Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign

Fog-induced visibility reduction is responsible for a variety of hazards in the transport sector. Therefore there is a large demand for an improved understanding of fog formation and thus improved forecasts. Improved fog forecasts require a better understanding of the numerous complex mechanisms dur...

Full description

Bibliographic Details
Main Authors: E. Hammer, M. Gysel, G. C. Roberts, T. Elias, J. Hofer, C. R. Hoyle, N. Bukowiecki, J.-C. Dupont, F. Burnet, U. Baltensperger, E. Weingartner
Format: Article
Language:English
Published: Copernicus Publications 2014-10-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/14/10517/2014/acp-14-10517-2014.pdf
_version_ 1828254842458472448
author E. Hammer
M. Gysel
G. C. Roberts
T. Elias
J. Hofer
C. R. Hoyle
N. Bukowiecki
J.-C. Dupont
F. Burnet
U. Baltensperger
E. Weingartner
author_facet E. Hammer
M. Gysel
G. C. Roberts
T. Elias
J. Hofer
C. R. Hoyle
N. Bukowiecki
J.-C. Dupont
F. Burnet
U. Baltensperger
E. Weingartner
author_sort E. Hammer
collection DOAJ
description Fog-induced visibility reduction is responsible for a variety of hazards in the transport sector. Therefore there is a large demand for an improved understanding of fog formation and thus improved forecasts. Improved fog forecasts require a better understanding of the numerous complex mechanisms during the fog life cycle. During winter 2012/13 a field campaign called ParisFog aiming at fog research took place at SIRTA (Instrumented Site for Atmospheric Remote Sensing Research). SIRTA is located about 20 km southwest of the Paris city center, France, in a semi-urban environment. In situ activation properties of the prevailing fog were investigated by measuring (1) total and interstitial (non-activated) dry particle number size distributions behind two different inlet systems; (2) interstitial hydrated aerosol and fog droplet size distributions at ambient conditions; and (3) cloud condensation nuclei (CCN) number concentration at different supersaturations (SS) with a CCN counter. The aerosol particles were characterized regarding their hygroscopic properties, fog droplet activation behavior and contribution to light scattering for 17 developed fog events. Low particle hygroscopicity with an overall median of the hygroscopicity parameter, &kappa;, of 0.14 was found, likely caused by substantial influence from local traffic and wood burning emissions. Measurements of the aerosol size distribution at ambient RH revealed that the critical wet diameter, above which the hydrated aerosols activate to fog droplets, is rather large (with a median value of 2.6&mu;m) and is highly variable (ranging from 1 to 5&mu;m) between the different fog events. Thus, the number of activated fog droplets was very small and the non-activated hydrated particles were found to contribute significantly to the observed light scattering and thus to the reduction in visibility. Combining all experimental data, the effective peak supersaturation, SS<sub>peak</sub>, a measure of the peak supersaturation during the fog formation, was determined. The median SS<sub>peak</sub> value was estimated to be in the range from 0.031 to 0.046% (upper and lower limit estimations), which is in good agreement with previous experimental and modeling studies of fog.
first_indexed 2024-04-13T02:05:04Z
format Article
id doaj.art-98f766ee47904f3d8ff3508bed315a66
institution Directory Open Access Journal
issn 1680-7316
1680-7324
language English
last_indexed 2024-04-13T02:05:04Z
publishDate 2014-10-01
publisher Copernicus Publications
record_format Article
series Atmospheric Chemistry and Physics
spelling doaj.art-98f766ee47904f3d8ff3508bed315a662022-12-22T03:07:30ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242014-10-011419105171053310.5194/acp-14-10517-2014Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaignE. Hammer0M. Gysel1G. C. Roberts2T. Elias3J. Hofer4C. R. Hoyle5N. Bukowiecki6J.-C. Dupont7F. Burnet8U. Baltensperger9E. Weingartner10Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandCNRM/GAME – Meteo-France/CNRS, 42 av. Gaspard Coriolis, 31057 Toulouse, FranceHygeos, 165 Avenue de Bretagne, 59000 Lille, FranceLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandInstitut Pierre-Simon Laplace, Université Versailles Saint Quentin, 78280 Guyancourt, FranceCNRM/GAME – Meteo-France/CNRS, 42 av. Gaspard Coriolis, 31057 Toulouse, FranceLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandLaboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, SwitzerlandFog-induced visibility reduction is responsible for a variety of hazards in the transport sector. Therefore there is a large demand for an improved understanding of fog formation and thus improved forecasts. Improved fog forecasts require a better understanding of the numerous complex mechanisms during the fog life cycle. During winter 2012/13 a field campaign called ParisFog aiming at fog research took place at SIRTA (Instrumented Site for Atmospheric Remote Sensing Research). SIRTA is located about 20 km southwest of the Paris city center, France, in a semi-urban environment. In situ activation properties of the prevailing fog were investigated by measuring (1) total and interstitial (non-activated) dry particle number size distributions behind two different inlet systems; (2) interstitial hydrated aerosol and fog droplet size distributions at ambient conditions; and (3) cloud condensation nuclei (CCN) number concentration at different supersaturations (SS) with a CCN counter. The aerosol particles were characterized regarding their hygroscopic properties, fog droplet activation behavior and contribution to light scattering for 17 developed fog events. Low particle hygroscopicity with an overall median of the hygroscopicity parameter, &kappa;, of 0.14 was found, likely caused by substantial influence from local traffic and wood burning emissions. Measurements of the aerosol size distribution at ambient RH revealed that the critical wet diameter, above which the hydrated aerosols activate to fog droplets, is rather large (with a median value of 2.6&mu;m) and is highly variable (ranging from 1 to 5&mu;m) between the different fog events. Thus, the number of activated fog droplets was very small and the non-activated hydrated particles were found to contribute significantly to the observed light scattering and thus to the reduction in visibility. Combining all experimental data, the effective peak supersaturation, SS<sub>peak</sub>, a measure of the peak supersaturation during the fog formation, was determined. The median SS<sub>peak</sub> value was estimated to be in the range from 0.031 to 0.046% (upper and lower limit estimations), which is in good agreement with previous experimental and modeling studies of fog.http://www.atmos-chem-phys.net/14/10517/2014/acp-14-10517-2014.pdf
spellingShingle E. Hammer
M. Gysel
G. C. Roberts
T. Elias
J. Hofer
C. R. Hoyle
N. Bukowiecki
J.-C. Dupont
F. Burnet
U. Baltensperger
E. Weingartner
Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign
Atmospheric Chemistry and Physics
title Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign
title_full Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign
title_fullStr Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign
title_full_unstemmed Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign
title_short Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign
title_sort size dependent particle activation properties in fog during the parisfog 2012 13 field campaign
url http://www.atmos-chem-phys.net/14/10517/2014/acp-14-10517-2014.pdf
work_keys_str_mv AT ehammer sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT mgysel sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT gcroberts sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT telias sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT jhofer sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT crhoyle sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT nbukowiecki sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT jcdupont sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT fburnet sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT ubaltensperger sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign
AT eweingartner sizedependentparticleactivationpropertiesinfogduringtheparisfog201213fieldcampaign