Do we / why do we want to develop an ASM? Climate working group for WRF –2005 - workshop on model developments for climate studies with WRF (summary of.

Slides:



Advertisements
Similar presentations
WCRP polar climate predictability initiative Vladimir Ryabinin
Advertisements

Powering our future with weather, climate and water A large part of my presentation will address Extreme events A few words on the meeting organized yesterday.
Draft Essential Principles with Fundamental Concepts By Marlene Kaplan & David Herring NOAA & NASA.
Hurricanes Innovative Grid-Enable Multiple-scale Hurricane modeling system Konstantinos Menelaou International Hurricane Research Center Department of.
How do geotechnical properties contribute to failures and resulting fluxes to the deep sea? Subsurface flows and impacts on chemical fluxes, geotechnics,
The role of climate change on the ecosystems of the Luquillo LTER Craig A. Ramseyer & Thomas L. Mote University of Georgia.
Introduction to Breakout Session 2.2 Essential Variables for GEO SBAs (Chair: Antonio Bombelli) Coordinator of the GEO Task CL-02 “Global Carbon Observations.
IPCC Climate Change Report Moving Towards Consensus Based on real world data.
Consequences of Global climate Change. Impact of Global Warming Sea level rising Altered precipitation pattern Change in soil moisture content Increase.
Urban Air Pollution, Tropospheric Chemistry, and Climate Change: An Integrated Modeling Study Chien Wang MIT.
Milankovitch Theory of Climate Change The Earth changes its: a)orbit (eccentricity), from ellipse to circle at 100,000 year cycles, b)wobble (precession),
Impact of Global Warming Sea level rising Altered precipitation pattern Change in soil moisture content Increase in some extreme weather More flood more.
FreshNor FreshNor The freshwater budget of the Nordic Seas A Nordic research network Jens Hesselbjerg Christensen Danish Meteorological Institute.
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Importance of the atmospheric boundary layer. Life cycle of the Sun and the Earth The earth will be inhabitable for another 0.5 billion years, if we protect.
Paleoclimatology Why is it important? Angela Colbert Climate Modeling Group October 24, 2011.
US CLIVAR Themes. Guided by a set of questions that will be addressed/assessed as a concluding theme action by US CLIVAR Concern a broad topical area.
WRF-VIC: The Flux Coupling Approach L. Ruby Leung Pacific Northwest National Laboratory BioEarth Project Kickoff Meeting April 11-12, 2011 Pullman, WA.
How does it all work? Synthesis of Arctic System Science Discover, clarify, and improve our understanding of linkages, interactions, and feedbacks among.
Martin Sommerkorn WWF International Arctic Programme.
The Future of Arctic Sea Ice Authors: Wieslaw Maslowski, Jaclyn Clement Kinney, Matthew Higgins, and Andrew Roberts Brian Rosa – Atmospheric Sciences.
 Impacts on the Environment.  Crops o Moderate warming and more carbon dioxide in the atmosphere may help plants to grow faster. However, more severe.
Arctic Systems Modeling Workshop, Montreal July 2009 Atmospheric Breakout: Led by John Walsh, Notes by Scott Elliott First list atmospheric issues mentioned.
Global Climate Change Project Based Learning Environmental Issues and Global Climate Change… “How can I affect change in my world?” Global Climate Change.
Key Questions to Answer on Storm Simulation Xiangdong Zhang International Arctic Research Center University of Alaska Fairbanks, Fairbanks, AK 99775, USA.
24 Global Ecology. Figure 24.2 A Record of Coral Reef Decline.
Arctic Systems Modeling Workshop, Montreal July 2009 (notes by Elliott) Afternoon Breakout Summaries: Day 1 Holland leads Ice Sheets Sea level change the.
Ocean - Proshutinsky/Haidvogel (CG Left Bay) What science questions exist for the arctic that are best answered with coupled regional models? o process.
Earth’s Atmosphere and Climate. The Atmosphere Atmosphere – envelope of air around Earth that allows the support of life. It extends from 0 to 600 km.
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,
ROMS in Alaska Waters Kate Hedstrom, ARSC/UAF Enrique Curchitser, IMCS/Rutgers August, 2007.
Arctic System Model Workshop Background and Objectives International Arctic Research Center Hosted by National Center for Atmospheric Research May 19-22,
