The earliest onset of the Asian summer monsoon occurs in early to middle May over the South China Sea.This onset is signified by the development of low-level westerlies and leads to heavy convective rainfall oversouthern China (pre-Mei-Yu). In June, low-level westerly surges over the northern South China Sea are associatedwith the Mei-Yu rainfall system in the Yangtze region and southern Japan. In this work, the ECMWFdata for 1981-86 are used to study the tropical circulations associated with the development of low-levelwesterlies during both events.Composites of horizontal wind, geopotential height, moisture, and vertical velocity during six May onsets andnine lune surges, respectively, indicate that both events occur with the approach of a midlatitude trough-frontsystem. The possible triggering of the South China Sea summer monsoon onset by the midlatitude system mayexplain why the South China Sea onset occurs prior to other regions of the Asian monsoon. During boreal spring,this is the only Asian monsoon region where midlatitude fronts can move into the Tropics without having toovercome significant terrain barriers.Following the two events, opposite teleconnection-like patterns develop in the Tropics in both hemispheres.During the May onsets, the arrival of the midlatitude trough/front appears to lead to a southwestward extensionof a cyclogenesis zone into the equatorial Indian Ocean. Along this zone, cyclonic vortices develop over theAndaman Sea, the Bay of Bengal, and perhaps the southern equatorial Indian Ocean, and increased deep convectionis indicated by the OLR composites. During the June surges, a pair of anticyclones develop straddlingthe equator at the longitudes of Indochina. This anticyclonic couplet is associated with decreased deep convectionand propagates westward to dominate the flow changes over the Bay of Bengal and the southern Indian Ocean.The steady 4-5 m S-I westward speed and near-perfect symmetry with respect to the equator indicate thepossibility of an equatorial Rossby wave generation in conjunction with the June westerly surges in the northernSouth China Sea.
展开▼
机译:亚洲夏季风最早发生在5月初至中海南海,这是由低空西风的发展所预示的,并导致中国南部(梅雨前)的强对流降雨。 6月,南中国海北部的低空西风潮与扬子地区和日本南部的梅雨雨系统有关。在这项工作中,使用1981-86年的ECMWF数据研究了这两个事件期间与低层西风发展相关的热带环流。5月6次发作和9月的暴风潮期间水平风,地势高度,湿度和垂直速度的合成,分别表明这两个事件都发生在中纬度海盆前线系统附近。中纬度系统可能引发南海夏季风爆发,可能解释了为什么南海爆发先于亚洲季风的其他区域。在寒冬期间,这是亚洲唯一的季风地区,中纬度锋面可以进入热带而不必克服明显的地形障碍。在这两个事件之后,两个半球在热带地区形成了相反的遥相关样模式。中纬度槽/前缘的到来似乎导致回旋区向西南延伸到赤道印度洋。沿着该区域,气旋涡在安达曼海,孟加拉湾,甚至是赤道南部印度洋上发展,OLR合成物表明深对流增加。在六月的海浪期间,一对反气旋在印度支那的经度上横越赤道。这种反气旋对联与深度对流减少有关,并向西传播,主导了孟加拉湾和印度洋南部的流量变化。稳定的西移4-5 m SI和相对于赤道的近乎完美的对称性说明了可能赤道的罗斯比波的产生以及南海北部地区六月的西风潮。
展开▼