Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO
|
|
|
- Conrad George
- 5 years ago
- Views:
Transcription
1 Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO Institutions: University of Miami; University of Colorado; NOAA ETL Investigators: P. Kollias (UM); J. Hare and A. White (CU); C. Fairall, G. Feingold, and R. Hill (ETL)
2 Understanding the Dynamics and Microphysics of Small Cumuli and Precipitation Onset
3 Scientific Questions to Be Addressed 1. What is the range of the dynamical and microphysical structures in trade-wind cumuli, and how do these structures affect the lifecycle of clouds under varying wind shear, stability, and aerosol conditions? 2. What microphysical / dynamical factors and time scales are involved in the production of large-drop concentrations in fair-weather cumulus clouds? 3. How do the raindrop size distributions evolve from the initial to mature precipitating stages of shallow cumuli?
4 Scientific Questions to be Addressed 4. How is the marine boundary layer altered by precipitation from trade-wind cumuli? 5. What are the statistical properties of precipitating trade-wind cumuli from the cloud to mesoscale scale?
5 Approaches Coordination with Surface-Based Radars and Aircraft and Integration of Observations Continuous Monitoring for Cloud Statistics Intensive Process Studies LES Studies
6 Ship-Based Radars 915-MHz wind profiler--pbl 3-D winds, inversion height, cloud and precipitation structure 9.4 GHz Doppler Radar (upward pointing) Reference reflectivity; Doppler spectra 35 GHz Scanning Doppler cloud radar Reflectivity and Doppler moments; Cloud mapping and microphysical properties; precipitation mapping 94-GHz Doppler radar (stabilized/scanning)--high resolution Doppler spectra; cloud and precipitation microphysics
7 W-Band Cloud Reflectivities
8 Dynamical and Microphysical Structure of Trade-Wind Cumuli Boundary Layer/Cloud Characterizations Inversion Height Horizontal wind Bragg/Rayleigh scattering Updrafts/Downdrafts Entrainment Bragg halo, W-band cloud boundaries 915-MHz wind profiler (SNR) Updraft-Downdraft structures
9 Large drop Formation in Trade-Wind Cumuli High resolution data from NOAA/K (4 /sec) Detection of large drop production Doppler spectrum width from W-band
10 Raindrop DSD evolution in early precipitation stages W/X dual wavelength precipitation retrievals X-band reflectivity (cloud top, morphology) W-band Mie scattering, Doppler spectra Vertical air motion (within 5 cms -1 ) DSD retrieval if Dmax > 1.7 mm Differential reflectivity and mean Doppler X-band Doppler spectra W-band Doppler spectra
11 Cloud Scale to Mesoscale Radar data collection at the highest of temporal and spatial resolution are expected providing a detail 2-D or 3-D mapping of cloud entities The NOAA/K scanning radar is expected to sample a km swath around the ship providing the link between the individual cloud observed overhead and the mesoscale organization of precipitating and non-precipitating tradewind cumuli. Despite strong gaseous attenuation in a tropical environment (0.5 db/km) we anticipate that the NOAA/K will be able to observe first rain echoes (-5 to 0 dbz) at 50 km range.
12 Observing Strategies and Coordination with Other RICO Observing Systems Aircraft Surface-Based Radars
13 UM Cloud and Precipitation Mobile Observatory UM W-band Doppler radar Frequency: 94.2 GHz (wavelength = 3.19 mm) Antenna: 0.91 m, Cassengrain 0.24 o beamwidth (8-10 m at 1 km range) Vertical resolution: 30 m, Temporal Resolution: sec PRF: 5-10 khz (4-8 ms -1 ) Nyquist Doppler spectra, raw I/Q Sensitivity: km UM X-band Doppler radar Frequency: 9.4 GHz (wavelength = 3.2 cm) Antenna: 2 m, Cassengrain Vertical resolution: 60 m, Temporal Resolution: sec PRF: khz (8-20 ms -1 ) Nyquist Doppler spectra, raw I/Q Sensitivity: km Ceilometer Broadband radiometers IRT Surface Met. Rain gauge ** NOAA/ETL 2 channel Microwave Radiometer
Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO
Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO Institutions: University of Miami; University of Colorado; NOAA ETL Investigators: P. Kollias
