天气与气候

新疆天山极端干湿事件时空演变特征

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  • 1.新疆师范大学地理科学与旅游学院,新疆 乌鲁木齐 830054
    2.新疆师范大学丝绸之路经济带城市发展中心,新疆 乌鲁木齐 830054
曹丽君(1994-),女,硕士研究生,主要研究方向为自然资源开发与规划. E-mail: 1429681889@qq.com

收稿日期: 2020-06-22

  修回日期: 2020-07-21

  网络出版日期: 2021-03-05

基金资助

国家自然科学基金项目(41761004);新疆师范大学丝绸之路经济带城市发展研究中心开放课(XJNURWJD062017B02)

Spatio-temporal evolution of the extreme dry and wet events in Tianshan Mountains, Xinjiang, China

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  • 1. College of Geography Science and Tourism, Xinjiang Normal University, Urumqi 830054, Xinjiang, China
    2. Study Center for Belt Urban Development along Silk Road Economic Belt, Xinjiang Normal University, Urumqi 830054, Xinjiang, China

Received date: 2020-06-22

  Revised date: 2020-07-21

  Online published: 2021-03-05

摘要

基于新疆天山26个气象站1960—2017年的气象资料,采用FAO Penman-Monteith模型计算了各气象站月地表湿润指数,标准化后统计极端干湿事件频率。运用线性趋势分析法、反距离加权法探究了极端干湿事件频率的时空演变特征,并采用相关分析、偏相关分析及交叉小波分析分别探讨了气象因子和大气环流对极端干湿事件变化的影响。结果表明:(1) 新疆天山极端干、湿事件分别呈减少、增加趋势,年际倾向率分别为-0.40次·(10a)-1、0.37次·(10a)-1。夏季为天山极端干、湿事件的共同高发季节,也是极端干旱下降趋势最大的季节,而秋季是极端湿润上升趋势最大的季节。(2) 天山北坡是极端干旱事件和极端湿润事件的共同高发区域,极端干、湿事件发生频率高达4.44次·a-1、2.76次·a-1,也是极端干旱下降、极端湿润上升速率最快的区域,平均年际倾向率分别为-0.75次·(10a)-1、0.58次·(10a)-1。(3) 平均相对湿度是导致该区域极端干湿事件变化的主要气象因子,厄尔尼诺-南方涛动(El Ni?o-Southern Oscillation)是主要大气环流因素。

本文引用格式

曹丽君,孙慧兰,兰小丽,张乐乐,卢宝宝,刘天弋 . 新疆天山极端干湿事件时空演变特征[J]. 干旱区研究, 2021 , 38(1) : 188 -197 . DOI: 10.13866/j.azr.2021.01.20

Abstract

The FAO Penman-Monteith model was used to calculate the monthly surface humid index at 26 meteorological stations in the Tianshan Mountains, Xinjiang, China, based on their meteorological data from 1960 to 2017. The extreme dry and wet event frequencies were calculated after standardizing the data. Subsequently, the Mann-Kendall trend analysis and inverse distance weighting methods were used to explore their spatio-temporal evolutionary characteristics. Pearson and partial correlation analyses and cross wavelet transform were used to investigate the influence of meteorological factors and atmospheric circulation on the extreme dry and wet events. The results showed that (1) the interannual decrease and increase in extreme dry and wet events were -0.40 and 0.37 times per decade, respectively. The highest occurrence of extreme dry and wet events and the largest decrease in extreme dry events occurred in summer, while the largest increase in extreme wet events was in autumn; (2) the northern slope exhibited the highest incidence of extreme dry and wet events, with a frequency of 4.36 and 2.76 times a year, respectively. It also exhibited the fastest rate of decline in extreme dry and increase in extreme wet events, with an average annual incidence of -0.75 and 0.58 times per decade, respectively; and (3) the average relative humidity was the primary meteorological factor influencing the changes in extreme dry and wet events in the region, and the El Ni?o-Southern Oscillation was the main atmospheric circulation factor.

