Atmospheric Chemistry and Physics (Jul 2020)
Multidecadal trend analysis of in situ aerosol radiative properties around the world
- M. Collaud Coen,
- E. Andrews,
- E. Andrews,
- A. Alastuey,
- T. P. Arsov,
- J. Backman,
- B. T. Brem,
- N. Bukowiecki,
- C. Couret,
- K. Eleftheriadis,
- H. Flentje,
- M. Fiebig,
- M. Gysel-Beer,
- J. L. Hand,
- A. Hoffer,
- R. Hooda,
- R. Hooda,
- C. Hueglin,
- W. Joubert,
- M. Keywood,
- J. E. Kim,
- S.-W. Kim,
- C. Labuschagne,
- N.-H. Lin,
- Y. Lin,
- C. Lund Myhre,
- K. Luoma,
- H. Lyamani,
- H. Lyamani,
- A. Marinoni,
- O. L. Mayol-Bracero,
- N. Mihalopoulos,
- M. Pandolfi,
- N. Prats,
- A. J. Prenni,
- J.-P. Putaud,
- L. Ries,
- F. Reisen,
- K. Sellegri,
- S. Sharma,
- P. Sheridan,
- J. P. Sherman,
- J. Sun,
- G. Titos,
- G. Titos,
- E. Torres,
- T. Tuch,
- R. Weller,
- A. Wiedensohler,
- P. Zieger,
- P. Zieger,
- P. Laj,
- P. Laj,
- P. Laj
Affiliations
- M. Collaud Coen
- Federal Office of Meteorology and Climatology, MeteoSwiss, Payerne, Switzerland
- E. Andrews
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- E. Andrews
- NOAA/Global Monitoring Laboratory, Boulder, CO, USA
- A. Alastuey
- Institute of Environmental Assessment and Water Research (IDAEA), Spanish Research Council (CSIC), Barcelona, Spain
- T. P. Arsov
- Institute for Nuclear Research and Nuclear Energy, Bulgarian Academy of Sciences, Sofia, Bulgaria
- J. Backman
- Atmospheric composition research, Finnish Meteorological Institute, Helsinki, Finland
- B. T. Brem
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen PSI, Switzerland
- N. Bukowiecki
- Atmospheric Sciences, Department of Environmental Sciences, University of Basel, Basel, Switzerland
- C. Couret
- German Environment Agency (UBA), Zugspitze, Germany
- K. Eleftheriadis
- Institute of Nuclear and Radiological Science & Technology, Energy & Safety N.C.S.R. “Demokritos”, Attiki, Greece
- H. Flentje
- German Weather Service, Meteorological Observatory Hohenpeissenberg, Hohenpeißenberg, Germany
- M. Fiebig
- NILU – Norwegian Institute for Air Research, Kjeller, Norway
- M. Gysel-Beer
- Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen PSI, Switzerland
- J. L. Hand
- Cooperative Institute for Research in the Atmosphere (CIRA), Colorado State University, Fort Collins, CO, USA
- A. Hoffer
- MTA-PE Air Chemistry Research Group, Veszprém, Hungary
- R. Hooda
- Atmospheric composition research, Finnish Meteorological Institute, Helsinki, Finland
- R. Hooda
- The Energy and Resources Institute, IHC, Lodhi Road, New Delhi, India
- C. Hueglin
- Empa, Swiss Federal Laboratories for Materials Science and Technology, Duebendorf, Switzerland
- W. Joubert
- South African Weather Service, Research Department, Stellenbosch, South Africa
- M. Keywood
- CSIRO Oceans and Atmosphere, PMB1 Aspendale VIC, Australia
- J. E. Kim
- Environmental Meteorology Research Division, National Institute of Meteorological Sciences, Seogwipo, Korea
- S.-W. Kim
- School of Earth and Environmental Sciences, Seoul National University, Seoul, Korea
- C. Labuschagne
- South African Weather Service, Research Department, Stellenbosch, South Africa
- N.-H. Lin
- Department of Atmospheric Sciences, National Central University, Taoyuan, Taiwan
- Y. Lin
- NILU – Norwegian Institute for Air Research, Kjeller, Norway
- C. Lund Myhre
- NILU – Norwegian Institute for Air Research, Kjeller, Norway
- K. Luoma
- Institute for Atmospheric and Earth System Research, University of Helsinki, Helsinki, Finland
- H. Lyamani
- Andalusian Institute for Earth System Research, IISTA-CEAMA, University of Granada, Junta de Andalucía, Granada, Spain
- H. Lyamani
- Department of Applied Physics, University of Granada, Granada, Spain
- A. Marinoni
- Institute of Atmospheric Sciences and Climate, National Research Council of Italy, Bologna, Italy
- O. L. Mayol-Bracero
- University of Puerto Rico, Rio Piedras Campus, San Juan, Puerto Rico
- N. Mihalopoulos
- Environmental Chemistry Processes Laboratory, Department of Chemistry, University of Crete, Heraklion, Greece
- M. Pandolfi
- Institute of Environmental Assessment and Water Research (IDAEA), Spanish Research Council (CSIC), Barcelona, Spain
- N. Prats
- Izaña Atmospheric Research Center, State Meteorological Agency (AEMET), Tenerife, Spain
- A. J. Prenni
- National Park Service, Air Resources Division, Lakewood, CO, USA
- J.-P. Putaud
- European Commission, Joint Research Centre (JRC), Ispra, Italy
- L. Ries
- German Environment Agency (UBA), Zugspitze, Germany
- F. Reisen
