Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 The International H 2 O Project (IHOP_2002) -- Two.

Slides:



Advertisements
Similar presentations
List of Nominations Connecting User Needs with Weather Research and Forecasts Rebecca E. Morss National Center for Atmospheric Research Boulder, Colorado,
Advertisements

Introduction to data assimilation in meteorology Pierre Brousseau, Ludovic Auger ATMO 08,Alghero, september 2008.
Predictability Issues Associated with Explosive Cyclogenesis in the North-West Pacific Edmund K.M. Chang School of Marine and Atmospheric Sciences Stony.
Louisville, KY August 4, 2009 Flash Flood Frank Pereira NOAA/NWS/NCEP/Hydrometeorological Prediction Center.
Bores During IHOP_2002 and Speculation on Nocturnal Convection David B. Parsons, Crystal Pettet and June Wang NCAR/ATD Acknowledgements to Tammy Weckwerth,
The Structure and Climatology of Boundary Layer Winds in the Southeast United States and its Relationship to Nocturnal Tornado Episodes Alicia C. Wasula.
UNSTABLE, DRI and Water Cycling Ronald Stewart McGill University.
Jiangfeng Wei Center for Ocean-Land-Atmosphere Studies Maryland, USA.
Danielle M. Kozlowski NASA USRP Intern. Background Motivation Forecasting convective weather is a challenge for operational forecasters Current numerical.
Analysis of Precipitation Distributions Associated with Two Cool-Season Cutoff Cyclones Melissa Payer, Lance F. Bosart, Daniel Keyser Department of Atmospheric.
UNSTABLE The UNderstanding Severe Thunderstorms and Alberta Boundary Layers Experiment Neil Taylor 1, Dave Sills 2, John Hanesiak 3, Jason Milbrandt 4.
ELBOW 2001 The Effects of Lake Breezes On Weather Project David Sills, MSC-MRB Peter Taylor, York University Patrick King, MSC-MRB Wayne Hocking, University.
Severe Weather.
Case Studies of Warm Season Cutoff Cyclone Precipitation Distribution Jessica Najuch Department of Earth and Atmospheric Sciences University at Albany,
A Diagnostic Analysis of a Difficult- to-Forecast Cutoff Cyclone from the 2008 Warm Season Matthew A. Scalora, Lance F. Bosart, Daniel Keyser Department.
An Examination of the Tropical System – Induced Flooding in Central New York and Northeast Pennsylvania in 2004.
The Understanding Severe Thunderstorms and Alberta Boundary Layers Experiment (UNSTABLE): Overview and Preliminary Results Neil M. Taylor 1, D. Sills 2,
Earth’s Weather and Climate
Chapter 24 Section 4 Handout
UNDERSTANDING TYPHOONS
Impact of the 4D-Var Assimilation of Airborne Doppler Radar Data on Numerical Simulations of the Genesis of Typhoon Nuri (2008) Zhan Li and Zhaoxia Pu.
Develop and use models to explain how relationships between the movement and interactions of air masses, high and low pressure systems, and frontal boundaries.
Wednesday, November 16th Attendance Attendance Go over Unit Test 3 Go over Unit Test 3 Make-up work and/or weather dvd Make-up work and/or weather dvd.
Storms and Weather Forecasts
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.
Transition of Radar Refractivity to Operational Radars OS&T Briefing, 6 April 2004 Interested parties: NCAR, McGill University, NEXRAD Office of Science.
Geog 1900: Extreme Weather and Climate. Review of last lecture Atmosphere: A mixture of gas molecules, microscopically small particles of solid and liquid,
The fear of the LORD is the beginning of wisdom 陳登舜 ATM NCU Group Meeting REFERENCE : Liu., H., J. Anderson, and Y.-H. Kuo, 2012: Improved analyses.
GHP and Extremes. GHP SCIENCE ISSUES 1995 How do water and energy processes operate over different land areas? Sub-Issues include: What is the relative.
