The impacts of aerosols on climate are significant, but also very uncertain.
[~ 17 model years](Motivation: Variation in the climate response across models will be a function of (a) different climate sensitivity in the GCMs, (b) different
impact of aerosols on climate (due to location with respect to clouds, water uptake, natural aerosols, mixing, etc), and (c) different 3D constituent fields from the composition models.
Not exact matches
«We've shown that under clean and humid conditions, like those that exist over the ocean and some land in the tropics, tiny
aerosols have a big
impact on weather and
climate and can intensify storms a great deal,» said Fan, an expert
on the effects
of pollution
on storms and weather.
Unfortunately, current simulation models, which combine global
climate models with
aerosol transport models, consistently underestimate the amount
of these
aerosols in the Arctic compared to actual measurements during the spring and winter seasons, making it difficult to accurately assess the
impact of these substances
on the
climate.
«There is a link between the chemistry that goes
on in this type
of air motion and the subsequent effects
on the trace gases and
aerosols in the atmosphere that ultimately
impact climate.»
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.
In the tug
of war,
aerosols don't necessarily counter the
impacts of climate change
on sea ice (or the planet as a whole for that matter).
Moving the chemical complexity
of the ocean to the laboratory represented a major advance that will enable many new studies to be performed,» said Kimberly Prather, Distinguished Chair in Atmospheric Chemistry at the University
of California, San Diego and director
of the Center for
Aerosol Impacts on Climate and the Environment, who led the team
of more than 30 scientists involved in this project.
He is particularly interested in the role
of aerosols and clouds in the atmosphere, and has worked
on the processes that describe these components
of the atmosphere, the computational details that are needed to describe them in computer models, and
on their
impact on climate.
These changes made China a unique region to investigate the
impact of aerosols on regional
climate and the hydrological cycle.
From its base in Namibia, the Observations
of Clouds above
Aerosols and their Interactions (ORACLES) study will use airborne instruments this fall to probe the
impact on climate and rainfall
of the interaction between clouds over the southeastern Atlantic Ocean and smoke from vegetation burning in southern Africa.
He is leading projects investigating the
impacts of snow and ice impurities
on climate and water resources, and the
aerosol sub-grid progress and parameterizations in
climate models.
From the Physical Science Basis: «Shindell et al. (2009) estimated the
impact of reactive species emissions
on both gaseous and
aerosol forcing species and found that ozone precursors, including methane, had an additional substantial
climate effect because they increased or decreased the rate
of oxidation
of SO2 to sulphate
aerosol.
'' Nunn - McCurdy certified NPOESS — Priority placed
on continuity
of operational weather measurements — Pre Nunn - McCurdy: 3 orbits and 6 spacecraft — Post Nunn - McCurdy: 2 orbits and 4 spacecraft •
Impacts to
Climate Sensors — Five climate oriented sensors de-manifested • APS (aerosols), TSIS (solar
Climate Sensors — Five
climate oriented sensors de-manifested • APS (aerosols), TSIS (solar
climate oriented sensors de-manifested • APS (
aerosols), TSIS (solar irrad.)
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.
I have devoted 30 years to conducting research
on topics including
climate feedback processes in the Arctic, energy exchange between the ocean and atmosphere, the role
of clouds and
aerosols in the
climate system, and the
impact of climate change
on the characteristics
of tropical cyclones.
I added several comments e.g. about the (minor)
impact of human
aerosols on temperature, which implies that the effect
of GHGs is also less than incorporated in
climate models.
The estimates — based
on analysis
of fire's
impact on emissions
of carbon dioxide, nitrous oxide, and methane; albedo or the reflectivity
of Earth's surface; and release
of aerosols and other particulates — suggest fire plays a major large role in
climate than conventionally believed.
As part
of that calculation, researchers have relied
on simplifying assumptions when accounting for the temperature
impacts of climate drivers other than carbon dioxide, such as tiny particles in the atmosphere known as
aerosols, for example.»
«Evidence for
climate change in the satellite cloud record» «Cloud feedback mechanisms and their representation in global
climate models» «A net decrease in the Earth's cloud,
aerosol, and surface 340 nm reflectivity during the past 33 yr (1979 — 2011)» «New observational evidence for a positive cloud feedback that amplifies the Atlantic Multidecadal Oscillation» «
Impact of dataset choice
on calculations
of the short - term cloud feedback»
Current global
climate models suggest that the water vapor feedback to global warming due to carbon dioxide increases is weak but these models do not fully resolve the tropopause or the cold point, nor do they completely represent the QBO [Quasi Biennial Oscillation], deep convective transport and its linkages to SSTs, or the
impact of aerosol heating
on water input to the stratosphere.
Aerosol collections on the NOAA Ron Brown for subsequent processing of INP activation temperature spectra and composition analyses, add a valuable measurement to the ACAPEX and related CalWater2 (NOAA) studies for use in parameterizing and modeling the impacts of marine boundary layer and other aerosols on climate and radiation via aerosol - indirect effects on mixed phase
Aerosol collections
on the NOAA Ron Brown for subsequent processing
of INP activation temperature spectra and composition analyses, add a valuable measurement to the ACAPEX and related CalWater2 (NOAA) studies for use in parameterizing and modeling the
impacts of marine boundary layer and other
aerosols on climate and radiation via
aerosol - indirect effects on mixed phase
aerosol - indirect effects
on mixed phase clouds.
Pitari, G., E. Mancini, V. Rizi, and D.T. Shindell, 2002:
Impact of future
climate and emission changes
on stratospheric
aerosols and ozone.
