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1.
本文通过西太平洋西北部海表温度与北半球500hpa西副高和极涡环流指数的典型相关分析,得到了一些有意义的环流超前与滞后的相关事实,证实了环流有3—6个月的滞后相关的存在。  相似文献   

2.
本文统计了1970~1989年20年西南低涡生成的资料,得到了西南低涡生成的月际和年际分布的其本事实。在此基础上分析了生成低涡的500hPa环流背景和九龙涡生成的地理环境,试图揭示西南涡生成的机理,最后,文章利用非热成风适应原理,对低涡生成机理进行了理论分析。  相似文献   

3.
本文通过对1980年以来长江上游10次洪涝过程的500hpa环流形势分析,并用车比雪夫多项式对500hpa高度场进行展开,研究了各类洪涝过程的中期演变特征,发现代表不同洪涝过程环流形势变化的不同的车氏系数值都有明显的特征变化,结合欧洲中心中期数值预告96小时500hpa高度场的车氏系数分析,可为洪涝暴雨的中期预报提供一种新的思路。  相似文献   

4.
本文利用热成风适应原理,采取分解分析法对青藏高原500hpa暖性高压的生成机制作了一些定性和定量的讨论。结果表明:在扰动的水平尺度大于热成风适应的特征尺度的条件下,当源地有明显的负值非热成风涡度出现时,流场将向温度场适应,而温度场由于高原的加热作用存在暖中心或暖脊,则适应的结果在高原大气500hpa形成暖性高压,并伴随高层辐合,低层辐散及下沉运动。  相似文献   

5.
本文着重分析了青藏高原500hpa高压因伊朗高压脊东伸、分裂产生过程中和东移过程中,西风带波动、印度季风低压以及100hpa层流型的一系列变化,从而说明青藏高原500hpa高压产生和东移的环流背景。  相似文献   

6.
为探讨西北地区东部的持续大暴雨过程成因及预警指标,利用2010年7月22~23日500~700hPa大气环流背景及天气影响系统和西峰新一代多普勒天气雷达回波资料分析,结果得到:500hPa西太平洋副热带高压外围河套地区环境场的演变高压外围低涡发展及维持,是这次持续性大暴雨过程的大气环流背景和影响天气系统,700hPa强盛的水汽场输送场与汇聚作用为这次持续性大暴雨过程提供了充沛的水汽条件,随着500hPa河套地区低涡-切变辐合系统的准静止维持造成这次持续性大暴雨过程;大暴雨前1.5~9.7km垂直方向上,存在明显的东南风场与西南风场的切变,风向随高度顺转,对应持续的暖平流;天气雷达强度回波反射率因子≥40dBz,暴雨期间维持少变;径向速度回波的水平辐合和气旋性涡旋运动与河套低涡切变天气系统对应一致;垂直液态水含量≥35kg.m2的雨团范围大、持续时间长;云顶回波高度维持在8km以上,对监测预警持续大暴雨天气具有一定指示意义。  相似文献   

7.
本文应用车贝雪夫一傅里叶展开方法,分析1981年和1982年梅雨期间以及梅雨期前后的500hpa中高纬度环流特征。分析结果表明:梅雨期是环流形势的转折期,因此超长波的位相和振幅特征各年均有若干相似之处;而在梅雨期中的降水间隙期,长波和超长波的位相、振幅会发生突变,这种突变正反映了季风的相对中断期。  相似文献   

8.
复杂地形对西南低涡生成和移动影响的数值试验分析   总被引:1,自引:0,他引:1  
为探讨四川盆地周边复杂地形对西南低涡发生发展以及移动的影响,利用NCEP 1°×1°再分析资料和中尺度非静力平衡模式WRF V3.4.1,对2010年7月16日至18日发生在四川盆地的一次西南低涡暴雨过程进行了再现模拟(控制试验)以及降低盆地周边不同地形高度的3组敏感性试验。结果表明,控制试验模拟出的西南低涡位置和强度与实况基本吻合。秦岭、大巴山山脉对西南低涡的形成不具有决定性影响,但对西南低涡的维持和发展具有非常重要的作用;横断山脉、云贵高原对西南低涡的生成位置、强度以及移动路径均很重要;青藏高原大地形对偏东气流的阻挡而产生的绕流有利于西南低涡的生成,对西南低涡的移动也有重要影响。除西南低涡以外,四川盆地周边地形所产生的一些局地小低涡的现象也值得关注。  相似文献   

