Research Articles |
|
|
|
|
Spatio-temporal patterns of drought in North Xinjiang, China, 1961–2012 based on meteorological drought index |
WU Yanfeng1, Batur BAKE1*, ZHANG Jusong2, Hamid RASULOV3 |
1 College of Grassland and Environmental Science, Xinjiang Agricultural University, Urumqi 830052, China;
2 College of Agronomy, Xinjiang Agricultural University, Urumqi 830052, China;
3 Faculty of Hydrometeorology, Tajik Agrarian University, Dushanbe 734003, Tajikistan |
|
|
Abstract Drought, which is one of the most frequently occurring severe hazards with long time scales and covering wide geographical areas, is a natural phenomenon resulting in significant economic losses in agriculture and industry. Drought is caused by an imbalance between the inputs of and the demand for water which is insufficient to meet the demands of human activities and the eco-environment. As a major arid and semi-arid area and an important agricultural region in Northwest China, North Xinjiang (NX) shows great vulnerability to drought. In this paper, the characteristics of inter-annual and seasonal drought were analyzed in terms of drought occurrence and drought coverage, by using the composite index of meteorological drought and the data of daily precipitation, air temperature, wind speed, relative humidity and sunshine duration from 38 meteorological stations during the period 1961–2012. Trend analysis, wavelet analysis and empirical orthogonal function were also applied to investigate change trend, period and regional characteristics, respectively. In NX, annual and seasonal drought occurrence and drought coverage all showed a decreasing trend that was most significant in winter (with rates of –0.26 month/10a and –15.46%, respectively), and drought occurrence in spring and summer were more frequent than that in autumn and winter. Spatially, drought was severe in eastern regions but mild in western regions of NX. Annual and seasonal drought occurrence at 38 meteorological stations displayed decreasing trends and were most significant in “Shihezi-Urumqi-Changji”, which can help to alleviate severe drought hazards for local agricultural production and improve human livelihood. NX can be approximately classified into three sub-regions (severe drought region, moderate drought region and mild drought region), which were calculated from annual drought frequencies. The cross wavelet transform suggested that SOI (Southern Oscillation Index), AOI (Arctic Oscillation Index), AAOI (Antarctic Oscillation Index), PAOI (Pacific/North American Oscillation Index) and NAOI (North Atlantic Oscillation Index) have significant correlation with the variation of drought occurrence in NX. To prevent and mitigate the occurrence of drought disasters in NX, agricultural and government managers should pay more attention to those drought events that occur in spring and summer.
|
Received: 17 September 2014
Published: 10 August 2015
|
Fund: This study was supported by International Science & Technology Cooperation Program of China (2010DFA92720), the Scientific Innovation Research Project for Graduate Students of Xinjiang, and Soil Science Key Discipline Project of Xinjiang Uygur Autonomous Region. |
Corresponding Authors:
|
|
|
Cao L G, Pan S M, Wang Q, et al. 2014. Changes in extreme wet events in Southwestern China in 1960–2011. Quaternary International, 321: 116–124.Cao X, Wan Y, Cui Y L, et al. 2013. Analysis on change tendency of relative moisture index in northern piedmont of middle Tianshan Mountain over recent 30 years. Agricultural Research in the Arid Areas, 31(3): 244–251. (in Chinese)Dai A G. 2013. Increasing drought under global warming in observations and models. Nature Climate Change, 3(1): 52–58.Dai X G, Wang P, Zhang K J. 2013. A study on precipitation trend and fluctuation mechanism in northwestern China over the past 60 years. Acta Physica Sinica, 62(12): 1–11. (in Chinese)Easterling D R, Meehl G