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dc.contributor.authorLander, Mark
dc.contributor.authorSadler, James C.
dc.contributor.authorMaliekal, Jose
dc.contributor.authorHori, Arnold
dc.date.accessioned2021-09-07T17:37:58Z
dc.date.available2021-09-07T17:37:58Z
dc.date.issued1989-09-01
dc.identifier.citationLander, M.A., J.C. Sadler, J.A. Maliekal , and Hori, A., 1989, Tropical Wind Stress from Time-Averaged Winds, J. Appl. Meteor. , 28 (9), 904-912. Available on publisher's site at http://journals.ametsoc.org/doi/abs/10.1175/1520-0450%281989%29028%3C0904%3ATWSFTA%3E2.0.CO%3B2
dc.identifier.doihttps://doi.org/10.1175/1520-0450(1989)028<0904:TWSFTA>2.0.CO;2
dc.identifier.urihttp://hdl.handle.net/20.500.12648/2192
dc.descriptionCopyright 1989 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyright@ametsoc.org.
dc.description.abstractOceanwide direct measurement of the surface wind stress is impracticable; instead, the wind stress must be parameterized in terms of individual shipboard wind reports. The number of ship observations, however, are insufficient over the tropical oceans for an adequate analysis of the wind stress. A method is developed to take advantage of the monthly mean wind field which can be determined by meshing several sources of data with the ship observations. It is shown that a single empirical correction factor can be used to estimate the surface pseudostress from monthly mean winds for all months throughout the oceanic tropics.
dc.titleTropical Wind Stress from Time-Averaged Winds
dc.typearticle
dc.source.journaltitleJournal of Applied Meteorology
dc.source.volume28
dc.source.issue9
refterms.dateFOA2021-09-07T17:37:58Z
dc.description.institutionSUNY Brockport
dc.source.peerreviewedTRUE
dc.source.statuspublished
dc.description.publicationtitleEarth Sciences Faculty Publications
dc.contributor.organizationThe College at Brockport
dc.contributor.organizationUniversity of Hawaii, Honolulu
dc.languate.isoen_US


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