Ship-based measurements of cloud microphysics and PBL properties in precipitating trade cumulus clouds during RICO
Ship-based measurements of cloud microphysics and PBL properties in precipitating trade cumulus clouds during RICO Allen White and Jeff Hare, University of Colorado/CIRES Bruce Albrecht and Pavlos Kolias,
Radar Observations of Updrafts, Downdrafts, and Turbulence in Fair-Weather Cumuli
1750 JOURNAL OF THE ATMOSPHERIC SCIENCES Radar Observations of Updrafts, Downdrafts, and Turbulence in Fair-Weather Cumuli P. KOLLIAS, B.A.ALBRECHT, R.LHERMITTE, AND A. SAVTCHENKO Division of Meteorology
Boundary Layer Structure, Turbulence and Shallow Cumulus Observations During RICO 2005
Boundary Layer Structure, Turbulence and Shallow Cumulus Observations During RICO 2005 A Thesis Defense By Shaunna Donaher University of Miami, RSMAS April 9 th, 2007 Introduction/ Motivation Previous
Vertical structure and precipitation properties in typhoon rainbands
The 4 th THORPEX-Asia Science workshop, Kunming, China on 31 Oct.-2 Nov. 2012 Vertical structure and precipitation properties in typhoon rainbands Dong-Kyun Kim, Yeon-Hee Kim, Kwan-Young Chung Forecast
P1.17 SENSITIVITY OF THE RETRIEVAL OF STRATOCUMULUS CLOUD LIQUID WATER AND PRECIPITATION FLUX TO DOPPLER RADAR PARAMETERS
P1.17 SENSITIVITY OF THE RETRIEVAL OF STRATOCUMULUS CLOUD LIQUID WATER AND PRECIPITATION FLUX TO DOPPLER RADAR PARAMETERS Yefim L. Kogan*, Zena N. Kogan, and David B. Mechem Cooperative Institute for Mesoscale
Convective Structures in Clear-Air Echoes seen by a Weather Radar
Convective Structures in Clear-Air Echoes seen by a Weather Radar Martin Hagen Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen, Germany Weather Radar Weather radar are normally used to locate
Towards simultaneous retrieval of water cloud and drizzle using ground-based radar, lidar, and microwave radiometer
Towards simultaneous retrieval of water cloud and drizzle using ground-based radar, lidar, and microwave radiometer Stephanie Rusli David P. Donovan Herman Russchenberg Introduction microphysical structure
Introduction. Suita. Kobe. Okinawa. Tsukuba. Tokyo? in in in in 2017 See Poster #16 2. in 2015
1 Introduction We developed the X band Phased Array Weather Radar (PAWR) to watch and predict severe weather disasters caused by localized heavy rainfalls or tornadoes. The PAWR measures 3 dimentional
Novel Product Line FMCW Cloud Radars
Novel Product Line RPG Dual Polarization Dual Frequency Scanning Cloud Radar Systems: Configurations and Applications Edited by Dr. Alexander Myagkov and Dr. Thomas Rose 1 2 Benefit from high operation
(Preliminary) Observations of Tropical Storm Fay Dustin W Phillips Kevin Knupp, & Tim Coleman. 34th Conference on Radar Meteorology October 8, 2009
(Preliminary) Observations of Tropical Storm Fay Dustin W Phillips Kevin Knupp, & Tim Coleman 34th Conference on Radar Meteorology October 8, 2009 Outline I. Research Equipment MIPS, MAX, KJAX (WSR-88D)
Active rain-gauge concept for liquid clouds using W-band and S-band Doppler radars
Active rain-gauge concept for liquid clouds using W-band and S-band Doppler radars Leyda León-Colón *a, Sandra L. Cruz-Pol *a, Stephen M. Sekelsky **b a Dept. of Electrical and Computer Engineering, Univ.
On Trade-Wind Cumulus Cold Pools
On Trade-Wind Cumulus Cold Pools Paquita Zuidema & Zhujun Li Reg Hill, Ludovic Bariteau, Bob Rilling, Chris Fairall, Alan Brewer, Bruce Albrecht, Jeff Hare key finding from RICO: nearly all cloud producing
On Trade-Wind Cumulus Cold Pools
On Trade-Wind Cumulus Cold Pools Paquita Zuidema & Zhujun Li U of Miami Reg Hill, Ludovic Bariteau, Bob Rilling, Chris Fairall, Alan Brewer, Bruce Albrecht, Jeff Hare AGU Dec 2011 key finding from RICO:
RPG Dual Polarization Dual Frequency Scanning Cloud Radar Systems: Configurations and Applications
RPG Dual Polarization Dual Frequency Scanning Cloud Radar Systems: Configurations and Applications Edited by Dr. Alexander Myagkov and Dr. Thomas Rose RPG Radiometer Physics GmbH Werner-von-Siemens-Str.