Weather Your Name. What is Weather? Insolation Atmosphere.
Flash Flood Forecasting on a Tropical Small Island towards Disaster Preparedness – Trinidad Glendell De Souza Science & Technology Officer Caribbean Meteorological.
By Christopher Gitro NWS Binghamton, NY.  Flash flooding remains the number 1 weather killer across the US  29 flash flood related fatalities in BGM’s.
Strategic Plan for Korean Participation in T-PARC 2008 Hee-Sang Lee Forecast Research Lab., NIMR/ KMA April. 7-8, 2008 Tsukuba, Japan.
Importance of the atmospheric boundary layer (1).
Potential Benefits of Multiple-Doppler Radar Data to Quantitative Precipitation Forecasting: Assimilation of Simulated Data Using WRF-3DVAR System Soichiro.
World Weather Research Programme Synoptic Predictabilities (THORPEX) Mesoscale Weather Forecasting Research Tropical Meteorology Research Nowcasting Verification.
Nowcasting Trends Past and Future By Jim Wilson NCAR 8 Feb 2011 Geneva Switzerland.
Northeast Convective Flash Floods: Helping Forecasters Stay Ahead of Rising Water Joe Villani - National Weather Service, Albany, NY Derek Mallia - University.
ATMS 373- Mountain Meteorology Packet#1 –What is meant by “Mountain Meteorology”?
Steve Koch National Severe Storms Laboratory Steve Koch National Severe Storms Laboratory WELCOME to the WoF – HiW Workshop of 2014.
Do Now 2/11/13 1. ________ is any form of condensed water vapor in the atmosphere falling back to Earth. 2. Name the global winds that blow from east to.
ASCL Workshop— Boulder, CO Fundamental Concepts for Essential Principal: Atmospheric circulations transport matter, gases, particles, energy and momentum.
WMO-JMA Public Forum Workshop of the World Conference on Disaster Reduction: Reducing Risks of Weather, Climate and Water Extremes through Advanced Detecting,
National Weather Service Water Science and Services John J. Kelly, Jr. Director, National Weather Service NOAA Science Advisory Board November 6, 2001.
Ensemble variability in rainfall forecasts of Hurricane Irene (2011) Molly Smith, Ryan Torn, Kristen Corbosiero, and Philip Pegion NWS Focal Points: Steve.
Weather Prediction and Usefulness for Forecasting Howie Bluestein David Parsons.
GEOGRAPHY 120: EARTH SYSTEM II. Atmospheric Sciences at a Glance.
Weather Fronts and Storms
Tammy M. Weckwerth Various Features Influencing Convection Initiation on 12 June 2002 during IHOP_2002* Tammy M. Weckwerth (NCAR) WWRP Symposium on Nowcasting.
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.
High impact weather nowcasting and short-range forecasting using advanced IR soundings Jun Li Cooperative Institute for Meteorological.
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Heavy Rain Climatology of Upper Michigan Jonathan Banitt National Weather Service Marquette MI.
The Water Cycle - Kickoff by Kevin Trenberth -Wide Ranging Discussion -Vapor -Precip/Clouds -Surface Hydrology (Land and Ocean) -Observations and scales.
60 min Nowcasts 60 min Verification Cold Front Regime
5th Grade Science Chp. 9 Weather.
NWS Forecast Office Assessment of GOES Sounder Atmospheric Instability
Overview of The International H2O Project (IHOP_2002)
Overview of USWRP’s International H2O Project (IHOP_2002)
Hui Liu, Jeff Anderson, and Bill Kuo
Open Science Conference
Unit 4 Lessons Vocabulary.
Severe Weather.
Severe Weather.
Neil Taylor Hydrometeorology and Arctic Lab
Edward I. Tollerud1, Brian D. Jamison2, Fernando Caracena1, Steven E
UNSTABLE Science Question 1: ABL Processes
Science of Rainstorms with applications to Flood Forecasting
Moisture Variability and Nocturnal Convection
Severe Weather DCI: 6.ESS2.6
Presentation transcript:

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 The International H 2 O Project (IHOP_2002) -- Two years Later Expected Outcomes, Pleasant Surprises and Future Challenges David Parsons and Tammy Weckwerth NCAR/ATD Boulder, CO USA

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Motivation

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Motivation Floods, especially flash floods, cause more deaths each year than tornadoes, hurricanes, lightning and wind storms Significant property losses due to flash floods and they are the highest percentage of federal aid events. (Recently >$8 billion per year and rising). Warnings are difficult: often night time events, public perception of precipitation events, dependent on hydrology and meteorology, and increases in skill will help (current warnings often < 1h). The problem of poor forecasts of flash floods and warm season convective is a problem that is international in scope. It has been argued that improvements in QPF for non-flood situations will have significant economic and social benefit. IHOP_2002 research will benefit other warm season warning and prediction problems

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Goals of IHOP_2002 Improved understanding and prediction of warm season rainfall (0 –12 h forecast) Improved characterization of the time varying 3-D distribution of water vapor Four overlapping research components –Convective initiation –Quantitative precipitation forecasting –Atmospheric Boundary Layer –Instrumentation (optimal mix)

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Isentropic Airflow and Sounding Domain Isentropic streamlines (37 C) for 2330 UTC 4 May The dashed lines are isobars at 100 hPa intervals (from Carlson and Ludlam 1968)

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 IHOP Summary: 13 May to 25 June >200 Technical participants from France, the US, Germany and Canada ~2500 additional soundings > 50 instrument platforms, 6 aircraft, 45 IOPs 268 h of airborne water vapor lidar measurements 76 h of airborne satellite evaluation measurements (S-HIS and NAST) Dedicated GOES-11 data

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Convective Initiation – Expected Outcomes

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Atmospheric Boundary Layer Studies Expected Outcomes

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 QPF – Expected Outcomes IHOP Research Forecast Models (courtesy of Steve Koch, NOAA/FSL)

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Instrumentation (Optimal Mix) Expected Outcomes

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Instrumentation (Optimal Mix) Expected Outcomes

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Some Pleasant Surprises BORRREEEEESSSSS !!!!!!!!!!

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Some Pleasant Surprises BORRREEEEESSSSS !!!!!!!!!!

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 One Example of Several Pleasant Instrumentation Surprises --- Refractivity

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Some Pleasant Surprises Use of Data Set for Diverse and Unexpected Applications U wind for LLJ anomaly from the diurnal mean Obs Climate Model

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 CAM3 Diurnal Composite (SGP, IHOP period)

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Some Successes Over the Past Year Rapid movement toward collaborative work, sometimes stretching well beyond the expected boundaries Rapid movement toward a mix of case studies and climatologies Healthy mix of observations and modeling work

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Will IHOP_2002 be considered a success? Publications are one measure of success –Some refereed publications are starting to appear –Strong showing in conference literature –Special issue in Monthly Weather Review

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Will IHOP_2002 be considered a success? Impact on operational forecasting will be another measure utilized –Prediction #1 – Radar refractivity will become operational in large part due to IHOP_2002 –Operational interest and eventual operational impact of reference radiosonde results –Prediction #2 – Strong (possibly under appreciated) impact on operations through new conceptual model and increased knowledge of how to model convection

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Impact on operational forecasting will be another measure utilized Potential to contribute to big picture questions facing NWP –Increase and improve utilization of satellite data sets over land –Improved treatment of land surface processes –Improved assimilation of water (cloud, vapor and precipitation) Propose a meeting Thursday at lunch to discuss the long awaited assimilation workshop

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Impact on operational forecasting will be another measure utilized Tammy Weckwerth if you have ideas on other contributions of IHOP_2002 to prediction of warm season convection Appreciate thoughts from PIs on how IHOP_2002 will address the other two big picture issues and how transfers to operations will occur

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Prospective on Future Experiments IHOP_2002 –Regional-scale meridional gradient in mixing ratio, soil moisture and vegetation –High CAPE but strong CIN (the original conditionally unstable environment) –“Relatively” low impact of transient synoptic disturbances –Strong terrain impact to the west of the experimental domain –Large systems are nocturnal

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Prospective on Future Experiments CSIP –Smaller impact of gradients in soil moisture and vegetation –Lower CAPE but less CIN –Stronger impact of transient synoptic disturbances –Modest terrain impacts within the experimental domain –Lack of “continental” propagation of large convective systems

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Prospective on Future Experiments German QPF experiment –Smaller impact of gradients in soil moisture and vegetation –Lower CAPE but less CIN –Large terrain impacts within the experimental domain so that terrain may control convective systems –Strong impact of transient synoptic disturbances

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 THORPEX The THORPEX slides on the European flood are courtesy of Melvyn Shapiro, Co-chair, THORPEX International Science Steering Committee

1 st Example: Central European Floods August 2002 Prague

Dundee Satellite Station: 1241 UTC 11 Aug France Italy The Storm

Dresden Germany

Central European Floods Cyclogenesis off Japan Courtesy of Shapiro and Thorpe

1

1 2

7 6 5

Flood

2 nd Example: Minnesota Flood: June 2002 Moderate drought on 1 June Widespread rainfall in excess of 5 inches. Flood with >$340 million in federal disaster aid. 80% of homes and businesses damaged in Roseau, MN Locally most significant flood on record.

Minnesota Flood: 9-11 June 2002

Convection along Mei-Yu Front Wisc. flood, previous wave packet ?

1 st Downstream Cyclogenesis

2 nd Downstream cyclogenesis Mn flood from frontal overrunning

Atmospheric Technology Division Opening Remarks, IHOP_2002 Science Team Meeting Toulouse, June 2004 Thank for your attention and for your hard work on IHOP_2002