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[PDF] Top 20 CCN activation and cloud processing in sectional aerosol models with low size resolution

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CCN activation and cloud processing in sectional aerosol models with low size resolution

CCN activation and cloud processing in sectional aerosol models with low size resolution

... simplified low resolution model agreed fairly well with the reference model under marine and rural condi- ...tions. In the polluted urban case, the simplified model, which cannot ... See full document

10

Aerosol activation and cloud processing in the global  aerosol-climate model ECHAM5-HAM

Aerosol activation and cloud processing in the global aerosol-climate model ECHAM5-HAM

... decreases with 15 drops/cm 3 or 20%, because less particles from the Aitken and accumulation modes are ...The activation of coarse mode aerosol occurs at relatively small supersaturation ... See full document

11

Parameterization of cloud droplet formation for global and regional models: including adsorption activation from insoluble CCN

Parameterization of cloud droplet formation for global and regional models: including adsorption activation from insoluble CCN

... parameterization and the parcel model for individual Whitby (1978) ...apparent, with an average error of less than 10% (Table ...marine aerosol size distribu- tion, where a systematic ... See full document

40

Microphysical processing of aerosol particles in orographic clouds

Microphysical processing of aerosol particles in orographic clouds

... time in the atmosphere, aerosol par- ticles undergo various modifications which may affect their ability to serve as CCN and ...Thereby, aerosol processing within clouds plays a ... See full document

20

Adaptive method of lines for multi-component aerosol condensational growth and cloud droplet activation

Adaptive method of lines for multi-component aerosol condensational growth and cloud droplet activation

... equally in logarithm of radius and in all cases covered at least two decades of the 1 nm–10 µm size ...the models. The discrepancies between the results obtained with the same ... See full document

45

Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong

Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong

... nm in the hazy period and at ∼ 325 nm in the non-episode ...Sulfate and organics accounted for large mass fractions (78 % in total) during the whole cam- paign as shown in Table ... See full document

16

Tight coupling of particle size, number and composition in atmospheric cloud droplet activation

Tight coupling of particle size, number and composition in atmospheric cloud droplet activation

... area) and with (hatched surface area) an (unrealistically large) influence of surface active material assuming the surface active molecules do not reduce the Raoult effect, and our new formulation ... See full document

8

Chemical composition and sources of coastal marine aerosol particles during the 2008 VOCALS-REx campaign

Chemical composition and sources of coastal marine aerosol particles during the 2008 VOCALS-REx campaign

... particle size distri- butions from east to west on 28 October 2008 were highly uniform evidenced by a near constant droplet mode size at ...µm and a progressively smaller Aitken mode size from ... See full document

16

Importance of including ammonium sulfate ((NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>) aerosols for ice cloud parameterization in GCMs

Importance of including ammonium sulfate ((NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>) aerosols for ice cloud parameterization in GCMs

... (2005) and Lohmann and Hoose (2009) eval- uated the influence of ammonium sulfate aerosols in the ECHAM climate ...Lohmann and Hoose (2009) have produced several improvements in ice ... See full document

11

Comparison of MODIS 3 km and 10 km resolution aerosol optical depth retrievals over land with airborne sunphotometer measurements during ARCTAS summer 2008

Comparison of MODIS 3 km and 10 km resolution aerosol optical depth retrievals over land with airborne sunphotometer measurements during ARCTAS summer 2008

... km aerosol retrieval grid cells, and the location of the P-3/AATS flight track during the ...scene, and it is apparent that the projected P-3 track intersected the plume at the exact time of the ... See full document

24

Aerosol-cloud interaction inferred from MODIS satellite data and global aerosol models

Aerosol-cloud interaction inferred from MODIS satellite data and global aerosol models

... two models. However, the global aerosol modelling (AeroCom) exercise (Textor et ...that in fact the opposite is the case, since Oslo- CTM2 has slightly a larger fraction of coarse mode particles ... See full document

21

Aerosol effects on deep convective clouds: impact of changes in aerosol size distribution and aerosol activation parameterization

Aerosol effects on deep convective clouds: impact of changes in aerosol size distribution and aerosol activation parameterization

... Conant, W. C., Dulac, F., Heintzenberg, J., Heymsfield, A. J., Holben, B., Howell, S., Hudson, J., Jayaraman, A., Kiehl, J. T., Krishnamurti, T. N., Lubin, D., McFarquhar, G., Novakov, T., Ogren, J. A., Podgorny, I. A., ... See full document

34

Size-resolved measurement of the mixing state of soot in the megacity Beijing, China: diurnal cycle, aging and parameterization

Size-resolved measurement of the mixing state of soot in the megacity Beijing, China: diurnal cycle, aging and parameterization

... P ¨oschl, U., Martin, S. T., Sinha, B., Chen, Q., Gunthe, S. S., Huffman, J. A., Borrmann, S., Farmer, D. K., Garland, R. M., Helas, G., Jimenez, J. L., King, S. M., Manzi, A., Mikhailov, E., Pauliquevis, T., Petters, M. ... See full document

44

Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM

Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM

... efficient in the removal of aerosols from the atmosphere, and thus strongly influence global aerosol concentrations, and clouds, and their respective radiative ...forcings. In ... See full document

23

Aerosols indirectly warm the Arctic

Aerosols indirectly warm the Arctic

... with CCN>10 cm −3 will have a net cooling ...increased aerosol loading is the combined result of these two competing ...ASCOS and three previous experiments in the central Arctic ... See full document

22

PDF EN Jornal Brasileiro de Pneumologia 3 18 english

PDF EN Jornal Brasileiro de Pneumologia 3 18 english

... heat and moisture ...reduces aerosol deposition and the number of deposited particles by as much as ...heat and moisture exchangers be removed during ... See full document

1

A statistical analysis of North East Atlantic (submicron) aerosol size distributions

A statistical analysis of North East Atlantic (submicron) aerosol size distributions

... the aerosol size distribution is influenced by air mass origin which determines difference aerosol sources and evolution processes (Dall’Osto et ...each size distribution type over time ... See full document

12

A broad supersaturation scanning (BS2) approach for rapid measurement of aerosol particle hygroscopicity and cloud condensation nuclei activity

A broad supersaturation scanning (BS2) approach for rapid measurement of aerosol particle hygroscopicity and cloud condensation nuclei activity

... O., and Pöschl, ...ysis and modeling of aerosol particle mixing state with regard to hygroscopic growth and CCN activation, ... See full document

18

Effects of boundary layer particle formation on cloud droplet number and changes in cloud albedo from 1850 to 2000

Effects of boundary layer particle formation on cloud droplet number and changes in cloud albedo from 1850 to 2000

... larger in 2000 than in 1850. Large differences in continental CDNC can also be seen in less industrialized regions, like over the equatorial Africa and South ...increases in ... See full document

11

Retrieving aerosol in a cloudy environment: aerosol availability as a function of spatial and temporal resolution

Retrieving aerosol in a cloudy environment: aerosol availability as a function of spatial and temporal resolution

... Yu, H., Kaufman, Y. J., Chin, M., Feingold, G., Remer, L. A., Anderson, T. L., Balkanski, Y., Bel- louin, N., Boucher, O., Christopher, S., DeCola, P., Kahn, R., Koch, D., Loeb, N., Reddy, M. S., Schulz, M., Takemura, ... See full document

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