Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece

<p>The evaluation of chemical transport models, CTMs, is essential for the assessment of their performance regarding the physical and chemical parameterizations used. While regional CTMs have been widely used and evaluated over Europe, their validation over Greece is limited. In this study, we...

Full description

Bibliographic Details
Main Authors: I. Skoulidou, M.-E. Koukouli, A. Manders, A. Segers, D. Karagkiozidis, M. Gratsea, D. Balis, A. Bais, E. Gerasopoulos, T. Stavrakou, J. van Geffen, H. Eskes, A. Richter
Format: Article
Language:English
Published: Copernicus Publications 2021-04-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/21/5269/2021/acp-21-5269-2021.pdf
_version_ 1830141184498991104
author I. Skoulidou
M.-E. Koukouli
A. Manders
A. Segers
D. Karagkiozidis
M. Gratsea
D. Balis
A. Bais
E. Gerasopoulos
T. Stavrakou
J. van Geffen
H. Eskes
A. Richter
author_facet I. Skoulidou
M.-E. Koukouli
A. Manders
A. Segers
D. Karagkiozidis
M. Gratsea
D. Balis
A. Bais
E. Gerasopoulos
T. Stavrakou
J. van Geffen
H. Eskes
A. Richter
author_sort I. Skoulidou
collection DOAJ
description <p>The evaluation of chemical transport models, CTMs, is essential for the assessment of their performance regarding the physical and chemical parameterizations used. While regional CTMs have been widely used and evaluated over Europe, their validation over Greece is limited. In this study, we investigate the performance of the Long Term Ozone Simulation European Operational Smog (LOTOS-EUROS) v2.2.001 regional chemical transport model in simulating nitrogen dioxide, NO<span class="inline-formula"><sub>2</sub></span>, over Greece from June to December 2018. In situ NO<span class="inline-formula"><sub>2</sub></span> measurements obtained from 14 stations of the National Air Pollution Monitoring Network are compared with surface simulations over the two major cities of Greece, Athens and Thessaloniki. Overall the LOTOS-EUROS NO<span class="inline-formula"><sub>2</sub></span> surface simulations compare very well to the in situ measurements showing a mild underestimation of the measurements with a mean relative bias of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mo>-</mo><mn mathvariant="normal">10</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="13608f3dc1bc69445c2e36410c40a5f7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-21-5269-2021-ie00001.svg" width="32pt" height="10pt" src="acp-21-5269-2021-ie00001.png"/></svg:svg></span></span> %, a high spatial correlation coefficient of 0.86 and an average temporal correlation of 0.52. The CTM underestimates the NO<span class="inline-formula"><sub>2</sub></span> surface concentrations during daytime by <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mo>-</mo><mn mathvariant="normal">50</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="14b9b639daf2a06845c53389ea229fd7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-21-5269-2021-ie00002.svg" width="32pt" height="10pt" src="acp-21-5269-2021-ie00002.png"/></svg:svg></span></span> <span class="inline-formula">±</span> 15 %, while it slightly overestimates during night-time <span class="inline-formula">∼</span> 10 <span class="inline-formula">±</span> 35 %. Furthermore, the LOTOS-EUROS tropospheric NO<span class="inline-formula"><sub>2</sub></span> columns are evaluated against ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) NO<span class="inline-formula"><sub>2</sub></span> measurements in Athens and Thessaloniki. We report that the CTM tropospheric NO<span class="inline-formula"><sub>2</sub></span> column simulations over both urban and rural locations represent the diurnal patterns and hourly levels for both summer and winter seasons satisfactorily. The relative biases range between <span class="inline-formula">∼</span> <span class="inline-formula">−</span>2 % and <span class="inline-formula">−</span>35 %, depending on season and relative NO<span class="inline-formula"><sub>2</sub></span> load observed. Finally, the CTM was assessed also against space-borne Sentinel-5 Precursor (S5P) carrying the Tropospheric Monitoring Instrument (TROPOMI) tropospheric NO<span class="inline-formula"><sub>2</sub></span> observations. We conclude that LOTOS-EUROS simulates extremely well the tropospheric NO<span class="inline-formula"><sub>2</sub></span> patterns over the region with very high spatial correlation of 0.82 on average, ranging between 0.66 and 0.95, with negative biases in the summer and positive in the winter. Updated emissions for the simulations and model improvements when extreme values of boundary layer height are encountered are further suggested.</p>
first_indexed 2024-12-17T09:15:59Z
format Article
id doaj.art-62e925d5c147484880c02babe273c572
institution Directory Open Access Journal
issn 1680-7316
1680-7324
language English
last_indexed 2024-12-17T09:15:59Z
publishDate 2021-04-01
publisher Copernicus Publications
record_format Article
series Atmospheric Chemistry and Physics
spelling doaj.art-62e925d5c147484880c02babe273c5722022-12-21T21:54:59ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242021-04-01215269528810.5194/acp-21-5269-2021Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over GreeceI. Skoulidou0M.