{"id":87652,"date":"2025-06-01T06:50:34","date_gmt":"2025-06-01T06:50:34","guid":{"rendered":"https:\/\/exam.pscnotes.com\/mcq\/?p=87652"},"modified":"2025-06-01T06:50:34","modified_gmt":"2025-06-01T06:50:34","slug":"inversion-of-rainfall-is-associated-with","status":"publish","type":"post","link":"https:\/\/exam.pscnotes.com\/mcq\/inversion-of-rainfall-is-associated-with\/","title":{"rendered":"‘Inversion of Rainfall” is associated with"},"content":{"rendered":"

‘Inversion of Rainfall” is associated with<\/p>\n

[amp_mcq option1=”Orographic rainfall” option2=”Convectional rainfall” option3=”Cyclonic rainfall (Tropical)” option4=”Cyclonic rainfall (Temperate)” correct=”option1″]<\/p>\n

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\n
This question was previously asked in<\/div>\n
UPSC NDA-1 – 2019<\/div>\n<\/div>\n
Download PDF<\/a>Attempt Online<\/a><\/div>\n<\/div>\n
\n‘Inversion of Rainfall’ is associated with Orographic rainfall.
\n<\/section>\n
\nInversion of rainfall refers to the phenomenon where, in mountainous regions, rainfall increases with altitude up to a certain height (the zone of maximum precipitation), but then decreases above that level. This pattern is typically observed in orographic rainfall, which occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools, leading to condensation and precipitation on the windward slopes. However, at very high altitudes, the amount of moisture in the air may decrease, temperatures become very low, and other factors limit further precipitation, causing the rainfall amount to decrease beyond the optimum level.
\n<\/section>\n
\nConvectional rainfall occurs due to vertical uplift of heated air, often leading to thunderstorms, and doesn’t typically exhibit this specific altitude-dependent inversion pattern across a mountain slope. Cyclonic rainfall (Tropical or Temperate) is associated with large-scale weather systems (low-pressure systems, fronts) where precipitation patterns are influenced by convergence and uplift over broader areas, not primarily by the forced ascent over a single mountain barrier which causes the distinct rainfall profile described as inversion.
\n<\/section>\n","protected":false},"excerpt":{"rendered":"

‘Inversion of Rainfall” is associated with [amp_mcq option1=”Orographic rainfall” option2=”Convectional rainfall” option3=”Cyclonic rainfall (Tropical)” option4=”Cyclonic rainfall (Temperate)” correct=”option1″] This question was previously asked in UPSC NDA-1 – 2019 Download PDFAttempt Online ‘Inversion of Rainfall’ is associated with Orographic rainfall. Inversion of rainfall refers to the phenomenon where, in mountainous regions, rainfall increases with altitude up … <\/p>\n

Detailed Solution‘Inversion of Rainfall” is associated with<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1093],"tags":[1119,1107,1106],"class_list":["post-87652","post","type-post","status-publish","format-standard","hentry","category-upsc-nda-1","tag-1119","tag-the-atmosphere","tag-world-and-physical-geography","no-featured-image-padding"],"yoast_head":"\n'Inversion of Rainfall" is associated with<\/title>\n<meta name=\"description\" content=\"'Inversion of Rainfall' is associated with Orographic rainfall. Inversion of rainfall refers to the phenomenon where, in mountainous regions, rainfall increases with altitude up to a certain height (the zone of maximum precipitation), but then decreases above that level. This pattern is typically observed in orographic rainfall, which occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools, leading to condensation and precipitation on the windward slopes. However, at very high altitudes, the amount of moisture in the air may decrease, temperatures become very low, and other factors limit further precipitation, causing the rainfall amount to decrease beyond the optimum level.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/exam.pscnotes.com\/mcq\/inversion-of-rainfall-is-associated-with\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"'Inversion of Rainfall" is associated with\" \/>\n<meta property=\"og:description\" content=\"'Inversion of Rainfall' is associated with Orographic rainfall. Inversion of rainfall refers to the phenomenon where, in mountainous regions, rainfall increases with altitude up to a certain height (the zone of maximum precipitation), but then decreases above that level. This pattern is typically observed in orographic rainfall, which occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools, leading to condensation and precipitation on the windward slopes. 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