Multi‐year lags in tree drought recovery, termed 'drought legacy effects', are important for
understanding the impacts of drought on forest ecosystems, including carbon (C) cycle …

Climate change can directly affect forest hydrology by altering precipitation,
evapotranspiration, and streamflow generation, or indirectly by changing disturbance …

Globally, intrinsic water-use efficiency (iWUE) has risen dramatically over the past century in
concert with increases in atmospheric CO2 concentration. This increase could be further …

Despite a long history of discussion of 'non‐stationarity'in dendrochronology, researchers
and modellers in diverse fields commonly rely on the implicit assumption that tree growth …

The stable carbon isotopic composition (δ 13 C) measured in tree rings is a standard proxy
for paleoclimate reconstructions and is increasingly being used as a paleophysiological …

The US Southwest has been entrenched in a two‐decade‐long megadrought (MD), the most
severe since 800 CE, which threatens the long‐term vitality and persistence of regional …

Recent analyses on the length of drought recovery in forests have shown multi-year
legacies, particularly in semi-arid, coniferous ecosystems. Such legacies are usually …

Increases in terrestrial water‐use efficiency (WUE) have been reported in many studies,
pointing to potential changes in physiological forcing of global carbon and hydrological …

Increasing water‐use efficiency (WUE), the ratio of carbon gain to water loss, is a key
mechanism that enhances carbon uptake by terrestrial vegetation under rising atmospheric …

Tree growth is generally considered to be temperature limited at upper elevation treelines,
yet climate factors controlling tree growth at semiarid treelines are poorly understood. We …