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Sulfuric acid condensation sink calculated for the Arctic Ocean 2018 expedition

Andrea Baccarini, Julia Schmale, Josef Dommen

Newer versions of this dataset are available

The condensation sink is a measure of the sulfuric acid lifetime against condensation on preexisting aerosol particles. Dimensionally it is the inverse of a time (reported in per second) and it is calculated starting from the aerosol size distribution.

A large condensation sink means that sulfuric acid and other gaseous species with a similarly low volatility (e.g., iodic and methanesufonic acid) will rapidly condense and their atmospheric concentration will decrease.

Measurements were performed on the 4th deck of icebreaker Oden during August and September 2018 along the track of the Arctic Ocean 2018 expedition.

AtmosphereGas phaseAtmospheric gas phase dataAO2018Arctic OceanIcebreaker OdenArctic Ocean 2018Atmospheric ScienceAtmospheric ChemistryAtmospheric PhysicsClouds Aerosol ScienceMicrobiology-Ocean-Cloud-Coupling in the High ArcticMOCCHAHigh ArcticNorth PoleAerosol-Cloud-Interaction 2018Condensation sinkNew particle formation

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Name

ao2018-aerosol-condensation-sink

Version

1

Citation

Andrea Baccarini, Julia Schmale, Josef Dommen (2020) Sulfuric acid condensation sink calculated for the Arctic Ocean 2018 expedition. Dataset version 1. Bolin Centre Database. https://doi.org/10.17043/ao2018-aerosol-condensation-sink-1

References

Baccarini A, Karlsson L, Dommen J, Duplessis P, Vüllers J, Brooks IM, Saiz-Lopez A, Salter M, Tjernström M, Baltensperger U, Zieger P, Schmale J (2020) Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions. Nature Comm. (in press). https://doi.org/10.1038/s41467-020-18551-0

Dal Maso M et al. (2002) Condensation and coagulation sinks and formation of nucleation mode particles in coastal and boreal forest boundary layers. J. Geophys. Res. Atmos. 107, https://doi.org/10.1029/2001JD001053

Data description

The condensation sink was calculated using the merged particle size distribution measured during the campaign. The calculation is based on the work of Dal Maso et al. 2002. The time resolution is 10 minutes and the condensation sink was calculated only for data that were not affected by the ship exhaust.

The datetime is reported as UTC in the format yyyy-mm-dd HH:MM:SS.

Comments

The ship track with latitude and longitude information can be found in the Navigation, meteorological and surface seawater data from the Arctic Ocean 2018 expedition data set.

The merged particle size distribution data used to calculate the condensation sink can be found in the Size distribution of aerosol particles between 2.5 and 920 nm measured during the Arctic Ocean 2018 expedition dataset.

The data creator ORCIDs are the following:

Project

Arctic Ocean 2018. This work was supported by the Swiss National Science Foundation (grant no. 200021_169090), the Swiss Polar Institute, the BNP Paribas Swiss Foundation (Polar Access Fund 2018), the Knut-and-Alice-Wallenberg Foundation within the ACAS project (Arctic Climate Across Scales, project no. 2016.0024), the Bolin Centre for Climate Research (RA2), the Swedish Research Council (project no. 2018-05045 and project no. 2016-05100).

Publisher

Bolin Centre Database

First name

Julia

Last name or organisation

Schmale

Email address

julia.schmale@epfl.ch

Address

Extreme Environments Research Laboratory, EPFL Valais Wallis

Postal code

CH-1951

City

Sion

Country

Switzerland

GCMD science keyword

Earth science > Atmosphere

GCMD location

Ocean > Arctic Ocean

Dataset language

English

Begin date

2018-08-02

End date

2018-09-19

DOI

10.17043/ao2018-aerosol-condensation-sink-1

Time

2020-09-23T10:00:39.743607+00:00

Versions

  • 1 2022-01-26T13:47:47.726277+00:00
  • 1 2021-12-03T16:09:29.762374+00:00
  • 1 2021-10-29T06:23:12.267616+00:00
  • 1 2021-10-26T09:31:53.500557+00:00
  • 1 2020-09-23T10:00:39.743607+00:00
  • 1 2020-09-23T10:00:39+00:00