Climate, soils and natural vegetation of Rajasthan
Key facts
- The State Action Plan on Climate Change gives Rajasthan's average annual precipitation as around 570 mm, with most rain during the June-September Indi...
- 19 May 2016: IMD recorded 51.0 degrees Celsius at Phalodi, showing the intensity of Rajasthan's summer heat.
- 19 February 2015: the Soil Health Card Scheme was launched nationally from Suratgarh, Rajasthan, linking soil testing with balanced fertiliser advice.
- India State of Forest Report 2023 records Rajasthan's forest cover at 16,548.21 sq km, equal to 4.84% of the calculated area.
Key Points at a Glance
- 1
CET Graduation syllabus includes Rajasthan geography topics such as climatic conditions, soils, natural vegetation, wildlife and sanctuaries; this topic is in scope.
- 2
Rajasthan's climate is best read through the west-to-south-east rainfall gradient: western Rajasthan is arid to semi-arid, while eastern and southern Rajasthan include semi-arid, sub-humid and humid zones.
- 3
The State Action Plan on Climate Change gives Rajasthan's average annual precipitation as around 570 mm, with most rain during the June-September Indian summer monsoon.
- 4
19 May 2016: IMD recorded 51.0 degrees Celsius at Phalodi, showing the intensity of Rajasthan's summer heat.
- 5
19 February 2015: the Soil Health Card Scheme was launched nationally from Suratgarh, Rajasthan, linking soil testing with balanced fertiliser advice.
- 6
India State of Forest Report 2023 records Rajasthan's forest cover at 16,548.21 sq km, equal to 4.84% of the calculated area.
- 7
Keoladeo Ghana National Park is useful for revision because its Ramsar and UNESCO status links Rajasthan vegetation, wetland ecology and conservation.
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Syllabus Fit and Physical Frame
This topic is within the CET Graduation Level geography block because the current RSSB syllabus lists Rajasthan geography themes such as geological structure and physiographic divisions, climatic conditions and regions, soils, natural vegetation, wildlife and sanctuaries, and water-conservation methods. Read climate, soil and vegetation together: the Aravalli range, the Thar Desert, the eastern plains and the south-eastern plateau create the basic map for most questions.
West of the Aravalli, rainfall is low, daily temperature range is high, sandy and saline tendencies are common, and vegetation is mainly thorny scrub or grassland. East and south-east of the Aravalli, rainfall and river action are stronger, so alluvial, black, red and forest soils become more visible, farming density increases, and dry deciduous vegetation appears more clearly.
For CET, build district links. Jaisalmer, Barmer, Bikaner and Jodhpur point to the arid desert belt. Jaipur, Alwar, Bharatpur and Dausa point to the semi-arid to sub-humid transition. Kota, Bundi, Baran and Jhalawar point to Hadoti, black-soil association and stronger monsoon influence. Udaipur, Sirohi, Dungarpur, Banswara and Pratapgarh point to hilly and relatively wetter southern Rajasthan.
Core cue: Rajasthan is not only desert. From west and north-west towards the south-east, moisture, soil depth and vegetation type change in a clear regional gradient.
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