August- September NSF NOAA NRL NCAR UW UM AGU, San Francisco, 12 December 2006.

Slides:



Advertisements
Similar presentations
Structure & Structure Change IWTC VI, Topic 1 Chair: Jeff Kepert (Substituting for Hugh Willoughby) Rapporteurs Environmental Effects (E. Ritchie) Inner.
Advertisements

Hurricanes and climate ATOC 4720 class22. Hurricanes Hurricanes intense rotational storm that develop in regions of very warm SST (typhoons in western.
Advanced Research WRF High Resolution Simulations of Hurricanes Katrina, Rita and Wilma (2005) Kristen L. Corbosiero, Wei Wang, Yongsheng Chen, Jimy Dudhia.
Hurricanes. Midlatitude Cyclones vs. Tropical Storms  Midlatitude Cyclones  Cover large area  Have cold fronts and warm fronts  Less violent (except.
Summary of NOAA's 2011 Hurricane Field Program (IFEX) Shirley Murillo – 2011 HFP Field Program Director 1.
August- September NSF NOAA NRL NCAR UW UM RAINEX Workshop, Miami, 5-7 June 2006.
Vorticity Structures Accompanying Eyewall Replacement in Hurricane Rita (2005) R.A. Houze, Jr., and B.F. Smull Department of Atmospheric Sciences University.
February 5th, TRMM Conference The 3-D Reflectivity Structure of Intense Atlantic Hurricanes as seen by the TRMM PR Deanna Hence, Robert Houze.
Deanna Hence, Stacy Brodzik and Robert Houze University of Washington Introduction Methodology TCSP Storms RAINEX Storms Combined TCSP + RAINEX Storms.
Initializing a Hurricane Vortex with an EnKF Yongsheng Chen Chris Snyder MMM / NCAR.
August- September NSF NOAA NRL NCAR UW UM 27th Conference on Hurricanes and Tropical Meteorology, Monterey, CA, 27 April 2006.
Mesoscale Observations in Hurricanes Robert Houze University of Washington First US-China Symposium on Meteorology, Norman, Oklahoma, 26 February 2008.
RAINEX: Convective Structures in Tropical Cyclones Robert Houze D. Hence, A. Didlake, B. Smull, W.-C. Lee, M. Bell Hurricane Workshop NCAR Boulder 23 February.
Three-Dimensional Precipitation Structure of Tropical Cyclones AMS Hurricane and Tropical Meteorology Conference May 2nd, 2008 Deanna A. Hence and Robert.
Convective-scale Downdrafts in the Principal Rainband of Hurricane Katrina (2005) Anthony C. Didlake, Jr. COGS Seminar UW, Dept. Atmos Sci., Seattle, November.
The Relative Contribution of Atmospheric and Oceanic Uncertainty in TC Intensity Forecasts Ryan D. Torn University at Albany, SUNY World Weather Open Science.
Principal Rainband of Hurricane Katrina as observed in RAINEX Anthony C. Didlake, Jr. 28 th Conference on Hurricanes and Tropical Meteorology April 29,
Observational and Modeling Study of Hurricane Rainbands and Intensity Changes aka Rainband and Intensity Change Experiment “RAINEX” Shuyi S. Chen and Robert.
Convective-scale diagnostics Rob Rogers NOAA/AOML Hurricane Research Division.
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.
Some Preliminary Modeling Results on the Upper-Level Outflow of Hurricane Sandy (2012) JungHoon Shin and Da-Lin Zhang Department of Atmospheric & Oceanic.
Real-Time Dissemination of Airborne Doppler Radar Data from the NOAA P-3 Aircraft: A Progress Report PI: John Gamache (HRD) Collaborators: Peter Dodge,
Vortex Rossby Waves in Hurricanes Katrina and Rita (2005) Falko Judt and Shuyi S. Chen Rosenstiel School of Marine and Atmospheric Science, University.
10-15% of eye trajectories escape into the eyewall with more frequent escapes during passes with stronger mesovortices along the eyewall edge Escape trajectories.
NSF Hurricane Research National Science Foundation Pamela Stephens Geosciences Directorate.
Observed Vorticity Structure in Hurricane Rita (2005) Methodology Improvements Michael M. Bell National Center for Atmospheric Research/ Earth Observing.
The Rapid Intensification of Hurricane Karl (2010): Insights from New Remote Sensing Measurements Collaborators: Anthony Didlake (NPP/GSFC),Gerry Heymsfield.
Sensitivity of Tropical Cyclone Inner-Core Size and Intensity to the Radial Distribution of Surface Entropy Flux Wang, Y., and Xu, 2010: Sensitivity of.
Hurricane structure and intensity change : Effects of wind shear and Air-Sea Interaction M é licie Desflots Rosenstiel School of Marine & Atmospheric Science.
Work summarized in collaboration with: Roger Smith, Jun Zhang, S. Braun, Jason Dunion On the dynamics of secondary eyewall formation in Hurricane Edouard.
Rapid Intensification of Hurricane Earl (2010): Vorticity and Mass Flux Budgets 1. Motivation: Various studies have emphasized the importance of different.
