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- The overall diabatic heating is positive in the whole troposphere in summer, with the most intense heating located in the boundary layer. 夏季高原地区总非绝热加热是正值,且最大加热率出现在边界层内。
- Results show that vertical diabatic heating plays a dominant role in the variation in intensity and location of WPSH in July 2003. 运用全型垂直涡度倾向方程理论,研究了空间非绝热加热在垂直方向的变化对2003年7月副高强度和位置变异的影响。
- The experiment with only topography can not reproduce the Somali Jet fairlv, it further proves the relative importance of diabatic heating over the topography. 在不考虑非绝热加热作用而只考虑地形的模拟实验中;索马里低空气流不能完整地模拟出来.
- Computations for the linear response of the model atmosphere to the Northern Hemisphere topography and diabatic heating in January 1979 are also presented. 文中给出了模式参数选择、数值求解的详细方案以及该模式大气的扰动流函数场对于北半球大尺度地形和1979年1月平均非绝热加热场的响应的实际计算结果。
- A nonlinear baroclinic system with forcing and dissipationincluded is derived in terms of the high truncated spherical low-orderspectral model with diabatic heating, eddy viscosity and topographiceffect considered. 本文考虑到非绝热加热、涡动粘性及地形效应,在高截断球面低阶谱模式基础上,导出了具有强迫耗散的非线性斜压系统。
- The NCEP/NCAR reanalysis data are employed to analyze the diurnal variation of the diabatic heating and atmospheric circulation over the Tibetan Plateau and it's surrounding areas. 摘要通过使用NCEP/NCAR再分析资料,分析了夏季青藏高原地区非绝热加热场的日变化特征以及高原上空环流场的日变化特点。
- It is shown that to the north of a heating region, although there is no diabatic heating, there still exists deep negative vorticity forcing due to the horizontal inhomogeneous in the westerly flow. 因而高层热源北部边界附近的西风向南偏转进入加热区,造成加热区北部边界及其以北发生次级辐散;
- Abstract: Based upon potential vorticity theory and thermal adaptation principle, the feature of atmospheric motion as a result of spatial inhomogeneous diabatic heating is investigated. 摘 要: 利用位涡方程和热力适应原理,讨论了因非绝热加热的空间不均匀性导致的大气 动力特征的变化,进一步阐明了副热带地区的深对流凝结潜热加热的垂直非均匀性使副热带高压在中低空出现在热源区以东,在高空出现在热源区以西。
- Abstract : The NCEP/NCAR reanalysis data are employed to analyze the diurnal variation of the diabatic heating and atmospheric circulation over the Tibetan Plateau and it's surrounding areas. 摘要 : 通过使用NCEP/NCAR再分析资料,分析了夏季青藏高原地区非绝热加热场的日变化特征以及高原上空环流场的日变化特点。
- THE IMPACT OF BASIC FLOW AND DIABATIC HEATING ON MOTION AND STRUCTURE OF TROPICAL CYCLONE 环境气流及非绝热加热对热带气旋结构和移动的影响
- Heat sometimes causes a prickly rash on the skin. 热有时使皮肤上生剌痛的疹子。
- The Diurnal Variation of the Atmospheric Circulation and Diabatic Heating over the Tibetan Plateau 夏季青藏高原加热和环流场的日变化
- Diabatic Heating over the Tibetan Plateau and the Seasonal Variations of the Asian Circulation and Summer Monsoon Onset 青藏高原加热与亚洲环流季节变化和夏季风爆发
- This is a highly efficient new heating system. 这是个高效的新取暖系统。
- Impact of diabatic heating over the Tibetan Plateau on subsidence over northeast Asian arid region 西藏高原上空非绝热加热对亚洲东北干燥区域上空下沉的影响
- The system works on the principle that heat rises. 该项装置是按照热力上升的原理运转的。
- FEATURES OF 500hPa DIABATIC HEATING OVER THE NORTHERN HEMISPHERE DURING EL NINO AND ANTI-EL NINO YEARS 厄尔尼诺年和反厄尔尼诺年北半球500hPa非绝热热流量场的特征
- The heat had blistered the paint of the building. 酷热使建筑物上的油漆起了浮泡。
- Keywords Rainstorm in Southern China;tropical disturbance;meso-scale moist convection;diabatic heating;topography; 华南暴雨;热带扰动;中尺度湿对流;非绝热加热;地形;
- It is this molecular motion that we call heat. 就是这种分子运动我们称之为热。