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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 …
[HTML][HTML] Opportunistic experiments to constrain aerosol effective radiative forcing
Aerosol–cloud interactions (ACIs) are considered to be the most uncertain driver of present-
day radiative forcing due to human activities. The nonlinearity of cloud-state changes to …
day radiative forcing due to human activities. The nonlinearity of cloud-state changes to …
An underestimated negative cloud feedback from cloud lifetime changes
As the atmosphere warms, part of the cloud population shifts from ice and mixed-phase
('cold') to liquid ('warm') clouds. Because warm clouds are more reflective and longer-lived …
('cold') to liquid ('warm') clouds. Because warm clouds are more reflective and longer-lived …
Hydrological consequences of solar geoengineering
As atmospheric carbon dioxide concentrations rise and climate change becomes more
destructive, geoengineering has become a subject of serious consideration. By reflecting a …
destructive, geoengineering has become a subject of serious consideration. By reflecting a …
Constraining the aerosol influence on cloud liquid water path
The impact of aerosols on cloud properties is one of the largest uncertainties in the
anthropogenic radiative forcing of the climate. Significant progress has been made in …
anthropogenic radiative forcing of the climate. Significant progress has been made in …
Aerosol-cloud-climate cooling overestimated by ship-track data
The effect of anthropogenic aerosol on the reflectivity of stratocumulus cloud decks through
changes in cloud amount is a major uncertainty in climate projections. In frequently …
changes in cloud amount is a major uncertainty in climate projections. In frequently …
[HTML][HTML] The CLoud–Aerosol–Radiation interaction and forcing: Year 2017 (CLARIFY-2017) measurement campaign
The representations of clouds, aerosols, and cloud–aerosol–radiation impacts remain some
of the largest uncertainties in climate change, limiting our ability to accurately reconstruct …
of the largest uncertainties in climate change, limiting our ability to accurately reconstruct …
Substantial cloud brightening from ship** in subtropical low clouds
The influence of aerosol particles on cloud reflectivity remains one of the largest sources of
uncertainty in our understanding of anthropogenic climate change. Commercial ship** …
uncertainty in our understanding of anthropogenic climate change. Commercial ship** …
Radiative forcing of climate: The historical evolution of the radiative forcing concept, the forcing agents and their quantification, and applications
We describe the historical evolution of the conceptualization, formulation, quantification,
application, and utilization of “radiative forcing”(RF) of Earth's climate. Basic theories of …
application, and utilization of “radiative forcing”(RF) of Earth's climate. Basic theories of …
Albedo susceptibility of northeastern Pacific stratocumulus: the role of covarying meteorological conditions
Quantification of the radiative adjustment of marine low-clouds to aerosol perturbations,
regionally and globally, remains the largest source of uncertainty in assessing current and …
regionally and globally, remains the largest source of uncertainty in assessing current and …