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Arid Land Geography >

2021 , Vol. 44 >Issue 5: 1290 - 1298

DOI: https://doi.org/10.12118/j.issn.1000–6060.2021.05.10

Climatology and Hydrology

Spatial and temporal changes of high wind days over category 6 and above in Inner Mongolia from 1961 to 2018

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  • 1. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, College of Applied Meteorology, Nanjing University of Information Science & Technology, Jiangsu 210044, Nanjing, China
    2. Jiangsu Key Laboratory of Agricultural Meteorology, Nanjing University of Information Science & Technology, Jiangsu 210044, Nanjing, China
    3. Ecology and Agrometeorology Center of Inner Mongolia Autonomous Region, Hohhot 010051, Inner Mongolia, China

Received date: 2020-07-03

  Revised date: 2020-12-17

  Online published: 2021-09-22

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Abstract

Research on changes in strong wind days is important for regional climate change, disaster prevention and mitigation, and wind energy development. Therefore, the spatial and temporal distribution characteristics of strong wind days in Inner Mongolia, China were analyzed using statistical methods based on daily wind speed data of 85 meteorological stations in and around Inner Mongolia from 1961 to 2018. The results showed that: (1) Over the past 58 years, the number of strong wind days in Inner Mongolia decreased overall, and the climate tendency rate was -16.52 d·(10a)-1. On a seasonal scale, the number of strong spring wind days was the largest, accounting for 44.30% of the year, the most significant decline [-6.24 d·(10a)-1] of all seasons. On a wind level scale, strong wind days of level 6 were the most frequent, accounting for 80.93% of all strong wind days, the most significant decline [-11.99 d·(10a)-1] of all levels. (2) The spatial distribution of strong wind days was large in the central part of Inner Mongolia and small in the northeastern and southwestern parts. Strong wind days occurred more frequently in Xilin Gol League, Ulanqab City, and Chifeng City but less frequently in Ordos City and Hohhot City. (3) Level 6 strong wind days were mainly concentrated in central cities, and level 8 (and higher) strong wind days were distributed in western and eastern cities. All cities showed a decreasing trend. Ulanqab City showed the highest climate trend rate of -5.49 d·(10a)-1, and Hohhot City showed the lowest trend rate of -0.01 d·(10a)-1.

Key words： high wind days; spatial and temporal distribution; climate tendency rate; Inner Mongolia

Cite this article

XING Lizhu,ZHANG Fangmin,HUANG Jin,LI Yunpeng . Spatial and temporal changes of high wind days over category 6 and above in Inner Mongolia from 1961 to 2018[J]. Arid Land Geography, 2021 , 44(5) : 1290 -1298 . DOI: 10.12118/j.issn.1000–6060.2021.05.10

