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Process-Based Modelling of Vegetation-Climate Synergies Driving Evapotranspiration Dynamics in Karst Ecosystems 喀斯特生态系统植被-气候协同作用驱动蒸散动力学的过程模拟
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-15 DOI: 10.1002/eco.70176
Guikai Sun, Zhong Cheng, Ruifeng Song, Yujie Shao, Junqi Huang, Chongxun Mo, Yunchuan Yang, Mingquan Li

Evapotranspiration (ET), a critical element of regional hydrological cycles and energy balances, connects terrestrial ecological and hydrological processes in karst ecosystems. Following large-scale ecological restoration, Guangxi's significant vegetation changes have altered regional energy-water dynamics via enhanced ET. This study applied a process-based PT-JPL model with locally optimized parameters to quantify ET dynamics and vegetation change impacts in Guangxi (2001–2018). Using the Geodetector method, we investigated single-factor controls and synergistic interactions between vegetation/climate drivers. The results of this study showed that the parameter-optimized PT-JPL model has good accuracy in Guangxi. The actual ET of Guangxi showed an increasing trend with a rate of 3.5 mm a−1 from 2001 to 2018. The changes in vegetation significantly increased regional ET in Guangxi. The average annual ET under vegetation changes was 7.4 mm higher than that under constant vegetation compared to no change in vegetation. The changes in ET are not the effect of the influencing factor alone but the synergistic effect of influencing factors. The synergistic effect of Rad and LAI on ET was found to be very significant using the Geodetector's interactive detector.

蒸散发(Evapotranspiration, ET)是区域水循环和能量平衡的关键要素,它连接着喀斯特生态系统的陆地生态和水文过程。在大规模生态恢复后,广西植被的显著变化通过增强的ET改变了区域能量-水动态。本研究采用基于过程的PT-JPL模型和局部优化参数,量化了2001-2018年广西ET动态和植被变化的影响。利用Geodetector方法,我们研究了植被/气候驱动因子之间的单因素控制和协同作用。研究结果表明,参数优化后的PT-JPL模型在广西具有较好的精度。2001 - 2018年广西实际蒸散发呈增加趋势,速率为3.5 mm a−1。植被变化显著增加了广西区域ET。植被变化条件下的年平均ET比植被不变条件下的年平均ET高7.4 mm。ET的变化不是单个影响因素的作用,而是各影响因素的协同作用。利用Geodetector的交互探测器发现,Rad和LAI对ET的协同效应非常显著。
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引用次数: 0
Groundwater Changes the Climate Niche of an Amazonian Mound-Building Termite 地下水改变亚马逊土墩白蚁的气候生态位
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-12 DOI: 10.1002/eco.70175
Pedro Aurélio Costa Lima Pequeno

Rainfall is a major dimension of species climate niches. It has been proposed that groundwater can change species responses to rainfall by creating ‘hydrological refugia’ under a drier climate. However, the available evidence is conflicting and biased towards plants. This study tested whether shallow water tables (< 5 m deep) provide hydrological refugia to the Amazonian mound-building termite, Amitermes excellens. This termite builds mounds up to 4 m tall in the Lavrado, the largest continuous savanna in northern Amazonia. Google Street View was used to remotely survey A. excellens mounds in 131 sites along a road network covering the study region (~795 km). For each site, published products on environmental and land use variables were also obtained. Mound abundance was modelled as a function of an interaction between mean water table depth and mean annual rainfall, while accounting for other factors. The analysis showed that mound abundance was higher on sandier soils and inside Indigenous lands but decreased with fire frequency and the Normalized Difference Vegetation Index. After accounting for these effects, a climate–groundwater interaction was found: Mound abundance increased with annual rainfall over deeper water tables but was consistently low over shallow water tables regardless of rainfall. Thus, groundwater can drastically change the realized climate niche of both plants and animals. However, shallow groundwater need not provide hydrological refugia under drier climates. Given that termites concentrate much of the terrestrial animal biomass and are major detritivores in the tropics, climate–groundwater interactions may have neglected impacts on global biogeochemical cycles.

