Editorial Type:
Article
Article Type:
Research Article

Predicting Mesoscale Variability of the North Atlantic Using a Physically Motivated Scheme for Assimilating Altimeter and Argo Observations

Yimin Liu Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada

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Keith R. Thompson Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada

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Print Publication:
01 Jul 2009
DOI:
https://doi.org/10.1175/2008MWR2625.1
Page(s):
2223–2237
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Abstract

A computationally efficient scheme is described for assimilating sea level measured by altimeters and vertical profiles of temperature and salinity measured by Argo floats. The scheme is based on a transformation of temperature, salinity, and sea level into a set of physically meaningful variables for which it is easier to specify spatial covariance functions. The scheme also allows for sequential correction of temperature and salinity biases and online estimation of background error covariance parameters. Two North Atlantic applications, both focused on predicting mesoscale variability, are used to assess the effectiveness of the scheme. In the first application the background is a monthly temperature and salinity climatology and skill is assessed by how well the scheme recovers Argo profiles that were not assimilated. In the second application the backgrounds are short-term forecasts made by an eddy-permitting model of the North Atlantic. Skill is assessed by the quality of forecasts with lead times of 1–60 days. Both applications show that the scheme has useful skill.

Corresponding author address: Keith Thompson, Department of Oceanography, Dalhousie University, Halifax, NS B3H 4J1, Canada. Email: keith.thompson@dal.ca

Abstract

A computationally efficient scheme is described for assimilating sea level measured by altimeters and vertical profiles of temperature and salinity measured by Argo floats. The scheme is based on a transformation of temperature, salinity, and sea level into a set of physically meaningful variables for which it is easier to specify spatial covariance functions. The scheme also allows for sequential correction of temperature and salinity biases and online estimation of background error covariance parameters. Two North Atlantic applications, both focused on predicting mesoscale variability, are used to assess the effectiveness of the scheme. In the first application the background is a monthly temperature and salinity climatology and skill is assessed by how well the scheme recovers Argo profiles that were not assimilated. In the second application the backgrounds are short-term forecasts made by an eddy-permitting model of the North Atlantic. Skill is assessed by the quality of forecasts with lead times of 1–60 days. Both applications show that the scheme has useful skill.

Corresponding author address: Keith Thompson, Department of Oceanography, Dalhousie University, Halifax, NS B3H 4J1, Canada. Email: keith.thompson@dal.ca

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