References

[1] 张晓龙, 沈冰, 黄领梅. 基于ITPCAS再分析资料中国近地面风速时空变化特征[J]. 干旱区研究, 2020, 37(1):1-9.
[1] [ Zhang Xiaolong, Shen Bing, Huang Lingmei. Spatiotemporal variation of near surface wind speed over China based on ITPCAS reanalyzed dataset[J]. Arid Zone Research, 2020, 37(1):1-9. ]
[2] Pryor S C, Schoof J T, Barthelmie R J, et al. Winds of change: Projections of near-surface winds under climate change scenarios[J]. Geophysical Research Letters, 2006, 33(11):L11702, doi: 10.1029/2006GL026000.
[3] 王楠, 游庆龙, 刘菊菊. 1979-2014年中国地面风速的长期变化趋势[J]. 自然资源学报, 2019, 34(7):1531-1542.
[3] [ Wang Nan, You Qinglong, Liu Juju. The long-term trend of surface wind speed in China from 1979 to 2014[J]. Journal of Natural Resources, 2019, 34(7):1531-1542. ]
[4] 马爱华, 岳大鹏, 赵景波, 等. 近60 a来内蒙古极端降水时空变化及其影响[J]. 干旱区研究, 2020, 37(1):74-85.
[4] [ Ma Aihua, Yue Dapeng, Zhao Jingbo, et al. Spatiotemporal variation and effect of extreme precipitation in Inner Mongolia in recent 60 years[J]. Arid Zone Research, 2020, 37(1):74-85. ]
[5] 李玲萍, 李岩瑛, 孙占峰, 等. 河西走廊东部沙尘暴特征及地面气象因素影响机制[J]. 干旱区研究, 2019, 36(6):1457-1465.
[5] [ Li Lingping, Li Yanying, Sun Zhanfeng, et al. Sandstorm and its affecting meteorological factors in east Hexi Corridor[J]. Arid Zone Research, 2019, 36(6):1457-1465. ]
[6] Pryor S C, Barthelmie R J, Young D T, et al. Wind speed trends over the contiguous United States[J]. Journal of Geophysical Research Atmospheres, 2009, 114:D14105, doi: 10.1029/2008JD011416.
[7] Mcvicar T R, Niel T G V, Li L T, et al. Wind speed climatology and trends for Australia, 1975-2006: Capturing the stilling phenomenon and comparison with near-surface reanalysis output[J]. Geophysical Research Letters, 2008, 35:L20403, doi: 10.1029/2008GL035627.
[8] Azorin-Molina C, Vicente-Serrano S M, Mcvucar T R, et al. Homogenization and assessment of observed near-surface wind speed trends over Spain and Portugal, 1961-2011[J]. Journal of Climate, 2014, 27(10):3692-3712.
[9] Kaiser-Weiss A K, Kaspar F, Heene V, et al. Comparison of regional and global reanalysis near-surface winds with station observations over Germany[J]. Advances in Science and Research, 2015, 12(1):187-198, doi: 10.5194/asr-12-187-2015.
[10] Xu M, Chang C P, Fu C B, et al. Steady decline of east Asian monsoon winds, 1969-2000: Evidence from direct ground measurements of wind speed[J]. Journal of Geophysical Research Atmospheres, 2006, 111:D24111, doi: 10.1029/2006JD007337.
[11] 任国玉, 郭军, 徐铭志, 等. 近50年中国地面气候变化基本特征[J]. 气象学报, 2005, 63(6):942-956.
[11] [ Ren Guoyu, Guo Jun, Xu Mingzhi, et al. Climate changes of China’s mainland over the past half century[J]. Acta Meteorologica Sinica, 2005, 63(6):942-956. ]
[12] Jiang Y, Luo Y, Zhao Z C, et al. Changes in wind speed over China during 1956-2004[J]. Theoretical and Applied Climatology, 2010, 99(3):421-430.
[13] 江滢, 罗勇, 赵宗慈, 等. 近50年中国风速变化及原因分析[C]// 中国气象学会. 中国气象学会2007年年会气候变化分会场论文集. 北京: 中国气象学会, 2007: 80-89.
[13] [ Jiang Ying, Luo Yong, Zhao Zongci, et al. Analysis of wind speed variation and its causes in recent 50 years in China[C]// Chinese Meteorological Society. Proceedings of the 2007 Annual Meeting of the Chinese Meteorological Society on Climate Change. Beijing: Chinese Meteorological Society, 2007: 80-89. ]
