ETH On-going and planned projects with ECHAM Martin Wild, Doris Folini, Adeline Bichet, Maria Hakuba, Christoph Schär IACETH.

Slides:



Advertisements
Similar presentations
The Canadian Climate Impacts Scenarios (CCIS) Project is funded by the Climate Change Action Fund and provides climate change scenarios and related information.
Advertisements

CMIP5: Overview of the Coupled Model Intercomparison Project Phase 5
Water Vapor and Cloud Feedbacks Dennis L. Hartmann in collaboration with Mark Zelinka Department of Atmospheric Sciences University of Washington PCC Summer.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Climate models in (palaeo-) climatic research How can we use climate models as tools for hypothesis testing in (palaeo-) climatic research and how can.
“what a climate model is, and what uncertainty means” Noah S. Diffenbaugh Department of Environmental Earth System Science and Woods Institute for the.
Climate Change and Malaysia
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 16: 05/20/2010 ATM S 111, Global Warming: Understanding the Forecast.
Climate Forcing and Physical Climate Responses Theory of Climate Climate Change (continued)
Observed Reductions of Surface Solar Radiation at Sites in the United States and Worldwide from 1961 to 1990 Beate Liepert Lamont-Doherty Earth Observatory.
METR112-Climate Modeling
Earth Systems Science Chapter 6 I. Modeling the Atmosphere-Ocean System 1.Statistical vs physical models; analytical vs numerical models; equilibrium vs.
MET 112 Global Climate Change - Lecture 11 Future Predictions Craig Clements San Jose State University.
METR112-Climate Modeling Basic concepts of climate Modeling Components and parameterization in the model sensitivity of the model.
National Oceanic and Atmospheric Administration Geophysical Fluid Dynamics Laboratory Princeton, NJ Evolution of Stratospheric.
METR112-Climate Modeling Basic concepts of climate Modeling Components and parameterization in the model sensitivity of the model.
Last Class – Global What transformations occur as energy flows through the earth system. Relationship between distance from the source and amount of energy.
Image: NASA ECHAM5/6 projects by Quentin Bourgeois, Junbo Cui, Gabriela Sousa Santos, Tanja Stanelle C2SM’s research group - Isabelle Bey.
January 10, 2006 Global and Regional Climate Change: Causes, Consequences, and Vulnerability Climate Science in the Public Interest
Evaluation of IPCC Soil Moisture Simulations for the latter half of the 20 th Century Haibin Li 1, Alan Robock 1, Martin Wild 2 1 Department of Environmental.
Overview of Coupled Model Intercomparison Project (CMIP) and IPCC AR5 Activities Ronald J Stouffer Karl Taylor, Jerry Meehl and many others June 2009.
4. Models of the climate system. Earth’s Climate System Sun IceOceanLand Sub-surface Earth Atmosphere Climate model components.
INGV Mediterranean Sea Level Rise Scenarios from CIRCE S. Dobricic on behalf of the CIRCE project team: M. Adani, S. Gualdi, S. Somot, W. May, S. Castellari,
Influence of the sun variability and other natural and anthropogenic forcings on the climate with a global climate chemistry model Martin Schraner Polyproject.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
21st century climate change as simulated by European climate models U. Cubasch, H. Huebener Thanks to: F. Niehörster, I. Fast, T. Spangehl.
CLIMARES, NERSC, October 2009 Arctic climate and future scenarios Ola M. Johannessen and Mats Bentsen Nansen Environmental and Remote Sensing Center.
Helgi Björnsson, Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland Contribution of Icelandic ice caps to sea level rise: trends and.
Use of CCSM3 and CAM3 Historical Runs: Estimation of Natural and Anthropogenic Climate Variability and Sensitivity Bruce T. Anderson, Boston University.
CIRCE project RL5 WP1 Task 1 TAU group Prof. Pinhas Alpert Department of Geophysics and Planetary Sciences, Faculty of Exact Sciences, Tel-Aviv University,
Modern Climate Change Darryn Waugh OES Summer Course, July 2015.
Climate Change Science and the Limits of Confidence John Nielsen-Gammon Dept. of Atmospheric Sciences Texas A&M University.
