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Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss M. Collaud Coen E. Andrews, C. Lund Myhre, J. Hand, M. Pandolfi, and P. Laj and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative properties over the world (52 stations) [email protected] Collaud Coen et al., ACPD, 2020 Analysed aerosol properties: Scattering and backscattering coef. Absorption coef. Single scattering albedo Scattering and absorption Ångström exponent Backscattering fraction Methodology: Detection of rupture by visual inspection + station history Mann-Kendall with three prewhitening methods Sen’s slope LMS and GLS/ARB
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Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

Oct 08, 2020

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Page 1: Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

Federal Department of Home Affairs FDHA

Federal Office of Meteorology and Climatology MeteoSwiss

M. Collaud Coen

E. Andrews, C. Lund Myhre, J. Hand, M. Pandolfi, and P. Laj

and the SARGAN group: trend analysis of aerosol radiative properties

Multidecadal trend analysis of in-situ aerosol

radiative properties over the world (52 stations)

[email protected] Coen et al., ACPD, 2020

Analysed aerosol properties:

Scattering and backscattering coef.

Absorption coef.

Single scattering albedo

Scattering and absorption Ångström exponent

Backscattering fraction

Methodology:

Detection of rupture by visual

inspection + station history

Mann-Kendall with three

prewhitening methods

Sen’s slope

LMS and GLS/ARB

Page 2: Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

EGU, Mai 2020Collaud Coen et al., ACPD, 2020

Present day (2016-2018) scattering coef. trend

49% ss negative trends (mostly in Europa, North America)

13% ss positive

38% not ss

Scattering coefficient trend [Mm-1/y]

Page 3: Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

EGU, Mai 2020Collaud Coen et al., ACPD, 2020

60% ss negative (also in Asia)

36% not ss

3% ss positive (by only one method)

Absorption coef. [Mm-1/y]

Present day (2016-2018) absorption coef. trend

Page 4: Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

EGU, Mai 2020Collaud Coen et al., ACPD, 2020

Present day single scattering albedo trends

18% ss negative trend

(mostly in North America and Western Europa)

52% ss positive trend

30% not ss trend

SSA= scattering/(scattering + absorption)

Page 5: Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

EGU, Mai 2020Collaud Coen et al., ACPD, 2020

Mean trend [%/y]

Regions Scattering coef. Absorption coef. Single scattering albedo

nb tot/ss all ss nb tot/ss all Ss nb tot/ss all Ss

all 37/23 -2.11 -2.85 33/21 -2.94 -4.02 27/19 0.02 0.01

Africa 1/0 -4.6 1/1 -3.84 ) -3.84 1/0 -0.02

Asia 3/0 -1.3 3/2 -3.31 -4.83 3/3 0.12 0.12

Europe 12/8 -2.92 -4.03 15/11 -3.72 -4.45 11/8 -0.03 -0.09

N.-America 14/10 -2.66 -3.66 6/2 -1.85 -4.24 6/5 -0.01 -0.01

Pacific 2/1 0.96 3.57 2/1 -1.4 -3.74 2/1 0.13 0.27

Polar regions 5/4 0.15 -0.05 6/4 -2.25 -2.47 4/2 0.05 0.11

Page 6: Multidecadal trend analysis of in-situ aerosol radiative ...and the SARGAN group: trend analysis of aerosol radiative properties Multidecadal trend analysis of in-situ aerosol radiative

EGU, Mai 2020Collaud Coen et al., ACPD, 2020

• Decrease of aerosol burden

• Larger decrease of the absorption coef. (mainly driven by black

carbon) than the scattering coef.

• 50% of ss positive SSA trend (increase of the aerosol negative

climate forcing)

• 20% of ss negative SSA trend (decrease of the aerosol

negative climate forcing).

• Environmental pollution regulations have positive effects

for health and the environment but may have an adverse

effect on efforts to reduce climate change.

Conclusion