降雨是物种气候生态位的一个主要维度。有人提出,地下水可以通过在干燥气候下创造“水文避难所”来改变物种对降雨的反应。然而,现有的证据是相互矛盾的,并且偏向于植物。本研究测试了浅水层(5米深)是否为亚马逊土墩白蚁Amitermes excellens提供了水文避难所。这只白蚁在亚马逊北部最大的连续稀树草原Lavrado建造高达4米的土丘。利用谷歌街景对覆盖研究区(~795 km)的131个站点的a . excellens土丘进行了远程调查。对于每个站点,还获得了关于环境和土地利用变量的公布产品。在考虑其他因素的同时,将土丘丰度建模为平均地下水位深度和年平均降雨量之间相互作用的函数。分析表明,沙质土壤和土着土地上的土丘丰度较高,但随着火灾频率和归一化植被指数的变化而降低。在考虑了这些影响之后,发现了气候-地下水的相互作用:土丘丰度随着年降雨量的增加而增加,但无论降雨量如何,浅水面的土丘丰度一直很低。因此,地下水可以极大地改变植物和动物已实现的气候生态位。然而,在干旱气候下,浅层地下水不需要提供水文避难所。考虑到白蚁集中了大部分陆生动物生物量,并且是热带地区的主要营养动物,气候-地下水相互作用可能忽略了对全球生物地球化学循环的影响。
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引用次数: 0
Environmental Drivers of Fish Taxonomic Distinctness and Functional Diversity in a Tropical River Basin 热带河流流域鱼类分类特征和功能多样性的环境驱动因素
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-09 DOI: 10.1002/eco.70165
Arvind Kumar Dwivedi, Kritish De

Biodiversity studies have traditionally focused on species rank, yet recent research highlights the inadequacy of this approach alone. Instead, scientists emphasise taxonomic and functional surrogacy methods, such as indices of taxonomic distinctness and functional diversity, to grasp the relationships among species and their functional characteristics within ecosystems. Despite being a significant river in the Deccan Plateau region, understanding of the taxonomic distinctiveness and functional diversity of the fish community of the Bhima River basin remains elusive. Thus, we conducted this study to understand the relationship between these indices and environmental drivers affecting the fish community in the Bhima River basin. We studied taxonomic distinctness (Δ+), variation in taxonomic distinctness (λ+), functional dispersion (FDis), functional divergence (FDiv) and functional evenness (FEve) of the fish community. By correlation and regression analyses, we found a significant association between taxonomic distinctness and functional diversity indices. We also found that these indices are mainly influenced by annual temperature range, mean temperature diurnal range and precipitation of the dry season. We recommend conducting a comprehensive assessment of fish populations and studying the potential effects of climate change on fish diversity to improve understanding of their distribution in the Bhima River basin.

传统上,生物多样性研究的重点是物种等级,但最近的研究强调了这种方法的不足。相反,科学家们强调分类学和功能替代方法,如分类学独特性和功能多样性指数,以掌握生态系统中物种之间的关系及其功能特征。尽管比马河是德干高原地区的一条重要河流,但对比马河流域鱼类群落的分类特征和功能多样性的了解仍然难以实现。因此,本研究旨在了解这些指标与影响碧马河流域鱼类群落的环境驱动因素之间的关系。我们研究了鱼类群落的分类独特性(Δ+)、分类独特性变异(λ+)、功能分散度(FDis)、功能发散度(FDiv)和功能均匀度(FEve)。通过相关分析和回归分析,我们发现分类独特性与功能多样性指数之间存在显著的相关性。这些指标主要受年气温变化幅度、平均气温日变化幅度和旱季降水的影响。我们建议对鱼类种群进行全面评估,并研究气候变化对鱼类多样性的潜在影响,以提高对比马河流域鱼类分布的认识。
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引用次数: 0
California Trees Seasonally Use Augmented Water Sources: Water Isotope Tracking in a Groundwater-Dependent Ecosystem 加利福尼亚树木季节性地使用增加的水源:地下水依赖生态系统中的水同位素跟踪
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-08 DOI: 10.1002/eco.70166
Jory Chapin Lerback, Erik Oerter, Ate Visser, A. Jake Harm

