Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO

Similar documents
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 cumulus clouds during RICO

Boundary Layer Structure, Turbulence and Shallow Cumulus Observations During RICO 2005

Aircraft Observations for ONR DRI and DYNAMO. Coupled Air-sea processes: Q. Wang, D. Khelif, L. Mahrt, S. Chen

On Trade-Wind Cumulus Cold Pools

P1.17 SENSITIVITY OF THE RETRIEVAL OF STRATOCUMULUS CLOUD LIQUID WATER AND PRECIPITATION FLUX TO DOPPLER RADAR PARAMETERS

Lecture 11: Doppler wind lidar

NOAA Research Vessel Ronald H. Brown Participation and Operations During NAME

On Trade-Wind Cumulus Cold Pools

APPENDIX 2 OVERVIEW OF THE GLOBAL PRECIPITATION MEASUREMENT (GPM) AND THE TROPICAL RAINFALL MEASURING MISSION (TRMM) 2-1

In Situ Comparisons with the Cloud Radar Retrievals of Stratus Cloud Effective Radius

On Trade-Wind Cumulus Cold Pools

NARVAL. North Atlantic Rainfall Validation. Christian Klepp, Stephan Bakan, Gerhard Peters, Bjorn Stevens, Lutz Hirsch, Johannes Quaas

Novel Product Line FMCW Cloud Radars

Radar Observations of Updrafts, Downdrafts, and Turbulence in Fair-Weather Cumuli

P1.6 Simulation of the impact of new aircraft and satellite-based ocean surface wind measurements on H*Wind analyses

Remote Sensing in Meteorology: Satellites and Radar. AT 351 Lab 10 April 2, Remote Sensing

(Preliminary) Observations of Tropical Storm Fay Dustin W Phillips Kevin Knupp, & Tim Coleman. 34th Conference on Radar Meteorology October 8, 2009

WELCOME TO THE FIRST RICO PLANNING WORKSHOP. RICO NOVEMBER 24, 2004 JANUARY 24, 2005 Antigua and Barbuda

SANDRINE BONY AND BJORN STEVENS

REVISION OF THE STATEMENT OF GUIDANCE FOR GLOBAL NUMERICAL WEATHER PREDICTION. (Submitted by Dr. J. Eyre)

Robert Houze University of Washington (with contributions from B. Smull)

Measurements are infrequent in this region due to difficulty in making both ship- and air-based measurements Natural pristine region far removed from

C-130 and instrumentation for RICO

Status-quo of COPS Scientific Preparation, Candidate Instrumentation, Workshop Overview

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

The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter

Interpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation

Convective Structures in Clear-Air Echoes seen by a Weather Radar

Snow Microphysical Retrieval Based on Ground Radar Measurements

OWLeS (Ontario Winter Lake-effect Systems)

HY-2A Satellite User s Guide

Meteorology 311. RADAR Fall 2016

Steven Greco* and George D. Emmitt Simpson Weather Associates, Charlottesville, VA. 2. Experiments

LAUNCH Concept. Lindenberg Observatory

Turbulence Measurements. Turbulence Measurements In Low Signal-to-Noise. Larry Cornman National Center For Atmospheric Research

RPG Dual Polarization Dual Frequency Scanning Cloud Radar Systems: Configurations and Applications

Zhongxun LIU (ISAE/NUDT), Nicolas JEANNIN(ONERA), François VINCENT (ISAE), Xuesong WANG(NUDT)

Tr a n s r e g i o n a l C o l l a b o r a t i v e Re s e a r c h C e n t r e TR 172

EUREC 4 A. A proposal for a HALO deployment out of Barbados to measure the winter North Atlantic Trades in February 2020

AN ANALYSIS OF A SHALLOW COLD FRONT AND WAVE INTERACTIONS FROM THE PLOWS FIELD CAMPAIGN

Cloud Observations at UFS Schneefernerhaus Towards the Evaluation of Satellite Observations and Numerical Weather Prediction

