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Technique to Use Satellite Microwave Spectrometer Data in Moisture Budget Studies of Cyclones
Publisher: American Meteorological Society
Abstract: This note focuses on a new method of analysis, suitable for use with data from satellite microwave spectrometers, that may benefit hydrometeorological analysis and prediction. The method being proposed involves application ...
Experiments In Automatic Cloud Tracking Using SMS-GOES Data
Publisher: American Meteorological Society
Abstract: A description is given of the component parts of a computer system for automatically tracking clouds shown by sequences of pictures obtained by geostationary weather satellites. The component programs perform the following ...
Observations of a Colorado Tornado. Part I: Mesoscale Environment and Tornadogenesis
Publisher: American Meteorological Society
Abstract: On 2 July 1987 a nonmesocyclone tornado was observed in northeastern Colorado during the Convection Initiation and Downburst Experiment (CINDE). This tornado, reaching FI?F2 intensity, developed under a rapidly growing ...
Measurement of Clear-Air Gradients and Turbulence Properties with Radar Wind Profilers
Publisher: American Meteorological Society
Abstract: An experiment comparing balloon and profiler observations was carried out to evaluate the capability of Doppler radar wind profilers to remotely measure useful meteorological quantities other than wind. The site chosen was ...
An Electronically Stabilized Phased Array System for Shipborne Atmospheric Wind Profiling
Publisher: American Meteorological Society
Abstract: The design, construction, and first results are presented of a 915-MHz Doppler wind profiler that may be mounted on a moving platform such as a mobile land vehicle, ocean buoy, or a ship. The long dwell times in multiple ...
Contamination of Wind Profiler Data by Migrating Birds: Characteristics of Corrupted Data and Potential Solutions
Publisher: American Meteorological Society
Abstract: Winds measured with 915- and 404-MHz wind profilers are frequently found to have nonrandom errors as large as 15 m s?1 when compared to simultaneously measured rawinsonde winds. Detailed studies of these errors which occur ...