Snow Microphysical Retrieval Based on Ground Radar Measurements
Snow Microphysical Retrieval Based on Ground Radar Measurements V. Chandrasekar Colorado State University June 27, 2007 1 Outline Role of inter comparing ground and space borne radar Class of measurements
On Trade-Wind Cumulus Cold Pools
On Trade-Wind Cumulus Cold Pools Paquita Zuidema & Zhujun Li contributions from Reg Hill, Ludovic Bariteau, Bob Rilling, Chris Fairall, Alan Brewer, Bruce Albrecht, Jeff Hare if you can t explain something
NOAA Research Vessel Ronald H. Brown Participation and Operations During NAME
NOAA Research Vessel Ronald H. Brown Participation and Operations During NAME Draft: 4 March 2002 Walter A. Petersen 1, Robert Cifelli 1, Steven A. Rutledge 1 and Christopher W. Fairall 2 1 Department
NOTES AND CORRESPONDENCE. On the Use of 50-MHz RASS in Thunderstorms
936 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 0 NOTES AND CORRESPONDENCE On the Use of 50-MHz RASS in Thunderstorms PETER T. MAY Bureau of Meteorology Research Centre, Melbourne, Victoria, Australia
1306 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 15
1306 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 15 The Effect of Vertical Air Motions on Rain Rates and Median Volume Diameter Determined from Combined UHF and VHF Wind Profiler Measurements
Remote Sensing in Meteorology: Satellites and Radar. AT 351 Lab 10 April 2, Remote Sensing
Remote Sensing in Meteorology: Satellites and Radar AT 351 Lab 10 April 2, 2008 Remote Sensing Remote sensing is gathering information about something without being in physical contact with it typically
Some comments on weather modification and its science base
Some comments on weather modification and its science base Woods Hole -- July 31, 2002 Gabor Vali University of Wyoming Collaborators: R.D. Kelly, D. Leon, S. Haimov, S. Gill 1 BASC - WxMod Jul 31, 2002
Aircraft Observations for ONR DRI and DYNAMO. Coupled Air-sea processes: Q. Wang, D. Khelif, L. Mahrt, S. Chen
Aircraft Observations for ONR DRI and DYNAMO (NOAA/ONR/NSF) Coupled Air-sea processes: Q. Wang, D. Khelif, L. Mahrt, S. Chen Deep convection/mjo initiation: Dave Jorgensen, S. Chen, R. Houze Aerosol/Cloud
The EarthCARE mission: An active view on aerosols, clouds and radiation
The EarthCARE mission: An active view on aerosols, clouds and radiation T. Wehr, P. Ingmann, T. Fehr Heraklion, Crete, Greece 08/06/2015 EarthCARE is ESA s sixths Earth Explorer Mission and will be implemented
In Situ Comparisons with the Cloud Radar Retrievals of Stratus Cloud Effective Radius
In Situ Comparisons with the Cloud Radar Retrievals of Stratus Cloud Effective Radius A. S. Frisch and G. Feingold Cooperative Institute for Research in the Atmosphere National Oceanic and Atmospheric
S and Ka-band reflectivity comparison
S and Ka-band reflectivity comparison For Rayleigh scattering and in the absence of propagation effects, the true S and Kaband reflectivity values are equivalent Measured S and Ka-band radar reflectivity
Contents. 3. Flying strategies Needs for turbulence measurements Vertical structure Horizontal spatial variability Thin interfaces Clouds
Contents 1. Planetary Boundary Layer and clouds - Definition - PBL vertical structure - BL Clouds Shallow convection clouds Deep convective clouds Marine Stratocumulus - PBL in complex terrain 2. Probing
Signal Postprocessing and Reflectivity Calibration of the Atmospheric Radiation Measurement Program 915-MHz Wind Profilers
1038 J O U R N A L O F A T M O S P H E R I C A N D O C E A N I C T E C H N O L O G Y VOLUME 30 Signal Postprocessing and Reflectivity Calibration of the Atmospheric Radiation Measurement Program 915-MHz
APPENDIX 2 OVERVIEW OF THE GLOBAL PRECIPITATION MEASUREMENT (GPM) AND THE TROPICAL RAINFALL MEASURING MISSION (TRMM) 2-1
APPENDIX 2 OVERVIEW OF THE GLOBAL PRECIPITATION MEASUREMENT (GPM) AND THE TROPICAL RAINFALL MEASURING MISSION (TRMM) 2-1 1. Introduction Precipitation is one of most important environmental parameters.
Susceptibility of trade wind cumulus clouds to precipitation. Katrin Lonitz. Berichte zur Erdsystemforschung. Reports on Earth System Science
Susceptibility of trade wind cumulus clouds to precipitation Katrin Lonitz Berichte zur Erdsystemforschung Reports on Earth System Science 147 2014 Berichte zur Erdsystemforschung 147 2014 Susceptibility
Satellite measurements of CCN and cloud properties at the cloudy boundary layer: The Holy Grail is it achievable?
