The occurrence of rain after summer and winter after rain is a result of
changes in temperature and pressure systems in the Earth’s atmosphere.
which heats up the air near the surface and causes it to rise. This rising air
cools down as it rises higher into the atmosphere, and the moisture in the air
condenses into clouds. When the clouds become saturated with moisture, they
release the moisture as precipitation, such as rain or thunderstorms. This is
why it often rains during the summer months, especially in the tropics and
other regions that have warm and moist conditions.
In contrast, during the winter season, the sun’s energy is weaker and the
Earth’s surface cools down, which causes the air near the surface to sink. This
sinking air compresses and warms up, and the moisture in the air is forced to
condense into clouds. When the clouds become saturated with moisture, they
release the moisture as precipitation, such as snow or ice. This is why it
often snows during the winter months, especially in regions that have cold and
dry conditions.
In summary, rain after summer and winter after rain is due to the changes
in temperature and pressure systems in the Earth’s atmosphere that result from
the differences in the sun’s energy and the Earth’s surface temperature during
the different seasons.