LOAC (Light Optical Aerosol Counter)

Slides:



Advertisements
Similar presentations
Optical Properties of Aerosol Particles Introduction Atmospheric aerosol particles play a significant role in determining Earth's climate, through their.
Advertisements

LOAC (Light Optical Particle Counter) a new aerosols counter for the determination of their sizes and their main nature under meteorological balloons P.
LOAC (Light Optical Aerosol Counter): a new small balloon-borne aerosol counter/sizer with some particle characterization capabilities J.-B. Renard, G.
Meteorology is the study of weather, weather phenomena, and weather forecasting. It uses two kinds of observations: Qualitative: not based on numbers.
Lecture 12 Content LIDAR 4/15/2017 GEM 3366.
Earth System Science Teachers of the Deaf Workshop, August 2004 S.O.A.R. High Earth Observing Satellites.
GEOS-5 Simulations of Aerosol Index and Aerosol Absorption Optical Depth with Comparison to OMI retrievals. V. Buchard, A. da Silva, P. Colarco, R. Spurr.
TRMM Tropical Rainfall Measurement (Mission). Why TRMM? n Tropical Rainfall Measuring Mission (TRMM) is a joint US-Japan study initiated in 1997 to study.
Holger Vömel NCAR Science Day 17 April 2015 Exploration of the tropical tropopause region during Strateole-2.
JERAL ESTUPINAN National Weather Service, Miami, Florida DAN GREGORIA National Weather Service, Miami, Florida ROBERTO ARIAS University of Puerto Rico.
Some Impacts of Atmospheric Aerosols Direct and Indirect Effects on Climate directly scattering solar radiation altering number and size distribution of.
Atmospheric structure from lidar and radar Jens Bösenberg 1.Motivation 2.Layer structure 3.Water vapour profiling 4.Turbulence structure 5.Cloud profiling.
Atmospheric Measurements at Capel Dewi field station Prof. Geraint Vaughan.
Aerosols and climate Rob Wood, Atmospheric Sciences.
MAOS (Mobile Aerosol Observing System) and the G1 Aircraft at Cape Cod Allie Marquardt Collow.
TROPOSPHERE The troposphere is the lowest layer of Earth's atmosphere. The troposphere starts at Earth's surface and goes up to a height of 7 to 20 km.
ULM Project Ulrich Lemmin Baikal-Selenga workshop, Geneva, 31 October 2012.
Satellite basics Estelle de Coning South African Weather Service
Lidar remote sensing for the characterization of the atmospheric aerosol on local and large spatial scale.
LIDAR: Introduction to selected topics
Stratosphere Troposphere
Daily Starter 1. What has more mass: –one pound of air or one pound of gold –Explain your answer 2. True or false – Water boils at the same temperature.
ATMOSPHERE.
Visualization, Exploration, and Model Comparison of NASA Air Quality Remote Sensing data via Giovanni Ana I. Prados, Gregory Leptoukh, Arun Gopalan, and.
Max Planck Institute for Chemistry P.O. Box 3060 Biogeochemistry Department D Mainz, Germany Manaus plume tracking LBA-Claire 2001 Manaus Fligh track.
1
1 Interaction Between Radiation and the Material Prof. Arnon Karnieli The Remote Sensing Laboratory Jacob Blaustein Institute for Desert Research Ben-Gurion.
CCN measurements at an urban location Julia Burkart University of Vienna Istitute of Aerosol Physics, Biophysics and Environmental Physics.