A Portable Regional Weather and Climate Downscaling System Using GEOS-5, LIS-6, WRF, and the NASA Workflow Tool Eric M. Kemp 1,2 and W. M. Putman 1, J.
Towards development of a Regional Arctic Climate System Model --- Coupling WRF with the Variable Infiltration Capacity land model via a flux coupler Chunmei.
UNCLASS1 Dr. Gene Whitney Assistant Director for Environment Office of Science and Technology Policy Executive Office of the President WISP Meeting - July.
Chemistry-Climate Working Group Meeting (March 22-24, 2006) Background –SSC expectations and the next IPCC (Bill Collins) Summarize where we are now Discuss.
The evolution of climate modeling Kevin Hennessy on behalf of CSIRO & the Bureau of Meteorology Tuesday 30 th September 2003 Canberra Short course & Climate.
Arctic Research Office May, 2002 Update on SEARCH from the Agency Perspective.
Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european capacity building initiative initiative européenne.
Experience with ROMS for Downscaling IPCC Climate Models 2008 ROMS/TOMS European Workshop, Grenoble, 6-8 October Bjørn Ådlandsvik, Paul Budgell, Vidar.
Physical Effects of Climate Change. Effects of Climate Change in the Atmosphere  Heat Waves  Drought  Wildfires  Storms  Floods
Scientific Plan Introduction –History of LBA Background –Definition of Amazon –7 Themes with achievements Motivation for Phase II –Unresolved questions.
Earth’s climate and how it changes
Ocean Response to Global Warming/Global Change William Curry Woods Hole Oceanographic Institution Environmental Defense May 12, 2005 Possible changes in.
Presented by LCF Climate Science Computational End Station James B. White III (Trey) Scientific Computing National Center for Computational Sciences Oak.
Breakout sessions 13:15-14:45Five Breakout sessions 1.Atmosphere – Walsh/Elliot 2.Sea Ice/Ocean – Proshutinsky/Flato/Gerdes 3.Terrestrial/Permafrost –
Breakout Group 6 Ocean and Atmosphere Group Terrestrial Group.
What science is needed for adaptation? “effective adaptation requires a sound physically- based understanding of climate change, often at levels of detail.
Metrics and MODIS Diane Wickland December, Biology/Biogeochemistry/Ecosystems/Carbon Science Questions: How are global ecosystems changing? (Question.
Coordinated climate change experiments to be assessed as part of the IPCC AR5 Gerald A. Meehl National Center for Atmospheric Research Boulder, Colorado.
What are the key uncertainties? 1.The Common Causes and Remarkability of Recent Changes in the Arctic System 2.The Nature and Importance of Threshold Events,
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
WWRP 1 THORPEX-WCRP Collaborations and other climate relevant activities of the WWRP WCRP/JSC31 WMO/WWRP/THORPEX
How Convection Currents Affect Weather and Climate.
Dmitry Dukhovskoy, Andrey Proshutinsky and Mary-Louise Timmermans Center for Ocean-Atmospheric Prediction Studies Florida State University Acknowledgement:
Climate. Weather vs. Climate Weather – the condition of Earth’s atmosphere at a particular time and place. – Short-term: Hours and days – Localized: Town,
Climates can change suddenly or slowly.  ICE AGE: Period in which huge sheets of ice spread out beyond the polar regions.  El NINO: A disturbance of.
Climate Mission Outcome A predictive understanding of the global climate system on time scales of weeks to decades with quantified uncertainties sufficient.
Climate Change – is it really happening? Kathy Maskell Walker Institute for Climate System Research, University of Reading.
ESSL Holland, CCSM Workshop 0606 Predicting the Earth System Across Scales: Both Ways Summary:Rationale Approach and Current Focus Improved Simulation.
The Water Cycle - Kickoff by Kevin Trenberth -Wide Ranging Discussion -Vapor -Precip/Clouds -Surface Hydrology (Land and Ocean) -Observations and scales.
Towards development of a Regional Arctic Climate System Model ---
Craig Nicolson, UMass-Amherst
Terrestrial-atmosphere (1)
Group 3 Overarching theme: What are the impacts of a warmer Arctic and when/where are the tipping points? Mid-level themes – (past, present, and future)
Regional and Global Ramifications of Boundary Current Upwelling
IPCC Climate Change Report
National Center for Atmospheric Research
Climate and Terrestrial Biodiversity
Presentation transcript:

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 workshop in BAMS) –Develop WRF for high-res climate modeling (cloud resolving scale - 4km) –Evolve WRF towards regional climate system model - couple with ocean model (ROMS), include atmos chemistry –Use WRF for not only downscaling but also upscaling research - two-way coupling between WRF and global model (CCSM) - group at SUNY-Stonybrook Address issue related to improvements in tropical simulations with higher resolution model - tropical channel model based on WRF –Goal to include new developments in standard release of WRF, encourages community development Several efforts are already underway to build regional “physical” climate system model (atmos - ocean - ice - land) –Atmospheric chemistry - several Arctic “impacts” with this Benefit of coordination between these existing efforts, but need to maintain reason for each effort Stretched grid / time slice global models - run AGCM at higher resolution Why do we want to develop an ASM? - see next slide

What science questions are best answered with coupled regional models? Downscaling for impacts assessment –Is a system model needed for this? Upscaling of Arctic processes to global climate –Ex. Arctic C fluxes, changes in Arctic terrestrial ecosystems, impact of aerosols on clouds –Small scale processes that have a climatic signifcance –Need to add other examples here Abrupt climate change - rapid decline in sea ice, methane outgassing,… Role of internal Arctic vs external forcing for change in climate Paleoclimate studies –Glacial inception Coastal erosion Regional specific parameterizations Resolve processes in regional model which are sub-grid scale in global models

What are the existing modeling and model validation efforts aimed towards answering these questions? WRF Climate working group SMHI, AWI-Potsdam, Jens Christensen European project Coupled ARCMIP recently started DAMOCLES - links to CARCMIP

What model and model validation projects are on the horizon aimed towards answering these questions? See previous slide

What arctic science questions cannot be answered with limited area regional coupled Arctic models? Stratospheric processes –Importance of stratosphere / troposphere coupling Whole atmosphere processes - above stratosphere, space weather Some processes are still too small scale to be resolved even with a regional model –Hydrology, ecosystem, other? –Could be addressed with multiple nested domains Not all human interactions are / can be included in a system model Meridional transport for one-way regional model –This can be addressed with nested regional model within global model Very long time processes –Changes in deep ocean circ, ice sheet changes, ecosystem changes

What science questions are missing from existing efforts?

What human systems are relevant to the physical systems being addressed? Are there existing models for these human systems? Land use change / fire / insect outbreaks (C) Hydrology (C) –River runoff temperature –Carbon sources / sinks –Nutrients / sediment Permafrost (C) –Transportation issue / infrastructure –Physical changes - drying of lakes, altered sfc energy budget, Coastal processes Sources of aerosols Industrial development / energy production (O) Transportation (O)

What human systems are relevant to the physical systems being addressed? Are there existing models for these human systems? Global politics / Militarization of the Arctic (O) Fisheries (O) Terrestrial ecosystems (C) Oceanic ecosystems (C) Human health (O) –Air quality, transportation of pollutants (airborne and water), disease vectors Extreme events Sea level rise (C) Population growth / demographic change (O)

What human systems are relevant to the physical systems being addressed? Are there existing models for these human systems? Which of these human system processes need to be dealt with interactively in an ASM and which can be modeled with offline effort? Coupled processes –Fire - land change - atmos change Offline processes

What are reasonable boundaries on the “Arctic system” for your area of research? Storm tracks (or part of) should be included –How far south does this need to extend? –Topographic influence on storms - Greenland, Rockies Size of domain depends on quality of lateral BCs that are available - reanalysis vs GCSMs –Use of upscaling to improve global simulation of atmos circulation Include all land areas that drain into Arctic Ocean Atmospheric differences between high latitudes (>60) and lower latitudes –Pronounced diurnal / seasonal cycle –Atmos. Stability Different size domain for downscaling or upscaling studies Ocean currents –Ocean convection regions