3D Vortex and Warm Core Structure for Selected HS3 Cases Using NCAR- NOAA Dropsonde Data Jeffrey B. Halverson, P.I. UMBC Alex Martin, UMBC.
The Impact of FORMOSAT-3/COSMIC GPS RO Data on Typhoon Prediction
Dual-Aircraft Investigation of the inner Core of Hurricane Norbert. Part Ⅲ : Water Budget Gamache, J. F., R. A. Houze, Jr., and F. D. Marks, Jr., 1993:
How Do Outer Spiral Rainband Affect Tropical Cyclone Structure and Intensity? The working hypothesis is based on the fact that the outer rainbands are.
Tropical Transition in the Eastern North Pacific: Sensitivity to Microphysics Alicia M. Bentley ATM May 2012.
Shuyi S. Chen Joseph Tenerelli Rosenstiel School of Marine and Atmospheric Science University of Miami Effects of Environmental Flow and Initial Vortex.
The Rapid Intensification of Hurricane Karl (2010): Insights from New Remote Sensing Measurements Anthony Didlake (NPP/GSFC),Gerry Heymsfield (GSFC), Paul.
1 Aircraft observations of the multiscale structure and evolution of rapidly intensifying tropical cyclones Robert Rogers 1, Paul Reasor 1, Jun Zhang 2,
Real-Time High-Resolution MM5 and WRF Forecasts during RAINEX John P. Cangialosi 1*, S. S. Chen 1, W. Zhao 1, D. Ortt 1 W. Wang 2 and J. Michalakas 2 1.
Simulation of the Impact of New Aircraft- and Satellite-Based Ocean Surface Wind Measurements on Estimates of Hurricane Intensity Eric Uhlhorn (NOAA/AOML)
CHPR An integrated hurricane prediction and response system that allows: Strategic planning (weeks): energy, transportation, supply chains, financial,
2015 HS3 Science Team Meeting Ames Research Center, Moffett Field, CA.
Doppler Lidar Winds & Tropical Cyclones Frank D. Marks AOML/Hurricane Research Division 7 February 2007.
Predicting Hurricanes with Explicit Convection: The Advanced Hurricane-research WRF (AHW) Chris Davis NCAR Earth System Laboratory Mesoscale and Microscale.
Science Questions What is role of hot towers in TC intensification and RI? Are they a cause of intensification or an effect? How does wind and temperature.
Rainbands and Secondary Eye Wall Formation as Observed in RAINEX Derek Ortt and Shuyi S. Chen University of Miami-RSMAS.
Multi-Scale Analysis of the Kinematic and Thermodynamic Structure of TS Humberto Using Dropsonde and Satellite Data Jeffrey B. Halverson, UMBC Alex Martin,
Shuyi S. Chen Rosenstial School of Marine and Atmospheric Science University of Miami (DRAFT only!!! Improving Hurricane Structure and Intensity Forecast:
1 Current and planned research with data collected during the IFEX/RAINEX missions Robert Rogers NOAA/AOML/Hurricane Research Division.
Brandon Kerns*, Shuyi S. Chen, Chiaying Lee, and Falko Judt RSMAS/University of Miami I nterdepartmental H urricane C onference Miami, Florida 28 February.
INNER CORE STRUCTURE AND INTENSITY CHANGE IN HURRICANE ISABEL (2003) Shuyi S. Chen and Peter J. Kozich RSMAS/University of Miami J. Gamache, P. Dodge,
JP1.18 Physical processes associated with surface wind field uncertainty in Hurricanes Katrina and Rita (2005): Use of present and future observational.
Shuyi S. Chen Rosenstial School of Marine and Atmospheric Science University of Miami Overview of RAINEX Modeling of 2005 Hurricanes In the eye of Katrina.
2. WRF model configuration and initial conditions  Three sets of initial and lateral boundary conditions for Katrina are used, including the output from.
Shuyi S. Chen, Robert A. Houze Bradley Smull, David Nolan, Wen-Chau Lee Frank Marks, and Robert Rogers Observational and Modeling Study of Hurricane Rainbands.
Evolution of Hurricane Isabel’s (2003) Vortex Structure and Intensity
Rosenstial School of Marine and Atmospheric Science
Derek Ortt1 and Shuyi S. Chen, RSMAS/University of Miami
Yumin Moon & David S. Nolan (2014)
NOAA Intensity Forecasting Experiment (IFEX)
Hurricane Vortex X L Converging Spin up Diverging Spin down Ekman
Conceptual Models of Tropical Cyclone Structures
University of Washington (with J. C. DeHart, D. Hence, A. C. Didlake)
RAINEX briefing at the NOAA AOC in Tampa
Tropical Cyclone Structure
Bell, M. M. , M. T. Montgomery, and W. -C
Comparison of secondary eyewall and principal rainband in Hurricane Rita (2005) Not a modeling study Several theories out there for secondary eyewall formation.
Dual-Aircraft Investigation of the Inner Core of Hurricane Nobert
Western North Pacific Tropical Cyclone Formation and Structure Change
Presentation transcript:

