Climatology and Climate Change in Athena Simulations Project Athena Team ECMWF, June 7, 2010.

Slides:



Advertisements
Similar presentations
The Indian Summer Monsoon and Climate Change Andrew Turner with Pete Inness & Julia Slingo RMetS meeting, Wednesday 20 June 2007.
Advertisements

The effect of doubled CO 2 and model basic state biases on the monsoon-ENSO system Andrew Turner, P.M. Inness & J.M. Slingo IUGG meeting: JMS011 Monsoon.
The effect of doubled CO 2 and model basic state biases on the monsoon- ENSO system: the mean response and interannual variability Andrew Turner, Pete.
Willem A. Landman Francois Engelbrecht Ruth Park.
The Canadian Climate Impacts Scenarios (CCIS) Project is funded by the Climate Change Action Fund and provides climate change scenarios and related information.
The Canadian Climate Impacts Scenarios (CCIS) Project is funded by the Climate Change Action Fund and provides climate change scenarios and related information.
GCM Scenarios for Regional Studies over West Africa Gregory S. Jenkins Department of Meteorology Penn State University.
Resolution and Athena – some introductory comments Tim Palmer ECMWF and Oxford.
Observed Tropical Expansion: Impact on the Hydrological and Energy Cycles New Investigator Research Summary Joel Norris (Lead PI, UC San Diego) Robert.
Task: (ECSK06) Regional downscaling Regional modelling with HadGEM3-RA driven by HadGEM2-AO projections National Institute of Meteorological Research (NIMR)/KMA.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Preliminary Results from Project Athena Project Athena Team Presentation to the COLA Scientific Advisory Committee April 12, 2010 Very (Major Computing.
Is there one Indian Monsoon in IPCC AR4 Coupled Models? Massimo A. Bollasina – AOSC658N, 3 Dec 2007.
INTRODUCTION Although the forecast skill of the tropical Pacific SST is moderate due to the largest interannual signal associated with ENSO, the forecast.
Interannual Variability of Warm-Season Rainfall over the US Great Plains in NCAR/CAM and NASA/NSIPP Simulations: Intercomparisons for NAME. Alfredo Ruiz–Barradas.
Diagnosis of Summer Hydroclimate Variability over North America in 20 th Century Climate Simulations By Alfredo Ruiz-Barradas 1,and Sumant Nigam University.
Diagnosis of North American Hydroclimate Variability in IPCC’s Climate Simulations Alfredo Ruiz–Barradas 1 and Sumant Nigam University of Maryland ----o----
Impact of Sea Surface Temperature and Soil Moisture on Seasonal Rainfall Prediction over the Sahel Wassila M. Thiaw and Kingtse C. Mo Climate Prediction.
Exeter 1-3 December 2010 Monthly Forecasting with Ensembles Frédéric Vitart European Centre for Medium-Range Weather Forecasts.
Potential Predictability of Drought and Pluvial Conditions over the Central United States on Interannual to Decadal Time Scales Siegfried Schubert, Max.
Regional Climate Modeling in the Source Region of Yellow River with complex topography using the RegCM3: Model validation Pinhong Hui, Jianping Tang School.
Assessing the diurnal cycle of precipitation in the CSU MMF (T42) Michael S. Pritchard Richard C. J. Somerville John O. Roads Scripps Institution of Oceanography.
© Crown copyright Met Office Climate Projections for West Africa Andrew Hartley, Met Office: PARCC national workshop on climate information and species.
NARCCAP Users Meeting April 2011 Results from NCEP-driven RCMs Overview Based on Mearns et al. (BAMS, 2011) Results from NCEP-driven RCMs Overview Based.
The high resolution in seasonal climate predictions with EC-Earth François Massonnet C. Prodhomme, L. Batté, V. Guemas, F. J. Doblas-Reyes Polar Predictability.
“Nature Run” Diagnostics Thomas Jung ECMWF. Another “Nature Run” A large set of seasonal T L 511L91 integrations has been carried out for many summers.
Improvements of WRF Simulation Skills of Southeast United States Summer Rainfall: Focus on Physical Parameterization and Horizontal Resolution Laifang.
Challenges in Prediction of Summer Monsoon Rainfall: Inadequacy of the Tier-2 Strategy Bin Wang Department of Meteorology and International Pacific Research.
GFDL NCEPNASA Observation Fig Hourly summer (JJA) mean diurnal cycle of rainfall and low-level wind vectors. Rainfall amount is represented as the.
Preliminary Results of Global Climate Simulations With a High- Resolution Atmospheric Model P. B. Duffy, B. Govindasamy, J. Milovich, K. Taylor, S. Thompson,
