Abstract
A research is carried out to examine the effects of cloud-scale flow on drop growth and investigate if accretion alone can produce raindrops of sizes similar to those observed by the aircraft. A simple lagrangian collection model is used to produce drop-growth trajectory analyses using temporally evolving dual-Doppler-derived wind fields, interpolated to a three-dimensional grid. Radial velocity measurements are first synthesized on a Cartesian grid every 2.5 to 5 minutes. Drop trajectories are initialized at various positions in the lower part of the cloud. A range of initial droplet sizes between 30 and 100 mm diameter are used. The gridded velocity are interpolated to the position of the particle using a four-dimensional interpolating scheme. The interpolated values are then used in a first-order-accurate forward-in-time integration scheme to calculate drop-growth trajectories.
Original language | English (US) |
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Pages | 470-472 |
Number of pages | 3 |
State | Published - 1995 |
Event | Proceedings of the 1995 27th Conference on Radar Meteorology - Vail, CO, USA Duration: Oct 9 1995 → Oct 13 1995 |
Other
Other | Proceedings of the 1995 27th Conference on Radar Meteorology |
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City | Vail, CO, USA |
Period | 10/9/95 → 10/13/95 |
ASJC Scopus subject areas
- General Engineering