参考文献

[1] IPCC. Climate Change 2013: The Physical Science Basis by IPCC Working Group I[M]. Cambridge: Cambridge University Press, 2013: 1535
[2] Wentz F J, Ricciardulli L, Hilburn K, et al. How much more rain will global warming bring?[J]. Science, 2007,317(5835):233-235.
[3] Zhang Q, Singh V P, Li J F, et al. Analysis of the periods of maximum consecutive wet days in China[J]. Journal of Geophysical Research, 2011,116(23):D23106.
[4] 商沙沙, 廉丽姝, 马婷, 等. 近54 a中国西北地区气温和降水的时空变化特征[J]. 干旱区研究, 2018,35(1):68-76.
[4] [ Shang Shasha, Lian Lishu, Ma Ting, et al. Spatiotemporal variation of temperature and precipitation in Northwest China in recent 54 years[J]. Arid Zone Research, 2018,35(1):68-76. ]
[5] 黄萌田, 周佰铨, 翟盘茂. 极端天气气候事件变化对荒漠化、土地退化和粮食安全的影响[J]. 气候变化研究进展, 2020,16(1):17-27.
[5] [ Huang Mengtian, Zhou Baiquan, Zhai Panmao. Impacts of extreme weather and climate events on desertification, land degradeation and food security[J]. Climate Change Research, 2020,16(1):17-27. ]
[6] 许吟隆, 赵运成, 翟盘茂. IPCC特别报告SRCCL关于气候变化与粮食安全的新认知与启示[J]. 气候变化研究进展, 2020,16(1):37-49.
[6] [ Xu Yinlong, Zhao Yuncheng, Zhai Panmao. Advances in scientific understanding on climate change and food security from IPCC special report SRCCL[J]. Climate Change Research, 2020,16(1):37-49. ]
[7] 黄小燕, 李耀辉, 冯建英, 等. 中国西北地区降水量及极端干旱气候变化特征[J]. 生态学报, 2015,35(5):1359-1370.
[7] [ Huang Xiaoyan, Li Yaohui, Feng Jianying, et al. Climate characteristics of precipitation and extreme drought events in Northwest China[J]. Acta Ecologica Sinica, 2015,35(5):1359-1370. ]
[8] 刘维成, 张强, 傅朝. 近55年来中国西北地区降水变化特征及影响因素分析[J]. 高原气象, 2017,36(6):1533-1545.
[8] [ Liu Weicheng, Zhang Qiang, Fu Zhao. Variation characteristics of precipitation and it’s affecting factors in Northwest China over the past 55 Years[J]. Plateau Meteorology, 2017,36(6):1533-1545. ]
[9] 张永, 陈发虎, 勾晓华, 等. 中国西北地区季节间干湿变化的时空分布——基于PDSI数据[J]. 地理学报, 2007,62(11):1142-1152.
[9] [ Zhang Yong, Chen Fahu, Gou Xiaohua, et al. The temporal and spatial distribution of seasonal dry-wet changes over the northwestern China: Based on PDSI[J]. Journal of Geographical Sciences, 2007,62(11):1142-1152. ]
[10] 慈晖, 张强, 张江辉, 等. 1961—2010年新疆极端降水过程时空特征[J]. 地理研究, 2014,33(10):1881-1891.
[10] [ Ci Hui, Zhang Qiang, Zhang Jianghui, et al. Spatiotemporal variations of extreme precipitation events within Xinjiang during 1961-2010[J]. Geographical Research, 2014,33(10):1881-1891. ]
[11] 谢培, 顾艳玲, 张玉虎, 等. 1961—2015年新疆降水及干旱特征分析[J]. 干旱区地理, 2017,40(2):332-339.
[11] [ Xie Pei, Gu Yanling, Zhang Yuhu, et al. Precipitation and drought characteristics in Xinjiang during 1961-2015[J]. Arid Land Geography, 2017,40(2):332-339. ]
[12] 施雅风, 沈永平, 李栋梁, 等. 中国西北气候由暖干向暖湿转型的特征和趋势探讨[J]. 第四纪研究, 2003,23(2):152-164.
[12] [ Shi Yafeng, Shen Yongping, Li Dongliang, et al. Discussion on the present climate change from warn dry to warm wet in Northwest China[J]. Quaternary Sciences, 2003,23(2):152-164. ]
[13] 陈迪桃, 黄法融, 李倩, 等. 1966—2015年天山南北坡空气湿度差异及其影响因素[J]. 气候变化研究进展, 2018,14(6):562-572.
