Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic

In this study, more accurate information on the levels of aerosol optical depth (AOD) was calculated from the assimilation of the modeled AOD based on the optimal interpolation method. Additionally, more realistic levels of surface particulate matters over the Arctic were estimated using the assimil...

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Main Authors: Han, Kyung M., Jung, Chang H., Park, Rae-Seol, Park, Soon-Young, Lee, Sojin, Kulmala, Markku, Petäjä, Tuukka, Karasiński, Grzegorz, Sobolewski, Piotr, Yoon, Young Jun, Lee, Bang Young, Kim, Kiyeon, Kim, Hyun S.
Format: Other/Unknown Material
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
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Online Access:http://hdl.handle.net/10138/327162
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spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/327162 2023-05-15T14:25:39+02:00 Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic Han, Kyung M. Jung, Chang H. Park, Rae-Seol Park, Soon-Young Lee, Sojin Kulmala, Markku Petäjä, Tuukka Karasiński, Grzegorz Sobolewski, Piotr Yoon, Young Jun Lee, Bang Young Kim, Kiyeon Kim, Hyun S. 2021-02-23 http://hdl.handle.net/10138/327162 eng eng Multidisciplinary Digital Publishing Institute Han, K.M.; Jung, C.H.; Park, R.-S.; Park, S.-Y.; Lee, S.; Kulmala, M.; Petäjä, T.; Karasiński, G.; Sobolewski, P.; Yoon, Y.J.; Lee, B.Y.; Kim, K.; Kim, H.S. Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic. Appl. Sci. 2021, 11, 1959. http://hdl.handle.net/10138/327162 http://purl.org/eprint/entityType/JournalArticle http://purl.org/eprint/entityType/Expression 2021 ftunivhelsihelda 2022-11-02T23:58:18Z In this study, more accurate information on the levels of aerosol optical depth (AOD) was calculated from the assimilation of the modeled AOD based on the optimal interpolation method. Additionally, more realistic levels of surface particulate matters over the Arctic were estimated using the assimilated AOD based on the linear relationship between the particulate matters and AODs. In comparison to the MODIS observation, the assimilated AOD was much improved compared with the modeled AOD (e.g., increase in correlation coefficients from −0.15–0.26 to 0.17–0.76 over the Arctic). The newly inferred monthly averages of PM 10 and PM 2.5 for April–September 2008 were 2.18–3.70 μg m −3 and 0.85–1.68 μg m −3 over the Arctic, respectively. These corresponded to an increase of 140–180%, compared with the modeled PMs. In comparison to in-situ observation, the inferred PMs showed better performances than those from the simulations, particularly at Hyytiala station. Therefore, combining the model simulation and data assimilation provided more accurate concentrations of AOD, PM 10 , and PM 2.5 than those only calculated from the model simulations. Other/Unknown Material Arctic Arctic Helsingfors Universitet: HELDA – Helsingin yliopiston digitaalinen arkisto Arctic
institution Open Polar
collection Helsingfors Universitet: HELDA – Helsingin yliopiston digitaalinen arkisto
op_collection_id ftunivhelsihelda
language English
description In this study, more accurate information on the levels of aerosol optical depth (AOD) was calculated from the assimilation of the modeled AOD based on the optimal interpolation method. Additionally, more realistic levels of surface particulate matters over the Arctic were estimated using the assimilated AOD based on the linear relationship between the particulate matters and AODs. In comparison to the MODIS observation, the assimilated AOD was much improved compared with the modeled AOD (e.g., increase in correlation coefficients from −0.15–0.26 to 0.17–0.76 over the Arctic). The newly inferred monthly averages of PM 10 and PM 2.5 for April–September 2008 were 2.18–3.70 μg m −3 and 0.85–1.68 μg m −3 over the Arctic, respectively. These corresponded to an increase of 140–180%, compared with the modeled PMs. In comparison to in-situ observation, the inferred PMs showed better performances than those from the simulations, particularly at Hyytiala station. Therefore, combining the model simulation and data assimilation provided more accurate concentrations of AOD, PM 10 , and PM 2.5 than those only calculated from the model simulations.
format Other/Unknown Material
author Han, Kyung M.
Jung, Chang H.
Park, Rae-Seol
Park, Soon-Young
Lee, Sojin
Kulmala, Markku
Petäjä, Tuukka
Karasiński, Grzegorz
Sobolewski, Piotr
Yoon, Young Jun
Lee, Bang Young
Kim, Kiyeon
Kim, Hyun S.
spellingShingle Han, Kyung M.
Jung, Chang H.
Park, Rae-Seol
Park, Soon-Young
Lee, Sojin
Kulmala, Markku
Petäjä, Tuukka
Karasiński, Grzegorz
Sobolewski, Piotr
Yoon, Young Jun
Lee, Bang Young
Kim, Kiyeon
Kim, Hyun S.
Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic
author_facet Han, Kyung M.
Jung, Chang H.
Park, Rae-Seol
Park, Soon-Young
Lee, Sojin
Kulmala, Markku
Petäjä, Tuukka
Karasiński, Grzegorz
Sobolewski, Piotr
Yoon, Young Jun
Lee, Bang Young
Kim, Kiyeon
Kim, Hyun S.
author_sort Han, Kyung M.
title Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic
title_short Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic
title_full Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic
title_fullStr Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic
title_full_unstemmed Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic
title_sort data assimilation of aod and estimation of surface particulate matters over the arctic
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url http://hdl.handle.net/10138/327162
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
genre_facet Arctic
Arctic
op_relation Han, K.M.; Jung, C.H.; Park, R.-S.; Park, S.-Y.; Lee, S.; Kulmala, M.; Petäjä, T.; Karasiński, G.; Sobolewski, P.; Yoon, Y.J.; Lee, B.Y.; Kim, K.; Kim, H.S. Data Assimilation of AOD and Estimation of Surface Particulate Matters over the Arctic. Appl. Sci. 2021, 11, 1959.
http://hdl.handle.net/10138/327162
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