWP and blended flux products. In addition, some of these flux platforms will also measure direct turbulent fluxes, which can be used to improve algorithms for computation of air-sea exchange of heat and momentum in flux products and models. With these improved air-sea fluxes, the ocean’s influence on the atmosphere will be better quantified and lead to improved long-term weather forecasts, seasonal-interannual-decadal climate predictions, and regional climate projections.

Text
fmars-06-00430
Available under License Creative Commons Attribution.
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Accepted/In Press date: 5 July 2019
Published date: 31 July 2019

Identifiers

Local EPrints ID: 432962
URI: http://eprints.soton.ac.uk/id/eprint/432962
ISSN: 2296-7745
PURE UUID: 5d1d658d-d4a3-40f3-91f5-408481df2146

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Date deposited: 05 Aug 2019 16:30
Last modified: 16 Mar 2024 03:18

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Contributors

Author: Meghan F. Cronin
Author: Chelle L. Gentemann
Author: James Edson
Author: Iwao Ueki
Author: Mark Bourassa
Author: Shannon Brown
Author: Carol Anne Clayson
Author: Chris W. Fairall
Author: J. Thomas Farrar
Author: Sarah T. Gille
Author: Sergey Gulev
Author: Simon A. Josey
Author: Seiji Kato
Author: Masaki Katsumata
Author: Elizabeth Kent
Author: Marjolaine Krug
Author: Peter J. Minnett
Author: Rhys Parfitt
Author: Rachel T. Pinker
Author: Paul W. Stackhouse
Author: Sebastiaan Swart
Author: Hiroyuki Tomita
Author: Douglas Vandemark
Author: A. Robert Weller
Author: Kunio Yoneyama
Author: Lisan Yu
Author: Dongxiao Zhang

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