In this talk, I will begin by discussing the physical processes that govern the competition between heterogeneous and homogeneous ice nucleation in upper tropospheric cirrus clouds. Next, I will review the current knowledge of low-temperature ice nucleation from laboratory experiments and field measurements. I will then discuss the uncertainties and deficiencies in representations of cirrus processes in global models used to estimate the climate impacts of changes in cirrus clouds. Lastly, I will review the critical field measurements needed to advance our understanding of cirrus and their susceptibility to changes in aerosol properties
In this study the effect of dust aerosol on upper tropospheric cirrus clouds through heterogeneous i...
A parametrization of cirrus clouds formed by homogeneous nucleation is improved so that it can be us...
A multiple-mode ice microphysical scheme is applied in the European Centre/Hamburg (ECHAM) general c...
The relative importance of heterogeneous and homogeneous ice nucleation for cirrus formation remains...
One of the proposed concepts for mitigating the warming effect of increasing greenhouse gases is see...
The goal of this chapter is to synthesize information about what is now known about one of the three...
A parametrization of cirrus clouds formed by homogeneous nucleation is improved so that it can be us...
[1] Motivated by the need to study the climatic impact of aerosol-related cirrus cloud changes, a ph...
[1] Many factors control the ice supersaturation and microphysical properties in cirrus clouds. We e...
For application to Global Climate Models, large scale numerical models of cirrus cloud formation and...
Paper associated with the CWVC (Clouds, Water Vapour and Climate) dataset held on the CEDA archive
Along with minimizing parameter uncertainty, understanding the cause of temporal and spatial variab...
In order to study aerosol–cloud interactions in cirrus clouds, we apply a new multiple-mode ice micr...
Cirrus ice crystals are produced heterogeneously on ice-nucleating particles (INPs) and homogeneousl...
Numerical simulations of cirrus formation in the tropical tropopause layer (TTL) are used to evaluat...
In this study the effect of dust aerosol on upper tropospheric cirrus clouds through heterogeneous i...
A parametrization of cirrus clouds formed by homogeneous nucleation is improved so that it can be us...
A multiple-mode ice microphysical scheme is applied in the European Centre/Hamburg (ECHAM) general c...
The relative importance of heterogeneous and homogeneous ice nucleation for cirrus formation remains...
One of the proposed concepts for mitigating the warming effect of increasing greenhouse gases is see...
The goal of this chapter is to synthesize information about what is now known about one of the three...
A parametrization of cirrus clouds formed by homogeneous nucleation is improved so that it can be us...
[1] Motivated by the need to study the climatic impact of aerosol-related cirrus cloud changes, a ph...
[1] Many factors control the ice supersaturation and microphysical properties in cirrus clouds. We e...
For application to Global Climate Models, large scale numerical models of cirrus cloud formation and...
Paper associated with the CWVC (Clouds, Water Vapour and Climate) dataset held on the CEDA archive
Along with minimizing parameter uncertainty, understanding the cause of temporal and spatial variab...
In order to study aerosol–cloud interactions in cirrus clouds, we apply a new multiple-mode ice micr...
Cirrus ice crystals are produced heterogeneously on ice-nucleating particles (INPs) and homogeneousl...
Numerical simulations of cirrus formation in the tropical tropopause layer (TTL) are used to evaluat...
In this study the effect of dust aerosol on upper tropospheric cirrus clouds through heterogeneous i...
A parametrization of cirrus clouds formed by homogeneous nucleation is improved so that it can be us...
A multiple-mode ice microphysical scheme is applied in the European Centre/Hamburg (ECHAM) general c...