Supplementary Material for Estimates of ozone return dates from Chemistry-Climate Model Initiative Simulations

Size: px
Start display at page:

Download "Supplementary Material for Estimates of ozone return dates from Chemistry-Climate Model Initiative Simulations"

Transcription

1 Supplementary Material for Estimates of ozone return dates from Chemistry-Climate Model Initiative Simulations Sandip S. Dhomse 1, Douglas Kinnison 2, Martyn P. Chipperfield 1, Irene Cionni 3, Michaela Hegglin 4, N. Luke Abraham 5,6, Hideharu Akiyoshi 7, Alex T. Archibald 5,6, Ewa M. Bednarz 5, Slimane Bekki 8, Peter Braesicke 9, Neal Butchart 10, Martin Dameris 11, Makoto Deushi 12, Stacy Frith 13, Steven C. Hardiman 10, Birgit Hassler 11, Larry W. Horowitz 14, Rong-Ming Hu 8, Partick Joeckel 11, Beatrice Josse 15, Oliver Kirner 16, Stefanie Kremser 17, Ulrike Langematz 18, Jared Lewis 17, Marion Marchand 8, Meiyun Lin 14,19, Eva Mancini 20, Virginie Marecal 15, Martin Michou 15, Olaf Morgenstern 21, Fiona M. OĆonnor 10, Luke Oman 13, Giovanni Pitari 22, David A. Plummer 23, John A. Pyle 5,6, Laura E. Revell 24,25, Eugene Rozanov 25,26, Robyn Schofield 27,28, Andrea Stenke 25, Kane Stone 27,28, *, Kengo Sudo 29,30, Simone Tilmes 2, Daniele Visioni 20, Yousuke Yamashita 7,30, and Guang Zeng 21 1 School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, U.K. 2 National Center for Atmospheric Research (NCAR), Boulder, Colorado, USA. 3 Agenzia Nazionale per le Nuove Tecnologie, lenergia e lo Sviluppo Economica Sostenible (ENEA), Bologna, Italy. 4 Department of Meteorology, University of Reading, Reading, U.K. 5 Department of Chemistry, University of Cambridge, Lensfield Road, Cambridge, CB2 1EW, U.K. 6 National Centre for Atmospheric Science, U.K. 7 National Institute for Environmental Studies (NIES), Tsukuba, Japan. 8 IPSL/CNRS, Paris, France. 9 IMK-ASF, KIT, Karlsruhe, Germany. 10 Met Office Hadley Centre, Exeter, U.K. 11 Deutsches Zentrum fur Luft- und Raumfahrt (DLR), Institut fur Physik der Atmosphare, Oberpfaffenhofen, Germany. 12 Meteorological Research Institute (MRI), Tsukuba, Japan. 13 NASA/GSFC, USA. 14 NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. 15 Meteo-France, Toulouse, France. 16 Steinbuch Centre for Computing (SCC), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany. 17 Bodeker Scientific, Alexandra 9, New Zealand. 18 Institut für Meteorologie, Freie Universitat Berlin, Berlin, Germany. 19 Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ 08540, USA. 20 Dept. of Physical and Chemical Sciences and Center of Excellence CETEMPS, Universita del láquila, Italy. 21, New Zealand. 22 Department of Physical and Chemical Sciences, Universitat dell Aquila, Italy. 23 Climate Research Division, Environment and Climate Change Canada, Montreal, Canada. 24 Bodeker Scientific, Alexandra, New Zealand. 25 ETH Zurich, Institute for Atmospheric and Climate Science, Zurich, Switzerland. 26 Physikalisch-Meteorologisches Observatorium Davos World Radiation Centre, Davos Dorf, Switzerland. 27 School of Earth Sciences, University of Melbourne, Melbourne, Australia. 28 ARC Centre of Excellence for Climate System Science, Sydney, Australia. 29 Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan. 30 Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan. 1

2 * Now at Massachusetts Institute of Technology (MIT), Boston, Massachusetts, USA Correspondence: Sandip Dhomse, Douglas Kinnison, Martyn Chipperfield This document contains additional figures to support those presented in the main document. For discussion of the figures and references see the main text. 2

3 Arctic (Mar) Arctic (Mar) ACCESS-CCM CESM1-CAM4 CESM1- CHASER-MIROC EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM3 HadGM3-ES IPSL MRI-ESM1r1 -UKCA -CCM IMCAT median MMM SBUV MOD Figure S1. (a) Total column ozone time series (DU) for Arctic in March from 19 individual CCMs for March for the simulations along with observations from the SBUV merged ozone dataset. The MMM, median (MedM) and are shown with thick green, blue and red lines, respectively. Light blue shaded region indicates 10th and 90th percentile range. Light green and red regions show 1-σ variability w.r.t. MMM and mean lines. (b) Same as (a) but adjusted total ozone time series w.r.t. mean observations. The dashed black line indicates 1980 reference value. 3

4 SH midlat SH midlat 340 ACCESS-CCM CESM1-CAM4 CESM1- CHASER-MIROC EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM3 HadGM3-ES IPSL MRI-ESM1r1 -UKCA -CCM IMCAT median MMM SBUV MOD Figure S2. As Figure S1 but for annual mean total column ozone for SH mid-latitudes. 4

5 380 NH midlat (annual) NH midlat (annual) ACCESS-CCM CESM1-CAM4 CESM1- CHASER-MIROC EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM3 HadGM3-ES IPSL MRI-ESM1r1 -UKCA -CCM IMCAT median MMM SBUV MOD Figure S3. As Figure S1 but for annual mean total column ozone for NH mid-latitudes. 5

6 ACCESS-CCM CESM1-CAM4 CESM1- CHASER-MIROC EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM3 HadGM3-ES IPSL MRI-ESM1r1 -UKCA -CCM IMCAT median MMM SBUV MOD Figure S4. As Figure S1 but for annual mean total column ozone for the tropics (20S-20N). 6

7 ACCESS-CCM CESM1-CAM4 CESM1- CHASER-MIROC EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM3 HadGM3-ES IPSL MRI-ESM1r1 -UKCA -CCM IMCAT median MMM SBUV MOD Figure S5. As Figure S1 but for annual mean near global mean (60S-60N) total column ozone. 7

8 SH mid-lat NH mid-lat SH mid-lat REF-C1 REF-C1SD SBUV MOD NH mid-lat REF-C1 REF-C1SD SBUV MOD Figure S6. total column ozone time series (DU) from REF-C1 (blue), REF-C1SD (dark cyan) and (red) simulations for (left) SH mid-latitudes and (right) NH mid-latitudes. Dashed black lines show 1980 reference value for a given zonal latitude band. The top row shows the unadjusted modelled values and the bottom row shows the time series adjusted w.r.t. mean observations. Also shown are merged SBUV observations. 8

