Abstract The Russian invasion of Ukraine hampers the ability to adequately describe
conditions across the Arctic, thus biasing the view on Arctic change. Here we benchmark the …

Temperature anomalies and changes in the diurnal temperature range (DTR) are expected
to pose physiological challenges to biota; hence, both spatial and temporal variations in …

Reliable precipitation simulation over the Tibetan Plateau (TP) remains a challenge,
manifested by a prominent systematic wet bias in the warm season. Previous studies have …

Arctic and subarctic ecosystems are experiencing rapid changes in vegetation composition
and productivity due to global warming. Tundra wetlands are especially susceptible to these …

Terrestrial ecosystems affect climate by reflecting solar irradiation, evaporative cooling, and
carbon sequestration. Yet very little is known about how plant traits affect climate regulation …

Gross primary production (GPP) is a critical component of the global carbon cycle and plays
a significant role in the terrestrial carbon budget. The impact of environmental factors on …

Three-dimensional urban landscapes significantly alter surface energy dynamics and local
climates. However, it remains unclear how heat fluxes impact the microclimate at the …

The Tibetan Plateau (TP) is distributed with large areas of permafrost, which have received
increasing attention as the climate warms. Accurately modeling the extent of permafrost and …

Arctic vegetation changes, such as increasing shrub-cover, are expected to accelerate
climate warming through increased absorption of incoming radiation and corresponding …

The Arctic is experiencing amplified climate warming, decreasing sea ice extent,
increasingly earlier springtime snowmelt, and a related increase in fire activity. The transition …