Orographic rainfall occurs when moist air is forced to rise over a mountain or hill, leading to cooling and condensation of the moisture in the air. This results in increased rainfall on the windward side of the mountain, while the leeward side experiences a rain shadow effect with drier conditions.
Drought is a condition of insufficient water supply over an extended period of time, leading to dry conditions and water scarcity. This lack of water or rainfall can have detrimental effects on agriculture, ecosystems, and human populations, impacting food production and creating challenges for water management.
14.9 inches of Rainfall.
In south-eastern Mexico, along the Gulf of Mexico coast.
It ranges from 20 inches on the southern coasts to 80 inches in the Alpine regions
Orographic rainfall occurs when moist air is forced to rise over a mountain or hill, leading to cooling and condensation of the moisture in the air. This results in increased rainfall on the windward side of the mountain, while the leeward side experiences a rain shadow effect with drier conditions.
It's all because of the addition of organic matter. When you increase organic matter content to the soil, it increases fertility, and helps better retain moisture.
The instruments commonly used to measure rainfall include rain gauges, tipping bucket rain gauges, and weighing-type rain gauges. Rain gauges measure the amount of precipitation that falls at a specific location over a certain period.
Black volcanic soil and a tropical climate with moderate rainfall are most suitable for crops like coffee, bananas, and pineapples. These conditions provide the necessary nutrients and drainage for these crops to thrive without being waterlogged.
Drought is a condition of insufficient water supply over an extended period of time, leading to dry conditions and water scarcity. This lack of water or rainfall can have detrimental effects on agriculture, ecosystems, and human populations, impacting food production and creating challenges for water management.
- The natural vegetation of South Asia varies from one climate region to another, depending on rainfall and temparation. Long ago most of the region was probaly coverd with forest over the centuries, however trees have been cut down for firewood and shelter and tto create cropland and fields for grazing. Today only about one-sexth of the subentinent is forest of this land much is coverd with low, thorny scrub rather than tall trees. - South Asia's vegetation is affected by altitude, rainfull, and human activity
The Himalayas mountain range influences the rainfall pattern in Pakistan by intercepting the monsoon winds from the south. As these moist winds rise and cool over the mountains, they release moisture in the form of heavy rainfall on the windward side (northern Pakistan), leading to a significant amount of precipitation. The leeward side (southern Pakistan) experiences a rain shadow effect, receiving less rainfall due to the barrier effect of the mountains.