共查询到20条相似文献，搜索用时 125 毫秒
1.
Yong L. McHall 《大气科学进展》1994,11(2):251-251
ＡｎＩｎｔｒｏｄｕｃｔｉｏｎｔｏｔｈｅＮｅｗＢｏｏｋ－ＧＥＯＳＴＲＯＰＨＩＣＷＡＶＥＣＩＲＣＵＬＡＴＩＯＮＳ￥Ｙｏｎｇ．Ｌ．ＭｃＨａｌｌＤｅｐｔ．ｏｆＥａｒｔｈ，ＡｔｍｏｓｐｈｅｒｉｃａｎｄＰｌａｎｅｔａｒｙＳｃｉｅｎｃｅｓ，ＭＩＴＰｕｂｌｉｓｈｅｄ... 相似文献
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Mozheng Wei 《大气科学进展》1996,13(1):67-90
ＡＬｏｗ－ｏｒｄｅｒＭｏｄｅｌｏｆＴｗｏ－ｄｉｍｅｎｓｉｏｎａｌＦｌｕｉｄＤｙｎａｍｉｃｓｏｎｔｈｅＳｕｒｆａｃｅｏｆａＳｐｈｅｒｅＭｏｚｈｅｎｇＷｅｉ（ＣＲＣｆｏｒＳｏｕｔｈｅｒｎＨｅｍｉｓｐｈｅｒｅＭｅｔｅｏｒｏｌｏｇｙ，ＣＳＩＲＯＤｉｖｉｓｉｏ... 相似文献
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This research is supported by the Research Grants Council of the University Grants Committee of Hong Kong Grant . C. H. So Johnny C. L. Chan Department of Physics Materials Science City University of Hong Kong 《大气科学进展》1997,(2)
ＲｅｇｉｏｎａｌａｎｄＳｙｎｏｐｔｉｃ－ｓｃａｌｅＦｅａｔｕｒｅｓＡｓｏｃｉａｔｅｄｗｉｔｈＩｎａｃｔｉｖｅＰｅｒｉｏｄｓｏｆｔｈｅＳｕｍｍｅｒＭｏｎｓｏｏｎｏｖｅｒＳｏｕｔｈＣｈｉｎａ①Ｃ．Ｈ．ＳｏａｎｄＪｏｈｎｎｙＣ．Ｌ．ＣｈａｎＤｅｐａｒｔｍｅ... 相似文献
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ＳｏｍｅＡｓｐｅｃｔｓｏｆｔｈｅＣｈａｒａｃｔｅｒｉｓｔｉｃｓｏｆＭｏｎｓｏｏｎＤｉｓｔｕｒｂａｎｃｅｓＵｓｉｎｇａＣｏｍｂｉｎｅｄＢａｒｏｔｒｏｐｉｃ－ＢａｒｏｃｌｉｎｉｃＭｏｄｅｌ￥Ｎ．Ｒ．ＰａｒｉｊａａｎｄＳ．Ｋ．Ｄａｓｈ（ＣｅｎｔｒｅｆｏｒＡ... 相似文献
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Ｂｅｈａｖｉｏｕｒ ｏｆ Ｃｏｕｐｌｅｄ Ｍｏｄｅｓ ｉｎ ａ Ｓｉｍｐｌｅ Ｎｏｎｌｉｎｅａｒ Ａｉｒ－Ｓｅａ Ｉｎｔｅｒａｃｔｉｏｎ ＭｏｄｅｌＬｉＣｈｏｎｇｙｉｎａｎｄＬｉａｏＱｉｎｇｈａｉ（ＬＡＳＧ，ＩｎｓｔｉｔｕｔｅｏｆＡｔｍｏｓｐｈｅｒｉ... 相似文献
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Wen Jingsong 《大气科学进展》1995,12(2):187-194
ＴｈｅＥｆｆｅｃｔｏｆＷｅａｋＳｈｅａｒ－ｉｎｄｕｃｅｄＭｏｔｉｏｎｏｎＢｒｏｗｎｉａｎＣｏａｇｕｌａｔｉｏｎｏｆＡｅｒｏｓｏｌＰａｒｔｉｃｌｅｓＷｉｎｊｉｎｇｓｏｎｓ（Ｃ．Ｓ．Ｗｉｎ）（温景嵩）（Ｄｅｐａｒｔｍｅｎｔｏｆｐｈｙｓｉｃｓ，Ｎａｎｋａｉ... 相似文献
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ＳＨＯＲＴ－ＴＥＲＭＣＬＩＭＡＴＥＣＨＡＮＧＥＡＮＤＩＴＳＣＡＵＳＥＡＮＤＣＬＩＭＡＴＥＰＲＥＤＩＣＴＩＯＮＩＮＣＨＩＮＡ￥ＷｅｉＦｅｎｇｙｉｎｇ（魏凤英）（ＩｎｓｔｉｔｕｔｅｏｆＳｙｎｏｐｔｉｃａｎｄＤｙｎａｍｉｃＭｅｔｅｏｒｏｌｏｇｙ．）Ｂｅｉｊ... 相似文献
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ＷＡＭ模式是继１９８０－１９８３年美、日、英、德、荷兰等国的海洋专家组成ＳＷＡＭＰ研究组，针对世界各国十个有代表性的海浪数值模式，进行分类和对比试验研究之后，西欧一些国家自１９８５年起，由Ｓ．Ｈａｓｓｅｌｍａｎｎ、Ｋ．Ｈａｓｓｅｌｍａｎｎ、Ｅ．Ｂａｕｅｒ、Ｐ．Ａ．Ｅ．Ｍ．Ｊａｎｓｓｅｎ、Ｇ．Ｊ．Ｋｏｍｅｎ、Ｌ．Ｂｅｒｔｏｔｔｉ、Ｐ．Ｌｉｏｎｅｌｌｏ、 Ａ．Ｇｕｉｌｌａｕｍｅ、Ｖ．Ｃ．Ｃａｒｄｏｎｅ 相似文献
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Ｔｈｅ Ｅａｓｔ Ａｓｉａｎ Ｍｏｎｓｏｏｎ Ｓｉｍｕｌａｔｉｏｎ ｗｉｔｈ ＩＡＰ ＡＧＣＭｓ－Ａ Ｃｏｍｐｏｓｉｔｅ ＳｔｕｄｙＷａｎｇＨｕｉｊｕｎａｎｄＢｉＸｕｎｑｉａｎｇ（ＩｎｓｔｉｔｕｔｅｏｆＡｔｍｏｓｐｈｅｒｉｃＰｈｙｓｉｃｓ（ＩＡＰ），... 相似文献
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Renguang Wu 《Climate Dynamics》2010,34(5):629-642
Analysis of the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) data for the period 1998–2007 reveals large
subseasonal fluctuations in sea surface temperature (SST) of the South China Sea during the summer monsoon onset. These subseasonal
SST changes are closely related to surface heat flux anomalies induced by surface wind and cloud changes in association with