Lidar Working Group on Space-Based Winds, Snowmass, Colorado, July 17-21, 2007 A study of range resolution effects on accuracy and precision of velocity.
20 – 24 October, th Intl. ChArMEx workshop, Trieste, Italy 1/18 Variability of Mediterranean aerosols properties at three regional background sites.
Chapter 1 Introduction to the Atmosphere ATMO 1300 Spring 2010.
Desert Aerosols By: Michelle Alvarado William Cullen Bryant High School NASA COSI Outreach Program Mentors: Prof. Jeffrey C. Steiner, Earth and Atmospheric.
Atmosphere Chapter 11 Notes. Composition of the Atmosphere Currently: – Nitrogen (N 2 ): 78% – Oxygen (O 2 ): 21% – Argon (Ar) – Carbon dioxide (CO 2.
Earth Science Golodolinski/Black 2009
Page 1 Validation by Balloons and Aircraft - ESRIN - 9– 13 December 2002 Observations of aerosol and clouds obtained during the M-55 Geophysica ENVISAT.
Measurement Example III Figure 6 presents the ozone and aerosol variations under a light-aerosol sky condition. The intensity and structure of aerosol.
Field Methods of Monitoring Atmospheric Systems Remote Sensing Copyright © 2006 by DBS.
Department of Mechanical Engineering The Pearlstone Center for Aeronautical Engineering Studies Ben-Gurion University of the Negev P.O.B. 653, Beer Sheva.
In Situ and Remote Sensing Characterization of Spectral Absorption by Black Carbon and other Aerosols J. Vanderlei Martins, Paulo Artaxo, Yoram Kaufman,
The Planetary Boundary Layer (PBL) is essentially what it says- ‘a layer that bounds the planet,’ specifically this planet, Earth. The PBL is one of two.
Wu Sponsors: National Aeronautics and Space Administration (NASA) Goddard Space Flight Center (GSFC) Goddard Institute for Space Studies (GISS) New York.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
PHAT-TACO Experiment On board ACES-23 Hannah Gardiner, Bill Freeman, Randy Dupuis, Corey Myers, Andrea Spring Science Presentation Team Philosohook.
© 2010, TSI Incorporated Global Sizing Velocimetry (GSV)
Aerosol Limits for Target Tracking Ronald Petzoldt ARIES IFE Meeting, Madison, WI April 22-23, 2002.
1 Atmospheric profiling to better understand fog and low level cloud life cycle ARM/EU workshop on algorithms, May 2013 J. Delanoe (LATMOS), JC.
#1  About 78% of the air is composed of this gas.
ACKNOWLEDGEMENTS: Rob Albee, Jim Wendell, Stan Unander, NOAA Climate Forcing program, DOE ARM program, NASA, Met. Service Canada, Chinese Met. Agency,
Aerosol counting measurements with the LOAC light instrument using weather balloons Gwenael BERTHET, Damien VIGNELLES, Jean-Baptiste RENARD, Fabrice JEGOU,
A new method for first-principles calibration
Phillip Alexander Spence 2 nd period ESS Satellite “Air” Meteor 3M Mission.
Ms. Longo Earth Science Weather & Water. 10/
LPCE:CETP: CESR: LONG DURATION FLIGHTS OF BALLOONS FOR THE STUDY OF STRATOSPHERIC CHEMISTRY IN THE FRAME OF THE TARANIS PROJECT LPCE:Gwenaël BERTHET CETP:
UNIVERSITY OF BASILICATA CNR-IMAA (Consiglio Nazionale delle Ricerche Istituto di Metodologie per l’Analisi Ambientale) Tito Scalo (PZ) Analysis and interpretation.
Topic 5A INSOLATION. WORDS TO KNOW Radiation Insolation Intensity Altitude Zenith Latitude Tropic of Cancer Tropic of Capricorn Solstice Equinox Duration.
Topic 6: Insolation and the Earth ’ s Surface. Insolation- The portion of the Sun ’ s radiation that reaches the Earth INcoming SOLar RadiATION Angle.
Properties of Particulate Matter
CHAPTER ONE- SECTION 1- THE AIR AROUND YOU. Key Concepts: 1. What is the composition of Earth’s Atmosphere? 2. How is the atmosphere important to living.
Aerosols measurements by the LOAC instruments under meteorological balloons (BLD) J.-B. RENARD AND THE LOAC TEAM LPCER-CNRS, ORLÉANS.
Eric BOURRIANNE LPC2E - CNRS, ORLEANS
Science fair- Put your logbook inside your board.
ATMOSPHERIC AEROSOL: suspension of condensed-phase particles in air
ATMOSPHERE.
The Atmosphere.
Atmosphere Characteristics
ATOC 4720: class 17 Atmospheric aerosols
Atmosphere 11-1.
大气圈地球化学及其环境效益.
Meteorological Instrumentation and Observations
Presentation transcript:

LOAC (Light Optical Aerosol Counter) Jean-Baptiste RENARD (LPC2E-CNRS, Orléans, France)

Project funded by the “Agence Nationale de la Recherche” Light Optical Aerosols Counter Project funded by the “Agence Nationale de la Recherche” Collaboration between national research laboratory (LPC2E, LSCE/CEA, LA), private companies (Environnement-SA, Aerophile SAS, MeteoModem), and the French Space Agency 90 copies produced at the end of 2014 50 scientific flights under different kinds of balloons

