摘要
根据日本GMS资料和部分常规资料,对我国南方地区春末夏初的10个中尺度对流复合体(MCCS)做了分析。它们的基本特征与美国MCC相近,它们主要活动在夜间,一般在山地背风一侧斜坡上或坡底附近形成;并在对流层中低层中低纬度地区几个天气系统的迭加处获得发展;向东们南方向移动,与700~500hPa之间的平均气流方向大体一致,冷云罩面积约为1.4×10 ̄5km ̄2,比美洲的(2~3×10 ̄5km ̄2)略小;持续时间为12小时左右,比美洲的(10小时)稍长。云区形状呈椭圆形,但伤心率≥0.6.云顶最低温度一般在一86℃以下,出现在冷云罩面积达到最大之前4~6小时。
Ten mesoscale convective complexes(MCCs ) over the southern China mainlandduring late spring and early summer were computed and analysed using GMS S-VISSRdata and conventional data.The results show that they are nocturnal and initiate atslope or near slope bottom of plateau or mountains leeward , and develop at the specialfavorable area where several synoptic systems from low-and midlatitude are merging orinteracting with each other.They move toward east by south and tend to the mean flowin 700~500hPa layer.The coldcloud-shield is about 1.4 × 10 ̄5km ̄2, which is smallerthan that of MCC in the America (2~3× 10 ̄5km ̄2),but it lasts for about 12 hours whilethe American shield about 10 h0urs. The eccentricity of cloud shape(≥0.6) is slightlysmaller than that in the America(≥0.7).The minimum temperature of cloud top isgenerally colder than一86℃,which appears 4~6hours earlier than the time of themaximum coldDcloudDshield extent.
出处
《应用气象学报》
CSCD
北大核心
1995年第1期9-17,共9页
Journal of Applied Meteorological Science
基金
"85-906-08-05"课题
关键词
中尺度
对流复合体
冷云罩
中国
南方地区
The southern China mainland
Mesoscale convective complexes(MCCs)
Cold-cloud-shild.