副热带的

The relationship between the subtropical anticyclone and subtropical easterlies is discussed, aiming at the problem of high temperature and drought in the globe.

仅就2006年发生在四川、重庆的高温干旱问题，讨论了副热带高压与东风层的关系，进而对地球的章动、转速的变化做了对比分析。

It is found that in summer, the region between the southern edge of the westerlies and the northern margin in the subtropical anticyclone of the West Pacific is a favorable location for strong deep summer convection and MCS development.

夏季汛期降水主要受东亚夏季风的影响，非台风暴雨的出现与夏季风的进退一致。夏季在东亚西风带南缘和西太平洋副热带高压之间的地区，是夏季最有利于深对流和MCS发展的地区。

The correlogram of CEF and OLR and the composite chart of 850hPa wind field while CEF is stronge...

结果表明，夏季海洋大陆赤道缓冲区的对流上升运动(90°E～120°E，5°N～5°S)、澳州大陆冷性高压(10°S～30°S，120°E～155°E)的发展，都影响2～3候以后105°E夏季越赤道气流；澳洲大陆北部的冷性高压，西太平洋副热带高压西端位置西伸或东缩造成的东中国海季风区上升运动的变化，又是南北半球环流同时影响CEF变化的具体表现。

The distribution of water temperature, salinity, density, dissolved oxygen content, geostrophic current and their relationships with ENSO events were analyzed.

摘 要：根据日本气象厅RyofuMaru调查船干1972～1977和1989～1990年间夏季在155°E断面观测的水文资料，分析了该断面上北太平洋副热带海域(18°～30°N)的主要水文要素-温度、盐度、密度、溶解氧含量和地转流等的分布特征及其与ENSO现象之间的关系。

It is also suggested that the interannual and long-term variations in SST of the South China Sea may be resulted from the meridional wind anomaly and zonal migration of the subtropical high over the western Pacific.

相关和合成分析表明，南海SST的年际和长期变化可能是由南海上空的经向风异常和西太平洋副热带高压的纬向变动引起的。

The results indicated that the effect of deep warm-wet air coming along the behind subtropical high , moving eastward deepening upper trough , shear line and cyclone trough was caused in Zhuanghe , but no strong thunderstorm . The main impact of system is surface cyclone trough ; Low vortex , shear line in 700hPa , 850hPa strengthen the lower convergence , forming a strong momentum of increase and pieces of water vapor ; strong and wide potential pseudo-equivalent temperature frontal zone lied in Zhuanghe area , the establishment of potential instability are indispensable conditions for producing heavy rain .

结果表明：受副热带高压后部深厚的暖湿气流及西风带高空槽、切变线及气旋倒槽等动力系统共同影响，庄河地区出现了大暴雨天气，但没有出现强雷暴，此过程主要影响系统是地面气旋倒槽；700hPa、850hPa低涡、切变线使中低层辐合加强，形成了较强的动力抬升和水汽辐合；庄河地区处于强而宽的假相当位温锋区中，位势不稳定的建立是造成此次强降水的必要条件。

Over the northern SCS, analysis results find the lower troposphere is convectively unstable during the entire onset period. The favorable atmospheric conditions for convection are attributed to low-level moisture convergence caused by the frontal southwesterly flow during the first stage, and the retreat of western Pacific subtropical high and warm-moist southwesterly flow from the Bay of Bengal during the later stages.

分析结果显示，在1998年南海夏季季风肇始发展过程中，南海北部的大气大多呈现对流不稳定的形势，第一阶段锋前西南气流造成低层强烈的水气辐合，第二阶段之后锋面远离且太平洋副热带高压东退，来自孟加拉湾的西南气流夹带大量暖湿水气使得南海北部在整个季风肇始期间都是有利於对流的状况。

A numerical simulation technique is adopted to draw the surface projection map and its isograms of the pH values in the precipitation over Jiangxi Province.

采用数字模拟技术，绘制了江西省降雨pH值曲面投影图及其等值线图，发现江西省在南昌-鹰潭-临川-吉安-赣州一线形成南北方向的&r&字形的严重酸雨带，并指出这条严重酸雨带的走向与信风环流圈和副热带高压带纬向环流一致。

Along 90°E the easterly wind in mid-upper layer is obviously weakened to the south of the plateau, and the westerly wind in mid-upper layer along 140°E is enhanced to the south of 35°N but it is obviously weakened to the north of 35°N.

利用p-σ九层区域气候模式进行高原隆升对东亚副热带西风急流影响的敏感性试验，分析高原隆升过程中西风急流垂直结构和水平结构的变化，并对其变化的原因进行初步分析。

It is found that a severe acid-rain band is formed along the southern-north direction of Nanchang-Yingtan-Linchuan-Jian-Ganzhou in the Province,taking a shape of "r".

提出了矿山废石堆的硫化矿物是造成严重酸雨的主要致酸物质来源，揭示了江西省降雨pH值随副热带高压脊季节性南北推移而变化的规律。

For a big chunk of credit-card losses; the number of filings (and thus charge-off rates) would be rising again, whether

年美国个人破产法的一个改动使得破产登记急速下降，而后引起了信用卡大规模的亏损。

Eph. 4:23 And that you be renewed in the spirit of your mind

弗四23 而在你们心思的灵里得以更新