Research Objectives A robust dataset was collected as Hurricane Frances made landfall on the eastern coast of Florida on 5 September 2004. This dataset.

Slides:



Advertisements
Similar presentations
Most Hurricanes are Category 1-3 on the Saffir-Simpson scale. Few are 4 & climatology.
Advertisements

[ ] Preliminary Results of Full-Scale Monitoring of Hurricane Wind Speeds and Wind Loads on Residential Buildings Peter L. Datin Graduate Research Assistant.
DYMECS: Dynamical and Microphysical Evolution of Convective Storms (NERC Standard Grant) University of Reading: Robin Hogan, Bob Plant, Thorwald Stein,
DYMECS: Dynamical and Microphysical Evolution of Convective Storms (NERC Standard Grant) University of Reading: Robin Hogan, Bob Plant, Thorwald Stein,
EXPLORING THE USE OF A PHYSICALLY BASED LIGHTNING CESSATION NOWCASTING TOOL E. V. Schultz 1, W. A. Petersen 2, L. D. Carey 1 1 Univ. of Alabama in Huntsville.
Water Budget of Typhoon Nari (2001) Yang, M.-J.*, S. A. Braun, and D.-S. Chen, 2011: Water budget of Typhoon Nari (2001). Mon. Wea. Rev., 139, ,
Erin Binder and Clemens Grohs Department of Marine and Environmental Systems Florida Tech A Comparative Study of two Thunderstorm events during Field Projects.
~525 m ~800 m ~1200 m Hurricane Rita (2005) 2D wind mapping using DOW data and surface roughness DOW Radar in Galveston, Texas. Hurricane Ike (2008) Correlation.
Research on Landfalling Hurricanes Utilizing Ground- Based Mobile Research Platforms Kevin Knupp, Dan Cecil, Walt Petersen, and Larry Carey University.
Using geospatial analysis techniques to investigate the spatial properties of tropical cyclone rain fields Corene J. Matyas Department of Geography, University.
The evolution and dynamics of an oceanic quasi-linear convective system occurred on Sept. 10, 2004 over the Taiwan Strait Zhao Kun 1,2 and Ben Jong-Dao.
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.
Hurricane Frances (2004) Hurricane Rita (2005) Hurricane Ike (2008) Supported by National Science Foundation grants , , , ,
Deanna Hence, Stacy Brodzik and Robert Houze University of Washington Introduction Methodology TCSP Storms RAINEX Storms Combined TCSP + RAINEX Storms.
Dual-Doppler Wind Retrieval from two operational Doppler radars Yong Kheng Goh, Anthony Holt University of Essex, U. K. for ERAD04, Visby.
1 Cloud Dynamical and Microphysical Problems that Could be Addressed by an Integrated Remote Sensing System R. A. Houze Presented at NCAR CAPRIS Discussion,
Rapid Update Cycle Model William Sachman and Steven Earle ESC452 - Spring 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.
An Examination of the Tropical System – Induced Flooding in Central New York and Northeast Pennsylvania in 2004.
Convective-scale Downdrafts in the Principal Rainband of Hurricane Katrina (2005) Anthony C. Didlake, Jr. COGS Seminar UW, Dept. Atmos Sci., Seattle, November.
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.
Analysis of Three Dimensional Wind Fields from Two Operational Radars Yong Kheng Goh* and Anthony Holt * Doppler radar and wind-field.
Dual-Doppler Wind Retrieval from two operational Doppler radars Yong Kheng Goh, Anthony Holt University of Essex, U. K. for CARPE DIEM, Bologna 29 Nov.
VERTICAL VELOCITY AND BUOYANCY CHARACTERISTICS OF COHERENT ECHO PLUMES IN THE CONVECTIVE BOUNDARY LAYER, DETECTED BY A PROFILING AIRBORNE RADAR Atmospheric.
Robert A. Houze University of Washington Robert A. Houze University of Washington Using the TRMM Precipitation Radar for Storm Structure Analysis Precipitation.
A Spatial Climatology of Convection in the Northeast U.S. John Murray and Brian A. Colle Stony Brook University Northeast Regional Operational Workshop.
Rain Rate Cross-band Velocity Along-band Velocity Cold Pool Pressure Mixing ratio θ θe Δθ e “Gap” stations exhibited minimal Δθ e decrease “Wake” stations.
Some Preliminary Modeling Results on the Upper-Level Outflow of Hurricane Sandy (2012) JungHoon Shin and Da-Lin Zhang Department of Atmospheric & Oceanic.
Vortex Rossby Waves in Hurricanes Katrina and Rita (2005) Falko Judt and Shuyi S. Chen Rosenstiel School of Marine and Atmospheric Science, University.
MESOSCALE OCEANIC VARIABILITY EXPERIMENT (MOVE) Shay et al. SCIENTIFIC GOAL: To observe and understand the role of mesoscale oceanic processes on littoral,
Study Design and Summary Atmospheric boundary layer (ABL) observations were conducted in Sapporo, Japan from April 2005 to July Three-dimensional.
Measuring gaps in tropical cyclone rainbands using Level II radar reflectivity data Corene Matyas Department of Geography, University of Florida Funding:
A Conceptual Model for the Hydrometeor Structure of Mesoscale Convective Systems during the MJO Active Stage Hannah C. Barnes Robert A. Houze, Jr. University.
Earth-Sun System Division National Aeronautics and Space Administration SPoRT SAC Nov 21-22, 2005 Regional Modeling using MODIS SST composites Prepared.
WSR – 88D Observations of Tropical Cyclone Low-level Wind Maxima Lubbock Severe Weather Conference February, Ian M. Giammanco 1, John L. Schroeder.
Alvarado radar loop as received from Mexico. This is the radar reflectivity animation covering the period September 16, Z to September 17, 2010.
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:
Jorgensen, D. P., 1984a: Mesoscale and convective-scale characteristics of mature Hurricanes. Part I: General observations by research aircraft. J. Atmos.
Analysis of Cloud-to-Ground Lightning Within 16 Landfalling Hurricanes Danielle Nagele.
Hurricane Karl’s landfall as seen by high-resolution radar data and WRF Jennifer DeHart and Robert Houze Cyclone Workshop NASA grants: NNX13AG71G.
GPS Doppler & Buoy 0 – 3 km 3 – 6 km 6 – 10 km Obs Cell Bunkers SFC Cell C CSCN Cell B BSBN 1040 UTC C E B F D A 1108 UTC Cell mergers Upwind flank development.
Cloud structure and organization under suppressed conditions during DYNAMO/AMIE/CINDY2011 Angela Rowe and Robert Houze, Jr. University of Washington 31.
Mesoscale and Convective Structure of a Hurricane Rainband Barnes, G. M., E. J. Zipser, D. Jorgensen, and F. Marks, Jr., 1983: J. Atmos. Sci., 40,
Chasing April Showers Convective storms on Wednesday 11 th April, 2012 WCD Friday 4 th May, 2012 Thorwald Stein DYMECS research assistant *Not by running.
94-GHz Doppler Radar Observations of Mammatus in Tropical Anvils During Crystal- Face Experiment Ieng Jo Radar Meteorology Group Univ. of Miami.
Doppler Lidar Winds & Tropical Cyclones Frank D. Marks AOML/Hurricane Research Division 7 February 2007.
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.
Reflections on Radar Observations of Mesoscale Precipitation
Kevin Knupp, Walt Peterson and Dan Cecil
Rosenstial School of Marine and Atmospheric Science
Derek Ortt1 and Shuyi S. Chen, RSMAS/University of Miami
Yumin Moon & David S. Nolan (2014)
Water Budget of Typhoon Nari(2001)
Chapter 11 Hurricanes.
Conceptual Models of Tropical Cyclone Structures
Convective Contribution to Hurricane Genesis
Convective Contribution to the Genesis of Hurricane Ophelia (2005)
Jennifer C. DeHart, Robert A. Houze, Jr. and Deanna A. Hence
Jennifer C. DeHart, Robert A. Houze, Jr., and Robert F. Rogers
Comparison of secondary eyewall and principal rainband in Hurricane Rita (2005) Not a modeling study Several theories out there for secondary eyewall formation.
Tong Zhu and Da-Lin Zhang 2006:J. Atmos. Sci.,63,
A Multiscale Numerical Study of Hurricane Andrew (1992)
Ming-Jen Yang and Robert A. House Jr. Mon. Wea. Rev., 123,
Dual-Aircraft Investigation of the Inner Core of Hurricane Nobert
Case Study: Evaluation of PBL Depth in an Erroneous HRRR forecast for CI Keenan Eure.
Presentation transcript:

Research Objectives A robust dataset was collected as Hurricane Frances made landfall on the eastern coast of Florida on 5 September This dataset included dual-Doppler coverage of a convective cell in an outer rainband. Using this dataset, the objectives of this research are: 1. To characterize the kinematic structure of the convective cell and compare it to current conceptual models. 2. Examine changes in the kinematic structure of the convective cell as it crosses the coastline.

Conceptual Models/Previous Research  Powell (1990) Hence and Houze (2008) 

Conceptual Models/Previous Research Eastin and Link (2009)

Hurricane Frances (2004)

Hurricane Frances SMART-R Deployment SR-1 deployed at Merritt Island Regional Airport SR-2 deployed at the Space Coast Regional Airport in Titusville. Both radars sampled the northern portions of Frances, including the convective outer rainband. Several shear features are evident

Shear Features 1 and 2

Shear Feature 3 from the Melbourne, FL, WSR-88D

Shear Feature 3

Data Processing Radar data were processed through REORDER and CEDRIC resulting in 35 x 20 x 2.2 km grids of reflectivity, velocity, and horizontal convergence with 100 m spatial resolution. Two radar volumes were processed: When the convective cell was immediately off shore When the convective cell was immediately on shore Roughly 5 minutes elapsed between radar volumes

Preliminary Analysis Summary Preliminary analysis shows: The convective cell compares nicely with conceptual models: convergence on inside of convection and speed max on outside The convective cell seems to straddle the shear feature The shear feature most pronounced at the lowest levels (especially the speed minimum) Horizontal convergence decreases substantially with height Horizontal convergence also decreases as the cell makes landfall

Next Steps… Compute vertical velocity and vorticity for both volumes. Construct vertical slices to evaluate dBz structure and kinematic properties Compare with WSR-88D

References Hence, D.A. and R.A> Houze Jr., 2008: Kinematic structure of convective-scale elements in the rainbands of Hurricanes Katrina and Rita (2005). Journal of Geophysical Research, 113, D15108, doi: /2007JD Powell, M.D., 1990a: Boundary layer structure and dynamics in outer hurricane rainbands. Part I: Mesoscale rainfall and kinematic structure. Monthly Weather Review, 118,