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Seasonal Moisture Flux Variability over North America in NASA/NSIPP’s AMIP Simulation and Atmospheric Reanalysis By Alfredo Ruiz-Barradas and Sumant Nigam.
Regional Climate Simulations of summer precipitation over the United States and Mexico Kingtse Mo, Jae Schemm, Wayne Higgins, and H. K. Kim.
CPPA Past/Ongoing Activities - Ocean-Atmosphere Interactions - Address systematic ocean-atmosphere model biases - Eastern Pacific Investigation of Climate.
CLIVAR/OCB Working Group: Oceanic Carbon Uptake in CMIP5 Models Ocean CO 2 uptake (Gt/yr) (climate change - control) Friedlingstein et al. [2006]
Regional Climate Modeling Simulations of the West African Climate System Gregory S. Jenkins, Amadou Gaye, Bamba Sylla LPASF AF20.
Mechanisms of drought in present and future climate Gerald A. Meehl and Aixue Hu.
Fine-resolution global time slice simulations Philip B. Duffy 1,2,3 Collaborators: G. Bala 1, A. Mirin 1 1 Lawrence Livermore National Laboratory 2 University.
Change of program Implementation Plan. T. Satomura Current status of and contribution by NICAM. T. Matsuno & T. Nasuno (~ 20 min) Comments. J. Shukla Discussion.
NARCCAP WRF Simulations L. Ruby Leung Pacific Northwest National Laboratory NARCCAP Users Meeting February , 2008 Boulder, CO.
LASG/IAP Collaboration between CLIVAR/AAMP and GEWEX/MAHASRI A proposal to foster interaction l Coordinated GCM/RCM Process study on Monsoon ISO l Multi-RCM.
Modes of variability and teleconnections: Part II Hai Lin Meteorological Research Division, Environment Canada Advanced School and Workshop on S2S ICTP,
The NTU-GCM'S AMIP Simulation of the Precipitation over Taiwan Area Wen-Shung Kau 1, Yu-Jen Sue 1 and Chih-Hua Tsou 2 1 Department of Atmospheric Sciences.
Diurnal Water and Energy Cycles over the Continental United States from three Reanalyses Alex Ruane John Roads Scripps Institution of Oceanography / UCSD.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Understanding and predicting the contrast.
1 Spatio-temporal Distribution of Latent Heating in the Southeast Asian Monsoon Region School of Earth and Atmospheric Sciences Georgia Institute of Technology.
1 An Assessment of the CFS real-time forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
Arctic climate simulations by coupled models - an overview - Annette Rinke and Klaus Dethloff Alfred Wegener Institute for Polar and Marine Research, Research.
Teleconnection Patterns and Seasonal Climate Prediction over South America The Final Chapter??? Tércio Ambrizzi and Rosmeri P. da Rocha University of São.
1 An Assessment of the CFS real-time forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
Predictability of Monthly Mean Temperature and Precipitation: Role of Initial Conditions Mingyue Chen, Wanqiu Wang, and Arun Kumar Climate Prediction Center/NCEP/NOAA.
1/39 Seasonal Prediction of Asian Monsoon: Predictability Issues and Limitations Arun Kumar Climate Prediction Center
ESSL Holland, CCSM Workshop 0606 Predicting the Earth System Across Scales: Both Ways Summary:Rationale Approach and Current Focus Improved Simulation.
Intraseasonal, seasonal, and interannual variations of the Arctic temperature in paleoclimates, present, and future experiments in CMIP5 model outputs.
Summer Monsoon – Global Ocean Interactions Ben Kirtman George Mason University Center for Ocean-Land-Atmosphere Studies Acknowledgements: Randy Wu and.
The North American Monsoons (NAM) can provide upwards of 70% of the annual precipitation to the southwest United States and Mexico. Already susceptible.
Mingyue Chen, Wanqiu Wang, and Arun Kumar
M.-E. Demory, P.L. Vidale, J. Donners, M. Roberts, A. Clayton
Can recently observed precipitation trends over the Mediterranean area be explained by climate change projections? Armineh Barkhordarian1, Hans von Storch1,2.
Hervé Douville Météo-France CNRM/GMGEC/VDR
Ensemble Spread and Resolution in Minerva Simulations
Simulating daily precipitation variability.
North American Regional Climate Change Assessment Program
Alfredo Ruiz-Barradas Sumant Nigam
Workshop 1: GFDL (Princeton), June 1-2, 2006
Predictability of Indian monsoon rainfall variability
Precipitation variability over Arizona and
Lindsey Long and Jae Schemm NOAA/NWS/NCEP/CPC
Sub Topic – The Indian Summer Monsoon and Climate Change By- Mali B.B.
Frank Bryan & Gokhan Danabasoglu NCAR
Presentation transcript:

Climatology and Climate Change in Athena Simulations Project Athena Team ECMWF, June 7, 2010

Qualitative to Quantitative: Beyond Animations Athena Catalog – 8 NICAM (7 km) Boreal summer cases – 9 IFS T2047 (10 km) Boreal summer cases – 20 IFS T month hindcasts – 48 IFS 13-month hindcasts at T1279 (16 km), T511 (40 km), T159 (128 km) – 47 year IFS AMIP runs at T1279, T159 – 47 year IFS timeslice runs at T1279, T159 – Multiple ensemble members for select seasons at T1279, T511, T159 Sufficient data for quantitative, climatological analysis

10km: IFS T2047 JJA Mean Rainfall at native resolution (8 seasons)

7km: NICAM JJA Mean Rainfall at native resolution (8 seasons)

40 km: Chen et al. 0.5 degree JJA Mean Rainfall (8 seasons)

25 km: TRMM JJA Mean Rainfall (8 seasons)

128 km: IFS T159 JJA Mean Rainfall native resolution (8 seasons)

LARGE BIASES REMAIN

Diurnal Cycle of Precipitation Large variations between models Standard GCM is locked to the sun SP-CCSM captures some aspects of DC. Hi-res IFS gets N. Plains right for wrong reason, locks to sun over SE US. NICAM is noisy, but does best job of capturing diurnal cycle structure.

Low Level Jet Low-level jet is a critical component of Great Plains maximum All higher resolution models are reasonably accurate Dynamics do not explain differences in phase and amplitude Suggests representation of convection is responsible

Atmosphere-Ocean Interactions Modest improvement with resolution All data at T159

Clear improvement in representing interannual variability

AMIP and Timelice Experiments AMIP Experiment – , observed boundary conditions Timeslice Experiment – SST/Sea ice anomaly added to AMIP boundary conditions – Anomaly taken from CCSM3.0 2xCO 2 IPCC integration – Same length of integration, ‘ ’ – Annual means analyzed here Large seasonal variations in forcing anomaly New ice-free regions during DJF

Annual Mean Time Slice Forcing (CMIP3 CCSM3 2xCO2 - Control

Annual Mean Time Slice Forcing (CMIP3 CCSM3 2xCO2 - Control

Annual Mean Time Slice Forcing (CMIP3 CCSM3 2xCO2 - Control

Annual Mean Time Slice Forcing (CMIP3 CCSM3 2xCO2 - Control

Summary – Unique data set and analysis opportunities Small fraction at COLA Full catalog in archive at NICS Data to become available to the community – Impact of Resolution Orographic features clearly improved Diurnal cycle can be well-represented – Plateau in benefit of resolution with parameterized convection? – Some improvements seen with non-parameterized convection Large tropical biases remain – More than increased resolution needed

Summary (cont’d) – Impact of Resolution on Large Scales Improved blocking and synoptic statistics Atlantic air-sea coupling – Climate Change Increased warming seen over Europe with higher resolution Dramatically improved representation of orographic precipitation, snow depth Sensitivity to choice of forcing anomaly?