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GLOMAP
Global Model of Aerosol Processes
Science highlights
The highlights are ordered most recent first.
Proceedings of the National Academy: The role of organics in aerosol particle formation
Southern hemisphere wind speed trends cause aerosol forcing over last two decades
First quantification of global
CCN
sources
Global estimate of cloud drop concentrations
The concept of
CCN
formation potential
Boundary layer nucleation impacts the long term change in cloud drop number
Do high latitude forests warm or cool the climate?
Iron fertilsation as a climate geoengineering option
A new estimate of the contribution of
DMS
to the
CCN
annual cycle
Quantification of a significant marine organic aerosol source
Comparison of bin and modal aerosol schemes
First global estimate of
CCN
from boundary layer nucleation
Large contribution of boundary layer nucleation to global aerosol
Oxidant limitation controls global sulphate aerosol changes
First global model synthesis of marine boundary layer aerosol measurements
Arctic haze sensitive to aerosol wet scavenging
Modelling dust aerosol during
ACE
-ASIA
Key uncertainties in modelling
CCN
Vertical profiles of aerosol number concentrations
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Pages in this section
Modeling Boundary Layer Particle Formation
Oxidant limitation on sulphate trends
Marine Boundary Layer Aerosol
Key uncertainties to model CCN
Vertical profile of aerosol number
Global modelling of Arctic aerosol
Modelling dust aerosol during ACE ASIA
CCN from boundary layer nucleation
First comparison of bin and modal aerosol schemes
Quantification of a significant marine organic aerosol source
A new estimate of the contribution of DMS to the CCN annual cycle
Iron fertilisation as a climate geoengineering option
Do high latitude forests warm or cool climate?
Boundary layer nucleation influences the long term change in cloud drop number
The concept of "CCN formation potential"
First estimate of global cloud drop concentrations
First quantification of global CCN sources
Southern hemisphere wind speed trends cause aerosol forcing over last two decades
The role of organics in aerosol particle formation
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