Article

 

Covariability of Surface Wind and Stress Responses to Sea Surface Temperature Fronts Public Deposited

Contenu téléchargeable

Télécharger le fichier PDF
https://ir.library.oregonstate.edu/concern/articles/bv73c207f

Descriptions

Attribute NameValues
Creator
Abstract
  • The responses of surface wind and wind stress to spatial variations of sea surface temperature (SST) are investigated using satellite observations of the surface wind from the Quick Scatterometer (QuikSCAT) and SST from the Advanced Microwave Scanning Radiometer on the Advanced Microwave Scanning Radiometer for Earth Observing System (EOS) (AMSR-E) Aqua satellite. This analysis considers the 7-yr period June 2002–May 2009 during which both instruments were operating. Attention is focused in the Kuroshio, North and South Atlantic, and Agulhas Return Current regions. Since scatterometer wind stresses are computed solely as a nonlinear function of the scatterometer-derived 10-m equivalent neutral wind speed (ENW), qualitatively similar responses of the stress and ENW to SST are expected. However, the responses are found to be more complicated on the oceanic mesoscale. First, the stress and ENW are both approximately linearly related to SST, despite a nonlinear relationship between them. Second, the stress response to SST is 2 to 5 times stronger during winter compared to summer, while the ENW response to SST exhibits relatively little seasonal variability. Finally, the stress response to SST can be strong in regions where the ENW response is weak and vice versa. A straightforward algebraic manipulation shows that the stress perturbations are directly proportional to the ENW perturbations multiplied by a nonlinear function of the ambient large-scale ENW. This proportionality explains why both the stress and ENW depend linearly on the mesoscale SST perturbations, while the dependence of the stress perturbations on the ambient large-scale ENW explains both the seasonal pulsing and the geographic variability of the stress response to SST compared with the less variable ENW response.
  • Keywords: Wind stress, Mesoscale processes, Atmosphere-ocean interaction, Satellite observations, Sea surface temperature
Resource Type
DOI
Date Available
Date Issued
Citation
  • O’Neill, Larry W., Dudley B. Chelton, Steven K. Esbensen, 2012: Covariability of Surface Wind and Stress Responses to Sea Surface Temperature Fronts. Journal of Climate, 25, 5916–5942. doi: http://dx.doi.org/10.1175/JCLI-D-11-00230.1
Journal Title
Journal Volume
  • 25
Journal Issue/Number
  • 17
Déclaration de droits
Funding Statement (additional comments about funding)
  • This research was supported by NASA Grants NAS5-32965 and NNX10A098G; Contract 1283973 from the NASA Jet Propulsion Laboratory for funding of Ocean Vector Winds Science Team activities; and Award NA03NES4400001 to Oregon State University’s Cooperative Institute for Oceanographic Satellite Studies from the National Oceanic and Atmospheric Administration, U.S. Department of Commerce. Part of this research was performed while the lead author held a National Research Council Research Associateship Award at the Naval Research Laboratory in Monterey, California.
Publisher
Peer Reviewed
Language
Replaces

Des relations

Parents:

This work has no parents.

Articles