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- 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;
- Climatic Features of SCS Summer Monsoon Onset and Its Possible Mechanism 南海夏季风建立的气候特征及其机制的讨论
- AIR-SEA HEAT FLUX EXCHANGE FEATURE OVER THE SOUTH CHINA SEA BEFORE AND AFTER THE SCS SUMMER MONSOON ONSET 南海夏季风爆发前后海-气界面热交换特征
- Characteristics of Convection Activities over Sumatra Area and Its Relationship with SCS Summer Monsoon Onset 苏门答腊地区对流活动及其与南海夏季风建立的关系
- NUMERICAL SIMULATION EXPERIMENTS OF THE IMPACTS OF LOCAL SEA-LAND THERMODYNAMIC CONTRASTS ON THE SCS SUMMER MONSOON ONSET 局地海陆热力对比对南海夏季风爆发影响的数值试验
- SCS summer monsoon onset 南海夏季风爆发
- 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。
- The results show that onset time of SCS summer monsoon is significantly negative related with its intensity. 结果表明：南海夏季风爆发日期和强度指数呈显著的反相关；
- Climatic tendency for 50-year manifests that the onset date of SCS summer monsoon gradually gets delayed and its intensity gets weak. 50年来的气候趋势是，爆发日期逐渐偏晚，强度指数逐渐减弱。
- South China Sea (SCS) summer monsoon onset in the 4th pentad of May 2004, it's close to normal year. 2003年南海夏季风首先于5月第5候在南海南部建立，在南部维持1-2候后向北推进，6月第1候全面爆发。
- 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。
- However, the correlation of SSTA over the East Pacific with SCS summer monsoon intensity index is negative before onset, but after onset their correlation become positive. 东太平洋海温异常在南海夏季风爆发之前，与强度指数反相关，而爆发之后，与强度指数正相关。
- These reflect that SCS summer monsoon activities have close relationships with ENSO events. 这体现了南海夏季风活动与ENSO事件的密切关系。
- 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。
- Zhou Bing, He Jinhai, Wu Guoxiong, et al.Discussion on choices of East Asian subtropical monsoon indices.In: He Jinhai, ed.Dates of Summer Monsoon Onset in the South China Sea and Monsoon Indices.Beijing: Chinese Meteorological Press,2001. 周兵,何金海,吴国雄等。关于东亚副热带季风指数选择的讨论。见:何金海等主编。南海夏季风建立日期的确定与季风指数。北京:气象出版社,2001。
- The results show that before the summer monsoon onset, the air-sea heat exchange near Xisha area is weak, the vapor flux is small and the main trend is that the ocean is being heated; while after its onset, the air-sea heat exchange is balanced roughly. 结果表明：季风爆发前，西沙海气界面热量交换较弱，水汽通量较小，以海洋获得热量为主；季风爆发后，海气界面热量交换接近平衡。
- Impact of the Convection over the Indo-China Peninsula on the Onset of SCS Summer Monsoon 中南半岛对流对南海夏季风建立过程的影响
- EOF EXPANSION OF SUMMER MONSOON ONSET OVER THE SOUTH CHINA SEA 南海夏季风爆发的EOF分析
- On the Process of Summer Monsoon Onset over East Asia 东亚地区夏季风爆发过程
- Heavy rains occur during a summer monsoon. 暴雨出现在一个夏季季风期
