Profilers & Surface Gauges NE Corner of Stuart Hwy & McMillans 2835-MHz Precip. Profiler: 0.3-18 km 920-MHz Wind Profiler: 0.3-3 km 50-MHz Wind Profiler:

Slides:



Advertisements
Similar presentations
Ewan OConnor, Robin Hogan, Anthony Illingworth Drizzle comparisons.
Advertisements

Convection Initiative discussion points What info do parametrizations & 1.5-km forecasts need? –Initiation mechanism, time-resolved cell size & updraft.
Radar/lidar observations of boundary layer clouds
Robin Hogan Department of Meteorology University of Reading Observations of boundary- layer turbulence using Doppler lidar and surface fluxes.
Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
Allison Parker Remote Sensing of the Oceans and Atmosphere.
Echo Tops Fairly accurate at depicting height of storm tops Inaccurate data close to radar because there is no beam angle high enough to see tops. Often.
Research on Landfalling Hurricanes Utilizing Ground- Based Mobile Research Platforms Kevin Knupp, Dan Cecil, Walt Petersen, and Larry Carey University.
Matthew Shupe Ola Persson Paul Johnston Cassie Wheeler Michael Tjernstrom Surface-Based Remote-Sensing of Clouds during ASCOS Univ of Colorado, NOAA and.
Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
International Research Centre for Telecommunications and Radar High resolution atmospheric profiling with the S-band Doppler polarimetric radar TARA Christine.
Observed Updraft & Mass Flux in Shallow Cumulus at ARM Southern Great Plains site Preliminary results Yunyan Zhang, Steve Klein & Pavlos Kollias CFMIP/GCSS.
Where (not) to measure rainfall Neil I. Fox University of Missouri - Columbia.
Cirrus Production by a Mesoscale Convective System Sampled During TWP-ICE: Analysis via Water Budget Equations Jasmine Cetrone and Robert Houze University.
ASR Science Team Meeting, Bethesda, MD, 17 March 2010 R. Houze, C. Long, S. Medina, C. Zhang AMIE/CINDY/DYNAMO: Observations of the Madden-Julian Oscillation.
AMS 28th Conf. on Hurricanes & Tropical Meteorology Orlando, Florida - 29 April 2007 Convection in the Genesis Phase of Ophelia (2005) Wen-Chau Lee*Michael.
Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the.
IRCTR: International Research Centre for Telecommunications and Radar Evaluation of particle shape and orientation within ice clouds using the S-band Doppler.
Mesoscale Convective Systems Robert Houze Department of Atmospheric Sciences University of Washington Nebraska Kansas Oklahoma Arkansas.
Institut für Physik der Atmosphäre POLDIRAD Polarization Diversity Doppler Radar Martin Hagen DLR Oberpfaffenhofen.
WHAT IS Z?  Radar reflectivity (dBZ)  Microwave energy reflects off objects (e.g. hydrometeors) and the return is reflectivity WHAT IS R?  Rainfall.
Convective-scale diagnostics Rob Rogers NOAA/AOML Hurricane Research Division.
Profilers. Wind profilers are phased array radars that measure the wind as a function of height above a fixed location. Characteristics: Wavelength: 33.
MAPR Multiple Antenna Profiler Radar
International Research Centre for Telecommunications and Radar High resolution 3D wind profiling using an S-band polarimetric FM-CW radar: dealiasing techniques.
Surface and Boundary-Layer Fluxes during the DYNAMO Field Program C. Fairall, S. DeSzoeke, J. Edson, + Surface cloud radiative forcing (CF) Diurnal cycles.
SCOS97-NARSTO Data Analysis Conference SCOS97-NARSTO Upper-Air Meteorological Data Wind / RASS Profiler Processing / Objective QC Bob Weber NOAA/ETL Boulder,
MAGIC Cloud Radars Karen Johnson First MAGIC Science Workshop 5/2014.
The Role of Polarimetric Radar for Validating Cloud Models Robert Cifelli 1, Timothy Lang 1, Stephen Nesbitt 1, S.A. Rutledge 1 S. Lang 2, and W.K. Tao.
The three-dimensional structure of convective storms Robin Hogan John Nicol Robert Plant Peter Clark Kirsty Hanley Carol Halliwell Humphrey Lean Thorwald.
Real-Time Dissemination of Hurricane Wind Fields Determined from Airborne Doppler Radar John Gamache NOAA/AOML/Hurricane Research Division Collaborators:
Assimilating Reflectivity Observations of Convective Storms into Convection-Permitting NWP Models David Dowell 1, Chris Snyder 2, Bill Skamarock 2 1 Cooperative.
Use of Profilers in TRMM Ground Validation Kenneth Gage 1, and Christopher Williams 1,2 1 NOAA Aeronomy Laboratory, Tropical Dynamics and Climate Group.
Potential Benefits of Multiple-Doppler Radar Data to Quantitative Precipitation Forecasting: Assimilation of Simulated Data Using WRF-3DVAR System Soichiro.
Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO Institutions: University of Miami; University.
Matthew Miller and Sandra Yuter Department of Marine, Earth, and Atmospheric Sciences North Carolina State University Raleigh, NC USA Phantom Precipitation.
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:
Matthew Shupe Ola Persson Paul Johnston Duane Hazen Clouds during ASCOS U. of Colorado and NOAA.
KNMI 35 GHz Cloud Radar & Cloud Classification* Henk Klein Baltink * Robin Hogan (Univ. of Reading, UK)
National S&T Center for Disaster Reduction Rainfall estimation by BMRC C-Pol radar ICMCS-V Lei FengBen Jong-Dao Jou 1 Lei Feng and 1,2 Ben Jong-Dao.
Image structures: rain shafts, cold pools, gusts Separate rain fall velocity from air velocity – turbulence retrieval– microphysical retrieval Diurnal.
Boundary-layer turbulence, surface processes, and orographic precipitation growth in cold clouds or: The importance of the lower boundary Qun Miao Ningbo.
Wind Profiler Radar for diagnosis of precipitating clouds K. Krishna Reddy 1, Baio Geng 1, Ryuichi Shirooka 1, Tomoki Ushiyama 1, Hiroyuki Yamada 1, Hisayuki.
BACKGROUND -- Disdrometers measure the rainfall drop size distribution
Japan Blue Radar Observation at Ping-Tung June 10, 2008 Lei Feng 2, Tetsuya Sano 1, Tsung-Jung Lee 2, Satoshi Endo 1 and Ben Jong –Dao Jou 3 1.Hydrosheric.
Ieng Jo, Bruce A. Albrecht and Pavlos Kollias Division of Meteorology and Physical Oceanography Rosenstiel School of Marine and Atmospheric Science (RSMAS),
94-GHz Doppler Radar Observations of Mammatus in Tropical Anvils During Crystal- Face Experiment Ieng Jo Radar Meteorology Group Univ. of Miami.
An Outline for Global Precipitation Mission Ground Validation: Building on Lessons Learned from TRMM Sandra Yuter and Robert Houze University of Washington.
Ordinary Cells Multicell storms Supercells
05/03/2016FINNISH METEOROLOGICAL INSTITUTE Jarmo Koistinen, Heikki Pohjola Finnish Meteorological Institute CARPE DIEM FMI (Partner 5) progress report.
Cheng-Zhong Zhang and Hiroshi Uyeda Hydroshperic Atmospheric Research Center, Nagoya University 1 November 2006 in Boulder, Colorado Possible Mechanism.
Mobile Integrated Profiling System (MIPS) Observations of Boundary Layer and Water Vapor Variations around Boundaries and Storms Kevin Knupp University.
Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO Institutions: University of Miami; University.
Card 2. Option to use “Aerosol Plus” a parameter that characterizes the user defined aerosols and optical properties.
Reflections on Radar Observations of Mesoscale Precipitation
Tadashi Fujita (NPD JMA)
By SANDRA E. YUTER and ROBERT A. HOUZE JR
Development of Assimilation Methods for Polarimetric Radar Data
A dual-polarization QPE method based on the NCAR Particle ID algorithm Description and preliminary results Michael J. Dixon1, J. W. Wilson1, T. M. Weckwerth1,
PACS/EPIC Enhanced Monitoring
The DYMECS project A statistical approach for the evaluation of convective storms in high-resolution models Thorwald Stein, Robin Hogan, John Nicol, Robert.
COPE: The COnvective Precipitation Experiment. Met Office interests
Identifying tornadoes using Doppler radar
The three-dimensional structure of convective storms
Alejandro López Ontavilla
Studying Hector: meteorology and tracer transport
Weather balloons are launched twice a day
Sensitivity of WRF microphysics to aerosol concentration
Weather’s Elements.
Henk Klein Baltink Atmospheric Research Section
Presentation transcript:

Profilers & Surface Gauges NE Corner of Stuart Hwy & McMillans 2835-MHz Precip. Profiler: km 920-MHz Wind Profiler: km 50-MHz Wind Profiler: 2-8 km Joss-Waldvogel Disdrometer Two Rain Gauges ARM Site 50-MHz Boundary Layer Radar: km

2835-MHz Profiler Vertical Beam (only) Precipitation Mode (60 m Pulse) Reflectivity Doppler Velocity Velocity Variance

2835-MHz Profiler Vertical Beam (only) Cloud Mode (500 m Pulse) Reflectivity Doppler Velocity Velocity Variance

920-MHz Profiler Vertical Beam (North or East) Reflectivity Doppler Velocity Velocity Variance

50-MHz Profiler Vertical Beam (North or East) Reflectivity Doppler Velocity Velocity Variance

Surface Disdrometer and Rain Gauges Disdrometer Reflectivity Disdrometer Rain Rate Rain Accumulations

50-MHz and 2835-MHz Spectra Air Motion Hydrometeor

Observed D 0 - Z DR D 0 Retrieved from profiler pair Z DR Estimated from CPOL Brandes et al. (2004): D 0 = 0.171Z DR Z DR Z DR Bringi et al. (2002): D 0 = 1.81Z DR D 0 -Z DR Regression: 1.38 Z DR 0.547

Vertical Air Motion 50-MHz profiler Estimate updraft and downdraft statistics during convection – we have multiple years of data to analyze

50-MHz Boundary Layer Radar – ARM site Low altitude mode (0 – 3 km)

50-MHz Boundary Layer Radar – ARM site High altitude mode (2 – 8 km)