9.
本文采用“相当正压层”的方法,分析计算了那曲、拉萨站的探空资料,求得其“相当正压层”高度约为270hpa。又以此方法分析计算了我国平原地区一些代表站的“相当正压层”高度。结果发现,其高度不是500hpa,而是在400~300hpa之间,平均约在356hpa左右。这是个值得注意的现象。  相似文献   

10.
本文采用简单的二维模式,在绝热条件下,讨论了当空气对流运动空间分市不均匀时,对流层上、中层与低层环流的耦合和相互作用,对西南低涡的维持和发展的影响,得到一些有益的结论,且与天气事实基本相符。  相似文献   

11.
四道沟金矿是地质条件较为复杂的矿床,对其成因问题前人观点众说不一。比较典型的主要有岩浆热液成因和沉积变质成因,成因不同直接影响着找矿方向。根据矿床地质特征和工作实践认为:该矿床成因应为沉积变质- 岩浆热液叠加改造型矿床。所以沉积变质和岩浆热液成矿的有利条件均应成为找矿的主要方向。据此开展的找矿工作已初步获得突破性进展。  相似文献   

12.
形成旋扭构造的动力可概括为五个方面:地块随着地球自转速率的变化,局部发生的旋扭;漂移在软流圈之上的地块遇到上拱的“热柱”受到局部牵制而旋扭;地幔熔融体物质对流循环产生蠕动式旋扭;岩石圈拖曳牵动引起旋扭;重力控制下密度分异所引起的水平漫流碰接于上升物质而旋转。欧亚大陆上分布着涡轮状、帚状、莲花状、连环状等各种旋扭构造。  相似文献   

13.
Typhoon Durian (2001),which formed over the South China Sea (SCS),was simulated by using the Weather Research and Forecasting (WRF) model. The genesis of typhoon Durian which formed in the monsoon trough was reproduced by numerical simulations. The simulated results agree reasonably well with observations. Two numerical experiments in which the sea surface temperature (SST) was either decreased or increased were performed to investigate the impact of the SST on the genesis of the ty-phoon. When the SST was decreased by 5℃ uniformly for all grids in the model,the winds calculated became divergent in the lower troposphere and convergent in the upper troposphere,creating conditions in which the amount of total latent heat release (TLHR) was low and the tropical cyclone (TC) could not be formed. This simulation shows the importance of the convergence in the lower tropo-sphere and the divergence in the upper troposphere for the genesis of the initial vortex. When the SST was increased by 1℃ uni-formly for all grids,a stronger typhoon was generated in the results with an increase of about 10 m s-1 in the maximum surface wind speed. Only minor differences in intensity were noted during the first 54 h in the simulation with the warmer SST,but apparent dif-ferences in intensity occurred after 54 h when the vortex began to strengthen to typhoon strength. This experiment shows that warmer SST will speed the strengthening from tropical storm strength to typhoon strength and increase the maximum intensity reached,while only minor impact can be seen during the earlier stage of genesis before the TC reaches the tropical storm strength. The results sug-gest that the amount of TLHR may be the dominant factor in determining the formation and the intensification of the TC.  相似文献   

14.
极地平流层位势高度变化与中国冬季气温的关系   总被引:1,自引:0,他引:1  
平流层异常对于对流层的影响研究,尤其是将平流层的异常信号加入中长期天气预报已成为近年来的研究热点。首先利用NCEP/NCAR再分析资料和国家气候中心提供的160站气温资料,采用SVD方法深入分析平流层位势高度场与中国冬季气温的关系。结果表明,极涡与中国东北地区温度有着非常密切的联系。即当中高纬地区位势高度场减弱时(极涡增强),东北地区的温度上升;中高纬地区位势高度场增强时(极涡减弱),东北地区的温度下降。进一步通过挑选出的6个东北亚型强极涡年,6个北美型强极涡年和8个弱极涡年,分别对冬季位势高度场和温度场进行合成分析、小波分析和交叉谱分析。结果发现,东北亚型强极涡和中国东北地区冬季气温的关系最为密切,平流层关键区位势高度场和东北地区地面温度场都有着50天左右的振荡周期,并且关键区位势高度场的季节内振荡有着超前于温度场的特征;北美型强极涡和东北地区温度的联系较小;弱极涡与东北地区温度的关系也不太明显。  相似文献   