9 REF-C1 REF-C1SD SBUV MOD REF-C1 REF-C1SD SBUV MOD Figure S7. As Figure S6 but for the tropics (20S-20N) and near global average (60S-60N). 9

10 tco return dates (senc2fghg) tco return dates (senc2fn2o) SH mid-lat (annual) NH mid-lat (annual) tco return dates (senc2fch4) Arctic (Mar) SH mid-lat (annual) NH mid-lat (annual) tco return dates (senc2rcpch485) Arctic (Mar) SH mid-lat (annual) NH mid-lat (annual) Arctic (Mar) SH mid-lat (annual) NH mid-lat (annual) Arctic (Mar) Figure S8. Estimated return dates (red triangles) of total column ozone from the, SEN-C2-fN2O, SEN-C2-fCH4 and SEN-C2-CH4RCP85 simulations for different latitude bands. The estimated 1-σ uncertainties are shown with vertical black lines. Estimates for individual models are shown with coloured dots. Some individual models do not predict a return of column ozone in the tropics. Return dates from (see Figure 4 in main paper) are shown with grey triangles. 10

11 tco return dates (senc2rcp45) tco return dates (senc2rcp85) SH mid-lat (annual) NH mid-lat (annual) Arctic (Mar) SH mid-lat (annual) NH mid-lat (annual) Arctic (Mar) Figure S9. As Figure S8 but for the SEN-C2-RCP45 and SEN-C2-RCP85 simulations. 11

12 50 hpa o3 (ppm) hpa o3 (ppm) SH midlat 50 hpa o3 (ppm) hpa o3 (ppm) Tropics ACCESS-CCM (annual) 2.4 HadGEM3-ES IMCAT ACCESS-CCM HadGEM3-ES EMAC-L47MA MRI-ESM1r1 Global (annual) EMAC-L47MA MRI-ESM1r1 CESM1-CAM4 EMAC-L90MA -UKCA 2.8 CESM1-CAM4 EMAC-L90MA -UKCA 2.2 CESM1- GEOSCCM GOZCARDS CESM1- GEOSCCM GFDL-AF3/CM3 -CCM GFDL-AF3/CM3 -CCM ACCESS-CCM ACCESS-CCM HadGEM3-ES IMCAT ACCESS-CCM HadGEM3-ES IMCATHadGEM3-ES EMAC-L47MA MRI-ESM1r1 EMAC-L47MA MRI-ESM1r1 CESM1-CAM4 EMAC-L90MA -UKCA EMAC-L47MA CESM1-CAM4 MRI-ESM1r1 EMAC-L90MA -UKCA CESM1- GEOSCCM CESM1-CAM4 GOZCARDS EMAC-L90MA CESM1- -UKCA GEOSCC GFDL-AF3/CM3 -CCM GFDL-AF3/CM3 -CCM CESM1- GEOSCCM GOZCARDS GFDL-AF3/CM3 -CCM 50 hpa o3 (ppm) 2.2 IMCAT GOZCARDS IMCAT GOZCARDS Figure S10. Time series of adjusted ozone at 50 hpa from the simulations for Antarctic, SH midlatitudes, tropics and global mean. The dark red line shows the and the shaded region indicates corresponding 1-σ standard deviation. The reference value for year 1980 is shown with dashed black line. Also shown are observations from the GOZCARDS merged dataset. 12

13 5 hpa o3 (ppm) hpa o3 (ppm) SH midlat 5 hpa o3 (ppm) hpa o3 (ppm) ACCESS-CCM CESM1-CAM4 CESM EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM3 HadGEM3-ES MRI-ESM1r1 -UKCA -CCM IMCAT GOZCARDS IMCAT GOZCARDS 5 hpa o3 (ppm) ACCESS-CCM CESM1-CAM4 CESM1- EMAC-L47MA EMAC-L90MA GEOSCCM GFDL-AF3/CM ACCESS-CCM ACCESS-CCM HadGEM3-ES EMAC-L47MA MRI-ESM1r1 CESM1-CAM4 EMAC-L90MA -UKCA CESM1- GEOSCCM CESM1-CAM4 GFDL-AF3/CM3 -CCM CESM1- HadGEM3-ES MRI-ESM1r1 -UKCA -CCM 7.0 ACCESS-CCM HadGEM3-ES IMCATHadGEM3-ES EMAC-L47MA MRI-ESM1r1 EMAC-L47MA CESM1-CAM4 MRI-ESM1r1 EMAC-L90MA -UKCA EMAC-L90MA CESM1- -UKCA GEOSCC GFDL-AF3/CM3 -CCM GEOSCCM GOZCARDS GFDL-AF3/CM3 -CCM IMCAT GOZCARDS IMCAT GOZCARDS Figure S11. As Figure S10 but for 5 hpa. 13

14 CO2 4 3 RCP6.0 RCP8.5 fixed@1960 CH4 425 N2O PPMV PPMV 2 PPMV Figure S12. Volume mixing ratios (vmrs) of CO 2, CH 4 and N 2O used in the (RCP6.0) scenario (red lines). The values for reference year 1960 are shown with green lines and the CH 4 vmr used in the SEN-C2-CH4RCP85 simulation is shown with an orange line. 14

15 GEOSCCM 500 -UKCA 500 SOCOL 500 tco(du) 500 IMCAT SEN-C2-fCH4 SEN-C2-fN2OrefC2 BSVertOzone senc2fn2o senc2fghgsbuv MODSEN-C2-fN2O senc2fch4 senc2fods senc2ch485 SEN-C2-CH4RCP85 BSVertOzone Figure S13. Evolution of Arctic (March) stratospheric ozone columns (DU) from selected models for, SEN-C2-fCH4, SEN-C2- fn2o and SEN-C2-CH4RCP85 simulations. Also shown are observations 15 from the merged SBUV dataset.