The EarthCARE mission: An active view on aerosols, clouds and radiation

WIND PROFILER NETWORK OF JAPAN METEOROLOGICAL AGENCY

The Next Generation Polarimetric Airborne Doppler Radar

LAUNCH Concept. Lindenberg Observatory

WP11 PHYSICAL ACCESS TO RIs

The Retrieval of Stratus Cloud Droplet Effective Radius with Cloud Radars

The difficult art of evaluation clouds and convection representation in GCM s

A HIGH RESOLUTION HYDROMETEOR PHASE CLASSIFIER BASED ON ANALYSIS OF CLOUD RADAR DOPLLER SPECTRA. Edward Luke 1 and Pavlos Kollias 2

Lower Troposphere Remote Sensing Activities at UMBC

Summary of ABL group discussions: IHOP Planning meeting National Center for Atmospheric Research Boulder, CO April, 2001

Evolution of NOAA s Observing System Integrated Analysis (NOSIA)

Airborne Studies of High Wind and Rain Effects Using IWRAP

UFO Database. UFO Dissemination Workshop 23/04/2015. NLR, Amsterdam. Oleg A. Krasnov and the UFO team

Working Group Initiation of Convection

Rapid Environmental Changes observed by Remote Sensing Systems in the local vicinity of an unusual Colorado Tornado

Contents. 3. Flying strategies Needs for turbulence measurements Vertical structure Horizontal spatial variability Thin interfaces Clouds

A NEW METHOD OF RETRIEVAL OF WIND VELOCITY OVER THE SEA SURFACE IN TROPICAL CYCLONES OVER THE DATA OF MICROWAVE MEASUREMENTS. A.F.

Development of Spaceborne Dualfrequency. and Its Role for the Global Precipitation Measurement

Projects in the Remote Sensing of Aerosols with focus on Air Quality

UK Contribution to YMC Observational Field Campaign

Weather Compass Webquest: Lab/Activity Edition

Clouds, Precipitation and their Remote Sensing

Objectives of CPEA Project

Myung-Sook Park, Russell L. Elsberry and Michael M. Bell. Department of Meteorology, Naval Postgraduate School, Monterey, California, USA

SURF Progresses Contents

ARM Climate Research Facility: Goals and Objectives

Lab 6 Radar Imagery Interpretation

Enhancing information transfer from observations to unobserved state variables for mesoscale radar data assimilation

Validation experiments of GPM/DPR on the pure oceanic precipitating clouds by instruments on board R/V Mirai

Lecture 4b: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ.

F O U N D A T I O N A L C O U R S E

Improved Microwave Radiometric Imaging of Surface Wind Speed Dynamics in the Hurricane Eye-Wall

Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling

Some comments on weather modification and its science base

Projeto Temático FAPESP 2013/ Climate Ecosystems Atmospheric Composition

Recent Improvement of Integrated Observation Systems in JMA

Susceptibility of trade wind cumulus clouds to precipitation. Katrin Lonitz. Berichte zur Erdsystemforschung. Reports on Earth System Science

Reprint 850. Within the Eye of Typhoon Nuri in Hong Kong in C.P. Wong & P.W. Chan

On Surface fluxes and Clouds/Precipitation in the Tropical Eastern Atlantic

2D Wind Field Estimation with Higher Spatial Resolution Using Dual Compact X-Band Weather Radars

Introduction. Suita. Kobe. Okinawa. Tsukuba. Tokyo? in in in in 2017 See Poster #16 2. in 2015

Accident Prevention Program

Lecture 4: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ.

Aerosol-Cloud-Drizzle-Turbulence Interactions in Boundary Layer Clouds

Aerosol-Cloud-Drizzle-Turbulence Interactions in Boundary layer Clouds

University of Notre Dame 2. University of Utah 3. US Army Dugway Proving Grounds 4. University of Virginia 5. Oregon State University 6

The 5th Meeting of the Coordinating Group of the RA II WIGOS Satellite Project

Airborne Remote Sensing for Ocean and Coastal Applications

Threshold radar reflectivity for drizzling clouds

Validation of MÉRA total precipitation at Stornoway (Scotland) with a 24 GHz micro rain radar: A Preliminary Investigation

NOAA ESRL Physical Science Division Arc7c Cruises and Science

Flight Report Sunday September 21, 2014 Summary

RELAMPAGO (working closely with CACTI) is an international project...

