Water potential directly controls the function of leaves, roots and microbes, and gradients in
water potential drive water flows throughout the soil–plant–atmosphere continuum …

Both low soil water content (SWC) and high atmospheric dryness (vapor pressure deficit,
VPD) can negatively affect terrestrial gross primary production (GPP). The sensitivity of GPP …

This study presents the global climate model IPSL‐CM6A‐LR developed at Institut Pierre‐
Simon Laplace (IPSL) to study natural climate variability and climate response to natural and …

Abstract The Coupled Model Intercomparison Project Phase 6 (CMIP6) dataset is used to
examine projected changes in temperature and precipitation over the United States (US) …

Deep water formation is the driver of the global ocean circulation, yet it was poorly
represented in the previous generation of climate models. We here quantify biases in …

This paper explored the projected changes in precipitation, maximum temperature (T max),
and minimum temperature (T min) over the Yangtze River Basin (YRB) based on 23 Global …

The Pliocene epoch has great potential to improve our understanding of the long-term
climatic and environmental consequences of an atmospheric CO 2 concentration near∼ …

Chemical loss of Arctic ozone due to anthropogenic halogens is driven by temperature, with
more loss occurring during cold winters favourable for formation of polar stratospheric …

Abstract The Arctic Ocean is strongly stratified by salinity in the uppermost layers. This
stratification is a key attribute of the region as it acts as an effective barrier for the vertical …

This study presents the version of the LMDZ global atmospheric model used as the
atmospheric component of the Institut Pierre Simon Laplace coupled model (IPSL‐CM6A …