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Effects of stencil width on surface ocean geostrophic velocity and vorticity estimation from gridded satellite altimeter data Public Deposited

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https://ir.library.oregonstate.edu/concern/articles/v692tc279

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  • This paper examines the effect of “stencil width” on surface ocean geostrophic velocity and vorticity estimated from differentiating gridded satellite altimeter sea surface height products. In oceanographic applications, the value of the first derivative at a central grid point is generally obtained by differencing the sea surface heights at adjacent grid points. This is called a “three-point stencil centered difference”. Here the stencil width is increased from three to five, seven, and nine points, using well-known formulae from the numerical analysis literature. The discrepancies between velocities computed with successive stencils decreases with increasing stencil width, suggesting that wide stencil results are more reliable. Significant speed-dependent biases (up to 10–20%) are found between results computed from three-point stencils versus those computed from wider stencils. The geostrophic velocity, and the variance of geostrophic velocity, are underestimated with thin stencils. Similar results are seen in geostrophic velocities computed from high-resolution model output. In contrast to the case when three-point stencils are used, wider stencils yield estimates of the anisotropy of velocity variance that are insensitive to the differences in grid spacing between two widely used altimeter products. Three-point stencils yield incorrect anisotropies on the 1/4° anisotropic AVISO grid; we recommend the use of 7-point stencils. Despite the demonstrated inadequacies of the three-point stencils, the conclusions of earlier studies based on them, that the zonally averaged midlatitude eddy kinetic energy field is nearly isotropic, are found to pertain also with wider stencils. Finally, the paper also examines the strengths and limitations of applying noise-suppressing differentiators, versus classic centered differences, to altimeter data.
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  • Arbic, B. K., R. B. Scott, D. B. Chelton, J. G. Richman, and J. F. Shriver (2012), Effects of stencil width on surface ocean geostrophic velocity and vorticity estimation from gridded satellite altimeter data, Journal of Geophysical Research, 117, C03029, doi:10.1029/2011JC007367.
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  • 117
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  • C3
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  • B.K.A. acknowledges funding provided by Office of Naval Research grant N00014-11-1-0487 and National Science Foundation (NSF) grants OCE-0924481 and OCE-09607820. R.B.S. acknowledges funding provided by NSF grants OCE-0960834 and OCE-0851457, a contract with the National Oceanography Centre, Southampton, and a NASA subcontract to Boston University. D.B.C.’s contributions to this study were supported by NASAgrant NNX08AR37G. J.F.S. and J.G.R. were supported by the projects“ Global and remote littoral forcing in global ocean models” and “Ageostrophicvorticity dynamics of the ocean”, respectively, both sponsored by theOffice of Naval Research under program element 601153N. This is NRLcontribution NRL/JA/7320-2010-557 and has been approved for public release. This is UTIG contribution 2397.
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  • description.provenance : Made available in DSpace on 2012-04-20T19:02:44Z (GMT). No. of bitstreams: 1 CheltonDudleyCEOASEffectsStencilWidth.pdf: 1840438 bytes, checksum: b4cf9a98aeeb4d06c9efbba73861c974 (MD5) Previous issue date: 2012-03-17
  • description.provenance : Submitted by Deanne Bruner (deanne.bruner@oregonstate.edu) on 2012-04-20T19:02:44Z No. of bitstreams: 1 CheltonDudleyCEOASEffectsStencilWidth.pdf: 1840438 bytes, checksum: b4cf9a98aeeb4d06c9efbba73861c974 (MD5)

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