Aerosol indirect effects in a multi-scale aerosol-climate model PNNL-MMF

In that paper, several cloud fields with the same stochastic properties as real clouds are generated assuming variable cloud tops, vertical profile of water droplet, mixed phase,

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

A nucleation scavenging scheme that diagnoses cloud scavenging ratios for aerosol mass and number distributions based on cloud droplet and ice crystal number concen- trations has

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

We find that neglecting transport of cloud-borne particles introduces little error, but that diagnosing cloud- borne particles produces global mean biases of 20% and lo- cal errors

Relationship between aerosol number concentration and cloud droplet number concen- tration (CDNC) with (a) showing that the volcanically induced cloud albedo e ff ect is larger

We have seen that aerosol effects on accumulated surface precipitation are small, and we have explained this by the micro- and macrophysical buffers. Does the near-surface

mixing ratio of 5 hydrometeors (cloud water, cloud ice, rain water, snow, graupel/hail) in every time step using prognostic equation saturation process and microphysical in-