排序方式: 共有43条查询结果,搜索用时 765 毫秒
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本文建立了一个考虑天气尺度水平变形场的二维、滞弹性、非静力平衡锋生模式,对冷锋过山时的锋生锋消机制进行了数值研究,试验结果表明:当无地形影响时,由于变形场的锋生作用与摩擦等因子的锋消作用相互抵消,冷锋最终达到其强度的准定常状态;当考虑地形影响时,地形强迫环流与锋面环流相互作用,使得锋面强度在山前和山后发生变化,在冷锋开始爬坡时锋生,爬过半山腰后开始锋消,过山顶后锋面强度变化不明显或者有微弱锋生,到达山脚后开始强烈锋生,并在地形下游其强度达到最大;总之,冷锋在翻越山脉或从高原移到平原之后,锋面发展的强度比冷锋不遇到地形时的更大。 相似文献
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Peng WEI Xin XU Ming XUE Chenyue ZHANG Yuan WANG Kun ZHAO Ang ZHOU Shushi ZHANG Kefeng ZHU 《大气科学进展》2023,40(3):337-349
An extremely heavy rainfall event occurred in Zhengzhou, China, on 20 July 2021 and produced an hourly rainfall rate of 201.9 mm, which broke the station record for mainland China. Based on radar observations and a convection-permitting simulation using the WRF-ARW model, this paper investigates the multiscale processes, especially those at the mesoscale,that support the extreme observed hourly rainfall. Results show that the extreme rainfall occurred in an environment characteristic of warm-sec... 相似文献
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Wu Rongsheng 《Acta Meteorologica Sinica》1991,5(1):62-70
It is convenient to use σ-coordinates to discuss the dynamic effect of orography and the flow in Ekman boundary layer.In this paper,the theory of mixing length is generalized to the σ-coordinate system.Then the governing equations,describing the motion in the boundary layer over the mountain regions are derived.The features of flow in the boundary layer,especially the effects of Ekman pumping,are discussed indetails.It is pointed out that there are three factors affecting the vertical motion at the top of the boundary layer:(1) vorticity distribution in the boundary layer,which is directly related to the divergence and convergence of air flow caused by friction,(2) the upslope or downslope motion of flow over the mountain slopes,and(3) the mutual effect of orography and friction induced by the ageostrophic component climbing upward or downward in the boundary layer over mountain regions. 相似文献
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Identification of homogeneous rainfall regimes in parts of Western Ghats region of Karnataka 总被引:1,自引:0,他引:1
In view of the ongoing environmental and ecological changes in the Western Ghats, it is important to understand the environmental
parameters pertaining to the sustenance of the region. Rainfall is one such parameter governing the hydrological processes
crucial to agriculture planning, afforestation and eco-system management. Therefore, it is essential to understand rainfall
distribution and its variation in relevance to such activities. The present study is an attempt to gain in-depth understanding
in this direction. The study area comprises of one coastal district and its adjoining areas in Karnataka State. Mean annual
rainfall data of 93 rain gauge stations distributed over the study area for a period of 10–50 years are used for the study.
In order to assess the variation of rainfall across the ghats, several bands were constructed parallel to the latitudes to
facilitate the analysis. The statistical analyses conducted included cluster analysis and analysis of variance. The study
revealed that there exist three distinct zones of rainfall regimes in the study area, namely, Coastal zone, Transition zone
and Malanad zone. It is observed that, the maximum rainfall occurs on the windward side ahead of the geographical peak. Further,
mean monthly rainfall distribution over the zones has been depicted to enable agricultural planning in the study area. 相似文献
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The influence of meteorology on clouds at Kleiner Feldberg 总被引:1,自引:0,他引:1
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ANALYSES OF THE DYNAMIC EFFECTS ON WINTER CIRCULATION OF THE TWO MAIN MOUNTAINS IN THE NORTHERN HEMISPHERE——Ⅰ.RELATIONSHIP AMONG GENERAL CIRCULATION,TELECONNECTION AND STATIONARY WAVES 下载免费PDF全文
The distribution of troughs and ridges of geopotential height,the teleconnection patterns and the propagation pat-terns of stationary waves are the main features of the January mean geopotential height field at 500hPa.Data analysesand numerical experiments indicate that these three characteristics are associated to one another and closely related tothe mechanical forcing of the Rocky Mountains and Tibetan Plateau.There exists a prominent negative correlation inthe intensity variation between the American trough and the Asian trough at high and middle latitudes.Such negativecorrelation,in connection with the interannual variation of the intensity of the jets in front of the two troughs,leads tothe existence of similar teleconnection patterns in North America and East Asia.On the other hand,the different propa-gation behaviour of quasi-stationary waves downstream of the two main mountains results in a fundamental differencein the distribution of correlation chains in North America and East Asia. 相似文献