Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product

<p>The TROPOspheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5 Precursor (S5P) satellite was launched on 13 October 2017 to provide the atmospheric composition for atmosphere and climate research. The S5P is a Sun-synchronous polar-orbiting satellite providing global daily coverage...

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Main Authors: K. Lakkala, J. Kujanpää, C. Brogniez, N. Henriot, A. Arola, M. Aun, F. Auriol, A. F. Bais, G. Bernhard, V. De Bock, M. Catalfamo, C. Deroo, H. Diémoz, L. Egli, J.-B. Forestier, I. Fountoulakis, K. Garane, R. D. Garcia, J. Gröbner, S. Hassinen, A. Heikkilä, S. Henderson, G. Hülsen, B. Johnsen, N. Kalakoski, A. Karanikolas, T. Karppinen, K. Lamy, S. F. León-Luis, A. V. Lindfors, J.-M. Metzger, F. Minvielle, H. B. Muskatel, T. Portafaix, A. Redondas, R. Sanchez, A. M. Siani, T. Svendby, J. Tamminen
Format: Article
Language:English
Published: Copernicus Publications 2020-12-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/13/6999/2020/amt-13-6999-2020.pdf
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author K. Lakkala
K. Lakkala
J. Kujanpää
C. Brogniez
N. Henriot
A. Arola
M. Aun
M. Aun
F. Auriol
A. F. Bais
G. Bernhard
V. De Bock
M. Catalfamo
C. Deroo
H. Diémoz
H. Diémoz
L. Egli
J.-B. Forestier
I. Fountoulakis
K. Garane
R. D. Garcia
R. D. Garcia
J. Gröbner
S. Hassinen
A. Heikkilä
S. Henderson
G. Hülsen
B. Johnsen
N. Kalakoski
A. Karanikolas
T. Karppinen
K. Lamy
S. F. León-Luis
A. V. Lindfors
J.-M. Metzger
F. Minvielle
H. B. Muskatel
T. Portafaix
A. Redondas
R. Sanchez
A. M. Siani
T. Svendby
J. Tamminen
spellingShingle K. Lakkala
K. Lakkala
J. Kujanpää
C. Brogniez
N. Henriot
A. Arola
M. Aun
M. Aun
F. Auriol
A. F. Bais
G. Bernhard
V. De Bock
M. Catalfamo
C. Deroo
H. Diémoz
H. Diémoz
L. Egli
J.-B. Forestier
I. Fountoulakis
K. Garane
R. D. Garcia
R. D. Garcia
J. Gröbner
S. Hassinen
A. Heikkilä
S. Henderson
G. Hülsen
B. Johnsen
N. Kalakoski
A. Karanikolas
T. Karppinen
K. Lamy
S. F. León-Luis
A. V. Lindfors
J.-M. Metzger
F. Minvielle
H. B. Muskatel
T. Portafaix
A. Redondas
R. Sanchez
A. M. Siani
T. Svendby
J. Tamminen
Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product
Atmospheric Measurement Techniques
author_facet K. Lakkala
K. Lakkala
J. Kujanpää
C. Brogniez
N. Henriot
A. Arola
M. Aun
M. Aun
F. Auriol
A. F. Bais
G. Bernhard
V. De Bock
M. Catalfamo
C. Deroo
H. Diémoz
H. Diémoz
L. Egli
J.-B. Forestier
I. Fountoulakis
K. Garane
R. D. Garcia
R. D. Garcia
J. Gröbner
S. Hassinen
A. Heikkilä
S. Henderson
G. Hülsen
B. Johnsen
N. Kalakoski
A. Karanikolas
T. Karppinen
K. Lamy
S. F. León-Luis
A. V. Lindfors
J.-M. Metzger
F. Minvielle
H. B. Muskatel
T. Portafaix
A. Redondas
R. Sanchez
A. M. Siani
T. Svendby
J. Tamminen
author_sort K. Lakkala
title Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product
title_short Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product
title_full Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product
title_fullStr Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product
title_full_unstemmed Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation product
title_sort validation of the tropospheric monitoring instrument (tropomi) surface uv radiation product
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2020-12-01
description <p>The TROPOspheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5 Precursor (S5P) satellite was launched on 13 October 2017 to provide the atmospheric composition for atmosphere and climate research. The S5P is a Sun-synchronous polar-orbiting satellite providing global daily coverage. The TROPOMI swath is 2600 km wide, and the ground resolution for most data products is <span class="inline-formula">7.2×3.5</span> km<span class="inline-formula"><sup>2</sup></span> (<span class="inline-formula">5.6×3.5</span> km<span class="inline-formula"><sup>2</sup></span> since 6 August 2019) at nadir. The Finnish Meteorological Institute (FMI) is responsible for the development of the TROPOMI UV algorithm and the processing of the TROPOMI surface ultraviolet (UV) radiation product which includes 36 UV parameters in total. Ground-based data from 25 sites located in arctic, subarctic, temperate, equatorial and Antarctic areas were used for validation of the TROPOMI overpass irradiance at 