Sustainable groundwater management must account for the needs of groundwater dependent ecosystems. To understand the relationship of ecosystems and seasonal water use, we studied the stable isotope composition (δ18O and δ2H) of water in streamside trees in a semi-arid streamside environment (Livermore, California, USA). We sampled seven trees at two sites every other month from April 2024 through April 2025 for tree xylem stable water isotope signatures. These data were compared to potential source waters: precipitation, imported surface water, soil water and regional groundwaters. Large daily precipitation events were found to be isotopically similar to regional groundwater and were thus treated as one water source. A Bayesian mixing model using stable water isotopes was used to determine the ratios of these three potential source waters (small daily precipitation events, groundwater/large daily precipitation events and imported water) present in tree xylem water. On average, tree water sources include 32% imported water (SD = 9%), 35% small daily precipitation events (SD = 10%) and 33% groundwater (SD = 3%), with significant seasonal variation (tsummer-winter = 30.8, p < 0.01), particularly drawing more imported water (more than 55%) in the summer. While small daily precipitation events contribute only 10% of the total precipitation in our dataset, it represents a third of water used by trees. In addition, while these ecosystems are designated as groundwater dependent ecosystems, the trees use approximately one third imported water and even more during dry summer months. This approach provides water managers with a practical tool for quantifying ecosystem water needs, supporting data-driven decisions and regulatory compliance. While California's Sustainable Groundwater Management Act emphasizes supporting groundwater dependent ecosystems, it allows flexibility in demonstrating benefits. Our methodology provides a way to document that management actions (such as managed aquifer recharge with imported water) deliver measurable co-benefits to GDEs.

可持续的地下水管理必须考虑到依赖地下水的生态系统的需要。为了了解生态系统与季节水分利用的关系,我们研究了半干旱河滨环境(美国加利福尼亚州利弗莫尔)河滨树木水分的稳定同位素组成(δ18O和δ2H)。从2024年4月到2025年4月,我们每隔一个月在两个地点采样7棵树,以获取树木木质部稳定水同位素特征。这些数据与潜在水源:降水、进口地表水、土壤水和区域地下水进行了比较。发现大的日降水事件在同位素上与区域地下水相似,因此被视为一个水源。利用稳定水同位素建立贝叶斯混合模型,确定了木质部水中这三种潜在水源(小日降水事件、地下水/大日降水事件和进口水)的比例。树木水源平均包括32%的进口水源(SD = 9%)、35%的日小降水事件(SD = 10%)和33%的地下水(SD = 3%),且具有显著的季节变化(夏冬= 30.8,p < 0.01),特别是夏季吸收更多的进口水源(超过55%)。虽然小的日降水事件只占我们数据集中总降水的10%,但它代表了树木使用的水的三分之一。此外,虽然这些生态系统被指定为依赖地下水的生态系统,但树木使用大约三分之一的进口水,在干旱的夏季甚至更多。这种方法为水资源管理者提供了一种实用的工具,用于量化生态系统的水需求,支持数据驱动的决策和法规遵从。虽然加州的《可持续地下水管理法》强调支持依赖地下水的生态系统,但它允许灵活地展示效益。我们的方法提供了一种记录管理行动(例如用进口水管理含水层补给)为gde带来可衡量的协同效益的方法。
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引用次数: 0
Life on the Edge: Ecosystem Features of Lakes Across a Mountain–Prairie Elevation Gradient in Western Canada 边缘上的生命:加拿大西部山脉-草原海拔梯度湖泊的生态系统特征
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-07 DOI: 10.1002/eco.70148
Paola Ayala-Borda, Jean-François Lapierre, Milla Rautio, Sarah Ellen Johnston, Matthew J. Bogard

