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1)  east airflow
偏东气流
1.
The results show that although lack of the high and low configuration and Mid-latitude and low-latitude interaction on the weather situation,however the east airflow of long-range typhoon periphery provided abundant water vapor and instability in energy.
但是远距离台风外围偏东气流本身的暖湿特征提供了丰沛水汽和不稳定能量;与低层西南气流形成的辐合加强了低层的上升运动,提供了降雨所需的动力条件。
2)  eastward back-flow
偏东回流
3)  a south-easterly air flow
东南气流.
4)  easterly flow
东风气流
1.
The first strong precipitation is caused by strengthening local convective clouds generated in the subtropical high,vapor transportation and dynamic conditions offered by strengthened easterly flow in bottom of the troposphere air promote the development of convection;New clouds in the humid air environment will be rapidly strengthened and developed.
通过对常规气象资料分析,发现①第一时段的强降水由副热带高压内部产生的局地对流云团加强造成,对流层底层东风气流的加强提供的水汽输送和动力抬升作用,促进了对流发展;②新生云团进入潮湿的大气环境中能够得到迅速的发展加强。
2.
The first strong precipitation is caused by strengthening local convective cluster generated in the subtropical high,the vapor transportation and dynamic conditions offered by strengthened easterly flow in bottom of the troposphere air promote the development of convection;new cluster in the humid air environment will be rapidly strengthened and developed.
通过对常规气象资料分析发现:第一时段的强降水由副热带高压内部产生的局地对流云团加强造成,对流层底层东风气流的加强提供的水汽输送和动力抬升作用,促进了对流发展;新生云团进入潮湿的大气环境中能够得到迅速的发展。
5)  northeast flow
东北气流
6)  Air deviation
空气偏流
补充资料:东偏小室去日最远每逃暑之地戏作五字
【诗文】:
肃肃檐阴转,泠泠笕水鸣。
高墉日气远,方簟午风清。
渴爱餐浆美,慵便葛屦轻。
新秋忽在眼,结束问山程。



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