Module 4 Changes in Climate. Global Warming? Climate change –The pattern(s) of variation in climate (temperature, precipitation) over various periods.
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
Status of the Sea Ice Model Testing of CICE4.0 in the coupled model context is underway Includes numerous SE improvements, improved ridging formulation,
IPCC WG1 AR5: Key Findings Relevant to Future Air Quality Fiona M. O’Connor, Atmospheric Composition & Climate Team, Met Office Hadley Centre.
Integrated projections of U.S. air quality benefits from avoided climate change Fernando Garcia Menendez Rebecca K. Saari, Erwan Monier, Noelle E. Selin.
Volcanic Climate Impacts and ENSO Interaction Georgiy Stenchikov Department of Environmental Sciences, Rutgers University, New Brunswick, NJ Thomas Delworth.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 10) Projected Future Changes Primary Source: IPCC WG-I Chapter 10 - Global.
© Crown copyright Met Office AR5 Proposed runs for CMIP5 John Mitchell, after Karl Taylor, Ron Stouffer and others ENES, arch 2009.
Human fingerprints on our changing climate Neil Leary Changing Planet Study Group June 28 – July 1, 2011 Cooling the Liberal Arts Curriculum A NASA-GCCE.
Research Needs for Decadal to Centennial Climate Prediction: From observations to modelling Julia Slingo, Met Office, Exeter, UK & V. Ramaswamy. GFDL,
CLIMARES WP 110 Climate model scenarios for the Arctic region for the next decades Current state: Klaus Dethloff, AWI WP Leader: Erich Roeckner, MPI Planing.
IACETH Institute for Atmospheric and Climate Sciences Indirect aerosol effects in EC earth Trude Storelvmo and Ulrike Lohmann, ETH-Zurich.
The evolution of climate modeling Kevin Hennessy on behalf of CSIRO & the Bureau of Meteorology Tuesday 30 th September 2003 Canberra Short course & Climate.
OCO 10/27/10 GFDL Activities in Decadal Intialization and Prediction A. Rosati, S. Zhang, T. Delworth, Y. Chang, R. Gudgel Presented by G. Vecchi 1. Coupled.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
Aerosols and climate - a crash course Marianne T. Lund CICERO Nove Mesto 17/9-15.
Contribution of MPI to CLIMARES Erich Roeckner, Dirk Notz Max Planck Institute for Meteorology, Hamburg.
Climate Modeling Research & Applications in Wales John Houghton C 3 W conference, Aberystwyth 26 April 2011.
© Crown copyright Met Office Uncertainties in the Development of Climate Scenarios Climate Data Analysis for Crop Modelling workshop Kasetsart University,
CE 401 Climate Change Science and Engineering modeling of climate change predictions from models 10 February 2011 team selection and project topic proposal.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 12 Future Predictions Eugene Cordero San Jose State University Outline  Scenarios.
Of what use is a statistician in climate modeling? Peter Guttorp University of Washington Norwegian Computing Center
How Much Will the Climate Warm? Alex Hall and Xin Qu UCLA Department of Atmospheric and Oceanic Sciences UCLA Institute of the Environment Environmental.
Regional Patterns of Climate Change Kenneth Hunu & Bali White EESC W4400 Dynamics of Climate Variability and Climate Change December 5, 2006.
Coordinated climate change experiments to be assessed as part of the IPCC AR5 Gerald A. Meehl National Center for Atmospheric Research Boulder, Colorado.
Burning issues at climate science – policy interface Judith Curry.
How Convection Currents Affect Weather and Climate.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
The Great 20 th Century Drying of Africa Ninth Annual CCSM Workshop Climate Variability Working Group 9 July 2004, Santa Fe Jim Hurrell, Marty Hoerling,
Key ingredients in global hydrological response to external forcing Response to warming => Increased horizontal moisture fluxes => Poleward expansion of.
Impact of Solar and Sulfate Geoengineering on Surface Ozone
Introduction to Climate Modeling
Climate Modeling General Circulation Models
An Approach to Enhance Credibility of Decadal-Century Scale Arctic
National Center for Atmospheric Research
Slides for GGR 314, Global Warming Chapter 4: Climate Models and Projected Climatic Change Course taught by Danny Harvey Department of Geography University.
GFDL-NCAR/CCSM collaborations
Presentation transcript:

ETH On-going and planned projects with ECHAM Martin Wild, Doris Folini, Adeline Bichet, Maria Hakuba, Christoph Schär IACETH

ETH Simulations with ECHAM5-HAM Model ECHAM5-HAM (updated from Stier et al. 2005), Version Oct Detailed aerosol treatment (prognostic equations for number and mass) Experiments (carried out by Doris Folini at CSCS) - Transient simulations (atmosphere only, prescribed SSTs) - Historic emission inventories: NIES - Resolutions from T42L19 to T106L31 List of Ensembles Simulations#members: 1870 – 2000, default “all forcings“ simulations, T42 (T63)13 (9) Sensitivity experiments: 1950 – 2000, SO2 emissions at level of 1950, T – 2000, BC / OC emissions at level of 1950, T – 2000, all anth. aerosol emissions constant, T42 (T63) 6 (3) 1870 – 2000, all anth. aerosol emissions constant, no volcanoes: – 2000, fixed climatological SSTs, T42 (T63)13 (1)

ETH What are the origins of these changes? What is their impact on climate system components and climate change? How will these components evolve in the future? Atmospheric transmission Wild et al. 2005: Science 308 “dimming” “brightening” Research focus Significant decadal changes in the observed components of the Earth energy and water balance Observed precipitation NH mean land “dimming” “brightening”

ETH What are the origins of these changes? => sensitivity studies, impact of various types of aerosol on decadal changes in surface solar radiation Research focus: origins of changes Surface solar radiation: constant versus variable aerosol emissions Varying only SO 2 or BC emissions Folini et al. in prep. constant aerosol emissions variable aerosol emissions

ETH Impact of dimming on precipitation in China Suppression of precipitation with dimming in China constant aerosol emissions historic aerosol emissions Annual mean precipitation Research focus: impacts

ETH Impact of dimming on precipitation in China Suppression of convective precipitation with dimming Summer precipitation large scale convective total precipitation JJA constant aerosol emissions variable aerosol emissions

ETH PhD Thesis Adeline Bichet: Precipitation evolution since the late 19th century Research focus: impacts Bichet et al., submitted Impact of SSTs and aerosols on global land precipitation

ETH Research focus: impacts Master Thesis Maria Hakuba Impact of reduced Greenland topography on precipitation Overall increase in precipitation with decreasing topography Change in precipitation with topography reduced by 50% T106 simulations

ETH Research focus: scenarios Surface clear sky insolation in NH midlatitudes ECHAM5-HAM with ENSEMBLE SSTs Transition into a new dimming? Coupled model desirable How will the Earth energy and water balance components evolve in the future?

ETH Research focus on changes in the energy and water cycles based on multidecadal transient simulations Near term experiments: Carry out multidecadal transient simulations with new model versions ECHAM6 and ECHAM6-HAM (sensitivity studies) Use ECHAM6-HAM with new emission inventories from IPCC AR5, comparison to NIES and other inventories, comparison to earlier ECHAM5- HAM simulations Mid term experiments: Use a coupled Atmosphere-Ocean version of ECHAM6 (ECHAM6-HAM?) to study impacts of changes in the radiation balance on various climate system components including ocean feedbacks. High resolution (T213?) time slice experiments for present and future climates (e.g. for mass balance changes of polar ice sheets) All simulation data can be made available to other interested groups Future Plans with ECHAM

ETH