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Global Change Biology · 2026 · Vol. 32 · Issue 4 · Wiley
Forest canopy, air temperatures and air humidity (, , and ) play a central rol in regulating energy and gas exchange between vegetation and the atmosphere. Although often treated as independent drivers of canopy processes, and are dynamically coupled to via surface energy fluxes and atmospheric boundary layer (ABL) development. We investigated how plant physiology mediates this coupling. Using data from a tropical ecosystem, w...
Global Change Biology · 2025 · Vol. 31 · Issue 11 · Wiley
In late June 2021, multiple days of record‐breaking heat caused an unprecedented amount of foliage death in the forests of the Pacific Northwest, USA. Portions of tree canopies with healthy green foliage prior to the heat changed to red or orange shortly after the event. The change in foliage color could be readily seen in satellite imagery and was corroborated as foliar death (heat scorch) by aerial surveys and extensive obse...
Agricultural and Forest Meteorology · 2025 · Vol. 372 · Elsevier
David E Reed; Housen Chu; Brad G. Peter; Jiquan Chen; Michael Abraha; Brian Amiro; Ray G. Anderson; M. Altaf Arain; Paulo Arruda; Greg A. Barron-Gafford; Carl Bernacchi; Daniel P. Beverly; Sebastien C. Biraud; T. Andrew Black; Peter D. Blanken; Gil Bohrer; Rebecca Bowler; David R. Bowling; M. Syndonia Bret-Harte; Mario Bretfeld; Nathaniel A. Brunsell; Stephen H. Bullock; Gerardo Celis; Xingyuan Chen; Aimee T. Classen; David R. Cook; Alejandro Cueva; Higo J. Dalmagro; Kenneth Davis; Ankur Desai; Alison J. Duff; Allison L. Dunn; David Durden; Colin W. Edgar; Eugenie Euskirchen; Rosvel Bracho; Brent Ewers; Lawrence B. Flanagan; Christopher Florian; Vanessa Foord; Inke Forbrich; Brandon R. Forsythe; John Frank; Jaime Garatuza-Payan; Sarah Goslee; Christopher Gough; Mark Green; Timothy Griffis; Manuel Helbig; Andrew C. Hill; Ross Hinkle; Jason Horne; Elyn Humphreys; Hiroki Ikawa; Go Iwahana; Rachhpal Jassal; Bruce Johnson; Mark Johnson; Steven A. Kannenberg; Eric Kelsey; John King; John F. Knowles; Sara Knox; Hideki Kobayashi; Thomas Kolb; Randy Kolka; Ken W. Krauss; Lars Kutzbach; Brian Lamb; Beverly Law; Sung-Ching Lee; Xuhui Lee; Heping Liu; Henry W. Loescher; Sparkle L. Malone; Roser Matamala; Marguerite Mauritz; Stefan Metzger; Gesa Meyer; Bhaskar Mitra; J. William Munger; Zoran Nesic; Asko Noormets; Thomas L. O'Halloran; Patrick T O'Keeffe; Steven F. Oberbauer; Walter Oechel; Patty Oikawa; Paulo C. Olivas; Andrew Ouimette; Gilberto Pastorello; Jorge F. Perez-Quezada; Claire Phillips; Gabriela Posse; Bo Qu; William L. Quinton; Michele L. Reba; Andrew D. Richardson; Valentin Picasso; Adrian V. Rocha; Julio C. Rodriguez; Roel Ruzol; Scott Saleska; Russell L. Scott; Adam P. Schreiner-McGraw; Edward A.G. Schuur; Maria Silveira; Oliver Sonnentag; David L. Spittlehouse; Ralf Staebler; Gregory Starr; Christina Staudhammer; Chris Still; Cove Sturtevant; Ryan C. Sullivan; Andy Suyker; David Trejo; Masahito Ueyama; Rodrigo Vargas; Brian Viner; Enrique R. Vivoni; Dong Wang; Eric J. Ward; Susanne Wiesner; Lisamarie Windham-Myers; David Yannick; Enrico A. Yepez; Terenzio Zenone; Junbin Zhao; Donatella Zona
Climate Dynamics · 2023 · Springer
We present the first convection-permitting regional climate model (CPRCM) simulations at 4.5 km horizontal resolution for South America at near-continental scale, including full details of the experimental setup and results from the reanalysis-driven hindcast and climate model-driven present-day simulations. We use a range of satellite and ground-based observations to evaluate the CPRCM simulations covering the period 1998–200...
Global Change Biology · 2022 · Vol. 28 · Issue 8 · Wiley
Plants are critical mediators of terrestrial mass and energy fluxes, and their structural and functional traits have profound impacts on local and global climate, biogeochemistry, biodiversity, and hydrology. Yet, Earth System Models (ESMs), our most powerful tools for predicting the effects of humans on the coupled biosphere–atmosphere system, simplify the incredible diversity of land plants into a handful of coarse categorie...