Ecological transition zones such as mountain elevation gradients can influence the function and productivity of lakes through changes in climatic characteristics and catchment composition (i.e., land use/land cover). However, surveys of limnological features along such ecological transition zones show variable patterns, making it difficult to extrapolate past results to regions such as the eastern slopes of the Canadian Rocky Mountains. To test the effect of elevation and gradients of environmental variability across such an ecological transition zone, we sampled 11 lakes spanning a 600 m elevation gradient between the prairies and Montane Cordillera of southwest Alberta. We analysed the catchment composition, water chemistry, lake metabolic rates (based on oxygen isotopic analysis), dissolved organic matter (DOM) composition, and zooplankton community composition and diet based on fatty acid analysis. Changes in catchment composition and water temperature along the elevation gradient were not clearly linked to DOM content or composition. Most lakes were autotrophic in summer. ERrates of gross primary production (GPP) and ecosystem respiration (ER) shifted modestly when scaled with elevation, and increased with DOM content and water temperature. Net ecosystem production (NEP = GPP − ER) decreased slightly at higher elevation and peaked at intermediate DOM levels. Zooplankton polyunsaturated fatty acid content was also unrelated to elevation but linked to lake trophic state. Overall, climatic and landscape shifts with elevation transmit inconsistent effects to the limnology of these regional lakes, possibly due to the region's overall low precipitation regime and lakes' weak hydrological connectivity with surrounding terrestrial habitats.

生态过渡带,如山地高程梯度,可以通过气候特征和集水区组成(即土地利用/土地覆盖)的变化影响湖泊的功能和生产力。然而,沿着这些生态过渡带的湖泊特征调查显示出变化的模式,使得很难将过去的结果外推到诸如加拿大落基山脉东坡等地区。为了测试海拔和梯度对生态过渡带环境变异性的影响,我们在阿尔伯塔省西南部草原和山地科迪勒拉之间的海拔梯度为600 m的11个湖泊中取样。我们分析了流域组成、水化学、湖泊代谢率(基于氧同位素分析)、溶解有机质(DOM)组成,以及基于脂肪酸分析的浮游动物群落组成和饮食。流域组成和水温沿海拔梯度的变化与DOM含量或组成关系不明显。夏季大部分湖泊为自养湖泊。初级生产总值(GPP)和生态系统呼吸速率(ER)随海拔的变化变化不大,随DOM含量和水温的升高而升高。净生态系统产量(NEP = GPP−ER)在海拔较高的地区略有下降,在中等DOM水平时达到峰值。浮游动物多不饱和脂肪酸含量与海拔高度无关,但与湖泊营养状态有关。总体而言,气候和景观随海拔的变化对这些区域湖泊的湖泊学产生了不一致的影响,这可能是由于该地区总体降水较少,湖泊与周围陆地栖息地的水文连通性较弱。
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引用次数: 0
Root Canopy Morphology Controls on Hydrodynamics and Turbulence Around Floating Vegetation Islands 根冠层形态对漂浮植被岛周围水动力和湍流的控制
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-07 DOI: 10.1002/eco.70154
Naveed Anjum, Sohail Iqbal, Jawad Ashraf

Floating vegetation islands (FVI) act as dynamic eco-hydraulic elements in both natural and engineered waterways, yet their interactions with flow, particularly those influenced by root canopy morphology, remain insufficiently understood. This study employs a computational fluid dynamic (CFD)–based approach to investigate how different FVI root structures affect channel hydrodynamics and turbulence characteristics. The model was first validated and then used for simulation purposes. Three configurations were examined: tall roots (Case A), short roots (Case B) and a combination of tall and short roots (Case C). High-resolution CFD simulations were conducted in a rectangular open channel to analyse flow velocity patterns, turbulence dynamics and bed shear responses around these FVI. The results reveal that vegetation morphology strongly governs flow behaviour and energy distribution. Case A produced substantial flow blockage, pronounced velocity gradients and extensive wake zones associated with heightened erosion potential. Case B induced moderate flow reduction and exhibited faster flow recovery, resulting in lower shear stress but limited flow attenuation. Case C demonstrated a balanced response, achieving moderate velocity reduction and more uniform turbulence distribution throughout the flow depth. Turbulence intensity and bed shear stress patterns also varied considerably among configurations: Case A concentrated turbulent kinetic energy and exhibited sharp stress gradients, Case B maintained more consistent profiles, and Case C displayed a spatially distributed turbulence field and intermediate stress variability, promoting stable sediment transport and ecological equilibrium. These findings underscore the pivotal role of vegetation (root canopy) arrangement in regulating flow resistance, sediment dynamics and ecological functionality, suggesting that strategically designed FVI can optimize erosion control, enhance habitat complexity and improve hydraulic performance in riverine and channelized systems.

