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      西南     
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  southwest
    THE DYNAMICAL ANALYSIS OF THE GENERATION AND DEVELOPMENT OF THE SOUTHWEST LOW VORTEX
    西南低涡发生发展的动力学分析
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    THE DYNAMIC ANALYSES OF THE EFFECT OF LARGE-SCALE ENVIRONMENT FLOW FIELDS AND CUMULUS ON THE DEVELOPMENT OF SUB-SYNOPTIC SCALE SOUTHWEST VORTEX
    大尺度环境场和CISK与西南低涡发展的动力学分析
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    A CASE STUDY OF THE FLOW FIELD LOW VORTEX IN SOUTHWEST CHINA
    一次西南低涡流场中的分析
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    MESOANALYSIS OF THE SURFACE DATA DURING A SOUTHWEST VORTEX PROCESS
    一次西南低涡过程的地面场中尺度分析
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    NUMERICAL SIMULATIONS OF EXTREMELY INTENSE RAINSTORM AND SOUTHWEST VORTEX OVER SICHUAN IN JULY OF 1981
    四川“81.7”特大暴雨和西南涡的数值模拟
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  southwest china
    A CASE STUDY OF THE FLOW FIELD LOW VORTEX IN SOUTHWEST CHINA
    一次西南低涡流场中的分析
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    A POTENTIAL MECHANISM OF THE WARM VORTEX GENESIS IN SOUTHWEST CHINA
    暖性西南低涡生成的一种可能机制
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    SOME BASIC FACTS ABOUT THE SOUTHWEST CHINA VORTEX AND THEIR PRILMINARY ANALYSIS
    西南低涡的一些基本事实及初步分析
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    A Study on the Formation Processes of Acid Rain in Some Areas of Southwest China
    中国西南典型地区酸雨形成过程研究
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    ABNORMAL PRECIPITATION AND MODIFICATIONAL FACTORS IN FLOOD PERIODS OF THE SOUTHWEST CHINA
    中国西南汛期降水异常及影响因子
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  the southwest
    THE DYNAMICAL ANALYSIS OF THE GENERATION AND DEVELOPMENT OF THE SOUTHWEST LOW VORTEX
    西南低涡发生发展的动力学分析
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    SOME BASIC FACTS ABOUT THE SOUTHWEST CHINA VORTEX AND THEIR PRILMINARY ANALYSIS
    西南低涡的一些基本事实及初步分析
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    ABNORMAL PRECIPITATION AND MODIFICATIONAL FACTORS IN FLOOD PERIODS OF THE SOUTHWEST CHINA
    中国西南汛期降水异常及影响因子
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    Abstact Based on the data of the MICAPS and the NCEP2.5x2.5°from 1996 to 2005,the southwest vortext influencing the south china and the flash-flood-producing vortex are analyzed ,the results reveal the features of the vortexs action,the basis of the vortex and the flash-flood-producing rainstorm forecastings is offered to weather forecasters.
    利用1996~2005年近十年的MICAPS和NCEP2.5x2.5°再分析资料,对影响华南地区西南低涡以及致洪低涡活动进行系统性的统计研究,揭示低涡活动的特征,为华南地区的低涡及其致洪暴雨预报提供依据。
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    A NUMERICAL EXPERIMENT ON “93.8”HEAVY RAIN OF THE SOUTHWEST OF SHANGDONG
    “93.8”鲁西南大暴雨的数值试验
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  sw
    THE RELATIONSHIP BETWEEN THE SW MONSOON SURGE ON 850 MB IN THE NORTHWEST PART OF SOUTH CHINA SEA AND THE HEAVY PRECIPITA-TION IN GUANGDONG
    850毫巴南海西北部西南季风潮及其与广东强降水的关系
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    Numerical Simulation and Diagnosis of the Formation Process of SW Vortex Ⅱ: The diagnosis of vorticity equation and energy conversion function
    一次西南低涡形成过程的数值试验和诊断——Ⅱ:涡度方程和能量转换函数的诊断分析
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    AGRICULTURAL SIGNIFICANCE OF THE FOEHN EFFECT IN THE SW MONSOON:A CASE STUDY IN THE AILAO MOUNTAIN
    哀牢山(西南季风山地)焚风效应的农业意义
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    HEAT AND MOMENTUM BUDGETS IN SOUTH CHINA DURING ACTIVE SW MONSOON PERIOD
    华南西南季风活跃期间大气热量和动量的收支
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    INFLUENCE OF PHYSICAL PROCESSES AND RESOLUTION OF MM 4 ON MESOSCALE SIMULATION OF THE EVOLUTION OF THE SW VORTEX
    物理过程和分辨率对西南涡演变的中尺度模拟影响
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  southwest
       Lichuan, located at the foot of the Wuling Mountain in southwest Hubei Province of central China, is well known in the world for the discovery of the living fossil Metasequoia glyptostroboides Hu >amp;amp; Cheng in the 1940s.
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       The isogram of the PCGA was drawn out with 0.2 contours, which showed a geographical model with a northeast-southwest variation trend of the phenotypic characters of M.
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       Shear strengths of undisturbed and remolded soil under typical forests in Jinyun Mountain, Chongqing City, southwest China
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       Soil fractal features of typical forest stands in Jinyun Mountain, Chongqing City, Southwest China
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       All their specimens are deposited in the insect specimen laboratory of the Department of Resources, Southwest Forestry College (Kunming, China).
