Overview HIBISCUS Small balloons and sondes : the local view Small balloons : several instruments on the same flight train –Lightweight (10 to 40 kg),

Slides:



Advertisements
Similar presentations
Weather Test Version M.
Advertisements

Earth’s Weather Patterns
Centro de Investigaciones en Láseres y Aplicaciones (LASER RESEARCH CENTER AND APPLICATIONS ) (CITEFA-CONICET) Buenos Aires - Argentina Collaboration between.
Holger Vömel NCAR Science Day 17 April 2015 Exploration of the tropical tropopause region during Strateole-2.
Chapter 5 Atmospheric Water and Weather
Vertical Air Motion. Air Parcels Ascend/Descend Adiabatically Expansional CoolingCompressional heating.
AOS 100: Weather and Climate Instructor: Nick Bassill Class TA: Courtney Obergfell.
Bore mission of 4 June. First event Homestead observations only leading Homestead at 6:45 Z.
Chapter 5 Atmospheric Water and Weather
NDAC H2O Workshop Bern 5-7 July 2006 Current activities and projects of water vapour measurements in the UTLS in France J. P. Pommereau CNRS Service d’Aeronomie,
Chapter 11: Winter Weather Heavy snowfall in St. Louis is typically associated with a developing low pressure system To examine snowfall within a developing.
Chapter 11: lightning. this girl is charged !! Source: Halliday, Resnick, and Walker, Fundamentals of Physics.
LIDAR network F.Fierli, C. Flamant, F. Cairo. Scientific Task for SOP ● provide the aerosol content before convection episodes to improve the estimate.
SCOUT-O3 BALLOON/SONDES CAMPAIGN NIAMEY 26 JULY- 26 AUGUST 2006 J. P. Pommereau, A. Garnier and SCOUT-O3 team Objectives: Convective transport across tropopause.
Influence of tropopause-level disturbances on convection Geraint Vaughan.
Things to look for on the weather maps Visible and IR satellite images (& radar too): Look at cloud movements and locations - do they correlate with what.
HIBISCUS General Objective
ENVISAT VALIDATION AT TROPICS J. P.POMMEREAU, A. GARNIER, F. GOUTAIL, F. BORCHI Service d ’Aéronomie CNRS, Verrières le Buisson, France A. HERTZOG and.
Dynamical perspective on the middle atmosphere research in Sweden , SRS-Meeting, Stockholm Heiner Körnich, MISU 1.
Cloud Resolving Model Studies of Tropical Deep Convection Observed During HIBISCUS By Daniel Grosvenor, Thomas W. Choularton, & Hugh Coe - The University.
MIR OZONE ISSUES Horizontal (STE) and vertical transport (long life time in UTLS) Photochemical production by precursors (biomass burning, lightning,..)
Vertical Structure of the Tropical Troposphere (including the TTL) Ian Folkins Department of Physics and Atmospheric Science Dalhousie University.
SAOZ NO x and Lightning J. P. Pommereau and F. Goutail Ground-based SAOZ in Bauru since 1995 Short duration small balloon flights MIR long duration flights.
Workshop Bauru STUDY OF THE IMPACT OF THE 8 FEB 2001 CONVECTIVE SYSTEM ON THE UTLS AIR COMPOSITION V. Marécal 1, E. D. Rivière 1, G. Held 2, S.
TLE Corte June 2008 BALLOON BORNE DC AND AC ELECTRIC MEASUREMENTS IN THE VICINTY OF TROPICAL CONVECTIVE CLOUDS. J.J. BERTHELIER 1, F. SIMOES 1, J.P. POMMEREAU.
Thunderstorms and Tornadoes Last Lecture: We looked at severe weather events in the lower latitudes Principal weather event is the formation and movement.
The troposphere, except in shallow, narrow, rare locations, is stable to dry processes. For the purpose of synoptic analysis, these areas can be ignored.
Julie Haggerty National Center for Atmospheric Research Friends and Partners of Aviation Weather October July 2014.
Meteorology of Winter Air Pollution In Fairbanks.
In Situ Measurements of Ozone during Hibiscus 2004 Contributions through provision of data and discussions: Niels Larsen (DMI ozonesondes) Gerhard Held,
Niamey 23 Aug 2006 Local storms Ex of successful flight (1) Ice geysers and water vapour enhancements in the TTL 1500 m3 plastic balloon, 9 kg payload.
A fine vertical wave structure & its relation with trace gas transport ATTREX/CONTRAST/CAST Science Team Meeting, Oct, 2014 Ji-Eun Kim University of Colorado,
MMS - Ozonesonde Wind and Temperature Comparison during CR-AVE T.P. Bui, J. Dean-Day, C. Chang, R. Castaneda NASA-Ames Research Center H. Voemel University.
Bauru November 2004 Modelling interpretation of in situ H2O, CH4 and CO2 measured by  SDLA balloon borne instrument (SF2 and SF4 flights). N. Huret(1),G.
Tropical Severe Local Storms Nicole Hartford. How do thunderstorms form?  Thunderstorms result from moist warm air that rises due to being less dense.
ESABC, Nov 2002 F. Goutail 1 ValBal AO 701 Small Balloons for Envisat Validation F. Goutail, A. Bazureau, J. P. Pommereau Service d ’Aéronomie, France.
A NASA / NSF / NRL airborne field campaign focusing on atmospheric composition, chemistry, and climate over Southeast Asia. Programmatic Context, Issues.
UP-Atmosphere Eric Angat Teacher. Altitude is also known as height, and it is often used to refer to the height above sea level.
Objective Evaluation of the Meso-NH Simulations during Hibiscus-Troccinox-Troccibras I.Forecasts for the TROCCINOX campaign II.Three case studies: 13 Feb,
1 UCAM halocarbon observations on SF balloons during HIBISCUS (2003/2004) A. D. Robinson (1), J. D. McIntyre (1), B. Gostlow (1), J. Levine (1), N. R.
Shi Kuang 1, Mike Newchurch 1,John Burris 2, Wesley Cantrell 1, Patrick Cullis 3, Ed Eloranta 4, Guanyu Huang 1, Bryan Johnson 3, Kevin Knupp 1, Lihua.
1 OWP5: SCOUT balloons (Stratosphere-Climate links with emphasis on the UTLS) Andrew Robinson Centre for Atmospheric Science, Cambridge University, Cambridge,
AOS 100: Weather and Climate Instructor: Nick Bassill Class TA: Courtney Obergfell.
A regional-model « climatology » of vertical mass and water-vapour transport for the Hibiscus-Troccinox-Troccibras campaign 2004 F. Gheusi, J.-P. Cammas,
Where can we profile through the TTL? Based on forecasts of ENSO and QBO phasing, we will likely encounter temperatures somewhere between 2009 and 2010.
Evaluation of model simulations with satellite observed NO 2 columns and surface observations & Some new results from OMI N. Blond, LISA/KNMI P. van Velthoven,
Contrasting potential vorticity structures in two summer extratropical cyclones Oscar Martínez-Alvarado NCAS-Atmospheric Physics Sue Gray John Methven.
Tropical Convection and UTLS Transport
. METEOROLOGICAL HAZARDS IN AVIATION Cpt. Ing. Naděžda Bartošová Ph.D.
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:
Page 1 SAOZ EUREKA Feb-Mar 05 Post campaign Meeting - Eureka 2005,- 30 May 2005 Outline Objectives Results Florence Goutail Service d’Aeronomie / CNRS,
Juliane Schwendike and Sarah Jones The Interaction between Convection and African Easterly Waves:
High resolution models: Tropical Convection and Transport through the Tropical Tropopause Layer Maria Russo, Scott Hosking, Peter Braesicke, John Pyle.
CO 2 Mixing/Advection by Fronts Aaron Wang Colorado State University.
Niels Larsen and Johannes K. Nielsen Danish Meteorological Institute Balloon-borne backscatter measurements of tropical cirrus from Bauru Microphysical.
North Atlantic Oscillation and its Influence on Ozone in London
CAST – sonde activities
Energy and Heat Transfer
Clare Lee & Anthony Baran
LATMOS-IPSL, CNRS/UVSQ
Summary Sondes RS 80 has dry bias. RS 92 virtually without bias
Huailin Chen, Bruce Gentry, Tulu Bacha, Belay Demoz, Demetrius Venable
Weather Maps & Weather Terms
Average Monthly Temperature and Rainfall
Breathtaking Cloud Tsunami Rolls Over Sydney
University of Colorado and NCAR START08/Pre HIPPO Workshop
Diurnal Variation of Nitrogen Dioxide
January West Coast Extratropical Cyclone
Today’s Warm-Up Tues 12/10 List and describe the five major types of air masses that affect weather in North America. Write at least 3-5 complete sentences.
Thule (Greenland) 76.5°N °W
Presentation transcript:

Overview HIBISCUS Small balloons and sondes : the local view Small balloons : several instruments on the same flight train –Lightweight (10 to 40 kg), low consuming, small size, robust instruments –Combination of meteorology, GPS location, clouds, tracers, chemistry, H2O, electric field 2 x 10ZL ( m3), 120 kg at hook, ascent/descent up to 30 km 4 x 3SF (3000 m3), 170 kg at hook, daytime ascent and natural night-time descent through the TTL (22km => 14km) 10 backscatter, 12 ozone and 2 UV radiation sondes SF2, Feb 13th 2004

ZL2 31 Jan 20: :30 Labs, SAOZ, SAOZ-BrO In SACZ Active Thunderstorm and heavy local rainfall 18:00 24:00

ZL1 5 Feb 20:00-22:24 Dirac, SAOZ, SAOZ-BrO 24:00 18:00 Active SACZ Some local Thunderstorms

SF2 13 Feb 20:16-00:30 Descartes SLS, µ Dirac, µLidar, SAW, SSS, µ SDLA 24:00 Just before Strong Cold front travelling NW towards Bauru 21:00

SF1 16 Feb 20:25-01:30 Descartes SLS, µ Dirac, UMIST, LABS, SAW, SSS, TDLAS, AIRS Flight behind SACZ moving fast to the NW 24:00 18:00 Falcon overpass

SF4 24 Feb 20:00-00:20 Dirac SLS, µ Lidar, SAW, SSS, µ SDLA, AIRS SACZ Strong Squall line coming from the NW Heavy rainfall in the evening 18:00 24:00 Carnaval

SF3 February 26, 20:00 02:04 Descartes SLS, µ Dirac, LABS, SAW, SSS, TDLAS Feb 26 18:00 Feb 27 00:00 LIS 22:00 Very active thunderstorms over Santa Catarina travelling fast NE, over Bauru at end of flight µ Dirac picture at Sunset

DMI backscatter/ozone sondes Feb10th to Feb 24th

Time evolution of Potential Vorticity during the campaign - MIMOSA contour advection Temperature deviation compared to averaged TroCCiBras sondes 30 Jan10 Feb24 Feb04 Mar

Small balloons and sondes : Combination of meteorology, GPS location, clouds, tracers, chemistry, H2O, electric field Flights in a variety of meteorological conditions : convection, horizontal transport, lightning,.. Flight reports available on the HIBISCUS WEB site Most of the data in the HIBISCUS/VINTERSOL data base (zardoz.nilu.no) Conclusion