Menon, S., and A.D. Del Genio, 2007: Evaluating the
impacts of carbonaceous
aerosols on clouds and
climate.
This section assesses (1) the
impact of meteorological (climatic) factors like wind, temperature and precipitation
on the natural
aerosol burden and (2) possible effects
of aerosols on climate parameters and biogeochemistry.
As is, the huge uncertainty about
aerosols means that in principle net human
impact on climate could have always netted out to something close to zero with most
of the temperature change due to natural trends.
The
impact of aerosols on the atmosphere is widely acknowledged as one
of the most significant and uncertain aspects
of climate change projections.
Aerosol impacts remain a source of major uncertainty in climate prediction in the Intergovernmental Panel on Climate Change (IPCC) 4th Assessment Report (2007).5 Recent and ongoing missions and instruments providing aerosol information include TOMS (1979 --RRB-, AVHRR (1979 --RRB-, MODIS (1999 --RRB-, MISR (1999 --RRB-, POLDER (2002 --RRB-, (A) ATSR (1991 --RRB-, PARASOL (2006 --RRB-, SCIAMACHY (2003 --RRB-, CALIPSO (2006 --RRB-, GLAS (2003 --RRB-, OMI (2004 --RRB-, and AIRS (2002
Aerosol impacts remain a source
of major uncertainty in
climate prediction in the Intergovernmental Panel on Climate Change (IPCC) 4th Assessment Report (2007).5 Recent and ongoing missions and instruments providing aerosol information include TOMS (1979 --RRB-, AVHRR (1979 --RRB-, MODIS (1999 --RRB-, MISR (1999 --RRB-, POLDER (2002 --RRB-, (A) ATSR (1991 --RRB-, PARASOL (2006 --RRB-, SCIAMACHY (2003 --RRB-, CALIPSO (2006 --RRB-, GLAS (2003 --RRB-, OMI (2004 --RRB-, and AIRS (2002
climate prediction in the Intergovernmental Panel
on Climate Change (IPCC) 4th Assessment Report (2007).5 Recent and ongoing missions and instruments providing aerosol information include TOMS (1979 --RRB-, AVHRR (1979 --RRB-, MODIS (1999 --RRB-, MISR (1999 --RRB-, POLDER (2002 --RRB-, (A) ATSR (1991 --RRB-, PARASOL (2006 --RRB-, SCIAMACHY (2003 --RRB-, CALIPSO (2006 --RRB-, GLAS (2003 --RRB-, OMI (2004 --RRB-, and AIRS (2002
Climate Change (IPCC) 4th Assessment Report (2007).5 Recent and ongoing missions and instruments providing
aerosol information include TOMS (1979 --RRB-, AVHRR (1979 --RRB-, MODIS (1999 --RRB-, MISR (1999 --RRB-, POLDER (2002 --RRB-, (A) ATSR (1991 --RRB-, PARASOL (2006 --RRB-, SCIAMACHY (2003 --RRB-, CALIPSO (2006 --RRB-, GLAS (2003 --RRB-, OMI (2004 --RRB-, and AIRS (2002
aerosol information include TOMS (1979 --RRB-, AVHRR (1979 --RRB-, MODIS (1999 --RRB-, MISR (1999 --RRB-, POLDER (2002 --RRB-, (A) ATSR (1991 --RRB-, PARASOL (2006 --RRB-, SCIAMACHY (2003 --RRB-, CALIPSO (2006 --RRB-, GLAS (2003 --RRB-, OMI (2004 --RRB-, and AIRS (2002 --RRB-.
The
aerosol indirect effects are the greatest source
of uncertainty in assessing the human
impact on climate change (reviewed here.
The
climate feedbacks involved with these changes, which are key in understanding the
climate system as a whole, include: + the importance
of aerosol absorption
on climate + the
impact of aerosol deposition which affects biology and, hence, emissions
of aerosols and
aerosol precursors via organic nitrogen, organic phosphorus and iron fertilization + the importance
of land use and land use changes
on natural and anthropogenic
aerosol sources + the SOA sources and
impact on climate, with special attention
on the
impact human activities have
on natural SOA formation In order to quantitatively answer such questions I perform simulations
of the past, present and future atmospheres, and make comparisons with measurements and remote sensing data, all
of which help understand, evaluate and improve the model's parameterizations and performance, and our understanding
of the Earth system.
Topics that I work
on or plan to work in the future include studies
of: + missing
aerosol species and sources, such as the primary oceanic
aerosols and their importance
on the remote marine atmosphere, the in - cloud and
aerosol water aqueous formation
of organic
aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing
aerosol parameterizations, such as the effect
of aerosol mixing
on cloud condensation nuclei and
aerosol absorption, the semi-volatility
of primary organic
aerosols, the importance
of in - canopy processes
on natural terrestrial
aerosol and
aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change
of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance
on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect
on key gas - phase species like ozone + the physical and optical properties
of aerosols, which affect
aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution
of absorbing
aerosols +
aerosol - cloud interactions, which include cloud activation, the
aerosol indirect effect and the
impact of clouds
on aerosol removal + changes
on climate and feedbacks related with all these topics In order to understand the
climate system as a whole, improve the
aerosol representation in the GISS ModelE2 and contribute to future IPCC
climate change assessments and CMIP activities, I am also interested in understanding the importance
of natural and anthropogenic
aerosol changes in the atmosphere
on the terrestrial biosphere, the ocean and
climate.