BROADBAND INSTRUMENTS ENEA/Univ. of Valencia TypeModelMeasurementSpectral interval FOVAcquisition PyranometerCMP21Global SW↓ irradiance 310-2800 nm180°30.

Slides:

Advertisements

Similar presentations

G. Pace 1, G.Cremona 4, A. di Sarra 1, D. Meloni 1, F. Monteleone 3, D. Sferlazzo 2, L. Vitali 4, G. Zanini 4 1 Italian National.

Advertisements

Proposed new uses for the Ceilometer Network

Consiglio Nazionale delle Ricerche 3 rd COPS and GOP workshop April 2006 Consiglio Nazionale delle Ricerche Istituto di Metodologie per lAnalisi.

Using a Radiative Transfer Model in Conjunction with UV-MFRSR Irradiance Data for Studying Aerosols in El Paso-Juarez Airshed by Richard Medina Calderón.

Radiative transfer simulations of the ATR-42 and Falcon 20 SW and LW radiation profiles above the ENEA Lampedusa supersite during the ChArMEx/ADRIMED SOP1a.

AMF2 Instruments and Measurements: AOS The following instruments are planned to be deployed aboard the R/V Ron Brown: Aerosol Observing System (AOS) consisting.

Overview of the Atmospheric Radiation Measurement (ARM) Program’s Mobile Facility (AMF) Dave Turner University of Wisconsin – Madison COPS Workshop

RADIATION PROGRAM AT TAMANRASSET ALGERIA RESULTS OF RADIATION MEASURE SINCE 1994 By.O.BOUZIANE.

Proposed participation of the MODIS Aerosol team and Si-Chee in the Dry/wet AMC + SMOCC campaign in Amazonia August-November 2002 (There are question marks.

May 10, 2004Aeronet workshop Can AERONET help with monitoring clouds? Alexander Marshak NASA/GSFC Thanks to: Y. Knyazikhin, K. Evans, W. Wiscombe, I. Slutsker.

Radiative Atmospheric Divergence using ARM Mobile Facility, GERB data and AMMA stations A proposal led by Tony Slingo to deploy the new ARM Mobile Facility.

Page 1© Crown copyright The Facility for Airborne Atmospheric Measurements (FAAM) BAe-146 Steve Abel First VOCALS Regional Experiment (REx) Preparatory.

General: Very likely both aircraft are to be based at Arica. The UK recce is early April, both Arica and Iquique will be visited. Total of 120 flight hours.

Aerosol Measurements in London using the OPAL Weather Station Network: Preliminary Results from the EM25 Campaign Claire McConnell Ralf Toumi (Imperial.

Radiative Properties of Clouds SOEE3410 Ken Carslaw Lecture 3 of a series of 5 on clouds and climate Properties and distribution of clouds Cloud microphysics.

Radiative Properties of Clouds SOEE3410 Ken Carslaw Lecture 3 of a series of 5 on clouds and climate Properties and distribution of clouds Cloud microphysics.

Radiative Properties of Clouds ENVI3410 : Lecture 9 Ken Carslaw Lecture 3 of a series of 5 on clouds and climate Properties and distribution of clouds.

TReSS (Transportable Remote Sensing Station) in Tamanrasset Overview of TReSS Status of implementation on April 1 st 2006 Operations in the framework of.

Overview The path to Skywatch Video tour of the facility Brief rooftop instrument overview Description of real-time and.

Balloon-Borne Sounding System (BBSS) Used for atmospheric profiling Measures P, T, RH, wind speed and direction Uncertainties arise from incorrect surface.

An Introduction to Using Angular Information in Aerosol Remote Sensing Richard Kleidman SSAI/NASA Goddard Lorraine Remer UMBC / JCET Robert C. Levy NASA.

Liam Tallis. Introduction Know the vertical distribution of water vapour in the atmosphere Profile for input into radiative transfer schemes Need to know.

Radiation: WHY CARE ??? the ultimate energy source, driver for the general circulation usefully applied in remote sensing (more and more)

Accent Plus Symposium, Urbino, Italy, Sep2013 Observations of Enhanced Black Carbon radiative forcing over an Urban Environment A.S.Panicker, G.