305, 310, 324 and 380 nm, overpass erythemally weighted dose rate/UV index, and erythemally weighted daily dose for the period from 1 January 2018 to 31 August 2019. The validation results showed that for most sites 60 %–80 % of TROPOMI data was within <span class="inline-formula">±20</span> % of ground-based data for snow-free surface conditions. The median relative differences to ground-based measurements of TROPOMI snow-free surface daily doses were within <span class="inline-formula">±10</span> % and <span class="inline-formula">±5</span> % at two-thirds and at half of the sites, respectively. At several sites more than 90 % of cloud-free TROPOMI data was within <span class="inline-formula">±20</span> % of ground-based measurements. Generally median relative differences between TROPOMI data and ground-based measurements were a little biased towards negative values (i.e. satellite data <span class="inline-formula">&lt;</span> ground-based measurement), but at high latitudes where non-homogeneous topography and albedo or snow conditions occurred, the negative bias was exceptionally high: from <span class="inline-formula">−30</span> % to <span class="inline-formula">−65</span> %. Positive biases of 10 %–15 % were also found for mountainous sites due to challenging topography. The TROPOMI surface UV radiation product includes quality flags to detect increased uncertainties in the data due to heterogeneous surface albedo and rough terrain, which can be used to filter the data retrieved under challenging conditions.</p>
url https://amt.copernicus.org/articles/13/6999/2020/amt-13-6999-2020.pdf
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spelling doaj-12cba6b4e567461998a5ec1839a9cc5c2020-12-21T13:08:25ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482020-12-01136999702410.5194/amt-13-6999-2020Validation of the TROPOspheric Monitoring Instrument (TROPOMI) surface UV radiation productK. Lakkala0K. Lakkala1J. Kujanpää2C. Brogniez3N. Henriot4A. Arola5M. Aun6M. Aun7F. Auriol8A. F. Bais9G. Bernhard10V. De Bock11M. Catalfamo12C. Deroo13H. Diémoz14H. Diémoz15L. Egli16J.-B. Forestier17I. Fountoulakis18K. Garane19R. D. Garcia20R. D. Garcia21J. Gröbner22S. Hassinen23A. Heikkilä24S. Henderson25G. Hülsen26B. Johnsen27N. Kalakoski28A. Karanikolas29T. Karppinen30K. Lamy31S. F. León-Luis32A. V. Lindfors33J.-M. Metzger34F. Minvielle35H. B. Muskatel36T. Portafaix37A. Redondas38R. Sanchez39A. M. Siani40T. Svendby41J. Tamminen42Space and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, FinlandClimate Research Programme, Finnish Meteorological Institute, Helsinki, FinlandSpace and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, FinlandLaboratoire D'Optique Atmosphérique, Univ. Lille, CNRS,UMR 8518, Lille, FranceLaboratoire D'Optique Atmosphérique, Univ. Lille, CNRS,UMR 8518, Lille, FranceClimate Research Programme, Finnish Meteorological Institute, Helsinki, FinlandClimate Research Programme, Finnish Meteorological Institute, Helsinki, FinlandTartu Observatory, University of Tartu, Tõravere, EstoniaLaboratoire D'Optique Atmosphérique, Univ. Lille, CNRS,UMR 8518, Lille, FranceLaboratory of Atmospheric Physics, School of Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceBiospherical Instruments, Inc, San Diego, USRoyal Meteorological Institute of Belgium, Brussels, BelgiumLaboratoire D'Optique Atmosphérique, Univ. Lille, CNRS,UMR 8518, Lille, FranceLaboratoire D'Optique Atmosphérique, Univ. Lille, CNRS,UMR 8518, Lille, FranceAosta Valley Regional Environmental Protection Agency (ARPA), Saint-Christophe, ItalyInstitute of Atmospheric Science and Climate, ISAC-CNR, Rome, ItalyPhysical Meteorological Observatory in Davos – World Radiation Center, Davos Dorf, SwitzerlandLACy, Laboratoire de l'Atmosphère et des Cyclones (UMR 8105 CNRS, Université de La Réunion, Météo-France), Saint-Denis, Reunion Island, FranceAosta Valley Regional Environmental Protection Agency (ARPA), Saint-Christophe, ItalyLaboratory of Atmospheric Physics, School of Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceAtmospheric Optics Group, Valladolid University, Valladolid, SpainIzaña Atmospheric Research Center (IARC), State Meteorological Agency (AEMET), Santa Cruz de Tenerife, SpainPhysical Meteorological Observatory in Davos – World Radiation Center, Davos Dorf, SwitzerlandSpace