16 GEOSCCM -UKCA SOCOL tco(du) IMCAT SEN-C2-fCH4 SEN-C2-fN2OrefC2 BSVertOzone senc2fn2o senc2fghgsbuv MODSEN-C2-fN2O senc2fch4 senc2fods senc2ch485 SEN-C2-CH4RCP85 BSVertOzone Figure S14. As Figure S13 but for NH mid-latitudes. 16

17 GEOSCCM 220 -UKCA 220 SOCOL tco(du) IMCAT 220 SEN-C2-fCH4 SEN-C2-fN2OrefC2 BSVertOzone senc2fn2o senc2fghgsbuv MODSEN-C2-fN2O senc2fch4 senc2fods senc2ch485 SEN-C2-CH4RCP85 BSVertOzone Figure S15. As Figure S13 but for near-global average (60S-60N). 17

18 SCO return year (senc2fghg) SCO return year (senc2fghg) mean EMAC-L90 CCSR ACCESS EMAC-L90 CCSR mean Arctic (Mar.) ACCESS SCO return year (senc2fghg) SCO return year (senc2fghg) mean EMAC-L90 SH midlat (annual) CCSR ACCESS EMAC-L90 mean NH midlat (annual) ACCESS CCSR Figure S16. Correlation plots of stratospheric column ozone (SCO) return dates from the SEN-C2fGHG simulations against SCO return dates from simulations for individual models within four latitude bands. 18

19 SCO return year (senc2fn2o) SCO return year (senc2fn2o) SOCO CCSR GEOS CHASER CCSR SOCO Arctic (Mar.) GEOS SCO return year (senc2fn2o) SCO return year (senc2fn2o) SH midlat (annual) SOCO GEOS CHASER CCSR CHASER SOCO GEOS NH midlat (annual) CCSR Figure S17. As Figure S16 but for simulation SEN-C2-fN2O. 19

20 SCO return year (senc2fch4) SCO return year (senc2fch4) SOCO CCSR GEOS CHASER CCSR SOCO Arctic (Mar.) GEOS SCO return year (senc2fch4) SCO return year (senc2fch4) SH midlat (annual) SOCO GEOS CCSR CHASER CHASER SOCO GEOS NH midlat (annual) CCSR Figure S18. As Figure S16 but for simulation SEN-C2-fCH4. 20

21 SCO return year (senc2ch485) SCO return year (senc2ch485) SOCO GEOS GEOS Arctic (Mar.) SOCO SCO return year (senc2ch485) SCO return year (senc2ch485) SH midlat (annual) SOCO GEOS SOCO GEOS NH midlat (annual) Figure S19. Same as S16 but for simulation SEN-C2-CH4RCP85. 21

Supplement of Estimates of ozone return dates from Chemistry-Climate Model Initiative simulations

Supplement of Estimates of ozone return dates from Chemistry-Climate Model Initiative simulations Supplement of Atmos. Chem. Phys., 18, 8409 8438, 2018 https://doi.org/10.5194/acp-18-8409-2018-supplement Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement

More information

Future changes in wintertime stratospheric Arctic variability in CCMI models

Future changes in wintertime stratospheric Arctic variability in CCMI models Future changes in wintertime stratospheric Arctic variability in CCMI models B. Ayarzagüena 1, U. Langematz 1, J. Abalichin 1, H. Akiyoshi 2, M. Michou 3, O. Morgenstern 4 & L. Oman 5 1 Institut für Meteorologie,

More information

CCM Modelling : LMDz-Reprobus

CCM Modelling : LMDz-Reprobus CCM Modelling : LMDz-Reprobus Marchand Marion, Slimane Bekki, Franck Lefèvre, François Lott, David Cugnet, Line Jourdain, Perrine Lemmenais, Virginie Poulain, Julien Jumelet, Slimane Bekki, marie-pierre

More information

Radiative forcing from tropospheric and stratospheric ozone

Radiative forcing from tropospheric and stratospheric ozone Radiative forcing from tropospheric and stratospheric ozone 1850-2100 David Stevenson (The University of Edinburgh) I. Cionni, V. Eyring, J. F. Lamarque, W. J. Randel, F. Wu, G. E. Bodeker, T. G. Shepherd,

More information

Drylands face potential threat under 2 C global warming target

Drylands face potential threat under 2 C global warming target In the format provided by the authors and unedited. SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE3275 Drylands face potential threat under 2 C global warming target Jianping Huang 1 *, Haipeng Yu 1,

More information

1" 2" 3" 4" 5" 6" 7" 8" 9" 10" 11" 12" 13" 14" 15" 16" 17" 18" 19" 20" 21" 22" 23" 24" 25" 26" 27" 28" 29" 30" 31" 32" 33" 34" 35"

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 " " 3" " 5" 6" 7" 8" 9" " " " 3" " 5" 6" 7" 8" 9" " " " 3" " 5" 6" 7" 8" 9" 3" 3" 3" 33" 3" 35" Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) Supplemental Online

More information

Impact of wind changes in the upper troposphere lower stratosphere on tropical ozone

Impact of wind changes in the upper troposphere lower stratosphere on tropical ozone Impact of wind changes in the upper troposphere lower stratosphere on tropical ozone Martin Dameris Deutsches Zentrum für Luft- und Raumfahrt (DLR) Institut für Physik der Atmosphäre, Oberpfaffenhofen

More information

Large divergence of satellite and Earth system model estimates of global terrestrial CO 2 fertilization

Large divergence of satellite and Earth system model estimates of global terrestrial CO 2 fertilization Large divergence of satellite and Earth system model estimates of global terrestrial CO 2 fertilization 4 5 W. Kolby Smith 1,2, Sasha C. Reed 3, Cory C. Cleveland 1, Ashley P. Ballantyne 1, William R.L.

More information

CESM2 (WACCM6): Stratospheric Evaluation

CESM2 (WACCM6): Stratospheric Evaluation CESM2 (WACCM6): Stratospheric Evaluation D. Kinnison, M. Mills, R. Garcia, D. Marsh, A. Gettelman, F. Vitt, S. Glanville, C. Bardeen, S. Tilmes, A. Smith, J-F. Lamarque, L. Emmons, A. Conley, J. Richter,

More information

Future freshwater stress for island populations

Future freshwater stress for island populations Future freshwater stress for island populations Kristopher B. Karnauskas, Jeffrey P. Donnelly and Kevin J. Anchukaitis Summary: Top left: Overview map of the four island stations located in the U.S. state

More information

Stratospheric Processes And their Role in Climate (SPARC)

Stratospheric Processes And their Role in Climate (SPARC) Stratospheric Processes And their Role in Climate (SPARC) Co-chairs: Joan Alexander (NWRA) Greg Bodeker (Bodeker Scientific) SPARC Office Director: Johannes Staehelin (ETH Zürich) Other SPARC Office staff:

More information

Assessing and understanding the role of stratospheric changes on decadal climate prediction

Assessing and understanding the role of stratospheric changes on decadal climate prediction MiKlip II-Status seminar, Berlin, 1-3 March 2017 Assessing and understanding the role of stratospheric changes on decadal climate prediction Martin Dameris Deutsches Zentrum für Luft- und Raumfahrt, Institut

More information

Supplement of Insignificant effect of climate change on winter haze pollution in Beijing

Supplement of Insignificant effect of climate change on winter haze pollution in Beijing Supplement of Atmos. Chem. Phys., 18, 17489 17496, 2018 https://doi.org/10.5194/acp-18-17489-2018-supplement Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.

