Improved VAD horizontal wind retrievals using high-altitude airborne Doppler radar
Information Technology and Software
Improved VAD horizontal wind retrievals using high-altitude airborne Doppler radar (GSC-TOPS-339)
A high-altitude airborne Doppler radar filter designed to compute profiles of horizontal winds.
Overview
Traditionally, velocity-azimuth display (VAD) wind retrievals are performed using a single rotation of a ground-based or airborne radar antenna. The processed data from this technique contains assumptions about the horizontal and vertical wind conditions which can result in large measurement errors. NASA has innovated a process for utilizing higher data density provided by an airborne radar to ingest more data into each VAD retrieval than the traditional VAD technique while keeping a similar or smaller spatial footprint.
The Technology
Our VAD technique uses four types of scanning (sequential, synthetic, single-scan and multi-scan) to select more representative sample of data points to feed into a VAD horizontal wind retrieval algorithms. The sequential scan and the synthetic scanned are paired together to control how the data is selected. The sequential selection strategies use all data over a given time interval while synthetic selection strategies use all data over a given along-track distance window. The single scan/multi-scan are paired together to control how much data is ingested. The single-scan strategy uses a number of data points equivalent to that of a single scan of the radar beam while a multi-scan strategy uses the equivalent of multiple scans of the radar beam. By utilizing these scanning methods, good data can be isolated from invalid data leading to more accurate measurement of wind properties.
Benefits
- Higher Measurement Accuracy
- Ingests more data over a smaller footprint
Applications
- Weather Monitoring
Technology Details
Information Technology and Software
GSC-TOPS-339
GSC-18554-1
Patent Pending
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