Understanding past temperature changes - Update of modeling results -

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Freie Universität Berlin Understanding past temperature changes - Update of modeling results - Ulrike Langematz

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Understanding past temperature changes - Update of modeling results -. Ulrike Langematz. GRIPS ozone perturbation studies CCMVal ongoing activities CCMVal future plans. GRIPS ozone perturbation studies. - PowerPoint PPT Presentation

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Page 1: Understanding past temperature changes - Update of modeling results -

Freie Universität Berlin

Understanding past temperature changes- Update of modeling results -

Ulrike Langematz

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Freie Universität Berlin

GRIPS ozone perturbation studies CCMVal ongoing activities CCMVal future plans

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Freie Universität Berlin

How much of the observed stratospheric thermal and dynamical changes can be attributed to stratospheric ozone changes?

GRIPS ozone perturbation studies

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Models for ozone change studies

GCMs: Atmospheric General Circulation Models, integrated with prescribed ozone perturbations

• from observations (Langematz, 2000; Rosier and Shine, 2000; Ramaswamy and Schwarzkopf, 2003; Langematz et al., 2003)

• from offline-CTM calculations (Stolarski et al.; Schwarzkopf et al.)

GCMs with parametrized chemistry (calculated ozone change) (Rind et al., 1998; Shindell et al., 2001)

CCMs: Chemistry Climate Models with interactive chemistry modules (calculated ozone change)

(Austin, 2002; Manzini et al., 2003, ….)

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GCM Ozone perturbations studies

Experimental design

20 year time slice experiments with modified O3 and CO2 in FUB-CMAM

„Change“ ≙ statistical, mean difference 2000 minus 1980

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(WMO, 1998)

Observed O3 trends 1979-1997

Ozone perturbations: Observed trends 1980-2000Constructed O3 trends for GCM

(Langematz, 2000)

annual mean

Two zonal mean ozone trend datasets available:

• Randel and Wu, 2000 • Langematz, 2000

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Annual and global mean temperature change due to observed O3 trend

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Shine et al., 2003

Models using Height-Resolved Observed Ozone Trends Dataset

– 1.25 to – 2.3 K/dec

– 0.25 to – 0.45 K/dec

GCM Ozone Perturbation Studies

SSU 1979-2003

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Shine et al., 2003

Models using Height-Resolved Observed Ozone Trends Dataset

Annual mean temperature change at 50 hPa

?

GCM Ozone Perturbation Studies

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GCM integrations with prescribed ozone changes

• do not reproduce the observed upper stratosphere cooling.

• do reproduce the weak middle atmosphere cooling.

• do not reproduce the lower stratosphere global mean cooling.

• do not reproduce the lower stratosphere mid-latitude cooling.

Main results

Missing processes? GHG? H2O?

Missing feedback? CCMs?

GCM Ozone Perturbation Studies

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2 Goals:

Model assessment Model improvement If model agreement Climate change assessment

GRIPS Task 3c

Coordinated GCM experiments of the period 1980-2000

with prescribed observed ozone changes

GRIPS: GCM Realitiy Intercomparison Project for SPARC (Coordinators: Steven Pawson and Kunihiko Kodera)

Extension of Shine et al., 2003, with focus on dynamics

GCM Ozone Perturbation Studies

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The GRIPS 3c task

Perform two 20 year equilibrium GCM integrations• 1980 control-run • 2000 „ozone change“ run

Only difference between runs: prescribed ozone distribution for radiation code

• 1980: 1980 ozone climatology (zonal & monthly mean)• 2000: 1980 ozone climatology +observed trends 1980-2000

Ozone climatology and trends available from• Langematz (2000) • Randel and Wu (2000)

GCM Ozone Perturbation Studies

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GRIPS Task 3c

New models

CCSR/NIES AGCM • Version 5.7b • T42 L55 (0-83 km)

• O3: climatology and trends: L(2000)

WACCM • NCAR CCM3 + TIME-GCM (Sassi et al. 2002) • T63 L66 (0-140 km)

• O3: climatology and trends: R&W (2000)

Kyushu University GCM • T21L37 (0-83 km) (Miyahara et al., 1995) • O3: climatology and trends: L(2000)

MRI/JMA98 Model • T42 L45 (0-83 km) (Shibata et al., 1999) • O3: AMIP climatology, R&W (2000) trends

New in 2005:

NASA-GSFC: 2 sets of runs using R&W and L- ozone trends (Steven Pawson) UMCAM (Peter Braesicke)

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WACCMNIESMRIKUFUB

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Annual and global mean temperature change(K/decade)

GRIPS Task 3c

–0.9 to –1.5 K/dec

– 0.25 to – 0.48 K/dec

altit

ude

[km

]

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Annual mean temperature change (K/decade)

SSU-satellite data, 1979-97

Scaife et al., 2000

FUB

KU NIES

WACCM MRI

GRIPS Task 3c

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Annual mean temperature change (K/decade)

FUB

KU NIES

WACCM MRI

GRIPS Task 3c

SSU-satellite data, 1979-03

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Lower stratosphere temperature change in NH mid-latitudesK/decade

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FUB-analyses 1979-2000

• Models do not show uniform response. Model deficit? • No model is able to reproduce mid-latitude temperature decrease. No ozone effect!

FUB

KU NIES

WACCM MRI

GRIPS Task 3c

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NCEP-data: 1979-2000

Lower stratosphere temperature change at high latitudes(K/decade)

FUB

KU

WACCM

NIES

MRI

• Models show different cooling due to SH spring ozone depletion. Radiation code? Ozone?• No model reproduces observed NH polar spring cooling. No ozone effect.

GRIPS Task 3c

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Summary

GCM ozone perturbation experiments:

- show consistent response to ozone perturbations- show global stratospheric cooling due to ozone

depletion

- do not explain polar lower stratosphere cooling in NH spring

- do not explain mid-latitude cooling in lower stratosphere

No uniform dynamical signal

Work in progress

GRIPS Task 3c

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Phase 1: Analysis of existing, uncoordinated CCM simulations of the period 1980-1999

different CCMs ! different experimental setups !

Validation of model results by comparison with observations

Goal: Definition of model deficits and suggestions for improvements

Quality and consistency of observational datasets?

CCMVal ongoing activities

CCMVal: CCM Validation activity for SPARC

Funded by EC-project SCOUT-O3 (Stratosphere-Climate Links With Emphasis On The UTLS)

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Previous CCM studies

Annual and global mean temperature change

Shine et al., 2003

Coupled chemistry models

CCMVal ongoing activities

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SCOUT-O3:Participating Chemistry-Climate Models (CCMs)

Acronym Resolution Experiments

EC39T30 (3.75°x3.75°)

L39 (10 hPa, 30 km)

1980-1999

(CFC, GHG, sol, volc, nud-QBO, AMIP-SST)

FUBCMAM CHEMT21 (5.6°x5.6°)

L34 (0.0068 hPa, 83 km)

1980-1999

([CFC], GHG, AMIP-SST)

MAECHAM4CHEMT30 (3.75°x3.75°)

L39 (0.01 hPa, 80 km)

1980-1999

(CFC, GHG, sol, volc, nud-QBO, AMIP-SST)

UMETRAC3.75º x 2.5º

L64 (0.01 hPa, 80 km)

1980-1999

(CFC, GHG, QBO, AMIP-SST)

UMUCAM3.75º x 2.5º

L58 (0.1 hPa, 63 km)

„1990“

(AMIP-SST)

UMSLIMCAT3.75º x 2.5º

L58 (0.1 hPa, 63 km)

1980-1999

(CFC, GHG, QBO, AMIP-SST)

SOCOL

LMD

UiO

U Aquila

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to do:

CCMVal ongoing activities

update Shine et al. CCM figure for CCMval models

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Some results from tropical analyses

CCMVal ongoing activities

Performed within SCOUT-O3 (Workpackage 1.9) at FUB

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Temperature

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Temperature trends 1980-1999

Identical forcings in both CCMsSimilar model formulation

Top at 10 hPa (30 km)High vert. res. in UTLS

Top at 0.01 hPa (80 km)Coarser vert. Res. in UTLS

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Tropopause Temperature

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Temperature trend at 70 hPa

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still to be done:

Global, annual mean temperature trend from CCMVal CCMs (Shine et al. 2003 figure)

CCMVal ongoing activities

appropriate observational data set ?

linear vs. multiple regression analysis ?

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CCMVal future plans

Coordinated reference and scenario CCM simulations for UNEP/WMO2006 Ozone Assessement

Reference simulation for 1980-2050

Identical forcings (provided on CCMVal webpage)

Analyse temperature change in these runs