Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)

Uncertainty in radiative forcing caused by aerosol-cloud interactions is about twice as large as for CO2 and remains the least well understood anthropogenic contribution to climate change. A major cause of uncertainty is the poorly quantified state of aerosols in the pristine preindustrial atmospher...

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Published in:Bulletin of the American Meteorological Society
Main Authors: Schmale, Julia, Baccarini, Andrea, Thurnherr, Iris, Henning, Silvia, Efraim, Avichay, Regayre, Leighton, Bolas, Conor, Hartmann, Markus, Welti, Andre, Lehtipalo, Katrianne, Aemisegger, Franziska, Tatzelt, Christian, Landwehr, Sebastian, Modini, Robin L., Tummon, Fiona, Johnson, Jill S., Harris, Neil, Schnaiter, Martin, Toffoli, Alessandro, Derkani, Marzieh, Bukowiecki, Nicolas, Stratmann, Frank, Dommen, Josef, Baltensperger, Urs, Wernli, Heinz, Rosenfeld, Daniel, Gysel-Beer, Martin, Carslaw, Ken S.
Other Authors: Institute for Atmospheric and Earth System Research (INAR), Department of Physics
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2020
Subjects:
Online Access:http://hdl.handle.net/10138/322097
id ftunivhelsihelda:oai:helda.helsinki.fi:10138/322097
record_format openpolar
institution Open Polar
collection HELDA – University of Helsinki Open Repository
op_collection_id ftunivhelsihelda
language English
topic CLOUD CONDENSATION NUCLEI
WAVE RADIATIVE STRUCTURE
SOUTHERN-OCEAN
PARTICLE NUMBER
SEA-ICE
SIZE DISTRIBUTIONS
EXTRATROPICAL CYCLONES
STRATOCUMULUS CLOUDS
CHEMICAL-COMPOSITION
BOUNDARY-LAYER
114 Physical sciences
spellingShingle CLOUD CONDENSATION NUCLEI
WAVE RADIATIVE STRUCTURE
SOUTHERN-OCEAN
PARTICLE NUMBER
SEA-ICE
SIZE DISTRIBUTIONS
EXTRATROPICAL CYCLONES
STRATOCUMULUS CLOUDS
CHEMICAL-COMPOSITION
BOUNDARY-LAYER
114 Physical sciences
Schmale, Julia
Baccarini, Andrea
Thurnherr, Iris
Henning, Silvia
Efraim, Avichay
Regayre, Leighton
Bolas, Conor
Hartmann, Markus
Welti, Andre
Lehtipalo, Katrianne
Aemisegger, Franziska
Tatzelt, Christian
Landwehr, Sebastian
Modini, Robin L.
Tummon, Fiona
Johnson, Jill S.
Harris, Neil
Schnaiter, Martin
Toffoli, Alessandro
Derkani, Marzieh
Bukowiecki, Nicolas
Stratmann, Frank
Dommen, Josef
Baltensperger, Urs
Wernli, Heinz
Rosenfeld, Daniel
Gysel-Beer, Martin
Carslaw, Ken S.
Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)
topic_facet CLOUD CONDENSATION NUCLEI
WAVE RADIATIVE STRUCTURE
SOUTHERN-OCEAN
PARTICLE NUMBER
SEA-ICE
SIZE DISTRIBUTIONS
EXTRATROPICAL CYCLONES
STRATOCUMULUS CLOUDS
CHEMICAL-COMPOSITION
BOUNDARY-LAYER
114 Physical sciences
description Uncertainty in radiative forcing caused by aerosol-cloud interactions is about twice as large as for CO2 and remains the least well understood anthropogenic contribution to climate change. A major cause of uncertainty is the poorly quantified state of aerosols in the pristine preindustrial atmosphere, which defines the baseline against which anthropogenic effects are calculated. The Southern Ocean is one of the few remaining near-pristine aerosol environments on Earth, but there are very few measurements to help evaluate models. The Antarctic Circumnavigation Expedition: Study of Preindustrial-like Aerosols and their Climate Effects (ACE-SPACE) took place between December 2016 and March 2017 and covered the entire Southern Ocean region (Indian, Pacific, and Atlantic Oceans; length of ship track >33,000 km) including previously unexplored areas. In situ measurements covered aerosol characteristics [e.g., chemical composition, size distributions, and cloud condensation nuclei (CCN) number concentrations], trace gases, and meteorological variables. Remote sensing observations of cloud properties, the physical and microbial ocean state, and back trajectory analyses are used to interpret the in situ data. The contribution of sea spray to CCN in the westerly wind belt can be larger than 50%. The abundance of methanesulfonic acid indicates local and regional microbial influence on CCN abundance in Antarctic coastal waters and in the open ocean. We use the in situ data to evaluate simulated CCN concentrations from a global aerosol model. The extensive, available ACE-SPACE dataset () provides an unprecedented opportunity to evaluate models and to reduce the uncertainty in radiative forcing associated with the natural processes of aerosol emission, formation, transport, and processing occurring over the pristine Southern Ocean. Peer reviewed
author2 Institute for Atmospheric and Earth System Research (INAR)
Department of Physics
format Article in Journal/Newspaper
author Schmale, Julia
Baccarini, Andrea
Thurnherr, Iris
Henning, Silvia
Efraim, Avichay
Regayre, Leighton
Bolas, Conor
Hartmann, Markus
Welti, Andre
Lehtipalo, Katrianne
Aemisegger, Franziska
Tatzelt, Christian
Landwehr, Sebastian
Modini, Robin L.
Tummon, Fiona
Johnson, Jill S.
Harris, Neil
Schnaiter, Martin
Toffoli, Alessandro
Derkani, Marzieh
Bukowiecki, Nicolas
Stratmann, Frank
Dommen, Josef
Baltensperger, Urs
Wernli, Heinz
Rosenfeld, Daniel
Gysel-Beer, Martin
Carslaw, Ken S.
author_facet Schmale, Julia
Baccarini, Andrea
Thurnherr, Iris
Henning, Silvia
Efraim, Avichay
Regayre, Leighton
Bolas, Conor
Hartmann, Markus
Welti, Andre
Lehtipalo, Katrianne
Aemisegger, Franziska
Tatzelt, Christian
Landwehr, Sebastian
Modini, Robin L.
Tummon, Fiona
Johnson, Jill S.
Harris, Neil
Schnaiter, Martin
Toffoli, Alessandro
Derkani, Marzieh
Bukowiecki, Nicolas
Stratmann, Frank
Dommen, Josef
Baltensperger, Urs
Wernli, Heinz
Rosenfeld, Daniel
Gysel-Beer, Martin
Carslaw, Ken S.
author_sort Schmale, Julia
title Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)
title_short Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)
title_full Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)
title_fullStr Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)
title_full_unstemmed Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE)
title_sort overview of the antarctic circumnavigation expedition : study of preindustrial-like aerosols and their climate effects (ace-space)
publisher American Meteorological Society
publishDate 2020
url http://hdl.handle.net/10138/322097
geographic Antarctic
Southern Ocean
The Antarctic
Pacific
Indian
geographic_facet Antarctic
Southern Ocean
The Antarctic
Pacific
Indian
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_relation 10.1175/BAMS-D-18-0187.1
ACE-SPACE, JS, IT, AT, SH, and MD received funding from EPFL, the Swiss Polar Institute, and Ferring Pharmaceuticals. ACE-SPACE was carried out with additional support from the European FP7 project BACCHUS (Grant Agreement 49603445). SL received funding from the Swiss Data Science Center project c17-02. AB received funding from the Swiss National Science Foundation (Grant 200021_169090). FT was supported by the Swiss National Science Foundation (Grant 20F121_138017). The U.K. Natural Environment Research Council sponsored the iDirac development (NE/K016377/1) and the Doctoral Training Partnership for CB. CT received funding from DFG within the SPP 1158 (Grant STR 453/121). KC is currently a Royal Society Wolfson Merit Award holder. LR, JSJ, and KC acknowledge funding from NERC under Grants AEROS, ACID-PRUF, GASSP, and A-CURE (NE/G006172/1, NE/I020059/1, NE/J024252/1, and NE/P013406/1), and were also supported by the U.K.-China Research and Innovation Partnership Fund through the Met Office Climate Science for Service Partnership China as part of the Newton Fund. This work used the ARCHER U.K. National Supercomputing Service, www.archer.ac.uk) and JASMIN super-data-cluster (https://doi.org/10.1109/BigData.2013.6691556), via the Center for Environmental Data Analysis. ARCHER project allocation n02-FREEPPE and the Leadership Project allocation n02-CCPPE were used to create the perturbed parameter ensemble. KL was funded by the European Commission's Horizon 2020 programme (MSCA-IF project Nano-CAVa, 656994). MG received funding from the ERC under Grant ERC-CoG-615922-BLACARAT. We thank MeteoSwiss for providing access to operational ECMWF data.
