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Wind-sand flow response law of concave surface upwind plane curve embankment under different wind directions
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作者 LI Liangying JI Shuai +2 位作者 XIN Guowei WANG Xu LI Qi 《Journal of Mountain Science》 2025年第12期4379-4391,共13页
Understanding the characteristics of windsand flow field in the curve section of desert highway under different wind directions is helpful for reducing the wind-sand damage in the curve section.Therefore,taking the de... Understanding the characteristics of windsand flow field in the curve section of desert highway under different wind directions is helpful for reducing the wind-sand damage in the curve section.Therefore,taking the desert section of Wuma Expressway in Zhongwei city,Ningxia,China as the research background,the wind-sand flow field and sand accumulation phenomenon of concave surface plane curve embankment under different wind directions is calculated and analyzed by computational fluid dynamics(CFD)numerical simulation method.The results show that:(1)Under different wind directions,along the direction of the route,at the starting point of the route,the windward slope of the embankment is a circular arc section,which reduces the resistance of wind-sand flow and promotes the acceleration of sand particles.In the middle of the route,the low-speed area of the windward slope toe and the leeward slope toe is small;at the end of the route,the high-speed area on the shoulder side of the leeward road rises upward.(2)Under different wind directions,the smaller the angle between the wind direction and the route,the stronger the lateral transport effect on the wind-blown sand flow,and the more sand particles transported along the route direction.(3)Under different wind directions,in the concave windward horizontal curve,with the increase of the angle,the sand area on the top of the embankment shows an increasing trend.Whenα=30°,45°,60°,75°,the percentage of the sand area on the top of the embankment to the total embankment area is 0%,33.3%,64.4%,71.0%,respectively.(4)Under different wind directions,along the route direction,the sand transport efficiency of the concave surface upwind plane curve embankment shows a decreasing trend.In the case of a certain radius of the horizontal curve,the angle range between the wind direction and the concave horizontal curve route is recommended to be 30°-45°. 展开更多
关键词 Desert highway wind-sand flow Flat curve Numerical simulation different wind directions
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Evolution of Surface Sensible Heat over the Tibetan Plateau Under the Recent Global Warming Hiatus 被引量:10
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作者 Lihua ZHU Gang HUANG +3 位作者 Guangzhou FAN Xia QU Guijie ZHAO Wei HUA 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2017年第10期1249-1262,共14页
Based on regular surface meteorological observations and NCEP/DOE reanalysis data, this study investigates the evolution of surface sensible heat(SH) over the central and eastern Tibetan Plateau(CE-TP) under the r... Based on regular surface meteorological observations and NCEP/DOE reanalysis data, this study investigates the evolution of surface sensible heat(SH) over the central and eastern Tibetan Plateau(CE-TP) under the recent global warming hiatus. The results reveal that the SH over the CE-TP presents a recovery since the slowdown of the global warming. The restored surface wind speed together with increased difference in ground-air temperature contribute to the recovery in SH.During the global warming hiatus, the persistent weakening wind speed is alleviated due to the variation of the meridional temperature gradient. Meanwhile, the ground surface temperature and the difference in ground-air temperature show a significant increasing trend in that period caused by the increased total cloud amount, especially at night. At nighttime, the increased total cloud cover reduces the surface effective radiation via a strengthening of atmospheric counter radiation and subsequently brings about a clear upward trend in ground surface temperature and the difference in ground-air temperature.Cloud–radiation feedback plays a significant role in the evolution of the surface temperature and even SH during the global warming hiatus. Consequently, besides the surface wind speed, the difference in ground-air temperature becomes another significant factor for the variation in SH since the slowdown of global warming, particularly at night. 展开更多
关键词 surface sensible heat Tibetan Plateau ground-air temperature difference surface wind speed global warming hiatus
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PiVLA:Vision-Language-Action Based on Parallel Intelligence
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作者 Fei Lin Tengchao Zhang +3 位作者 Jun Huang Qinghua Ni Jingwei Ge Yonglin Tian 《The International Journal of Intelligent Control and Systems》 2025年第3期253-259,共7页
The vision-language-action(VLA)paradigm is gradually becoming the core path of embodied intelligence.However,its training and validation,which rely on simulation environments,face serious sim2real challenges,such as n... The vision-language-action(VLA)paradigm is gradually becoming the core path of embodied intelligence.However,its training and validation,which rely on simulation environments,face serious sim2real challenges,such as navigation deviations in drones caused by wind speed differences between simulation and real-world environments.Existing iterative methods based on digital twins can alleviate the problem of virtual-real alignment to some extent.However,their high dependence on twin consistency limits their adaptability and scalability in complex environments.To break through this bottleneck,the PiVLA framework is proposed in this letter to reconstruct the VLA paradigm with parallel intelligence.Furthermore,we introduce the parallel deep foundation model(PDFM)and,based on it,propose model parallel control(MPC)and the parallel interaction protocol(PIP),establishing a unified interaction mechanism for disembodied agents and embodied agents.This provides a scalable and robust solution for complex tasks involving embodied intelligence. 展开更多
关键词 iterative methods simulation environmentsface parallel intelligence navigation deviations wind speed differences twin consistency digital twins embodied intelligencehoweverits
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