The Role of Midlatitude and Subtropical Air-Sea Interactions in the Formation and Variability of the Atmospheric Circulation Systems

不喜欢其他中纬度海洋区域，北太平洋次北极前区域的异常表面热通量由局部海洋表面温度（SST）控制，与其固有的十进制变异性有关。这个海洋热作用力的伴侣是风暴轨道的子午线移位。我们的GPS-sonde观察表明，前沿SST分销公司在静态稳定性和边界层中的下行动力传输中的空间不同源性，导致SST和表面风速之间的积极相关性。在南部Hem，风暴0轨道核心在一年内与印度海洋中的主要海洋前沿区相关的表面Baroclinic Zone，在那里一个极前喷气式飞机（PFJ）与表面Westerlies形式执行到动力艾迪热传输。我们是第一个提出在风暴轨道、PFJ和海洋前沿区域中可能的动态关联的人。在南太平洋，在阿索克 ... More 在冬季，当较高级别的纸张被困在密集的亚热带喷气式飞机（STJ）中，下面是表面的障碍。我们的新概念可以为北太平洋风暴中的季节性比赛提供一个可行的解释。我们已经证实，Okhotsk表面的高性能响应于寒冷的上升，由一个较高水平的阻塞高度到其西北方向，以及一个放大器应该对来自北欧的罗斯比波浪列车传播的本地中断。由于不符合先前的标准，我们已经揭示了夏季亚热带抗生素表格对凉爽的东方海洋和温暖的海洋之间形成的热对比做出了反应，大陆干燥到东部。到澳大利亚南部，在那里有一个PFJ重叠器，带着一个带层极夜间喷气式飞机的垂直波浪形形式，通过一个静态的罗斯波火车从较低的stratosphere向下传播到生成局部的异常循环。Less（低）

・Unlike in other mid-latitude oceanic regions, anomalous surface heat flux in the North Pacific sub-arctic frontal zone is controlled by local sea-surface temperature (SST) anomalies associated with its inherent decadal variability. This oceanic thermal forcing accompanies meridional shift of the storm track. Our GPS-sonde observations have revealed that the frontal SST distribution accompanies spatial imhomogeneities in static stability and thereby downward momentum transport in the boundary layer, leading to positive correlation between SST and surface wind speed.・In the Southern Hemisphere, the storm0track core is anchored throughout the year along the surface baroclinic zone associated with the major oceanic frontal zone in the Indian Ocean, where a polar-front jet (PFJ) with surface westerlies forms due to poleward eddy heat transport. We are the first to point out a possible dynamical association among a storm-track, PFJ and oceanic frontal zone. Over the South Pacific, the assoc … More iation is disturbed in winter when upper-level eddies are trapped into an intensified subtropical jet (STJ), below which surface baroclinicity. Our new concept can provide a plausible interpretation for the seasonal march in the North Pacific storm-track.・We have revealed that the surface Okhotsk High forms in response to cold advection by anomalous low-level easterlies induced by an upper-level blocking high to its northwest, which amplifies due to local breaking of an Rossby wave-train propagating from northern Europe.・As opposed to the previous understanding, we have revealed that the summertime subtropical anticyclones form in response to the profound thermal contrast between the cool eastern ocean and the warm, dry continent to its east.・To the south of Australia, where a PFJ overlaps with the stratospheric polar-night jet, a vertical waveguide forms through which stationary Rossby wave-trains propagate from the lower stratosphere downward to generate localized anomalous circulation in the troposphere. Less