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Journal of Arid Land  2017, Vol. 9 Issue (6): 924-937    DOI: 10.1007/s40333-017-0105-4
Orginal Article     
Precipitation changes in the mid-latitudes of the Chinese mainland during 1960-2014
Yuling HU1, Shigong WANG1,2,*(), Xuping SONG1, Jiaxin WANG2
1 Key laboratory of Arid Climate Change and Reducing Disaster in Gansu Province, College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China
2 Plateau Environment and Meteorology Key Laboratory of Education Bureau of Sichuan Province, College of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225, China
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Abstract  

Based on daily precipitation data from 163 meteorological stations, this study investigated precipitation changes in the mid-latitudes of the Chinese mainland (MCM) during 1960-2014 using the climatic trend coefficient, least-squared regression analysis, and a non-parametric Mann-Kendall test. According to the effects of the East Asian summer monsoon on the MCM and the climatic trend coefficient of annual precipitation during 1960-2014, we divided the MCM into the western MCM and eastern MCM. The western MCM was further divided into the western MCM1 and western MCM2 in terms of the effects of the East Asian summer monsoon. The main results were as follows: (1) During the last four decades of the 20th century, the area-averaged annual precipitation presented a significant increasing trend in the western MCM, but there was a slight decreasing trend in the eastern MCM, where a seesaw pattern was apparent. However, in the 21st century, the area-averaged annual precipitation displayed a significant increasing trend in both the western and eastern MCM. (2) The trend in area-averaged seasonal precipitation during 1960-2014 in the western MCM was consistent with that in the eastern MCM in winter and spring. However, the trend in area-averaged summer precipitation during 1960-2014 displayed a seesaw pattern between the western and eastern MCM. (3) On an annual basis, both the trend in rainstorms and heavy rain displayed a seesaw pattern between the western and eastern MCM. (4) The precipitation intensity in rainstorms, heavy rain, and moderate rain made a greater contribution to changes in the total precipitation than precipitation frequency. The results of this study will improve our understanding of the trends and differences in precipitation changes in different areas of the MCM. This is not only useful for the management and mitigation of flood disasters, but is also beneficial to the protection of water resources across the MCM.



Key wordsprecipitation changes      the mid-latitudes of the Chinese mainland      seesaw pattern      rainy days      precipitation intensity      precipitation frequency     
Received: 07 June 2017      Published: 20 December 2017
Corresponding Authors:
Cite this article:

Yuling HU, Shigong WANG, Xuping SONG, Jiaxin WANG. Precipitation changes in the mid-latitudes of the Chinese mainland during 1960-2014. Journal of Arid Land, 2017, 9(6): 924-937.

URL:

http://jal.xjegi.com/10.1007/s40333-017-0105-4     OR     http://jal.xjegi.com/Y2017/V9/I6/924

