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Titlebook: Radar and Atmospheric Science; A Collection of Essa Roger M. Wakimoto,Ramesh Srivastava Book 2003 American Meteorological Society 2003 Atmo

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發(fā)表于 2025-3-23 11:08:05 | 只看該作者
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發(fā)表于 2025-3-23 14:47:24 | 只看該作者
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發(fā)表于 2025-3-24 00:58:47 | 只看該作者
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發(fā)表于 2025-3-24 02:26:25 | 只看該作者
Recent Developments in Observation, Modeling, and Understanding Atmospheric Turbulence and Waves,Doppler radar profilers have come into widespread use, more has been learned about the use of radar as a tool in observing atmospheric turbulence and waves. While much of the paper is devoted to recent developments in observations of turbulence and waves, the review also places these developments in
16#
發(fā)表于 2025-3-24 08:33:44 | 只看該作者
The Assimilation of Radar Data for Weather Prediction,d meteorological fields from Doppler radar observations. For example, Lhermitte and Atlas (1961) and Atlas (1964) described the velocity-azimuth display (VAD) method for determining a horizontally averaged wind profile from single-Doppler radial velocity observations. Lhermitte (1970) developed a me
17#
發(fā)表于 2025-3-24 12:04:23 | 只看該作者
Innovative Signal Utilization and Processing,with it. Its roots are embedded in the branches of mathematics and engineering that deal with the processing of time series data, in our case from received radar echoes. These weak radar echoes contain not only returns from weather (e.g., precipitation), but also a variety of artifacts that we wish
18#
發(fā)表于 2025-3-24 15:38:09 | 只看該作者
Global and Local Precipitation Measurements by Radar,radar for precipitation estimation is that measurements can be made over large areas, with either fairly high temporal and spatial resolution or extensive spatial coverage (about 10 000 km. for ground-based radars and an order of magnitude more for space-based radars). To sample the area covered by
19#
發(fā)表于 2025-3-24 21:04:24 | 只看該作者
Cloud Microphysical Properties, Processes, and Rainfall Estimation Opportunities,nships is revisited, this time from the combined approach of rain-forming physical processes that shape the RDSD, and a formulation of the RDSD into the simplest free parameters of the rain intensity ., rainwater content ., and median volume drop diameter .. This is accomplished through a theoretica
20#
發(fā)表于 2025-3-25 02:06:01 | 只看該作者
Some Educational Innovations in Radar Meteorology,e educational activities in academia and is purposely limited to the mid-1950s onward. The review is influenced by the personal experiences of the authors, in particular, through their experiences at their graduate institutions (S. Rutledge, University of Washington; V. Chandrasekar, Colorado State
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