查询词典 southerlies

Significant precipitation occurred over northern and northeastern Taiwan during the passage of both types of anafronts, whereas it was larger in the cold-type than that in the warm-type. For the warm-type, significant rainfall also occurred over southeastern Taiwan because the orographic lifting of the warmer and moist southerlies.

暖型与冷型上滑锋在台湾北部与东北部均有较显著降水，但冷型上滑锋的降水强度较大；暖型上滑锋在东南部锋上的降水强度有另ㄧ大值，此乃因锋前南风分量带来暖湿空气，且东南部位在迎风面，因地形举升故有较大降水。

Those anomalous atmospheric circulations stimulated the strong anomalous southerlies along the east coastal regions of China, which persistently transferred the warm and wet air to the northeastern areas of China, thus raising the moisture content and air temperature there and providing proper warm and wet conditions for the occurrence of the extreme snowstorm event.

这些异常环流在中国东部沿岸地区引起了强劲的偏南风，由此给中国东部北方地区源源不断地输送暖湿空气，使得该地的水汽含量和气温不断升高，为这次暴风雪事件的发生准备了良好的暖空气条件。

The convergence between anomalous northerlies from the central northern Pacific and anomalous southerlies from northerneast Australian can trigger strong westerly anomalies over the central and eastern tropical Pacific and then cause El 〓 event.

EL 〓的爆发和维持需要中太平洋地区的来自南北半球的经向风辐合所引起赤道中东太平洋的异常西风，其中来自澳大利亚东北部的异常南风的作用更为显著。

The southerlies prevailed in the prefrontal areas of warm-type anafronts during the period of dominance of the subtropical ridge.

暖型上滑锋受到太平洋高压脊西伸至台湾邻近海面影响，锋前为南风分量；冷型上滑锋受到大陆高压笼罩台湾地区影响，锋前与锋后均为北风分量。

The function always enhances southerlies and brings heavy rainfall and more latent heating over tropical land to southeast of the Tibet , prevail northerlies , less rainfall and more sensible heating over tropical land to southwest of the Tibet .

结果表明，青藏高原的&热力滑轮&作用引起：高原东南面热带陆地上空的偏南气流加强，降水增加，凝结潜热加强；高原西南面热带陆地上空出现偏北气流，降水减弱，陆面的感热加热加强。

Anomalous anticyclone at the upper level is form in response to the enhanced convective heating off the equator, resulting in increased geopotential height and temperature over the Tibetan Plateau and in favor of the early BOB seasonal transition. Another effect of Positive SST anomalies over the Warm Pool is to induce anomalously strong zonal monsoon circulation. The anomalous zonal monsoon circulation strengths the southerlies in upper levels due to Coriolis force. Thus the enhanced warm meridional advection in connection with the warming over the Tibetan Plateau lead to early seasonal transition over the BOB region.

高空大气通过热力适应过程对这种异常对流加热的响应是产生异常反气旋环流，则高原上空的位势高度偏高，温度偏高，引起季节转换偏早；暖池海温异常偏高的另一作用是，它激发出异常强的季风纬向环流，在高层，季风纬向环流受到柯氏力作用又使得南风加强，导致孟加拉湾东部地区经向暖平流及其北部下沉增温加强，加速了孟加拉湾季节转换进程。

Following the above conditions,anomalous southerlies transport water vapor to the north and cause moreprecipitation over there.The key condition for the above-normal production year is that SST anomalies over the northwesternportion are warmer than that over the southeastern portion during the winter season.

在此南北分布状态下，风场与辐散风距平均由南向北吹，不仅降低北区冬季东北季风强度，亦将热带水汽往北传送，让北方海域之大气总含水量增加，藉由辐合距平之举升机制，降水量亦随之增加，而水汽递出之南方海域则是二者皆减少。

The Somali jet is rapidly enhanced two pentads prior to the onset of SCSSM, thus accelerating the eastward extension of the westerly over the Bay of Bengal and leading to the eastward retreat of the western Pacific subtropical high . At the same time, the rapid enhancement of SCS CEF can also result in the northward march of WPSH and the onset of SCSSM. The earlier establishment and stronger southerlies correspond to the earlier onset time of SCSSM, and vice versa. Both composite and correlation analyses show that the 150hPa Asia-Australia CEF in boreal spring has important influences on EASM.

相关分析和合成分析的结果还显示，春季150hPa亚澳越赤道气流对东亚夏季风有重要影响：当春季该气流偏弱时，北半球夏季西太平洋副高强度偏强，位置偏南偏西，南亚高压强度也偏强，这样的环流背景使江淮流域6—7月降水偏多，华南华北降水偏少；反之，当春季该气流偏强时，夏季西太副高强度偏弱，位置偏北偏东，南亚高压强度也偏弱，江淮流域夏季降水偏少，华南华北降水偏多。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。