Satellite measurements of CCN and cloud properties at the cloudy boundary layer: The Holy Grail is it achievable? C 1 Daniel Rosenfeld, The Hebrew University of Jerusalem E -85 D C -89-93 E -85 D C -93-89
Meteorology 311. RADAR Fall 2016
Meteorology 311 RADAR Fall 2016 What is it? RADAR RAdio Detection And Ranging Transmits electromagnetic pulses toward target. Tranmission rate is around 100 s pulses per second (318-1304 Hz). Short silent
Interpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation
Interpretation of Polar-orbiting Satellite Observations Outline Polar-Orbiting Observations: Review of Polar-Orbiting Satellite Systems Overview of Currently Active Satellites / Sensors Overview of Sensor
Rainfall Characteristics Analysis in Landslides Area Based on Micro Rain Radar
2017 2nd International Conference on Civil Engineering and Rock Engineering (ICCERE 2017) ISBN: 978-1-60595-513-1 Rainfall Characteristics Analysis in Landslides Area Based on Micro Rain Radar Zhiwang
Thunderstorm Downburst Prediction: An Integrated Remote Sensing Approach. Ken Pryor Center for Satellite Applications and Research (NOAA/NESDIS)
Thunderstorm Downburst Prediction: An Integrated Remote Sensing Approach Ken Pryor Center for Satellite Applications and Research (NOAA/NESDIS) Topics of Discussion Thunderstorm Life Cycle Thunderstorm
Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning
Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning Thunderstorms are responsible for most of what we refer to as severe weather,
Assessing uncertainty in radar measurements on simplified meteorological scenarios
Advances in Geosciences, 7, 141 146, 2006 SRef-ID: 1680-7359/adgeo/2006-7-141 European Geosciences Union 2006 Author(s). This work is licensed under a Creative Commons License. Advances in Geosciences
The EarthCARE mission: An active view on aerosols, clouds and radiation
The EarthCARE mission: An active view on aerosols, clouds and radiation T. Wehr, T. Fehr, P. Ingmann, J. v. Bismarck ESRIN, Frascati, Italy 20/10/2015 EARTH Clouds, Aerosols and Radiation Explorer EarthCARE
Warm rain and climate: VOCALS, CloudSat, Models. Robert Wood University of Washington
Warm rain and climate: VOCALS, CloudSat, Models Robert Wood University of Washington Warm rain a missing climatology Image: NASA GSFC Shipboard remote sensing shows frequent precipitation from shallow
AN ANALYSIS OF A SHALLOW COLD FRONT AND WAVE INTERACTIONS FROM THE PLOWS FIELD CAMPAIGN
AN ANALYSIS OF A SHALLOW COLD FRONT AND WAVE INTERACTIONS FROM THE PLOWS FIELD CAMPAIGN P.105 Carter Hulsey and Kevin Knupp Severe Weather Institute and Radar & Lightning Laboratories, University of Alabama
P1.6 Simulation of the impact of new aircraft and satellite-based ocean surface wind measurements on H*Wind analyses
P1.6 Simulation of the impact of new aircraft and satellite-based ocean surface wind measurements on H*Wind analyses Timothy L. Miller 1, R. Atlas 2, P. G. Black 3, J. L. Case 4, S. S. Chen 5, R. E. Hood
"Cloud and Rainfall Observations using Microwave Radiometer Data and A-priori Constraints" Christian Kummerow and Fang Wang Colorado State University
"Cloud and Rainfall Observations using Microwave Radiometer Data and A-priori Constraints" Christian Kummerow and Fang Wang Colorado State University ECMWF-JCSDA Workshop Reading, England June 16-18, 2010
WELCOME TO THE FIRST RICO PLANNING WORKSHOP. RICO NOVEMBER 24, 2004 JANUARY 24, 2005 Antigua and Barbuda
WELCOME TO THE FIRST RICO PLANNING WORKSHOP RICO NOVEMBER 24, 2004 JANUARY 24, 2005 Antigua and Barbuda AGENDA TODAY: Wednesday February 25 1. Introduction and welcome 1:00-1:15 pm (Ochs and Rauber) 2.
