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Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula

Concentrations of fine particulate matter smaller than 2.5 μm in diameter (PM(2.5)) over the Korean Peninsula experience year-to-year variations due to interannual variation in climate conditions. This study develops a multiple linear regression model based on slowly varying boundary conditions to p...

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Autores principales: Jeong, Dajeong, Yoo, Changhyun, Yeh, Sang-Wook, Yoon, Jin-Ho, Lee, Daegyun, Lee, Jae-Bum, Choi, Jin-Young
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Korean Meteorological Society 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8960088/
https://www.ncbi.nlm.nih.gov/pubmed/35371395
http://dx.doi.org/10.1007/s13143-022-00275-4
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author Jeong, Dajeong
Yoo, Changhyun
Yeh, Sang-Wook
Yoon, Jin-Ho
Lee, Daegyun
Lee, Jae-Bum
Choi, Jin-Young
author_facet Jeong, Dajeong
Yoo, Changhyun
Yeh, Sang-Wook
Yoon, Jin-Ho
Lee, Daegyun
Lee, Jae-Bum
Choi, Jin-Young
author_sort Jeong, Dajeong
collection PubMed
description Concentrations of fine particulate matter smaller than 2.5 μm in diameter (PM(2.5)) over the Korean Peninsula experience year-to-year variations due to interannual variation in climate conditions. This study develops a multiple linear regression model based on slowly varying boundary conditions to predict winter and spring PM(2.5) concentrations at 1–3-month lead times. Nation-wide observations of Korea, which began in 2015, is extended back to 2005 using the local Seoul government’s observations, constructing a long-term dataset covering the 2005–2019 period. Using the forward selection stepwise regression approach, we identify sea surface temperature (SST), soil moisture, and 2-m air temperature as predictors for the model, while rejecting sea ice concentration and snow depth due to weak correlations with seasonal PM(2.5) concentrations. For the wintertime (December–January–February, DJF), the model based on SSTs over the equatorial Atlantic and soil moisture over the eastern Europe along with the linear PM(2.5) concentration trend generates a 3-month forecasts that shows a 0.69 correlation with observations. For the springtime (March–April–May, MAM), the accuracy of the model using SSTs over North Pacific and 2-m air temperature over East Asia increases to 0.75. Additionally, we find a linear relationship between the seasonal mean PM(2.5) concentration and an extreme metric, i.e., seasonal number of high PM(2.5) concentration days. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s13143-022-00275-4.
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spelling pubmed-89600882022-03-29 Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula Jeong, Dajeong Yoo, Changhyun Yeh, Sang-Wook Yoon, Jin-Ho Lee, Daegyun Lee, Jae-Bum Choi, Jin-Young Asia Pac J Atmos Sci Original Article Concentrations of fine particulate matter smaller than 2.5 μm in diameter (PM(2.5)) over the Korean Peninsula experience year-to-year variations due to interannual variation in climate conditions. This study develops a multiple linear regression model based on slowly varying boundary conditions to predict winter and spring PM(2.5) concentrations at 1–3-month lead times. Nation-wide observations of Korea, which began in 2015, is extended back to 2005 using the local Seoul government’s observations, constructing a long-term dataset covering the 2005–2019 period. Using the forward selection stepwise regression approach, we identify sea surface temperature (SST), soil moisture, and 2-m air temperature as predictors for the model, while rejecting sea ice concentration and snow depth due to weak correlations with seasonal PM(2.5) concentrations. For the wintertime (December–January–February, DJF), the model based on SSTs over the equatorial Atlantic and soil moisture over the eastern Europe along with the linear PM(2.5) concentration trend generates a 3-month forecasts that shows a 0.69 correlation with observations. For the springtime (March–April–May, MAM), the accuracy of the model using SSTs over North Pacific and 2-m air temperature over East Asia increases to 0.75. Additionally, we find a linear relationship between the seasonal mean PM(2.5) concentration and an extreme metric, i.e., seasonal number of high PM(2.5) concentration days. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s13143-022-00275-4. Korean Meteorological Society 2022-03-28 2022 /pmc/articles/PMC8960088/ /pubmed/35371395 http://dx.doi.org/10.1007/s13143-022-00275-4 Text en © The Author(s) under exclusive licence to Korean Meteorological Society and Springer Nature B.V. 2022 This article is made available via the PMC Open Access Subset for unrestricted research re-use and secondary analysis in any form or by any means with acknowledgement of the original source. These permissions are granted for the duration of the World Health Organization (WHO) declaration of COVID-19 as a global pandemic.
spellingShingle Original Article
Jeong, Dajeong
Yoo, Changhyun
Yeh, Sang-Wook
Yoon, Jin-Ho
Lee, Daegyun
Lee, Jae-Bum
Choi, Jin-Young
Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula
title Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula
title_full Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula
title_fullStr Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula
title_full_unstemmed Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula
title_short Statistical Seasonal Forecasting of Winter and Spring PM(2.5) Concentrations Over the Korean Peninsula
title_sort statistical seasonal forecasting of winter and spring pm(2.5) concentrations over the korean peninsula
topic Original Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8960088/
https://www.ncbi.nlm.nih.gov/pubmed/35371395
http://dx.doi.org/10.1007/s13143-022-00275-4
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