漂浮植被岛(FVI)在自然水道和人工水道中都扮演着动态生态-水力元素的角色,但它们与水流的相互作用,特别是受根冠形态影响的相互作用,仍未得到充分的了解。本研究采用基于计算流体动力学(CFD)的方法研究了不同FVI根结构对通道流体力学和湍流特性的影响。首先验证了该模型,然后将其用于仿真目的。研究了三种结构:高根(案例A)、短根(案例B)和高根和短根的组合(案例C)。在矩形明渠中进行了高分辨率CFD模拟,以分析FVI周围的流速模式、湍流动力学和床层剪切响应。结果表明,植被形态对水流行为和能量分布有很大的影响。情况A产生了大量的流动阻塞,明显的速度梯度和广泛的尾迹区,与增强的侵蚀潜力有关。案例B诱导了适度的流动减少,并表现出更快的流动恢复,导致较低的剪切应力,但有限的流动衰减。案例C表现出平衡的响应,实现了适度的速度降低和整个流深更均匀的湍流分布。不同配置的湍流强度和床层剪应力模式也存在较大差异:Case A湍流动能集中,应力梯度明显;Case B剖面较为一致;Case C湍流场空间分布,应力变异性中等,有利于稳定输沙和生态平衡。这些发现强调了植被(根冠层)排列在调节水流阻力、泥沙动力学和生态功能方面的关键作用,表明策略性设计植被覆盖度可以优化侵蚀控制,增加生境复杂性,改善河流和渠化系统的水力性能。
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引用次数: 0
Groundwater-Surface Water Interactions in Intermittently Closed and Open Lake and Lagoon (ICOLL) Wetlands: Implications for Salinity and Ecological Functioning 间歇性封闭和开放湖泊和泻湖(ICOLL)湿地地下水-地表水相互作用:盐度和生态功能的影响
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-07 DOI: 10.1002/eco.70149
Bianca R. Palombi, Hannah E. Power, Peter Reinhard, Kate Tunstill, Warren Brown, Alex Callen, Gabriel C. Rau

Coastal wetlands are dynamic ecosystems where freshwater-saltwater interactions are governed by both hydrological and oceanic processes. However, climate change and human interventions such as lagoon breaching increasingly disrupt these interactions, posing challenges for ecosystem conservation. This study investigates the hydrogeological controls on water levels and salinity in a coastal freshwater wetland enclosed by Avoca Lagoon, an Intermittently Closed and Open Lake and Lagoon (ICOLL) in New South Wales, Australia. The wetland supports the endangered Green and Golden Bell Frog (GGBF, Litoria aurea), which requires low salinity for breeding. Using a multidisciplinary approach—combining groundwater and surface water monitoring, electrical resistivity tomography and lagoon bathymetry and salinity profiling—the study identifies strong hydraulic connectivity between the wetland and the lagoon, mediated by both lateral and vertical saltwater intrusion pathways. We identify four distinct hydrological stages of the lagoon that influence groundwater-surface water interactions within the wetland. Groundwater discharge plays a critical but often constrained buffering role, sustaining freshwater conditions while being limited by anthropogenic regulation of lagoon water levels. These findings highlight the narrow hydrological range supporting GGBF habitat and the vulnerability of the system to even minor water level fluctuations. They also underscore the need for adaptive management strategies—such as dynamic berm operation, managed aquifer recharge and protection of recharge zones—to balance flood mitigation with wetland conservation. This study advances understanding of groundwater-surface water interactions that underpin ecological resilience and demonstrates that groundwater connectivity must be integrated into ICOLL management frameworks to enhance preparedness for future climate variability and sea level rise.