MAGIC hyperspectral observations for studying cloud properties A.Marshak (NASA GSFC), P. McBride (GESTAR/ASTRA), C. Chiu (University of Reading) W. Wiscombe.

Direct LW radiative effect of Saharan dust aerosols Vincent Gimbert, H.E. Brindley, J.E. Harries Imperial College London GIST 24, 16 Dec 2005, Imperial.

Applications and Limitations of Satellite Data Professor Ming-Dah Chou January 3, 2005 Department of Atmospheric Sciences National Taiwan University.

Solar Energy Part 1: Resource San Jose State University FX Rongère January 2009.

Page 1© Crown copyright 2004 Cirrus Measurements during the EAQUATE Campaign C. Lee, A.J. Baran, P.N. Francis, M.D. Glew, S.M. Newman and J.P. Taylor.

What are the four principal windows (by wavelength interval) open to effective remote sensing from above the atmosphere ? 1) Visible-Near IR ( );

Infrared Interferometers and Microwave Radiometers Dr. David D. Turner Space Science and Engineering Center University of Wisconsin - Madison

Sponsors: National Aeronautics and Space Administration (NASA) NASA Goddard Space Flight Center (GSFC) NASA Goddard Institute for Space Studies (GISS)

Introduction Invisible clouds in this study mean super-thin clouds which cannot be detected by MODIS but are classified as clouds by CALIPSO. These sub-visual.

Aerosol Optical Depth measurements in the Azores Fernanda Carvalho 1 Diamantino Henriques 1 Paulo Fialho 2 Vera Bettencourt 1 1 Instituto de Meteorologia.

ARM Data Overview Chuck Long Jim Mather Tom Ackerman.

Overview of Climate V. Ramaswamy (“Ram”) U.S. National Oceanic and Atmospheric Administration Geophysical Fluid Dynamics Laboratory Princeton University.

Monday, Oct. 2: Clear-sky radiation; solar attenuation, Thermal nomenclature.

1 Clear-Sky irradiance observations and models to analyze aerosol characteristic over Semi-arid Reno, NV. By: Addison Liming Jayne Boehmler Marcela Loria-Salazar.

Optical properties Satellite observation ? T,H 2 O… From dust microphysical properties to dust hyperspectral infrared remote sensing Clémence Pierangelo.

Measuring UV aerosol absorption. Why is aerosol UV absorption important ? Change in boundary layer ozone mixing ratios as a result of direct aerosol forcing.

1 NOAA-UPRM COOP Program in Atmospheric Sciences and Meteorology, Department of Physics, University of Puerto Rico at Mayagüez, Mayagüez, PR Yaítza.

Radiative Atmospheric Divergence using ARM Mobile Facility, GERB data and AMMA stations –led by Tony Slingo, ESSC, Reading University, UK Links the ARM.

1 Ground-based Remote Sensing of Aerosols Pawan K Bhartia Laboratory for Atmospheres NASA Goddard Space Flight Center Maryland, USA.

Air – Sea Measurements from Ships: Fluxes, Time Series, Remote Sensing Dr. Jeff Hare CIRES – University of Colorado and NOAA Earth Systems Research Lab.

1 « TReSS » ATMOSPHERIC OPTICAL REMOTE SENSING TRANSPORTABLE-MOBILE PLATFORM Pierre H. Flamant, Claude Loth Juan Cuesta, Dimitri Edouard, Florian Lapouge*

Ground-based infrared retrievals of atmospheric dust properties over Niamey, Niger A case study: dust storm event (7-10 March 2006)* ATMS 790 R- Graduate.

Chapter 3 Atmospheric Radiative Transfer and Climate To date, we have learned 1)The greenhouse effects, through understanding the simplest greenhouse model,

Implementation of Male’ Declaration on Control and Prevention of Air Pollution and its Likely Transboundary Effects for South Asia MALDIVES 12 – 13 September.

