As global land surface temperature continues to rise and heatwave events increase in
frequency, duration, and/or intensity, our key food and fuel cropping systems will likely face …

Atmospheric carbon dioxide concentration ([CO2]) is increasing, which increases leaf‐scale
photosynthesis and intrinsic water‐use efficiency. These direct responses have the potential …

Soil carbon sequestration is seen as an effective means to draw down atmospheric CO2, but
at the same time warming may accelerate the loss of extant soil carbon, so an accurate …

Executive summary Land and climate interact in complex ways through changes in forcing
and multiple biophysical and biogeochemical feedbacks across different spatial and …

The soil microbiome governs biogeochemical cycling of macronutrients, micronutrients and
other elements vital for the growth of plants and animal life. Understanding and predicting …

Soil is a vital resource for feeding the burgeoning global population, and it is also essential
for realizing most of the 'United Nations Sustainable Development Goals (SDGs)'. For …

Soils contain more carbon than the atmosphere and vegetation combined. An increased
flow of carbon from the atmosphere into soil pools could help mitigate anthropogenic …

With accumulation of carbon cycle observations and model developments over the past
decades, exploring interannual variation (IAV) of terrestrial carbon cycle offers the …

Soil is a key component of Earth's critical zone. It provides essential services for agricultural
production, plant growth, animal habitation, biodiversity, carbon sequestration and …

Soil respiration (R s) represents the largest flux of CO2 from terrestrial ecosystems to the
atmosphere, but its spatial and temporal changes as well as the driving forces are not well …