Bounding global aerosol radiative forcing of climate change
Aerosols interact with radiation and clouds. Substantial progress made over the past 40
years in observing, understanding, and modeling these processes helped quantify the …
years in observing, understanding, and modeling these processes helped quantify the …
A chronology of global air quality
Air pollution has been recognized as a threat to human health since the time of Hippocrates,
ca 400 BC. Successive written accounts of air pollution occur in different countries through …
ca 400 BC. Successive written accounts of air pollution occur in different countries through …
Short-Lived Climate Forcers (Chapter 6)
Short‑lived climate forcers (SLCFs) affect climate and are, in most cases, also air pollutants.
They include aerosols (sulphate, nitrate, ammonium, carbonaceous aerosols, mineral dust …
They include aerosols (sulphate, nitrate, ammonium, carbonaceous aerosols, mineral dust …
Direct radiative effects of airborne microplastics
Microplastics are now recognized as widespread contaminants in the atmosphere, where,
due to their small size and low density, they can be transported with winds around the …
due to their small size and low density, they can be transported with winds around the …
The contribution of global aviation to anthropogenic climate forcing for 2000 to 2018
Global aviation operations contribute to anthropogenic climate change via a complex set of
processes that lead to a net surface warming. Of importance are aviation emissions of …
processes that lead to a net surface warming. Of importance are aviation emissions of …
[HTML][HTML] Future warming from global food consumption
Food consumption is a major source of greenhouse gas (GHG) emissions, and evaluating its
future warming impact is crucial for guiding climate mitigation action. However, the lack of …
future warming impact is crucial for guiding climate mitigation action. However, the lack of …
Map** carbon accumulation potential from global natural forest regrowth
To constrain global warming, we must strongly curtail greenhouse gas emissions and
capture excess atmospheric carbon dioxide,. Regrowing natural forests is a prominent …
capture excess atmospheric carbon dioxide,. Regrowing natural forests is a prominent …
The Community Land Model version 5: Description of new features, benchmarking, and impact of forcing uncertainty
Abstract The Community Land Model (CLM) is the land component of the Community Earth
System Model (CESM) and is used in several global and regional modeling systems. In this …
System Model (CESM) and is used in several global and regional modeling systems. In this …
[HTML][HTML] Contribution of the world's main dust source regions to the global cycle of desert dust
Even though desert dust is the most abundant aerosol by mass in Earth's atmosphere, the
relative contributions of the world's major source regions to the global dust cycle remain …
relative contributions of the world's major source regions to the global dust cycle remain …
[HTML][HTML] Effective radiative forcing and adjustments in CMIP6 models
The effective radiative forcing, which includes the instantaneous forcing plus adjustments
from the atmosphere and surface, has emerged as the key metric of evaluating human and …
from the atmosphere and surface, has emerged as the key metric of evaluating human and …