The Retrieval of Stratus Cloud Droplet Effective Radius with Cloud Radars
JUNE 00 FRISCH ET AL. 835 The Retrieval of Stratus Cloud Droplet Effective Radius with Cloud Radars SHELBY FRISCH NOAA/Environmental Technology Laboratory, Boulder, Colorado, and Colorado State University,
Airborne Studies of High Wind and Rain Effects Using IWRAP
Airborne Studies of High Wind and Rain Effects Using IWRAP Robert F. Contreras, Stephen J. Frasier, and Tao Chu OVWST Meeting July 5-7, 2006 Salt Lake City, Utah Department of Electrical & Computer Engineering
Observing turbulence in convective clouds. Statistics of Convective Cloud Turbulence from a Comprehensive Turbulence
Statistics of Convective Cloud Turbulence from a Comprehensive Turbulence Retrieval Method for Radar Observations Matthew M. Feist a*, Chris D. Westbrook a, Peter A. Clark a, Thorwald HM. Stein a, Humphrey
Vertical Velocity Statistics in Fair-Weather Cumuli at the ARM TWP Nauru Climate Research Facility
6590 J O U R N A L O F C L I M A T E VOLUME 23 Vertical Velocity Statistics in Fair-Weather Cumuli at the ARM TWP Nauru Climate Research Facility PAVLOS KOLLIAS Department of Atmospheric and Oceanic Sciences,
Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning
Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds featuring vigorous updrafts, precipitation and lightning Thunderstorm: a cumulonimbus cloud or collection of cumulonimbus clouds
C-RITE Workshop Physical Processes in Convection Lawrence Carey
Lightning Image Courtesy Phillip Bitzer Lightning Image Courtesy Phillip Bitzer C-RITE Workshop Physical Processes in Convection Lawrence Carey 5/23/2017 C-RITE - Cloud Electricity and Lightning 1 Properties
LAUNCH Concept. Lindenberg Observatory
Concept Lindenberg Observatory LAUNCH-2005 International Lindenberg Campaign for Assessment of Humidity- and Cloud- Profiling Systems and its Impact on High-Resolution Modelling Objectives Basic Techniques
CHAPTER 2 VALIDATION OF RAIN RATE ESTIMATION IN HURRICANES FROM THE STEPPED FRQUENCY MICROWAVE RADIOMETER (SFMR)
CHAPTER 2 VALIDATION OF RAIN RATE ESTIMATION IN HURRICANES FROM THE STEPPED FRQUENCY MICROWAVE RADIOMETER (SFMR) ALGORITHM CORRECTION AND ERROR ANALYSIS 2.1 Abstract Simultaneous observations by the Lower
2.2 Sounding composite construction. 2.3 Vertical velocity retrieval
7.1 DROPSONDE DERIVED STRUCTURE OF MESOSCALE CONVECTIVE SYSTEMS OBSERVED DURING BAMEX James Correia Jr and R. W. Arritt ; Dept. of Agronomy, Iowa State University, Ames, IA 1. Introduction The Bow echo
SANDRINE BONY AND BJORN STEVENS
EUREC 4 A, THE FIELD STUDY: A DRAFT WHITE PAPER SANDRINE BONY AND BJORN STEVENS This draft white paper is meant to sketch out developing plans for the 2019-2020 EUREC 4 A field study. A more complete document
WEATHER RADAR PRINCIPLES
2017 RA-IV WMO Tropical Meteorology Course 1 March 2017 WEATHER RADAR PRINCIPLES Stacy Stewart Senior Hurricane Specialist NOAA/National Hurricane Center, Miami, Florida COURSE OBJECTIVES Part 1. Brief
Evaluation of raindrop size distribution. retrievals based on the Doppler spectra. using three beams. Christine Unal
Evaluation of raindrop size distribution retrievals based on the Doppler spectra using three beams Christine Unal Remote-sensing of the environment (RE) In this talk: Differential reflectivity Z dr cannot
OBSERVATIONS OF THE 24 JUNE 2003 BOW ECHO CASE DURING BAMEX
PJ5.14 OBSERVATIONS OF THE 24 JUNE 2003 BOW ECHO CASE DURING BAMEX Dustin Phillips 1 and Kevin Knupp Department of Atmospheric Science University of Alabama Huntsville 1. INTRODUCTION In the late 1970s
The Next Generation Polarimetric Airborne Doppler Radar
The Next Generation Polarimetric Airborne Doppler Radar Wen Chau Lee, James Moore, J. Vivekanandan, Eric Loew, J. Salazar Peisang Tsai, and Vanda Grubišić National Center for Atmospheric Research* Boulder,
APPLICATION OF SPECTRAL POLARIMETRY TO A HAILSTORM AT LOW ELEVATION ANGLE
13A.3 1 APPLICATION OF SPECTRAL POLARIMETRY TO A HAILSTORM AT LOW ELEVATION ANGLE T.-Y. Yu 1,2,3,, H. Le 1,2, Y. Wang 4,5, A. Ryzhkov 3,4,5, and M. Kumjian 6 1 School of Electrical and Computer Engineering,
The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter
The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter S. Ellis 1*, R. Rauber 2, P. Tsai 1, J. Emmett 1, E. Loew 1, C. Burghart 1, M. Dixon 1, J. Vivekanandan
12B.3 GROUND-BASED AND. easily. configurable. and airborne. the following remote. (i) S-band dual- Dual-polarization. performed by the.