A, Parmesan C, et al. 2000. Climate ex-tremes: observations, modeling, and impacts. Science, 289: 2068–2074.Gong P, Sun J L, Gong Y S. 2013. Long-term change characteristics of gale days on the Yellow Sea. Modern Agricultural Science and Technology, (12): 185–187. (in Chinese)Grinsted A, Moore J C, Jevrejeva S. 2004. Application of the cross wavelet transform and wavelet coherence to geophysical time series. Nonlinear Processes in Geophysics, 11(5/6): 561–566.Jiang F Q, Hu R J. 2004. Climate change and expanded flood control and drought disasters in nearly 50 years in Xinjiang province. Journal of Desert Research, 24(1): 35–40. (in Chinese)Katz R W, Brown B G. 1992. Extreme events in a changing climate: variability is more important than averages. Climate Change, 21(3): 289–302.Keyantash J, Dracup J A. 2002. The quantification of drought: an evaluation of drought indices. Bulletin of the American Meteorological Society, 83(8): 1167–1180.Kim D H, Yoo C, Kim T W. 2011. Application of spatial EOF and multivariate time series model for evaluating agricultural drought vulnerability in Korea. Advances in Water Resources, 34(3): 340–350.Li B Z, Zhou G S. 2014. Advance in the study on drought index. Acta Ecologica Sinica, 34(5): 1043–1052. (in Chinese)Li J F, Zhang Q, Chen X H, et al. 2012. SPI-based drought variation in Xinjiang, China. Journal of Applied Meteorological Science, 23(3): 322–330. (in Chinese)Li X S. 2013. Changing characteristics of snowautumn in Xinjiang from 1961 to 2010. PhD Dissertation. Lanzhou: Northwest Normal University. (in Chinese)Li Z, Cheng Y N, Yang J, et al. 2014. Potential evapotranspiration and its attribution over the past 50 years in the arid region of Northwest China. Hydrological Processes, 28(3): 1025–1031.Liu Y L, Yu H M. 2012. Drought changes of critical period of crop growth in Heilongjiang province based on CI index. Journal of Meteorology and Environment, 28(1): 48–54. (in Chinese)Mahmood R, Li S L, Khan B. 2010. Causes of recurring drought patterns in Xinjiang, China. Journal of Arid Land, 2(4): 279−285.McKee T B, Doesken N J, Kleist J. 1993. The relationship of drought frequency and duration to time scales. In: Proceedings of the 8th Conference on Applied Climatology. Boston: American Meteorological Society, 179–184.McKee T B, Doesken N J, Kleist J. 1995. Drought monitoring with multiple time scales. In: Proceedings of the 9th Conference on Applied Climatology. Boston: American Meteorological Society, 233–236.Palmer W C. 1965. Meteorological Drought. Washington: US Department of Commerce, Weather Bureau.Pan S K, Zhang M J, Wang B L, et al. 2013. Study on the drought index variation for Xinjiang in recent 51 years. Journal of Arid Land Resource and Environment, 27(3): 32–39. (in Chinese)Pei Y S, Jiang G Q, Zhai J Q. 2013. Theoretical framework of drought evolution driving mechanism and the key problems. Advance in Water Science, 24(3): 449–456. (in Chinese)Pu Z C, Zhang S Q. 2011. Spatial-temporal variation of dry-wet climate on summer in recent 48 years in Xinjiang. Journal of Arid Land Resource and Environment, 35(1): 23–31. (in Chinese)Shafer B A, Dezman L E. 1982. Development of a Surface Water Supply Index (SWSI) to assess the severity of drought conditions in snowpack runoff areas. In: Proceedings of the Western Snow Conference. Colorado: Colorado State University, 164–175.Shao J, Li Y. 2014. Spatiotemporal distribution and variation of drought and waterlog in different time scales in Sinkiang. Journal of Irrigation and Drainage, 33(1): 68–73. (in Chinese)Sheffield J, Wood E F, Roderick M L. 2012. Little change in global drought over the past 60 years. Nature, 491(7424): 435–438.Shi Y F, Shen Y P, Hu R J. 2002. Preliminary study on signal, impact and foreground of climatic shift from warm-dry to warm-humid in northwest China. Journal of Glaciology and Geocryology, 24(3): 219–226. (in Chinese)Song X Y, Li L J, Fu G B, et al. 