Rainfall-runoff characteristics and their threshold behaviors on a karst hillslope in a peak-cluster depression region DOI
Sheng Wang,

Yan Yan,

Zhiyong Fu

и другие.

Journal of Hydrology, Год журнала: 2021, Номер 605, С. 127370 - 127370

Опубликована: Дек. 23, 2021

Язык: Английский

Hillslope Hydrology in Global Change Research and Earth System Modeling DOI Creative Commons
Ying Fan, Martyn Clark, David M. Lawrence

и другие.

Water Resources Research, Год журнала: 2019, Номер 55(2), С. 1737 - 1772

Опубликована: Фев. 1, 2019

Abstract Earth System Models (ESMs) are essential tools for understanding and predicting global change, but they cannot explicitly resolve hillslope‐scale terrain structures that fundamentally organize water, energy, biogeochemical stores fluxes at subgrid scales. Here we bring together hydrologists, Critical Zone scientists, ESM developers, to explore how hillslope may modulate grid‐level fluxes. In contrast the one‐dimensional (1‐D), 2‐ 3‐m deep, free‐draining soil hydrology in most land models, hypothesize 3‐D, lateral ridge‐to‐valley flow through shallow deep paths insolation contrasts between sunny shady slopes top two globally quantifiable organizers of water energy (and vegetation) within an grid cell. We these processes likely impact predictions where when) and/or limiting. further that, if implemented will increase simulated continental storage residence time, buffering terrestrial ecosystems against seasonal interannual droughts. efficient ways capture mechanisms ESMs identify critical knowledge gaps preventing us from scaling up processes. One such gap is our extremely limited subsurface, stored (supporting released stream baseflow aquatic ecosystems). conclude with a set organizing hypotheses call syntheses activities model experiments assess on change predictions.

Язык: Английский

Процитировано

551

Microclimatic buffering in forests of the future: the role of local water balance DOI Open Access
Kimberley T. Davis, Solomon Z. Dobrowski, Zachary A. Holden

и другие.

Ecography, Год журнала: 2018, Номер 42(1), С. 1 - 11

Опубликована: Июнь 21, 2018

Forest canopies buffer climate extremes and promote microclimates that may function as refugia for understory species under changing climate. However, the biophysical conditions maintain microclimatic buffering its stability through time are largely unresolved. We posited forest is sensitive to local water balance canopy cover, we measured this effect during growing season across a gradient in forests of northwestern United States (US). found maximum temperature vapor pressure deficit (VPD), with biologically meaningful sizes. For example, season, VPD at least 50% were 5.3°C 1.1 kPa lower on average, respectively, compared areas without cover. Canopy was greater higher levels varied balance, implying effects subject changes hydrology. project mid‐21st century predict how such impact ability western US extremes. Our results suggest some will lose their capacity sites become increasingly limited. Changes combined accelerating losses due increases frequency severity disturbance create potentially non‐linear microclimate forests.

Язык: Английский

Процитировано

367

California forest die-off linked to multi-year deep soil drying in 2012–2015 drought DOI
Michael L. Goulden, Roger C. Bales

Nature Geoscience, Год журнала: 2019, Номер 12(8), С. 632 - 637

Опубликована: Июль 1, 2019

Язык: Английский

Процитировано

310

A low-to-no snow future and its impacts on water resources in the western United States DOI
Erica R. Siirila‐Woodburn, Alan M. Rhoades, Benjamin J. Hatchett

и другие.

Nature Reviews Earth & Environment, Год журнала: 2021, Номер 2(11), С. 800 - 819

Опубликована: Окт. 26, 2021

Язык: Английский

Процитировано

305

Why is Tree Drought Mortality so Hard to Predict? DOI Creative Commons
Anna T. Trugman, Leander D. L. Anderegg, William R. L. Anderegg

и другие.

Trends in Ecology & Evolution, Год журнала: 2021, Номер 36(6), С. 520 - 532

Опубликована: Март 2, 2021

Язык: Английский

Процитировано

197

Which trees die during drought? The key role of insect host‐tree selection DOI Creative Commons
Nathan L. Stephenson, Adrian J. Das,

Nicholas J. Ampersee

и другие.

Journal of Ecology, Год журнала: 2019, Номер 107(5), С. 2383 - 2401

Опубликована: Апрель 4, 2019

Abstract During drought, the tree subpopulations (such as size or vigour classes) that suffer disproportionate mortality can be conceptually arrayed along a continuum defined by actions of biotic agents, particularly insects. At one extreme, stress dominates: insects are absent simply kill most physiologically stressed trees. opposite host selection outbreaking trees independently their stress, instead selecting based on other traits. Intermediate responses also possible. Yet for mixed‐species forests, we lack broad understanding relative importance in determining exactly which during and whether these differ among co‐occurring species. an extreme documented roles native bark beetles five species California’s Sierra Nevada. We analysed patterns agents 12 permanent plots 89 temporary plots. Most was associated with beetles. However, growth rates (an indicator chronic stress) sizes suffered greatest beetle‐related differed sharply taxa, variously conforming domination ( Abies concolor ), Pinus lambertiana P. ponderosa ) mix two Calocedrus decurrens ). Quercus kelloggii remained relatively low. Thus, even drought substantial proportions survived because they were mostly avoided fatal insect attack. Conversely, comparatively unstressed died selectively killed Synthesis . Native primarily responsible drought. idiosyncratic host‐tree different beetle taxa meant suffering strikingly taxa—for example, high small species, but large another. If proves to generally common phenomenon, it could help explain weak broadscale correlations between traits

Язык: Английский

Процитировано

150

Plant sizes and shapes above and belowground and their interactions with climate DOI Creative Commons
Shersingh Joseph Tumber‐Dávila, H. Jochen Schenk, Enzai Du

и другие.

