1) deep convective system
深对流系统
1.
Although potential vorticity is a common and useful physical quantity for meteorological analysis,it is a little weak in deep convective systems due to the apparent slant of moist isentropic surfaces.
位涡在诊断分析中是一个常用且有效的物理量,但在深对流系统中由于湿等熵面的倾斜变得较弱。
2) Deep moist MCS
中尺度深湿对流系统
3) deep MCS
中尺度深对流系统
4) convection system
对流系统
1.
The definition of spatial chaos for convection system with a forced term;
带强迫项对流系统的空间混沌定义
6) deep convection
深对流
1.
Based on FY-2C hourly infrared T_(BB) dataset from June to August in 2007,the distribution and spatiotemporal variations of deep convection over China and its vicinity during the summer of 2007 is analyzed and compared with the atmospheric circulation background based on the NCEP final analysis dataset and the climatological distribution of deep convection based on 10-year T_(BB) dataset.
利用逐时FY-2C卫星红外亮温(T_(BB))资料讨论了2007年夏季(6—8月)我国深对流活动的时空演变特征,并同10年的深对流活动特征进行了对比分析。
补充资料：对流型地热系统
对流型地热系统
convective geothermal system
对流型地热系统(eonveetive geothermalsystem)对流是指流体各部分发生相对位移而引起的热量交换。对流现象只在流体(气体或液体)中出台湾有高温地热系统18个，发电潜力10。一500MW。 (任湘)
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条