YANG Jinhu, REN Chuanyou, JIANG Zhihong. Characteristics of Extreme Temperature Event and Its Response to Regional Warming in Northwest China in Past 45 Years[J]. Chinese Geographical Science, 2008, 18(1): 70-76. doi: 10.1007/s11769-008-0070-0
Citation: YANG Jinhu, REN Chuanyou, JIANG Zhihong. Characteristics of Extreme Temperature Event and Its Response to Regional Warming in Northwest China in Past 45 Years[J]. Chinese Geographical Science, 2008, 18(1): 70-76. doi: 10.1007/s11769-008-0070-0

Characteristics of Extreme Temperature Event and Its Response to Regional Warming in Northwest China in Past 45 Years

doi: 10.1007/s11769-008-0070-0
Funds:  Under the auspices of National Natural Science Foundation of China (No. 40375032,No. 40675043)
  • Received Date: 2007-03-19
  • Rev Recd Date: 2007-10-18
  • Publish Date: 2008-03-20
  • Using the daily maximum and minimum temperature dataset from 128 stations from 1960 to 2004 in Northwest China,daily extreme high temperature(EHT)and extreme low temperature(ELT)thresholds were determined by centesimal method for different stations at first,then yearly EHT and ELT events were counted up in different stations,and the characteristics of their spatio-temporal distribution were diagnosed at last.The study drew following conclusions:1)The consistent anomaly distribution characteristic was the most important mode of the EHT and ELT events in Northwest China.2)The spatial distribution of the EHT and ELT events can be divided into five subregions,namely,the north of Qinghai and west of Gansu,the north of Xinjiang,the south of Xinjiang,the east of Northwest China and the south of Qinghai.3)The EHT events showed remarkable increasing trend in all of five sub-regions,but only in the north of Qinghai and west of Gansu area,sudden change phenomenon occurred;the ELT events showed decreasing trend in all of five sub-regions,and sudden change phenomenon occurred in Northwest China except for south of Qinghai.4)In all of five sub-regions the EHT events showed remarkable 12-14yr period oscillation,and the ELT event showed significant 13-15yr and 7-8yr period oscillation.5)The EHT and ELT events displayed remarkable positive and negative responses to regional warming of Northwest China respectively.
  • [1] Bonsai B K,Zhang X B,Vincent L Aet al.,2001,Characteristic of daily and extreme temperature over Canada.J.Climate,5(14):1959-1976.

    [2] Changnon S A,Roger A,Pielke Jr et al.,2000.Human factors explain the increased losses from weather and climate extremes.Bull.of the Amer.Mete.Soci.,81(3):437-442.

    [3] Cooter E J,LeDuk S K,1993.Recent frost data trends in the northern United States.Int.J.Climatology,15:65-75.

    [4] Easterling D R,Evans J L,Groisman P Y et al.,2000.Observed variability and trends in extreme climate events:A brief review.Bull.of the Amer.Mete.Soci.,81(3):417-425.

    [5] Filch P,Alexander L V,Della-Marta P Met al.,2002.Observed coherent changes in climate extremes during the second half of the 20th century.Clim.Res.,19:193-212.

    [6] Gruza G,Rankova E,Razuvaev V,1999.Indicators of climate change for the Russian federation.Climatic Change,42:219242.

    [7] Horton B,1995.Geographical distribution of changes in maximum and minimum temperatures.Atmos.Res.,37:101-117.

    [8] Karl T R,Jones,P D,Knight R Wet al.,1993.Anew perspective on recent global wanning:Asymmetric trends of daily maximum and minimum temperature.Bull.of the Amer.Mete.Soci.,74(6):1007-1023.

    [9] Karl T R,Kukla G,Razuvayev V Net al.,1991.Global Warming:Evidence for asymmetric diurnal temperature change.Geophys.Res.Lett.,18:2253-2256.

    [10] Kattenberg A,Giorgi F,2001.The Scientific of climate change.In:Houghton J T et al.(eds.).The Third Assessment Report of the Intergovernmental Panel on Climate Change.Cambridge:Cambridge University Press,156-159.

    [11] Ma Zhuguo,Fu Congbin,Ren Xiaobo et al.,2003.Trend of annual extreme temperature and its relationship to regional warming in northern China.Acta Geographica Sinica,58(supp.):11-20.(in Chinese)

    [12] Manton M J,Della-Marta P M,Hayiock M R et al.,2001.Trend in extreme daily rainfall and temperature in southeast Asia and the South Pacific:1961-1998.Int.J.Climatology,21:269-284.

    [13] Ren Fumin,Zhai Panmao,1998.Analysis of extreme temperature in China from 1951-1990.Chinese Journal of Atmosphere,22(2):217-227.(in Chinese)

    [14] Zhai P M,Sum A J,Ren Fumin et al.,1999.Changes of climate extremes in China.Climatic Change,42:203-218.

    [15] Zhai Panmao,Pan Xiaohua,2003.Change in extreme temperature and precipitation over northern China during the second half of the 20th century.Acta Geographica Sinica,58(supp.):1-10.(in Chinese)
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Characteristics of Extreme Temperature Event and Its Response to Regional Warming in Northwest China in Past 45 Years

doi: 10.1007/s11769-008-0070-0
Funds:  Under the auspices of National Natural Science Foundation of China (No. 40375032,No. 40675043)

Abstract: Using the daily maximum and minimum temperature dataset from 128 stations from 1960 to 2004 in Northwest China,daily extreme high temperature(EHT)and extreme low temperature(ELT)thresholds were determined by centesimal method for different stations at first,then yearly EHT and ELT events were counted up in different stations,and the characteristics of their spatio-temporal distribution were diagnosed at last.The study drew following conclusions:1)The consistent anomaly distribution characteristic was the most important mode of the EHT and ELT events in Northwest China.2)The spatial distribution of the EHT and ELT events can be divided into five subregions,namely,the north of Qinghai and west of Gansu,the north of Xinjiang,the south of Xinjiang,the east of Northwest China and the south of Qinghai.3)The EHT events showed remarkable increasing trend in all of five sub-regions,but only in the north of Qinghai and west of Gansu area,sudden change phenomenon occurred;the ELT events showed decreasing trend in all of five sub-regions,and sudden change phenomenon occurred in Northwest China except for south of Qinghai.4)In all of five sub-regions the EHT events showed remarkable 12-14yr period oscillation,and the ELT event showed significant 13-15yr and 7-8yr period oscillation.5)The EHT and ELT events displayed remarkable positive and negative responses to regional warming of Northwest China respectively.

YANG Jinhu, REN Chuanyou, JIANG Zhihong. Characteristics of Extreme Temperature Event and Its Response to Regional Warming in Northwest China in Past 45 Years[J]. Chinese Geographical Science, 2008, 18(1): 70-76. doi: 10.1007/s11769-008-0070-0
Citation: YANG Jinhu, REN Chuanyou, JIANG Zhihong. Characteristics of Extreme Temperature Event and Its Response to Regional Warming in Northwest China in Past 45 Years[J]. Chinese Geographical Science, 2008, 18(1): 70-76. doi: 10.1007/s11769-008-0070-0
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