The change character of monsoon rainband over Heilongjiang Province for the past 40 years

Jin-rong Li , Bin-hui Liu

Journal of Forestry Research ›› 2006, Vol. 17 ›› Issue (1) : 71 -74.

PDF
Journal of Forestry Research ›› 2006, Vol. 17 ›› Issue (1) : 71 -74. DOI: 10.1007/s11676-006-0017-1
Article

The change character of monsoon rainband over Heilongjiang Province for the past 40 years

Author information +
History +
PDF

Abstract

Precipitation in Heilongjiang Province of China increased slightly from 1960 to 2000. Adopting the method proposed by Arthur N. Samel, we separated monsoon rainband rain and calculated the initial and final date of monsoon rainband of each year and each station. For the period of 1960–2000, the change of annual precipitation in Heilongjiang Province, with an increasing trend of 2.229 mm per decade, is not significant; the duration and total monsoon rain decreased significantly, with a decreasing trend of −6.9 day per decade and −17.5 mm per decade separately. That change comes from early leaving date of summer monsoon rainband for the period of 1960–1975 and later arriving date of summer monsoon rainband for the period of 1990–2000. The weakening of summer monsoon makes its contribution to the annual precipitation decreased significantly, with a decreasing trend of 4.4 % per decade.

Keywords

Precipitation / Monsoon rainband / Summer monsoon / Heilongjiang Province / China

Cite this article

Download citation ▾
Jin-rong Li, Bin-hui Liu. The change character of monsoon rainband over Heilongjiang Province for the past 40 years. Journal of Forestry Research, 2006, 17(1): 71-74 DOI:10.1007/s11676-006-0017-1

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Ding Y.H., Johnny C.L. The east Asian summer monsoon: an overview [J]. Meteorol. Atmos. Phys., 2005, 89: 117-142.

[2]

Eastering D.R., Horton B., Jones P.D., Peterson T.C., Karl T.R., Parker D.E. et al. Maximum and minimum temperature trends for the globe [J]. Science, 1997, 277: 364-367.

[3]

Frei C., Schär C., Lüthi D., Davies H.C. Heavy precipitation processes in a warm climate [J]. Geophys. Res. Lett., 1998, 25: 1431-1434.

[4]

Kang I.S., Ho C.H., Lim Y.K. Principal modes of climatological seasonal and intraseasonal variations of the Asian summer monsoon [J]. Monthly Whether Review, 1999, 127: 322-340.

[5]

Liu B.H., Xu M., Herderson M., Qi Y. Observed trends of precipitation amount, frequency, and intensity in China, 1960–2000 [J]. Journal of Geophysical Research, 2005, 110: D08103

[6]

Liu B. H., Xu M., Henderson M., Qi Y., Li Y. Taking China’s temperature: daily range, warming trends, and regional variations, 1955–2000 [J]. Journal of Climate, 2004, 17: 4453-4462.

[7]

Liu B.H., Xu M., Henderson M., Gong W.G. A spatial analysis of pan evaporation trends in China, 1955–2000 [J]. Journal of Geophysical Research, 2004, 109: D15102

[8]

Samel A.N., Wang W.C., Liang X.Z. The monsoon rainband over China and relationships with the Eurasian circulation [J]. Journal of Climate, 1999, 12: 115-131.

AI Summary AI Mindmap
PDF

112

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/