Disaster damage index and disaster grades are constructed by using multi index method on the basis of overall consideration, based on the disaster data of 671 wind disasters taking place in 38 counties (cities) in Northern Xinjiang from 1980 to 2019, and by selecting six disaster factors including the death toll, the number of collapsed houses, the number of collapsed sheds, the number of damaged green houses, the number of livestock deaths and the affected area caused by each wind disaster event. The results show that in space, wind disasters are the most frequent in Bortala Mongol Autonomous Prefecture and Altay Prefecture, and the losses caused by wind disasters are the most severe along Tianshan Mountain in Northern Xinjiang and Altay Prefecture. In terms of time, wind disasters in Northern Xinjiang are mainly concentrated in spring and summer (from March to August), of which April and May are the months with the highest frequency. In recent 40 years, the occurrence times and extent of harm of wind disasters in Northern Xinjiang have shown a linear growth trend; the occurrence times of wind disasters at various grades and the extent of harm have increased significantly during the years around 2000; it is found, upon examination, there was a sudden change of climate in the late 1990s, and the increase rate is inversely proportional to the grade of wind disaster. Therefore, the wind disasters in Bortala Mongol Autonomous Prefecture, Altay Prefecture and the area along Tianshan Mountain in Northern Xinjiang from April to May each year are the areas in Northern Xinjiang with the highest wind disaster risk. The study can provide scientific basis for wind disaster prevention and control in Northern Xinjiang.
Published in | Earth Sciences (Volume 13, Issue 1) |
DOI | 10.11648/j.earth.20241301.14 |
Page(s) | 39-48 |
Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
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Copyright © The Author(s), 2024. Published by Science Publishing Group |
Wind Disasters, Disaster Damage Index, Grades, Temporal and Spatial Distribution, Northern Xinjiang
[1] | XU Hailiang, CHEN Yaning. (2003) Hazard assessment of wind sand disaster in Tarim Basin [J]. Journal of Natural Disasters, 12(2): 35-39. |
[2] | AI Xiaoqiu, PENG Yongbo, CHENG Yingyao. (2018) Wind induced failure and dynamical behaviors of urban trees [J]. Journal of Natural Disasters, 27(1): 27-32. |
[3] | LI Zhengnong, HAO Yanfeng. (2020) Research review about wind effects on crops [J]. Journal of Natural Disasters, 12(2): 54-62. |
[4] | WANG Bing, ZHENG Jing, WANG Zhichun, et al.. (2019) Study on the grade criterion and risking zoning of rubber wind disasters in Guangdong [J]. Journal of Natural Disasters, 28(5): 189-197. |
[5] | WANG Yanhong, HE Weiming, YU Feihai, et al.. (2010) Advances in the responses of plants to wind-induced mechanical stimulation [J]. Acta Ecologica Sinica, 30(3): 794-800. |
[6] | YU Yunjiang, SHI Peijun, HE Liping, et al.. (2002) Research on the effects of wind-sand current on the plant growth [J]. Advance in Earth Sciences, 17(2): 262-267. |
[7] | Telewski F W, Jaffe M J. (1986) Thigmomophogenesis: Field and laboratory studies of Abiesfraseri in response to wind or mechanical perturbation [J]. Physiologia Plantarum, 66(2): 211-218. |
[8] | Li Maochun, Hu Yunxi. (2005) The effect of the sand blown by the wind to the emergence of cotton in Alar reclamation area [J]. Xinjiang Meteorology, 28(6): 23-24. |
[9] | LIU Jing, MA Liwen, ZHANG Xiaoyu, et al.. (2003) Study on monitoring indexes of wheat hot and dry wind in Ningxia Yellow River Irrigation Area [J]. Chinese Journal of Agrometeorology, 24(6): 11-14. |
[10] | LIU Xuemin. (2016) The resistance analysis of low-rise buildings in strong wind[D]. Dalian: Dalian University of Technology. |
[11] | GAO Yang. (2017) Wind tunnel test research on extreme wind pressure characteristic on local roof of low-rise buildings [D]. Xiangtan: Hunan University of Science and Technology. |
[12] | YIN Lidan, MA Ning. (2019) Analysis of seismic and wind-resistant performance of viscous-elastic buckling-restrained braced frame [J]. Journal of Natural Disasters, 28(1): 16-23. |
[13] | WANG Qiuxiang, LI Hongjun. (2003) Analysis on gale disasters of Xinjiang in recent 20 year s[J]. Journal of Desert Research, 23(5): 545-548. |