METEOROLOGICAL DATA COLLECTION NETWORK OF IMD. Meteorological instrument Observer Meteorological Observation (In situ & Remote sensing)

Vertically resolved aerosol optical properties over the ARM SGP site B. Schmid, H. Jonsson, A. Strawa, B. Provencal, K. Ricci, D. Covert, R. Elleman, W.

A new method for first-principles calibration

Proposed Instrument for Deployment at Climate Reference Network (CRN) Sites: Multi-Filter Rotating Shadowband Radiometer (MFRSR) The MFRSR measures solar.

Airborne Sunphotometry and Closure Studies during the SAFARI-2000 Dry Season Campaign B. Schmid BAER/NASA Ames Research Center, Moffett Field, CA, USA.

Airborne Sunphotometry and Closure Studies in the SAFARI-2000 Dry Season Campaign B. Schmid 1, P.B. Russell 2, P.Pilewskie 2, J. Redemann 1, P.V. Hobbs.

Radiative transfer simulations of the ATR-42 SW and LW irradiance profiles above Lampedusa Island Daniela Meloni with contributions from: ChArMEx/ADRIMED.

Cloudnet meeting Oct Martial Haeffelin SIRTA Cloud and Radiation Observatory M. Haeffelin, A. Armstrong, L. Barthès, O. Bock, C. Boitel, D.

The Use of Spectral and Angular Information In Remote Sensing

Lampedusa P.I & Institution: Alcide di Sarra, ENEA Data Manager: TBD Carlo Bommarito, Francesco Monteleone, Giandomenico Pace, Damiano Sferlazzo, Daniela.

Radiative Transfer Modeling: Deriving Forcing on Climate in Support of GMI Don Wuebbles Department of Atmospheric Sciences University of Illinois, Urbana,

The study of cloud and aerosol properties during CalNex using newly developed spectral methods Patrick J. McBride, Samuel LeBlanc, K. Sebastian Schmidt,

Consulting and Technology Technical Excellence | Pragmatic Solutions | Proven Delivery Calibration Test Sites Selection and Characterisation WP 240 Equipment.

Solar radiation measurement networks in Taiwan -With contributions from- Central Weather Bureau CWB) Environmental Protection Administration (EPA) Sheng-Hsiang.

Extinction measurements

DETERMINATION OF PHOTOSYNTHETICALLY ACTIVE RADIATION

Ground-based Remote Sensing an overview of sensors and applications

Site Instrumental de Recherche par Télédétection Atmosphérique

CH 3: The Electromagnetic Spectrum

Diurnal Variation of Nitrogen Dioxide

716 Investigating the Role of Aerosols and Clouds on the Radiation Budget in Niamey, Niger Allison Marquardt Collow and Mark Miller Department of Environmental.

Thule (Greenland) 76.5°N °W

Presentation transcript:

BROADBAND INSTRUMENTS ENEA/Univ. of Valencia TypeModelMeasurementSpectral interval FOVAcquisition PyranometerCMP21Global SW↓ irradiance nm180°30 s PyranometerPSPDiffuse SW↓ irradiance nm180°30 s PyrheliometerCHP1Direct SW radiance nm5°30 s PyrgeometerCGR4LW↓ irradiance µm180°30 s Pyrgeometer (Univ. of Valencia) CGR4LW↓ irradiance µm180°30 s PyrometerKT 19 IISky Brightness Temperature µm2.6°2 s

BROADBAND INSTRUMENTS: ENEA/Univ. of Valencia/PMOD TypeModelMeasurementSpectral interval FOVAcquisition PyranometerCMP21Global SW↓ irradiance nm180°30 s PyranometerPSPDiffuse SW↓ irradiance nm180°30 s PyrheliometerCHP1Direct SW radiance nm5°30 s PyrgeometerCGR4LW↓ irradiance µm180°30 s PyrgeometerPIRLW↑ irradiance µm180°1 min PyrometerKT 19 IISky Brightness Temperature µm2.6°2 s PyranometerCM22Reflected SW↑ irradiance nm180°1 min PyrgeometerCGR3LW↓ irradiance8-14 µm150°1 min

Comparison of ENEA and PMOD/WRC broadband radiometers Average SW ratio = 1.010±0.003 (SZA<45°) Average LW differences: -0.1±1.6 Wm -2 (DAY) 1.4±1.2 Wm -2 (NIGHT)

