Roughness length variability over heterogeneous surfaces

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Authors
Ellis, Matthew A.
Subjects
Advisors
Wang, Qing
Date of Issue
2010-03
Date
Publisher
Monterey, California. Naval Postgraduate School
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Abstract
Monin-Obukhov similarity theory and the empirical formulae of Businger et al. (1971) and Dyer (1974) are used to calculate roughness lengths and surfacelayer heat fluxes from multilevel observations of wind, temperature, and humidity measured at three locations in the Weather Information Network Display System at Cape Canaveral Air Force Station, Florida. Relationships between roughness length and surface-layer wind speed and direction in varying thermal stability conditions are analyzed during two four-day periods: a diurnally-cycling coastal wind circulation regime on 1-4 June 2008 and the passage of Tropical Storm Fay on 18-21 August 2008. Spatial and temporal variations in roughness lengths for a period of one year are compared to landscape features near the three observation platforms using shadow analysis of satellite photographs. Wind speeds during the coastal wind event remained below 10 ms-1, and roughness lengths calculated from observations below 60 m corresponded to surface roughness elements within about 300 m. At the same height in the tropical storm case, for wind speeds exceeding 20 ms-1, evidence is presented that indicates roughness lengths are related to surface features up to 1.5 km upstream.
Type
Thesis
Description
Series/Report No
Department
Meteorology
Organization
Naval Postgraduate School (U.S.)
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Format
xviii, 77 p. : ill. ;
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Distribution Statement
Approved for public release; distribution is unlimited.
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This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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