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  southwest china
       Shear strengths of undisturbed and remolded soil under typical forests in Jinyun Mountain, Chongqing City, southwest China
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       Soil fractal features of typical forest stands in Jinyun Mountain, Chongqing City, Southwest China
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       mandshurica growing in different environments on Gaoligong Mountains, Yunnan Province of Southwest China and on Changbai Mountains, Jilin Province of Northeast China.
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       From 1984 to 1986, a national comprehensive scientific investigation on KD in Chuxiong region of Yunnan Province in the southwest China was conducted.
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       Chronological and geochemical constraints on the assumed large permian volcanic province in Southwest China
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  the southwest
       Now these sites are known as the Arshan and Khalyuta deposits spaced 20 km apart and located at 45-47 km to the southwest and west of Ulan-Ude, respectively.
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       The sampling localities covered a wide part of the species range: from the Peter the Great Bay (the Sea of Japan) at the southwest to the Mednyi Island (Commander Islands) at the northeast.
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       The southwest part of Peter the Great Bay, from the mouth of the Tumen River up to Furugelm Isl, was contaminated by HCHs to a greater extent than Amursky Bay.
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       The histomorphology of the digestive gland of the bivalve mollusk Crenomytilus grayanus from Sivuchya Bay, which is located in the southwest of Peter the Great Bay and subjected to the effect of polluted waters of Tumannaya River, was studied.
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       The Otava River is situated in the southwest of the Czech Republic.
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  sw
       The NE-SW compressive stress from the Qinling orogenic belt and detachment layers in the covering strata are the two most important determinants of deformation style.
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       On various short-wave (SW) radio paths, intense variations of Doppler frequency shift were observed.
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       The oxygenic and cooperative respiration of the wood-decaying fungus Fomitopsis pinicola (Sw.: Fr.) Pers.
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       The possibilities of increasing the rates of physicochemical processes (PCP) occurring in shock waves (SW) have been recently investigated in a number of studies [1-5].
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       A mode with different partial velocities and temperatures of the components is observed in the SW front in mixtures of gases with different masses and cross sections of particles.
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  其他



         First in this paper the mean 2-year mean winter and summer wind fields below 6kmover Tibetan Plateau and its surrounding are presented.In winter the main features on 1.5km(fig.1)and 3 km(fig.2)level are the splitting of the westlies over the plateau,the lineof convergence to the east of the plateau and the“dead-water”regions(characterized by calmwind and little disturbances,except small local vortices)respectively to the east and west of theplateau.On 6km(fig.4)the minor features disappear but the splitting...
            本文利用1954—1956年的高空及地面记录,作出了平均流场,并计算了垂直速度、冷暖平流及辐射等,得出下面几点结论:1)冬季在1.5千米及3千米的西风,在高原西边有明显的分支,东边有明显的会合,且在东西两边各有一“死水区”(风速很小),在高原北面形成了高压脊,而在其南面形成了低槽,到了6千米除了二个“死水区”消失以外,其余基本上没有变化。2)夏季1.5千米及3千米在高原附近的流线,绕高原作气旋性旋转,而到了6千米则相反而呈反气旋性旋转,其中心在高原西南部分,且随高度增加而向西偏。3)夏季在高原上基本上是上升运动,可能达到9千米;冬季在高原上估计可能是下沉运动(除西南角有部分上升运动)。4)夏季可以肯定高原是一个热源,而冬季除了西南角有—部分是热源外,其他地区可能是一冷源。
文摘来源
         ~~
            本文指出当高空槽自亚洲西部移到印度北部时,北纬40°以南的槽线成西北—东南向,此后高空槽在东移过程中又逐渐转为东北—西南向。但低空的低槽被阻于印度的西北部,并且很快就消失。当槽过高原后有很明显的减弱,过了汉口就消失,但它对于我国华东华南的天气影响是很明显的。当它经过高原时,其移动速度约为每天11—12个经度。
文摘来源
         In this paper,an analysis is made on the structure of the July meanflow field at 850 mb,700 mb,500 mb over the continent of Asia during theyear 1951—1955 and the mean contours at 200 mb over Asia for July andAugust,1956.The vertical cross-sections of the mean flow and temperaturefields along 75°E,90°E,105°E and 120°E for July and August,1956 havebeen constructed.The three-dimensional flow structure over continent ofAsia is constituted of the following three basic currents:(1) the westerliesof middle latitud...
            作者分析了1951—55时期中850、700及500毫巴的7月平均气流场的构造,以及1956年7、8两月亚洲上空200毫巴平均等高线图.又作了1956年7、8两月东经75度、90度、105度和120度经线上平均风场和温度场的剖面.我们发现,在夏季有三种基本气流组成亚洲大陆上空三度空间的气流场:即,(1)中纬度的西风气流,(2)高空热带和副热带的东风气流,(3)位于高空热带和副热带东风气流下面的西南季风.此外,对于1956年从春季到夏季的过渡时期中,亚洲上空大气环流的转变,亦作了研究.我们发现,从春季到夏季的过渡时期中,亚洲上空的大气环流有着一个跳躍的转变.在这个时期中,喜马拉雅山南边的高空副热带西风急流向北撤退,在西藏高原的纬度上空,建立一个副热带高压脊线,并且在亚洲南部上空(北纬12度以南)建立一支高空东空急流.同时印度的西南季风和我国长江流域的梅雨时期开始出现.作者又发现,夏季在中国大陆上,雨带的北移和西风带北撤以及相应的西风带强度的削弱有着密切的联系.
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