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从图 3 （给出了采样期间后向气流轨 迹的计算结果）可看出 2017
从图 3 （给出了采样期间后向气流轨 迹的计算结果）可看出 2017 年秋季长春市的气团 主要来源于西北和西南方向，可能由于长春市位于 长白山脉的西北方向，东南方向的气团被长白山拦 截．
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From Figure 3 (the results of the calculating backward flow route from a sampling period) can be seen in the fall of 2017, the air mass mainly from Changchun northwest and southwest directions, may be due to the northwest direction Changchun Changbai the air mass southeast Changbai Mountain was blocked.
正在翻译中..
From Figure 3 (the calculation of the backward air flow track during sampling period) it can be seen that the air mass in Changchun City in autumn 2017 mainly originated in the northwest and southwest direction, possibly due to changchun city is located in the northwest direction of the Changbai Mountains, the air mass in the southeast direction was stopped by Changbai Mountain.
正在翻译中..
It can be seen from Figure 3 (the calculation results of the backward airflow path during the sampling period are given) that in autumn 2017, the air mass of Changchun City mainly came from the northwest and southwest directions. It may be because Changchun City is located in the northwest direction of Changbai Mountains, and the air mass in the southeast direction was intercepted by Changbai Mountains
正在翻译中..
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