Schmale , J , Baccarini , A , Thurnherr , I , Henning , S , Efraim , A , Regayre , L , Bolas , C , Hartmann , M , Welti , A , Lehtipalo , K , Aemisegger , F , Tatzelt , C , Landwehr , S , Modini , R L , Tummon , F , Johnson , J S , Harris , N , Schnaiter , M , Toffoli , A , Derkani , M , Bukowiecki , N , Stratmann , F , Dommen , J , Baltensperger , U , Wernli , H , Rosenfeld , D , Gysel-Beer , M & Carslaw , K S 2019 , ' Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE) ' , Bulletin of the American Meteorological Society , vol. 100 , no. 11 , pp. 2260-2283 . https://doi.org/10.1175/BAMS-D-18-0187.1
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container_title Bulletin of the American Meteorological Society
container_volume 100
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container_start_page 2260
op_container_end_page 2283
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spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/322097 2024-01-07T09:40:03+01:00 Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE) Schmale, Julia Baccarini, Andrea Thurnherr, Iris Henning, Silvia Efraim, Avichay Regayre, Leighton Bolas, Conor Hartmann, Markus Welti, Andre Lehtipalo, Katrianne Aemisegger, Franziska Tatzelt, Christian Landwehr, Sebastian Modini, Robin L. Tummon, Fiona Johnson, Jill S. Harris, Neil Schnaiter, Martin Toffoli, Alessandro Derkani, Marzieh Bukowiecki, Nicolas Stratmann, Frank Dommen, Josef Baltensperger, Urs Wernli, Heinz Rosenfeld, Daniel Gysel-Beer, Martin Carslaw, Ken S. Institute for Atmospheric and Earth System Research (INAR) Department of Physics 2020-11-30T01:25:48Z 24 application/pdf http://hdl.handle.net/10138/322097 eng eng American Meteorological Society 10.1175/BAMS-D-18-0187.1 ACE-SPACE, JS, IT, AT, SH, and MD received funding from EPFL, the Swiss Polar Institute, and Ferring Pharmaceuticals. ACE-SPACE was carried out with additional support from the European FP7 project BACCHUS (Grant Agreement 49603445). SL received funding from the Swiss Data Science Center project c17-02. AB received funding from the Swiss National Science Foundation (Grant 200021_169090). FT was supported by the Swiss National Science Foundation (Grant 20F121_138017). The U.K. Natural Environment Research Council sponsored the iDirac development (NE/K016377/1) and the Doctoral Training Partnership for CB. CT received funding from DFG within the SPP 1158 (Grant STR 453/121). KC is currently a Royal Society Wolfson Merit Award holder. LR, JSJ, and KC acknowledge funding from NERC under Grants AEROS, ACID-PRUF, GASSP, and A-CURE (NE/G006172/1, NE/I020059/1, NE/J024252/1, and NE/P013406/1), and were also supported by the U.K.-China Research and Innovation Partnership Fund through the Met Office Climate Science for Service Partnership China as part of the Newton Fund. This work used the ARCHER U.K. National Supercomputing Service, www.archer.ac.uk) and JASMIN super-data-cluster (https://doi.org/10.1109/BigData.2013.6691556), via the Center for Environmental Data Analysis. ARCHER project allocation n02-FREEPPE and the Leadership Project allocation n02-CCPPE were used to create the perturbed parameter ensemble. KL was funded by the European Commission's Horizon 2020 programme (MSCA-IF project Nano-CAVa, 656994). MG received funding from the ERC under Grant ERC-CoG-615922-BLACARAT. We