A new mesoscale NWP system for Australia

Exploring the Atmosphere with Lidars

Vertical structure and precipitation properties in typhoon rainbands

Ultra clean layers and low albedo ( grey ) clouds in CSET

A synthesis of published VOCALS studies on marine boundary layer and cloud structure along 20S

Transcription:

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)

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 ; Cloud dynamics and precipitation physics 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

Scanning Doppler Lidar (NOAA ETL) Range resolved radial wind speed and intensity measurement once a second Resolution/Range: ~20 cm s-1 ; 5 km Scanning: Motion compensated hemispheric scanner Measurements: Aerosol distributions and wind motions around and below clouds

Ship-Board Instrumentation

R/V Seward Johnson General Specifications Length Overall - 204 feet. Length between Perpendiculars - 183 feet. Beam Overall - 36 feet. Fuel Capacity - 60,000 Gal. Fuel Consumption - 70 gal./hr., normal cruise. Potable Water - 15,000 gal. with RO Unit (120 gal. hr.). Accommodations - 40 (including crew). Speed - 13 knots. Year Built/Converted - 1984/1994.

R/V Seward Johnson

Ship Operations Remote Sensing and In Situ -- Continuous Rawindsondes 6/day Coordination with Island-ased Radars Approx 20 km off shore (daily (?) repositioning) Scanning for Ka-Band Radar and Doppler Lidar

Statistical Properties of precipitating trade wind cumuli from cloud scale to mesoscale 10-15 UM (W/X) o NOAA/K cloud entity swath NOAA 915-MHz 500m NOAA/K meso-scale swath 30 km

Coordination with Other RICO Operations Operations Center Needs: Ship info for mission planning; Ship positioning and operations Mode: Internent; Telephone; Radio (?) Schedule: Before and after planning meetings; regular 6 per day soundings; on-demand Surface-Based Radars Needs: Positioning of ship; Ship operations; Met Input for islandbased radar operations Mode: Radio, Internet, Telephone Schedule: On demand; scheduled times) Aircraft Needs: Ship operations and positioning; Observational input for in-flight operations Mode: Radio Schedule: On demand

Scientific Questions to be Addressed 5. Can we find evidence for cloud processing of aerosol in the aerosol size distributions? 6. Can we detect changes in cloud microphysics under different aerosol loadings?

UM Cloud and Precipitation Mobile Observatory UM W-band Doppler radar Frequency: 94.2 GHz (wavelength = 3.19 mm) Antenna: 0.91 m, Cassengrain 0.24o beamwidth (8-10 m at 1 km range) Vertical resolution: 30 m, Temporal Resolution: 0.5-1 sec PRF: 5-10 khz (4-8 ms-1) Nyquist Doppler spectra, raw I/Q Sensitivity: -52 dbz @ 1 km UM X-band Doppler radar Frequency: 9.4 GHz (wavelength = 3.2 cm) Antenna: 2 m, Cassengrain Vertical resolution: 60 m, Temporal Resolution: 0.5-1 sec PRF: 1-2.5 khz (8-20 ms-1) Nyquist Doppler spectra, raw I/Q Sensitivity: -25 dbz @ 10 km Ceilometer Broadband radiometers IRT Surface Met. Rain gauge ** NOAA/ETL 2 channel Microwave Radiometer

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 largedrop concentrations in fair-weather cumulus clouds? 3. How do the raindrop size distributions evolve from the initial to mature precipitating stages of shallow cumuli?

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?

Approaches Coordination with Surface-Based Radars and Aircraft and Integration of Observations Continuous Monitoring for Cloud Statistics