机译:重力波在中层和下热层(MLT)区域破裂引起的大风和风切变的模拟
State Key Laboratory of Space Weather, Center for Space Science and Applied Research, Chinese Academy of Sciences,Beijing 100190, China,College of Mathematics and Information Science, Henan Normal University, Xinxiang 453007, China;
State Key Laboratory of Space Weather, Center for Space Science and Applied Research, Chinese Academy of Sciences,Beijing 100190, China;
High Altitude Observatory, National Center for Atmospheric Research, Boulder, CO 80307, USA;
Atmospheric and Planetary Sciences, Hampton University, Hampton, VA 23668, USA;
State Key Laboratory of Space Weather, Center for Space Science and Applied Research, Chinese Academy of Sciences,Beijing 100190, China;
Meteorology and atmospheric dynamics (mesoscale meteorology; middle atmosphere dynamics; turbulence);
机译:中层和下热层(MLT)区域重力波破裂引起的大风和风切变的模拟
机译:重力波与中层和下层热层中潮汐背景之间非线性相互作用引起的大风和风切变
机译:对热带地区下大气和介质层层较低的热圈(MLT)对热性引起的重力波耦合的案例研究:观察证据
机译:流星雷达估计中层低层热圈中的重力波方差和动量通量:通过对三个热带地区的模拟和观测,对不同方法进行评估
机译:背景风和温度对更年期区域的钻孔,强风切变和同心重力波的影响。
机译:风电场感应重力波的灵敏度和反馈
机译:中间层和低层热(mLT)区重力波破碎引起的大风和风剪的模拟