[13] [ Chen Ditao, Huang Farong, Li Qian, et al. Spatial variation of humidity and its influencing factors in the north and south slopes of the Tianshan Mountains, China during 1966-2015[J]. Climate Change Research, 2018,14(6):562-572. ]
[14] 王晶, 肖海峰. 2000—2015年新疆粮食生产时空演替与驱动因素分析[J]. 中国农业资源与区划, 2018,39(2):58-66.
[14] [ Wang Jing, Xiao Haifeng. The spatial-temporal pattern changes and driving factors of grain production in Xinjiang province[J]. Chinese Journal of Agricultural Resources and Regional Planning, 2018,39(2):58-66. ]
[15] 程新宇杰, 高路. 基于综合自然区划的天山区域气温变化研究[J]. 山地学报, 2018,36(2):194-205.
[15] [ Cheng Xinyujie, Gao Lu. Temperature changes in Tianshan Mountains based on integrated physicogeographical regionalization[J]. Mountain Research, 2018,36(2):194-205. ]
[16] 刘友存, 焦克勤, 赵奎, 等. 中国天山地区降水对全球气候变化的响应[J]. 冰川冻土, 2017,39(4):748-759.
[16] [ Liu Youcun, Jiao Keqin, Zhao Kui, et al. The response of precipitation to global climate change in the Tianshan Mountains, China[J]. Journal of Glaciology and Geocryology, 2017,39(4):748-759. ]
[17] 丁之勇, 董义阳, 鲁瑞洁. 1960—2015年中国天山南、北坡与山区极端气温时空变化特征[J]. 地理科学, 2018,38(8):1379-1390.
[17] [ Ding Zhiyong, Dong Yiyang, Lu Ruijie. Spatio-temporal variability of temperature extremes in Tianshan Mountains area, Northwest China, during 1960-2015[J]. Scientia Geographica Sinica, 2018,38(8):1379-1390. ]
[18] 钟巧, 焦黎, 李稚, 等. 博斯腾湖流域潜在蒸散发时空演变及归因分析[J]. 干旱区地理, 2019,42(1):103-112.
[18] [ Zhong Qiao, Jiao Li, Li Zhi, et al. Spatial and temporal changes of potential evapotranspiration and its attribution in the Bosten Lake Basin[J]. Arid Land Geography, 2019,42(1):103-112. ]
[19] 祝昌汉. 再论总辐射的气候学计算方法(二)[J]. 南京气象学院学报, 1982(2):196-206.
[19] [ Zhu Changhan. A further discussion on the climatological calculating method of total radiation[J]. Journal of Nanjing Meteorology, 1982(2):196-206. ]
[20] 马柱国, 华丽娟, 任小波. 中国近代北方极端干湿事件的演变规律[J]. 地理学报, 2003,58(增刊):69-74.
[20] [ Ma Zhuguo, Hua Lijuan, Ren Xiaobo. The extreme dry/wet events in northern China during recent 100 years[J]. Journal of Geographical Sciences, 2003,58(Suppl. ): 69-74. ]
[21] 孙卫国, 程炳岩. 交叉小波变换在区域气候分析中的应用[J]. 应用气象学报, 2008,19(4):479-487.
[21] [ Sun Weiguo, Cheng Bingyan. Application of Cross Wavelet Transformation to analysis on regional climate variations[J]. Journal of Applied Meterological Science, 2008,19(4):479-487]
[22] Torrence C, Compo G P. A practical guide to wavelet analysis[J]. Bulletin of the American Meteorological Society, 1998,79(1):1-78.
[23] Li Y, Huang S Z, Ma L, et al. Spatiotemporal changes in extreme wet and dry conditions and linkages with planetary oscillations[J]. Journal of Coastal Research, 2018,84(Suppl. ): 134-143.
[24] 曹立国, 潘少明, 贾培宏, 等. 1960—2009年河西地区极端干湿事件的演变特征[J]. 自然资源学报, 2014,29(3):480-489.
[24] [ Cao Liguo, Pan Shaoming, Jia Peihong, et al. Temporal and spatial characteristics of the extreme drought and wet events changes in Hexi Area from 1960 to 2009[J]. Journal of Natural Resources, 2014,29(3):480-489. ]
