Simulation of a torrential rainstorm in Xinjiang and gravity wave analysis<xref rid="cpb_27_5_059201_fn1" ref-type="fn">*</xref><fn id="cpb_27_5_059201_fn1"><label>*</label><p>Project supported by China Special Fund for Meteorological Research in the Public Interest (Grant No. GYHY201406002), the National Natural Science Foundation of China (Grant Nos. 41575065 and 41405049), the National Natural Science Foundation International Cooperation Project, China (Grant No. 41661144024), and Strategic Priority Research Program of Chinese Academy of Sciences (Grant No. XDA17010100).</p></fn>

Simulation of a torrential rainstorm in Xinjiang and gravity wave analysis**

Project supported by China Special Fund for Meteorological Research in the Public Interest (Grant No. GYHY201406002), the National Natural Science Foundation of China (Grant Nos. 41575065 and 41405049), the National Natural Science Foundation International Cooperation Project, China (Grant No. 41661144024), and Strategic Priority Research Program of Chinese Academy of Sciences (Grant No. XDA17010100).

Yang Rui^{1, 2}, Liu Yi¹, Ran Ling-Kun^{1, †}, Zhang Yu-Li¹

Power spectrum density (m²·s⁻²) of the vertical velocity at an altitude of 19 km along the line shown in Fig. 4(a). Solid lines represent the wave phase velocities of −5 m/s, −10 m/s, and −25 m/s.