STATISTICAL FEATURES OF THE ULTRA-SHORT-RANGE PRECIPITATION DURING EARLY RAINY SEASON IN FUJIAN PROVINCE

Lin Xinbin; Liu Zengji; Zou Yan; Ren Hanlong; Zhou Rongzhen

Vol.13, NO.4, 2002

Article Contents

Article Navigation > Journal of Applied Meteorological Science > 2002 > 13(4): 469-477

Lin Xinbin, Liu Zengji, Zou Yan, et al. Statistical features of the ultra-short-range precipitation during early rainy season in Fujian Province. J Appl Meteor Sci, 2002, 13(4): 469-477.

Citation:

Lin Xinbin, Liu Zengji, Zou Yan, et al. Statistical features of the ultra-short-range precipitation during early rainy season in Fujian Province. J Appl Meteor Sci, 2002, 13(4): 469-477.

Lin Xinbin, Liu Zengji, Zou Yan, et al. Statistical features of the ultra-short-range precipitation during early rainy season in Fujian Province. J Appl Meteor Sci, 2002, 13(4): 469-477.

Citation:

Lin Xinbin, Liu Zengji, Zou Yan, et al. Statistical features of the ultra-short-range precipitation during early rainy season in Fujian Province. J Appl Meteor Sci, 2002, 13(4): 469-477.

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STATISTICAL FEATURES OF THE ULTRA-SHORT-RANGE PRECIPITATION DURING EARLY RAINY SEASON IN FUJIAN PROVINCE

Meteorological Bureau of Fujian Prov ince, Fuzhou 350001

Received Date: 2000-07-07
Rev Recd Date: 2000-12-13
Publish Date: 2002-08-31

Abstract

Abstract

The climatic frequency and probability of the ultra-short-range rainfall during the early rainy season (in May and June) over Fujian Province are classified and compared. Results show that the rainfall features are different in regions with different topographical features, including the height above the sea, the distance to the sea, the direction of the mountains, hills, valleys, etc. Results reveal that the topographical differences play an important role in rainfall in Fujian Province.
- Topography;
- Rainy season;
- Ultra-short-range;
- Precipitation;
- Climatic feature

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References(3)

Figures and Tables

图 1 福建省不同高度下各时段平均短历时降水气候概率比较图

(1:>800 m，2:400~800 m；3:100~400 m；4:35~100 m；5: < 35 m)

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图 2 福建省不同离海距离下各时段平均短历时降水气候概率比较图

(1~5表示离海距离级序，6表示海岛)

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图 3 在离海距离相同而海拔高度不同情况下短历时降水气候概率的比较

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图 4 在海拔高度相近而离海距离不同情况下短历时降水气候概率的比较 (a) 海拔高度为200~300 m；(b) 海拔高度为150~200 m；(c) 海拔高度为30~50 m；

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图 5 戴云山脉东西两侧各代表站短历时降水气候概率对比

(a)5月；(b)6月

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图 6 武夷山区与建溪和沙溪河谷盆地各站前汛期短历时降水气候概率

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图 7 戴云山山脉东西两侧不同高度前汛期短历时降水气候的综合比较图

(1:5月；2:前汛期；3:6月)

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表 1 不同海拔高度下短历时降水平均气候概率PP_i值的分布表

表 2 各级离海距离内短历时降水平均气候概率PP_j值的分布表

References

[1]	林之光.中国气候.北京:气象出版社, 1987. 73~81.
[2]	刘增基, 林新彬, 等.闽南地区汛期短历时降水气候特征.气象, 1997, 22(8): 50~54. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX708.011.htm
[3]	邹燕, 刘增基.闽北地区汛期短历时降水气候特征.福建气象, 1999, (5): 9~12.