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dc.contributor.authorKöpp, F.
dc.contributor.authorSchwiesow, R. L.
dc.contributor.authorWerner, Ch
dc.date.accessioned2017-06-09T13:59:56Z
dc.date.available2017-06-09T13:59:56Z
dc.date.copyright1984/01/01
dc.date.issued1984
dc.identifier.issn0733-3021
dc.identifier.otherams-10648.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145788
dc.description.abstractWe have demonstrated practical measurement of profiles of horizontal wind magnitude and direction to altitudes of 750 m by making radial velocity measurements with a Doppler lidar using conical scanning. Comparison with surface anemometers and with profiles measured by balloon sondes allows one to evaluate the consistency between lidar measurements and more conventional sensors. Overall we find a correlation coefficient of 0.83 and an rms difference of 1.3 m s?1 for magnitude and a correlation coefficient of 0.91 and an rms difference of 12° for direction when the lidar and sonde profiles are compared. The differences are not a result of lidar errors because comparisons of 20 s averages between the lidar and a sonic anemometer show a correlation coefficient of 0.98, an rms difference of 0.19 m s?1, and a long-term average difference of 0.05 m s?1 for a single component. Profile differences are attributable to horizontal inhomogeneity in the wind field and uncertainty inherent in balloon sondes. Impaired visibility reduces the effective range of the lidar, and the vertical extent of the lidar sample region increases with height.s
dc.publisherAmerican Meteorological Society
dc.titleRemote Measurements of Boundary-Layer Wind Profiles Using a CW Doppler Lidar
dc.typeJournal Paper
dc.journal.volume23
dc.journal.issue1
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1984)023<0148:RMOBLW>2.0.CO;2
dc.journal.fristpage148
dc.journal.lastpage154
dc.treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 001
dc.contenttypeFulltext


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