More information

Twenty-first-century projections of North Atlantic tropical storms from CMIP5 models

Twenty-first-century projections of North Atlantic tropical storms from CMIP5 models SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1530 Twenty-first-century projections of North Atlantic tropical storms from CMIP5 models SUPPLEMENTARY FIGURE 1. Annual tropical Atlantic SST anomalies (top

More information

Decadal shifts of East Asian summer monsoon in a climate. model free of explicit GHGs and aerosols

Decadal shifts of East Asian summer monsoon in a climate. model free of explicit GHGs and aerosols Decadal shifts of East Asian summer monsoon in a climate model free of explicit GHGs and aerosols Renping Lin, Jiang Zhu* and Fei Zheng International Center for Climate and Environment Sciences, Institute

More information

Early benefits of mitigation in risk of regional climate extremes

Early benefits of mitigation in risk of regional climate extremes In the format provided by the authors and unedited. DOI: 10.1038/NCLIMATE3259 Early benefits of mitigation in risk of regional climate extremes Andrew Ciavarella 1 *, Peter Stott 1,2 and Jason Lowe 1,3

More information

Desert Amplification in a Warming Climate

Desert Amplification in a Warming Climate Supporting Tables and Figures Desert Amplification in a Warming Climate Liming Zhou Department of Atmospheric and Environmental Sciences, SUNY at Albany, Albany, NY 12222, USA List of supporting tables

More information

Supporting Information for Relation of the double-itcz bias to the atmospheric energy budget in climate models

Supporting Information for Relation of the double-itcz bias to the atmospheric energy budget in climate models GEOPHYSICAL RESEARCH LETTERS Supporting Information for Relation of the double-itcz bias to the atmospheric energy budget in climate models Ori Adam 1, Tapio Schneider 1,2, Florent Brient 1, and Tobias

More information

Snow occurrence changes over the central and eastern United States under future. warming scenarios

Snow occurrence changes over the central and eastern United States under future. warming scenarios Snow occurrence changes over the central and eastern United States under future warming scenarios Liang Ning 1,2,3* and Raymond S. Bradley 2 1 Key Laboratory of Virtual Geographic Environment of Ministry

More information

The Implication of Ural Blocking on the East Asian Winter Climate in CMIP5 Models

The Implication of Ural Blocking on the East Asian Winter Climate in CMIP5 Models The Implication of Ural Blocking on the East Asian Winter Climate in CMIP5 Models Hoffman H. N. Cheung, Wen Zhou (hncheung-c@my.cityu.edu.hk) City University of Hong Kong Shenzhen Institute Guy Carpenter

More information

Reconciling the Observed and Modeled Southern Hemisphere Circulation Response to Volcanic Eruptions Supplemental Material

Reconciling the Observed and Modeled Southern Hemisphere Circulation Response to Volcanic Eruptions Supplemental Material JOURNAL OF GEOPHYSICAL RESEARCH, VOL.???, XXXX, DOI:10.1002/, 1 2 3 Reconciling the Observed and Modeled Southern Hemisphere Circulation Response to Volcanic Eruptions Supplemental Material Marie C. McGraw

More information

Stratosphere troposphere coupling and annular mode variability in chemistry climate models

Stratosphere troposphere coupling and annular mode variability in chemistry climate models JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2009jd013770, 2010 Stratosphere troposphere coupling and annular mode variability in chemistry climate models Edwin P. Gerber, 1 Mark P. Baldwin,

More information

Chemistry Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes

Chemistry Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes VOLUME 23 J O U R N A L O F C L I M A T E 15 OCTOBER 2010 Chemistry Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes NEAL BUTCHART, a I. CIONNI, b V. EYRING,

More information

Trends of Lower- to Mid-Stratospheric Water Vapor Simulated in Chemistry-Climate Models

Trends of Lower- to Mid-Stratospheric Water Vapor Simulated in Chemistry-Climate Models ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2015, VOL. 8, NO. 1, 57 62 Trends of Lower- to Mid-Stratospheric Water Vapor Simulated in Chemistry-Climate Models HU Ding-Zhu 1, HAN Yuan-Yuan 1, SANG Wen-Jun

More information

Geophysical Research Letters

Geophysical Research Letters FRONTIER ARTICLE Key Points: There is substantial improvement in the comparison between modeled and observed stratospheric temperature trends over the satellite era Observations and models show weaker

More information

Evaluation of CMIP5 Simulated Clouds and TOA Radiation Budgets in the SMLs Using NASA Satellite Observations

Evaluation of CMIP5 Simulated Clouds and TOA Radiation Budgets in the SMLs Using NASA Satellite Observations Evaluation of CMIP5 Simulated Clouds and TOA Radiation Budgets in the SMLs Using NASA Satellite Observations Erica K. Dolinar Xiquan Dong and Baike Xi University of North Dakota This talk is based on Dolinar

More information

Improved predictability of the troposphere using stratospheric final warmings

Improved predictability of the troposphere using stratospheric final warmings JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116,, doi:10.1029/2011jd015914, 2011 Improved predictability of the troposphere using stratospheric final warmings Steven C. Hardiman, 1 Neal Butchart, 1 Andrew J.

More information

Multimodel climate and variability of the stratosphere

Multimodel climate and variability of the stratosphere JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116,, doi:10.1029/2010jd014995, 2011 Multimodel climate and variability of the stratosphere N. Butchart, 1 A. J. Charlton Perez, 2 I. Cionni, 3 S. C. Hardiman, 1 P.

More information

Quantitative performance metrics for stratospheric-resolving chemistry-climate models

Quantitative performance metrics for stratospheric-resolving chemistry-climate models Atmos. Chem. Phys., 8, 5699 5713, 2008 Author(s) 2008. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Quantitative performance metrics for

More information

Stratospheric Change and its Role for Climate Prediction (SHARP): A contribution to SPARC

Stratospheric Change and its Role for Climate Prediction (SHARP): A contribution to SPARC Stratospheric Change and its Role for Climate Prediction (SHARP): A contribution to SPARC U. Langematz, Freie Universität Berlin, Germany (ulrike.langematz@met.fu-berlin.de) and the SHARP consortium 32

More information

Changes in the El Nino s spatial structure under global warming. Sang-Wook Yeh Hanyang University, Korea

Changes in the El Nino s spatial structure under global warming. Sang-Wook Yeh Hanyang University, Korea Changes in the El Nino s spatial structure under global warming Sang-Wook Yeh Hanyang University, Korea Changes in El Nino spatial structure Yeh et al. (2009) McPhaden et al. (2009) Why the spatial structure

More information

Characterizing the role of diabatic processes for the modification of mid-latitude Rossby waves and Jetstream winds

