Articles | Volume 15, issue 3
https://doi.org/10.5194/os-15-831-2019
https://doi.org/10.5194/os-15-831-2019
Research article
 | 
28 Jun 2019
Research article |  | 28 Jun 2019

Characterizing ERA-Interim and ERA5 surface wind biases using ASCAT

Maria Belmonte Rivas and Ad Stoffelen

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Cited articles

Belmonte Rivas, M., Stoffelen, A., Verspeek, J., Neyt, X., and Craig, A.: Cone metrics: a new tool for the intercomparison of scatterometer records, IEEE J. Select. Top. Appl. Earth Obs. Remote Sens., 10, 2195–2204, https://doi.org/10.1109/JSTARS.2017.2647842, 2017. 
Booth, J. F., Kwon, Y., Ko, S., Small, R. J., and Msadek, R.: Spatial patterns and intensity of the surface storm tracks in CMIP5 models, J. Climate, 30, 4965–4981, https://doi.org/10.1175/JCLI-D-16-0228.1, 2017. 
Braun, S. A. and Tao, W.: Sensitivity of high-resolution simulations of Hurricane Bob (1991) to planetary boundary layer parameterizations, Mon. Weather Rev., 128, 3941–3961, https://doi.org/10.1175/1520-0493(2000)129<3941:SOHRSO>2.0.CO;2, 2000. 
Chaudhuri, A. H., Ponte, R. M., Forget, G., and Heimbach, P.: A comparison of atmospheric reanalysis surface products over the ocean and implications for uncertainties in air-sea boundary forcing, J. Climate, 26, 153–170, https://doi.org/10.1175/JCLI-D-12-00090.1, 2013. 
Chelton, D. B. and Freilich, M. H.: Scatterometer based assessment of 10-m wind analyses from the operational ECMWF and NCEP numerical weather prediction models, Mon. Weather Rev., 133, 409–429, https://doi.org/10.1175/MWR-2861.1, 2005. 
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Short summary
This paper describes the differences between ocean surface winds provided by ERA reanalyses and satellite scatterometer observations. This work is motivated by the widespread use of reanalysis winds for ocean forcing in marine forecasting centers and the application of observations to characterize reanalysis wind errors, which we conjecture are related to deficiencies in the physics of the underlying assimilating model (insufficient wind variability at high spatial and temporal frequencies).