Composition-Climate Interactions: The recent past

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Composition-Climate Interactions: The recent past Peter Braesicke I Fügen Sie auf der Masterfolie ein frei wählbares Bild ein (z.b. passend zum Vortrag) KIT Universität des Landes Baden-Württemberg und nationales Forschungszentrum in der Helmholtz-Gemeinschaft www.kit.edu

Structure Composition-Climate Interactions (with a focus on ozone and the Arctic) (and in three parts) Introduction Structure of the atmosphere Why does ozone matter? Modelling the atmosphere The recent past Observations (an aside: Antarctic climate change) Simulations of the recent past Expectations for the future Common sense (ozone recovery) Projecting the future (surprises?) 2

Polar Meteorology and Ozone 3

Zonal Mean Total Column Ozone Trends 4

Regional Total Column Ozone Trends Regional (trend) assessments are becoming more important. After the ozone assessment (2014) is before the next one Example: Grey crosses: not significant! 1995-2013 Coldewey-Egbers et al., GRL, 2014 5

Role of Natural Variability ENSO signal: Detection and attribution of natural variability is important! Coldewey-Egbers et al., GRL, 2014 6

Christophe Lerot, BIRA/IASB Excursion to the Southern Hemisphere ESA Ozone_CCI 7

Temperatures in PSCs PSCs over Kiruna WMO, 2014 8

Catalytic Ozone Destruction PSCs allow the formation of ClO and BrO WMO, 2014 9

Observed Ozone and Temperature Change ERA-Interim Reality: Mean(1998 to 2002) - Mean(1979 to 1983) Ozone Difference [%] 90º-75ºS Temp. Difference [K] 90º-75ºS James Keeble 10

Observed circulation and surface changes ERA-Interim Reality: Mean(1998 to 2002) - Mean(1979 to 1983) Height Difference [m] 90º-75ºS Surface Temp. Difference [K] December James Keeble 11

Understanding: Designing experiments http://www.ukca.ac.uk/wiki/index.php/ukca Model: UMUKCA @ N48L60 3.75 x2.5, 0 84km CheS Chemistry (Look-up J) CheST+ Chemistry (Fast-Jx) Boundary conditions: Hadley Centre SSTs/SI Atmosphere Ocean Composition Model Time slices for 2000 conditions 12

Modelled ozone loss and response Ozone Difference [%] 90º-75ºS Height Difference [m] 90º-75ºS Temperature Difference [K] 13

ΔEPF Effects on surface climate ~60ºS Δ TP Height Keeble et al., ACP, 2014 14

Antarctic Ozone and Climate WMO, 2014 15

Movie Time Monthly mean temperatures [K] at 30hPa Total column ozone [DU] (integrated from the TOA to the surface) 16

Radiative Forcing Annual mean radiative forcing due to stratospheric ozone changes between 1979 1981 and 1995 1997 WMO, 2014 17

Modelled Ozone Trends Braesicke and Pyle, QJRMS, 2004 18

Mid-Latitude Ozone Change Braesicke and Pyle, GRL, 2003 19

Temperature Trends Shine et al., QJRMS, 2003 20

Jet Shifts WMO, 2014 21

Ozone and Climate (Change) WMO, 2014 22

HALO Research Aircraft Gimballed Limb Observer for Radiance Imaging of the Atmosphere (GLORIA) 23

POLSTRACC Winter 2015/16 24

The importance of model resolution Preliminary result by Björn-Martin Sinnhuber 25

Peter Braesicke peter.braesicke@kit.edu http://www.imk-asf.kit.edu Thank you for your attention! QUESTIONS? A GREAT WIND IS BLOWING, AND THAT GIVES YOU EITHER IMAGINATION OR A HEADACHE. CATHERINE II OF RUSSIA (1729-1796) 26