Instrument and pump: 350 g Electric consumption: ~3 W No lenses => no risk of misalignment Concentrations for 19 size classes between 0.2 and 100 mm Automatic check every 10 minutes and electronic recalibration if necessary (ex. strong changes in temperature) Total weigh (gondola, batteries and LOAC): 1 kg for use with meteo balloons

Principle of measurements 2 scattering angles measurements (field of view of few degrees) ~12°, insensitive to the refractive index of the particles (mainly diffraction) => accurate size determination and counting ~60°, strongly sensitive to the refractive index of the particles => indication of the nature of the particles Detection of the maximum of intensity for particle that crosses the laser beam Real-time stray light correction

Calibrated with beads and real irregular particles Similar statistical approach for the detection of irregular particles (all natural solid particles are irregular) At a given diameter, same scattered flux for different natures of particles (at small scattering angles) LOAC can be used for liquid and irregular particles but not for perfect solid spheres

Small field of view (few degrees) at small scattering angles => large irregular particles are less luminous than expected Confirmation by modelling (Mie) calculations including a roughness surface coefficient

Determination of the main nature of the particles: Speciation The 60° measurements are very sensitive to the refractive index of the particles More absorbing are the particles, lower are the scattered flux The 60° size distribution is often lower than the 12° real size distribution The ratio of the 2 size distributions varies with the nature of the particles

The 12°/60° ratio is compared to charts obtained in laboratory for different families of particles: - Liquid droplets - Minerals - Carbons This is an open data base and other natures of particles can be considered (no more than 3 or 4 different natures)

Pollution carbon particles Saharan sand plume Size distribution Size distribution speciation speciation

Sea salt Inside a cloud Size distribution Size distribution speciation

LOAC is used at ground and under all kinds of balloons: tethered, meteo, low troposphere, stratosphere “Modular” instrument : LOAC can work with different kinds of pump (between 1.3 and 2.7 l/mn) and with different kinds of inlets depending on the sampling conditions

Beginning of the fog Permanent measurements at ground in the south sunburn of Paris to study fog events End of the fog Welas and Fog Monitor : optical counters

Permanent measurements on board the touristic balloon “AOG” in Paris, from ground to an altitude of 250 m Strong pollution event on 11 December 2013 and inversion layer at an altitude of 200 m Close to the ground, various natures At 200m, black carbon

Counting measurements can be converted to PM 2.5 and PM10 mass (mg/m3) Mean densities used from speciation results: 1.4 g/cm3 for carbon 2.2 g/cm3 for minerals and salts 0 g/cm3 for droplets (small changes in case of humidity > 65%) Comparison with microbalance measurements from AirParif ambient air network Very good agreement

LOAC has performed 19 flight under BPCL (long duration tropospheric balloons) and BLD (Meteo balloon) during the Charmex campaign, summer 2013, above the Mediterranean Sea BPCL trajectory on 17 June 2013, altitude of 2000 m

Flight inside a Saharan sand plume Detection of large particles Particles transported during several days No sedimentation Indirect detection of strong electro-magnetic field inside the plume

Vertical profiles of aerosol content with BLD (meteo) balloons 17 June 2013, Minorca 23 June 2014, Ury (France) Liquid particles Liquid droplets + soot Sand plume Cirrus

Fly on-board Unmanned Airborne Vehicles (Fly-N-Sense Society) Environmental studies, analysis of local sources

CONCLUSIONS Actual scientific campaigns: LOAC can provide size distribution and main nature of the aerosols Light instrument for ground and airborne measurements Now a commercial instrument Actual scientific campaigns: Pollution studies in the Paris region (ground, tethered balloon) VOLTAIRE, long-term monitoring of the stratosphere (~25 flights per year at different latitudes)

Future Improved version of LOAC in development STRATEOLE, long duration balloons (several months) in the lower equatorial stratosphere (coordinated by LMD-CNRS) LOAC for space application (CNES) : Studies of planetary atmospheres Earth Mars Titan Saturn

Contact for science application: jbrenard@cnrs-orleans.fr LOAC is commercialized by the MeteoModem company: http://www.meteomodem.com LOAC on board Unmanned Airborne Vehicles is commercialized by the Fly-N-Sense company : http://www.fly-n-sense.com/