meghalaya
No, Kawai is not the wettest place on Earth. Mawsynram in India holds the record for the highest average annual rainfall, receiving over 467 inches of rainfall per year, while Kawai receives around 350 inches annually.
The average rainfall in Eurasia varies by region, ranging from less than 10 inches in some areas to over 60 inches in others. Overall, the average annual precipitation in Eurasia is approximately 27 inches.
Patchy rain refers to rain showers that are scattered or intermittent, occurring in some areas but not in others. It can result in varying amounts of rainfall over a region, with some areas experiencing rain while others remain dry. This type of rainfall pattern is common in unsettled weather conditions.
In Georgia, rainfall amounts tend to increase with higher elevation. This is due to a phenomenon known as orographic precipitation, where moist air is forced to rise over mountains, cool, and condense into rainfall. Therefore, higher elevation areas like the Appalachian Mountains in northern Georgia generally receive more rainfall compared to lower elevation regions in the south.
A precipitation map provides information about rainfall across an area of land. It shows the distribution of rainfall amounts over a specific region, helping to identify areas with high or low precipitation levels. These maps are useful for monitoring and understanding patterns of rainfall for various purposes such as agriculture, water resource management, and climate studies.
Areas that receive over 400 cm of rainfall are rain forests. The areas that receive less than 20 cm of rainfall are desert areas.
cherranpunji
In 1900, areas receiving over sixty inches of annual precipitation primarily produced rice and corn (maize). These crops thrived in the humid, warm climates found in regions such as the southern United States and parts of Southeast Asia, where abundant rainfall supported their growth.
no Depends what you define as being a "rainforest." The marine climate of British Columbia's west coast from the Alaska border right down to the Washington state border produces heavy rainfall in some forested areas that could be classified as "rain forest" (typically receiving over 90 in. of rainfall a year). These forests do support significant black bear populations though they tend to thrive in areas farther inland where the rainfall is around 50-60 in. annually.
Most areas of the desert receive little rainfall, just a few millimeters of precipitation. Some areas have received absolutely no rainfall in over 400 years.
The line drawn on a map to separate two areas with different amounts of rainfall over a specific period of time is called a "rainfall isohyet." Isohyets connect points of equal rainfall, allowing for visual representation of precipitation distribution across a region.
The highest recorded rainfall in Brazil occurred in 1981 in the city of Guaraniaçu, Paraná, where approximately 1,463 millimeters (57.7 inches) fell within a 24-hour period. This extreme event highlights Brazil's diverse climate and the potential for severe weather, particularly in its tropical regions. The Amazon rainforest also experiences significant rainfall, with some areas receiving over 2,000 millimeters (79 inches) annually.
The Cascade Range receives significant rainfall, with some areas experiencing over 100 inches (2,500 mm) annually, particularly on the western slopes. The heavy precipitation is primarily due to orographic lift, where moist air from the Pacific Ocean is forced upward by the mountains, leading to increased rainfall. In contrast, the eastern side of the Cascades is much drier, with some regions receiving less than 20 inches (500 mm) per year.
Antarctica.. a desert is defined by how much rainfall it receives. Although it is made of ice, Antarctica has almost no rainfall per year, some areas have had NO rainfall for thousands of years, so technically, the continent is a desert.
Runoff and rainfall are closely related hydrological processes. When rainfall occurs, some of the water infiltrates the ground, while the excess flows over the surface as runoff, especially in areas where the soil is saturated or impermeable. The amount of runoff generated depends on factors such as the intensity and duration of rainfall, land use, and soil characteristics. In general, higher rainfall amounts can lead to increased runoff, particularly in urbanized or deforested areas.
C. E. Hounam has written: 'Climate of the south west wheat belt of N.S.W. with special reference to rainfall over marginal areas' -- subject- s -: Climate, Rain and rainfall 'Problems of evaporation assessment in the water balance' -- subject- s -: Evaporation - Meteorology -, Water balance - Hydrology - 'Climate of the west Australian wheat belt with special reference to rainfall over marginal areas' -- subject- s -: Climate, Rain and rainfall
The region in Georgia that receives the most annual rainfall is typically the northeastern part of the state, including areas like the Blue Ridge Mountains and the Chattahoochee National Forest. These areas benefit from orographic lifting, which occurs when moist air is forced to rise over elevated terrain, leading to increased rainfall.