Difference between revisions of "KDP estimation"
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The LROSE method for estimating KDP is based on an updated version of the technique developed by Hubbert and Bringi (1995). | The LROSE method for estimating KDP is based on an updated version of the technique developed by Hubbert and Bringi (1995). | ||
| − | An Iterative Filtering Technique for the Analysis of | + | Hubbert, J. and V.N. Bringi, 1995: An Iterative Filtering Technique for the Analysis of Copolar Differential Phase and Dual-Frequency Radar Measurements. J. Atmos. Oceanic Technol., 12, 643–648. [https://journals.ametsoc.org/doi/pdf/10.1175/1520-0426%281995%29012%3C0643%3AAIFTFT%3E2.0.CO%3B2 Link] |
Revision as of 00:04, 25 February 2020
The LROSE procedure to estimating KDP from PHIDP
Basics
KDP is estimated from the range derivative of PHIDP. PHIDP accumulates along a radar beam as it passes through a precipitating medium and estimating KDP can identify regions of large phase shifts.
The LROSE method for estimating KDP is based on an updated version of the technique developed by Hubbert and Bringi (1995).
Hubbert, J. and V.N. Bringi, 1995: An Iterative Filtering Technique for the Analysis of Copolar Differential Phase and Dual-Frequency Radar Measurements. J. Atmos. Oceanic Technol., 12, 643–648. Link