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- The main results are obtained as follow: the pre-flood season in South China is composed of the frontal precipitation period and the summer monsoon precipitation period. 分析发现,华南前汛期降水由锋面降水和夏季风降水两个时段组成。
- Heavy rains occur during a summer monsoon. 暴雨出现在一个夏季季风期
- Summer monsoon precipitation 季风降水
- This implies that increased precipitation from a strong summer monsoon triggered glacier advances in the Himalaya during interglacial times. 因此,这一区域的高山冰川回应夏天季风强度的变化。
- On May 17th, the precipitation of SCS changes abruptly, the regional averaged precipitation increases and exceeds 6 mm/day, which indicates the onset of SCS summer monsoon. 突变检验表明,5月17日,南海SCS4区降水发生明显的突变,与5月15日相比,SCS4区降水场形势发生明显变化,其区域平均降水突增超过6 mm/day,标志着南海夏季风降水的爆发。
- The effects of sulfate aerosols over China on East Asian summer monsoon and precipitation were investigated using the latest version of general circulation model (GCM) CAM3. 0模式离线耦合一个气溶胶同化系统,模拟研究了中国区域硫酸盐气溶胶的直接气候效应对东亚夏季风及其降水的影响。
- Impact of Indochina Deforestation on the East Asian Summer Monsoon. 印度支那半岛采伐森林对东亚夏季风的作用。
- Further dynamic analysis reveals the dynamic mechanism for the late occurrence of ASM precipitation in Indian monsoon area and the abrupt occurrence of Indian summer monsoon onset. 通过进一步的诊断,揭示了亚洲夏季风降水在印度季风区出现较晚以及印度夏季风爆发的动力机制。
- The Arctic oscillation was close related with the frequency of blocking high over the Baikal Lake area and the intensity of East Asian summer monsoon and summer precipitation over North China. 在年代际尺度上,北极涛动与贝加尔湖地区阻塞高压发生频率、东亚夏季风强度和华北夏季降水的关系较为密切。
- By use of the SCSMEX situ observational precipitation and NCEP/NCAR reanalysis data sets, this study discussed the low frequency (LF) variational characteristics of the East Asian summer monsoon circulation (EASMC) with EOF and MSSA analysis methods. 利用1998年SCSMEX试验期降水观测资料和NCEP/NCAR再分析资料, 将物理量场在降水EOF分析得到的时间系数上展开,分析东亚夏季风环流低频变化特征。
- The paper concerns low-frequency summer monsoon in the Southern Hemisphere. 本文是研究南半球低频夏季风的。
- For example, Ana Barros of Duke University has been leading a multi-institutional study aimed at defining monsoon precipitation patterns in the Annapurna range since 1999. 例如,杜克大学的巴罗士(AnaBarros)带领一个多机构合作的研究计画,自1999年开始致力于确立安纳布尔纳峰地区的季风降雨型态。
- Results show that SCS summer monsoon onset is enhanced with its LFO. 结果表明,南海夏季风的低频振荡对南海夏季风的爆发具有加强的作用;
- Numerical results also indicate that: the development of cumulus convection, triggered by the SCS cold surge,is a fundamental factor in forming the strong monsoon precipitation and low-level stationary disturbances over indonesia and Borneo. 数值研究还指出; 印尼加里曼丹的强季风降水及常驻性低层扰动形成的基本因子是南海冷涌所触发的积云对流发展。
- It is indicated that the variation of deuterium excess is accordant with that of the relative humidity over the western Arabian Sea,which suggests that the vapor for monsoon precipitation in New Delhi originates mainly from the western Arabian Sea. 结合西阿拉伯海风速和印度西北地区季风降水量资料分析结果;认为西阿拉伯海是新德里季风水汽的主要来源.
- About 70% of the total rainfall as heavy downpour in the summer monsoon months and 30% in winter. 夏季季风季节的暴雨占总降雨量的70%25,冬季占30%25。
- The mechanism of the effect on the South China Sea summer monsoon of the Indo-China Peninsula is also discussed. 同时还就中南半岛影响南海夏季风建立和维持的机制进行了讨论。
- Winter monsoon normally blows from the north or from the east while summer monsoon typically blows from the southwest. 冬季季候风一般从北面或东面吹来,而夏季季候风则主要是西南风。
- The West African Monsoon Dynamics. Part II: The Preonset and Onset of the Summer Monsoon. 西非季风动力学,第二部分:夏季风提前爆发和爆发。
- Furthermore, the heat storage anomaly of December in the SCS can be used as a predictor for the onset of the SCS summer monsoon. 进一步分析还发现,南海12月份热含量异常可以作为南海夏季风爆发的一种预报指标。