Difference between revisions of "World Cultures Portfolio/South Asia"
From ThePlaz.com
(→Sources: fix spelling) |
(remove to-be verbs - only 2! must have edited before!) |
||
Line 15: | Line 15: | ||
As one moves south-west towards Southwest Asia, one moves into the tropics. This region us wetter and receives significantly more rain. Larger populations also crowd this wetter region. For the most part this region borders South East Asia and receives about 200-400 inches per year with some spots receiving up to 400 inches per year (Textbook). | As one moves south-west towards Southwest Asia, one moves into the tropics. This region us wetter and receives significantly more rain. Larger populations also crowd this wetter region. For the most part this region borders South East Asia and receives about 200-400 inches per year with some spots receiving up to 400 inches per year (Textbook). | ||
− | The western ghats also receive a lot of rain. This occurs because of the normal rain-trapping properties of the mountains, which | + | The western ghats also receive a lot of rain. This occurs because of the normal rain-trapping properties of the mountains, which occurs all over the globe. |
In the middle of Sri Lanka, Mount Pidurutalagala receives an excess of 400 inches of rain per year. On the map a small spot of dark green shows the mountains peak. Again the mountains are what cause this small sport of heavy rain. | In the middle of Sri Lanka, Mount Pidurutalagala receives an excess of 400 inches of rain per year. On the map a small spot of dark green shows the mountains peak. Again the mountains are what cause this small sport of heavy rain. | ||
− | The rain levels in India vary along with the season. In January, India receives almost no rain except in the southern and north-eastern corners (Encarta Map). However, the story in July differs greatly (Encarta Map). Rainfalls heavily during the summer, especially in the north-eastern corner. However, there's one fluke. A dry patch exists just west of the northern tip of Sri Lanka (Encarta Map). Unfortunately | + | The rain levels in India vary along with the season. In January, India receives almost no rain except in the southern and north-eastern corners (Encarta Map). However, the story in July differs greatly (Encarta Map). Rainfalls heavily during the summer, especially in the north-eastern corner. However, there's one fluke. A dry patch exists just west of the northern tip of Sri Lanka (Encarta Map). Unfortunately no explanation could arose. |
Commonly a monsoon gets defined as the rain and wind which comes from southwest India during different seasons (Wikipedia). However, a monsoon, properly defined, represents a wind pattern that reverses direction with the seasons (Wikipedia). And change with the seasons it does, as it can pour inches of rain in the few months from July to September (Baldauf). This provides almost all of India's water for the entire year. | Commonly a monsoon gets defined as the rain and wind which comes from southwest India during different seasons (Wikipedia). However, a monsoon, properly defined, represents a wind pattern that reverses direction with the seasons (Wikipedia). And change with the seasons it does, as it can pour inches of rain in the few months from July to September (Baldauf). This provides almost all of India's water for the entire year. |
Revision as of 23:40, 3 January 2007
World Cultures South Asia Report about Rainfall
Intro/Basics - Africa - Middle East - South Asia - China - Japan - Korea - Latin America
World Cultures Daily Questions
Notebook
- Page 56 - South Asia Political Map, Geo Notes
- Page 58 - Indian Ancient Civilization Notes Instructions, Page 2 - Maurya Empire and Small Kingdoms, Page 3 - Gupta Empire and Muslim Empire, Page 4 - Mughal Empire
- Page 59 - Hinduism Questions
- Page 60 - Hindu Basics Notes, Figure
- Page 61 - Wife Burning Article, Page 2, Page 3
- Page 62 - Kumbah Mela Festival Article
- Page 63 - Portfolio Instructions
- Page 64 - Monsoon Picture Assignment
- Page 65 - Comparisons Project Instructions