12B.3 GROUND-BASED AND AIRBORNE WEATHER RADARS AND LIDAR FOR OBSERVING THE ATMOSPHERE J. (Vivek) Vivekanandan*, Eric Loew, Scott Spuler, Wen-Chau Lee and Tammy Weckwerth Earth Observing Laboratory National
Automated rain rate estimates using the Ka-band ARM zenith radar (KAZR)
doi:1.5194/amt-8-3685-215 Author(s) 215. CC Attribution 3. License. Automated rain rate estimates using the Ka-band ARM zenith radar (KAZR) A. Chandra 1, C. Zhang 1, P. Kollias 2, S. Matrosov 3, and W.
J8.6 Lightning Meteorology I: An Introductory Course on Forecasting with Lightning Data
Zajac and Weaver (2002), Preprints, Symposium on the Advanced Weather Interactive Processing System (AWIPS), Orlando, FL, Amer. Meteor. Soc. J8.6 Lightning Meteorology I: An Introductory Course on Forecasting
Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 05 SOME OBSERVING INSTRUMENTS. Instrument Enclosure.
Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology
Introduction. Effect of aerosols on precipitation: - challenging problem - no agreement between the results (quantitative and qualitative)
Introduction Atmospheric aerosols affect the cloud mycrophysical structure & formation (observations, numerical studies) An increase of the aerosol particles: - increases CCN concentrations - decreases
1. Introduction. 2. The data. P13.15 The effect of a wet radome on dualpol data quality
P3.5 The effect of a wet radome on dualpol data quality Michael Frech Deutscher Wetterdienst Hohenpeissenberg Meteorological Observatory, Germany. Introduction Operational radar systems typically are equipped
EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphe
EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphere and ocean in this region. Two aircraft, the National
Retrieving stratocumulus drizzle parameters using Doppler radar and lidar
Retrieving stratocumulus drizzle parameters using Doppler radar and lidar EWAN J. O CONNOR, ROBIN J. OGAN AND ANTONY J. ILLINGWORT Department of Meteorology, University of Reading, United Kingdom Submitted
State of the art of satellite rainfall estimation
State of the art of satellite rainfall estimation 3-year comparison over South America using gauge data, and estimates from IR, TRMM radar and passive microwave Edward J. Zipser University of Utah, USA
A Method for Estimating Rain Rate and Drop Size Distribution from Polarimetric Radar Measurements
830 IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 39, NO. 4, APRIL 2001 A Method for Estimating Rain Rate and Drop Size Distribution from Polarimetric Radar Measurements Guifu Zhang, J. Vivekanandan,
Annual Report for Blue Waters Allocation: Sonia Lasher-Trapp, Oct 2017
Annual Report for Blue Waters Allocation: Sonia Lasher-Trapp, Oct 2017 Project Information: Untangling Entrainment Effects on Hail and Rain in Deep Convective Clouds o Sonia Lasher-Trapp, UIUC, slasher@illinois.edu
S. L. Durden and S. Tanelli Jet Propulsion Laboratory California Institute of Technology 4800 Oak Grove Dr., Pasadena, CA 91109, USA
Progress In Electromagnetics Research Letters, Vol. 8, 115 124, 2009 APPLICATION OF CLUTTER SUPPRESSION METHODS TO A GEOSTATIONARY WEATHER RADAR CONCEPT S. L. Durden and S. Tanelli Jet Propulsion Laboratory
Aerosol-Cloud-Drizzle-Turbulence Interactions in Boundary Layer Clouds
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Aerosol-Cloud-Drizzle-Turbulence Interactions in Boundary Layer Clouds Bruce Albrecht University of Miami Rosenstiel School
Aerosol-Cloud-Drizzle-Turbulence Interactions in Boundary layer Clouds
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Aerosol-Cloud-Drizzle-Turbulence Interactions in Boundary layer Clouds Bruce Albrecht University of Miami Rosenstiel School
Robert Houze University of Washington (with contributions from B. Smull)
Robert Houze University of Washington (with contributions from B. Smull) Winter MONEX Summer MONEX Presented at: International Conference on MONEX and its Legacy, 3-7 Feb 2005, New Delhi Johnson & Houze
SPATIAL AND TEMPORAL VARIABILITY OF DROP SIZE DISTRIBUTION FROM VERTICALLY POINTING MICRO RAIN RADAR (MRR)
