Journal
SOLA
Volume 1, Issue -, Pages 205-208Publisher
METEOROLOGICAL SOC JAPAN
DOI: 10.2151/sola.2005-053
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Funding
- Ministry of Education Culture, Sports, Science and Technology (MEXT), Japan [B-2-15340157]
- Kyoto University
- Category 7 of MEXT [RR2002]
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The diurnal variation of precipitation over the Bengal region is numerically investigated using a non-hydrostatic mesoscale model. We focused on northeastern Bangladesh, where the maximum of late night-early morning precipitation is observed. Simulated characteristics of diurnal variation of precipitation agree, to a large extent, with observable evidence. The mechanism of the high late night-early morning precipitation in a case of June 14 to 21 is investigated using the model results. At night, strong southwesterly monsoon winds transport a large amount of moisture over Bangladesh. This high equivalent potential temperature (theta(e)) air mass climbs the slope of the Meghalaya Plateau or climbs over a deep (several hundreds meters to 1 km) pool of cold air, and triggers precipitation over northeastern Bangladesh. The triggered systems develop into mesoscale squall lines and propagate southward or southsouthwestward at a speed of about 10 m s(-1). It is found that the katabatic mountain wind is not a major player in the diurnal variation of precipitation over the northeastern Bangladesh area.
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