3 rd EULAG Workshop CAM-EULAG June 2012 West African Extreme Daily Precipitation in Observations and Stretched-Grid Simulations by CAM-EULAG William J.

Slides:



Advertisements
Similar presentations
ISU Atmospheric Component Update – Part I Justin Glisan Iowa State University.
Advertisements

GCM Scenarios for Regional Studies over West Africa Gregory S. Jenkins Department of Meteorology Penn State University.
Willem A. Landman & Francois Engelbrecht.  Nowcasting: A description of current weather parameters and 0 to 2 hours’ description of forecast weather.
The Effects of Lake Michigan on Mature Mesoscale Convective Systems Nicholas D. Metz and Lance F. Bosart Department of Atmospheric and Environmental Sciences.
Variability of the Atlantic ITCZ Associated with Amazon Rainfall and Convectively Coupled Kelvin Waves Hui Wang and Rong Fu School of Earth and Atmospheric.
Atlantic ITCZ: A Leaky Barrier for African Aerosol Aaron Adams and Chidong Zhang Rosenstiel School of Marine and Atmospheric Science University of Miami,
Vertical cloud structures of the boreal summer intraseasonal variability based on CloudSat observations and ERA-interim reanalysis Speaker : Li-Chiang.
Interannual Variability in Summer Hydroclimate over North America in CAM2.0 and NSIPP AMIP Simulations By Alfredo Ruiz–Barradas 1, and Sumant Nigam University.
Assessment of hailstorms in WRF weather simulations over Switzerland in summer Sensitivity, climatology, comparison with observation data Andrey.
Climate System Analysis Group Simulating the Characteristics of Extreme Rainfall Events in Southern Africa using Regional Climate Models Babatunde J. Abiodun.
Interannual Variability of Warm-Season Rainfall over the US Great Plains in NASA/NSIPP and NCAR/CAM2.0 AMIP Simulations By Alfredo Ruiz-Barradas and Sumant.
Simulations of carbon transport in CCM3: uncertainties in C sinks due to interannual variability and model resolution James Orr (LSCE/CEA-CNRS and IPSL,
WCRP Metrics/Methodologies for Extremes September 2010 Based in part on … Some Scale Considerations for Predicting/Projecting Extreme Precipitation William.
Template provided by: “posters4research.com” The environment and characteristics of convective events over Niamey, Niger: AMMA SOP2 observations and climatological.
Simulated Sea Surface Salinity Variability in the Tropical Pacific Xiaochun Wang Yi Chao JPL/Caltech Terrain-Following Ocean Models User Workshop Seattle,
Convectively Coupled Kelvin Waves Multi-Scale Study Over Africa in 2011 Matthew Janiga.
A Spatial Climatology of Convection in the Northeast U.S. John Murray and Brian A. Colle Stony Brook University Northeast Regional Operational Workshop.
Orographic triggering and mesoscale organization of extreme storms in subtropical South America Kristen Lani Rasmussen Robert A. Houze, Jr. ICAM 2013,
Forecasting the MJO with the CFS: Factors affecting forecast skill of the MJO over the Maritime Continent Augustin Vintzileos CPC/NCEP – CICS/ESSIC, University.
Monitoring Extreme Rain Events using Giovanni Amita Mehta and Ana Prados NASA-UMBC Joint Center for Earth Systems Technology (JCET)
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.
Grigory Nikulin and Colin Jones Rossby Centre Swedish Meteorological and Hydrological Institute and CORDEX-Africa modeling groups Simulated precipitation.
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.
The Caribbean Low Level Jet variability during August and September and its relation with the regional hydroclimate Ernesto Muñoz.
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.
Kuala Lumpur, Malaysia, 8th-11th November 2012
1 Climate Ensemble Simulations and Projections for Vietnam using PRECIS Model Presented by Hiep Van Nguyen Main contributors: Mai Van Khiem, Tran Thuc,
Alaska Coastal Climatologies Wind/Wave PRIDE Alaska Coastal Climatologies Wind/Wave Workshop Anchorage, Alaska August 2, 2005 Storm Track Capabilities.
West African Monsoon Modeling and Evaluation (WAMME) Project Yongkang Xue, Bill Lau, Kerry Cook With contributions from many collaborators C20C Workshop.
Squall Lines moving over Santarem Julia Cohen Federal University of Para, Brazil David Fitzjarrald Atmospheric Sciences Research Center/ University at.
Collaborative Research: Towards Advanced Understanding and Predictive Capability of Climate Change in the Arctic using a High- Resolution Regional Arctic.
Model representation of the diurnal cycle and moist surges along the Gulf of California during NAME Emily J. Becker and Ernesto Hugo Berbery Department.
11 Predictability of Monsoons in CFS V. Krishnamurthy Center for Ocean-Land-Atmosphere Studies Institute of Global Environment and Society Calverton, MD.
Vegetation Phenology and the Hydrological Cycle of Monsoons
High-resolution RCM simulation of Kansas convective storms: Preliminary results William J. Gutowski, Jr., & David Flory Dept. Geol. & Atmospheric Sciences.
Data assimilation and Forecast activities in support of NAME Data assimilation and Forecast activities in support of NAME The NAME Team at CPC: Kingtse.
Regional Climate Modeling Simulations of the West African Climate System Gregory S. Jenkins, Amadou Gaye, Bamba Sylla LPASF AF20.
KoreaCAM-EULAG February 2008 Implementation of a Non-Hydrostatic, Adaptive-Grid Dynamics Core in the NCAR Community Atmospheric Model William J. Gutowski,
Thomas R. Karl Director, National Climatic Data Center, NOAA Editor, Journal of Climate, Climatic Change & IPCC Climate Monitoring Panel Paul D. Try, Moderator.
NAMAP / NAMAP2 integrating modeling and field activities in NAME Dave Gutzler U. New Mexico presented to NAME SWG6 Tucson, 23 Apr 2004
El Nino, Indian Ocean dynamics and extremely rainy years in East Africa Emily Black, Julia Slingo and Ken Sperber Introduction Rainfall.
Implementation of Grid Adaptation in CAM: Comparison of Dynamic Cores Babatunde J. Abiodun 1,2 William J. Gutowski 1, and Joseph M. Prusa 1,3 1 Iowa State.
Mixed Layer Ocean Model: Model Physics and Climate
The MJO Cloud Population over the Indian Ocean
West African Monsoon Region of Analysis Total West African Monsoon Region of analysis: 15 o W – 10 o E, 5 o N – 20 o N Sub-Sahel Region of analysis: 15.
NARCCAP Meeting September 2009 Results from NCEP-driven RCMs ~ Overview ~ Results from NCEP-driven RCMs ~ Overview ~ William J. Gutowski, Jr. & Raymond.
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.
Results: Model Skill Cool season RegCM2 precipitation exhibits negative (positive) bias in the south central U. S. (northwestern U.S.). Warm season precipitation.
Precipitation efficiency and its dependence on physical factors A look into the cloud response to climate warming Chung-Hsiung Sui 1 Institute of Hydrological.
The frequency distribution of daily precipitation over the U.S. Emily J. Becker 1, E. Hugo Berbery 1, and R. Wayne Higgins 2 1: Department of Atmospheric.
Module 17 MM5: Climate Simulation BREAK. Regional Climate Simulation for the Pan-Arctic using MM5 William J. Gutowski, Jr., Helin Wei, Charles Vörösmarty,
An Overview of the La Niña Michelle L’Heureux.
Diurnal Variations in Southern Great Plain during IHOP -- data and NCAR/CAM Junhong (June) Wang Dave Parsons, Julie Caron and Jim Hack NCAR ATD and CGD.
Analysis and modelling of the 2010 Pakistan heavy precipitation events Milind Mujumdar Centre for Climate Change Research (CCCR), Indian Institute of Tropical.
Analysis of Typhoon Tropical Cyclogenesis in an Atmospheric General Circulation Model Suzana J. Camargo and Adam H. Sobel.
Synthesis of work on Budget of Water Vapor and Trace gases in Amazonia Transport and Impacts of Moisture, Aerosols and Trace Gases into and out of the.
Cécile Hannay, Julio Bacmeister, Rich Neale, John Truesdale, Kevin Reed, and Andrew Gettelman. National Center for Atmospheric Research, Boulder EGU Meeting,
University Allied Workshop (1-3 July, 2008)
Tropical and subtropical convection in South Asia and South America
Anne Sophie Daloz Director : Colin Jones
Ulrike Romatschke University of Washington, University of Vienna
Climatology of Inverted Troughs over the Gulf of Maine
Validation of Satellite Precipitation Estimates using High-Resolution Surface Rainfall Observations in West Africa Paul A. Kucera and Andrew J. Newman.
Phil Arkin, ESSIC University of Maryland
Precipitation variability over Arizona and
Twentieth Century & Future Trends.
Climate sensitivity of the CCM3 to horizontal resolution and interannual variability of simulated tropical cyclones J. Tsutsui, K. Nishizawa,H. Kitabata,
Assessing the Water Cycle in Regional Climate Simulation
Presentation transcript:

3 rd EULAG Workshop CAM-EULAG June 2012 West African Extreme Daily Precipitation in Observations and Stretched-Grid Simulations by CAM-EULAG William J. Gutowski, Jr. 1 Abayomi Abatan 1 Babatunde J. Abiodun 2 Joseph M. Prusa 3 1 Iowa State University, Ames, IA 2 University of Cape Town, South Africa 3 Teraflux Corp., Boca Raton, FL

CAM-EULAG – West Africa June rd EULAG Workshop CAM-EULAG: Simulation Cores: EULAG (stretched-grid & uniform), FV Cores: EULAG (stretched-grid & uniform), FV Physics: CAM3 (same settings as for FV) Physics: CAM3 (same settings as for FV) Experiment: AMIP-type, observed SSTs Experiment: AMIP-type, observed SSTs Horizontal resolutions : Horizontal resolutions : 2˚x2.5˚ [CAM-EULAG uniform; FV]2˚x2.5˚ [CAM-EULAG uniform; FV] Stretched-grid (CEU-SG): 0.5˚ over West AfricaStretched-grid (CEU-SG): 0.5˚ over West Africa Vertical grid: 26 levels Vertical grid: 26 levels Period: 1996 – 2007 (discard first two yr.) Period: 1996 – 2007 (discard first two yr.)