-E. Koukouli1A. Manders2A. Segers3D. Karagkiozidis4M. Gratsea5D. Balis6A. Bais7E. Gerasopoulos8T. Stavrakou9J. van Geffen10H. Eskes11A. Richter12Laboratory of Atmospheric Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceLaboratory of Atmospheric Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceTNO, Climate, Air and Sustainability, Utrecht, the NetherlandsTNO, Climate, Air and Sustainability, Utrecht, the NetherlandsLaboratory of Atmospheric Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceInstitute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, GreeceLaboratory of Atmospheric Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceLaboratory of Atmospheric Physics, Aristotle University of Thessaloniki, Thessaloniki, GreeceInstitute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, GreeceRoyal Belgian Institute for Space Aeronomy, Brussels, BelgiumRoyal Netherlands Meteorological Institute (KNMI), De Bilt, the NetherlandsRoyal Netherlands Meteorological Institute (KNMI), De Bilt, the NetherlandsInstitute of Environmental Physics and Remote Sensing, University of Bremen, Bremen, Germany<p>The evaluation of chemical transport models, CTMs, is essential for the assessment of their performance regarding the physical and chemical parameterizations used. While regional CTMs have been widely used and evaluated over Europe, their validation over Greece is limited. In this study, we investigate the performance of the Long Term Ozone Simulation European Operational Smog (LOTOS-EUROS) v2.2.001 regional chemical transport model in simulating nitrogen dioxide, NO<span class="inline-formula"><sub>2</sub></span>, over Greece from June to December 2018. In situ NO<span class="inline-formula"><sub>2</sub></span> measurements obtained from 14 stations of the National Air Pollution Monitoring Network are compared with surface simulations over the two major cities of Greece, Athens and Thessaloniki. Overall the LOTOS-EUROS NO<span class="inline-formula"><sub>2</sub></span> surface simulations compare very well to the in situ measurements showing a mild underestimation of the measurements with a mean relative bias of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mo>-</mo><mn mathvariant="normal">10</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="13608f3dc1bc69445c2e36410c40a5f7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-21-5269-2021-ie00001.svg" width="32pt" height="10pt" src="acp-21-5269-2021-ie00001.png"/></svg:svg></span></span> %, a high spatial correlation coefficient of 0.86 and an average temporal correlation of 0.52. The CTM underestimates the NO<span class="inline-formula"><sub>2</sub></span> surface concentrations during daytime by <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mo>-</mo><mn mathvariant="normal">50</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="14b9b639daf2a06845c53389ea229fd7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-21-5269-2021-ie00002.svg" width="32pt" height="10pt" src="acp-21-5269-2021-ie00002.png"/></svg:svg></span></span> <span class="inline-formula">±</span> 15 %, while it slightly overestimates during night-time <span class="inline-formula">∼</span> 10 <span class="inline-formula">±</span> 35 %. Furthermore, the LOTOS-EUROS tropospheric NO<span class="inline-formula"><sub>2</sub></span> columns are evaluated against ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) NO<span class="inline-formula"><sub>2</sub></span> measurements in Athens and Thessaloniki. We report that the CTM tropospheric NO<span class="inline-formula"><sub>2</sub></span> column simulations over both urban and rural locations represent the diurnal patterns and hourly levels for both summer and winter seasons satisfactorily. The relative biases range between <span class="inline-formula">∼</span> <span class="inline-formula">−</span>2 % and <span class="inline-formula">−</span>35 %, depending on season and relative NO<span class="inline-formula"><sub>2</sub></span> load observed. Finally, the CTM was assessed also against space-borne Sentinel-5 Precursor (S5P) carrying the Tropospheric Monitoring Instrument (TROPOMI) tropospheric NO<span class="inline-formula"><sub>2</sub></span> observations. We conclude that LOTOS-EUROS simulates extremely well the tropospheric NO<span class="inline-formula"><sub>2</sub></span> patterns over the region with very high spatial correlation of 0.82 on average, ranging between 0.66 and 0.95, with negative biases in the summer and positive in the winter. Updated emissions for the simulations and model improvements when extreme values of boundary layer height are encountered are further suggested.</p>https://acp.copernicus.org/articles/21/5269/2021/acp-21-5269-2021.pdf
spellingShingle I. Skoulidou
M.-E. Koukouli
A. Manders
A. Segers
D. Karagkiozidis
M. Gratsea
D. Balis
A. Bais
E. Gerasopoulos
T. Stavrakou
J. van Geffen
H. Eskes
A. Richter
Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece
Atmospheric Chemistry and Physics
title Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece
title_full Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece
title_fullStr Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece
title_full_unstemmed Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece
title_short Evaluation of the LOTOS-EUROS NO<sub>2</sub> simulations using ground-based measurements and S5P/TROPOMI observations over Greece
title_sort evaluation of the lotos euros no sub 2 sub simulations using ground based measurements and s5p tropomi observations over greece
url https://acp.copernicus.org/articles/21/5269/2021/acp-21-5269-2021.pdf
work_keys_str_mv AT iskoulidou evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT mekoukouli evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT amanders evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT asegers evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT dkaragkiozidis evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT mgratsea evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT dbalis evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT abais evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT egerasopoulos evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT tstavrakou evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT jvangeffen evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT heskes evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece
AT arichter evaluationofthelotoseurosnosub2subsimulationsusinggroundbasedmeasurementsands5ptropomiobservationsovergreece