[1]付建新,曹广超*,郭文炯.祁连山区风速和风向时空变化特征[J].山地学报,2020,(4):495-506.[doi:10.16089/j.cnki.1008-2786.000528]
　FU Jianxin,CAO Guangchao*,GUO Wenjiong.Temporal and Spatial Variation Characteristics of Average Wind Speed and Direction in the Qilian Mountains, China[J].Mountain Research,2020,(4):495-506.[doi:10.16089/j.cnki.1008-2786.000528]
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祁连山区风速和风向时空变化特征()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2020年第4期
页码:
495-506
栏目:
山地环境
出版日期:
2020-09-27

文章信息/Info

Title:
Temporal and Spatial Variation Characteristics of Average Wind Speed and Direction in the Qilian Mountains, China
文章编号:
1008-2786-(2020)4-495-12
作者:
付建新1; 曹广超2; 3*; 郭文炯1
1.太原师范学院 城镇与区域发展研究所,山西 晋中 030619; 2.青海师范大学 青海省自然地理与环境过程重点实验室,西宁 810008; 3.青藏高原地表过程与生态保育教育部重点实验室,西宁 810008
Author(s):
FU Jianxin1; CAO Guangchao2; 3*; GUO Wenjiong1
1. Institute of Urban and Regional Development, Taiyuan Normal University, Jinzhong 030619, Shanxi, China; 2. Key Laboratory of Qinghai Province Physical Geography and Environmental Process, Qinghai Normal University,Xining 810008,China; 3. Ministry of Education Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation, Xining 810008, China
关键词:
平均风速;  最大风速的风向;  时空变化;  祁连山区
Keywords:
mean wind speed;  maximum wind speed and direction;  temporal and spatial changes;  the Qilian Mountains
分类号:
P942
DOI:
10.16089/j.cnki.1008-2786.000528
文献标志码:
A
摘要:
摘 要:分析山地的风速和风向,对认识山地地区的气候变化和合理利用风力资源具有重要的意义。本文基于祁连山区11个气象站点的平均风速、最大风速和最大风速的风向数据,利用多种数学方法和ArcGIS空间分析法对风速和风向的时空变化分布规律作了探讨。结果表明:(1)祁连山区春季的平均风速和最大风速是年内风速变化的峰值区,其中中段和东段的最大风速出现在冬季。(2)全区的平均风速和最大风速年变化整体均呈下降趋势,下降率分别为-0.07和-1.56 m·s-1·(10a)-1。(3)1970—1979年风力资源最丰富; 年际和季节(冬季除外)平均风速的突变均发生在1993年,东段和中段的平均风速均在1990—1999年发生突变,全区和各个区段平均风速的周期均为22a。(4)祁连山区平均风速自西向东呈递减趋势。(5)最大风速的风向以西南风为主,而东段则以偏东南风为主。
Abstract:
Research on wind speed and direction in mountainous areas play an important role in understanding climate change and utilizing wind resources rationally. Based on the records of average wind speed, maximum wind speed and direction collected at 11 meteorological stations in the Qilian Mountains, spatial and temporal distribution of wind speed and direction was analyzed by using multiple mathematical and ArcGIS spatial analysis methods. Main conclusions were as follows. First, average and maximum wind speed in spring were the highest in a year, and the wind speed in the middle and east segments reached maximum in winter. Second, inter-annual variability of average and maximum wind speed presented a downward trend with a variation rate of -0.07 and -1.56 m·s-1·(10a)-1. Third, wind resources were the most abundant from 1970 to 1979; The annual and seasonal(excepted winter)average wind speed changed abruptly in 1993, abrupt changes in the average wind speed was most pronounced in the eastern and middle sections from 1990 to 1999; The circle of the average wind speed was 22a in the entire study area and its sections. forth, average wind speed showed a decreasing trend from west to east in the research area. Lastly, wind direction of maximum wind speed was dominated by southwest wind and it was dominated by southeast wind at the eastern segment.

参考文献/References:

[1] 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.[DING Yihui, LI Xiao, LI Qiaoping. Advances of surface wind speed changes over China under global warming[J]. Journal of Applied Meteorological Science, 2020, 31(1): 1-12]
[2] 郭小娇,龚晓萍,石建省,等.典型岩溶区潜在蒸散发变化及其影响因素[J].地质学报,2019,93(12):3269-3281.[GUO Xiaojiao, GONG Xiaoping, DAN Jiansheng, et al. The temporal variations of potential evapotranspiration and influence factors for a typical karst area[J]. Acta Geologica Sinica, 2019, 93(12): 3269-3281]
[3] 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.[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]
[4] 道然·加帕依,车罡.新疆东部地区风速的年代际变化及其成因[J].干旱气象,2008,26(3):14-21.[DAORAN Japayi, CHE Gang. Inter-decadal variation characteristics of wind speed in East Xinjiang[J]. Arid Meteorology, 2008, 26(3): 14-21]
[5] PRYOR S C, BARTHELMIE R J, RILEY E S. Historical evolution of wind climates in the USA[J]. Journal of Physics. Conference Series, 2007, 75:12065-12073.
[6] 牟初夫,王礼茂,屈秋实,等.主要新能源发电替代减排的研究综述[J].资源科学,2017,39(12):2323-2334.[MOU Chufu, WANG Limao, QU Qiushi, et al. Review of emission reduction research on major new energy Generation[J]. Resources Science, 2017, 39(12): 2323-2334]
[7] 郑崇伟.21世纪海上丝绸之路:风能资源详查[J].哈尔滨工程大学学报,2018,39(1):16-22.[ZHENG Chongwei. Wind energy evaluation of the 21 st Century Maritime Silk Road[J]. Journal of Harbin Engineering University, 2018, 39(1): 16-22]
[8] 石岚,徐丽娜,郝玉珠.基于风速高相关分区的风电场风速预报订正[J].应用气象学报,2016,27(4):506-512.[DAN Lan, XU Li'na, HAO Yuzhu. The correction of forecast wind speed in a wind farm based on partitioning of the high correlation of wind speed[J]. Journal of Applied Meteorological Science, 2016, 27(4): 506-512]
[9] 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.[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]
[10] 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.[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]
[11] 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.[LI Yuejia, HE Xinguang, LU Xi'an, et al. Spatio-temporal variability of wind speed in the Yangtze River Basin during 1960-2015[J]. Tropical Geography, 2018, 38(5): 660-667]
[12] 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):963-971.[HAN Liu, WANG Jingpu, WANG Guangzhen, et al. Spatial and temporal characteristics of average wind speed in the wind erosion region of northern China[J]. Arid Land Geography, 2018, 41(5): 963-971]
[13] 郭小芹,丁文魁,钱莉,等.祁连山东北缘最大风速气候特征[J].干旱区地理,2015,38(3):446-453.[GUO Xiaoqin, DING Wenkui, QIAN Li, et al. Climate characteristics of the maximum wind speed in northeastern margin of Qilian Mountains[J]. Arid Land Geography, 2015, 38(3): 446-453]
[14] 杜文涛,秦翔,孙维君,等.祁连山老虎沟冰川积累区风速、风向变化特征研究[J].冰川冻土,2012,34(1):29-36.[DU Wentao, QIN Xiang, SUN Weijun, et al. Wind characteristics in accumulation area of the Laohugou glacier No.12, Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2012, 34(1): 29-36]
[15] 罗永忠,郭小芹,刘绪珍.1961年气候变化对祁连山草地生产力影响评价[J].山地学报,2017,35(4):437-443.[LUO Yongzhong, GUO Xiaoqin, LIU Xuzhen. Impact of climate change on grassland productivity of Qilian mountains in 1961-2013[J]. Mountain Research, 2017, 35(4): 437-443]
[16] 周万福,肖宏斌,孙安平,等.祁连地形云与垂直风的关系[J].山地学报,2012,30(6):641-647.[ZHOU Wanfu, XIAO Hongbin, SUN Anping, et al. The relation between orographic cloud and vertical wind in Qilian[J]. Mountain Research, 2012, 30(6): 641-647]
[17] 王海军,张勃,靳晓华,等.基于GIS的祁连山区气温和降水的时空变化分析[J].中国沙漠,2009,29(6):1196-1202.[WANG Haijun, ZHANG Bo, JIN Xiaohua, et al. Spatio-temporal variations analysis of air temperature and precipitation in Qilian Mountainous region based on GIS[J]. Journal of Desert Research, 2009, 29(6): 1196-1202]
[18] 付建新,曹广超,李玲琴,等.1960—2014年祁连山中东段及其附近地区气温时空变化特征[J].干旱区研究,2018,35(3):549-561.[FU Jianxin, CAO Guangchao, LI Lingqin, et al. Spatiotemporal variation of air temperature in the middle and eastern parts of the Qilian Mountains and the nearby regions during the period of 1960-2014[J]. Arid Zone Research, 2018, 35(3): 549-561]
