1) Q vector divergence
Q矢量散度
1.
Using NCEP 1°× 1°reanalyzed data, a heavy rain process occurred in south seacoast of Zhejiang province caused by the eastly wave on August 3～4 in 2001 was analyzed, including its evolution and the cause of cyclonic vortex emerged by the eastly wave with Q vector divergence.
根据Q矢量散度分析讨论了这次过程中的暴雨演变以及东风波诱生中尺度低涡发生发展的原因。
2) Q-vector divergence
Q矢量散度
1.
Diagnosis fields such as 850 hPaQ-vector divergence and frontgenesis function in 11 torrential rain cases are analyzed, disclosing the distribution characteristics of Q-vector divergence field and frontgenesis function field, as well as the space-time relationship between the main weather system on the middle and low layers in troposphere and belt of torrential rain.
应用 Q矢量理论对 1998年广西 6月 16～ 2 6日连续性暴雨过程进行诊断分析 ,共分析了 11个时次的 85 0h Pa Q矢量散度、锋生函数等诊断场 ,揭示了广西“98。
3) front of Q vector divergence
Q矢量散度梯度
4) wet Q vector divergence field
湿Q矢量散度场
5) wet Q vector divergence
湿Q矢量散度
6) Precipitation amount forced by Q vector divergence
Q矢量散度强迫产生的降水量
补充资料：矢量
即“向量①”(51页)。
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