Impact of cloud-borne aerosol representation on aerosol direct and indirect effects

The C-ToF-AMS usually has two di ff erent operational modes: (i) the MS (Mass Spectrum) mode which is used to collect averaged mass spectra of the non-refractory aerosol and can

It is shown that subgrid treatment of cloud activation and autoconversion of cloud water to rain reduce the impact of anthropogenic aerosols on cloud properties and thus reduce

The C-ToF-AMS usually have two different operational mode: The MS (Mass Spectrum) mode which is used to collect averaged mass spectra of the non-refractory aerosol and can provide

this section we focus on four simulations that represent well the sensitivity of the cloud and precipitation properties to aerosol loading through the modification of aerosol

Absolute error (in km) in the cloud top height retrieval with SNGome as function of cloud top height and optical thickness... 1, but as a function of solar zenith angle in

The second aerosol indirect e ff ect – the cloud life-time or Albrecht-e ff ect – in- volves aerosol particles altering the cloud macro-structure (Albrecht, 1989; Pincus and

the ambiguity of the ACI empirical form (Eq. 5), we quantify the relation between cloud and aerosol properties with statistical parameters making only the assumption that the

P ¨oschl, U.: Aerosol- and updraft-limited regimes of cloud droplet formation: influence of par- ticle number, size and hygroscopicity on the activation of cloud condensation