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Temperature mutation and globe warming stagnate study in typical area of Yellow River basin in recently 60years |
HUANG Xing, MA Long, LIU Ting-xi, WANG Jing-ru, LIU Dan-hui, LI Hong-yu |
College of Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Hohhot 010018, China |
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Abstract The part of Yellow River in Inner Mongolia was chosen as a typical area of Yellow River Basin. The regional annual average maximum temperature (AMaxT), annual average minimum temperature (AMinT) and annual average temperature (AvT) from 1951 to 2012 were selected and analyzed by Mann-Kendall method. The temperature variations before and after the mutation and the warming stagnate following the mutation were also discussed. Annual (or seasonal) AMinT mutation happened first on 1977 to 1987. Then the AvT and AMaxT mutation happened on 1978 to 1993 and 1978 to 1994, respectively. The mutation period of average autumn and winter temperature were same as AMaxT. The earliest intra-annual mutation was winter (1977 to 1978), and the latest was summer (1987 to 1994). The winter and AMaxT had more variations than summer and AMinT. The increase ratio or AMinT was 0.231~0.604℃/10a which have the most contribution. All the annual (or seasonal) temperatures had a warming stagnate from 1997 to 2007 after the mutation, successively. The stagnate occurred in spring and not stagnate occurred in summer. Mostly annual and seasonal temperature stagnate happened later than the global period which winter firstly, then autumn, the AvT was the last one (on 2007). The AMaxT increase rate was lower in the period of after mutation and before stagnate. However, the decrease rate of AMaxT if faster after stagnate. The AMinT was on the contrary. This indicates that the AMinT was sensitive to temperature increase and the AMaxT was sensitive to the temperature decrease. In seasonal, the spring AMaxT increase rate is higher from mutation to stagnate, and the spring AMinT decrease rate was the fastest after the temperature stagnate which is -0.324℃/a.
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Received: 20 March 2016
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[1] |
李远平,杨太保.柴达木盆地气温降水突变与周期特征分析[J]. 地理与地理信息科学, 2007,23(3):105-108.
|
[2] |
Li B, Chen Y, Shi X. Why does the temperature rise faster in the arid region of northwest China[J]. Journal of Geophysical., 2012, 117:D16115-D16121.
|
[3] |
Somolon S, Dahe D, Manning M, et al. Climate Change 2007:The Physical Science Basis:Contribution of Working Group I to the Fourth Assessment Report of the Intergovernment Panel on Climate Change[M]. Cambridge, UK:Cambridge University Press, 2007:1-18.
|
[4] |
符淙斌,王强.气候突变的定义和检测方法[J]. 大气科学, 1992,16(4):482-492.
|
[5] |
王有清,姚檀栋.冰芯记录中末次间冰期~冰期旋回气候突变事件的研究进展[J]. 冰川冻土, 2002,24(5):550-558.
|
[6] |
Aesowy A M. Hasanean H M. Annual and seasonal climatic analysis of surface air temperature variations at six southern Mediterranean stations[J]. Theoretical and Applied Climatology, 1998,61:55-68.
|
[7] |
吕少宁,李栋梁,文军,等.全球变暖背景下青藏高原气温周期变化与突变分析[J]. 高原气象, 2010,6:1378-1385.
|
[8] |
周晓宇,赵春雨,张欣宜,等.1961-2009年辽宁省气温、降水变化特征及突变分析[J]. 干旱区资源与环境, 2013,10:87-93.
|
[9] |
郑景云,郝志新,方修琦,等.中国过去2000年极端气候事件变化的若干特征[J]. 地理科学进展, 2014,1:3-12.
|
[10] |
徐丽梅,郭英,刘敏,等.1957年至2008年海河流域气温变化趋势和突变分析[J]. 资源科学, 2011,5:995-1001.
|
[11] |
宁向玲,董婕,延军平.陕北地区气温突变及其对旱涝灾害的影响[J]. 干旱区资源与环境, 2011,(12):102-106.
|
[12] |
宋辞,裴韬,周成虎.1960年以来青藏高原气温变化研究进展[J]. 地理科学进展, 2012,(11):1503-1509.
|
[13] |
闫敏华,邓伟,陈泮勤.三江平原气候突变分析[J]. 地理科学, 2003,23(6):661-667.
