13 AND 14 AUGUST STILL HEAVY RAIN FORECASTS WEATHER REPORTS
Precipitation is liquid water in the form of droplets that have dropped from atmospheric water vapor and then become heavy enough to fall under gravity. Rain is a major component of the water cycle and is responsible for storing most of the fresh water on Earth. It provides the right conditions for many types of ecosystems, as well as hydroelectric power plants and water for crop irrigation.
The main cause of rainfall production is the increase of humidity with three-dimensional areas of temperature and the contrast of humidity called the weather front. If sufficient moisture and upward motion are present, it is possible to rain from compressed clouds (strong wind waves.), Such as cumulonimbus, which can be arranged in narrow rainbands. In mountainous areas, heavy rainfall is possible where upscale flow is maximized on the side of the terrain wind at high pressure which forces the moist air to condense and rains along the sides of the mountains. To the left of the mountains, the desert climate may exist due to the dry air caused by the downslope flow, which causes the mass of the air to warm and dry. The monsoon trough, or movement of the interglacial convergence
IMPORTANT LINK:-
GUJARATI MAA NEWS VACHAVA CLICK HERE
CLICK HERE TO GET REPORT IN GUJRATI
Precipitation is liquid water in the form of droplets that have dropped from atmospheric water vapor and then become heavy enough to fall under gravity. Rain is a major component of the water cycle and is responsible for storing most of the fresh water on Earth. It provides the right conditions for many types of ecosystems, as well as hydroelectric power plants and water for crop irrigation.
The main cause of rainfall production is the increase of humidity with three-dimensional areas of temperature and the contrast of humidity called the weather front. If sufficient moisture and upward motion are present, it is possible to rain from compressed clouds (strong wind waves.), Such as cumulonimbus, which can be arranged in narrow rainbands. In mountainous areas, heavy rainfall is possible where upscale flow is maximized on the side of the terrain wind at high pressure which forces the moist air to condense and rains along the sides of the mountains. To the left of the mountains, the desert climate may exist due to the dry air caused by the downslope flow, which causes the mass of the air to warm and dry. The monsoon trough, or movement of the interglacial convergence
IMPORTANT LINK:-
GUJARATI MAA NEWS VACHAVA CLICK HERE
CLICK HERE TO GET REPORT IN GUJRATI
