As global temperatures continue their inexorable rise, the intricate interactions between vegetation and the Earth’s atmospheric processes are coming under intense scientific scrutiny. A groundbreaking study by Li, Wang, Chen, and colleagues, soon to be published in Communications Earth & Environment, reveals a startling development: the control that vegetation exerts over terrestrial evapotranspiration is significantly weakening in a warmer world. This finding challenges long-held assumptions about the feedback mechanisms between the biosphere and the climate system and could profoundly reshape our understanding of future hydrological cycles and global water budgets.
Evapotranspiration, the combined process of water evaporation from land surfaces and transpiration by plants, is a cornerstone of the terrestrial water cycle. Vegetation modulates this process by regulating water loss through stomatal openings, facilitating soil moisture retention, and even impacting local and regional climate conditions through energy exchange with the atmosphere. Historically, robust vegetation cover has been considered a stabilizing force for evapotranspiration rates, buffering ecosystems and climates against variability. The new study, however, exposes how global warming is eroding this stabilizing influence in complex and consequential ways.
Using advanced climate-vegetation coupled models alongside extensive remote sensing data spanning multiple continents and decades, the research team systematically examined how evapotranspiration responds to rising temperatures, changing precipitation patterns, and shifting vegetation dynamics. Their analyses indicate a statistically significant decline in the sensitivity of evapotranspiration to vegetation density under warming scenarios. In other words, despite persistent or even increasing plant biomass in some regions, the capacity of vegetation to regulate water flux is diminishing, suggesting physiological and structural changes in plant communities that alter their water use efficiency and transpiration rates.
One key mechanism identified is the thermal stress placed on plant stomata, which regulate gas exchange and water loss. Higher temperatures cause increased vapor pressure deficits, leading plants to close their stomata more frequently to avoid excessive water loss, thereby reducing transpiration even when soil moisture may be sufficient. This physiological response decouples vegetation density from evapotranspiration, meaning that denser forests or grasslands no longer translate directly into higher evapotranspiration rates as they might have historically.
Furthermore, changes in species composition driven by climate change—such as shifts from deep-rooted trees to more drought-tolerant shrubs or grasses—affect the overall canopy conductance and water uptake strategies, contributing to alterations in evapotranspiration patterns. In some arid and semi-arid regions, vegetation expansion has actually led to decreased surface evaporation because the new plant types are less transpiring and more efficient at conserving water, upending traditional expectations about vegetation’s hydrological role.
The implications extend beyond local ecosystems. Since evapotranspiration contributes significantly to atmospheric moisture content that drives precipitation, a weakening vegetation control could disrupt feedback loops that regulate rainfall patterns, potentially exacerbating droughts in some regions while causing unpredictable precipitation surges elsewhere. This hydrological shift poses profound risks for agriculture, water resource management, and biodiversity conservation, particularly in areas already vulnerable to climate extremes.
Temperature-driven reduction in transpiration efficiency also affects energy balance at the land surface. Less transpiration means less latent heat flux, increasing sensible heat flux, which can lead to local warming and exacerbate heatwave severity. This phenomenon creates a vicious cycle where warming impairs vegetation’s cooling effect, thereby intensifying heat stress and further curtailing evapotranspiration.
In addition to temperature impacts, the study identifies altered soil moisture regimes as a contributing factor. Warming accelerates soil drying, limiting plant water availability and pushing ecosystems toward drought stress thresholds more frequently. Despite the maintenance or growth of canopy cover, the physiological capability of plants to transpire is compromised, undermining their traditional hydrological role.
The scientists caution that existing Earth system models may underestimate these processes, as many models assume stable vegetation-evapotranspiration relationships under climate change. Their findings call for urgent refinement of biosphere-atmosphere interaction modules to incorporate dynamic plant physiological responses and species composition changes to improve future climate projections.
One of the study’s most eye-opening conclusions is the spatial heterogeneity of this weakening control. Tropical rainforests, historically massive contributors to continental evapotranspiration, show marked sensitivity declines linked to episodic droughts and elevated temperatures. Meanwhile, boreal forests demonstrate complex interactions, where warming extends growing seasons but also increases drought vulnerability sporadically. Mid-latitude grasslands and savannas exhibit their own unique responses shaped by precipitation variability and land use changes.
The research also explores potential adaptive responses by vegetation but notes their limited capacity to counteract the overarching climate-driven constraints. For example, some species may evolve or acclimate to tolerate higher vapor pressure deficits, but the pace of climate change likely exceeds these adaptive windows, leaving significant portions of the global land surface in a state of hydrological imbalance.
Critically, the disjunction between vegetation cover and evapotranspiration efficiency could lead to overestimation of carbon-water feedback benefits that dense plant growth is expected to provide under warming scenarios. As transpiration drives nutrient cycling and energy transfer in ecosystems, its weakening might slow down biogeochemical cycles, affecting long-term ecosystem productivity and resilience.
This pioneering study underscores a paradigm shift in how scientists understand terrestrial water and energy dynamics in the Anthropocene. It reveals that simply preserving or expanding vegetation cover may not suffice for sustaining hydrological regulation or mitigating climate impacts. Targeted strategies that consider plant physiological stress, species turnover, and ecohydrological feedbacks are necessary for effective ecosystem management and climate adaptation.
In the broader context, these findings amplify the urgency of integrated climate policies that factor in ecohydrological vulnerabilities. Sustainable land management practices that enhance soil water retention, promote species diversity adaptable to heat and drought stress, and protect key hydrological contributors are imperative. Researchers argue for coordinated global monitoring systems capable of tracking real-time changes in evapotranspiration and vegetation health to inform adaptive responses.
As climate models embrace these nuanced biosphere-atmosphere interactions, policymakers and communities stand better equipped to anticipate and mitigate cascading effects on water security, food production, and ecosystem services. The weakened vegetation control on evapotranspiration delineated by Li and colleagues signifies both a scientific challenge and a clarion call to rethink the interface between life and climate on a rapidly warming planet.
In summary, the newly revealed weakening of vegetation’s influence on terrestrial evapotranspiration in a warming world disrupts conventional wisdom, unearthing complex ecological and climatic feedbacks. This profound insight not only enhances our mechanistic understanding of global hydrological cycles but also stresses the intricate vulnerabilities of Earth’s life-support systems in the face of relentless climate change. As scientists decode these evolving patterns, the integration of physiological, ecological, and climatological perspectives will be pivotal in charting resilient pathways forward for humanity and the biosphere.
Subject of Research: The influence of vegetation on global terrestrial evapotranspiration under climate warming and its implications for hydrological and ecological processes.
Article Title: Weakening vegetation control on global terrestrial evapotranspiration in a warmer world.
Article References:
Li, H., Wang, W., Chen, Z. et al. Weakening vegetation control on global terrestrial evapotranspiration in a warmer world. Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03372-8
Image Credits: AI Generated
DOI: 10.1038/s43247-026-03372-8
Keywords: climate change, evapotranspiration, vegetation control, terrestrial hydrology, global warming, water cycle, plant physiology, vapor pressure deficit, biogeochemical cycles, ecohydrological feedback