SPATIAL AND TEMPORAL VARIABILITY OF DROP SIZE DISTRIBUTION FROM VERTICALLY POINTING MICRO RAIN RADAR (MRR) Malte Diederich, Clemens Simmer and Alessandro Battaglia Meteorological Institute of the University
Vertical Profiles of Rain Drop-Size Distribution over Tropical Semi-Arid- Region, Kadapa (14.47 N; E), India
Vertical Profiles of Rain Drop-Size Distribution over Tropical Semi-Arid- Region, Kadapa (14.47 N; 78.82 E), India K.Hemalatha, D.Punyaseshudu Department of Physics, Rayaseema University, Kurnool Corresponding
Measuring snowfall with a low-power K-band radar (Micro Rain Radar) in polar regions
Measuring snowfall with a low-power K-band radar (Micro Rain Radar) in polar regions M. Maahn 1, P. Kollias 2, S. Kneifel 3, I. Gorodetskaya 4, G. Peters 5 and C. Simmer 6 1 Institute for Geophysics and
Raindrop Size Distributions and Z-R Relations in Coastal Rainfall For Periods With and Without a Radar Brightband
American Meteorological Society 11 th Conference on Mesoscale Processes October 2005, Albuquerque, NM JP4J.1 Raindrop Size Distributions and Z-R Relations in Coastal Rainfall For Periods With and Without
RAINDROP SIZE DISTRIBUTION RETRIEVAL AND EVALUATION USING AN S-BAND RADAR PROFILER
RAINDROP SIZE DISTRIBUTION RETRIEVAL AND EVALUATION USING AN S-BAND RADAR PROFILER by FANG FANG B.S.E.E. University of Central Florida, 3 A thesis submitted in partial fulfillment of the requirements for
NARVAL. North Atlantic Rainfall Validation. Christian Klepp, Stephan Bakan, Gerhard Peters, Bjorn Stevens, Lutz Hirsch, Johannes Quaas
NARVAL North Atlantic Rainfall Validation Christian Klepp, Stephan Bakan, Gerhard Peters, Bjorn Stevens, Lutz Hirsch, Johannes Quaas Klima Campus Meteorologisches Institut, Universität Hamburg Max-Planck-Institut
Atmospheric Lidar The Atmospheric Lidar (ATLID) is a high-spectral resolution lidar and will be the first of its type to be flown in space.
www.esa.int EarthCARE mission instruments ESA s EarthCARE satellite payload comprises four instruments: the Atmospheric Lidar, the Cloud Profiling Radar, the Multi-Spectral Imager and the Broad-Band Radiometer.
Chapter 3 Convective Dynamics 3.4. Bright Bands, Bow Echoes and Mesoscale Convective Complexes
Chapter 3 Convective Dynamics 3.4. Bright Bands, Bow Echoes and Mesoscale Convective Complexes Photographs Todd Lindley Bright band associated with stratiform precipitation in a squall line system 1 Bright
A new mesoscale NWP system for Australia
A new mesoscale NWP system for Australia www.cawcr.gov.au Peter Steinle on behalf of : Earth System Modelling (ESM) and Weather&Environmental Prediction (WEP) Research Programs, CAWCR Data Assimilation
Fine structure of vertical motion in the stratiform precipitation region observed by Equatorial Atmosphere Radar (EAR) in Sumatra, Indonesia
P6A.4 Fine structure of vertical motion in the stratiform precipitation region observed by Equatorial Atmosphere Radar (EAR) in Sumatra, Indonesia Noriyuki, NISHI*, Graduate School of Science, Kyoto University,
Development of Spaceborne Dualfrequency. and Its Role for the Global Precipitation Measurement
Development of Spaceborne Dualfrequency Precipitation Radar and Its Role for the Global Precipitation Measurement Shinsuke Satoh (1), Riko Oki (1), Nobuhiro Takahashi (2), and Toshio Iguchi (2) (1) National
A NEW THREE-DIMENSIONAL VISUALIZATION SYSTEM FOR COMBINING AIRCRAFT AND RADAR DATA AND ITS APPLICATION TO RICO OBSERVATIONS
A NEW THREE-DIMENSIONAL VISUALIZATION SYSTEM FOR COMBINING AIRCRAFT AND RADAR DATA AND ITS APPLICATION TO RICO OBSERVATIONS Dan K. Arthur 1, Sonia Lasher-Trapp 1, Ayman Abdel-Haleem 2, Nicholas Klosterman
Chapter 3 Convective Dynamics Part V ñ Bright Bands, Bow Echoes and MCCs. Bright band associated with stratiform precipitation in a squall line system
Chapter 3 Convective Dynamics Part V ñ Bright Bands, Bow Echoes and MCCs Photographs Todd Lindley (This part contains materials taken from UCAR MCS training module) Bright band associated with stratiform
10/21/2012. Chapter 10 Thunderstorms. Part II. Growth and Development of ordinary Cell Thunderstorms Thunderstorm Electrification.
