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中心强度 meaning in Chinese

core strength

Examples

  1. Light centre length
    发光中心强度
  2. Different parameterization schemes have different influences on the maximum intensity of rainfall and the distribution of rain area . suitable boundary layer parameterization scheme has obvious improvement on simulated results
    不同的边界层参数化方案对雨量中心强度、雨区分布、散度和涡度的预报均有一定的影响。
  3. Using the mm5 model to conduct investigation of numerical simulation for this case , it was basically possessed of a capability to reproduce the genesis , development and evolution of the large - scale and mesoscale weather systems
    本文以mm5模式模拟分析“雅安天漏”为代表,着重研究了不同边界层参数化方案对雨量中心强度、雨区分布的影响以及雅安暴雨时的纬向垂直环流结构。
  4. Whether in the aspect of total rain days or total rainfall amount in a year , ya ' an is always an extreme range , which has been called " ya - an - tian - lou " in chinese . the predicted average physical structures in the raining process are as follows : ( l ) positive vortex and convergent center in the lower and middle troposphere and negative vortex and divergent center in upper troposphere ; ( 2 ) the superposition of the low layer zonal - vertical circulation and the up layer zonal - vertical circulation forms a strong upward current
    从6种不同方案对暴雨过程预报的实验看,不同的边界层参数化方案对雨带特征的模拟都具有一定的能力,同时模式模拟的降水对参数化方案的选取是敏感的,不同的参数化方案模拟出的降水范围和雨量分布有所差异,主要表现在降雨量中心强度及雨区分布上。
  5. The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high , south asia high , low latitude systems , upper level jet ( ulj ) , low level greater wind speed axes , westerly trough and plateau trough , low level vortex , cold frontal , occluded front in qinghai lake , mesoscale low pressure , heat low - pressure in qinghai , shear line and convergence line , mesoscale cloud cluster , etc . the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area
    3 、西太平洋副高、南亚高压、低纬系统、高空急流、低空大风速轴;西风槽和高原槽、低涡、冷锋、青海湖锢囚锋以及中尺度低压、青海热低压、切变线与辐合线、中尺度云团等系统是高原东北部地区大到暴雨的主要相关系统。 100hpa上的南亚高压中心强度加强,位置东西摆动预示高原地区将有降水产生,中心强度减弱,降水过程结束。南亚高压西部副型是高原东北部地区大到暴雨的主要流型。
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Related Words

  1. 强度
  2. 中心前端
  3. 中心前回
  4. 中心桥
  5. 中心桥跨
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