the summer monsoon onset. The SST changes feed back on the atmosphere by modifying the atmospheric instability. The results
suggest that the South China Sea summer monsoon onset involves ocean–atmosphere coupling on subseasonal timescales. While
the SST response to surface heat flux changes is quick and dramatic, the time lag between the SST anomalies and the atmospheric
convection response varies largely from year to year. The spatial–temporal evolution of subseasonal anomalies indicates that
the subseasonal variability affecting the South China Sea summer monsoon onset starts over the equatorial western Pacific,
propagates northward to the Philippine Sea, and then moves westward to the South China Sea. The propagation of these subseasonal
anomalies is related to the ocean–atmosphere interaction, involving the wind-evaporation and cloud-radiation effects on SST
as well as SST impacts on lower-level convergence over the equatorial western Pacific and atmospheric instability over the
Philippine Sea and the South China Sea. 相似文献
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资料分析及其同南亚（印度）夏季风的比较,指出建立的突发性和经向分量的重要性是南海夏季风活动的两个最基本特征。根据南海夏季风经向分量与纬向分量同样重要的特征,并考虑南海地区大气环流的基本形势,提出了用对流层高低层散度差构成季风指数,它可以更好地描写南海夏季风的活动。资料分析和大气环流模式（GCM）数值模拟试验都清楚地表明南海夏季风年际异常对大气环流和气候有极为重要的影响,不仅影响东亚地区,而且通过东亚-太平洋-美洲（PJ或称EPA）波列影响美国的天气气候变化。 相似文献
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Using daily observational rainfall data covered 194 stations of China from 1961 to 1995 and NCEP model analyzed pentad precipitation data of global grid point from 1979 to 1997,the distribution of onset date of rainy season over Asian area from spring to summer is studied in this paper.The analyzed results show that there exist two stages of rainy season onset over East Asian region from spring to summer rainy season onset accompanying subtropical monsoon and tropical monsoon respectively.The former rain belt is mainly formed by the convergence of cold air and the recurred southwesterly flow from western part of subtropical high and westerly flow from the so-called western trough of subtropical region occurring during winter to spring over South Asia.The latter is formed in the process of subtropical monsoon rain belt over inshore regions of South China Sea originally coming from south of Changjiang (Yangtze) River Basin advancing with northward shift of subtropical high after the onset of tropical monsoon over South China Sea.The pre-flood rainy season over South China region then came into mature period and the second peak of rainfall