Title: The International H2O Project IHOP_2002 Two years Later Expected Outcomes, Pleasant Surprises and Fu
1The International H2O Project (IHOP_2002) -- Two
years LaterExpected Outcomes, Pleasant
Surprises and Future Challenges
- David Parsons and Tammy Weckwerth
- NCAR/ATD
- Boulder, CO
- USA
2Motivation
3Motivation
- 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 gt8 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 lt 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
4Goals 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)
5Isentropic Airflow and Sounding Domain
Isentropic streamlines (37 C) for 2330 UTC 4 May
1961. The dashed lines are isobars at 100 hPa
intervals (from Carlson and Ludlam 1968)
6IHOP Summary 13 May to 25 June
- gt200 Technical participants from France, the US,
Germany and Canada - 2500 additional soundings
- gt 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
7Convective Initiation Expected Outcomes
8Atmospheric Boundary Layer Studies Expected
Outcomes
9QPF Expected Outcomes
IHOP Research Forecast Models (courtesy of
Steve Koch, NOAA/FSL)
10Instrumentation (Optimal Mix)Expected Outcomes
11Instrumentation (Optimal Mix)Expected Outcomes
12Some Pleasant Surprises
- BORRREEEEESSSSS !!!!!!!!!!
13Some Pleasant Surprises
- BORRREEEEESSSSS !!!!!!!!!!
14One Example of Several Pleasant Instrumentation
Surprises --- Refractivity
15Some Pleasant SurprisesUse of Data Set for
Diverse and Unexpected Applications
U wind for LLJanomaly from the diurnal mean
Climate Model
Obs
16CAM3 Diurnal Composite (SGP, IHOP period)
17Some 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
18Will 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
19Will 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
20Impact 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
21Impact on operational forecasting will be another
measure utilized
- Email 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
22Prospective 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
23Prospective 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
24Prospective 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
25THORPEX
- The THORPEX slides on the European flood are
courtesy of Melvyn Shapiro, Co-chair, THORPEX
International Science Steering Committee
261st Example Central European Floods
Prague
August 2002
27The Storm
France
Italy
Dundee Satellite Station 1241 UTC 11 Aug. 2002
28Dresden Germany
29Central European Floods
Cyclogenesis off Japan
Courtesy of Shapiro and Thorpe
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Flood
412nd Example Minnesota Flood 9-11 June 2002
Moderate drought on 1 June Widespread rainfall
in excess of 5 inches. Flood with gt340
million in federal disaster aid. 80 of homes
and businesses damaged in Roseau, MN Locally
most significant flood on record.
42Minnesota Flood 9-11 June 2002
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48Wisc. flood, previous wave packet ?
Convection along Mei-Yu Front
491st Downstream Cyclogenesis
50Mn flood from frontal overrunning
2nd Downstream cyclogenesis
51Thank for your attention and for your hard work
on IHOP_2002