| 天气与气候 |
|
|
|
|
| Response of Desert Climate Change to Global Warming in Minqin, China |
| CHANG Zhao-feng1,2,3, HAN Fu-gui1,2,3, ZHONG Sheng-nian1,2,3 |
| 1.Minqin National Station for Desert Steppe Ecosystem Studies, Wuwei 733300, Gansu, China; 2.Gasu Key Laboratory of Desertification Combating, Lanzhou 730070, China; 3.Gansu Desert Control Research Institute, Lanzhou 730070, China |
|
|
|
|
Abstract Global warming is a widespread concern around the world in recent years. How does desert climate respond to global warming then? In this paper, Minqin county in Gansu province of China, a typical desert area in northwest China, was selected as an example to analyze the response by the use of temperature data, precipitation, relative air humidity, sandstorm days and other related data since 1961. The increase rate of annual average temperature in the study area was higher than the global increase rate in the 20th century and the last 100 years increase rate in China. Analysis of monthly average temperature showed different increase trend in Nov. to Dec. and Feb. to Jun., and the most significant climate warming happened in February. Change amplitude of the highest temperature increased significantly since 1980s the globally warmest period, but the lowest temperature dropped intermittently. So the instability of the highest and the lowest temperature increased. Analysis of annual precipitation showed an upward trend in the study area. Sandstorm days decreased significantly since 1956, and the increase of relative air humidity since 1961 in the study area was main reason.
|
|
Received: 03 August 2010
Published: 20 March 2011
|
|
|
[1]Houghton J T,Ding Y H,Griggs D J,et al.Climate change 2001:The scientific basis[M].Cambridge,UK:Cambridge University Press,2001:15-108. [2]Solomon S,Qin D H,Manning M,et al.Climate change 2007:The physical science basis[M].Cambridge,UK/New York,USA:Cambridge University Press,2007. [3]Kitoh A,Yukimoto S,Noda A,et al.Simulated changes in the Asian summer monsoon at times of increased atmospheric CO2[J].Journal of the Meteorological Society of Japan,1997,75(6):1019-1031. [4]Parker D E.Large-scale warming is not urban[J].Nature,2004,432:290-290. [5]Ding Y H.Global climate change[J].World Environment,2002,6:9-12. [6]Jauregui E.The dust storms of Mexico City[J].International Journal of Climatology,1989,9(2):169-180. [7]Dlugokencky E J,Myers R C,Lang P M,et al.Conversion of NOAA CMDL atmospheric dry air CH4 mole fractions to a gravimetrically prepared standard scale[J].Journal of Geophysical Research,2005,110:D18306. [8]Trenberth K E,Stepaniak D P,Caron J M.Interannual variations in the atmospheric heat budget[J].Journal of Geophysical Research,2002,107(4066). [9]王绍武,蔡静宁,朱锦红,等.中国气候变化的研究[J].气候与环境研究,2002(7):137-145. [10]丁一汇.中国西部环境变化的预测[M]//秦大河.中国西部环境演变评估.北京:科学出版社,2002:1-231. [11]沙万英,邵雪梅,黄玫.20世纪80年代以来中国的气候变暖及其对自然区域界限的影响[J].中国科学(D辑),2002,32(4):317-326. [12]任朝霞,杨达源.近50 a西北干旱区气候变化对农业的影响[J].干旱区资源与环境,2007,21(8):48-53. [13]魏文寿,袁玉江,喻树龙,等.中国天山山区235 a气候变化及降水趋势预测[J].中国沙漠,2008,28(5):803-808. [14]白美兰,郝润全,沈建国.近46 a气候变化对呼伦湖区域生态环境的影响[J].中国沙漠,2008,28(1):101-107. [15]张凯,司建华,王润元,等.气候变化对阿拉善荒漠植被的影响研究[J].中国沙漠,2008,28(5):879-885. [16]苏志珠,卢琦,吴波,等.气候变化和人类活动对我国荒漠化的可能影响[J].中国沙漠,2006,26(3):329-335. [17]韩邦帅,薛娴,王涛,等.沙漠化与气候变化互馈机制研究进展[J].中国沙漠,2008,28(3):410-416. [18]胡汝骥,樊自立,王亚俊,等.近50 a新疆气候变化对环境影响评估[J].干旱区地理,2001,24(2):97-103. [19]李耀辉,张书余.我国沙尘暴特征及其与干旱关系的研究进展[J].地球科学进展,2007,22(11):1169-1176. [20]张莉,任国玉.中国北方沙尘暴频数演化及其气候特征成因分析[J].气象学报,2003,61(6):744-750. |
| No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
| |
Shared |
|
|
|
|
| |
Discussed |
|
|
|
|