This chapter assesses simulations of future global climate change, spanning time horizons from the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) out to …
It is unequivocal that the increases in atmospheric carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …
Abstract The Southern Ocean between 30° S and 55° S is a major sink of excess heat and anthropogenic carbon, but model projections of these sinks remain highly uncertain …
S Palazzo Corner, M Siegert, P Ceppi… - Frontiers in …, 2023 - frontiersin.org
How do we halt global warming? Reaching net zero carbon dioxide (CO 2) emissions is understood to be a key milestone on the path to a safer planet. But how confident are we that …
The effect of the Southern Ocean on global climate change is assessed using Earth system model projections following an idealized 1% annual rise in atmospheric CO2. For this …
Abstract Earth System Models (ESMs) continue to diagnose a wide range of carbon budgets for each level of global warming. Here, we present emergent constraints on the carbon …
The benefits of implementing negative emission technologies in the global warming response to cumulative carbon emissions until the year 2420 are assessed following the …
We formulate a new conceptual model, named “MT 2”, to describe global ocean heat uptake, as simulated by atmosphere–ocean general circulation models (AOGCMs) forced by …
Abstract The IPCC Special Report on 1.5° C concluded that anthropogenic global warming is determined by cumulative anthropogenic CO2 emissions and the non-CO2 radiative …