CAM-EULAG – West Africa June rd EULAG Workshop CAM-EULAG: Stretched Grid

CAM-EULAG – West Africa June rd EULAG Workshop Extreme Precipitation: Observed & Simulated Behavior  Observation-Based Fields Precip: TRMM (0.25˚) & GPCP (1˚) Precip: TRMM (0.25˚) & GPCP (1˚) Other fields: ERA-Interim Reanalysis Other fields: ERA-Interim Reanalysis  Analysis Target region: West Africa (6N-16N, 5W-5E) Target region: West Africa (6N-16N, 5W-5E) “Precipitation event” = Daily precip ≥ 0.0 mm at a grid point “Precipitation event” = Daily precip ≥ 0.0 mm at a grid point Pool all “events” in the target region Pool all “events” in the target region Focus on precipitation intensity ≥ 99% Focus on precipitation intensity ≥ 99% Focus on “widespread” events: ≥ 15 simultaneous daily extreme events Focus on “widespread” events: ≥ 15 simultaneous daily extreme events

CAM-EULAG – West Africa June rd EULAG Workshop CAM-EULAG: West Africa Annual Cycle (Abiodun et al., Acta Geophys., 2011) Precip [mm/d], 600 hPa Zonal Wind [dashes] Intertropical Discontinuity [solid line] Region: 10 W – 10 E ERA-Interim +TRMM CEU - SG

CAM-EULAG – West Africa June rd EULAG Workshop Seasonal Average Precip. [mm/d] (6 N – 16 N, 5 W – 5 E)

CAM-EULAG – West Africa June rd EULAG Workshop CAM-EULAG: Precipitation Diurnal Cycle [mm/d] (Region: 10 W – 5 E) Hour of Day Stretched Grid (SG) Uniform TRMM Data: Diurnal Range ~ 2.5 – 9.5 mm/d Diurnal Max ~ hr UCT (Lee et al., JGR, 2007)

CAM-EULAG – West Africa June rd EULAG Workshop Monthly Timing of Extreme Precipitation

CAM-EULAG – West Africa June rd EULAG Workshop Interannual Variability of Extreme Precipitation

CAM-EULAG – West Africa June rd EULAG Workshop Composite Anomaly Meridional Wind JAS 700 hPa Day Before ERA-Interim +TRMM CEU - SG

CAM-EULAG – West Africa June rd EULAG Workshop Composite Anomaly Vertical Wind Extreme Precipitation Days [mb/s] April – May - June Day of Events1-Day before Events OBS. CEU

CAM-EULAG – West Africa June rd EULAG Workshop Composite Anomaly Vertical Wind Extreme Precipitation Days [mb/s] July - August - Sept. Day of Events1-Day before Events OBS. CEU

CAM-EULAG – West Africa June rd EULAG Workshop Spatial Simultaneity of Extremes April-May-June

CAM-EULAG – West Africa June rd EULAG Workshop Spatial Simultaneity of Extremes July-August-Sept.

CAM-EULAG – West Africa June rd EULAG Workshop Normalized Frequency vs. Intensity April-May-June

CAM-EULAG – West Africa June rd EULAG Workshop Normalized Frequency vs. Intensity July-August-September

CAM-EULAG – West Africa June rd EULAG Workshop % of Extremes as Consecutive-Day Events July-August-September

CAM-EULAG – West Africa June rd EULAG Workshop Dirunal Cycle – CEU Extremes

CAM-EULAG – West Africa June rd EULAG Workshop Dirunal Cycle – TRMM AMJ Extremes Early Morning Max Evening Max Mean

CAM-EULAG – West Africa June rd EULAG Workshop Dirunal Cycle – TRMM JAS Extremes Early Morning Max Evening Max Mean

CAM-EULAG – West Africa June rd EULAG Workshop (mm/hr) TRMM: Squall Line

CAM-EULAG – West Africa June rd EULAG Workshop (mm/hr) CEU: Stationary Convection … and more persistent episodes of daily extremes

CAM-EULAG – West Africa June rd EULAG Workshop SUMMARY  CAM-EULAG SG simulates well several aspects of mean climatology of West Africa, including diurnal cycle  CAM-EULAG SG simulates well some aspects of extreme precipitation  However, simulated extremes weaker than observations and are stationary  Extremes also tend to show daily persistence  Needed? Resolution sufficient for squall linesResolution sufficient for squall lines Or perhaps a super-parameterization approach can promote the needed propagation (M. Moncrieff, NCAR, pers. comm.)Or perhaps a super-parameterization approach can promote the needed propagation (M. Moncrieff, NCAR, pers. comm.)

CAM-EULAG – West Africa June rd EULAG Workshop Thank you!