Download presentation
Presentation is loading. Please wait.
Published byNora Wells Modified over 9 years ago
1
Desertification and Aeolian Sediment Transport in India
2
Climates of India -Area of Rajasthan is predominantly desert or an arid climate. -Climate is heavily influenced by monsoon season. -32% of land facing threat of desertification
3
-Upward eddie wind currents of greater than 3km/h can lift silt and very fine sand up to 4km
4
Causes of Desertification
9
The Himalayan Water Grab
10
The Source ●Half world’s population dependent ●Historical land and border disputes ●Dynamic and evolving systems o Hydrologically and o Politically ●Seasonal fluctuations and vulnerabilities
11
Observer
12
Complexities of Sediment Load ●Limited Knowledge ●Climatic evolution ●Anthropogenic effects ●Intrabasin and regional variability ●Source/sink dynamics
13
Gangetic river system 2,390tons/km 2 annually Tropical river system 216tons/km 2 annually Sediment delivery influenced primarily by climatic conditions Sediment delivery influenced by climate and anthropogenic factors
14
Heavily decreased sediment loads
15
Erosion/deposition equilibrium Aggrading environment Decreased flow “Hungry water” High erosion rate
16
Subsidence from oil extraction Decreasing sediment loads Decreasing deltaic aggradation Rising sea level
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.