TY - JOUR
T1 - Comparison of the SAWNUC model with CLOUD measurements of sulphuric acid-water nucleation
AU - Ehrhart, Sebastian
AU - Ickes, Luisa
AU - Almeida, Joao
AU - Amorim, Antonio
AU - Barmet, Peter
AU - Bianchi, Federico
AU - Dommen, Josef
AU - Dunne, Eimear M.
AU - Duplissy, Jonathan
AU - Franchin, Alessandro
AU - Kangasluoma, Juha
AU - Kirkby, Jasper
AU - Kürten, Andreas
AU - Kupc, Agnieszka
AU - Lehtipalo, Katrianne
AU - Nieminen, Tuomo
AU - Riccobono, Francesco
AU - Rondo, Linda
AU - Schobesberger, Siegfried
AU - Steiner, Gerhard
AU - Tomé, António
AU - Wimmer, Daniela
AU - Baltensperger, Urs
AU - Wagner, Paul E.
AU - Curtius, Joachim
N1 - Publisher Copyright:
© 2016. American Geophysical Union. All Rights Reserved.
PY - 2016/10/27
Y1 - 2016/10/27
N2 - Binary nucleation of sulphuric acid-water particles is expected to be an important process in the free troposphere at low temperatures. SAWNUC (Sulphuric Acid Water Nucleation) is a model of binary nucleation that is based on laboratory measurements of the binding energies of sulphuric acid and water in charged and neutral clusters. Predictions of SAWNUC are compared for the first time comprehensively with experimental binary nucleation data from the CLOUD chamber at European Organization for Nuclear Research. The experimental measurements span a temperature range of 208-292 K, sulphuric acid concentrations from 1.106 to 1.109 cm-3, and distinguish between ion-induced and neutral nucleation. Good agreement, within a factor of 5, is found between the experimental and modeled formation rates for ion-induced nucleation at 278 K and below and for neutral nucleation at 208 and 223 K. Differences at warm temperatures are attributed to ammonia contamination which was indicated by the presence of ammonia-sulphuric acid clusters, detected by an Atmospheric Pressure Interface Time of Flight (APi-TOF) mass spectrometer. APi-TOF measurements of the sulphuric acid ion cluster distributions ((H2SO4)i. HSO-4 with i = 0, 1, …, 10) show qualitative agreement with the SAWNUC ion cluster distributions. Remaining differences between the measured and modeled distributions are most likely due to fragmentation in the APi-TOF. The CLOUD results are in good agreement with previously measured cluster binding energies and show the SAWNUC model to be a good representation of ion-induced and neutral binary nucleation of sulphuric acid-water clusters in the middle and upper troposphere.
AB - Binary nucleation of sulphuric acid-water particles is expected to be an important process in the free troposphere at low temperatures. SAWNUC (Sulphuric Acid Water Nucleation) is a model of binary nucleation that is based on laboratory measurements of the binding energies of sulphuric acid and water in charged and neutral clusters. Predictions of SAWNUC are compared for the first time comprehensively with experimental binary nucleation data from the CLOUD chamber at European Organization for Nuclear Research. The experimental measurements span a temperature range of 208-292 K, sulphuric acid concentrations from 1.106 to 1.109 cm-3, and distinguish between ion-induced and neutral nucleation. Good agreement, within a factor of 5, is found between the experimental and modeled formation rates for ion-induced nucleation at 278 K and below and for neutral nucleation at 208 and 223 K. Differences at warm temperatures are attributed to ammonia contamination which was indicated by the presence of ammonia-sulphuric acid clusters, detected by an Atmospheric Pressure Interface Time of Flight (APi-TOF) mass spectrometer. APi-TOF measurements of the sulphuric acid ion cluster distributions ((H2SO4)i. HSO-4 with i = 0, 1, …, 10) show qualitative agreement with the SAWNUC ion cluster distributions. Remaining differences between the measured and modeled distributions are most likely due to fragmentation in the APi-TOF. The CLOUD results are in good agreement with previously measured cluster binding energies and show the SAWNUC model to be a good representation of ion-induced and neutral binary nucleation of sulphuric acid-water clusters in the middle and upper troposphere.
UR - https://www.scopus.com/pages/publications/84995694801
U2 - 10.1002/2015JD023723
DO - 10.1002/2015JD023723
M3 - Article
AN - SCOPUS:84995694801
SN - 0148-0227
VL - 121
SP - 12,401-12,414
JO - Journal of Geophysical Research
JF - Journal of Geophysical Research
IS - 20
ER -