Forest microclimates contrast strongly with the climate outside forests. To fully understand
and better predict how forests' biodiversity and functions relate to climate and climate …

Climate tipping points occur when change in a part of the climate system becomes self-
perpetuating beyond a warming threshold, leading to substantial Earth system impacts …

Proxy reconstructions from marine sediment cores indicate peak temperatures in the first half
of the last and current interglacial periods (the thermal maxima of the Holocene epoch …

Many feedback loops significantly increase warming due to greenhouse gas emissions.
However, not all of these feedbacks are fully accounted for in climate models. Thus …

Afforestation is one of the most practised carbon dioxide removal methods but is constrained
by the availability of suitable land and sufficient water resources. In this research, existing …

Coastal ecosystems represent a disproportionately large but vulnerable global carbon sink.
Sea-level-driven tidal wetland degradation and upland forest mortality threaten coastal …

This study examines the effect of land cover, vegetation health, climatic forcings, elevation
heat loads, and terrain characteristics (LVCET) on land surface temperature (LST) …

During the Quaternary period, the eastern Sahara's hydroclimate oscillated between wet
and dry intervals. These oscillations caused drastic changes in precipitation rates, often …

This study examines the projected changes in mean and extreme precipitation over the
Mediterranean (MED) and Sahara (SAH) regions based on the multi‐model ensemble mean …

Between 5 and 4 thousand years ago, crippling megadroughts led to the disruption of
ancient civilizations across parts of Africa and Asia, yet the extent of these climate extremes …