Second GALION Workshop 20-23 September 2010, Geneva, Switzerland Lidar products for VAAC Gelsomina Pappalardo Consiglio Nazionale delle Ricerche-Istituto.

Slides:



Advertisements
Similar presentations
IATA Positions for Consideration & Action by IVATF Summary of Flimsy 13 July 2011 IVATF - Montreal.
Advertisements

Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 A Cloud Object Based Volcanic.
Consiglio Nazionale delle Ricerche 3 rd COPS and GOP workshop April 2006 Consiglio Nazionale delle Ricerche Istituto di Metodologie per lAnalisi.
Volcanic Ash - developments since 2010 © Crown copyright Met Office Ian Cameron, Met Office Executive Head Aviation, June 2014.
International standard for aerosol lidar Laurent Sauvage and George Georgoussis On behalf of the whole expert group ISO TC146/SC5/WG6.
World Meteorological Organization Working together in weather, climate and water WMO OMM WMO CAeM Report to ICG-WIGOS February 2015.
Atmospheric structure from lidar and radar Jens Bösenberg 1.Motivation 2.Layer structure 3.Water vapour profiling 4.Turbulence structure 5.Cloud profiling.
Slide: 1 27 th CEOS Plenary |Montréal | November 2013 Agenda Item: 15 Chu ISHIDA(JAXA) on behalf of Rick Lawford, GEO Water CoP leader GEO Water.
ULM Project Ulrich Lemmin Baikal-Selenga workshop, Geneva, 31 October 2012.
Frascati nov 2009 A.-C. Engvall, A. Stohl, N. I. Kristiansen, A. Fahre Vik, K. Tørseth, and others Norwegian Institue for Air Research NILU Dept.
Tianfeng Chai 1,2, Alice Crawford 1,2, Barbara Stunder 1, Roland Draxler 1, Michael J. Pavolonis 3, Ariel Stein 1 1.NOAA Air Resources Laboratory, College.
Ben Kravitz November 5, 2009 LIDAR. What is LIDAR? Stands for LIght Detection And Ranging Micropulse LASERs Measurements of (usually) backscatter from.
WMO WIGOS from the CAS Perspective Sandro Fuzzi National Research Council, Italy WMO: Research Dept.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Implementation activities I 13:30 – 15:00 Technology and Methodology I Birgit Heese: Capabilities and limits of aerosol measurements with ceilometer Dietrich.
WMO TECHNICAL CONFERENCE ON METEOROLOGICAL AND ENVIRONMENTAL INSTRUMENTS AND METHODS OF OBSERVATION TECO-2012, Brussels, Belgium, October 2012 INTEGRATED.
Geneva, September 2010 EARLINET-ASOS Symposium Second GALION Workshop Uncertainties evaluation for aerosol optical properties Aldo Amodeo CNR-IMAA.
Environment Canada Meteorological Service of Canada Environnement Canada Service météorologique du Canada Modeling Volcanic Ash Transport and Dispersion:
Helen DacreDepartment of MeteorologyUniversity of Reading 1 Helen Dacre 1, Alan Grant 1, Natalie Harvey 1, Helen Webster 2, Ben Johnson 2, David Thomson.
EARLINET-ASOS Symposium 20 September 2010, Geneva, Switzerland EARLINET: Future plans Gelsomina Pappalardo Consiglio Nazionale delle Ricerche-Istituto.
CREST Lidar Network (CLN)
2nd INT’L. SYMPOSIUM ON VOLCANIC ASH & AVIATION SAFETY June 2004 Alexandria, Virginia USA CONFERENCE HIGHLIGHTS.
FOREST FIRE AEROSOLS Optical and microphysical properties from EARLINET observations D. Balis Laboratory of Atmospheric Physics, Aristotle University of.
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.
Second GALION Workshop, WMO, Geneva, 20 ‐ 23 September 2010 A d v a n c e d L I D A R S y s t e m s Established in Athens, Greece in 2002 COMPANY SCOPE.
April nd IBTrACS Workshop 1 Operational Procedures How can we build consistent, homogeneous, well- documented climate quality data?
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Airline Meteorologist Perspective on Volcanic Ash UPS/A4A 30 OCT 2012.
International Civil Aviation Organization Aviation System Block Upgrades Module N° B0-105/PIA2 Meteorological information supporting enhanced operational.
© Crown copyright Met Office London VAAC The Eyjafjallajökull volcanic eruption.
1 GOES-R AWG Product Validation Tool Development Aviation Application Team – Volcanic Ash Mike Pavolonis (STAR)
1 GOES-R AWG Product Validation Tool Development Aviation Application Team – Volcanic Ash Mike Pavolonis (STAR)
WE Surface-based Global Observing System for Weather.