[14] | WU Meihua, WANG Huaijun. (2016) Formation and risk analysis of meteorological disasters in Xinjiang [J]. Arid Land Geography, 39(11): 1212-1220. |
[15] | ZHU Gang, GAO Huijun, ZENG Guang. (2015) Lake change research and reasons analysis in Xinjiang arid regions during the past 35 years [J]. Arid Land Geography, 38(1): 103-110. |
[16] | HU Ruji, FAN Zili, WANG Yajun, et a1.. (2001) Assessment about the impact of climate change on environment in Xinjiang since recent 50 years [J]. Arid Land Geography, 24(2): 97-103. |
[17] | Mansur Sabit, NasimaNasirdin, et a1.. (2012) The spatio-temporal changes and intensity of gale disasters in Southern Xinjiang recent 60 years [J]. Geographical Reseach, 31(5): 803-810. |
[18] | Mansur•Shabit, Lutubula•Yiming. (2012) The characteristics of gale disaster and its impact on agricultural production in Southern Xinjiang in last 60 years [J]. Agricultural Research in the Arid Areas, 30(1): 265-269. |
[19] | HE Yi, YANG Taibao, CHEN Jie, et a1.. (2015) Wind speed change in north and south Xinjiang from 1960 to 2013 [J]. Arid Land Geography, 38(3): 249-259. |
[20] | WANG Yuzhu, YAN Haowen, WANG Xiaoping, et a1.. (2020) Spatio-temporal analysis of gale concentration in Xinjiang [J]. Arid Land Geography, 43(3): 623-632. |
[21] | CAO Xing, WAN Yu, LU Hui, et a1.. (2015) Gale and its change in Dabancheng, Xinjiang in recent 30 Years [J]. Arid Zone Research, 32(1): 116-122. |
[22] | CHEN Hongwu, XIN Yu, CHEN Pengxiang, et a1.. (2010) Variation tendency of the extreme value of wind speeds and gale frequency over the windy regions in Xinjiang [J]. Climatic and Environmental Research, 15(4): 479-490. |
[23] | TAN Zhiqiang, SANG Jianren, JI Xiaoling, et a1.. (2017) Mechanism of a strong wind and blowing sand process in Ningxia [J]. Arid Land Geography, 40(6): 1134-1142. |
[24] | DONG Jiarui, LI Haining, LIU Hao. (2020) Analysis on the weather process of gale disaster in Naiman Banner [J]. Modern Agricultural Science and Technology, 16: 150-151. |
[25] | LIU Lina, SHI Qingdong, ZHANG Fei. (2007) The variation tendency of accumulated temperature in the past 41 years in the north area of Xinjiang [J]. Journal of Arid Land Resources and Environment, 21(10): 52-56. |
[26] | Statistics Bureau of Xinjiang Uygur Autonomous Region. (2019) Xinjiang statistical yearbook [M]. China Statistics Press. |
[27] | ZHANG Jiabao, LI Decai, MENG Qihui, et al.. (1986) Xinjiang short term forecast Guide Manual [M]. Volksverlag Xinjiang, 271-272. |
[28] | WANG Xu, CHU Changjiang, MOU Huan. (2020) Spatial pattern and interannual variation characteristics of snow disaster in Xinjiang [J]. Arid Zone Reseatch, 36(6): 1488-1495. |
[29] | CHEN Jiading, LIU Wanru, WANG Renguan. (1982) Lecture notes on probability and statistics [M]. Beijing: Higher Education Press. |
[30] | SHI Neng, ZHU qiangen. An abrupt change in the intensity of the East Asian summer monsoon index and its relationship with temperature and precipitation over East China [J]. International Journal of Climatology, 1996, 16(1): 1-8. |
[31] | LU Xiaorong, ZHOU Qi, WANG Yao. (2015) Temporal and spatial distribution characteristics of late spring cold weather in Manas County and its preventive measures [J]. Modern Agricultural Science and Technology, 9: 257-258. |
[32] | GAO Jing. (2010) Research on the temporal and spatial distribution characteristics of strong wind and circulation feature weather in Xingjiang [D]. Lanzhou: Lanzhou University. |
APA Style
Hu, F., Liu, C., Hu, M., Xie, X., Lv, X. (2024). Research on the Differences of Climatic Characteristics of Different Levels of Gale Disasters in Northern Xinjiang. Earth Sciences, 13(1), 39-48. https://doi.org/10.11648/j.earth.20241301.14
ACS Style
Hu, F.; Liu, C.; Hu, M.; Xie, X.; Lv, X. Research on the Differences of Climatic Characteristics of Different Levels of Gale Disasters in Northern Xinjiang. Earth Sci. 2024, 13(1), 39-48. doi: 10.11648/j.earth.20241301.14
AMA Style
Hu F, Liu C, Hu M, Xie X, Lv X. Research on the Differences of Climatic Characteristics of Different Levels of Gale Disasters in Northern Xinjiang. Earth Sci. 2024;13(1):39-48. doi: 10.11648/j.earth.20241301.14
