Volcanic effects on climate: recent advances and future avenues
Volcanic eruptions have long been studied for their wide range of climatic effects. Although
global-scale climatic impacts following the formation of stratospheric sulfate aerosol are well …
global-scale climatic impacts following the formation of stratospheric sulfate aerosol are well …
Future global climate: scenario-based projections and near-term information
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 …
from the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) out to …
Observationally-constrained projections of an ice-free Arctic even under a low emission scenario
The sixth assessment report of the IPCC assessed that the Arctic is projected to be on
average practically ice-free in September near mid-century under intermediate and high …
average practically ice-free in September near mid-century under intermediate and high …
Human influence on the climate system (Chapter 3)
The AR5 concluded that human influence on the climate system is clear, evident from
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …
Large ensemble climate model simulations: introduction, overview, and future prospects for utilising multiple types of large ensemble
Single model initial-condition large ensembles (SMILEs) are valuable tools that can be used
to investigate the climate system. SMILEs allow scientists to quantify and separate the …
to investigate the climate system. SMILEs allow scientists to quantify and separate the …
Human influence on joint changes in temperature, rainfall and continental aridity
Despite the pervasive impact of drought on human and natural systems, the large-scale
mechanisms conducive to regional drying remain poorly understood. Here we use a …
mechanisms conducive to regional drying remain poorly understood. Here we use a …
Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
The mechanisms underlying decadal variability in Arctic sea ice remain actively debated.
Here, we show that variability in boreal biomass burning (BB) emissions strongly influences …
Here, we show that variability in boreal biomass burning (BB) emissions strongly influences …
[HTML][HTML] Forced and internal components of observed Arctic sea-ice changes
The Arctic sea-ice cover is strongly influenced by internal variability on decadal timescales,
affecting both short-term trends and the timing of the first ice-free summer. Several …
affecting both short-term trends and the timing of the first ice-free summer. Several …
[HTML][HTML] Northern Hemisphere continental winter warming following the 1991 Mt. Pinatubo eruption: reconciling models and observations
LM Polvani, A Banerjee… - Atmospheric Chemistry and …, 2019 - acp.copernicus.org
It has been suggested, and is widely believed, that the anomalous surface warming
observed over the Northern Hemisphere continents in the winter following the 1991 eruption …
observed over the Northern Hemisphere continents in the winter following the 1991 eruption …
Climate impacts from large volcanic eruptions in a high‐resolution climate model: The importance of forcing structure
Explosivevolcanic eruptions have large climate impacts and can serve as observable tests
of the climatic response to radiative forcing. Using a high‐resolution climate model, we …
of the climatic response to radiative forcing. Using a high‐resolution climate model, we …