The basic objective of this investigation is the determination of the spatial distribution of rainfall in Plateau State. Nigeria. The results show that the greatest amounts of rainfall are obtained in the southern and western parts of the State and on the southern and western margins of the high Plateau in particular. This pattern of rainfall distribution is explained partly by the movements and positions of the ITD (intertropical discontinuity) at various times of the year, and partly by the interplay of the direction of rainbearing south-westerly winds with the physiographic features in the State.
In general, also, the rainfall amounts are higher on the highland parts of the Stale than on the lowlands. Conversely, rainfall variabilities are higher on the lowlands of the State than on the high Plateau. Furthermore, rainfall variabilities are higher at the beginning and at the cessation of rainfalls than in the middle of the rainy season. Examples of implications of high rainfall variability and low probability of receiving certain given threshold amounts of rainfall at different phenological stages of crop developments, are given. These examples serve to substantiate the need for supplementary irrigation facilities in the Slate.
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The central plateau of India, located in the Deccan region, lies in the rain shadow area of the Western Ghats mountain range. This geographical setup hinders the monsoon winds from bringing in sufficient moisture, resulting in scanty rainfall. Additionally, the plateau's high elevation and lack of significant water bodies further contribute to its arid conditions.
On steep hillsides as well as places which have very little rainfall - such as the Tibetan plateau.
From community wells cactus stalks larg rivers or heavy rainfall
In the moderate eastern plateau region, rainfall patterns are influenced by the region's elevation and topography, which can lead to cooler temperatures compared to surrounding areas. Generally, higher rainfall can support more vegetation, which may contribute to localized cooling effects through processes like transpiration. Conversely, lower rainfall can result in drier conditions, potentially leading to higher average temperatures. Overall, there is an interplay between rainfall and temperature that shapes the region's climate and ecology.
The Deccan Plateau is located in the rain shadow region of the Western Ghats mountain range. The Western Ghats block the moisture-laden winds from the Arabian Sea, resulting in decreased rainfall over the plateau. Additionally, the plateau's higher elevation and distance from the coast contribute to its arid climate.
The Indians of the Southwest lived in an arid region, while the Columbia Plateau region received abundant rainfall.
yes
The Indians of the Southwest lived in an arid region, while the Columbia Plateau region received abundant rainfall.
The interior of the Deccan Plateau receives less than 60 cm of rainfall annually due to its location in the rain shadow region, blocked by the Western Ghats from the moisture-bearing southwest monsoon winds. This geographic feature causes the plateau to experience dry conditions and reduced precipitation compared to coastal areas.
The regions in the interior of the Deccan Plateau and the Sahyadris receive low rainfall due to the rain shadow effect. This occurs because the Western Ghats block the moisture-laden winds coming from the Arabian Sea, causing precipitation to fall on the windward side (coastal areas) and leaving the leeward side (interior plateau) relatively dry.
True.