沿海湿地是动态生态系统,其中淡水-盐水的相互作用受水文和海洋过程的控制。然而,气候变化和人类干预(如泻湖破裂)日益破坏了这些相互作用,给生态系统保护带来了挑战。本研究调查了澳大利亚新南威尔士州一个间歇性封闭和开放的湖泊和泻湖(ICOLL)——Avoca泻湖所包围的沿海淡水湿地的水位和盐度的水文地质控制。湿地是濒临灭绝的绿金铃蛙(GGBF, Litoria aurea)的栖息地,它们需要低盐度才能繁殖。该研究采用多学科方法,结合地下水和地表水监测、电阻率层析成像、泻湖测深和盐度剖面,确定了湿地和泻湖之间强大的水力连通性,由横向和垂直盐水入侵途径介导。我们确定了影响湿地内地下水-地表水相互作用的泻湖的四个不同的水文阶段。地下水排放起着关键但往往有限的缓冲作用,维持淡水条件,同时受到人为调节泻湖水位的限制。这些发现突出了支持GGBF栖息地的狭窄水文范围以及该系统对即使是较小的水位波动的脆弱性。它们还强调了适应性管理策略的必要性,例如动态护堤操作、有管理的含水层补给和补给区保护,以平衡洪水缓解与湿地保护。该研究促进了对地下水-地表水相互作用的理解,地下水相互作用是支撑生态恢复力的基础,并表明地下水连通性必须纳入ICOLL管理框架,以加强对未来气候变率和海平面上升的准备。
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引用次数: 0
Quantifying the Influence of Vegetation on Net Snow Accumulation Across Elevations, Aspects and During Years With High and Low Snowfall 植被对不同海拔、各向异性和多、少降雪年份净积雪影响的量化
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-06 DOI: 10.1002/eco.70156
Baylee M. Olds, Margaret A. Wolf, Sara A. Goeking, Paul D. Brooks

Seasonal snowmelt from forested mountain catchments is the primary water source for both people and ecosystems in the western United States. As changes in climate and vegetation alter relationships between snow accumulation and water availability, quantifying the influence of ecosystem structure on snow water resources is a critical challenge. To address this knowledge gap, we performed 2 years of distributed snow surveys to quantify how vegetation structure, topography and winter conditions interact to control net snow accumulation. The ratio of net snow water equivalence (SWE) at peak accumulation to winter snowfall (SWE:P) was 0.85 (range 0.67–1.03). This variability in SWE:P was associated with seven distinct vegetation environments that differentially influenced snow accumulation across all sites and years. Greatest snow accumulation was found in open areas immediately north of forests (SWE:P = 1.03 ± 0.05), followed by small gaps in conifer forests (SWE:P = 0.95 ± 0.07), small gaps in aspen forests (SWE:P = 0.88 ± 0.08), nonshaded open areas (SWE:P = 0.88 ± 0.05), under aspen canopies (SWE:P = 0.81 ± 0.04), under coniferous canopies (SWE:P = 0.76 ± 0.04) and lowest in open areas in south-facing forest edges (SWE:P = 0.67 ± 0.07). These spatial patterns in net SWE input were more pronounced in nontopographically shaded environments, suggesting that the influence of vegetation on local hydroclimate and net snow accumulation was greater in areas with higher solar radiation input. The consistency of these patterns across high and low elevations and during low- and high-snow years suggests that forest structure can be used to distribute spatial patterns in snow water input in both undisturbed forests and in response to forest management.

