Preprints
https://doi.org/10.5194/egusphere-2026-241
https://doi.org/10.5194/egusphere-2026-241
04 Mar 2026
 | 04 Mar 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Saturation effect of background temperature and aridity on vegetation phenology sensitivity to urban warming

Zhang Zhenzhen, Zhang Yongqi, Cui Shufen, Sun Liheng, Lin Xingwen, Wu Chaofan, Zhang Zhaoyang, Chen Yuanjian, and Wen Quingqing

Abstract. In this study, urban warming effects on vegetation phenology were assessed for 293 cities in China. The variations in urban warming effects were expected to be attributed to the baseline land surface temperature (LST) and the aridity index (AI) of each locale. LST and AI related phenology and their temperature sensitivity (Rt-SOS and Rt-EOS) was quantified. We observed an urban-rural phenological disparity of 12.06 days for Start of Season (ΔSOS) and 9.86 days for End of Season (ΔEOS) among the studied cities. Spatially, cities in high latitude regions and coastal areas exhibited pronounced negative ΔSOS shifts and positive ΔEOS shifts, positively correlating with Rt-SOS and Rt-EOS, respectively. Employing a continent-wide preseason temperature (T), we observed a logistic decrease for SOS and an increase for EOS, illustrating the "saturated effect" of warming on plant phenology-patterns echoed within urban settings. First-order derivatives of those logistic curves identified a highest phenological sensitivity at T=4°C and T=6°C, as well as the warming benefit range of 3.5°C10°C and 2°C14°C for SOS and EOS respectively. Substituting T with LST, weaker ΔSOS and ΔEOS would be presented in warmer regions only when LST exceeded 12.5°C and 4°C for spring and autumn, respectively. Except for LST, AI exhibited a positive correlation with ΔSOS and ΔRt-SOS, but a negative one with ΔEOS and ΔRt-EOS. Collectively, LST and AI explained 75.05% and 76.21% of the phenological variance across the continent for ΔSOS and ΔEOS, respectively. These findings lay the groundwork for predicting vegetation changes under global warming at large scales.

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Zhang Zhenzhen, Zhang Yongqi, Cui Shufen, Sun Liheng, Lin Xingwen, Wu Chaofan, Zhang Zhaoyang, Chen Yuanjian, and Wen Quingqing

Status: open (until 23 Apr 2026)

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Zhang Zhenzhen, Zhang Yongqi, Cui Shufen, Sun Liheng, Lin Xingwen, Wu Chaofan, Zhang Zhaoyang, Chen Yuanjian, and Wen Quingqing
Zhang Zhenzhen, Zhang Yongqi, Cui Shufen, Sun Liheng, Lin Xingwen, Wu Chaofan, Zhang Zhaoyang, Chen Yuanjian, and Wen Quingqing

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Short summary
We wanted to know how city warming affects when plants start/stop growing—this helps prepare for ecosystem shifts amid global warming. We studied 293 Chinese cities, analyzing how local surface temperatures and dryness shape these timelines. In cities, plants start ~12 days earlier and stop ~10 days later than rural areas; extreme heat lessens this effect. Local temperature/dryness explain most differences. These results help predict plant changes, supporting natural system protection.
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