Interdecadal Variation of Spring Extreme High-Temperature Events in the Western Tianshan Mountains and Its Relationship with the Tropical SST

<div>(a) The difference in the spring average zonal circulation (vectors) and vertical velocity (shaded areas; Pa·s<sup>−1</sup>) averaged within 25°N–35°N, and (b) the difference in meridional circulation (vectors) and vertical velocity (shaded areas; Pa·s<sup>−1</sup>) averaged within 60°E–75°E between P2 and P1 periods.</div>

Advances in Meteorology

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Figure 6

Figure 6: Interdecadal Variation of Spring Extreme High-Temperature Events in the Western Tianshan Mountains and Its Relationship with the Tropical SST 

Figure 6 | Interdecadal Variation of Spring Extreme High-Temperature Events in the Western Tianshan Mountains and Its Relationship with the Tropical SST 