[1] Allen M R, Ingram W J.2002. Constraints on future changes in climate and the hydrologic cycle. Nature, 419(6903): 224-232.
[2] Buishand T A.1982. Some methods for testing the homogeneity of rainfall records. Journal of Hydrology, 58(1-2): 11-27.
[3] Fu J L, Qian W H, Lin X, et al.2008. Trends in graded precipitation in China from 1961 to 2000. Advances in Atmospheric Sciences, 25(2): 267-278.
[4] Gemmer M, Becker S, Jiang T.2004. Observed monthly precipitation trends in China 1951-2002. Theoretical and Applied Climatology, 77(1-2): 39-45.
[5] IPCC. 2001. Climate change 2001: The Scientific Basis. Cambridge: Cambridge University Press, 785.
[6] IPCC. 2007. Technical summary. In: Solomon S, Qin D, Manning M, et al. Climate Change 2007: the Physical Science Basis. Contribution of Working Group I to the 4th Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press. 2-4.
[7] Jia W X.2012. Temporal and spatial changes of precipitation in Qilian Mountains and Hexi Corridor during 1960-2009. Acta Geographica Sinica, 67(5): 631-644. (in Chinese)
[8] Karl T R, Knight R W.1998. Secular trends of precipitation amount, frequency, and intensity in the United States. Bulletin of American Meteorological Society, 79(2): 231-241.
[9] Kendall M G.1938. A new measure of rank correlation. Biometrika, 30(1-2): 81-93.
[10] Kendall M G.1975. Rank Correlation Methods. London: Griffin, 202.
[11] Kundzewicz Z W.2005. Flood risk in the changing world-Yangtze floods. In: Jiang T, King L, Gemmer M, et al. Climate Change and Yangtze Floods. Beijing: Science Press, 246-258.
[12] Li D L, Wei L, Cai Y, et al.2003. The present facts and the future tendency of the climate change in Northwest China. Journal of Glaciology and Geocryology, 25(2): 135-142. (in Chinese)
[13] Li J P, Wu Z W, Jiang Z H, et al.2010. Can global warming strengthen the East Asian summer monsoon? Journal of Climate, 23(24): 6696-6705.
[14] Liu B, Xu M, Henderson M, et al.2005. Observed trends of precipitation amount, frequency, and intensity in China, 1960-2000. Journal of Geophysical Research: Atmospheres, 110(D8): D08103.
[15] Liu R, Liu S C, Cicerone R J, et al.2015. Trends of extreme precipitation in Eastern China and their possible causes. Advances in Atmospheric Sciences, 32(8): 1027-1037.
[16] Maniak U.1997. Hydrologie und Wasserwirtschaft. Berlin: Springer, 650.
[17] Meng X J, Zhang S F, Zhang Y Y, et al.2013. Temporal and spatial changes of temperature and precipitation in Hexi Corridor during 1955-2011. Journal of Geographical Sciences, 23(4): 653-667.
[18] Qian W, Lin X.2005. Regional trends in recent precipitation indices in China. Meteorology and Atmospheric Physics, 90(3-4): 193-207.
[19] Semenov V A, Bengtsson L.2002. Secular trends in daily precipitation characteristics: greenhouse gas simulation with a coupled AOGCM. Climate Dynamics, 19(2): 123-140.
[20] Shen S H, Sheng Q.2008. Changes in pan evaporation and its cause in China in the last 45 years. Acta Meteorologica Sinica, 66(3): 452-460. (in Chinese)
[21] Shi N, Tu Q P, Chen J Q.1995. Temperature, rainfall variations and their anomalies over China under the cold-warm background in the 20th century. Acta Meteorologica Sinica, 9(4): 445-455.
[22] Shi N, Huang X X, Yang Y.2003. Spatiotemporal features of the trend variation of global land annual rainfall fields from 1948~2000. Chinese Journal of Atmospheric Sciences, 27(6): 971-982. (in Chinese)
[23] Shi Y F, Shen Y P, Li D L, et al.2003. Discussion on the present climate change from warm-dry to warm-wet in northwest China. Quaternary Sciences, 23(2): 152-164. (in Chinese)
[24] Shi Y F, Shen Y P, Kang E, et al.2007. Recent and future climate change in Northwest China. Climatic Change, 80(3-4): 379-393.
[25] Shin N, Deng Z W.2000. Space/time features of the secular variation in 1951-1998 Northern 500-hPa Height. Meteorology and Atmospheric Physics, 73(1-2): 35-46.
[26] Tian R X, Gao L, Gao Y X.1995. Spatial and temporal variation of annual rainfall in the northwest arid areas of China. Plateau Meteorology, 14(1): 90-95. (in Chinese)
[27] Trenberth K E.1998. Atmospheric moisture residence times and cycling: Implications for rainfall rates and climate change. Climatic Change, 39(4): 667-694.
[28] Trenberth K E, Dai A G, Rasmussen R M, et al.2003. The changing character of precipitation. Bulletin of the American Meteorological Society, 84(9): 1205-1217.
[29] Wang S W, Zhu J H, Cai J N.2004. Interdecadal variability of temperature and precipitation in China since 1880. Advances in Atmospheric Sciences, 21(3): 307-313.
[30] Wang Y Q, Zhou L.2005. Correction to “Observed trends in extreme precipitation events in China during 1961-2001 and the associated changes in large-scale circulation”. Geophysical Research Letters, 32(17): L17708.
[31] Zhai P M, Ren F M, Zhang Q.1999. Detection of trends in China’s precipitation extremes. Acta Meteorologica Sinica, 57(2): 208-216. (in Chinese)
[32] Zhang Q, Singh V P, Li J F, et al.2012. Spatio-temporal variations of precipitation extremes in Xinjiang, China. Journal of Hydrology, 434-435: 7-18.
[33] Zhu S J, Chang Z F.2011. Temperature and precipitation trends in Minqin Desert during the period of 1961-2007. Journal of Arid Land, 3(3): 214-219.
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