Overall, there was an increasing trend in the PRE during 2003–2022 (2.17 mm/yr) ( Figure 3A ).
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Precipitation controls the time-lag and cumulative effects of hydrothermal factors on the end of the growing season in a semi-arid region of China.
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The PRE during 2003–2011 showed a decreasing trend (−3.83 mm/yr) ( Figure 3B ), while the PRE during 2011–2022 exhibited an increasing trend (2.77 mm/yr) ( Figure 3C ).