RESEARCH ON CLIMATE CHANGES IN ZHEJIANG PROVINCE
-
摘要: 为了区分不均一与局地气候的突变,采用功效不同的SNHT、Buishand、Pettitt 三种均一性检验法对浙江省41 个气象观测站1960—2007 年的温度和降水的观测序列进行检验。通过对三种方法检验的站点数据做气候变化事实研究发现,近50 年浙江省与全球呈现一致的气温年代际变化特征,0.19 ℃/(10 a)的平均气温倾向率比0.13 ℃/(10 a)的全球平均值高,略低于0.22 ℃/(10 a)的全国平均值。全省年平均降水量呈上升趋势,这与中国降水量总体下降的变化趋势相反,但与长江流域以南的变化趋势一致;强降水、高温热浪等极端天气事件频率增大,城市局地气候趋于“ 热干” 化;≥10 ℃的初日提早10 天左右,而终日推迟了近10 天,在持续日数增加的同时,有效积温也相应增大。Abstract: In order to track down the inhomogeneities in station data records caused by station relocation or measuring technique changes, three homogeneity tests are applied to evaluate the daily station series (1960— 2007) of surface air temperature and precipitation in Zhejiang province, and then using the useful station data, a detailed study has been undertaken of climate change features of Zhejiang province. The study reveals that annual mean temperature in Zhejiang presents a similar trend to the global one, and the warming rate, 0.19℃/(10 a), is higher than the global rate of 0.13 ℃/(10 a) and lower than 0.22 ℃/(10 a), the rate for China. Annual average precipitation also presents an increasing trend, which is consistent with that of the south of the Yangtze River basin, but opposite to the general decreasing trend of China. The frequency of heavy rain and heat wave increases and local climate in the inner parts of cities presents a “dry & heat” trend. The study also shows that the beginning of 10 ℃ effective accumulated temperature is nearly ten days earlier, and the ending is almost ten days later, than normal; meanwhile, the annual accumulated days and the effective accumulated temperature both present increasing trends.
-
Key words:
- climatology /
- climate change /
- homogeneity test /
- Zhejiang province
-
[1] 葛全胜,王绍武,方修琦. 气候变化研究中若干不确定性的认识问题[J]. 地理研究,2010,29(2):191-203. [2] SOLOMON S, QIN D, MANNING M, et al. Climate Change 2007: The physical science basis, contribution of working group i to the fourth assessment report of the intergovernmental panel on climate change[M]. Cambridge: Cambriage University Press, 2007: 996. [3] BALINT M, JABBOUR J, MCMULLEN C, et al. Climate change science compendium 2009[M]. SCOPE, WMO, 2009: 683. [4] ALLISON I, BINDOFF N L, BINASCHADLER, et al. The copenhagen diagnosis. Sydney, Australia: The University of New South Wales Climate Change Research Centre (CCRC)[R]. 2009: 60. [5] SINGER S F, ANDERSON W, GOLDBERG F, et al. Nature, not human activity, rules the climate: Summary for policymakers of the report of the Nongovernmental International Panel on Climate Change (NIPCC)[R]. Chicago, IL: The Heatland Institute, 2008: 40. [6] IDSO C, SINGER S F. Climate change reconsidered: 2009 Report of the Nongovernmental International Panel on Climate Change (NIPCC)[R]. Chicago: The Heartland Institute, 2009: 868. [7] SINGER S F. Human contribution to climate change remains questionable[J]. EOS, 1999, 80: 183-187. [8] SINGER S F. Science editor bias on climate change[J]. Science, 2003, 301: 595-596. [9] 顾骏强,施能,王永波. 近50 年浙江省旱、涝气候变化及特征[J]. 热带气象学报,2001,17(4):429-435. [10] 陈兴芳,晃淑懿. 台风活动的气候突变[J]. 热带海洋学报,1997,13(2): 97-104. [11] 王大钧,张运福,陈列,等. 近40 年来中国降水量、雨日变化趋势及与全球温度变化的关系[J]. 热带气象学报,2006,22(3):283-289. [12] WIJNGAARD J B, KLEIN TANK A M G, KONNEN G P. Homogeneity of 20th century European daily temperature and precipitation series[J]. Int J Climatol, 2003, 23: 679-692. [13] 刘小宁,孙安健. 年降水量序列非均一性检验方法探讨[J]. 气象, 1995,8: 3-6. [14] 刘小宁. 我国40 年年平均风速的均一性检验[J]. 应用气象学报,2000,11(1):27-34. [15] POTTER K W. Illustration of a new test for detecting a shift in mean precipitation series[J]. Mon Wea Rev, 1981, 109(9): 2 040-2 045. [16] EASTERLING D R, PETERSON T C. Techniques for detecting and adjusting for artificial discontinuities in climatological time series: A review[C]//Fifth international meeting on statistical climatology. 1992: 28-32. [17] EASTERLING D R, PETERSON T C. A new method for detecting undocumented discontinuities in climatological time series[J]. Int J Climatol, 1995, 15: 369-377. [18] HERZOG J, MULLER W G. Homogenization of various climatological parameters in the German Weather Service[C]//Proceedings of the first seminar for homogenization of surface climatological data. 1996: 101-111. [19] 王绍武. 20 世纪气候学理论研究的十项成就[J]. 地球科学进展,2000,15(3): 277-282. [20] 王绍武. 现代气候学研究进展[M]. 北京:气象出版社. 2001: 3-22. [21] 秦大河,等. 中国气候与环境演变(上) [M]. 北京:科学出版社. 2005: 52-54. [22] 宋艳华,张润仙,罗律,等. 气候变暖背景下清远气温变化特征[J]. 气象与环境学报,2008, 24(3): 38-41. [23] 王英,曹明奎,陶波,等. 全球气候变化背景下中国降水量空间格局的变化特征[J]. 地理研究,2006,25(6):1 031-1 041.
点击查看大图
计量
- 文章访问数: 1832
- HTML全文浏览量: 5
- PDF下载量: 1839
- 被引次数: 0