|
[14] |
马晓华,赵景波.1958-2013年豫南地区极端气温变化特征及周期分析[J]. 资源科学, 2014,(9):1825-1833.
|
[15] |
于秀晶,李栋梁,胡靖彪.吉林近50a来气候的年代际变化特征及其突变分析[J]. 冰川冻土, 2004,26(6):779-783.
|
[16] |
杨东,刘洪敏.1956~2008辽宁省近53年的降水量变化[J]. 干旱区资源与环境, 2011,(1):96-101.
|
[17] |
何云玲,鲁枝海.近60年昆明市气候变化特征分析[J]. 地理科学, 2012,9:1119-1124.
|
[18] |
Carter B. There is a problem with global warming it stopped in 1998[R].[EB/OL]. Telegraph 09 April 2006.
|
[19] |
Easterling D R. Wehner M F, Is the climate warming or cooling[J]. Geophys. Res. Lett., 2009,36:1160-1172.
|
[20] |
Balmaseda M A. Trenberth K E, Kallen E. Distinctive climate signals in reanalysis of global ocean heat content[J]. Geophys. Reslett., 2013.40:1754-1759.
|
[21] |
Levitus S, Antonow J I, Boyer T P. et al. Global ocean heat content 1995-2008in light of recently revealed instrumentation proble-ms[J]. Geophy. Res. Lett., 2009,36:L07608.
|
[22] |
Lyman J M, Good S A, Gouretski V V, et al. Robust wairming of the global upper ocean[J]. Nature, 2010,465:334-337.
|
[23] |
Meel G A. Hu A, Arblaster J M. et al. Externally forced and internally generated decadal climate variability associated with the interdecadal Pacific Oscillation[J]. J. Climate, 2013,26:7298-7310.
|
[24] |
Kosaka Y. Xie S P. Recent global warming hiatus tied ti equat orial Pacific suiface cooling[J]. Nature, 2013,501:403-407.
|
[25] |
Trenber K E, Fasullo T T, Balmaseda M A. Earth Energy Imbalance[J]. J climate, 2014b,27:3129-3144.
|
[26] |
Chen X, Tung K K. Varying planetary heat sink led to global warming slowdown and acceleration[J]. Science, 2014,345:897-907.
|
[27] |
Huber M, Knutti R. Natural variability, radiatiue forcing and climate response in the recent. Hiatus reconciled[J]. Nature Geoscience, 2014,(7):615-656.
|
[28] |
常军,王永光,赵宇,等.近50年黄河流域降水量及雨日的气候变化特征[J]. 高原气象, 2014,33(1):43-54.
|
[29] |
刘勤,严昌荣,张燕卿,等.近50年黄河流域气温和降水量变化特征分析[J]. 中国农业气象, 2012,33(4):475-480.
|
[30] |
汤懋苍,白重瑗,冯松,等.本世纪青藏高原气候的三次突变及与天文因素的相关.[J]. 高原气象, 1998,17(3):250-257.
|
[31] |
王海军,张勃,赵传燕,等.中国北方近57年气温时空变化特征[J]. 地理科学进展, 2009,28(4):643-650.
|
[32] |
韩翠华,郝志新.1951~2010年中国气温变化分区及其区域特征[J]. 地理科学进展, 2013,6(32):887-896.
|
[33] |
王绍武,罗勇,赵宗慈,等.全球变暖的停滞还能持续多久?[J]. 气候变化研究进展, 2014,10(6):465-468.
|
[34] |
宋斌,智协飞,胡耀星.全球变暖停滞的形成机制研究进展.[J]. 大气科学学报, 2015,38(2):145-154.
|
[35] |
Kerr R A. What happened to global warming? scientists say just wait a bit[J]. Science, 2009,326:28-29.
|
[36] |
张文.近百年来气候突变与极端事件的检测与归因的初步研究[D]. 扬州:扬州大学, 2007.
|
[37] |
Qian Weihong, Zhang Henian, Zhu Yafen. Interannual and interdecadal variability of East Asian Acas and their impact on temperature of China in winter season for the last century[J]. Advances in Atmospheric Science, 2001,18(4):511-523.
|
|
|
|