Forests can store large amounts of carbon and provide essential ecosystem services.
Massive tree planting is thus sometimes portrayed as a panacea to mitigate climate change …

As a step towards understanding the fundamental drivers of polar climate change, we
evaluate contributions to polar warming and its seasonal and hemispheric asymmetries in …

The ocean is taking up additional heat but how this affects ocean circulation and heat
transport is unclear. Here, using coupled model intercomparison project phase 5/6 …

Abstract The western South Atlantic along the Brazilian margin is an important region for the
Atlantic Meridional Overturning Circulation (AMOC) because surface currents in this area …

Arctic amplification of anthropogenic climate change is widely attributed to the sea-ice
albedo feedback, with its attendant increase in absorbed solar radiation, and to the effect of …

Arctic warming under increased CO2 peaks in winter, but is influenced by summer forcing
via seasonal ocean heat storage. Yet changes in atmospheric heat transport into the Arctic …

Arctic surface warming under greenhouse gas forcing peaks in winter and reaches its
minimum during summer in both observations and model projections. Many mechanisms …

Evaporation adds moisture to the atmosphere, while condensation removes it.
Condensation also adds thermal energy to the atmosphere, which must be removed from …

Driven primarily by variations in the earth's axis wobble, tilt, and orbit eccentricity, our planet
experienced massive glacial/interglacial reorganizations of climate and atmospheric CO 2 …

The ice–albedo feedback associated with sea ice loss contributes to polar amplification,
while the water vapor feedback contributes to tropical amplification of surface warming …