New Phytologist, Год журнала: 2022, Номер 235(3), С. 1032 - 1056

Опубликована: Фев. 12, 2022

Although the above and belowground sizes shapes of plants strongly influence plant competition, community structure, plant-environment interactions, remain poorly characterized across climate regimes. We investigated relationships among shoot root system size climate. assembled analyzed, to our knowledge, largest global database describing maximum rooting depth, lateral spread, terrestrial - more than doubling Root Systems Individual Plants 5647 observations. Water availability growth form greatly size, depth is primarily influenced by temperature seasonality. Shoot strongest predictor with diameter being two times wider width on average for woody plants. covaries size; however, geometries differ considerably climates, in arid climates having shorter shoots, but deeper, narrower systems. Additionally, estimates spread systems are likely underestimated at scale.

Язык: Английский

Процитировано

124

The Influence of Topography on the Global Terrestrial Water Cycle DOI Creative Commons
Sebastian Gnann, Jane W. Baldwin, Mark Cuthbert

и другие.

Reviews of Geophysics, Год журнала: 2025, Номер 63(1)

Опубликована: Янв. 3, 2025

Abstract Topography affects the distribution and movement of water on Earth, yet new insights about topographic controls continue to surprise us exciting puzzles remain. Here we combine literature review data synthesis explore influence topography global terrestrial cycle, from atmosphere down groundwater. Above land surface, induces gradients contrasts in energy availability. Long‐term precipitation usually increases with elevation mid‐latitudes, while it peaks at low‐ mid‐elevations tropics. Potential evaporation tends decrease all climate zones. At is expressed snow distribution, vegetation zonation, geomorphic landforms, critical zone, drainage networks. Evaporation activity are often highest where neither temperature, nor availability, availability—often modulated by lateral moisture redistribution—impose strong limitations. Below drives groundwater local continental scales. In many steep upland regions, systems well connected streams provide ample baseflow, start losing foothills bedrock transitions into highly permeable sediment. We conclude presenting organizing principles, discussing implications change human activity, identifying needs knowledge gaps. A defining feature resulting presence contrasts, whose interactions explain patterns observe nature how they might future.

Язык: Английский

Процитировано

3

Lithologically Controlled Subsurface Critical Zone Thickness and Water Storage Capacity Determine Regional Plant Community Composition DOI Creative Commons
W. Jesse Hahm, Daniella Rempe, David Dralle

и другие.

Water Resources Research, Год журнала: 2019, Номер 55(4), С. 3028 - 3055

Опубликована: Март 13, 2019

Abstract Explanations for distinct adjacent ecosystems that extend across hilly landscapes typically point to differences in climate or land use. Here we document—within a similar climate—how contrasting regional plant communities correlate with underlying lithology and reveal how water storage capacity the critical zone (CZ) explain this relationship. We present observations of subsurface CZ structure groundwater dynamics from deep boreholes quantify catchment‐wide dynamic two Franciscan rock types Northern California Coast Ranges. Our field sites have Mediterranean climate, where rains are out phase solar energy, amplifying importance periods peak ecosystem productivity dry season. In deeply weathered (~30 m at ridge) Coastal Belt argillite sandstone, ample, seasonally replenished moisture supports an evergreen forest drainage sustains baseflow throughout summer. Central argillite‐matrix mélange, thin (~3 limits total (100–200 mm) rapidly sheds winter rainfall via shallow storm saturation overland flow, resulting low plant‐available (inferred predawn tree potential) negligible can drain streams This limitation mechanism explains presence oak savanna‐woodland bounded by ephemeral streams, despite >1,800 mm average precipitation. Through hydrologic monitoring characterization, which type result regionally extensive under climate.

Язык: Английский

Процитировано

141

Digging deeper: what the critical zone perspective adds to the study of plant ecophysiology DOI Creative Commons
Todd E. Dawson, W. Jesse Hahm, Kelsey L. Crutchfield-Peters

и другие.

New Phytologist, Год журнала: 2020, Номер 226(3), С. 666 - 671

Опубликована: Янв. 8, 2020

Summary The emergence of critical zone (CZ) science has provided an integrative platform for investigating plant ecophysiology in the context landscape evolution, weathering and hydrology. CZ lies between top vegetation canopy fresh, chemically unaltered bedrock plays a pivotal role sustaining life. We consider what perspective recently brought to study ecophysiology. specifically highlight novel research demonstrating importance deeper subsurface water nutrient relations. also point knowledge gaps opportunities, emphasising, particular, greater focus on roles deep, nonsoil resources how those influence coevolve with plants as frontier ecophysiological research.

Язык: Английский

Процитировано

98