- CSIRO Oceans and Atmosphere, PMB1 Aspendale VIC, Australia
- K. Sellegri
- Université Clermont Auvergne, CNRS, Laboratoire de Météorologie Physique (LaMP), Clermont-Ferrand, France
- S. Sharma
- Climate Chemistry Measurements Research, Climate Research Division, Environment and Climate Change Canada, Toronto, Canada
- P. Sheridan
- NOAA/Global Monitoring Laboratory, Boulder, CO, USA
- J. P. Sherman
- Department of Physics and Astronomy, Appalachian State University, Boone, NC, USA
- J. Sun
- State Key Laboratory of Severe Weather & Key Laboratory of Atmospheric Chemistry of CMA, Chinese Academy of Meteorological Sciences, Beijing, China
- G. Titos
- Andalusian Institute for Earth System Research, IISTA-CEAMA, University of Granada, Junta de Andalucía, Granada, Spain
- G. Titos
- Department of Applied Physics, University of Granada, Granada, Spain
- E. Torres
- University of Puerto Rico, Rio Piedras Campus, San Juan, Puerto Rico
- T. Tuch
- Leibniz Institute for Tropospheric Research (TROPOS), Leipzig, Germany
- R. Weller
- Glaciology Department, Alfred-Wegener-Institut Helmholtz Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
- A. Wiedensohler
- Leibniz Institute for Tropospheric Research (TROPOS), Leipzig, Germany
- P. Zieger
- Department of Environmental Science and Analytical Chemistry, Stockholm University, Stockholm, Sweden
- P. Zieger
- Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
- P. Laj
- Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, IGE, 38000 Grenoble, France
- P. Laj
- CNR-ISAC, National Research Council of Italy – Institute of Atmospheric Sciences and Climate, Bologna, Italy
- P. Laj
- University of Helsinki, Atmospheric Science division, Helsinki, Finland
- DOI
- https://doi.org/10.5194/acp-20-8867-2020
- Journal volume & issue
-
Vol. 20
pp. 8867 – 8908
Abstract
In order to assess the evolution of aerosol parameters affecting climate change, a long-term trend analysis of aerosol optical properties was performed on time series from 52 stations situated across five continents. The time series of measured scattering, backscattering and absorption coefficients as well as the derived single scattering albedo, backscattering fraction, scattering and absorption Ångström exponents covered at least 10 years and up to 40 years for some stations. The non-parametric seasonal Mann–Kendall (MK) statistical test associated with several pre-whitening methods and with Sen's slope was used as the main trend analysis method. Comparisons with general least mean square associated with autoregressive bootstrap (GLS/ARB) and with standard least mean square analysis (LMS) enabled confirmation of the detected MK statistically significant trends and the assessment of advantages and limitations of each method. Currently, scattering and backscattering coefficient trends are mostly decreasing in Europe and North America and are not statistically significant in Asia, while polar stations exhibit a mix of increasing and decreasing trends. A few increasing trends are also found at some stations in North America and Australia. Absorption coefficient time series also exhibit primarily decreasing trends. For single scattering albedo, 52 % of the sites exhibit statistically significant positive trends, mostly in Asia, eastern/northern Europe and the Arctic, 22 % of sites exhibit statistically significant negative trends, mostly in central Europe and central North America, while the remaining 26 % of sites have trends which are not statistically significant. In addition to evaluating trends for the overall time series, the evolution of the trends in sequential 10-year segments was also analyzed. For scattering and backscattering, statistically significant increasing 10-year trends are primarily found for earlier periods (10-year trends ending in 2010–2015) for polar stations and Mauna Loa. For most of the stations, the present-day statistically significant decreasing 10-year trends of the single scattering albedo were preceded by not statistically significant and statistically significant increasing 10-year trends. The effect of air pollution abatement policies in continental North America is very obvious in the 10-year trends of the scattering coefficient – there is a shift to statistically significant negative trends in 2009–2012 for all stations in the eastern and central USA. This long-term trend analysis of aerosol radiative properties with a broad spatial coverage provides insight into potential aerosol effects on climate changes.