Science Perspective and Status William D. Collins Lawrence Berkeley Laboratory ACME Chief Scientist And the ACME Project Team.

Slides:



Advertisements
Similar presentations
What? Remote, actively researched, monitored, measured, has a huge impact on global climate and is relatively cool?
Advertisements

WCRP polar climate predictability initiative Vladimir Ryabinin
What is Earth Science? Chapter 1.1 & 1.2.
CMIP5: Overview of the Coupled Model Intercomparison Project Phase 5
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Radiative Forcings of Wild Fire Aerosols and Impacts on Regional Climate Xiaohong Liu 1,*, Yiquan Jiang 1, Kai Zhang 2, Yun Qian 2, and Yuhang Wang 3 1.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Coupled Ocean and Atmosphere Climate Dynamics ENVI3410.
WFM 6311: Climate Risk Management © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 6311: Climate Change Risk Management Akm Saiful Islam Lecture-1: Module-1.
John J. Cassano - University of Colorado Wieslaw Maslowski -Naval Postgraduate School William Gutowski - Iowa State University Dennis Lettenmaier – University.
Gary Lagerloef, PhD Science on Tap, 7 April Apollo 17 December 1972 Climate Science in the Space Age Gary Lagerloef Oceanographer & Climate Scientist.
4. Models of the climate system. Earth’s Climate System Sun IceOceanLand Sub-surface Earth Atmosphere Climate model components.
ACME Land Group Overview and Roadmaps Group Leads: Peter Thornton and Bill Riley.
Next Gen AQ model Need AQ modeling at Global to Continental to Regional to Urban scales – Current systems using cascading nests is cumbersome – Duplicative.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
IPCC Fifth Assessment Report (AR5), due to be completed in AR5 NOMINATIONS CLOSED ON 12 MARCH 2010.
WRF-VIC: The Flux Coupling Approach L. Ruby Leung Pacific Northwest National Laboratory BioEarth Project Kickoff Meeting April 11-12, 2011 Pullman, WA.
WATER AND HOW IT AFFECTS WEATHER AND CLIMATE (C) Copyright
Climate 2010 Gary Strand High Performance Network Planning Workshop.
Observed Global Climate Change. Review of last lecture Air pollution. 2 categories 6 types of major pollutants: particulates, carbon oxides, sulfur dioxides,
Progress in climate-glacier-ice sheet modelling Jeremy Fyke (LANL) Bill Lipscomb (LANL) Bill Sacks (NCAR) Valentina Radic (UBC, Canada)
Page 1 Met Office contribution to RL5 Task ‘Large-scale interactions between atmospheric moisture and water availability - coupling of atmospheric.
JULES: Joint UK Land Environment Simulator A community land surface scheme.
Improvements of WRF Simulation Skills of Southeast United States Summer Rainfall: Focus on Physical Parameterization and Horizontal Resolution Laifang.
Preliminary Results of Global Climate Simulations With a High- Resolution Atmospheric Model P. B. Duffy, B. Govindasamy, J. Milovich, K. Taylor, S. Thompson,
CDC Cover. NOAA Lab roles in CCSP Strategic Plan for the U.S. Climate Change Science Program: Research Elements Element 3. Atmospheric Composition Aeronomy.
Climate Modeling Jamie Anderson May Monitoring tells us how the current climate has/is changing Climate Monitoring vs Climate Modeling Modeling.
Marine organic matter in sea spray Nd vs. SO4, binned into low-OM, intermediate OM, and high-OM groups Adding marine organic matter as a source into ACME.
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.
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I Working Group I Contribution to the IPCC Fourth Assessment Report Climate Change 2007:
Status of the Sea Ice Model Testing of CICE4.0 in the coupled model context is underway Includes numerous SE improvements, improved ridging formulation,
CCSM3.5+ Coupled Experiments Rich Neale Phil Rasch, Cecile Hannay, Jon Wolfe, Steve Yeager.
CPPA Past/Ongoing Activities - Ocean-Atmosphere Interactions - Address systematic ocean-atmosphere model biases - Eastern Pacific Investigation of Climate.
ETH On-going and planned projects with ECHAM Martin Wild, Doris Folini, Adeline Bichet, Maria Hakuba, Christoph Schär IACETH.
