[1]ZHENG Xiannian,YANG Xinghua,HE Qing,et al.Characteristics of Wind Velocity Fluctuation During the Sand-Storm Weather in Hinterland of Takliakan Desert[J].Research of Soil and Water Conservation,2020,27(01):366-371.
Copy
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
27
Number of periods:
2020 01
Page number:
366-371
Column:
Public date:
2020-02-20
- Title:
-
Characteristics of Wind Velocity Fluctuation During the Sand-Storm Weather in Hinterland of Takliakan Desert
- Author(s):
-
ZHENG Xiannian1,2,3, YANG Xinghua2,3, HE Qing2,3,4, JIN Lili2,3, YANG Fan2,3, Ali·Mamtimin 2,3, ZHOU Chenglong2,3, ZHANG Jiantao2,3
-
(1.Xinjiang Climate Center, Urumqi 830002 China; 2.Institute Desert Meteorology, CMA, Urumqi 830002, China; 3.Meteorological Field Test Base of Taklimakan Desert of China Meteorological Administration, Tazhong, Xinjiang 841000, China; 4.Xinjiang Meteorological Observatory, Urumqi 830002 China)
-
- Keywords:
-
constructed green land; near ground surface; wind velocity fluctuation; fluctuation intensity; Tazhong
- CLC:
-
Q359
- DOI:
-
-
- Abstract:
-
Basing on the observation data of 80 m wind speed in the near-surface layer during two sandstorms in the constructed green land of Taklimakan Desert, the characteristics of wind pulsation in the near-surface layer and its relationship with visibility, PM10 and PM2.5 under sandstorm weather are discussed. It lays the foundation for further research on wind erosion and potential sand blowing in turbulent conditions. The results show that:(1)the pulsation values of wind speeds at different heights are approximately Gaussian distribution with the change of height, and the volatility is consistent in time series; the pulsation frequency is unstable and no obvious periodicity, and there is significant correlation between adjacent heights;(2)the fluctuation intensity is increasing with the increase of wind speed, and increases at first and then decreases with the decrease of the height of the surface; the turbulence is inversely proportional to the height, and the overall increases with the decrease of the height, because the bottom layer is increased by the presence of surface vegetation;(3)the magnitude of ground wind speed in sandstorm process has a direct impact on horizontal visibility, PM10 and PM2.5. Wind speed pulsation changes are inversely related to horizontal visibility, and are proportional to PM10 and PM2.5.