Colloquium
Location
Physics : 401
Date & Time
February 26, 2014, 3:30 pm – 5:00 pm
Description
ABSTRACT: It is increasingly realized that clouds are at the heart of physical climate science. They are the most important player in the energy balance of the Earth by interacting with both shortwave and longwave radiation. Tiny changes in cloud properties can have major consequences for our climate.
Here I concentrate on how aerosols affect clouds, the
so-called aerosol indirect effects (AIEs), which remain one of the most
uncertain factors in our scientific understanding and projection of climate
change. Two cloud regimes will be discussed.
In one, aerosols invigorate maritime tropical convection at
a large scale. The invigoration effect manifests in characters of precipitation
radar reflectivity vertical profiles, cloud top ice particle size and cloud
glaciation temperature. Furthermore, lightning, as a hallmark of strong
convection, increases at a rate of 20-40 times per unit increase of aerosol
optical depth. Aerosol-induced lightning changes also have interesting
implications for ozone chemistry and wildfire activity.
In the other, aerosols change cloud properties of trade
cumuli at a large scale. They decreased cloud droplet size, decreased
precipitation efficiency and increased cloud amount. In addition we find
significantly higher cloud tops for polluted clouds. Changes in cloud
properties caused by aerosols perturbed the energy balance by more than 20Wm-2,
almost an order of magnitude higher than aerosol direct forcing alone. It
highlights the strong leverage of AIE in this cloud regime. Furthermore, the
precipitation reduction associated with enhanced aerosol leads to large changes
in the energetics of air-sea exchange within trade wind boundary layer.
Results from both regimes open up new opportunities for
future research in reducing uncertainty surrounding AIEs and climate adaptation/mitigation.
Location: Physics, Room 401