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This is an accepted version of this page This is the latest accepted revision, reviewed on 20 January 2025. Arid region in India and Pakistan Thar Desert Great Indian Desert Thar Desert in Rajasthan, India Map of the Thar Desert ecoregion Ecology Realm Indomalayan Biome Deserts and xeric shrublands Borders Northwestern thorn scrub forests Rann of Kutch seasonal salt marsh Geography Area ...
Representative deserts include the Sahara Desert in North Africa, the Australian Desert in Western and Southern Australia, Arabian Desert and Syrian Desert in Western Asia, the Kalahari Desert in Southern Africa, Sonoran Desert in the United States and Mexico, Mojave Desert in the United States, Thar Desert in India and Pakistan, Dasht-e Margo ...
Desert National Park is a national park in the Indian state of Rajasthan, near the towns of Jaisalmer and Barmer. It is one of the largest national parks, covering an area of 3,162 km 2 (1,221 sq mi) in the Thar Desert. Sand dunes form around 44% of the park. The major landform consists of craggy rocks and compact salt lake bottoms, intermedial ...
This is a list of the largest deserts in the world by area. ... Thar Desert: Subtropical: 238,254 [6] 77,220: Southern Asia: India and Pakistan: 19 Puntland Desert:
The Thar Desert, also known as the Great Indian Desert, is a large, arid region in the northwestern part of the Indian subcontinent that forms a natural boundary between India and Pakistan. It is the world's 16th largest desert, and the world's 9th largest subtropical desert. 85% of the Thar Desert is in India, and the remaining 15% is in ...
The Thar Desert of Sindh is divided into Nara, Achro, and Thar, all situated in the southern part of Sindh. [3] Historical records indicate that the normal monsoon is around 127.5 mm, but it reached a maximum of 443.9 mm in 2011 due to sudden climatic changes. Water scarcity is prevalent in many areas, leading to limitations in agriculture.
Monsoon deserts are similar. They occur in regions where large temperature differences occur between sea and land. Moist warm air rises over the land, deposits its water content and circulates back to sea. Further inland, areas receive very little precipitation. The Thar Desert near the India/Pakistan border is of this type. [36]
Many deserts, such as the Sahara, are hot year-round, but others, such as East Asia's Gobi Desert, become quite cold during the winter. [1] Temperature extremes are a characteristic of most deserts. High daytime temperatures give way to cold nights because there is no insulation provided by humidity and cloud cover. The diversity of climatic ...