- Page 66 - Kerosene/Dowry Article
- Page 67 - City of Joy Movie Notes, Page 2, Page 3, Page 4
- Page 67 - City of Joy Truth Path, Page 2
- Page 68 - Rickshaw Article
- Page 69 - More about Truths 1
- Page 70 - Notes on British Imperialism, Page 2
- Page 70 - Gandhi Notes/Video Notes, Page 2, Page 3, Page 4, Page 5
- Page 71 - Tea Seller Article, Truck Driver Article
- Page 72 - Indian Modern Leaders Slides/Notes, Page 2, Page 3, Page 4, Page 5, Page 6, Page 7
- Page 73 - Buddhism Notes Page 1, Page 2, Page 3, Page 4 (Face)
- Page 74 - AIDs in India Article
- Page 75 - Indian Modern Issues
- Page 76 - Kashmir Kite Festival Article
- Page 77 - Kashmir Notes, Page 2
Portfolio
- Portfolio
- Rainfall Map and Report
- South Asia Comparisons Graph
- Postcards
Misc
Test/Quizzes
- South Asia Test Topics
- Lots of Pop-quizzes given - be sure to study constantly and remember all numbers given because quiz questions come from seeming nowhere and cover the smallest bit of minutia
Africa: HDI Graph Reflections - Decolonization Report
Middle East: Population Density Report - Essay: A Peaceful Vacation
South Asia: Rainfall Report - South Asia Comparisons Graph - Postcards
China: Sphere of Influences Report - Mao Button Journal
Japan: Natural Resources Report - Japanese Violence Journal
Korea: Physical Map Report
Latin America: Landforms Report
Worldwide: T-Shirt Trade Report
Rainfall in South Asia varies greatly and has many effects on aspects of South Asian life. Not only does the rainfall map match closely with the climate map, but with the population map. Monsoons have a great deal of effects on the population, morale, and agriculture. India, a large nation, made up of many sections gets affected by many different climates. Dry as deserts, the western side lays, but rain ravages the eastern side. India's rain falls seasonally and unpredictability. But when it differs from it's normal habits, problems, such as floods and droughts emerge.
Various regions and countries make up South Asia. In the north-east lies Afghanistan and Pakistan. Both are very dry, similar to the rest of the Middle East. The Thar Desert exists here, a large dry region in Rajasthan (an Indian state) and Pakistan (Wikipedia). The desert covers 92,200 square miles and receives less then 40 inches of rain per year (WWF via Wikipedia; Textbook). Few people wish to live in this region and thus it's sparsely populated, similar to deserts around the world.
The north-west portion of South Asia contains Nepal, and Bangladesh, among others. The northern part of this region, the part bordering the plains of China, does not receive as much rain, and gets designated "temperate humid" on the Encarta climate map. The region then gets divided into further smaller sub-regions. The largest sub-region climate appears as "winter drought, hot summer." Small different sub-variations with different drought seasons and summer temperatures border this.
As one moves south-west towards Southwest Asia, one moves into the tropics. This region us wetter and receives significantly more rain. Larger populations also crowd this wetter region. For the most part this region borders South East Asia and receives about 200-400 inches per year with some spots receiving up to 400 inches per year (Textbook).
The western ghats also receive a lot of rain. This occurs because of the normal rain-trapping properties of the mountains, which occurs all over the globe.
In the middle of Sri Lanka, Mount Pidurutalagala receives an excess of 400 inches of rain per year. On the map a small spot of dark green shows the mountains peak. Again the mountains are what cause this small sport of heavy rain.
The rain levels in India vary along with the season. In January, India receives almost no rain except in the southern and north-eastern corners (Encarta Map). However, the story in July differs greatly (Encarta Map). Rainfalls heavily during the summer, especially in the north-eastern corner. However, there's one fluke. A dry patch exists just west of the northern tip of Sri Lanka (Encarta Map). Unfortunately no explanation could arose.