August- September NSF NOAA NRL NCAR UW UM AGU, San Francisco, 12 December 2006

KatrinaOpheliaRita Hurricanes investigated in RAINEX

Motivation for RAINEX Understanding Rapid Intensity Changes

How do interactions of environment, eyewalls & rainbands in the mature storm… … lead to intensity changes like these? rainband Intensity change problem: Intensity of Katrina (2005) Max Wind Speed (knots) August Willoughby 88

High-Resolution Multi-nested Vortex-Following Numerical Models at University of Miami: UM/RSMAS Coupled Atmos- Wave-Ocean Model 15 km 1.6 km 5 km Mini ensemble MM5 and WRF forecasts using GFS, NOGAPS, CMC, and GFDL forecast fields as initial and lateral boundary conditions Courtesy S. Chen

RitaKatrina Model forecast of eyewall & rainbands at 1.6 km resolution Rain rate Courtesy S. Chen

Distance from vortex center Day RainWind Katrina Courtesy S. Chen

Rita Rain Wind Rain Distance from vortex center Day Courtesy S. Chen

Targeted

RAINEX Flight Coordination ELDORA radar

Katrina

Katrina-28 August ELDORA data Barnes et al. ‘ 83 NRL

Katrina-28 August Confirms “ Barnes ” structure

Rita

RAINEX Flights in Hurricane Rita Cat. 5Concentric Eyewalls Sheared

Concentric eyewalls in Rita Unprecedented

Sample cross section through eyewalls of Rita Horizontal Distance (km)  Height (km)  Eye

Dropsonde in the “ moat ” region 1802 UTC 22 September ‘05 Rita-22 September

ELDORA observations of vorticity in the eyewalls Maybe first observation of “ axisymmetrization ”

Vorticity ELDORA observations of the inner eyewall EyeVorticity This has been called “ turbo-boosting ” of the eyewall Eye Heitht (km) warm air Vortex on eyewall

Inner eyewallOuter eyewall Turbo-boosting Eye Moat formation 2ndary eyewall taking over Courtesy Michael Bell Composite of all ELDORA data

Data Availability

KatrinaOpheliaRita Three important storms observed Innovative satellite-based flight control First use of ELDORA in hurricanes Data available via NCAR field catalog Operations and data analysis aided by high-resolution modeling RAINEX Technical Accomplishments

Formation of “ moat ” documented during eyewall replacement in Rita ELDORA shows high wave no. vorticity pattern in 2ndary eyewall ELDORA confirms internal structure of rainband in Katrina High-res. model captures eyewall replacement in Rita RAINEX Science Directions

Thanks