GUAN Yue,HE Qijin,LIU Jiahong,et al.Variation Characteristics of Extreme Temperature and Its Earliest and Latest Day Sequence in Huang-Huai-Hai Region During the Period 1961 to 2015[J].Research of Soil and Water Conservation,2021,28(01):147-152.
黄淮海地区1961—2015年极端气温及其初终日序的变化特征
- Title:
- Variation Characteristics of Extreme Temperature and Its Earliest and Latest Day Sequence in Huang-Huai-Hai Region During the Period 1961 to 2015
- 文章编号:
- 1005-3409(2021)01-0147-06
- 分类号:
- P467
- 文献标志码:
- A
- 摘要:
- 针对气候变化背景下极端事件频发的现状,采用百分位阈值法、线性回归、M-K突变检验、显著性检验等方法分析了1961—2015年黄淮海地区极端气温及其发生日序的时空变化特征。结果表明:(1)黄淮海地区的平均极端高温为32.6℃、极端低温为-9.0℃; 极端高温主要呈经向分布,极端低温呈纬向分布,极端低温受海陆位置影响较小。(2)1961—2015年极端高温呈高—低—高的变化趋势; 极端低温有显著升高趋势,其中京津冀地区升幅最大,气候倾向率均达到了0.6℃/10 a以上。(3)极端高温和极端低温的发生初日均呈提前趋势,但极端高温的终日推迟,而极端低温的终日提前结束。这表明黄淮海地区将出现秋季降温和春季升温提前趋势,将对冬小麦和夏玉米生产产生重大影响。
- Abstract:
- Considering the current situation of more extreme temperature events happened in the context of climate change, we described the characteristics of extreme temperature in Huang-Huai-Hai region from 1961 to 2015 based on daily temperature data. The methods including percentile thresholds, linear regression, m-k mutation test, significance test were employed to delineate the characteristics of extreme temperature and its occurrence sequence. Important results were obtained as follows.(1)In Huang-Huai-Hai region, the average extreme high temperature was 32.6℃, and the extreme low temperature was -9.0℃. Extreme high temperatures tended to distribute in a meridional direction, and extreme low temperatures distributed in a zonal direction, indicating that extreme low temperatures were less affected by the location of the sea and land.(2)From 1961 to 2015, the extreme high temperature showed a high-low-high trend, and the extreme low temperature showed the significantly increasing trend, of which the increase in Beijing-Tianjin-Hebei region was the largest, climate tendency rate reached above 0.6℃/decade.(3)The advance of the earliest day of extreme high temperature and the delay of the latest day indicated that that extreme high temperature might occur earlier and the duration prolonged. Extreme low temperature had the characteristics of early occurrence and early termination. It is indicated that the temperature in Huang-Huai-Hai region will fall earlier in autumn and rise earlier in spring, and will seriously affect the production of winter wheat and summer maize.
参考文献/References:
[1] Stocker T F, Qin D, Plattner G K, et al. Climate change 2013:The physical science basis[R]. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, 2013.
[2] 丁一汇,王会军.近百年中国气候变化科学问题的新认识[J].科学通报,2016,61(10):1029-1041.
[3] 曲建升,肖仙桃,曾静静.国际气候变化科学百年研究态势分析[J].地球科学进展,2018,33(11):1193-1202.
[4] 翟盘茂,潘晓华.中国北方近50年温度和降水极端事件变化[J].地理学报,2003,58(S1):1-10.
[5] 齐庆华,蔡榕硕,郭海峡.中国东部气温极端特性及其气候特征[J].地理科学,2019,39(8):1340-1350.
[6] Alexander L V, Zhang X, Peterson T C, et al. Global observed changes in daily climate extremes of temperature and precipitation[J]. Journal of Geophysical Research, 2006,111(5):1042-1063.
[7] Choi G, Collins D, Ren G, et al. Changes in means and extreme events of temperature and precipitation in the Asia-Pacific Network region, 1955-2007[J]. International Journal of Climatology, 2009,29(13):1906-1925.
[8] Manton M J, Dellamarta P M, Haylock M, et al. Trends in extreme daily rainfall and temperature in Southeast Asia and the South Pacific:1961-1998[J]. International Journal of Climatology, 2001,21(3):269-284.
