An Observational and Modeling Study of the Processes Leading to Deep, Moist Convection in Complex Terrain

A case study of orographic convection initiation (CI) that occurred along the eastern slopes of the Vosges Mountains in France on 6 August 2007 during the Convective and Orographically-Induced Precipitation Study (COPS) is presented. Global positioning system (GPS) receivers and two Doppler on Wheel...

Full description

Saved in:
Bibliographic Details
Published in:Monthly weather review 2014-08, Vol.142 (8), p.2687-2708
Main Authors: Weckwerth, T M, Bennett, L J, Miller, L J, Van Baelen, J, Di Girolamo, P, Blythe, A M, Hertneky, T J
Format: Article
Language:English
Subjects:
Atmospheric and Oceanic Physics
Boundary layer flow
Boundary layers
Case studies
Climate
Climatology
Convection
Convective development
Convective precipitation
Convergence
Doppler sonar
Earth Sciences
Easterlies
Floods
Global Positioning System
Global positioning systems
GPS
Hydrology
Mathematical models
Meteorology
Moist convection
Moisture
Moisture effects
Mountains
Numerical simulations
Ocean, Atmosphere
Physics
Positioning systems
Precipitation
Radar
Radiosondes
Sciences of the Universe
Simulation
Slopes
Storms
Temporal variability
Temporal variations
Three dimensional
Uplift
Water vapor
Water vapour
Weather
Weather forecasting
Westerlies
Wind
Wind fields
Winds
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:A case study of orographic convection initiation (CI) that occurred along the eastern slopes of the Vosges Mountains in France on 6 August 2007 during the Convective and Orographically-Induced Precipitation Study (COPS) is presented. Global positioning system (GPS) receivers and two Doppler on Wheels (DOW) mobile radars sampled the preconvective and storm environments and were respectively used to retrieve three-dimensional tomographic water vapor and wind fields. These retrieved data were supplemented with temperature, moisture, and winds from radiosondes from a site in the eastern Rhine Valley. High-resolution numerical simulations with the Weather Research and Forecasting (WRF) Model were used to further investigate the physical processes leading to convective precipitation.
ISSN:0027-0644
1520-0493
DOI:10.1175/MWR-D-13-00216.1