and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, FinlandClimate Research Programme, Finnish Meteorological Institute, Helsinki, FinlandRadiation Health Services Branch, Australian Radiation Protection And Nuclear Safety Agency, Yallambie, AustraliaPhysical Meteorological Observatory in Davos – World Radiation Center, Davos Dorf, SwitzerlandNorwegian Radiation and Nuclear Safety Authority, NorwaySpace and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, FinlandLaboratory of Atmospheric Physics, School of Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceSpace and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, FinlandLACy, Laboratoire de l'Atmosphère et des Cyclones (UMR 8105 CNRS, Université de La Réunion, Météo-France), Saint-Denis, Reunion Island, FranceIzaña Atmospheric Research Center (IARC), State Meteorological Agency (AEMET), Santa Cruz de Tenerife, SpainMeteorological and Marine Research Programme, Finnish Meteorological Institute, Helsinki, FinlandObservatoire des Sciences de l'Univers de La Réunion, UMS3365 (CNRS, Université de La Réunion, Météo-France), Saint-Denis, Reunion Island, FranceLaboratoire D'Optique Atmosphérique, Univ. Lille, CNRS,UMR 8518, Lille, FranceIsrael Meteorological Service, Bet-Dagan, IsraelLACy, Laboratoire de l'Atmosphère et des Cyclones (UMR 8105 CNRS, Université de La Réunion, Météo-France), Saint-Denis, Reunion Island, FranceIzaña Atmospheric Research Center (IARC), State Meteorological Agency (AEMET), Santa Cruz de Tenerife, SpainNational Meteorological Service, Buenos Aires, ArgentinaPhysics Department, Sapienza Università di Roma, Rome, ItalyNILU – Norwegian Institute for Air Research, Kjeller, NorwaySpace and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, Finland<p>The TROPOspheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5 Precursor (S5P) satellite was launched on 13 October 2017 to provide the atmospheric composition for atmosphere and climate research. The S5P is a Sun-synchronous polar-orbiting satellite providing global daily coverage. The TROPOMI swath is 2600 km wide, and the ground resolution for most data products is <span class="inline-formula">7.2×3.5</span> km<span class="inline-formula"><sup>2</sup></span> (<span class="inline-formula">5.6×3.5</span> km<span class="inline-formula"><sup>2</sup></span> since 6 August 2019) at nadir. The Finnish Meteorological Institute (FMI) is responsible for the development of the TROPOMI UV algorithm and the processing of the TROPOMI surface ultraviolet (UV) radiation product which includes 36 UV parameters in total. Ground-based data from 25 sites located in arctic, subarctic, temperate, equatorial and Antarctic areas were used for validation of the TROPOMI overpass irradiance at 305, 310, 324 and 380 nm, overpass erythemally weighted dose rate/UV index, and erythemally weighted daily dose for the period from 1 January 2018 to 31 August 2019. The validation results showed that for most sites 60 %–80 % of TROPOMI data was within <span class="inline-formula">±20</span> % of ground-based data for snow-free surface conditions. The median relative differences to ground-based measurements of TROPOMI snow-free surface daily doses were within <span class="inline-formula">±10</span> % and <span class="inline-formula">±5</span> % at two-thirds and at half of the sites, respectively. At several sites more than 90 % of cloud-free TROPOMI data was within <span class="inline-formula">±20</span> % of ground-based measurements. Generally median relative differences between TROPOMI data and ground-based measurements were a little biased towards negative values (i.e. satellite data <span class="inline-formula">&lt;</span> ground-based measurement), but at high latitudes where non-homogeneous topography and albedo or snow conditions occurred, the negative bias was exceptionally high: from <span class="inline-formula">−30</span> % to <span class="inline-formula">−65</span> %. Positive biases of 10 %–15 % were also found for mountainous sites due to challenging topography. The TROPOMI surface UV radiation product includes quality flags to detect increased uncertainties in the data due to heterogeneous surface albedo and rough terrain, which can be used to filter the data retrieved under challenging conditions.</p>https://amt.copernicus.org/articles/13/6999/2020/amt-13-6999-2020.pdf