While multiple studies have shown the Northern Hemisphere plays a stronger role than the Southern Hemisphere in transient climate change, this had not been included in calculations of the effect of
atmospheric aerosols on climate sensitivity.
Not exact matches
And by carefully measuring and modeling the resulting changes in
atmospheric composition, scientists could improve their estimate of how sensitive Earth's
climate is to CO2, said lead author Joyce Penner, a professor of
atmospheric science at the University of Michigan whose work focuses
on improving global
climate models and their ability to model the interplay between clouds and
aerosol particles.
«Scientists have talked about Arctic melting and albedo decrease for nearly 50 years,» said Ramanathan, a distinguished professor of
climate and
atmospheric sciences at Scripps who has previously conducted similar research
on the global dimming effects of
aerosols.
ARO scientists monitor a range of
atmospheric phenomena, from the influence of gases and
aerosols on Earth's
climate to the impact of pollutants in the atmosphere.
Sally, who was nominated by Dr. Beat Schmid, Associate Director,
Atmospheric Sciences and Global Change Division, was honored for her exceptional contribution in the field of
atmospheric science, particularly in her efforts to improve understanding of the radiative effect of clouds and
aerosols on the Earth's atmosphere and their representation in
climate models.
However, to make
climate models more accurate, we are focused
on developing a better understanding of the dynamics of organic
aerosols formed from plant - based organic vapors and their interaction with
aerosols emitted from human activities,» said Dr. Chen Song, a PNNL
atmospheric scientist.
Because small - scale
climate features, such as clouds and
atmospheric aerosol particles, have a large impact
on global
climate, it's important to improve the methods used to represent those
climate features in the models.
PNNL is using an integrative research approach that draws
on our depth and breadth of capabilities in
atmospheric chemistry,
climate physics, modeling, and measurement to address critical scientific questions related to the role of
aerosols in the
climate system.
Vision PNNL will take a leadership role in the incorporation of
aerosols into
climate models, through integrative research
on atmospheric aerosol interactions and through development of innovative instrumentation and measurement techniques.
The top priorities should be reducing uncertainties in
climate sensitivity, getting a better understanding of the effect of
climate change
on atmospheric circulation (critical for understanding of regional
climate change, changes in extremes) and reducing uncertainties in radiative forcing — particularly those associated with
aerosols.
Solar activity impacts
on climate are a fascinating topic, and encompass direct radiative processes, indirect effects via
atmospheric chemistry and (potentially)
aerosol formation effects.
It is my understanding that the uncertainties regarding
climate sensitivity to a nominal 2XCO2 forcing is primarily a function of the uncertainties in (1) future
atmospheric aerosol concentrations; both sulfate - type (cooling) and black carbon - type (warming), (2) feedbacks associated with
aerosol effects
on the properties of clouds (e.g. will cloud droplets become more reflective?)
Basic physical science considerations, exploratory
climate modeling, and the impacts of volcanic
aerosols on climate all suggest that SWCE could partially compensate for some effects — particularly net global warming — of increased
atmospheric CO2.
Surely after decades of satellite measurements, countless field experiments, and numerous finescale modeling studies that have repeatedly highlighted basic deficiencies in the ability of comprehensive
climate models to represent processes contributing to
atmospheric aerosol forcing, it is time to give up
on the fantasy that somehow their output can be accepted at face value.»
The focus of this physical
climate model is
on the role of
aerosols,
aerosol - cloud interactions, and
atmospheric chemistry in
climate variability and
climate change.
Heterogeneous ice nucleation
on atmospheric aerosols: a review of results from laboratory experiments / C. Hoose & O. Mohler Institute for Meteorology and
Climate Research —
Atmospheric Aerosol Research, Karlsruhe Institute of Technology, Karlsruhe, Germany / Published: 29 October 2012 Abstract: A small subset of the atmospheric aerosol population has the ability to induce ice formation at conditions under which ice would not form without them (heteroge - neous ice nucle
Aerosol Research, Karlsruhe Institute of Technology, Karlsruhe, Germany / Published: 29 October 2012 Abstract: A small subset of the
atmospheric aerosol population has the ability to induce ice formation at conditions under which ice would not form without them (heteroge - neous ice nucle
aerosol population has the ability to induce ice formation at conditions under which ice would not form without them (heteroge - neous ice nucleation).
«Scientists have talked about Arctic melting and albedo decrease for nearly 50 years,» said Ramanathan, a distinguished professor of
climate and
atmospheric sciences who has previously conducted similar research
on the global dimming effects of
aerosols.
Emissions scenarios were converted to projections of
atmospheric GHG and
aerosol concentrations, radiative forcing of the
climate, effects
on regional
climate, and climatic effects
on global sea level (IPCC, 2001a).
My research is focused
on the
climate effects of
atmospheric aerosol particles and
on broader interconnections within the
climate system.