Regional Disparity and Change of Wind Velocities in Wind Erosion Area of Loess Plateau During Last 50 Years
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Regional Disparity and Change of Wind Velocities in Wind Erosion Area of Loess Plateau During Last 50 Years
Bulletin of Soiland Water ConservationVol. 30, Issue 3, Pages: 40-43(2011)
作者机构:
1. 中国科学院 水利部水土保持研究所,陕西 杨凌,712100
2. 中国科学院 研究生院,北京,100049
3. 西北农林科技大学水土保持研究所,陕西 杨凌 7121003.
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Published:2011
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FAN Qing-cheng, WANG Fei, MU Xing-min, et al. Regional Disparity and Change of Wind Velocities in Wind Erosion Area of Loess Plateau During Last 50 Years[J]. Bulletin of Soiland Water Conservation, 2011, 30(3): 40-43.
DOI:
FAN Qing-cheng, WANG Fei, MU Xing-min, et al. Regional Disparity and Change of Wind Velocities in Wind Erosion Area of Loess Plateau During Last 50 Years[J]. Bulletin of Soiland Water Conservation, 2011, 30(3): 40-43.DOI:
Regional Disparity and Change of Wind Velocities in Wind Erosion Area of Loess Plateau During Last 50 Years
Wind is one of the main driving forces of soil wind erosion
effecting surface heat balance and water circulation. Based on wind speed data collected at 12 stations in wind erosion area of Loess Plateau during 1957-2009
accumulation deviation from average and Mann) Kendall test were used to analyze the characteristics of average wind velocity
maximum wind speed and days of air-suspended sands(DTS
wind velocity>6 m/s). T he results show that Guyuan and Yanchi Counties had the highest averages wind speed and Hequ County has the lowest. Counties of Guyuan
Henshan
and Suide had the most days of air-suspended sand. The annual average speeds at three stations
i.e.
Jingyuan County of Gansu Province
Yinchuan City of Ningxia Hui Autonoumous Region and Suide County of Shaanxi Province exhibited a linear increasing trend during the period
but showed decreasing trend at other stations. The annual maximum wind speeds of the study area decreased in the whole period. The annual maximum wind speeds were mostly found in April or May
when soil wind erosion occurred easily because of the tillage and low vegetation coverage at the early spring. T he most DT Ss were found in May and more DT Ss were recorded at Guyuan
Hengshan and Suide Counties are more than at the other areas.
Precise measurement and caculation of carbon sink on check dams in Loess Plateau——A case study at Gaoxigou small watershed, Yulin City, Shaanxi Province
Mechanism of sand-layer sliding induced by water content changes on sand covered loess slopes
Dynamics and driving factors of soil organic carbon sequestration during vegetation restoration on Loess Plateau
Change of climate comfortability and relationship with vegetation cover on Loess Plateau
A Discussion on Trees and Forest Suitability to Sites on the Loess Plateau
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Related Institution
College of Soil and Water Conservation Science and Engineering, Northwest A&F University, Yangling
College of Forestry, Northwest A&F University, Yangling
Nanjing University of Information Science & Technology, School of Hydrology and Water;Resources
Key Laboratory of Hydrometeorological Disaster;Mechanism and Early Warning of Ministry of Water Resources
Department of Biological and Food Engineering, Lyuliang University, Lüliang