Global Change Biology · 2022 · Vol. 28 · Issue 3 · Wiley
Climate warming in recent decades has negatively impacted forest health in the western United States. Here, we report on potential early warning signals (EWS) for drought‐related mortality derived from measurements of tree‐ring growth (ring width index; RWI) and carbon isotope discrimination (∆ 13 C), primarily focused on ponderosa pine ( Pinus ponderosa ). Sampling was conducted in the southern Sierra Nevada Mountains, near t...
Ecology · 2022 · Vol. 103 · Issue 2 · Wiley
Understanding spatial and temporal variation in plant traits is needed to accurately predict how communities and ecosystems will respond to global change. The National Ecological Observatory Network’s (NEON’s) Airborne Observation Platform (AOP) provides hyperspectral images and associated data products at numerous field sites at 1 m spatial resolution, potentially allowing high‐resolution trait mapping. We tested the accuracy...
Ecology · 2019 · Vol. 100 · Issue 6 · Wiley
In dealing with predicted changes in environmental conditions outside those experienced today, forest managers and researchers rely on process‐based models to inform physiological processes and predict future forest growth responses. The carbon and oxygen isotope ratios of tree‐ring cellulose (δ 13 C cell , δ 18 O cell ) reveal long‐term, integrated physiological responses to environmental conditions. We incorporated a submode...
Global Change Biology · 2019 · Vol. 25 · Issue 4 · Wiley
A century of fire suppression across the Western United States has led to more crowded forests and increased competition for resources. Studies of forest thinning or stand conditions after mortality events have provided indirect evidence for how competition can promote drought stress and predispose forests to severe fire and/or bark beetle outbreaks. Here, we demonstrate linkages between fire deficits and increasing drought st...
Global Ecology and Biogeography · 2019 · Vol. 28 · Issue 2 · Wiley
Aim C 4 grasses are distinct from C 3 grasses, because C 4 grasses respond in a different manner to light, temperature, CO 2 and nitrogen and often have higher resource‐use efficiencies. C 3 and C 4 grasses are typically represented in earth system models (ESMs) by different plant functional types (PFTs). The ability of ESMs to capture C 4 grass biogeography and ecology across differing time periods is important to assess, giv...
Journal of Biogeography · 2017 · Vol. 44 · Issue 11 · Wiley
Aims Understanding the functional response of ecosystems to past global change is crucial to predicting performance in future environments. One sensitive and functionally significant attribute of grassland ecosystems is the percentage of species that use the C 4 versus C 3 photosynthetic pathway. Grasses using C 3 and C 4 pathways are expected to have different responses to many aspects of anthropogenic environmental change th...
International Journal of Climatology · 2015 · Vol. 35 · Issue 11 · Wiley
Studies of regional drought history will be helpful for understanding current hydroclimate variability with global warming as well as predicting future hydroclimate shifts. Long‐term tree‐ring records are scarce in the western Qilian Mountains of northwestern China, which is also the western boundary of the natural distribution of Qilian Juniper ( Juniperus przewalskii Kom.) in this area. Here, we present an 850‐year ( AD 1161...
Global Ecology and Biogeography · 2015 · Vol. 24 · Issue 3 · Wiley
Aim C 4 photosynthesis is an adaptation that maintains efficient carbon assimilation in high‐light, high‐temperature conditions. Due to the importance of C 4 grasses for carbon and surface energy fluxes, numerous models have been proposed to describe their spatial distribution and forecast their responses to climate change. These models often rely on broad climatic predictors (e.g. temperature and precipitation) but fail to in...
Global Ecology and Biogeography · 2014 · Vol. 23 · Issue 3 · Wiley
Aim Numerous studies have documented ecological sorting of C 3 and C 4 grasses along air temperature gradients. However, phylogenetically structured analyses suggest that closely related C 3 and C 4 grasses (in the same PACMAD clade: P anicoideae, A rundinoideae, C hloridoideae, M icrairoideae, A ristidoideae and D anthonioideae) occur in environments with similar air temperature, challenging our understanding of how the photo...
Global Change Biology · 2013 · Vol. 19 · Issue 2 · Wiley
Assessing the ecological importance of clouds has substantial implications for our basic understanding of ecosystems and for predicting how they will respond to a changing climate. This study was conducted in a coastal Bishop pine forest ecosystem that experiences regular cycles of stratus cloud cover and inundation in summer. Our objective was to understand how these clouds impact ecosystem metabolism by contrasting two sites...
Global Change Biology · 2013 · Vol. 19 · Issue 1 · Wiley
A number of studies have demonstrated the ecological sorting of C 3 and C 4 grasses along temperature and moisture gradients. However, previous studies of C 3 and C 4 grass biogeography have often inadvertently compared species in different and relatively unrelated lineages, which are associated with different environmental settings and distinct adaptive traits. Such confounded comparisons of C 3 and C 4 grasses may bias our u...
Journal of Biogeography · 2009 · Vol. 36 · Issue 4 · Wiley
Aim Fog drip is a crucial water source for plants in many ecosystems, including a number of global biodiversity hotspots. In California, dozens of rare, drought‐sensitive plant species are endemic to coastal areas where the dominant summer moisture source is fog. Low clouds that provide water to these semi‐arid ecosystems through fog drip can also sharply reduce evaporative water losses by providing shade. We quantified the re...