SPECTRAL INSTRUMENTS ENEA TypeModelMeasurementSpectral interval FWHMAcquisition BrewerMK IIIGlobal irradiance nm0.55 nmFixed SZA Satlantic Hyperspectral Ocean Colour Radiometer HyperOCRGlobal downward spectral irradiance nm ( nm) 10 nm1 min Satlantic Hyperspectral Ocean Colour Radiometer HyperOCRDiffuse downward spectral irradiance nm ( nm) 10 nm1 min Diode array spectrometer DASGlobal downward spectral actinic flux nm3.3 nm1 s Microwave radiometer HATPROBrightness temperature K-Band (WV) V-Band (O 2 ) 230 MHz (K) MHz (V) 1 s

SPECTRAL INSTRUMENTS TypeModelMeasurementSpectral interval FWHMAcquisition MultiFilter Rotating Shadowband Radiometer MFR-7Global and diffuse irradiance 415, 496, 614, 672, 869, 937 nm 10 nm15 S MultiFilter Rotating Shadowband Radiometer UV-MFRGlobal and diffuse irradiance 299, 305, 311, 317, 324, 332, 367 nm 2 nm20 s Cimel sunphotometer CE-318Direct sun, almucantar, principle plane 340, 380, 440, 500, 675, 870, 1020 nm 2-10 nm~15 min Filter radiometerSP02Direct narrowband irradiance (FOV=5°) 412, 500, 862, 1020 nm 10 nm30 s Filter radiometerSP02-LDirect narrowband irradiance (FOV=2.5°) 412, 500, 812, 862 nm 10 nm30 s Solar Light sunphotometer (Univ. of Valencia) MICROTOPS II Direct narrowband irradiance (FOV=2.5°) 305, 312, 320, 940, 1020 nm 2 nm 10 nm ~15 min Precision spectroradiometer PSRDirect spectral irradiance nm1 nm1 min

J.L. Gómez-Amo UTMEA-TER, 24 July June

Direct SW radiative effect RF=F net (aerosol)-F net (pristine) Forcing efficiency FE=RF/AOD

J.L. Gómez-Amo UTMEA-TER, 24 July 2013

22 June – F36

J.L. Gómez-Amo UTMEA-TER, 24 July June

J.L. Gómez-Amo UTMEA-TER, 24 July 2013 Calculations with MODTRAN 4.3 Aerosol-free Sensitivities in the conditions of Lampedusa: 4 W/m 2 /°C for changes of T 23 W/m 2 /cm for changes of IWV

J.L. Gómez-Amo UTMEA-TER, 24 July June

9 June

230 km 37.6°N, 12.6°E 35.5°N, 12.6°E

Capo Granitola

TypeModelMeasurementSpectral interval FOVAcquisition PyranometerPSPGlobal SW↓ irradiance nm180°30 s PyranometerPSPDiffuse SW↓ irradiance nm180°30 s PyrgeometerPIRLW↓ irradiance µm180°30 s Spectrometer (Univ. of Valencia) Li-1800SW↓ irradiance µm180°5 min MultiFilter Rotating Shadowband Radiometer MFR-7Global and diffuse irradiance 415, 496, 614, 672, 869, 937 nm 10 nm15 S Spectrometer (Univ. of Valencia) Li-1800Direct normal SW radiation µm5°5 min PM10 sampler (Univ. of Florence) Tecora Skypost PM10 on teflon filters 12 hour

▼▼ 15 June30 June

▼▼ 15 June30 June

Satlantic spectroradiometers measurements 17 June: cloud-free day with low aerosol amount

SW irradiance 22 June28 June 2 July3 July

LW irradiance 22 June28 June 2 July 3 July

3 July – F42

22 June – F36 SZA interval: 25.3°-28.6° Average AOD (500 nm): SW ADRF (Wm -2 ) SW ADRFE (Wm -2 ) LW ADRF (Wm -2 ) LW ADRFE (Wm -2 ) WINDOW ADRF (Wm -2 ) WINDOW ADRFE (Wm -2 ) LW/SW (percent) % SPECTRAL RANGE MEASUREMENTS (Wm -2 ) MODEL (Wm -2 ) DIFFERENCE (Wm -2 ) LW359.9± WINDOW81.6±

