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Statistical characteristics of the spatial distribution of wind and snow in the Xinjiang Uygur Autonomous Region

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Abstract

At present, the wind and snow loads are calculated independently when determining the design specifications for building structures. Yet, when snow drifting occurs, the basic wind and snow pressures exist almost simultaneously. Therefore, building specifications based on the independent calculations of the wind and snow loads cannot be used effectively in areas that are severely impacted by snow drifting. Some parts of the Xinjiang Uygur Autonomous Region of China have suffered particularly severe snow drifting natural disasters. In this paper, we offer an analysis of the statistical characteristics of the spatial distribution of wind and snow in this region. In particular, we extract the values of the combined distribution of the wind and snowfall in the Xinjiang Uygur Autonomous Region of China by using parameters such as snowfall intensity, snowfall amount, wind speed, and wind direction as indicators that show the snow drifting disasters. This study found that, after heavy snowfall events, the accumulative wind scale is high and the accumulative snowfall is large in the Altay, the Bortala Mongol Autonomous, and the Tacheng Prefectures of northern Xinjiang, and the Kizilsu Kirghiz Autonomous Prefecture of western Xinjiang. It has an important practical significance for the design of building structures and the treatment of snow drifting disasters.

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Acknowledgements

The research reported herein was sponsored by the National Natural Science Foundation of China (Grant No. 51778381), the Hebei Province Natural Science Fund (Grant No. D2016210008 and Grant No. E2018210044) and the Hebei Province Social Science Fund (Grant No. HB21GL010). We would like to thank TopEdit (www.topeditsci.com) for English language editing of this manuscript.

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Correspondence to Qingkuan Liu or Jianqing Bu.

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Appendices

Appendix A

See Table 4.

Table 4 Appearance frequency of different daily wind scales in the Xinjiang Uygur Autonomous Region during the period of 1st, 2nd, 3rd, 11th, and 12th months from 1968 to 2016

Appendix B

See Table 5.

Table 5 Basic wind speed of each station in the Xinjiang Uygur Autonomous Region at different reoccurrence periods

Appendix C

See Table 6.

Table 6 Occurrence times of different snowfall grades in the Xinjiang Uygur Autonomous Region within 1st, 2nd, 3rd, 11th, and 12th months from 1968 to 2016

Appendix D

See Table 7.

Table 7 The numbers of occurrences of different wind scales for 6 days (including the day of snowfall) after the top ten maximum snowfall days in winter at all stations in the Xinjiang Uygur Autonomous Region

Appendix E

See Table 8.

Table 8 The normalized total snowfall and the normalized accumulated wind scale of all stations in the Xinjiang Uygur Autonomous Region

Appendix F

See Table 9.

Table 9 Accumulative snowfall and accumulative wind scale taken from the top ten maximum snowfall events at each station in the Xinjiang Uygur Autonomous Region

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Yu, X., Liu, M., Wang, J. et al. Statistical characteristics of the spatial distribution of wind and snow in the Xinjiang Uygur Autonomous Region. Nat Hazards 111, 1977–2009 (2022). https://doi.org/10.1007/s11069-021-05127-4

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  • DOI: https://doi.org/10.1007/s11069-021-05127-4

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