Characterizing the role of diabatic processes for the modification of mid-latitude Rossby waves and Jetstream winds Characterizing the role of diabatic processes for the modification of mid-latitude Rossby waves and Jetstream winds Andreas Schäfler 1, George Craig 2, Andreas Dörnbrack 1, Florian Harnisch 4, Uwe Marksteiner

More information

Intensification of the shallow BDC branch: mechanism and consequences for Age of Air

Intensification of the shallow BDC branch: mechanism and consequences for Age of Air Intensification of the shallow BDC branch: mechanism and consequences for Age of Air H. Garny1,2, M. Dameris1, W. Randel2, G. Bodeker3, R. Deckert1 T. Birner4 1 Deutsches Zentrum für Luft und Raumfahrt

More information

Laura Revell, Andrea Stenke, Beiping Luo, Stefanie Kremser, Eugene Rozanov, Timofei Sukhodolov and Thomas Peter

Laura Revell, Andrea Stenke, Beiping Luo, Stefanie Kremser, Eugene Rozanov, Timofei Sukhodolov and Thomas Peter Impacts of Mt. Pinatubo volcanic aerosol on the tropical stratosphere in chemistry-climate model simulations using CCMI and CMIP6 stratospheric aerosol data Laura Revell, Andrea Stenke, Beiping Luo, Stefanie

More information

Stratospheric ozone in the post-cfc era

Stratospheric ozone in the post-cfc era Atmos. Chem. Phys., 9, 2207 2213, 2009 Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Stratospheric ozone in the post-cfc

More information

Multimodel assessment of the upper troposphere and lower stratosphere: Extratropics

Multimodel assessment of the upper troposphere and lower stratosphere: Extratropics JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2010jd013884, 2010 Multimodel assessment of the upper troposphere and lower stratosphere: Extratropics M. I. Hegglin, 1 A. Gettelman, 2 P. Hoor,

More information

INVESTIGATING THE SIMULATIONS OF HYDROLOGICAL and ENERGY CYCLES OF IPCC GCMS OVER THE CONGO AND UPPER BLUE NILE BASINS

INVESTIGATING THE SIMULATIONS OF HYDROLOGICAL and ENERGY CYCLES OF IPCC GCMS OVER THE CONGO AND UPPER BLUE NILE BASINS INVESTIGATING THE SIMULATIONS OF HYDROLOGICAL and ENERGY CYCLES OF IPCC GCMS OVER THE CONGO AND UPPER BLUE NILE BASINS Mohamed Siam, and Elfatih A. B. Eltahir. Civil & Environmental Engineering Department,

More information

S16. ASSESSING THE CONTRIBUTIONS OF EAST AFRICAN AND WEST PACIFIC WARMING TO THE 2014 BOREAL SPRING EAST AFRICAN DROUGHT

S16. ASSESSING THE CONTRIBUTIONS OF EAST AFRICAN AND WEST PACIFIC WARMING TO THE 2014 BOREAL SPRING EAST AFRICAN DROUGHT S6. ASSESSING THE CONTRIBUTIONS OF EAST AFRICAN AND WEST PACIFIC WARMING TO THE 204 BOREAL SPRING EAST AFRICAN DROUGHT Chris Funk, Shraddhanand Shukla, Andy Hoell, and Ben Livneh This document is a supplement

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO1189 Different magnitudes of projected subsurface ocean warming around Greenland and Antarctica Jianjun Yin 1*, Jonathan T. Overpeck 1, Stephen M. Griffies 2,

More information

More extreme precipitation in the world s dry and wet regions

More extreme precipitation in the world s dry and wet regions More extreme precipitation in the world s dry and wet regions Markus G. Donat, Andrew L. Lowry, Lisa V. Alexander, Paul A. O Gorman, Nicola Maher Supplementary Table S1: CMIP5 simulations used in this

More information

Contents of this file

Contents of this file Geophysical Research Letters Supporting Information for Future changes in tropical cyclone activity in high-resolution large-ensemble simulations Kohei Yoshida 1, Masato Sugi 1, Ryo Mizuta 1, Hiroyuki

More information

Supplementary Figure S1: Uncertainty of runoff changes Assessments of. R [mm/yr/k] for each model and the ensemble mean.

Supplementary Figure S1: Uncertainty of runoff changes Assessments of. R [mm/yr/k] for each model and the ensemble mean. Supplementary Figure S1: Uncertainty of runoff changes Assessments of R [mm/yr/k] for each model and the ensemble mean. 1 Supplementary Figure S2: Schematic diagrams of methods The top panels show uncertainty

More information

Impact of Solar and Sulfate Geoengineering on Surface Ozone

Impact of Solar and Sulfate Geoengineering on Surface Ozone Impact of Solar and Sulfate Geoengineering on Surface Ozone Lili Xia 1, Peer J. Nowack 2, Simone Tilmes 3 and Alan Robock 1 1 Department of Environmental Sciences, Rutgers University, New Brunswick, NJ

More information

Composition-Climate Interactions: The recent past

Composition-Climate Interactions: The recent past 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

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION doi:10.1038/nature11576 1. Trend patterns of SST and near-surface air temperature Bucket SST and NMAT have a similar trend pattern particularly in the equatorial Indo- Pacific (Fig. S1), featuring a reduced

More information

Grey swan tropical cyclones

Grey swan tropical cyclones Grey swan tropical cyclones Ning Lin 1* and Kerry Emanuel 2 1 Department of Civil and Environmental Engineering, Princeton University, Princeton, NJ 08544, USA 2 Department of Earth, Atmospheric, and Planetary

More information

L Ordre du Jour / Agenda for CCMI Workshop

L Ordre du Jour / Agenda for CCMI Workshop L Ordre du Jour / Agenda for CCMI Workshop 13-15 Juin/June 2017, Toulouse Mardi 13 Juin / Tuesday 13 June **invited speakers in green 09:00-09:10 Marc Pontaud Béatrice Josse Jean Maziejewski Alison Ming

More information

Supplementary Information for Impacts of a warming marginal sea on torrential rainfall organized under the Asian summer monsoon

Supplementary Information for Impacts of a warming marginal sea on torrential rainfall organized under the Asian summer monsoon 1 2 3 4 5 6 7 8 9 10 11 Supplementary Information for Impacts of a warming marginal sea on torrential rainfall organized under the Asian summer monsoon 12 13 14 Atsuyoshi Manda 1, Hisashi Nakamura 2,4,

More information

Influence of Arctic Stratospheric Ozone on Surface Climate in CCMI models

Influence of Arctic Stratospheric Ozone on Surface Climate in CCMI models Influence of Arctic Stratospheric Ozone on Surface Climate in CCMI models Ohad Harari 1, Chaim I Garfinkel 1, Olaf Morgenstern 2, Guang Zeng 2, Simone Tilmes 3, Douglas Kinnison 3, Makoto Deushi 4, Patrick