15.
The Arctic vortex is a persistent large-scale cyclonic circulation in the middle and upper troposphere and the stratosphere. Its activity and variation control the semi-permanent active centers of Pan-Arctic and the short-time cyclone activity in the subarctic areas. Its strength variation, which directly relates to the atmosphere, ocean, sea ice and ecosystem of the Arctic, can affect the lower atmospheric circulation, the weather of subarctic area and even the weather of middle latitude areas. The 2003 Chinese Second Arctic Research Expedition experienced the transition of the stratosphereic circulation from a warm anticyclone to a cold cyclone during the ending period of Arctic summertime, a typical establishing process of the polar vortex circulation. The impact of the polar vortex: variation on the low-level circulation has been investigated by some scientists through studying the coupling mechanisms of the stratosphere and troposphere. The impact of the Stratospheric Sudden Warming (SFW) events on the polar vortex variation was drawing people's great attention in the fifties of the last century. The Arctic Oscillation ( AO), relating to the variation of the Arctic vortex, has been used to study the impact of the Arctic vortex on climate change. The recent Arctic vortex studies are simply reviewed and some discussions on the Arctic vertex are given in the paper. Some different views and questions are also discussed.  相似文献   

16.
本文较系统地阐述了河南省主要自然旅游资源的类型 ,依据其成因可划分为岩石圈、水圈、生物圈及大气圈旅游资源共 12类 ,2 2个景观类型  相似文献   

17.
木文采用对数压力坐标系的大气热力-动力学方程组,对城市热岛现象之一的热山波的特征、形成机制、存在条件及其对天气的影响进行了动力学和数值分析。  相似文献   

18.
按重晶石矿床地质特征、矿床成因,并结合国内重晶石矿床产出的情况,把重晶石矿床划分为:沉积型、热液型、残坡积型及火山-沉积型四类。其中沉积型重晶石矿床是我国目前最有远景的矿床类型,对改观国内重晶石矿的现状具有一定的现实意义。特别是寻找沉积型重晶石矿,必须重视对地层、岩相古地理等控矿因素的研究。最后指出寻找沉积型重晶石矿的一些有利地区。  相似文献   

19.
对大气非线性惯笥重力内波方程组,利用相平面分析法导出了相应的KdV方程。采用直接积分法求出两类有意义的孤立波解,讨论了波解的基本特征,并着重分析了一类奇异孤立波与某些天气系统(如青藏高原500hPa低涡)的可能联系。  相似文献   

20.
The influence of summer monsoon on tropical cyclone (TC) genesis over the Bay of Bengal (BoB) is explored using an empirical genesis potential (GP) index. The annual cycle of cyclogenesis frequency over the BoB shows an asymmetric bimodal pattern with the maximum genesis number appearing in late October and the second largest in early May. The two peaks correspond to the withdrawal and onset of the BoB summer monsoon, respectively. The semimonthly GP index calculated without TC days over the BoB is consistent with TC genesis frequency, indicating that the index captures the monsoon-induced changes in the environment that are responsible for the seasonal variation of TC genesis frequency. Of the four environmental variables (i.e., low-level vorticity, mid-level relative humidity, potential intensity, and vertical wind shear) that enter into the GP index, the potential intensity makes the largest contribution to the bimodal distribution, followed by vertical wind shear due to small wind speed during the summer monsoon onset and withdrawal. The difference in TC genesis frequency between autumn and late spring is mainly owing to the relative humid-ity difference because a divergence (convergence) of horizontal moisture flux associated with cold dry northerlies (warm wet wester-lies) dominates the BoB in late spring (autumn).  相似文献   

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