2014. Spatial–temporal variations of spring drought based on spring-composite index values for the Songnen Plain, Northeast China. Theoretical and Applied Climatology, 116(3–4): 371–384.Stocker T, Qin D, Plattner G K, et al. 2014. Climate Change 2013: The Physical Science Basis. Cambridge and New York: Cambridge University Press.Valdés-Galicia J F, Velasco V M. 2008. Variations of mid-term periodicities in solar activity physical phenomena. Advances in Space Research, 41(2): 297–305.Vicente-Serrano S M, Lopez-Moreno J I, Beguería S, et al. 2014. Evidence of increasing drought severity caused by temperature rise in southern Europe. Environmental Research Letters, 9(4): 044001.Wang B L, Zhang M J, Wei J L, et al. 2013. Changes in extreme events of temperature and precipitation over Xinjiang, northwest China, during 1960–2009. Quaternary International, 298: 141–151.Wang Y Y, Zhang B. 2012. Analysis of drought-flood spatial-temporal characteristics based on standard precipitation index in east region of Gansu in recent 40 years. Journal of Natural Resources, 27(12): 2135–2144. (in Chinese)Xie W S, Tian H, Wang S, et al. 2013. Study on spatial-temporal characteristics of drought in Huaihe River Basin based on CI index. Meteorological Monthly, 39(9): 1171–1175. (in Chinese)Xu C C, Li J X, Zhao J, et al. 2014. Climate variations in northern Xinjiang of China over the past 50 years under global warming. Quaternary International, 358: 83–92.Yang J H, Jiang Z H, Liu X Y, et al. 2012. Influence research on spring vegetation of Eurasia to summer drought-wetness over the northwest China. Arid Land Geography, 35(1): 10–21. (in Chinese)Yang L, Wong C M, Lau E H Y, et al. 2008. Synchrony of clinical and laboratory surveillance for influenza in Hong Kong. PLoS ONE, 3(1): e1399.Yao Y B, Yang J H, Yue P, et al. 2011. Climatic change of terrestrial surface humid index and its impact factors over the source region of three rivers in recent 50 years. Ecology and Environmental Sciences, 20(11): 1585–1593.Yu X G, He X Y, Zheng H F, et al. 2014. Spatial and temporal analysis of drought risk during the crop-growing season over northeast China. Natural Hazards, 71(1): 275–289.Zhang M J, He J Y, Wang B L, et al. 2013. Extreme drought changes in Southwest China from 1960 to 2009. Journal of Geographical Sciences, 23(1): 3–16.Zhang Q, Sun P, Li J F, et al. 2014. Spatiotemporal properties of droughts and related impacts on agriculture in Xinjiang, China. International Journal of Climatology, doi: 10.1002/joc.4052.Zhang S Q, Pu Z C. 2011. Temporal and spatial variation characteristics of reference evapotranspiration in Xinjiang. Transactions of the Chinese Society of Agricultural Engineering, 27(5): 73–79. (in Chinese)Zhang T F, Zhang B, Wang Y H, et al. 2013. Drought characteristics in the shiyang river basin during the recent 50 years based on a composite index. Acta Ecologica Sinica, 33(3): 975–984. (in Chinese)Zhang X Q, Lei Y C, Pang Y, et al. 2014. Tree mortality in response to climate change induced drought across Beijing, China. Climatic Change, 124(1–2): 179–190.Zhao Y, Yang Q, Ma Y F. 2012. Analysis on features of regional and continuous drought in North Xinjiang in spring and summer. Arid Zone Research, 29(3): 472–478. (in Chinese)Zhao Z P, Liu J Y, Shao Q Q. 2010. Spatial diversity of humidification and its impact on ecosystem venerability in china during the last 30 years. Journal of Natural Resources, 25(12): 2091–2100. (in Chinese)Zhou S W, Wang C H, Wu P, et al. 2012. Temporal and spatial distribution of strong precipitation days over the Tibetan Plateau. Arid Land Geography, 35(1): 23–31. (in Chinese)Zhuang X C, Yang S, Zhao Z B, et al. 2010. Drought index and its application in the analysis on drought monitoring in Altai Region, Xinjiang. Journal of Catastrophology, 25(3): 81–85. (in Chinese) |
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
|
Shared |
|
|
|
|
|
Discussed |
|
|
|
|