More information

Has the ozone hole contributed to increased Antarctic sea ice extent? M.Sigmond and J. Fyfe

Has the ozone hole contributed to increased Antarctic sea ice extent? M.Sigmond and J. Fyfe Has the ozone hole contributed to increased Antarctic sea ice extent? M.Sigmond and J. Fyfe It has been suggested that the increase of Southern Hemisphere sea ice extent since the 1970s can be explained

More information

Agenda for CCMI Workshop May 2014, Lancaster University

Agenda for CCMI Workshop May 2014, Lancaster University Agenda for CCMI Workshop 20-22 May 2014, Lancaster University Tuesday 20 th May Session 1: CCMI - quo vadis? 09:00-09:05 Paul Young Welcome 09:05-09:30 CCMI Co-chairs Goals of the workshop 09:30-09:45

More information

Report on the first SOLARIS workshop 4-6 October 2006, Boulder, Colorado, USA

Report on the first SOLARIS workshop 4-6 October 2006, Boulder, Colorado, USA Report on the first SOLARIS workshop 4-6 October 2006, Boulder, Colorado, USA K. Matthes, Freie Universität Berlin, Institut für Meteorologie, Berlin, Germany and National Center for Atmospheric Research,

More information

The 20th century warming and projections for the 21st century climate in the region of the Ukrainian Antarctic station Akademik Vernadsky

The 20th century warming and projections for the 21st century climate in the region of the Ukrainian Antarctic station Akademik Vernadsky The 20th century warming and projections for the 21st century climate in the region of the Ukrainian Antarctic station Akademik Vernadsky S.V.Krakovska, G.A.Djukel Ukrainian Hydrometeorological Institute,

More information

POLARCAT Model Intercomparison Project (POLMIP)

POLARCAT Model Intercomparison Project (POLMIP) Institute for Climate and Atmospheric Science UNIVERSITY OF LEEDS POLARCAT Model Intercomparison Project (POLMIP) S.R. Arnold 1,2, L.K. Emmons 2, S.A. Monks 1, K.S. Law 3, S. Tilmes 2, S. Turquety 4 J.

More information

Geophysical Research Letters. Supporting Information for. Ozone-induced climate change propped up by the Southern Hemisphere oceanic front

Geophysical Research Letters. Supporting Information for. Ozone-induced climate change propped up by the Southern Hemisphere oceanic front Geophysical Research Letters Supporting Information for Ozone-induced climate change propped up by the Southern Hemisphere oceanic front Authors and affiliations Fumiaki Ogawa, Geophysical Institute, University

More information

SST forcing of Australian rainfall trends

SST forcing of Australian rainfall trends SST forcing of Australian rainfall trends www.cawcr.gov.au Julie Arblaster (with thanks to David Karoly & colleagues at NCAR and BoM) Climate Change Science Team, Bureau of Meteorology Climate Change Prediction

More information

Significant anthropogenic-induced changes. of climate classes since 1950

Significant anthropogenic-induced changes. of climate classes since 1950 Significant anthropogenic-induced changes of climate classes since 95 (Supplementary Information) Duo Chan and Qigang Wu * School of Atmospheric Science, Nanjing University, Hankou Road #22, Nanjing, Jiangsu,

More information

Supplementary Figure 1 Observed change in wind and vertical motion. Anomalies are regime differences between periods and obtained

Supplementary Figure 1 Observed change in wind and vertical motion. Anomalies are regime differences between periods and obtained Supplementary Figure 1 Observed change in wind and vertical motion. Anomalies are regime differences between periods 1999 2013 and 1979 1998 obtained from ERA-interim. Vectors are horizontal wind at 850

More information

Long-term ozone changes and associated climate impacts in CMIP5 simulations

Long-term ozone changes and associated climate impacts in CMIP5 simulations JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES, VOL. 118, 5029 5060, doi:10.1002/jgrd.50316, 2013 Long-term ozone changes and associated climate impacts in CMIP5 simulations V. Eyring, 1 J. M. Arblaster,

More information

Effect of zonal asymmetries in stratospheric ozone on simulated Southern Hemisphere climate trends

Effect of zonal asymmetries in stratospheric ozone on simulated Southern Hemisphere climate trends Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L18701, doi:10.1029/2009gl040419, 2009 Effect of zonal asymmetries in stratospheric ozone on simulated Southern Hemisphere climate trends

More information

Polar vortex variability and stratosphere-troposphere coupling

Polar vortex variability and stratosphere-troposphere coupling FDEPS 2012, Lecture 4 Polar vortex variability and stratosphere-troposphere coupling Ted Shepherd Department of Meteorology University of Reading Polar temperatures at 30 hpa (approx 25 km) Forcing of

More information

JOURNAL OF GEOPHYSICAL RESEARCH

JOURNAL OF GEOPHYSICAL RESEARCH JOURNAL OF GEOPHYSICAL RESEARCH 1 2 Supporting Information for Stratospheric age of air variations between 1600-2100 S. Muthers, 1,2, A. Kuchar 3,4, A. Stenke 3, J. Schmitt 1,2, J. G. Anet 5, C. C. Raible

More information

Statistical downscaling of multivariate wave climate using a weather type approach

Statistical downscaling of multivariate wave climate using a weather type approach COWPLIP Workshop on Coordinated Global Wave Climate Projections Statistical downscaling of multivariate wave climate using a weather type approach Melisa Menendez, Fernando J. Mendez, Cristina Izaguirre,

More information

Attribution of anthropogenic influence on seasonal sea level pressure

Attribution of anthropogenic influence on seasonal sea level pressure Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L23709, doi:10.1029/2009gl041269, 2009 Attribution of anthropogenic influence on seasonal sea level pressure N. P. Gillett 1 and P. A.

