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981.
982.
983.
大气中对称不稳定机制的动力学分析及暴雨的分析与预报 总被引:1,自引:0,他引:1
用气块法从力学角度对对称不稳定机制及在对称不稳定条件下产生的环流进行分析,更全面地定义了对称不稳定及它的产生机制和中尺度环流形成的过程。对暴雨个例诊断分析表明,有些强降水区在降水前和降水过程中存在着不对称不稳定,说明对称不稳定条件下形成的环流对暴雨有引发和加强作用。在以往研究原基础上,总结出了利用常规观测资料分析对称不是否存在,及其能量大小的方法,用它来预报是否降水及降水的强度,从而提高降水预报准确率。 相似文献
984.
Yeli Yuan Lei Han Fangli Qiao Yongzeng Yang Ming Lu 《Dynamics of Atmospheres and Oceans》2011,51(1-2):55-74
A linearized instability analysis model with five unknowns was proposed to describe disturbance motions under general oceanic background conditions, including large-scale current shear, density stratification, frontal zone, and arbitrary topography. A unified linear theory of wavelike perturbations for surface gravity waves, internal gravity waves and inertial gravity waves was derived for the adiabatic case, and the solution was then found using Fourier integrals. In this theory, we discarded the assumptions widely accepted in the literature concerning derivations of wave motions such as the irrotationality assumption for surface gravity waves, the rigid-lid approximation for internal gravity waves, and the long-wave approximation for inertial gravity waves. Analytical solutions based on this theory indicate that the complex dispersion relationships between frequency and wave-number describing the propagation and development of the three types of wavelike perturbation motions include three components: complex dispersion relationships at the sea surface; vertical invariance of the complex frequency; and expressions of the vertical wave-number (phase). Classical results of both surface waves and internal waves were reproduced from the unified theory under idealized conditions. The unified wave theory can be applied in the dynamical explanation of the generation and propagation properties of internal waves that are visible in the satellite SAR images in the southern part of the China Seas. It can also serve as the theoretical basis for both a numerical internal-wave model and analytical estimation of the ocean fluxes transported by wavelike perturbations. 相似文献
985.
基于广东省1999—2015年闪电定位系统数据,利用数理统计方法得出广东省闪电气候年际变化特征、季节变化特征、月变化特征,利用最小二乘法得到闪电密度气候变化趋势系数和年、季节的气候倾向率。利用Matlab来对广东省1999—2013年的雷暴日进行分析,得出其年际周期变化规律,最后采用EOF方法,借助Arc GIS平台得出广东省闪电密度空间向量场分布图。结果表明:由1999—2015年,广东全省的地闪密度总体趋势是逐渐增加,闪电日数最多的月份集中在6—8月(夏季);雷暴日存在变化具有周期性、规律性,分别有13~16 a,7~11 a、2~6 a 3种不同尺度的周期;闪电密度空间分布特征主要有一致型、局部型、纬向型和经向型4种类型。 相似文献
986.
选取2015—2016年广东深圳地区的强降水过程为研究对象,降水过程按照天气条件划分为西风带型、西南季风型和热带气旋型,利用Parsivel激光雨滴谱仪和雨量筒测得的数据对广东深圳地区降水的微物理特征进行分析,结果表明:在不同降水量级的情况下,激光雨滴谱仪与雨量筒测得的分钟雨量都具有较好的对应关系,表明激光雨滴谱仪能够适应深圳地区多暴雨的环境;热带气旋带来的降水小粒径雨滴密度最大,大粒径雨滴密度最小,整个降水过程较为绵密;西南季风带来的降水小粒径雨滴密度最小,大粒径雨滴密度最大,整个降水显得很急促;西风带型降水的特征则介于前两者之间。 相似文献
987.
Diagnostic Analysis of the Quasi-Balanced Flow of a Mesoscale Vortex During the 12 June 2008 Guangxi Rainstorm 下载免费PDF全文
By using the high-resolution observation data and MM5 model simulation data, the analysis on the 12
June 2008 Guangxi flash-flood rainstorm shows that the associated major mesoscale weather system of this
event is a quasi-stationary mesoscale vortex, which resulted from the interaction between the midlatitude
synoptic-scale waves in the westerly belt and the low-latitude warm-moist flow under the terrain effect. The
genesis, development, and movement of the mesoscale vortex have significant impacts on the intensity and
persistence of the severe precipitation from the Guangxi flash-flood rainstorm. This vortex is characterized
by the coexistence of strong vorticity and divergence with the same order of magnitude. Well organized,
deep, and moist convection was observed for a long period of time, and was produced by the interaction
between the mesoscale vortex and the gravity waves. The latter was generated by the terrain effect and the
ageostrophic effect of high winds in the low-level jet. According to the quasi-balanced dynamical theory,
quasi-balanced flow must have existed in the mesoscale motions with both divergent and rotational winds.
Thus, based on the diagnosis of the quasi-balanced flow, the PV-ωinversion method is employed to analyze
the organized moist convection. The results show that 50%-70% of the vertical circulation in the rainstorm
areas was quasi-balanced, so the quasi-balanced flow could well reflect features of the strong vertical motions
associated with the coexistence of vorticity and divergence during this event. 相似文献
988.
QUASI-RESONANCE OF BAROCLINIC ATMOSPHERIC WAVES AND EXTRATROPICAL LOW-FREQUENCY OSCILLATION* 下载免费PDF全文
Lu Weisong 《Acta Meteorologica Sinica》1993,7(4):442-453
In operating the quasi-geostrophic two-layer model,the quasi-resonance occurs possibly in two cases:(1)pure barotropic waves;(2) two baroclinic and one barotropic waves.For case (2),we find the analytical solution of triad amplitude of quasi-resonance and approximate expression for the period of wave energy variation.Both the approximate expression and numerical calculation indicate that this period tends to approach the period (2πε)/(△ω) of the quasi-resonance frequency mismatch △ω itself for the baroclinic atmosphere than for the barotropic atmosphere.Physically,there is a feedback mechanism between the wave phase and amplitude,and the slowly varying phase difference between the barotropic wave and the baroclinic wave causes the conversion of kinetic energy and available potential energy,which gives rise to the wave-related low-frequency oscillation alternatively strengthening and weakening with the oscillation period identical to the above approximate formula.For △ω~(0.1-0.02) 0(ωj),the averaged energy period is 12-43 days and when △ω=0,it is 366 days.Therefore,the occurrence of frequency mismatch △ω is probably a new important mechanism for the formation of extratropical low-frequency oscillation in baroclinic atmosphere as well. 相似文献
989.
990.
Deng Hanqing Liu Chun Lu Yanyu He Dongyan Tian Hong 《Theoretical and Applied Climatology》2018,133(1-2):307-318
Theoretical and Applied Climatology - As global warming intensifies, more record-breaking (RB) temperature events are reported in many places around the world where temperatures are higher than... 相似文献