| タイトル | High Resolution Observations of Drop Size Distribution for GPM Ground Validation |
| 本文（外部サイト） | http://hdl.handle.net/2060/20120004227 |
| 著者（英） | Phillips, D.W.; Petersen, W.A.; Tokay, A.; Bringi, V.N.; Gatlin, Patrick N.; Wolff, D.B.; Thurai, M.T.; Carey, L. D.; Wingo, M.T. |
| 著者所属（英） | NASA Marshall Space Flight Center |
| 発行日 | 2012-01-22 |
| 言語 | eng |
| 内容記述 | During the Mid-latitude Convective Cloud Experiment (MC3E), NASA's GPM GV Disdrometer and Radar Observations of Precipitation (DROP) Facility deployed an array of disdrometers and rain gauges in northern Oklahoma to sample, with high resolution, the drop size distribution (DSD) for use in development of precipitation retrieval algorithms for the GPM core satellite. The DROP Facility instruments deployed during MC3E consisted of 16 autonomous Parsivel units, 5 two-dimensional video disdrometers (2DVD), a vertical pointing K-band radar and 32 tipping bucket rain gauges. There were several rainfall events during MC3E in which rain drops exceeding 5 mm in diameter were recorded. During a convective rainfall event one of the 2DVDs measured a large rain drop of 8 mm in diameter falling from a convective cell under which several other disdrometers revealed a broad DSD spectrum across this cell and median drop diameter of 3.1 mm. The NPOL radar, which was scanning over the disdrometer array in high resolution RHI mode (every 40 sec), during a stratiform rainfall event revealed a 1 km thick bright band with locally thicker segments that produced rainfall rates of 6-10 mm/hr and indications of DSD modulations as enhanced concentrations of mid-sized rain drops (1.5-3.0 mm) descended below cloud base. These observations are key in characterizing the DSD variability within the 4 km footprint of the GPM Dual-wavelength Precipitation Radar that will provide a global map of precipitation as well as DSD. |
| NASA分類 | Meteorology and Climatology |
| レポートNO | M12-1539 |
| 権利 | Copyright, Distribution as joint owner in the copyright |
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