More information

Climate Change Scenario, Climate Model and Future Climate Projection

Climate Change Scenario, Climate Model and Future Climate Projection Training on Concept of Climate Change: Impacts, Vulnerability, Adaptation and Mitigation 6 th December 2016, CEGIS, Dhaka Climate Change Scenario, Climate Model and Future Climate Projection A.K.M. Saiful

More information

Understanding the Relation between V PSC and Arctic Ozone Loss

Understanding the Relation between V PSC and Arctic Ozone Loss Understanding the Relation between V PSC and Arctic Ozone Loss Neil Harris European Ozone Research Coordinating Unit Department of Chemistry, University of Cambridge Ralph Lehmann, Markus Rex, Peter von

More information

EXPERT MEETING TO ASSESS PROGRESS MADE IN THE PROCESS TO FORMULATE AND IMPLEMENT ANATIONAL ADAPTATION PANS (NAPs)

EXPERT MEETING TO ASSESS PROGRESS MADE IN THE PROCESS TO FORMULATE AND IMPLEMENT ANATIONAL ADAPTATION PANS (NAPs) EXPERT MEETING TO ASSESS PROGRESS MADE IN THE PROCESS TO FORMULATE AND IMPLEMENT ANATIONAL ADAPTATION PANS (NAPs) LESOTHO'S EXPERIENCE MOKOENA FRANCE MINISTRY OF ENERGY AND METEOROLOGY OUTLINE Key Risks

More information

Robust Arctic sea-ice influence on the frequent Eurasian cold winters in past decades

Robust Arctic sea-ice influence on the frequent Eurasian cold winters in past decades SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2277 Robust Arctic sea-ice influence on the frequent Eurasian cold winters in past decades Masato Mori 1*, Masahiro Watanabe 1, Hideo Shiogama 2, Jun Inoue 3,

More information

Forcing of anthropogenic aerosols on temperature trends of the subthermocline

Forcing of anthropogenic aerosols on temperature trends of the subthermocline Forcing of anthropogenic aerosols on temperature trends of the subthermocline southern Indian Ocean Tim Cowan* 1,2, Wenju Cai 1, Ariaan Purich 1, Leon Rotstayn 1 and Matthew H. England 2 1 CSIRO Marine

More information

Review of the formulation of present generation stratospheric chemistry climate models and associated external forcings

Review of the formulation of present generation stratospheric chemistry climate models and associated external forcings JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2009jd013728, 2010 Review of the formulation of present generation stratospheric chemistry climate models and associated external forcings O. Morgenstern,

More information

Coordinated Ocean-ice Reference Experiments phase II (CORE-II)

Coordinated Ocean-ice Reference Experiments phase II (CORE-II) Coordinated Ocean-ice Reference Experiments phase II (CORE-II) Gokhan Danabasoglu, Stephen G. Yeager, William G. Large National Center for Atmospheric Research, Boulder, CO, USA Stephen M. Griffies NOAA

More information

Future changes in Elevated Stratopause Events

Future changes in Elevated Stratopause Events Future changes in Elevated Stratopause Events Janice Scheffler 1, Ulrike Langematz 1, Yvan J. Orsolini 2, Blanca Ayarzagüena 1 1 Institut für Meteorologie, Freie Universität Berlin 2 Norwegian Institute

More information

Supporting Online Material for

Supporting Online Material for www.sciencemag.org/cgi/content/full/1153966/dc1 Supporting Online Material for The Sensitivity of Polar Ozone Depletion to Proposed Geoengineering Schemes Simone Tilmes,* Rolf Müller, Ross Salawitch *To

More information

Tropospheric Ozone from GOME_2 also in combination with other stratospheric ozone measurements

Tropospheric Ozone from GOME_2 also in combination with other stratospheric ozone measurements Tropospheric Ozone from GOME_2 also in combination with other stratospheric ozone measurements Klaus-Peter Heue 1, Melanie Coldewey-Egbers 1, Andy Delcloo 2, Christophe Lerot 3, Diego Loyola 1, Pieter

More information

Monitoring Climate Change using Satellites: Lessons from MSU

Monitoring Climate Change using Satellites: Lessons from MSU Monitoring Climate Change using Satellites: Lessons from MSU Peter Thorne, Simon Tett Hadley Centre, Met Office, Exeter, UK UAH data from John Christy Residual uncertainty work in collaboration with John

More information

Sophie Oberländer, Ulrike Langematz, Stefanie Meul Institut für Meteorologie, Freie Universität Berlin

Sophie Oberländer, Ulrike Langematz, Stefanie Meul Institut für Meteorologie, Freie Universität Berlin Future changes in the Brewer-Dobson Circulation and possible causes derived from Chemistry-ClimateClimate Model Simulations, Ulrike Langematz, Stefanie Meul Institut für Meteorologie, Freie Universität

More information

Supplementary Material: Characterizing Changes in Drought Risk for the United States from Climate Change [1] October 12, 2010

Supplementary Material: Characterizing Changes in Drought Risk for the United States from Climate Change [1] October 12, 2010 Supplementary Material: Characterizing Changes in Drought Risk for the United States from Climate Change [1] Kenneth Strzepek a, Gary Yohe b, James Neumann c, Brent Boehlert d October 12, 2010 a Visiting

More information

Supplementary Figure 1 A figure of changing surface air temperature and top-1m soil moisture: (A) Annual mean surface air temperature, and (B) top

Supplementary Figure 1 A figure of changing surface air temperature and top-1m soil moisture: (A) Annual mean surface air temperature, and (B) top Supplementary Figure 1 A figure of changing surface air temperature and top-1m soil moisture: (A) Annual mean surface air temperature, and (B) top 1-m soil moisture averaged over California from CESM1.

More information

Analysis of radiative feedbacks in model simulations including interactive chemistry

Analysis of radiative feedbacks in model simulations including interactive chemistry Analysis of radiative feedbacks in model simulations including interactive chemistry Michael Ponater Simone Dietmüller Vanessa Rieger Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institute for Atmospheric

More information

Supplementary Material for On the evaluation of climate model simulated precipitation extremes

Supplementary Material for On the evaluation of climate model simulated precipitation extremes Supplementary Material for On the evaluation of climate model simulated precipitation extremes Andrea Toreti 1 and Philippe Naveau 2 1 European Commission, Joint Research Centre, Ispra (VA), Italy 2 Laboratoire

More information

Baseline Ozone in Western North America: Measurements and Models. David Parrish

Baseline Ozone in Western North America: Measurements and Models. David Parrish Baseline Ozone in Western North America: Measurements and Models David Parrish CIRES University of Colorado NOAA/ESRL Chemical Sciences Division Boulder, Colorado USA Consultant with David.D.Parrish, LLC

More information

NetCDF, NCAR s climate model data, and the IPCC. Gary Strand NCAR/NESL/CGD

NetCDF, NCAR s climate model data, and the IPCC. Gary Strand NCAR/NESL/CGD NetCDF, NCAR s climate model data, and the IPCC Gary Strand NCAR/NESL/CGD NCAR s climate model data A bit of history... 1960s - 1990s Self-designed self-implemented binary formats 1990s-2000s netcdf-3

More information

Impacts of historical ozone changes on climate in GFDL-CM3

Impacts of historical ozone changes on climate in GFDL-CM3 Impacts of historical ozone changes on climate in GFDL-CM3 Larry Horowitz (GFDL) with: Vaishali Naik (GFDL), Pu Lin (CICS), and M. Daniel Schwarzkopf (GFDL) WMO (2014) Figure ADM 5-1 1 Response of tropospheric

More information

Coupled chemistry climate model simulations of the solar cycle in ozone and temperature

Coupled chemistry climate model simulations of the solar cycle in ozone and temperature JOURNAL OF GEOPHYSICAL RESEARCH, VOL., XXXX, DOI:10.1029/, 1 2 Coupled chemistry climate model simulations of the solar cycle in ozone and temperature J. Austin 1, K. Tourpali 2, E. Rozanov 3, H. Akiyoshi

More information

The simulation of the Antarctic ozone hole by chemistry-climate models

The simulation of the Antarctic ozone hole by chemistry-climate models Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics The simulation of the Antarctic ozone hole by chemistry-climate models H.