@article{10.11648/j.earth.20241301.14, author = {Fan Hu and Chenliang Liu and Ming Hu and Xiaofeng Xie and Xinsheng Lv}, title = {Research on the Differences of Climatic Characteristics of Different Levels of Gale Disasters in Northern Xinjiang}, journal = {Earth Sciences}, volume = {13}, number = {1}, pages = {39-48}, doi = {10.11648/j.earth.20241301.14}, url = {https://doi.org/10.11648/j.earth.20241301.14}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20241301.14}, abstract = {Disaster damage index and disaster grades are constructed by using multi index method on the basis of overall consideration, based on the disaster data of 671 wind disasters taking place in 38 counties (cities) in Northern Xinjiang from 1980 to 2019, and by selecting six disaster factors including the death toll, the number of collapsed houses, the number of collapsed sheds, the number of damaged green houses, the number of livestock deaths and the affected area caused by each wind disaster event. The results show that in space, wind disasters are the most frequent in Bortala Mongol Autonomous Prefecture and Altay Prefecture, and the losses caused by wind disasters are the most severe along Tianshan Mountain in Northern Xinjiang and Altay Prefecture. In terms of time, wind disasters in Northern Xinjiang are mainly concentrated in spring and summer (from March to August), of which April and May are the months with the highest frequency. In recent 40 years, the occurrence times and extent of harm of wind disasters in Northern Xinjiang have shown a linear growth trend; the occurrence times of wind disasters at various grades and the extent of harm have increased significantly during the years around 2000; it is found, upon examination, there was a sudden change of climate in the late 1990s, and the increase rate is inversely proportional to the grade of wind disaster. Therefore, the wind disasters in Bortala Mongol Autonomous Prefecture, Altay Prefecture and the area along Tianshan Mountain in Northern Xinjiang from April to May each year are the areas in Northern Xinjiang with the highest wind disaster risk. The study can provide scientific basis for wind disaster prevention and control in Northern Xinjiang. }, year = {2024} }
TY - JOUR T1 - Research on the Differences of Climatic Characteristics of Different Levels of Gale Disasters in Northern Xinjiang AU - Fan Hu AU - Chenliang Liu AU - Ming Hu AU - Xiaofeng Xie AU - Xinsheng Lv Y1 - 2024/02/28 PY - 2024 N1 - https://doi.org/10.11648/j.earth.20241301.14 DO - 10.11648/j.earth.20241301.14 T2 - Earth Sciences JF - Earth Sciences JO - Earth Sciences SP - 39 EP - 48 PB - Science Publishing Group SN - 2328-5982 UR - https://doi.org/10.11648/j.earth.20241301.14 AB - Disaster damage index and disaster grades are constructed by using multi index method on the basis of overall consideration, based on the disaster data of 671 wind disasters taking place in 38 counties (cities) in Northern Xinjiang from 1980 to 2019, and by selecting six disaster factors including the death toll, the number of collapsed houses, the number of collapsed sheds, the number of damaged green houses, the number of livestock deaths and the affected area caused by each wind disaster event. The results show that in space, wind disasters are the most frequent in Bortala Mongol Autonomous Prefecture and Altay Prefecture, and the losses caused by wind disasters are the most severe along Tianshan Mountain in Northern Xinjiang and Altay Prefecture. In terms of time, wind disasters in Northern Xinjiang are mainly concentrated in spring and summer (from March to August), of which April and May are the months with the highest frequency. In recent 40 years, the occurrence times and extent of harm of wind disasters in Northern Xinjiang have shown a linear growth trend; the occurrence times of wind disasters at various grades and the extent of harm have increased significantly during the years around 2000; it is found, upon examination, there was a sudden change of climate in the late 1990s, and the increase rate is inversely proportional to the grade of wind disaster. Therefore, the wind disasters in Bortala Mongol Autonomous Prefecture, Altay Prefecture and the area along Tianshan Mountain in Northern Xinjiang from April to May each year are the areas in Northern Xinjiang with the highest wind disaster risk. The study can provide scientific basis for wind disaster prevention and control in Northern Xinjiang. VL - 13 IS - 1 ER -