[19] 戴声佩,张勃,王海军,等.1999—2007年祁连山区植被指数时空变化[J].干旱区研究,2010,27(4):585-591.[DAI Shengpei, ZHANG Bo, WANG Haijun, et al. Spatiotemporal variation of vegetation NDVI in the Qilian Mountains during the period from 1999 to 2007[J]. Arid Zone Research, 2010, 27(4): 585-591]
[20] 武正丽,贾文雄,刘亚荣,等.近10 a来祁连山植被覆盖变化研究[J].干旱区研究,2014,31(1):80-87.[WU Zhengli, JIA Wenxiong, LIU Yarong, et al. Change of vegetation coverage in the Qilian mountains in recent 10 years[J]. Arid Zone Research, 2014, 31(1): 80-87]
[21] 贾文雄,何元庆,李宗省,等.祁连山区气候变化的区域差异特征及突变分析[J].地理学报,2008,63(3):257-269.[JIA Wenxiong, HE Yuanqing, LI Zongsheng, et al. The regional difference and catastrophe of climatic change in Qilian Mt. Region[J]. Acta Geographica Sinica, 2008, 63(3): 257-269]
[22] 付建新,曹广超,李玲琴,等.1960—2014年祁连山日照时数时空变化特征[J].山地学报,2018,36(5):709-721.[FU Jianxin, CAO Guangchao, LI Lingqin, et al. Temporal and spatial variation characteristics of sunlight hours in the Qilian mountain, China from 1960 to 2014[J]. Mountain Research, 2018, 36(5): 709-721]
[23] 张忠孝.青海地理[M].西宁:青海人民出版社,2004:13-19.[ZHANG Zhongxiao. Geography in Qinghai[M]. Xining: Qinghai People's Publishing House, 2004: 13-19]
[24] 符淙斌,王强.气候突变的定义和检测方法[J].大气科学,1992,16(4):482-493.[FU Congbin, WANG Qiang. The definition and detection of the abrupt climatic change[J]. scientia Atmospherica Sinica, 1992, 16(4): 482-493]
[25] 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,2007:69-72.[WEI Fengying. Modern climatic statistical diagnosis and forecasting technology[M]. 2nd ed. Beijing: China Meteorological, 2007:69-72]
[26] 魏凤英,朱福康,谢宇.在“98.7”武汉强暴雨过程中不同尺度波动的作用及其相干性[J].高原气象,2005,24(1):49-55.[WEI Fengying, ZHU Fukang, XIE Yu. The effect of multi-scale waves in torrential rain process in Wuhan in July 1998 and its coherence[J]. Plateau Meteorology, 2005, 24(1): 49-55]
[27] 黄小燕,张明军,王圣杰,等.西北地区近50年日照时数和风速变化特征[J].自然资源学报,2011,26(5):825-835.[HUANG Xiaoyan, ZHANG Mingjun, WANG Shengjie, et al. Characteristics of variation in sunshine duration and wind speed in the last 50 years in northwest China[J]. Journal of Natural Resources, 2011, 26(5): 825-835]
[28] 徐丽娇,胡泽勇,赵亚楠,等.1961—2010年青藏高原气候变化特征分析[J].高原气象,2019,38(5):911-919.[XU Lijiao, HU Zeyong, ZHAO Ya'nan, et al. Climate change characteristics in Qinghai-Tibetan plateau during 1961-2010[J]. Plateau Meteorology, 2019, 38(5): 911-919]
[29] 何旭强,张勃,赵一飞,等.黑河流域1960—2009年平均风速时空变化特征[J].水土保持通报,2013,33(4):242-247.[HE Xuqiang, ZHANG Bo, ZHAO Yifei, et al. Temporal and spatial characteristics of average wind speed changes in Heihe river basin from 1960 to 2009[J]. Bulletin of Soil and Water Conservation, 2013, 33(4): 242-247]
[30] 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.[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]
[31] 熊敏诠.近30年中国地面风速分区及气候特征[J].高原气象,2015,34(1):39-49.[XIONG Minquan. Climate regionalization and characteristics of surface winds over China in recent 30 years[J]. Plateau Meteorology, 2015, 34(1): 39-49]

备注/Memo

备注/Memo:
收稿日期(Received date):2018-09-23; 改回日期(Accepted date): 2020-05-11
基金项目(Foundation item):国家重点研发计划项目(2017YFC0404304); 青海省科学技术厅自然基金项目(2018-ZJ-903); 祁连山国家公园青海研究中心开放项目(GKQ2019-01)。 [National Key Research and Development Program of China(2017YFC0404304); Natural Science Foundation of Qinghai Province of China(2018-ZJ-903); Open Project of Qilian Mountain National Park Research Center(Qinghai)(GKQ2019-01)]
作者简介(Biography):付建新(1980-),男,山西大同人,讲师,博士,主要研究方向:土地利用与区域发展。[FU Jianxin(1980-), male, born in Datong, Shanxi province, lecturer, Ph.D., research on land use and regional development]E-mail: fujx@163.com
*通讯作者(Corresponding author):曹广超(1971-),男,山东苍山人,教授,主要研究方向:青藏高原地区环境变化与地理信息系统应用。[Cao Guangchao(1971-), male, born in Cangshan, Shandong province, professor, Ph.D. supervisor, research on environmental change and application of geographic information system in the Tibet Plateau] E-mail: caoguangchao@126.com
更新日期/Last Update: 2020-07-30