بررسی حجم بارش حاصل از توسعه توفان حاره ای آشوبا بر روی دریای عرب

Tropical storms in the Arabian Sea are one of the phenomena that cause atmospheric anomalies in the region every year. In this research, in order to investigate the amount of precipitation resulting from the formation and development of tropical storm Ashuba, which occurred during June 7-12, 2015, the networked data of the National Center for Environmental Prediction and Atmospheric Sciences (NCEP/NCAR), model data ERA5 and GPM gauge estimated precipitation values were used. The results showed that the main factor in the formation and change of the path of this tropical storm was an abnormal sea surface temperature of more than 1.5 degrees, which caused an increase in power and heat transfer into the circulation system in the Arabian Sea region. With the increase in Balasu currents and also the increase in the relative temperature in the region, torrential rains occurred in most of the western regions of India, the average of which was more than 110 mm.