1 GOES-R Air Quality Proving Ground Leads: UAH UMBC NESDIS/STAR.
Determination of atmospheric structures, aerosol optical properties and particle type with the R-MAN 510 Raman dual polarization lidar super ceilometer.
1 CALIPSO: Validation activities and requirements Dave Winker NASA LaRC GALION, WMO Geneva, September 2010.
Second GALION workshop, WMO, Geneva September 2010 Aerosol Lidar Observations: A Missing Component Of Near-Real-Time Data Assimilation Requirements.
NASA and Earth Science Applied Sciences Program
WMO SDS-WAS programme. Regional Center for Northern Africa, Middle East and Europe. Activity Report Enric Terradellas, José M. Baldasano, Emilio.
NDACC Aerosol lidar measurements Initially called NDSC (Network for the Detection of Stratospheric Changes) the NDACC was established in 1991 for the monitoring.
Eruption Source Parameters: Improved input to volcanic-ash dispersion models. (Marianne Guffanti, USGS, 4 June 2008) In support of a long-standing interest.
Robin Hogan Ewan O’Connor The Instrument Synergy/ Target Categorization product.
20 Sept nd GALION WS WMO, Geneva 1 Optimisation of Instruments Arnoud Apituley Volker Freudenthaler Adolfo Comeron.
The University of Reading Helen Dacre The Eyjafjallajökull eruption: How well were the volcanic ash clouds predicted? Helen Dacre and Alan Grant Robin.
AGACC II: WP3: Aerosol properties and radiative forcing at Uccle Veerle De Bock Royal Meteorological Institute of Belgium
CGMS-40, Lugano, 5 – 9 November 2012 Toward deriving consistent volcanic ash products from geostationary satellites: Proposal for discussion in WG-II at.
Second GALION Workshop September 2010, Geneva, Switzerland Data assimilation (ICAP) Gelsomina Pappalardo 1, Judd Welton 2 1 Consiglio Nazionale delle.
The Global Cryosphere Watch Jeff Key NOAA/NESDIS, Madison, Wisconsin USA South America GCW Meeting, Santiago, October
The European Organisation for the Safety of Air Navigation V & V Some lessons learned in Europe FAA V&V Symposium, Atlantic City, October 2010 Nigel.
Task DI Progress report Gonéri Le Cozannet IGOS-Geohazards
II GALION workshop - Geneva, Switzerland – September 21-23, 2010 EARLINET contribution to SDS-WAS Europe – North Africa regional node Lucia Mona Istituto.
From science to routine operations – Ceilometer and Lidar networks for cloud and aerosol detection WMO TECO October 2012 W. Thomas Deutscher Wetterdienst.
The University of Reading Helen Dacre The Prediction And Observation Of Volcanic Ash Clouds During The Eyjafjallajökull Eruption Helen Dacre and Alan Grant.
ACCENT Symposium Sept ,Urbino (Italy) CEILOMETER FOR THE AEROSOL PROFILING: OPPORTUNITIES AND LIMITS Fabio Madonna, Ioannis Binietoglou, D’Amico.
Japan Meteorological Agency, May 2014 Coordination Group for Meteorological Satellites - CGMS Volcanic ash algorithm testbed by JMA for validation and.
UNIVERSITY OF BASILICATA CNR-IMAA (Consiglio Nazionale delle Ricerche Istituto di Metodologie per l’Analisi Ambientale) Tito Scalo (PZ) Analysis and interpretation.
CAS/GAW/SSC March 2016 Aeronautical Meteorology.
CGMS-43-NOAA-WP-04 Coordination Group for Meteorological Satellites - CGMS Status report of the CGMS Socioeconomic Benefits Tiger Team (SETT) Presented.
ISES Director’s Report Terry Onsager, April 9, 2015 Accomplishments Actions from 2014 Annual Meeting Complementary Activities Challenges.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Development of a visibility retrieval for the GOES-R Advanced Baseline.
Services & Products of Tokyo VAAC Jun Ryuzaki 30 October, 2012 FPAW in Orlando Tokyo Volcanic Ash Advisory Center Japan Meteorological Agency.
Žarko SIVČEV EUROCONTROL Directorate Network Management
Background on VAACs’ Best Practices
Babes-Bolyai University, RO - General and scientific background -
Lidar difficulties, retrievals, and successes
Mike Pavolonis (NOAA/NESDIS/STAR)
Performance Based Navigation –Civil Aviation Authority Actions
EARLINET/ACTRIS IOP in summer 2012
M. De Graaf1,2, K. Sarna2, J. Brown3, E. Tenner2, M. Schenkels4, and D
IATA Positions for Consideration & Action by IVATF Summary of Flimsy
Presentation transcript:

Second GALION Workshop September 2010, Geneva, Switzerland Lidar products for VAAC Gelsomina Pappalardo Consiglio Nazionale delle Ricerche-Istituto di Metodologie per l’Analisi Ambientale CNR-IMAA, Potenza, Italy

Second GALION Workshop September 2010, Geneva, Switzerland At the 5th International Workshop on Volcanic Ash, organized by WMO in cooperation with ICAO held in Santiago de Chile from 17 to 21 March 2010, the formation of a Scientific Steering/Advisory Group was proposed in order to create a single, authoritative source of scientific expertise in the field of volcanic ash affecting civil aviation with emphasis both on meteorological (remote sensing and in-situ observations, transport and dispersion modeling) as well as geophysical/volcanological issues such as eruption source parameters, ash characteristics, ash fallout and aggregation. This expertise was to be made available to the relevant ICAO IAVWOPS (International airways volcano watch operations group) group as a basis for future development of operational procedures, standards and guidance. This proposal was subsequently adopted by the WMO Executive Council at its 62nd session in Geneva and fully supported by the Secretary General of IUGG.

Second GALION Workshop September 2010, Geneva, Switzerland The eruption of the Icelandic volcano Eyjafjallajökull starting on 14 April 2010, leading to widespread airspace closures and unprecedented disruption to air traffic, prompted the formation of several national, regional and global groups and task forces under the egis of different governing bodies. ICAO decided to create an international Task Force on Volcanic Ash (IVATF) with the mandate to accelerate the production of guidance and standards in view of the serious effect of the aftermath of these eruptions on air traffic. The inaugural meeting of the VA-SAG was thus timed to follow-on to the first meeting of the ICAO IVATF, held in Montreal from 27 to 30 July 2010, and was expected to respond to the questions and deliverables determined by the IVATF and its sub-groups.

Second GALION Workshop September 2010, Geneva, Switzerland Task 1 Determine the ways and means to improve volcanic cloud detection/ avoidance systems for pre-flight and en-route decisions by operators and regulators Three sub-task leaders: - Gelsomina Pappalardo (CNR) for ground-based; - DLR (Ulrich Schumann and Hans Schlager) for air-borne measurements; - Mike Pavolonis (Wisconsin) for space-based sensing; and, - Fred Prata (NILU) will take overall responsibility as Task leader. Deliverable Guidance material identifying technologies and recommended system requirements for pertinent ground, airborne and space-based systems Milestones (progress reports) 13 October 2010; 12 January 2011; 6 April 2011; 1 June 2011

Second GALION Workshop September 2010, Geneva, Switzerland Expected reports will cover the following environments: 1) pre-eruptive 2) near-field 3) far-field

Second GALION Workshop September 2010, Geneva, Switzerland Discussion metrics OVERARCHING THEMES: - Availability of research data - Need for metadata: Need for visualization tools to merge diverse data types from different sources; Training to communicate knowledge to end users & non-specialists (websites, DVDs, ICAO documents)

Second GALION Workshop September 2010, Geneva, Switzerland Lidar technologies  ceilometers  Backscatter lidar (1 wavelenght, multiwavelenght)  Raman lidar (1 wavelenght, multiwavelenght)  HSRL (1 wavelenght, multiwavelenght)  Doppler lidar  Lidar products from each technology - Direct measured geometrical and optical properties - Retrieved aerosol typing/classification, microphysical properties and mass conversion  Qualitative and quantitative data (i.e. calibrated / not calibrated data)  Sensitivity/Expected accuracy  Best location (respect to the volcano source)

Second GALION Workshop September 2010, Geneva, Switzerland Lidar products  Geometrical properties layer identification (top, bottom and center of mass)  Optical properties profiles Extensive optical parameters (backscatter, extinction) Intensive optical parameters (Lidar ratio, depol., color ratio, Ångström exponent)  Optical properties in the identified layer Integrated backscatter, AOD Mean intensive optical parameters (Lidar ratio, depol., color ratio, Ångström exponent)  Aerosol Typing classification  Mass concentration estimate  Microphysical properties retrieved  Quicklook (lev 0)

Second GALION Workshop September 2010, Geneva, Switzerland Hypothesis Ceilometers or simple backscatter lidar (one wavelenght) for qualitative high resolution backscatter, close to the source Simple backscatter lidar (+ depol) more operational distributed in a dense network (mid - far distance). Advanced lidar systems (single wavelength Raman lidar + depol) are needed for calibrated optical profiles. Most advanced multiwavelenght Raman lidar as core sites for calibration, aerosol typing and microphysical inversion. We have to better explore sinergies with ancillary instruments (sun- photometers, radar, in-situ, etc.)