appeared.Meiyu,the rainy season over Changjiang-Huaihe River Basin and North China then formed consequently.The process of summer tropical monsoon onset over South China Sea in 1998 is also discussed in this paper.It indicated that the monsoon during summer tropical monsoon onset over South China Sea is the result of the westerly flow over middle part of South China Sea,which is from the new generated cyclone formed in north subtropical high entering into South China Sea,converged with the tropical southwesterly flow recurred by the intensified cross-equatorial flow. 相似文献
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ON THE PROCESS OF SUMMER MONSOON ONSET OVER EAST ASIA 总被引：6，自引：0，他引：6
Using daily observational rainfall data covered 194 stations of China from 1961 to 1995 andNCEP model analyzed pentad precipitation data of global grid point from 1979 to 1997,thedistribution of onset date of rainy season over Asian area from spring to summer is studied in thispaper.The analyzed results show that there exist two stages of rainy season onset over East Asianregion from spring to summer rainy season onset accompanying subtropical monsoon and tropicalmonsoon respectively.The former rain belt is mainly formed by the convergence of cold air and therecurred southwesterly flow from western part of subtropical high and westerly flow from the so-called western trough of subtropical region occurring during winter to spring over South Asia.Thelatter is formed in the process of subtropical monsoon rain belt over inshore regions of South ChinaSea originally coming from south of Changjiang (Yangtze) River Basin advancing with northwardshift of subtropical high after the onset of tropical monsoon over South China Sea.The pre-floodrainy season over South China region then came into mature period and the second peak of rainfallappeared.Meiyu,the rainy season over Changjiang-Huaihe River Basin and North China thenformed consequently.The process of summer tropical monsoon onset over South China Sea in 1998is also discussed in this paper.It indicated that the monsoon during summer tropical monsoononset over South China Sea is the result of the westerly flow over middle part of South China Sea,which is from the new generated cyclone formed in north subtropical high entering into SouthChina Sea,converged with the tropical southwesterly flow recurred by the intensified cross-equatorial flow. 相似文献
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DING Yihui LI Chongyin HE Jinhai CHEN Longxun GAN Zijun QIAN Yongfu YAN Junyue WANG Dongxiao SHI Ping FANG Wendong XU Jianping LI Li 《Acta Meteorologica Sinica》2006,20(2):159-190
