World Ocean Geostrophic Velocity Inverted from World Ocean Atlas 2013 with the P-Vector Method (NCEI Accession 0121576)
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title: World Ocean Geostrophic Velocity Inverted from World Ocean Atlas 2013 with the P-Vector Method (NCEI Accession 0121576)
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Anchor: https://www.ncei.noaa.gov/archive/archive-management-system/OAS/bin/prd/jquery/person/details/4670 Peter C. Chu
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abstract: This dataset comprises 3D gridded climatological fields of geostrophic velocity inverted from World Ocean Atlas-2013 (WOA2013) temperature and salinity fields using the P-vector method. It provides a climatological velocity field that is dynamically compatible to the WOA2013 (T, S) fields. The dataset has the same spatial resolution and temporal variation (annual, monthly, seasonal) as WOA2103 (T, S) fields, but does not cover the equatorial zone (5oS – 5oN) due to the geostrophic balance being the theoretical basis for the P-vector inverse method.
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title: Chu, Peter C. (2020). World ocean annual mean absolute geostrophic velocity on marine geoid of EIGEN-6C4 from WOA13 (NCEI Accession 0208329). NOAA National Centers for Environmental Information. Dataset. https://doi.org/10.25921/3j6v-dw36.
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supplementalInformation: See the following references for more information on the P-vector method and its use in computing these velocity fields: Chu, P.C., 2006: P-Vector Inverse Method. Springer, 605 pp, ISBN 3-540-33384-3. Chu, P.C., 1995: P-vector method for determining absolute velocity from hydrographic data. Journal of Marine Technological Society, 29 (2), 3-14. Chu, P.C., 2000: P-vector spirals and determination of absolute velocities. Journal of Oceanography, 56, 591-599.
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