[9] 周雅清,任国玉.中国大陆1956—2008年极端气温事件变化特征分析[J].气候与环境研究,2010,15(4):405-417.
[10] Gruza G V, Rankova E, Razuvaev V, et al. Indicators of Climate Change for the Russian Federation[J]. Climatic Change, 1999,42(1):219-242.
[11] Vincent L A, Mekis E. Changes in daily and extreme temperature and precipitation indices for Canada over the twentieth century[J]. Atmosphere-Ocean, 2006,44(2):177-193.
[12] 王琼,张明军,王圣杰,等.1962—2011年长江流域极端气温事件分析[J].地理学报,2013,68(5):611-625.
[13] 王怀军,潘莹萍,陈忠升.1960—2014年淮河流域极端气温和降水时空变化特征[J].地理科学,2017,37(12):1900-1908.
[14] 韩晖,李耀辉.气象极值变化及其导致的农业气象灾害趋势分析:以甘肃省为例[J].冰川冻土,2013,35(4):999-1006.
[15] 伍红雨,杜尧东.1961—2008年华南地区极端气温的非对称变化[J].生态学杂志,2010,29(11):2241-2248.
[16] 王冀,蒋大凯,张英娟.华北地区极端气候事件的时空变化规律分析[J].中国农业气象,2012,33(2):166-173.
[17] 黄琰,封国林,董文杰.近50年中国气温、降水极值分区的时空变化特征[J].气象学报,2011,69(1):125-136.
[18] Bonsal B R, Zhang X B, Vincent L A, et al. Characteristics of Daily and Extreme Temperatures over Canada[J]. Journal of Climate, 2001,14(9):1959-1976.
[19] 黄嘉佑.气象统计分析与预报方法[M].北京:气象出版社,2016.39-48.
[20] 王丽君.黄淮海平原夏玉米季干旱、高温的发生特征及对产量的影响[D].北京:中国农业大学,2018.
[21] 柏会子,肖登攀,刘剑锋,等.1965—2014年华北地区极端气候事件与农业气象灾害时空格局研究[J].地理与地理信息科学,2018,34(5):99-105.
[22] 卫捷,孙建华.华北地区夏季高温闷热天气特征的分析[J].气候与环境研究,2007,12(3):453-463.
[23] 曹祥会,龙怀玉,张继宗,等.河北省主要极端气候指数的时空变化特征[J].中国农业气象,2015,36(3):245-253.
[24] 邓梅,蔡海朝,马琴,等.1961—2010年湘中地区气候极值与农业气候指标动态变化趋势[J].中国农学通报,2018,34(25):145-150.
[25] 曹永旺,延军平.1961—2013年山西省极端气候事件时空演变特征[J].资源科学,2015,37(10):2086-2098.
[26] 黄小燕,王小平,王劲松,等.1960—2013年中国沿海极端气温事件变化特征[J].地理科学,2016,36(4):612-620.
[27] 张新宜,周晓宇,刘熠炎.1954—2013年湖北省黄石市极值气温变化特征分析[J].气象研究与应用,2015,36(2):85-92,95.
[28] 周雅清,任国玉.城市化对华北地区极端气温事件频率的影响[J].高原气象,2014,33(6):1589-1598.
[29] Li Q, Yang S, Xu W, et al. China experiencing the recent warming hiatus[J]. Geophysical Research Letters, 2015,42(3):889-898.
[30] 琚建华,任菊章.大气环流年代际变化对东亚北部冬季气温异常的影响[J].云南大学学报:自然科学版,2003,25(6):518-524.
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备注/Memo
收稿日期:2020-04-16 修回日期:2020-05-01
资助项目:国家重点研发计划项目(2016YFD0300106,2017YFD0300304,2017YFD0300404)
第一作者:管玥(1997—),女,贵州省安顺市人,硕士生,研究方向农业应对气候变化。E-mail:didididi_97@163.com
通信作者:何奇瑾(1981—),女,吉林省蛟河市人,博士,副教授,研究方向农业应对气候变化。E-mail:heqijin@cau.edu.cn