Tree growth and water-use efficiency at the Himalayan fir treeline and lower altitudes: roles of climate warming and CO <sub>2</sub> fertilization

Abstract. Alpine forests are increasingly exposed to rising temperatures and intensified drought, potentially pushing species beyond their tolerance limits. However, the extent to which rising atmospheric CO2 (Ca) can mitigate these stressors by enhancing tree intrinsic water-use efficiency (iWUE) remains unclear. We investigated the growth and physiological responses of Himalayan fir (Abies spectabilis) using basal area increment (BAI) and δ13C data to track ecophysiological processes over recent decades along an altitudinal gradient in regions with hydrologically distinct regions on the Tibetan Plateau. Significant growth increases were observed at all altitudes in wet regions, while negative growth trends were noted at lower altitudes in dry regions. Climate–growth correlation analysis revealed that growth is primarily constrained by growing season temperatures and spring moisture availability. Tree iWUE increased over time at all altitudes, with a stronger increase in wet regions. Tree growth at lower altitudes in dry stands was negatively related to iWUE, whereas BAI in wet regions was positively associated with iWUE during the post-1965 period. Structural equation modeling indicated that temperature was a key driver of BAI and iWUE at all altitudes in wet regions, while temperature had negative effects on BAI at lower altitudes in dry regions. These results suggest that elevated Ca and temperature can stimulate tree growth in high-altitude forests in wet regions, but the positive effects do not compensate for the negative impacts of reduced water availability at lower altitudes in dry regions. Warming-induced drought stress may thus emerge as a more significant driver of growth compared to increasing Ca levels in comparable alpine forests. Our findings provide critical insights for refining assumptions about CO2 fertilization and climate change effects in ecophysiological models.

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Publication Details

Journal
Biogeosciences
Published
2025-09-26
DOI
https://doi.org/10.5194/bg-22-4993-2025
Citations
2
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
2.21

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article

Tree growth and water-use efficiency at the Himalayan fir treeline and lower altitudes: roles of climate warming and CO 2 fertilization

Xing Pu, Lixin Lyu
2 citations
Biogeosciences
Plant Water Relations and Carbon Dynamics
2.21
article

Tree growth and water-use efficiency at the Himalayan fir treeline and lower altitudes: roles of climate warming and CO 2 fertilization

Xing Pu, Lixin Lyu
article en
2 citations

Abstract

Abstract. Alpine forests are increasingly exposed to rising temperatures and intensified drought, potentially pushing species beyond their tolerance limits. However, the extent to which rising atmospheric CO2 (Ca) can mitigate these stressors by enhancing tree intrinsic water-use efficiency (iWUE) remains unclear. We investigated the growth and physiological responses of Himalayan fir (Abies spectabilis) using basal area increment (BAI) and δ13C data to track ecophysiological processes over recent decades along an altitudinal gradient in regions with hydrologically distinct regions on the Tibetan Plateau. Significant growth increases were observed at all altitudes in wet regions, while negative growth trends were noted at lower altitudes in dry regions. Climate–growth correlation analysis revealed that growth is primarily constrained by growing season temperatures and spring moisture availability. Tree iWUE increased over time at all altitudes, with a stronger increase in wet regions. Tree growth at lower altitudes in dry stands was negatively related to iWUE, whereas BAI in wet regions was positively associated with iWUE during the post-1965 period. Structural equation modeling indicated that temperature was a key driver of BAI and iWUE at all altitudes in wet regions, while temperature had negative effects on BAI at lower altitudes in dry regions. These results suggest that elevated Ca and temperature can stimulate tree growth in high-altitude forests in wet regions, but the positive effects do not compensate for the negative impacts of reduced water availability at lower altitudes in dry regions. Warming-induced drought stress may thus emerge as a more significant driver of growth compared to increasing Ca levels in comparable alpine forests. Our findings provide critical insights for refining assumptions about CO2 fertilization and climate change effects in ecophysiological models.

BiogeosciencesVol. 22(18)
China West Normal University (CN), Chinese Academy of Sciences (CN), Beijing Botanical Garden (CN), Institute of Botany (CN), China National Botanical Garden
National Natural Science Foundation of China
Openalex Percentile: Top 11%
Plant Water Relations and Carbon Dynamics
2.21
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