• Nenhum resultado encontrado

Measurements of cloud condensation nuclei activity and droplet activation kinetics of fresh unprocessed regional dust samples and minerals

N/A
N/A
Protected

Academic year: 2017

Share "Measurements of cloud condensation nuclei activity and droplet activation kinetics of fresh unprocessed regional dust samples and minerals"

Copied!
43
0
0

Texto

Loading

Imagem

Table 2. FHH parameters and exponent comparisons for different regional dusts and individual clays/minerals
Fig. 1. Schematic of the experimental set-up used for size resolved CCN activation and droplet growth kinetics measurements.
Fig. 2. s c −D dry lines for different values of B FHH computed at σ =0.072 J m −2 , T = 298.15 K and A FHH = 2.50
Fig. 3. Activation curves for Soil 2 at s c = 0.3%. Shown are inversions without (blue) and with multiple charge corrections (brown)
+7

Referências

Documentos relacionados

We have investigated the evaporation and cloud forming abil- ity of a series of oxo-dicarboxylic acids: oxosuccinic acid, 2- oxoglutaric acid, 3-oxoglutaric acid, and 4-oxopimelic

We measured the number concentrations of cloud condensation nuclei (CCN) and the size distributions of CCN/CN (CN: condensation nuclei) ratios at supersaturations.. ( SS s) of

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

We use a global aerosol microphysics model to estimate the effect of particle formation through activation nucleation in the boundary layer (BL) on cloud droplet num- ber

As an initial application of the κ -based lookup tables, and to test the role of the parti- cle size distribution and aerosol hygroscopicity, sensitivity simulations were carried

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

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

A simple yet robust air-parcel model of cloud drop formation utilizing the adaptive method of lines was formulated. Implementation of the model was discussed and its source code