Chapter 10 Thunderstorms Part I Growth and Development of ordinary Cell Thunderstorms Thunderstorm Electrification Tornadoes Part II Simplified model depicting the life cycle of an ordinary thunderstorm
Status-quo of COPS Scientific Preparation, Candidate Instrumentation, Workshop Overview
Status-quo of COPS Scientific Preparation, Candidate Instrumentation, Workshop Overview Andreas Behrendt, Volker Wulfmeyer Institut für Physik und Meteorologie (IPM), Universität Hohenheim, Stuttgart Christoph
Lab 6 Radar Imagery Interpretation
Lab 6 Radar Imagery Interpretation Background Weather radar (radio detection and ranging) is another very useful remote sensing tool used in meteorological forecasting. Microwave radar was developed in
CuPIDO flight strategy
CuPIDO flight strategy an update based on the July 2004 UWKA facility request Bart Geerts, Rick Damiani, Jeff French Flight schedule: The facility request says that the flights are generally between 7
LAUNCH Concept. Lindenberg Observatory
Concept Lindenberg Observatory LAUNCH-2005 International Lindenberg Campaign for Assessment of Humidity- and Cloud- Profiling Systems and its Impact on High-Resolution Modelling Objectives Basic Techniques
Cloud and Dynamical Processes of Precipitating Warm Cumuli During RICO
Cloud and Dynamical Processes of Precipitating Warm Cumuli During RICO Bart Geerts and Gabor Vali, University of Wyoming Jeffrey French, NOAA Air Resources Laboratory 1 This proposal is linked to the Rain
Precipitation estimate of a heavy rain event using a C-band solid-state polarimetric radar
Precipitation estimate of a heavy rain event using a C-band solid-state polarimetric radar Hiroshi Yamauchi 1, Ahoro Adachi 1, Osamu Suzuki 2, Takahisa Kobayashi 3 1 Meteorological Research Institute,
A HIGH RESOLUTION HYDROMETEOR PHASE CLASSIFIER BASED ON ANALYSIS OF CLOUD RADAR DOPLLER SPECTRA. Edward Luke 1 and Pavlos Kollias 2
6A.2 A HIGH RESOLUTION HYDROMETEOR PHASE CLASSIFIER BASED ON ANALYSIS OF CLOUD RADAR DOPLLER SPECTRA Edward Luke 1 and Pavlos Kollias 2 1. Brookhaven National Laboratory 2. McGill University 1. INTRODUCTION
Zhongxun LIU (ISAE/NUDT), Nicolas JEANNIN(ONERA), François VINCENT (ISAE), Xuesong WANG(NUDT)
Institut Supérieur de l Aéronautique et de l Espace Radar Monitoring of Wake Turbulence in Rainy Weather: Modelling and Simulation Zhongxun LIU (ISAE/NUDT), Nicolas JEANNIN(ONERA), François VINCENT (ISAE),
THE DETECTABILITY OF TORNADIC SIGNATURES WITH DOPPLER RADAR: A RADAR EMULATOR STUDY
P15R.1 THE DETECTABILITY OF TORNADIC SIGNATURES WITH DOPPLER RADAR: A RADAR EMULATOR STUDY Ryan M. May *, Michael I. Biggerstaff and Ming Xue University of Oklahoma, Norman, Oklahoma 1. INTRODUCTION The
EFFECTS OF ALONG-TRACK INTEGRATION ON DOPPLER VELOCITY BIAS WITH A SPACEBORNE CLOUD-PROFILING RADAR
P3.11 EFFECTS OF ALONG-TRACK INTEGRATION ON DOPPLER VELOCITY BIAS WITH A SPACEBORNE CLOUD-PROFILING RADAR Akihisa Uematsu 1 *, Yuichi Ohno 1, Hiroaki Horie 1,2, Hiroshi Kumagai 1, and Nick Schutgens 3
Lecture 11: Doppler wind lidar
Lecture 11: Doppler wind lidar Why do we study winds? v Winds are the most important variable studying dynamics and transport in the atmosphere. v Wind measurements are critical to improvement of numerical
REVISION OF THE STATEMENT OF GUIDANCE FOR GLOBAL NUMERICAL WEATHER PREDICTION. (Submitted by Dr. J. Eyre)
WORLD METEOROLOGICAL ORGANIZATION Distr.: RESTRICTED CBS/OPAG-IOS (ODRRGOS-5)/Doc.5, Add.5 (11.VI.2002) COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS ITEM: 4 EXPERT