Presented by Global Coupled Climate and Carbon Cycle Modeling Forrest M. Hoffman Computational Earth Sciences Group Computer Science and Mathematics Division.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
WHAT IS THE WATER CYCLE? Water is always moving between the atmosphere (troposphere) and surface of Earth. Water is always moving between the atmosphere.
© Crown copyright Met Office AR5 Proposed runs for CMIP5 John Mitchell, after Karl Taylor, Ron Stouffer and others ENES, arch 2009.
Opportunities for Research in the Dynamics of Water Processes in the Environment at NSF Pam Stephens Directorate of Geosciences, NSF Directorate of Geosciences,
Research Needs for Decadal to Centennial Climate Prediction: From observations to modelling Julia Slingo, Met Office, Exeter, UK & V. Ramaswamy. GFDL,
CCSM Atmospheric Model Working Group Summary J. J. Hack, D. A Randall AMWG Co-Chairs CCSM Workshop, 28 June 2001 CCSM Workshop, 28 June 2001.
AMWG Breakout, CCSM Workshop June 25, 2002 Overview of CAM status and simulations Bill Collins and Dave Randall National Center for Atmospheric Research.
The evolution of climate modeling Kevin Hennessy on behalf of CSIRO & the Bureau of Meteorology Tuesday 30 th September 2003 Canberra Short course & Climate.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
AOM 4643 Principles and Issues in Environmental Hydrology.
Scientific Plan Introduction –History of LBA Background –Definition of Amazon –7 Themes with achievements Motivation for Phase II –Unresolved questions.
Contribution of MPI to CLIMARES Erich Roeckner, Dirk Notz Max Planck Institute for Meteorology, Hamburg.
Aims- 1. To understand the movement of water within the global hydrological cycle. 2. Explain how a balance is maintained within the cycle. Complete worksheet.
Climate Model Tests of the Early Anthropogenic Hypothesis Steve Vavrus Center for Climatic Research University of Wisconsin Bill Ruddiman (U. Virginia),
Presented by LCF Climate Science Computational End Station James B. White III (Trey) Scientific Computing National Center for Computational Sciences Oak.
March 31, 2004BGC Working Group Interactive chemistry in CAM Jean-François Lamarque, D. Kinnison and S. Walters Atmospheric Chemistry Division NCAR.
Skepticism: the Intertwining of Politics and Science M. Leach May 4, 2011.
Do we / why do we want to develop an ASM? Climate working group for WRF – workshop on model developments for climate studies with WRF (summary of.
Consistent Earth System Data Records for Climate Research: Focus on Shortwave and Longwave Radiative Fluxes Rachel T. Pinker, Yingtao Ma and Eric Nussbaumer.
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Representing Effects of Complex Terrain on Mountain Meteorology and Hydrology Steve Ghan, Ruby Leung, Teklu Tesfa, PNNL Steve Goldhaber, NCAR.
March 9, 2004CCSM AMWG Interactive chemistry in CAM Jean-François Lamarque, D. Kinnison S. Walters and the WACCM group Atmospheric Chemistry Division NCAR.
WFM 6311: Climate Risk Management © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 6311: Climate Change Risk Management Professor A.K.M. Saiful Islam Lecture-1:
Development of the Regional Arctic Climate System Model (RACM) --- Department of Civil and Environmental Engineering University of Washington May, 2010.
Status of CAM, March 2004 Phil Rasch. Differences between CAM2 and CAM3 (standard physics version) Separate liquid and ice phases Advection, sedimentation.
RAL, 2012, May 11 Research behaviour Martin Juckes, 11 May, 2012.
The Water Cycle.
Status and Outlook Evaluating CFSR Air-Sea Heat, Freshwater, and Momentum Fluxes in the context of the Global Energy and Freshwater Budgets PI: Lisan.
Catherine Senior WGCM-19, October 19th 2015
Mesoscale “Surprises” in Complex Terrain Revealed by Regional Climate Simulations Cliff Mass, Atmospheric Sciences University of Washington.
GFDL Climate Model Status and Plans for Product Generation
National Center for Atmospheric Research
Earth Climate System Model of INM RAS
The Water Cycle.
GFDL-NCAR/CCSM collaborations
Presentation transcript:

Science Perspective and Status William D. Collins Lawrence Berkeley Laboratory ACME Chief Scientist And the ACME Project Team

Science Questions Water cycle: – What are the processes and factors governing precipitation and the water cycle today and how will precipitation evolve over the next 40 years? Biogeochemistry: – What are the contributions and feedbacks from natural and managed systems to current greenhouse gas fluxes, and how will those factors and associated fluxes evolve in the future? Cryosphere: – What will be the long-term, committed Antarctic Ice Sheet contribution to sea level rise (SLR) from climate change during1970–2050?

Water Cycle Experiments Near-term: How will more realistic portrayals of features in the water cycle (resolution, clouds, aerosols, snowpack, river routing, land use) affect river flow and associated freshwater supplies at the watershed scale? Simulations: Preliminary simulation plan includes: 1.Prescribed SST experiments to quantify resolution effects. 2.Fully coupled experiments to examine feedbacks = f(resolution) 3.Conduct simulations under RCP hypothesis to test hypothesis. 20-year Return Daily Rainfall

Water Cycle Core Hypothesis Question: How will improved portrayals of earth system features affect the simulation of Earth’s water cycle, including river flow and freshwater supplies at the watershed scale? Hypothesis: – Changes in river flow over the last 40 years have been dominated primarily by land and water use and climate change associated with aerosol forcing. – During the next 40 years, GHG will produce changes to river flow with signatures that dominate those of other forcing agents in at least one of our domains.

V1 Atmospheric Capabilities New CapabilityEpic Lead Update convective parameterizationShaocheng Xie Improve NumericsMark Taylor Implement RRM for model evaluationSteve Klein Higher vertical resolutionPo-Lun Ma Surface Model InteractionsSusannah Burrows Polar Project UpdatesPeter Caldwell Implement short simulations for evaluationYun Qian Update SCAM for evaluationJeffrey Johnson Tuning and evaluationPhil Rasch New aerosol and cloud updatesHailong Wang Satellite simulator improvementsYuying Zhang Addition of elevation class decompositionRuby Leung / Steve Ghan Maintain chemistry capabilityPhilip Cameron-Smith

V1 Major Milestone QuarterMilestone Q3,Q4Exercise testing and evaluation procedure Make most Tier 1b diagnostics fully functional Assessment of convection schemes Elevation class decomposition Finalization of aerosol and cloud improvements Numerics improvements Tests of enhanced vertical resolution Q5Choose convection Assessment of candidate collection of parameterizations Downselect to decide on viable evaluation and tuning methods Attempt a credible simulation at higher vertical resolution Q6Final push to V1

Biogeochemical Experiments Near-term: How do carbon, nitrogen, and phosphorus cycles regulate climate system feedbacks, and how sensitive are these feedbacks to model structural uncertainty? Simulations: Simulation plan includes 1.Fixed-forcing control simulations, using pre-industrial (circa 1850 AD) boundary conditions 2.Transient-forcing control simulations, using historical forcings 3.Fixed-forcing C-N-P simulations 4.Transient-forcing C-N-P simulations Improvement in total soil organic C

V1 Land Capabilities New CapabilityEpic Lead Orographic downscalingRuby Leung Head-based soil hydrologyGautam Bisht Coupled C-N-P cyclesXiaojuan Yang Alternative plant-microbe competition (ECA)Bill Riley Initial crop model improvementsBeth Drewniak New (uncoupled) river routingRuby Leung V1 land model UQ frameworkKhachik Sargsyan V1 land benchmarking frameworkForrest Hoffman

V2 Land Capabilities

Cryospheric Experiments Near-term: Could a dynamical instability in the Antarctic Ice Sheet be triggered within the next 40 years? Simulations: Simulation plan focuses on 1.Rigorous testing of the ice sheet and its interactions with the atmosphere, underlying continent, ocean, and sea ice 2.Transient fully coupled simulation from 1970 to 2050.

V1 Land Ice Capabilities New CapabilityEpic Lead Stand-alone Antarctica simulations with MPASSteve Price Stand-alone Antarctica mass-balance simulations Steve Price Ocean/sea-ice runs with data atmos./ice sheetSteve Price Coupled ocean/sea-ice/land-ice runs w/data atm. Steve Price Fully coupled simulationsSteve Price Gravitationally self-consistent SLR modelSteve Price

V1 Sea Ice Capabilities New CapabilityEpic Lead MPAS-CICE modelAdrian Turner Improved snow modelElizabeth Hunke BiogeochemistryElizabeth Hunke

V1 Ocean Capabilities New CapabilityEpic Lead Stand-alone ocean validationTodd Ringler Ocean analysis coreTodd Ringler BiogeochemistryTodd Ringler Hybrid vertical coordinateTodd Ringler

3-year Roadmap Main Points Complete construction of v1-alpha EOY 2015 – 1 configuration, 2 resolutions, 2 levels of BGC activation Coupled system tuning Jun 2016 Start major experiments with ACME v1.0 code base Jul 2016 – The 3 experiments need not activate same functionality – But they should all share the same code base, with active functionality controlled by run-time switches All major 3 year experiments completed Jul 2017

QUESTIONS?