3 July – F42 SZA interval: 20.3°-22.0° Average AOD (500 nm): SW ADRF (Wm -2 ) SW ADRFE (Wm -2 ) LW ADRF (Wm -2 ) LW ADRFE (Wm -2 ) WINDOW ADRF (Wm -2 ) WINDOW ADRFE (Wm -2 ) LW/SW (percent) % SPECTRAL RANGE MEASUREMENTS (Wm -2 ) MODEL (Wm -2 ) DIFFERENCE (Wm -2 ) LW363.1± WINDOW87.1±

9 June MODIS Aqua – 12:35 UTC

J.L. Gómez-Amo UTMEA-TER, 24 July 2013 HYSPLIT back-trajectories

With University of Valencia

During the flights

22 JUNE, FLIGHT 1

22 JUNE, FLIGHT 2

22 June, FLIGHT 2

28 JUNE, FLIGHT 1

28 JUNE, FLIGHT 2

2 JULY

3 JULY

Radiosondaggi Voli ATR42+Falcon

J.L. Gómez-Amo UTMEA-TER, 24 July 2013 Lampedusa Capo Granitola MODIS Aqua – 22 June :35 UTC

During the flights

Meteorological station [air pressure, temperature, humidity, wind direction and velocity, precipitation]. Vaisala radio [temperature, pressure, humidity, wind, ozone vertical profiles]. Hat-Pro Microwave Radiometer [temperature and water vapor vertical profiles, integrated water vapour, liquid water content]. (Tri-axial SODAR [wind vertical profile; RSE]) Non-dispersive Infra-red (NDIR) analyzer [atmospheric CO 2 concentration]. Gas chromatograph [atmospheric concentration of CH 4, N 2 O, CFC-11 and CFC-12]. Cavity ring-down spectroscopy analyzer (CO 2, CO, CH 4 ). Ozone UV analyzer [ozone concentration; Agrigento Province]. Aerosol lidar [together with University of Rome; aerosol backscattering and depolarization profiles]. Visible Multi Filter Rotating Shadowband Radiometer [MFRSR; aerosol optical depth at several wavelengths, diffuse-to-direct irradiance ratio, column water vapor, aerosol single scattering albedo]. PM-10 aerosol sampler [daily chemical analyses performed at the University of Florence]. Cimel sun photometer [aerosol optical depth and optical properties]. Particle-Soot Absorption Probe [PSAP, aerosol absorption coefficient/soot concentration; ISPL]. Aerosol total deposition [CARAGA collector; LISA]. Middleton sun photometers [aerosol optical depth]

Brewer MK III spectrophotometer [total ozone, spectral UV, aerosol optical depth]. Precision Spectral Pyranometer/CMP21 [downward shortwave irradiance]. Precision Infrared Pyranometer/CGR4 [downward longwave irradiance]. Shaded Precision Spectral Pyranometer [diffuse downward shortwave irradiance]. Photosynthetic radiation radiometer [downward photosynthetically active radiation]. Actinic radiation spectrometer [actinic radiation spectra, photo dissociation rates]. UV-Multi Filter Rotating Shadowband Radiometer [MFRSR; aerosol optical depth at several wavelengths, diffuse-to-direct irradiance ratio, UV irradiance]. Total sky imager [cloud cover]. IR camera [cloud base height]. Water vapor Raman lidar [day/nighttime vertical profiles of water vapor, aerosol extinction (jointly with University of Rome)]. ENEA gas sampling unit [weekly analyses of 15 different halogen compounds, made at ENEA, Rome]. NOAA gas sampling unit [weekly analyses of CO 2, CH 4, SF 6, CO, 13 C, H 2, 18 O, made at NOAA]. WMO Global Atmosphere Watch NOAA Cooperative Air Sampling Network AERONET MWRNet Carboeurope

▼ ▼▼ 9 June15 June30 June