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Abstract:
The spatio-temporal characteristics of typhoon precipitation over China are analyzed in this study. The results show that typhoon precipitation covers most of central-eastern China. Typhoon precipitation gradually decreases from the southeastern coastal regions to the northwestern mainland. The maximum annual typhoon precipitation exceeds 700 mm in central-eastern Taiwan and part of Hainan, while the minimum annual typhoon precipitation occurs in parts of Inner Mongolia, Shanxi, Shaanxi and Sichuan, with values less than 10 mm. Generally, typhoons produce precipitation over China during April –C December with a peak in August. The annual typhoon precipitation time series for observation stations are examined for long-term trends. The results show that decreasing trends exist in most of the stations from 1957 to 2004 and are statistically significant in parts of Taiwan, Hainan, coastal Southeast China and southern Northeast China. The anomaly of typhoon precipitation mainly results from that of the general circulation over Asia and the Walker Cell circulation over the equatorial central and eastern Pacific. Typhoon torrential rain is one of the extreme rainfall events in the southeastern coastal regions and parts of central mainland. In these regions, torrential rains are mostly caused by typhoons.
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References
|
[1]
|
CHEN Lian-shou, DING Yi-hui. Introduction to WestPacific Typhoons [M]. Beijing: Science Press, 1979: 1-3. |
|
[2]
|
LIU Zi-cheng, LIANG Sheng-jun, ZHANG Jian-hong. Theeffect of landfalling typhoons on heavy rains in eastern part ofthe Loess Plateau [J]. Plateau Meteor., 1997, 16(4): 402-409. |
|
[3]
|
LI Jiang-nan, WANG An-yu, YANG Zhao-li, et al.Advancement in the study of typhoon rainstorm [J]. J. Trop.Meteor., 2003, 19 (suppl.): 152-159. |
|
[4]
|
LI Yong-kang, GAO Guo-dong. Climatic analysis on theheavy rainfall caused by tropical cyclonic storm in China [J]. J.Naijing Univ. (Nat. Sci.), 1995, 31(2): 310-319. |
|
[5]
|
WENG Xiang-yu, YE Meng, HE Xia-jiang. Analysis ofcharacteristics of precipitation induced by tropical cycloneslandfalling in west Guangdong [J]. J. Trop. Meteor., 2005,21(3): 301-308. |
|
[6]
|
CHEN Wen-yu, JIN De-shan, CHEN Ju-ying. Interrelationbetween the tropical cyclone action and the types of the rainband in summer in China as well as the action of ENSO [J].Marine Forecasts, 1997, 14(1): 25-36. |
|
[7]
|
RODGERS E B, ADLER R F, PIERCE H F. Contributionof tropical cyclones to the North Atlantic climatologicalrainfall as observed from satellites. [J]. J. Appl. Meteor., 2001,40(11): 1785-1800. |
|
[8]
|
REN Fu-min, GLEASON B, EASTERLING D R. Anumerical technique for partitioning cyclone tropicalprecipitation [J]. J. Trop. Meteor., 2001, 17(3): 308-313. |
|
[9]
|
WANG Yong-mei, REN Fu-min, WANG Xiao-ling, et al.The study on the objective technique for partitioning tropicalcyclone precipitation in China [J]. Meteor. Mon., 2006, 32(3):6-10. |
|
[10]
|
REN F M, WANG Y M, WANG X L, et al. EstimatingTropical Cyclone precipitation from station observations [J].Adv. Atmos. Sci., 2007, 24(4): 700-711. |
|
[11]
|
CHEN Min, ZHENG Yong-guang, TAO Zu-yu. Ananalysis on tropical cyclones’ climatic feature in the westernnorth Pacific for 1949 - 1996 [J]. J. Trop. Meteor., 1999, 15(1):10-16. |
|
[12]
|
LIN Hui-juan, ZHANG Yao-cun. Climatic features of thetropical cyclone influencing China and its relationship withthe sea surface temperature in the Pacific Ocean [J]. J. Trop.Meteor., 2004, 20(2): 219-224. |
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