Commonly a monsoon gets defined as the rain and wind which comes from southwest India during different seasons (Wikipedia). However, a monsoon, properly defined, represents a wind pattern that reverses direction with the seasons (Wikipedia). And change with the seasons it does, as it can pour inches of rain in the few months from July to September (Baldauf). This provides almost all of India's water for the entire year.
Agriculture powers 70% of India's economy (Baldauf). So when the rains come late, everyone suffers. This causes starvation among the poor villages and hardship in the cities. The rain also partially abates the heat, so when it's missing, everyone feels it (Baldauf). This heat causes a massive demand for air-conditioning, one which the power company can not keep up with. So once again, the lack of rains affect the Indian people.
But as a lack of water brings hardship, so does flooding. Floods, such as the ones near Nepal in 2004 left thousands homeless (Baldauf). Just as flood waters do in the United States, flooding wipes out houses in India, gutting everything in their paths.
So Indians demand a balance of rain each year. But when too much falls, or too little, or not at the right time, Indians suffer. Floods, drought, famine, and power outages can all result from India's haphazard rainfall. In addition, different sections of Inida receive different amounts of rain. This also happens to correspond to the population levels in certain regions.
Sources
- Ahmad, Ifikhar, Herbert Brodsky, Marylee Susan Crofts, and Elisabeth Gaynor Ellis. World Cultures: A Global Mosaic. Upper Saddle River, New Jersey: Prentice Hall, 2001.
- Baldauf, Scott. "India's monsoon: a time of washouts and waiting." The Christian Science Monitor. 20 July 2004. 2 Jan 2007 <http://www.csmonitor.com/2004/0720/p07s01-wosc.html>.
- "South Asia Annual Precipitation Map." Encarta. Microsoft. 17 Dec 2006 <http://encarta.msn.com/encnet/features/MapCenter/MapPrintPreview.aspx?lat=18.3870980570115&long=78.9589470696392&alt=2&mapsize=Medium&mapstyle=precipitationannual&mapstyleselectedindex=9&selectedent=47614&entityname=South%20Asia%20(region),%20Asia>.
- "South Asia Climate Map." Encarta. Microsoft. 17 Dec 2006 <http://encarta.msn.com/encnet/features/MapCenter/MapPrintPreview.aspx?lat=18.3870980570115&long=78.9589470696392&alt=2&mapsize=Medium&mapstyle=climate&mapstyleselectedindex=8&selectedent=47614&entityname=South%20Asia%20(region),%20Asia>.
- "South Asia January Precipitation Map." Encarta. Microsoft. 20 Dec 2006 <http://encarta.msn.com/encnet/features/MapCenter/MapPrintPreview.aspx?lat=18.3870980570115&long=78.9589470696392&alt=2&mapsize=Medium&mapstyle=precipitationjanuary&mapstyleselectedindex=10&selectedent=47614&entityname=>.
- "South Asia July Precipitation Map." Encarta. Microsoft. 20 Dec 2006 <http://encarta.msn.com/encnet/features/mapcenter/map.aspx?TextLatitude=39.45&TextLongitude=-98.907&TextAltitude=0&TextSelectedEntity=39070&SearchEnc=false&MapStyle=Comprehensive&MapSize=Medium&MapStyleSelectedIndex=0&searchTextMap=South+Asia&MapStylesList=Comprehensive&ZoomOnMapClickCheck=on>.
- "South Asia Population Map." Encarta. Microsoft. 17 Dec 2006 <http://encarta.msn.com/encnet/features/MapCenter/MapPrintPreview.aspx?lat=18.3870980570115&long=78.9589470696392&alt=2&mapsize=Medium&mapstyle=population&mapstyleselectedindex=6&selectedent=47614&entityname=South%20Asia%20(region),%20Asia>.
- "Thar Desert." Wikipedia, The Free Encyclopedia. 15 Dec 2006, 10:24 UTC. Wikimedia Foundation, Inc. 17 Dec 2006 <http://en.wikipedia.org/w/index.php?title=Thar_Desert&oldid=94484869>.