PDF Download

[1]XIAO Weiwei,AN Bin.Spatiotemporal Variability of Wind Speed in the Loess Plateau During 1960—2017[J].Research of Soil and Water Conservation,2023,30(04):103-109.[doi:10.13869/j.cnki.rswc.2023.04.020.]

Copy

Spatiotemporal Variability of Wind Speed in the Loess Plateau During 1960—2017

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 30 Number of periods: 2023 04 Page number: 103-109 Column: Public date: 2023-06-10

Title:: Spatiotemporal Variability of Wind Speed in the Loess Plateau During 1960—2017

Author(s):: XIAO Weiwei^1,2, AN Bin^1,2; (1.School of Tourism & Environment, Ankang University, Ankang, Shaanxi 725000, China; 2.Academician Expert Workstation of Shaanxi Association for Science and Technology, Ankang, Shaanxi 725000, China)

Keywords:: wind speed; climate tendency rate; temporal and spatial change; the Loess Plateau

CLC:: P425.4

DOI:: 10.13869/j.cnki.rswc.2023.04.020.

Abstract:: [Objective] The aim of this study is to explore the temporal and spatial variation characteristics of wind speed in the Loess Plateau, and then provide reference for regional disaster prevention and mitigation. [Methods] Based on the measured monthly wind speed data of 59 meteorological stations in the Loess Plateau during 1960 to 2017, the temporal and spatial variation trend of wind speed over annual and four seasons in the Loess Plateau was studied by using linear regression, Mann-Kendall test and sliding t-test, etc. [Results](1)The annual average wind speed in the Loess Plateau decreased significantly at the rate of -0.007 5 m/(s·a), with the largest decline in spring, followed by winter and autumn, with the smallest decline in summer. The monthly average wind speed showed a tendency of increasing first but decreasing afterwards, with the fastest decline in April and the slowest decline in July.(2)The wind speed of annual average, summer, autumn and winter decreased abruptly in 1980s, and the average wind speed in spring did not change abruptly. After the abrupt change, the average wind speed declined the fastest in winter and the slowest in autumn.(3)The spatial distribution of the average wind speed and the change rate of annual and seasonal wind speed showed the characteristics of high in the northwest and low in the southeast. Meteorological stations with decline of wind speed were the most in spring, and the least in summer.(4)The rise of AO index, climate warming and the increase of surface vegetation cover might lead to the long-term downward trend of wind speed in the Loess Plateau. [Conclusion] In the Loess Plateau, spring should be taken as the key period in terms of wind prevention, and the northwest should be taken as the key prevention area in which the construction of disaster prevention and mitigation capacity should be strengthened.

References:: [1] Mohammad R K, Hossein A, Hemila H. An investigation of near surface wind speed trends in arid and semiarid regions of Iran[J]. Theoretical and Applied Climatology, 2013,114(1/2):153-168.
[2] Mcvicar T R, Roderick M L, Donhue R J, et al. Global review and synthesis of trends in observed terrestrial near-surface wind speeds: Implications for evaporation[J]. Journal of Hydrology, 2012,416(3):182-205.
[3] Donohue R J, Mcvicar T R, Roderick M L. Assessing the ability of potential evaporation formulations to capture the dynamics in evaporative demand within a changing climate[J]. Journal of Hydrology(Amsterdam),2010,386(1/4):186-197.
[4] Lynch A H, Curry J A, Brunner R D, et al. Toward an integrated assessment of the impacts of extreme wind events on Barrow, Alaska[J]. Bulletin of the American Meteorological Society, 2004,85(2):209-222.
[5] Turner J, Steve R C, Gareth J M, et al. Antarctic climate change during the last 50 years[J]. International Journal of Climatology, 2005,25(3):279-294.
[6] 丁一汇,李霄,李巧萍.气候变暖背景下中国地面风速变化研究进展[J].应用气象学报,2020,31(1):1-12.
[7] 金巍,任国玉,曲岩,等.1971—2010年东北三省平均地面风速变化[J].干旱区研究,2012,29(4):648-653.
[8] 张志斌,杨莹,张小平,等.我国西南地区风速变化及其影响因素[J].生态学报,2014,34(2):471-481.
[9] 韩柳,王静璞,王光镇,等.中国北方风蚀区风速变化时空特征分析[J].干旱区地理,2018,41(5):65-73.
[10] 李悦佳,贺新光,卢希安,等.1960—2015年长江流域风速的时空变化特征[J].热带地理,2018,38(5):660-667.
[11] Zhang Ruhua, Zhang Shiyan, Luo Jiali, et al. Analysis of near-surface wind speed change in China during 1958—2015[J]. Theoretical and Applied Climatology, 2019,137(3/4):2785-2801.
[12] 赵宗慈,罗勇,江滢,等.近50年中国风速减小的可能原因[J].气象科技进展,2016,6(3):106-109.
[13] 杨庆,李明星,祖子清,等.中国区域的地表风速还在减弱吗[J].中国科学:地球科学,2021,51(7):1028-1042.
[14] 马芹,张晓萍,万龙,等.1957—2009年黄土高原地区风速变化趋势[J].自然资源学报,2012,27(12):2123-2134.
[15] 芦佳玉,延军平,王鹏涛,等.全球气候变暖背景下陕甘宁地区风速时空变化特征[J].中国沙漠,2017,37(3):554-561.
[16] 范清成,王飞,穆兴民,等.近50年黄土高原风蚀区风速的区域变化特征分析[J].水土保持通报,2011,31(3):40-43.
[17] 师玮,周俊菊,胡子瑛,等.甘肃省陇东地区近55年风速时空变化特征[J].生态学杂志,2017,36(12):3594-3601.
[18] 魏凤英.现代气候统计诊断与预测技术[M].2版.北京:气象出版社,2007.
[19] IPCC. Climate Change 2013: The Physical Science Basis[M]. New York: Cambridge University Press, 2013.
[20] 何毅,杨太保,陈杰,等.1960—2013年南北疆风速变化特征分析[J].干旱区地理,2015,38(2):249-259.
[21] Xu Xingkui, Levy Jason K, Lin Zhaohui, et al. An investigation of sand-dust storm events and land surface characteristics in China using NOAA NDVI data[J]. Global and Planetary Change, 2006,52(1/4):182-196.
[22] 毛东雷,蔡富艳,杨余辉,等.新疆策勒4个典型下垫面近地层风速脉动特征[J].干旱区研究,2017,34(1):126-135.
[23] 郭永强,王乃江,褚晓升,等.基于Google Earth Engine分析黄土高原植被覆盖变化及原因[J].中国环境科学,2019,39(11):4804-4811.
[24] 宋永永,马蓓蓓,李武斌,等.黄土高原县域城镇化的地域分异与动因机制[J].陕西师范大学学报:自然科学版,2019,47(4):9-21.
[25] 黄晓龙,杨雪,李涛,等.建站至2016年四川气象台站元数据变动特征分析[J].高原山地气象研究,2017,37(4):84-90.
[26] 刘学锋,梁秀慧,任国玉,等.台站观测环境改变对我国近地面风速观测资料序列的影响[J].高原气象,2012,31(6):1645-1652.
[27] 王恰.中国风电产业40年发展成就与展望[J].中国能源,2020,42(9):28-32,9.

Similar References:

Memo

Last Update: 2023-06-10