[25] 吴燕锋, 巴特尔·巴克, 魏小琴, 等. 阿勒泰地区极端干湿事件的时空变化特征[J]. 自然灾害学报, 2015,24(4):138-147.
[25] [ Wu Yanfeng, Bake Batur, Wei Xiaoqin, et al. Spatiotemporal change characteristics of extreme wet and dry events in Altay[J]. Journal of Natural Disasters, 2015,24(4):138-147. ]
[26] 贾艳青, 张勃. 1960-2016年中国北方地区极端干湿事件演变特征[J]. 自然资源学报, 2019,34(7):1543-1554.
[26] [ Jia Yanqing, Zhang Bo. Spatio-temporal changes of the extreme drought and wet events in Northern China from 1960 to 2016[J]. Journal of Natural Resources, 2019,34(7):1543-1554. ]
[27] 张明军, 李瑞雪, 黄小燕, 等. 中国天山山区风速变化特征[J]. 干旱区资源与环境, 2012,26(7):78-83.
[27] [ Zhang Mingjun, Li Ruixue, Huang Xiaoyan, et al. Changes of wind speed in Tianshan Mountains[J]. Journal of Arid Land Resources and Environment, 2012,26(7):78-83. ]
[28] 辛宏, 张明军, 李瑞雪, 等. 近50年中国天山日照时数变化及其影响因素[J]. 干旱区研究, 2011,28(3):485-491.
[28] [ Xin Hong, Zhang Mingjun, Li Ruixue, et al. Analysis on the change of sunshine duration and its affecting factors in the Tianshan Mountains in recent 50 years[J]. Arid Zone Research, 2011,28(3):485-491. ]
[29] 黄静, 张运, 汪明秀, 等. 近17年新疆干旱时空分布特征及影响因素[J]. 生态学报, 2020,40(3):1077-1088.
[29] [ Huang Jing, Zhang Yun, Wang Mingxiu, et al. Spatial and temporal distribution characteristics of drought and its relationship with meteorological factors in Xinjiang in last 17 years[J]. Acta Ecologica Sinica, 2020,40(3):1077-1088. ]
[30] 王妮, 崔彩霞, 刘艳. 新疆暴雨洪涝灾害损失的时空特征及其影响因素[J]. 干旱区研究, 2020,37(2):325-330.
[30] [ Wang Ni, Cui Caixia, Liu Yan. Temporal-spatial characteristics and influencing factors of rainstorm-flood disasters in Xinjiang[J]. Arid Zone Research, 2020,37(2):325-330. ]
[31] 王文静, 延军平, 刘永林. 新疆旱涝气候的南北差异性分析[J]. 干旱区研究, 2016,33(3):609-618.
[31] [ Wang Wenjing, Yan Junping, Liu Yonglin. Difference of drought/flood disasters in Xinjiang[J]. Arid Zone Research, 2016,33(3):609-618. ]
[32] 阿迪来·乌甫, 玉素甫江·如素力, 热伊莱·卡得尔, 等. 基于MODIS数据的新疆地表蒸散量时空分布及变化趋势分析[J]. 地理研究, 2017,36(7):1245-1256.
[32] [ Adilai Wufu, Yusufujiang Rusuli, Reyilai Kadeer, et al. Spatio-temporal distribution and evolution trend of evapotranspiration in Xinjiang based on MOD16 data[J]. Geographical Research, 2017,36(7):1245-1256. ]
[33] 李福夺, 杨兴洪. 新疆粮食生产波动——波动特征与影响因素[J]. 干旱区资源与环境, 2016,30(8):54-61.
[33] [ Li Fuduo, Yang Xinghong. The food production fluctuation in Xinjiang: Fluctuation characteristics, influence factors and policy recommendations[J]. Journal of Arid Land Resources and Environment, 2016,30(8):54-61. ]
[34] 向明燕, 范丽红, 海米提·依米提, 等. 新疆近45年气象灾害及其防御措施[J]. 干旱区研究, 2007,24(5):712-716.
[34] [ Xiang Mingyan, Fan Lihong, Haimit Yimiti, et al. Study on the change of meteorological disasters and the prevention measures in Xinjiang since recent 45 years[J]. Arid Zone Research, 2007,24(5):712-716. ]
[35] 罗青红, 宁虎森, 陈启民. 基于湿润指数的新疆甘家湖地表干湿状况变化趋势[J]. 干旱区研究, 2016,33(5):921-926.
[35] [ Luo Qinghong, Ning Husen, Chen Qimin. Trends of surface dry-wet state of Ganjiahu in Xinjiang based on humid index[J]. Arid Zone Research, 2016,33(5):921-926. ]
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