Elizabeth E. Webb

Google Earth Engine: A Global Analysis and Future Trends

Landscape topography structures the soil microbiome in arctic polygonal tundra

Regulation of priming effect by soil organic matter stability over a broad geographic scale

Determinants of carbon release from the active layer and permafrost deposits on the Tibetan Plateau

Soil and water threats in a changing environment

Soil microbiomes and climate change

Climate change and the permafrost carbon feedback

Climate Change 2022 – Impacts, Adaptation and Vulnerability

The Russian‐Ukrainian armed conflict will push back the sustainable development goals

Wetlands In a Changing Climate: Science, Policy and Management

A pan‐Arctic synthesis of CH₄ and CO₂ production from anoxic soil incubations

A review of modern treeline migration, the factors controlling it and the implications for carbon storage

Tundra soil carbon is vulnerable to rapid microbial decomposition under climate warming

Stochastic Community Assembly: Does It Matter in Microbial Ecology?

Tundra plant above-ground biomass and shrub dominance mapped across the North Slope of Alaska

Responses of tundra soil microbial communities to half a decade of experimental warming at two critical depths

The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores

Variability in above- and belowground carbon stocks in a Siberian larch watershed

Direct observation of permafrost degradation and rapid soil carbon loss in tundra

Permafrost thaw and soil moisture driving CO₂ and CH₄ release from upland tundra

Permafrost degradation stimulates carbon loss from experimentally warmed tundra

Tundra is a consistent source of CO₂ at a site with progressive permafrost thaw during 6 years of chamber and eddy covariance measurements