The SCSMEX is a joint atmospheric and oceanic experiment by international efforts, aiming at studying the onset, maintenance, and variability of the South China Sea (SCS) summer monsoon, thus improving the monsoon prediction in Southeast and East Asian regions. The field experiment carried out in May-August 1998 was fully successful, with a large amount of meteorological and oceanographic data acquired that have been used in four dimensional data assimilations by several countries, in order to improve their numerical simulations and prediction. These datasets are also widely used in the follow-up SCS and East Asian monsoon study. The present paper has summarized the main research results obtained by Chinese meteorologists which cover six aspects: (1) onset processes and mechanism of the SCS summer monsoon; (2) development of convection and mesoscale convective systems (MCSs) during the onset phase and their interaction with large-scale circulation; (3) low-frequency oscillation and teleconnection effect; (4) measurements of surface fluxes over the SCS and their relationship with the monsoon activity; (5) oceanic thermodynamic structures, circulation, and mesoscale eddies in the SCS during the summer monsoon and their relationship with ENSO events; and (6) numerical simulations of the SCS and East Asian monsoon. 相似文献
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东亚地区夏季风爆发过程 总被引：72，自引：5，他引：67
利用中国194站1961～1995年日降水资料及NCEP1979～1997年候格点降水资料,探讨了亚洲地区自春到夏的雨季开始分布。结果表明,东亚地区自春到夏存在副热带季风雨季开始和热带季风雨季开始。前者于4月初开始于华南北部和江南地区,随后向南和向西南扩展,于4月末扩展到华南沿海和中南半岛,这个雨带主要是冷空气和副热带高压西侧转向的SW风以及南亚地区冬春副热带南支西风槽中西风汇合而形成的,是副热带季风雨季开始。后者是南海热带季风爆发后使原来由江南移到华南沿岸的副热带季风雨带随副热带高压北进而北进,前汛期雨季进入盛期,江南出现第二次雨峰,形成梅雨期和江淮及华北雨季。同时,热带季风雨带也自东向西传播到达南亚地区而形成热带季风雨季。还讨论了1998年东亚地区夏季风爆发过程,指出南海夏季风爆发期的季风由副高北侧形成的新生气旋进入南海造成南海中部西风和南海越赤道气流转向的SW季风加强汇合而形成,因而是东亚季风系统中环流系统季节变化造成的,和印度季风无关。在南海季风爆发期阿拉伯海仍由副热带反气旋控制,南亚仍是上述副热带反气旋北侧NW风南下后转向的偏西副热带气流所控制,索马里低空急流仍未爆发,赤道西风并未影响南海。 相似文献
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本文计算、分析了1981年南海夏季风爆发前后华南地区平均的大气动力学和热力学结构,水汽和能量收支情况。分析表明,在季风爆发前后这些物理量场,特别是垂直运动场,都经历了一次明显的变化。南海夏季风的建立,是以副热带高压从南海东撒,越赤道气流北进为特征。它与以“爆发性涡旋”为开始,降水与西南气流同时开始的印度夏季风有所不同。另外,南海夏季风建立过程,主要变化发生在中、上层大气之中。这说明夏季风的建立,主要是大气环流季节性调整的结果,海陆差异需要有合适的大气环流配合才能产生明显的季风。对大气能量收支的分析表明,夏季风爆发前,华南地区主要是动能向总位能转换。所产生的总位能部分辐散到边界之外,部分消耗在对流层上层非绝热冷却过程之中,因而在对流层下部总位能才有稍明显的增长。夏季风爆发后,整个能量循环几乎相反。总位能大量转换为动能,以维持南海夏季风的增长。而整层大气中的非绝热加热以及总位能的辐合又补充了大气中总位能的损耗。潜热释放是夏季风爆发后大气的主要非绝热加热过程,它是南海夏季风维持,发展的主要能源。 相似文献