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© T. M. Whitmore Today South Asia - Huge & Complex region India, Sri Lanka, Nepal, Bhutan Bangladesh, Pakistan Environment
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© T. M. Whitmore Last time – Questions? East Asia continued Hong Kong (a special case of China) Japan Korea Taiwan (Formosa)
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© T. M. Whitmore S AsiaS Asia: Regions Barriers Regions Himalayas & foothills Himalayas Tectonic landscapes Tectonic Deserts Deserts The Great River valleysGreat River valleys The Deccan PlateauDeccan Coastal & southern lowlandslowlands
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Indus Ganges Brahmaputra E. Ghats Deccan Plateau W. Ghats Indus Ganges Indus Ganges Indus Ganges IndusBrahmaputra Ganges Indus Natural mountain barriers Thar Desert
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The Himalayas
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Himalayan Foothills
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© T. M. Whitmore Tectonic Landscapes Indian plate collision with Eurasian plate Indian plate collision with Eurasian plate Himalaya (and other( Mountain barriers to the N and W => severe earthquake hazard Oct. 2005 Pakistan Earthquake
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Oct.. 2005 7.6 quake
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N
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W. Ghats E. Ghats Deccan Plateau
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The Deccan Plateau
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W Ghats
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The Southern Lowlands
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© T. M. Whitmore Deserts West of Indus R. valley Thar or Great Indian
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The Thar Desert
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Copyright 2005 All Enthusiast, Inc.
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© T. M. Whitmore Great River Valleys Great River valleys Indus Ganges, Gangetic plain Ganges Brahmaputra & the delta (Bangladesh) Brahmaputra Valley population concentration
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Indus Ganges Brahmaputra
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© T. M. Whitmore The Gangetic Plain
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© T. M. Whitmore
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Indus Ganges Brahmaputra
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Bangladesh
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© T. M. Whitmore Climatic regions Dry and semi-arid in W Rainfall variable with elevation, aspect, location, and season Hot tropical and semi-tropical Seasonal progression of temperatures
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© T. M. Whitmore Monsoon The “monsoon” is the summer rainfall regime in most of S Asia and SE Asia The “monsoon” A system of alternating-direction winds Gives rise to “seasons” wet & dry
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Calicut in the W Ghats
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Dominant Wind Patterns in the Winter (October to April) – Dry Season H (Cold) L (Warm) Monsoon Region
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Dominant Wind Patterns in the Summer (April to October) – Wet Season H (Cold) L (Warm) Monsoon Region
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Average Annual Precipitations (in millimeters) Monsoon east Dry continental Gobi Desert Ganges Delta Borneo Raining every day with no dry season Mawsynram, India (467” of rain per year; 11860 mm). Most precipitation on earth
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Monthly precipitation (mm)
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© Pearson Education – Prentice Hall
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© T. M. Whitmore Environmental hazards Tectonic (mentioned already) Climatic Variable monsoons (too little & too much rain) monsoon Tropical cyclones (like our hurricanes) Tropical cyclones Huge populations live in low lying areas (subject to flooding) Huge populations live in low lying areas Human induced Deforestation & Desertification Deforestation Salinization Salinization Global climate change
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Variation in the monsoon Increased variability
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> 13 m
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1999 floods in Bangledesh: Dieter Ludwig/Sipa
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Bangladesh
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In 1991 over 100,000 were killed in a single storm; 300,000 killed by a single storm in 1970. Tropical Cyclones (hurricanes)
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Cyclone Sidr Category 4
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Cyclone Sidr Category 4 11/15/07
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> 13 m
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(Mumbai (Bombay)) >21m > 7m > 15 m
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> 13 m
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Chipko movement activists
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Salinization, caused by salty irrigation water Salinization, caused by high water table
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http://www.nytimes.com/2007/04/03/science/earth/03clim.html?ex=1176436800&en=0fbed4c342b8f550&ei=5070
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