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Coastal effects on radar propagation in atmospheric ducting conditions

Published online by Cambridge University Press:  22 February 2006

B. W. Atkinson
Affiliation:
Department of Geography, Queen Mary, University of London, London E1 4NS, United Kingdom Email: b.w.atkinson@qmul.ac.uk; mzh@mail.nerc-essc.ac.uk
M. Zhu
Affiliation:
Department of Geography, Queen Mary, University of London, London E1 4NS, United Kingdom Email: b.w.atkinson@qmul.ac.uk; mzh@mail.nerc-essc.ac.uk
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Abstract

Two models were used to assess the effects of coastal characteristics on radar propagation in ducting conditions in the Persian Gulf. The NCAR/Penn State MM5 model simulated atmospheric conditions at a 5-km horizontal spatial and hourly temporal resolution on a day on which observations of ducts existed. The output from this model was input to the AREPS propagation model to produce radar coverage over coastal areas. Four factors influenced radar propagation: the sea breeze; coastal configuration; orography; and ambient wind. The sea breeze alone allowed propagation to extend about 100 km inland in a layer 200 m deep. When the breeze was aided by a following ambient wind the propagation layer extended for 150 km and was 400 m deep. A coastal indentation caused differences in depth and intensity of propagation over a distance of about 30 km parallel to the coast in which the indentation occurred. Steep near-coastal orography blocked radar propagation.

Type
Research Article
Copyright
2006 Royal Meteorological Society

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