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This study aims to simulate the extraordinary flash flood event that occurred in Egypt from November 1-2, 1994, and evaluate the RegCM3 model's capability to capture the severe mesoscale processes responsible for this storm. The model was set up with different resolutions (40 km and 60 km) and employed various convective and cumulus schemes. The analysis includes synoptic situations and precipitation observations for the specified dates, providing insights into the storm's dynamics and the model's effectiveness in simulating such extreme weather events.
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Flash Flood Simulation over Egyptusing RegCM3 Dr. H. Hasanean Abdel Tawab Shalaby Bakr A.M. Badawy
Objective • The aim of the work to simulate the flash flood of November 1-2,1994, and study the ability of the RegCM3 to describe the sever mesoscale process responsible for development of the unusually intensive Storm of November 1-2, 1994
Model Setup • Domain Area: • (20° W to 45° E & 15° S to 40° N) cover EgyptArea • Case Study: • Flash Flood Event ( 1,2 November 1994 ) • Two Simulations:, • 40 km Resolution • 60 Km Resolution • Different Convective and Cumulus Schemes: • Arakawa-Schubert & Anthes-Kuo • Arakawa-Schubert & Scheme Grell • Fritsch-Chappell & Anthes-Kuo • Fritsch-Chappell & Scheme Grell
SLP_Obs. 01/11/1994 Synoptic Situation Precipitation 01/11/1994 Z500_Obs. 01/11/1994
SLP_Obs. 02/11/1994 Synoptic Situation Precipitation 02/11/1994 Z500_Obs. 02/11/1994
Arakawa-Schubert Convective Scheme& Anthes-Kuo Cumulus Scheme dx= 40 Km dx= 60 Km
Arakawa-Schubert Convective Scheme& Grell Cumulus Scheme dx= 40 Km dx= 60 Km
Fritsch-Chappell Convective Scheme & Anthes-Kuo Cumulus Scheme dx= 40 Km dx= 60 Km
Fritsch-Chappell Convective Scheme & Grell Cumulus Scheme dx= 40 Km dx= 60 Km