More information

Supplementary Material for. Atmospheric and Oceanic Origins of Tropical Precipitation Variability

Supplementary Material for. Atmospheric and Oceanic Origins of Tropical Precipitation Variability 1 2 Supplementary Material for Atmospheric and Oceanic Origins of Tropical Precipitation Variability 3 4 Jie He 1, Clara Deser 2 & Brian J. Soden 3 5 6 7 8 9 10 11 1. Princeton University, and NOAA/Geophysical

More information

Polar Ozone Depletion and Trends as Represented by the Whole Atmosphere Community Climate Model (WACCM)

Polar Ozone Depletion and Trends as Represented by the Whole Atmosphere Community Climate Model (WACCM) Polar Ozone Depletion and Trends as Represented by the Whole Atmosphere Community Climate Model (WACCM) Doug Kinnison 1, Susan Solomon 2, Diane Ivy 2, Mike Mills 1, Ryan Neely III 3, and Anja Schmidt 3

More information

Ocean carbon cycle feedbacks in the tropics from CMIP5 models

Ocean carbon cycle feedbacks in the tropics from CMIP5 models WWW.BJERKNES.UIB.NO Ocean carbon cycle feedbacks in the tropics from CMIP5 models Jerry Tjiputra 1, K. Lindsay 2, J. Orr 3, J. Segschneider 4, I. Totterdell 5, and C. Heinze 1 1 Bjerknes Centre for Climate

More information

The SPARC LOTUS Initiative

The SPARC LOTUS Initiative The SPARC LOTUS Initiative Project Leads: I. Petropavlovskikh S. Godin-Beekmann D. Hubert Group Leads: R. Damadeo V. Sofieva B. Hassler S. Frith and 30+ Contributors CEOS AC-VC-14 Meeting, May 2-4, 2018

More information

Supplemental Material for

Supplemental Material for Supplemental Material for Northern North Atlantic Sea Level in CMIP5 Climate Models: Evaluation of Mean State, Variability, and Trends against Altimetric Observations Kristin Richter, a Jan Even Øie Nilsen,

More information

Anthropogenic forcing of the Northern Annular Mode in CCMVal 2 models

Anthropogenic forcing of the Northern Annular Mode in CCMVal 2 models JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2009jd013347, 2010 Anthropogenic forcing of the Northern Annular Mode in CCMVal 2 models O. Morgenstern, 1 H. Akiyoshi, 2 S. Bekki, 3 P. Braesicke,

More information

The Impact of Polar Stratospheric Ozone Loss on Southern Hemisphere Stratospheric Circulation and Surface Climate

The Impact of Polar Stratospheric Ozone Loss on Southern Hemisphere Stratospheric Circulation and Surface Climate The Impact of Polar Stratospheric Ozone Loss on Southern Hemisphere Stratospheric Circulation and Surface Climate James Keeble, Peter Braesicke, Howard Roscoe and John Pyle James.keeble@atm.ch.cam.ac.uk

More information

COMPARISONS OF MIPAS O 3 PROFILES WITH GROUND-BASED MEASUREMENTS

COMPARISONS OF MIPAS O 3 PROFILES WITH GROUND-BASED MEASUREMENTS COMPARISONS OF MIPAS O 3 PROFILES WITH GROUND-BASED MEASUREMENTS T. Blumenstock (1), S. Mikuteit (1), F. Hase (1), I. Boyd (2), Y. Calisesi (3), C. DeClercq (4), J.-C. Lambert (4), R. Koopman (5), S. McDermid

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION In the format provided by the authors and unedited. SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2988 Hemispheric climate shifts driven by anthropogenic aerosol-cloud interactions Eui-Seok Chung and Brian

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION doi:10.1038/nature12310 We present here two additional Tables (Table SI-1, 2) and eight further Figures (Figures SI-1 to SI-8) to provide extra background information to the main figures of the paper.

More information

Southern Hemisphere Storminess under recent and anthropogenic climate conditions based on a multi model ensemble analysis

Southern Hemisphere Storminess under recent and anthropogenic climate conditions based on a multi model ensemble analysis Southern Hemisphere Storminess under recent and anthropogenic climate conditions based on a multi model ensemble analysis Jens Grieger G.C. Leckebusch, M. Schuster, U. Ulbrich (contact: jens.grieger@met.fu-berlin.de)

More information

Global Response to the Major Volcanic Eruptions in 9 Reanalysis Datasets

Global Response to the Major Volcanic Eruptions in 9 Reanalysis Datasets Global Response to the Major Volcanic Eruptions in 9 Reanalysis Datasets Masatomo Fujiwara and Takashi Hibino (Hokkaido Univ., Japan) Sanjay Kumar Mehta (Kyoto Univ., Japan) Lesley Gray, Daniel Mitchell,

More information

Continuous decline in lower stratospheric ozone offsets ozone layer recovery

Continuous decline in lower stratospheric ozone offsets ozone layer recovery Continuous decline in lower stratospheric ozone offsets ozone layer recovery William T. Ball 1,2, Justin Alsing 3, Daniel J. Mortlock 4,5,6, Johannes Staehelin 2, Joanna D. Haigh 4,7, Thomas Peter 2, Fiona

More information

HTAP-2 analysis for the Arctic

HTAP-2 analysis for the Arctic Institute for Climate and Atmospheric Science SCHOOL OF EARTH AND ENVIRONMENT Photo: Chuck Brock, NOAA. HTAP-2 analysis for the Arctic Steve R. Arnold 1, Louisa K. Emmons 2, Kathy S. Law 3, Sarah A. Monks

More information

Modeling polar ozone loss at the University of Colorado

Modeling polar ozone loss at the University of Colorado Modeling polar ozone loss at the University of Colorado CESM workshop Breckenridge, 06/21/2012 Matthias Brakebusch, Cora E. Randall, Douglas E. Kinnison, Simone Tilmes, Michelle L. Santee, Gloria L. Manney

More information