thank MeteoSwiss for providing access to operational ECMWF data. Schmale , J , Baccarini , A , Thurnherr , I , Henning , S , Efraim , A , Regayre , L , Bolas , C , Hartmann , M , Welti , A , Lehtipalo , K , Aemisegger , F , Tatzelt , C , Landwehr , S , Modini , R L , Tummon , F , Johnson , J S , Harris , N , Schnaiter , M , Toffoli , A , Derkani , M , Bukowiecki , N , Stratmann , F , Dommen , J , Baltensperger , U , Wernli , H , Rosenfeld , D , Gysel-Beer , M & Carslaw , K S 2019 , ' Overview of the Antarctic Circumnavigation Expedition : Study of Preindustrial-like Aerosols and Their Climate Effects (ACE-SPACE) ' , Bulletin of the American Meteorological Society , vol. 100 , no. 11 , pp. 2260-2283 . https://doi.org/10.1175/BAMS-D-18-0187.1 ORCID: /0000-0002-1660-2706/work/67132355 2f276a52-04d0-4ce9-81d2-5a7d653462c1 http://hdl.handle.net/10138/322097 000501823300009 unspecified openAccess info:eu-repo/semantics/openAccess CLOUD CONDENSATION NUCLEI WAVE RADIATIVE STRUCTURE SOUTHERN-OCEAN PARTICLE NUMBER SEA-ICE SIZE DISTRIBUTIONS EXTRATROPICAL CYCLONES STRATOCUMULUS CLOUDS CHEMICAL-COMPOSITION BOUNDARY-LAYER 114 Physical sciences Article publishedVersion 2020 ftunivhelsihelda https://doi.org/10.1109/BigData.2013.6691556) 2023-12-14T00:02:40Z Uncertainty in radiative forcing caused by aerosol-cloud interactions is about twice as large as for CO2 and remains the least well understood anthropogenic contribution to climate change. A major cause of uncertainty is the poorly quantified state of aerosols in the pristine preindustrial atmosphere, which defines the baseline against which anthropogenic effects are calculated. The Southern Ocean is one of the few remaining near-pristine aerosol environments on Earth, but there are very few measurements to help evaluate models. The Antarctic Circumnavigation Expedition: Study of Preindustrial-like Aerosols and their Climate Effects (ACE-SPACE) took place between December 2016 and March 2017 and covered the entire Southern Ocean region (Indian, Pacific, and Atlantic Oceans; length of ship track >33,000 km) including previously unexplored areas. In situ measurements covered aerosol characteristics [e.g., chemical composition, size distributions, and cloud condensation nuclei (CCN) number concentrations], trace gases, and meteorological variables. Remote sensing observations of cloud properties, the physical and microbial ocean state, and back trajectory analyses are used to interpret the in situ data. The contribution of sea spray to CCN in the westerly wind belt can be larger than 50%. The abundance of methanesulfonic acid indicates local and regional microbial influence on CCN abundance in Antarctic coastal waters and in the open ocean. We use the in situ data to evaluate simulated CCN concentrations from a global aerosol model. The extensive, available ACE-SPACE dataset () provides an unprecedented opportunity to evaluate models and to reduce the uncertainty in radiative forcing associated with the natural processes of aerosol emission, formation, transport, and processing occurring over the pristine Southern Ocean. Peer reviewed Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean HELDA – University of Helsinki Open Repository Antarctic Southern Ocean The Antarctic Pacific Indian Bulletin of the American Meteorological Society 100 11 2260 2283