On the stability of a coupled ocean atmosphere system in the presence of wave-CISK     

Sudha Selvarajan  B. N. Goswami 《Journal of Earth System Science》1992,101(2):153-176

The stability of a simple coupled ocean-atmosphere system similar to the one studied by Hirst with general ocean thermodynamics is investigated in which the atmospheric heating is determined by sea surface temperature anomalies as well as the convergence feedback (low level moisture convergence by the waves themselves). It is shown that the unstable coupled mode found by Hirst (UH mode) is profoundly modified by the convergence feedback. The feedback increases the unstable range of the UH mode and can increase its growth rate several folds. The maximally growing UH mode can become westward propagating for certain strength of convergence feedback. If the convergence feedback strength exceeds a critical value, several new unstable intraseasonal modes are also introduced. These modes are basically ‘advective’ modes. For relatively weak strengths of the convergence feedback the growth rates of these modes are smaller than that of the UH mode. As the atmosphere approaches ‘moist neutral’ state, the growth rates of these modes could become comparable or even larger than that of the UH mode. It is argued that these results explain why the El Nino and Southern Oscillation (ENSO) signal is clear in the eastern Pacific but not so in the western Pacific and they may also explain some of the differences between individual ENSO events. Our results also explain the aperiodic behaviour of some coupled numerical models. Importance of this process in explaining the observed aperiodicity of the ENSO phenomenon is indicated.  相似文献   

L_p估计的计算问题     

周世健 《测绘学院学报》1995,(2)

本文对Ｌｐ估计的直接算法进行了详细的分析和讨论，由于直接算法效率低，文中提出了一种快速算法（残差逐步下降法），采用可变尺度因子来修正Ｈｕｂｅｒ的常数尺度因子。最后，以实例加以分析和说明。  相似文献   

Interannual Fluctuations of Surface Air Temperature over North America and Its Relationship to the North Pacific SST Anomaly     

Wu Renguang  Chen Lieting 《大气科学进展》1995,12(1):20-28

The characteristics of interannual fluctuations of the surface air temperature over North America are investigated by using the surface air temperature data of 130 stations during 1941 through 1980. It is found that the surface air temperature bears about ten-year time scale oscillation over the southeastern and northwestern North America and along the west coast of the United States, and it has the characteristics of quasibiennial oscillation over the eastern North America. The ten-year scale oscillation of the surface air temperature is related to that of the sea surface temperature (SST) of North Pacific through the PNA pattern atmospheric circulation anomaly over North Pacific through North America. It is shown that the North Pacific SST has a closer association with the surface air temperature over North America than the central and eastern equatorial Pacific SST. The characteristics of the seasonal variations of the relationship between the North Pacific SST and the surface air temperature over No  相似文献   

Three－dimensional　Global　Scale　Permanent－wave　Solutions　of　the　Nonlinear　Quasigeostrophic　Potential　Vorticity　Equation　and　Energy　Dispersion     

H.L. Kuo 《大气科学进展》1995,12(4):387-404

The three-dimensional nonlinear quasi-geostrophic potential vorticity equation is reduced to a linear form in the stream function in spherical coordinates for the permanent wave solutions consisting of zonal wavenumbers from 0 to n and rn vertical components with a given degree n. This equation is solved by treating the coefficient of the Coriolis parameter square in the equation as the eigenvalue both for sinusoidal and hyperbolic variations in vertical direction. It is found that these solutions can represent the observed long term flow patterns at the surface and aloft over the globe closely. In addition, the sinusoidal vertical solutions with large eigenvalue G are trapped in low latitude, and the scales of these trapped modes are longer than 10 deg. lat. even for the top layer of the ocean and hence they are much larger than that given by the equatorial β-plane solutions. Therefore such baroclinic disturb-ances in the ocean can easily interact with those in the atmosphere.Solutions of the shallow water potential vorticity equation are treated in a similar manner but with the effective depth H = RT / g taken as limited within a small range for the atmosphere.The propagation of the flow energy of the wave packet consisting of more than one degree is found to be along the great circle around the globe both for barotropic and for baroclinic flows in the atmosphere.  相似文献   

青藏高原现代降水中dδ^18O／dT的变化   总被引：3，自引：2，他引：3  

章新平  姚檀栋 《冰川冻土》1995,17(4):308-314

不同时间尺度ｄδ＾１８Ｏ／ｄＴ的天气气候意义是不同的，其数值大小也是不一样的。本根据对青藏高原沱沱河、德令哈、西宁三站大气降水中δ＾１８Ｏ与温度关系的分析，并与具有长序列资料的地区进行比较。初步给出了青藏高原不同时间尺度ｄδ＾１８Ｏ／ｄＴ之间的差异。  相似文献   

岩石节理粗糙度系数的分形特征   总被引：5，自引：0，他引：5  

杜时贵  潘别桐 《水文地质工程地质》1993,20(3):36-39

岩石节理粗糙度系数JRC是估算节理抗剪强度和变形指标最重要的参数。通过对简易纵剖面仪获取的节理表面轮廓曲线的分形研究,讨论了节理表面轮廓曲线的自相似性和JRC的自相似性,并根据实测统计资料的分析,指出了分形理论研究JRC的适用条件和有效的使用方法。由实测统计资料的JRC尺寸效应自相似性分析,认为JRC尺寸效应具分形结构。本文介绍了一种确定JRC尺寸效应分维数D的方法,由此确定的分维数D具有明确的物理意义。  相似文献   

减小水平分量磁变仪记录非线性的技术措施   总被引：2，自引：0，他引：2  

朱兆才 《地震地磁观测与研究》1993,14(3):53-58

讨论了减小水平分量磁变仪记录非线性的技术措施。选择适宜的标度值(C/M)、选取适当的入射角α_0、选择适当的记录距离R是改善水平分量磁变仪记录状态的主要途径。文中对比作了具体分析。  相似文献   

中,俄,美大尺度岩石破裂实验考察报告     

李世愚  陆阳泉 《国际地震动态》1993,(7):5-8

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A dynamic network model for two‐phase immiscible flow     

Helge K. Dahle  Michael A. Celia 《Computational Geosciences》1999,3(1):1-22

A dynamic pore‐scale network model is formulated for two‐phase immiscible flow. Interfaces are tracked through the pore throats using a modified Poiseuille equation, whereas special displacement rules are used at the pore bodies. The model allows interfaces to move over several pore‐lengths within a time step. Initial computational results are presented for a drainage experiment to demonstrate some of the features of the model. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

Comparative hydrogeology – reference analysis of groundwater dynamics from neighbouring observation wells     

Markus Giese  Ezra Haaf  Benedikt Heudorfer  Roland Barthel 《水文科学杂志》2020,65(10):1685-1706

ABSTRACT

Groundwater level fluctuations are caused by spatial and temporal superposition of processes within and outside the aquifer system. Most of the subsurface processes are usually observed on a small scale. Upscaling to the regional scale, as required for future climate change scenarios, is difficult due to data scarcity and increasing complexity. In contrast to the limited availability of system characteristics, high-resolution data records of groundwater hydrographs are more generally available. Exploiting the information contained in these records should thus be a priority for analysis of the chronical lack of data describing groundwater system characteristics. This study analyses the applicability of 63 indices derived from daily hydrographs to quantify different dynamics of groundwater levels in unconfined gravel aquifers from three groundwater regions (Bavaria, Germany). Based on the results of two different skill tests, the study aids index selection for different dynamic components of groundwater hydrographs.  相似文献