[14] 孔锋, 李颖, 王一飞, 等. 1961-2016年中国近地表大风日数时空分异特征研究[J]. 安徽农业科学, 2017, 45(31):188-196.
[14] [ Kong Feng, Li Ying, Wang Yifei, et al. Spatial and temporal variation characteristics of near-surface gale days in China from 1961 to 2016[J]. Journal of Anhui Agricultural Sciences, 2017, 45(31):188-196. ]
[15] 俞海洋, 李婷, 陈笑娟, 等. 河北省近30年大风时空分布及成灾特征分析[J]. 灾害学, 2017, 32(2):59-63.
[15] [ Yu Haiyang, Li Ting, Chen Xiaojuan, et al. The spatio-temporal distribution and disaster characteristics analysis of the gale in Hebei Province for nearly 30 years[J]. Journal of Catastrophology, 2017, 32(2):59-63. ]
[16] 张占峰, 张焕平, 马小萍. 柴达木盆地平均风速与大风日数的变化特征[J]. 干旱区资源与环境, 2014, 28(10):90-94.
[16] [ Zhang Zhanfeng Zhang Huanping, Ma Xiaoping. Change features of average wind speed and strong wind days in Chaidamu Basin[J]. Journal of Arid Land Resources and Environment, 2014, 28(10):90-94. ]
[17] 高荣, 尤莉, 白颖哲. 通辽气象站1971-2017年大风日数的变化特征[J]. 内蒙古气象, 2018(3):18-21.
[17] [ Gao Rong, You Li, Bai Yingzhe. The variations of the gale days in Tongliao station from 1971 to 2017[J]. Meteorology Journal of Inner Mongolia, 2018(3):18-21. ]
[18] 杨晓玲, 周华, 杨梅, 等. 河西走廊东部大风日数时空分布及其对沙尘天气的影响[J]. 中国农学通报, 2017, 33(16):123-128.
[18] [ Yang Xiaoling, Zhou Hua, Yang Mei, et al. Gale days in east of Hexi Corridor: Spatial-temporal distribution and effect on sand-dust weather[J]. Chinese Agricultural Science Bulletin, 2017, 33(16):123-128. ]
[19] 王钦, 曾波, 邓力. 1981-2013年内蒙古地区风速的时空变化特征[J]. 内蒙古师范大学学报(自然科学汉文版), 2015, 44(5):674-679.
[19] [ Wang Qin, Zeng Bo, Deng Li. Characteristics of spatial and temporal changes of wind speed during 1981-2013 in Inner Mongolia Autonomous Region[J]. Journal of Inner Mongolia Normal University (Natural Science Edition), 2015, 44(5):674-679. ]
[20] 张宇. 1976-2017年内蒙古最大风速时空特征分析[J]. 内蒙古气象, 2019(4):22-25.
[20] [ Zhang Yu. Analysis of temporal-spatial variation characteristics of max-windspeed during 1976-2017 in Inner Mongolia[J]. Meteorology Journal of Inner Mongolia, 2019(4):22-25. ]
[21] 邢丽珠, 张方敏, 黄进, 等. 1961-2018年内蒙古风速变化及影响因素分析[J]. 干旱区资源与环境, 2020, 34(11):162-168.
[21] [ Xing Lizhu, Zhang Fangmin, Huang Jin, et al. Analysis of spatial and temporal change of wind velocity and its affecting factors in Inner Mongolia[J]. Journal of Arid Land Resources and Environment, 2020, 34(11):162-168. ]
[22] GB/T 28591-2012. 中华人民共和国国家标准: 风力等级[S]. 北京: 中国标准出版社, 2012.
[22] [GB/T 28591—2012. National Standard of the People’s Republic of China: Wind scale[S]. Beijing: Standards Press of China, 2012. ]
[23] 朱乾根, 林锦瑞, 寿绍文, 等. 天气学原理和方法[M]. 第四版. 北京, 气象出版社, 2007: 249.
[23] [ Zhu Qiangen, Lin Jinrui, Shou Shaowen, et al. Principles and methods of synoptic meteorology[M]. 4th ed. Beijing: China Meteorological Press, 2007: 249. ]
[24] 魏凤英. 现代气候统计诊断与预测技术[M]. 第二版. 北京, 气象出版社, 2007: 36-63.
[24] [ Wei Fengying. Modern climate statistical diagnosis and prediction technology[M]. 2nd ed. Beijiing: China Meteorological Press, 2007: 36-63. ]
[25] 王瑾, 闫庆武, 谭学玲, 等. 内蒙古地区植被覆盖动态及驱动因素分析[J]. 林业资源管理, 2019(4):159-167.
[25] [ Wang Jin, Yan Qingwu, Tan Xueling, et al. Vegetation coverage dynamics and its driving factors in Inner Mongolia based on FVC information entropy[J]. Forest Resources Management, 2019(4):159-167. ]
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