来自森林覆盖的山区集水区的季节性融雪是美国西部人类和生态系统的主要水源。由于气候和植被的变化改变了积雪和水分有效性之间的关系,量化生态系统结构对雪水资源的影响是一个关键的挑战。为了解决这一知识差距,我们进行了为期2年的分布式雪调查,以量化植被结构、地形和冬季条件如何相互作用来控制净雪积累。高峰累积期净雪水当量(SWE)与冬季降雪量之比(SWE:P)为0.85(0.67 ~ 1.03)。SWE:P的这种变异性与七种不同的植被环境有关,这些植被环境对所有地点和年份的积雪积累有不同的影响。森林正北的开阔地积雪量最大(SWE:P = 1.03±0.05),其次是针叶林的小林隙(SWE:P = 0.95±0.07)、白杨林的小林隙(SWE:P = 0.88±0.08)、无遮蔽的开阔地(SWE:P = 0.88±0.05)、白杨林的林隙(SWE:P = 0.81±0.04)、针叶林的林隙(SWE:P = 0.76±0.04),林缘向南的开阔地积雪量最少(SWE:P = 0.67±0.07)。净SWE输入的这些空间格局在非地形阴影环境中更为明显,表明在太阳辐射输入较高的地区,植被对当地水文气候和净积雪的影响更大。这些模式在高海拔和低海拔以及低雪年和高雪年的一致性表明,森林结构可以用来在未受干扰的森林和对森林管理的响应中分配雪水输入的空间格局。
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引用次数: 0
Spatial Distribution of Hydrological Services in Sichuan Forest Ecosystems Using LPJ Model 基于LPJ模型的四川森林生态系统水文功能空间分布
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-06 DOI: 10.1002/eco.70161
Yan Wenchao, Li Renhong, Wei Peng, Jia Cheng, Fang Fujin, Wang Yan, Zhang Wen, Chen Yuan, Ju Peijun

Amid escalating climate extremes in the 21st century, the hydrological regulatory functions of forest ecosystems have become crucial for climate adaptation strategies. Sichuan Province, encompassing critical headwaters of the Yangtze and Yellow River basins, sustains 23.7 million hectares of forests with distinctive elevational gradients (500–7500 m). This study implements the Lund–Potsdam–Jena Dynamic Global Vegetation Model (LPJ-DGVM) coupled with multitemporal Geographic Information Systems analysis (2010–2022) to systematically evaluate forest hydrological services. Through terrain-adjusted hydrological modelling and spatial clustering techniques, we quantify water retention capacities (annual average 2850 ± 320 m3/ha) and humidity stabilization effects (relative humidity enhancement: 8.3%–15.7%) across four major forest types. Geographically weighted regression reveals significant spatial heterogeneity in soil moisture storage (18.5–33.8% vol) and evapotranspiration rates (2.2–3.6 mm/day), with 62% of variations explained by bioclimatic drivers (temperature-precipitation synergy, r = 0.68) and anthropogenic pressure indices (population and gross domestic product composite, r = 0.59). Our proposed optimization framework integrates three implementation phases: (1) priority conservation of 12 critical water-yield zones (identified through hydrological sensitivity analysis), (2) rehabilitation of 850 km riparian corridors connecting fragmented habitats and (3) systematic resource integration through multifunctional landscape design. Scenario projections estimate 16%–24% enhancement in hydrological regulation efficiency, demonstrating viable pathways to reconcile ecological security (water provision capacity +19%), economic viability (ecotourism potential +28%) and social equity (disaster risk reduction for 4.3 million residents).

