What is the atmospheric pressure condition during summer season over the central part of India

The atmospheric pressure condition during the summer season over the central part of India is characterized by a significant drop in pressure compared to other seasons. This phenomenon can be attributed to the intense heating of the land surface, which leads to the formation of low-pressure areas.

During summer, particularly from March to June, the central region of India experiences high temperatures, which cause the air to rise rapidly. As the warm air ascends, it leaves behind a lower pressure zone at the surface. This low-pressure region attracts winds from surrounding areas, resulting in the southwest monsoon, which typically begins in June.

Furthermore, the high temperatures lead to increased humidity, contributing to the development of thunderstorms and heavy rainfall in some areas. It's essential to note that the variability in local topography can also influence the specific atmospheric conditions experienced across different regions within central India during the summer months. Overall, the dominant feature is the establishment of low pressure due to extreme heat.