1. Climate category (1) Made by : Anna, Annie

2. Content East Asia Monsoon Intertropical Convergence Zone –Influence ENSO –Pacific temperature –El Nino and La Nina –Influence to Taiwan Warm winter More spring rain Less typhoon –Southern Oscillation Index

3. Monsoon

4. (Image from: http://sq.k12.com.cn/discuz/attachment.php?aid=63993&noupdate=y es) The monsoon is the wind that changes direction with the seasons.

5. 黑線圍繞的區域是根據二度空間的大氣環流定義出來的亞洲季風 區、非洲季風區和澳洲季風區。暗紅色陰影區則是依地面觀測 定義出來的季風區 。 圖片來源： http://earth.fg.tp.edu.tw/learn/esf/magazine/980303.htm

6. The East Asian monsoon covers the countries like China, Japan, North Korea, South Korea, Taiwan, etc.

7. Do you know why the wind changes direction with the seasons?

8. The sea is harder to be heated or cooled down than the land. So the land temperature drops faster in winter than the sea. The sea temperature is higher than the land temperature in winter. In winter, the density of the colder air above the land is higher than the density of the hotter air above the sea. Therefore, the air goes from the land to the sea. The monsoon forms because of this. How about summer? Why does the summer monsoon go from the sea to the land?

9. This picture shows the directions of the monsoon in winter. The winds are from the continents. It’s usually the dry and cold monsoon. ( Image source: http://earth.fg.tp.edu.tw/learn/esf/magazine/980303.htm)

10. This picture shows the directions of the monsoon in summer. It’s the hot and wet monsoon. It brings a lot of rain. ( Image source ： http://earth.fg.tp.edu.tw/learn/esf/magazine/980303.htm)

11. The storm caused by monsoon ( 圖片 來源： http://zh.wikipedia.org/wiki/File:Bombay_flooded_stree t.jpg)

12. It scopes including the South China Sea and the northwest Pacific rim area.

13. Intertropical Convergence Zone Region: Near the equator, from about 5° north and 5° south ， it effects over land ventures farther north or south than the ITCZ over the oceans, and it causes the variation in land temperatures. Influence: a plethora of precipitation - solar heating in the region forces air to rise through convection which results inprecipitation The ITCZ is a key component of the global circulation system.

14. Influence the northeast, southeast trade winds : the subtropical highs or horse latitudes low pressure zone (ITCZ)trade winds Subtropical high (horse latitude) North east trade winds South east trade winds ITCZ equator

15. What is ENSO El Niño-Southern Oscillation “Southern” : near the equator. “Oscillation” : The change in the air pressure in the east and the west.

16. The temperature of the Pacific ENSO is a cyclic warming and cooling of centre and eastern Pacific. three influences to the temperature of the Pacific 1.The northeastern trade winds 2.cold ocean current up the coast of Chile 3.cold deep current of Peru North east trade wind Ocean current

17. El Nino- ( Pacific surface temperature) El Nino -December, 1997 ocean surface temperature the temperature around the equator at Eastern Pacific is five Celsius higher than usual The temperature here is 5 Celsius higher then normal

18. La Nina- ( Pacific surface temperature) The temperature of the Pacific cools down the temperature of the Pacific is low

19. El Nino and La Nina El Nino- The cold sources wane air pressure :east is high, west is low influence: South America (west)- flood Australia,Taiwan (east)-drought La Nina- The cold sources intense air pressure: east is low,west is high. influence: South America- drought Australia- flood

20. El Nino – air pressure Low air pressure: flood High air pressure: drought

21. La Nina- air pressure Low air pressure: flood High pressure : drought

22. Southern Oscillation Index It shows the ups and downs of the sea level pressure in index form –sea level pressure - the temperature difference of the pacific –The "index" number- the pressure measurement difference between Darwin and Tahiti

23. SOI Positive SOI- La Nina Negative SOI- El Nino

24. Influences to Taiwan (El Nino) Less typhoon in Taiwan Warm winter More spring rain

25. Typhoon, Warm winter The monsoonal characteristic in southern Taiwan is clear: summer- rainy winter -dry. ( north eastern wind) anomalous circulations North eastern wind El Ninoanticyclonicweaken La Ninacyclonic enhance

26. ENSO-more rain moist dry El Nino La Nina More rain Less rain hsu.as.ntu.edu.tw/group_meeting/20080923_Chen.ppt moist dry

27. The red numbers are the one that had big difference among the two The amount of rain in Taiwan ( Jan ) The difference between El Nino and Neutral ENSO The west has more rain The west

28. The red numbers are the one that had big difference among the two The east has more rain The amount of rain in Taiwan ( Jan ) The difference between El Nino and Neutral ENSO The east

29. Conclude The precipitation in Feb and Mar have larger amounts because of ENSOThe precipitation in Feb and Mar have larger amounts because of ENSO In January, when there is an El Nino there is more rain in the west of Taiwan,. When there is a La Nina there is more rain in the east. El Nino brings more spring rain to Taiwan