在21世纪极端气候不断升级的背景下,森林生态系统的水文调节功能已成为气候适应战略的关键。四川省,包括长江和黄河流域的关键源头,维持着2370万公顷的森林,具有独特的海拔梯度(500-7500米)。本研究采用隆德-波茨坦-耶拿动态全球植被模型(LPJ-DGVM),结合多时段地理信息系统分析(2010-2022)对森林水文服务进行系统评价。通过地形调整水文模型和空间聚类技术,我们量化了四种主要森林类型的保水能力(年平均2850±320 m3/ha)和湿度稳定效应(相对湿度增强:8.3%-15.7%)。地理加权回归显示,土壤水分储量(18.5-33.8% vol)和蒸散速率(2.2-3.6 mm/d)存在显著的空间异质性,其中62%的差异由生物气候驱动因素(温度-降水协同作用,r = 0.68)和人为压力指数(人口和国内生产总值复合,r = 0.59)解释。我们提出的优化框架包括三个实施阶段:(1)优先保护12个关键产水区(通过水文敏感性分析确定);(2)修复850公里的连接破碎栖息地的河岸走廊;(3)通过多功能景观设计进行系统的资源整合。情景预测估计,水文调节效率将提高16%-24%,展示了协调生态安全(供水能力+19%)、经济可行性(生态旅游潜力+28%)和社会公平(430万居民减少灾害风险)的可行途径。
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引用次数: 0
The Role of Leaf Wettability and Morphology on Leaf Surface Water Storage: A Cross-Biome Synthesis 叶片润湿性和形态对叶片地表水储存的作用:一个跨生物群系的合成
IF 2.1 3区 环境科学与生态学 Q2 ECOLOGY Pub Date : 2026-01-06 DOI: 10.1002/eco.70162
Ashley J. Cao, Zeyin Li, Paul O. Seibert, Cynthia Gerlein-Safdi

The presence of water on leaves impacts plant function and ecosystem fluxes by supplementing moisture, reducing evapotranspirational demand and encouraging pathogen spread. Maximum phytoelement water storage capacity (MWSC)—the maximum amount of water that can be held on the surface of the leaf- is an important but poorly constrained parameter that influences the effect of leaf wetting. Most studies on this parameter study one ecosystem and disagree on the measurement methodology. Here, both spraying and submergence techniques are used to measure MWSC of nine plant species from ecosystems selected across an aridity gradient. Our results show that spraying consistently yields higher MWSC, though the two methods were strongly and positively correlated (R2=0.84$$ {R}^2=0.84 $$). Hydrophobic leaves generally hold more water, and more hydrophobic leaves exhibit a greater difference between values derived from spraying and submergence. The presence of trichomes increased both hydrophobicity and spray-based holding capacity and decreased submergence-based holding capacity. Additional leaf surface structures like finely serrated leaf margins, while not captured by the contact angle measurement, enhanced spray-based holding capacity. Plant species from arid biomes have higher MWSC, while plant species from other biomes did not exhibit a significant difference in MWSC. Further investigation is needed to disentangle the effects of leaf orientation and time of sampling on these results. Data synthesis also highlights the need for standardized methodologies and data from dry sub-humid and arid ecosystems in future research to better compare results across different biomes.

水分在叶片上的存在通过补充水分、减少蒸散需求和促进病原体传播来影响植物功能和生态系统通量。最大植物元素储水能力(MWSC)是影响叶片润湿效果的一个重要但缺乏约束的参数,它是叶片表面能保持的最大水量。关于该参数的研究大多只研究一个生态系统,在测量方法上存在分歧。本文采用喷洒和浸没两种技术测量了不同干旱梯度生态系统中9种植物的MWSC。结果表明,尽管两种方法呈显著正相关(r2 = 0),但持续喷洒的MWSC产量较高。84 $$ {R}^2=0.84 $$)。疏水叶片通常具有更多的水分,疏水叶片在喷洒和浸没得到的数值之间表现出更大的差异。毛状体的存在增加了疏水性和喷雾式持水能力,降低了浸没式持水能力。额外的叶表面结构,如精细锯齿叶缘,而没有捕捉到的接触角测量,增强喷雾为基础的持有能力。干旱生物群系植物的MWSC较高,而其他生物群系植物的MWSC差异不显著。需要进一步研究叶片取向和采样时间对这些结果的影响。数据综合还强调,在未来的研究中需要标准化的方法和来自干燥半湿润和干旱生态系统的数据,以便更好地比较不同生物群系的结果。
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引用次数: 0
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Ecohydrology
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