Land–atmospheric feedbacks during droughts and heatwaves: state of the science and current challenges

DG Miralles, P Gentine, SI Seneviratne… - Annals of the New …, 2019 - Wiley Online Library
Droughts and heatwaves cause agricultural loss, forest mortality, and drinking water scarcity,
especially when they occur simultaneously as combined events. Their predicted increase in …

Global water availability boosted by vegetation-driven changes in atmospheric moisture transport

J Cui, X Lian, C Huntingford, L Gimeno, T Wang… - Nature …, 2022 - nature.com
Surface-water availability, defined as precipitation minus evapotranspiration, can be affected
by changes in vegetation. These impacts can be local, due to the modification of …

ESA CCI Soil Moisture for improved Earth system understanding: State-of-the art and future directions

W Dorigo, W Wagner, C Albergel, F Albrecht… - Remote Sensing of …, 2017 - Elsevier
Abstract Climate Data Records of soil moisture are fundamental for improving our
understanding of long-term dynamics in the coupled water, energy, and carbon cycles over …

Soil moisture− atmosphere feedbacks have triggered the shifts from drought to pluvial conditions since 1980

Y Qing, S Wang, ZL Yang, P Gentine - Communications Earth & …, 2023 - nature.com
Drought and pluvial transitions have attracted widespread attention. However, the dynamic
evolution and underlying mechanisms of drought and pluvial transitions remain poorly …

Plant evolution and climate over geological timescales

CK Boyce, JE Lee - Annual Review of Earth and Planetary …, 2017 - annualreviews.org
The terrestrial vegetation is unambiguously an important factor in the climate system,
modulating the exchange of energy, momentum, water vapor, and other trace gases …

Increased control of vegetation on global terrestrial energy fluxes

G Forzieri, DG Miralles, P Ciais, R Alkama… - Nature Climate …, 2020 - nature.com
Abstract Changes in vegetation structure are expected to influence the redistribution of heat
and moisture; however, how variations in the leaf area index (LAI) affect this global energy …

Land–atmosphere interactions: The LoCo perspective

JA Santanello Jr, PA Dirmeyer… - Bulletin of the …, 2018 - journals.ametsoc.org
Land–atmosphere (LA) interactions are a main driver of Earth's surface water and energy
budgets; as such, they modulate near-surface climate, including clouds and precipitation …

Reference evapotranspiration estimation and modeling of the Punjab Northern India using deep learning

MK Saggi, S Jain - Computers and Electronics in Agriculture, 2019 - Elsevier
Over the last decade, the combination of both big data and machine learning research
area's receiving considerable attention and expedite the prospect of the agricultural industry …

Afternoon rain more likely over drier soils

CM Taylor, RAM de Jeu, F Guichard, PP Harris… - Nature, 2012 - nature.com
Land surface properties, such as vegetation cover and soil moisture, influence the
partitioning of radiative energy between latent and sensible heat fluxes in daytime hours …

When does vapor pressure deficit drive or reduce evapotranspiration?

A Massmann, P Gentine, C Lin - Journal of Advances in …, 2019 - Wiley Online Library
Increasing vapor pressure deficit (VPD) increases atmospheric demand for water. While
increased evapotranspiration (ET) in response to increased atmospheric demand seems …