Investigation of nucleation events vertical extent: a long term study at two different altitude sites

In this work we present an analysis of the occurrence of nucleation events during more than three years of measurements at two different rural altitude sites, the puy de Dôme research station (1465 m a.s.l.) and the Opme station (660 m a.s.l.), central France. The collected database is a unique comb...

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Main Authors: J. Boulon, K. Sellegri, M. Hervo, D. Picard, J.-M. Pichon, P. Fréville, P. Laj
Format: Article
Language:English
Published: Copernicus Publications 2011-06-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/5625/2011/acp-11-5625-2011.pdf
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author J. Boulon
K. Sellegri
M. Hervo
D. Picard
J.-M. Pichon
P. Fréville
P. Laj
author_facet J. Boulon
K. Sellegri
M. Hervo
D. Picard
J.-M. Pichon
P. Fréville
P. Laj
author_sort J. Boulon
collection DOAJ
description In this work we present an analysis of the occurrence of nucleation events during more than three years of measurements at two different rural altitude sites, the puy de Dôme research station (1465 m a.s.l.) and the Opme station (660 m a.s.l.), central France. The collected database is a unique combination of scanning mobility particle sizer (10–400 nm), air ion spectrometers (from 0.8 to 42 nm for NTP-conditions), and, neutral clusters and air ion spectrometers (from 0.8 to 42 nm for NTP-conditions) measurements at these two different altitudes nearly located research stations, from February 2007 to June 2010. The seasonality of the frequency of nucleation events was studied at the puy de Dôme station and maximum of events frequency was found during early spring and early autumn. During the measurement period, neither the particle formation rates (<span style="border-top: 1px solid #000; color: #000;"><i>J</i></span><sub>2</sub>= 1.382 ± 0.195 s<sup>−1</sup>) nor the growth rates (<span style="border-top: 1px solid #000; color: #000;">GR</span><sub>1.3−20 nm</sub> = 6.20 ± 0.12 nm h<sup>−1</sup>) differ from one site to the other on average. Hovewer, we found that, on 437 sampling days in common to the two sites, the nucleation frequency was higher at the puy de Dôme station (35.9 %, 157 days) than at the low elevation station of Opme (20.8 %, 91 days). LIDAR measurements and the evolution of the potential equivalent temperature revealed that the nucleation could be triggered either (i) within the whole low tropospheric column at the same time from the planetary boundary layer to the top of the interface layer (29.2 %, 47 events), (ii) above the planetary boundary layer upper limit (43.5 %, 70 events), and (iii) at low altitude and then transported, conserving dynamic and properties, at high altitude (24.8 %, 40 events). This is the first time that the vertical extent of nucleation can be studied over a long observational period, allowing for a rigorous statistical analysis of the occurrence of nucleation over the whole lower troposphere. This work highlights the fact that nucleation can occur over a large vertical extent, at least the whole low tropospheric column, and also the fact that it occurs twice as frequently as actually detected in the planetary boundary layer. The role of sulfuric acid and ions in the nucleation process was investigated at the altitude station and no correlation was found between nucleation events and the estimated sulfuric acid concentrations. However, the contribution of ion-induced nucleation was found to be relatively high (12.49 ± 2.03 % of the total nucleation rate).
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spelling doaj.art-070ecd5c402347f5975e4663eed485612022-12-21T22:21:30ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-06-0111125625563910.5194/acp-11-5625-2011Investigation of nucleation events vertical extent: a long term study at two different altitude sitesJ. BoulonK. SellegriM. HervoD. PicardJ.-M. PichonP. FrévilleP. LajIn this work we present an analysis of the occurrence of nucleation events during more than three years of measurements at two different rural altitude sites, the puy de Dôme research station (1465 m a.s.l.) and the Opme station (660 m a.s.l.), central France. The collected database is a unique combination of scanning mobility particle sizer (10–400 nm), air ion spectrometers (from 0.8 to 42 nm for NTP-conditions), and, neutral clusters and air ion spectrometers (from 0.8 to 42 nm for NTP-conditions) measurements at these two different altitudes nearly located research stations, from February 2007 to June 2010. The seasonality of the frequency of nucleation events was studied at the puy de Dôme station and maximum of events frequency was found during early spring and early autumn. During the measurement period, neither the particle formation rates (<span style="border-top: 1px solid #000; color: #000;"><i>J</i></span><sub>2</sub>= 1.382 ± 0.195 s<sup>−1</sup>) nor the growth rates (<span style="border-top: 1px solid #000; color: #000;">GR</span><sub>1.3−20 nm</sub> = 6.20 ± 0.12 nm h<sup>−1</sup>) differ from one site to the other on average. Hovewer, we found that, on 437 sampling days in common to the two sites, the nucleation frequency was higher at the puy de Dôme station (35.9 %, 157 days) than at the low elevation station of Opme (20.8 %, 91 days). LIDAR measurements and the evolution of the potential equivalent temperature revealed that the nucleation could be triggered either (i) within the whole low tropospheric column at the same time from the planetary boundary layer to the top of the interface layer (29.2 %, 47 events), (ii) above the planetary boundary layer upper limit (43.5 %, 70 events), and (iii) at low altitude and then transported, conserving dynamic and properties, at high altitude (24.8 %, 40 events). This is the first time that the vertical extent of nucleation can be studied over a long observational period, allowing for a rigorous statistical analysis of the occurrence of nucleation over the whole lower troposphere. This work highlights the fact that nucleation can occur over a large vertical extent, at least the whole low tropospheric column, and also the fact that it occurs twice as frequently as actually detected in the planetary boundary layer. The role of sulfuric acid and ions in the nucleation process was investigated at the altitude station and no correlation was found between nucleation events and the estimated sulfuric acid concentrations. However, the contribution of ion-induced nucleation was found to be relatively high (12.49 ± 2.03 % of the total nucleation rate).http://www.atmos-chem-phys.net/11/5625/2011/acp-11-5625-2011.pdf
spellingShingle J. Boulon
K. Sellegri
M. Hervo
D. Picard
J.-M. Pichon
P. Fréville
P. Laj
Investigation of nucleation events vertical extent: a long term study at two different altitude sites
Atmospheric Chemistry and Physics
title Investigation of nucleation events vertical extent: a long term study at two different altitude sites
title_full Investigation of nucleation events vertical extent: a long term study at two different altitude sites
title_fullStr Investigation of nucleation events vertical extent: a long term study at two different altitude sites
title_full_unstemmed Investigation of nucleation events vertical extent: a long term study at two different altitude sites
title_short Investigation of nucleation events vertical extent: a long term study at two different altitude sites
title_sort investigation of nucleation events vertical extent a long term study at two different altitude sites
url http://www.atmos-chem-phys.net/11/5625/2011/acp-11-5625-2011.pdf
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