Seung Jin Joo

Dr. Seung Jin Joo

orcid

Research Focus & Metrics

Academic Career Length

25Years (2002-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 October 2002 in Forest Ecology and Management
Verified
Journal Article
Closed access
MYMyeong Hui Yim
Myeong Hui Yim
SJSeung Jin Joo
Seung Jin Joo
KNKaneyuki Nakane
Kaneyuki Nakane

1 March 2003 in Forest Ecology and Management
Verified
Journal Article
Closed access
MYMyeong Hui Yim
Myeong Hui Yim
SJSeung Jin Joo
Seung Jin Joo
KSKatsuyuki Shutou
Katsuyuki Shutou
KNKaneyuki Nakane
Kaneyuki Nakane

1 October 2006 in Forest Ecology and Management
Verified
Journal Article
Closed access
SJSeung Jin Joo
Seung Jin Joo
MYMyeong Hui Yim
Myeong Hui Yim
KNKaneyuki Nakane
Kaneyuki Nakane

1 February 2012 in Science of The Total Environment
Verified
Journal Article
Closed access
SJSeung Jin Joo
Seung Jin Joo
SPSoon-Ung Park
Soon-Ung Park
MPMoon-Soo Park
Moon-Soo Park
CLChang Seok Lee
Chang Seok Lee

1 March 2011 in Journal of Ecology and Field Biology
Verified
Journal Article
Closed access
SJSeung Jin Joo
Seung Jin Joo
MPMoon-Soo Park
Moon-Soo Park
GKGyung-Soon Kim
Gyung-Soon Kim
CLChang Suk Lee
Chang Suk Lee

10 September 2021 in Journal of Geophysical Research: Atmospheres
Verified
Journal Article
Open access
PDF file
KKKyoung‐Min Kim
Kyoung‐Min Kim
SKSi‐Wan Kim
Si‐Wan Kim
MCMyungje Choi
Myungje Choi
MKMijin Kim
Mijin Kim
Jhoon KimJhoon Kim
Jhoon Kim
LZLi Zhang
Li Zhang
Asian mineral dust substantially influences air quality as well as weather and climate. It is important to forecast dust storms as a part of air quality modeling to protect public health and minimize the disruption to essential daily routines. In this study, we simulated the dust episodes during the DRAGON‐NE Asia field campaign in April 2012 utilizing the Weather Research and Forecasting model coupled with chemistry (WRF‐Chem) with 5 dust emission options and evaluated the model results with the measurements from multiple instruments including Korean geostationary satellites Geostationary Ocean Color Imager (GOCI) and Meteorological Imager (MI). The model well predicted the dust occurrences, transport, and vertically elevated structure, compared to the satellite aerosol optical depths (AOD), the Aerosol Robotic Network (AERONET) AOD and size distribution parameter Angstrom Exponent (AE), the ground‐based lidar and in‐situ observations. However, the model dust concentration varied depending on the selected dust emission option. The model also did not accurately simulate both AOD and AE. When the model AOD agreed with the AERONET AOD, AE did not agree. In general, the model concentrations were overestimated for large size particles (diameter 6–20 μm) and were underestimated for small size particles (0.5–3.6 μm), compared to the observed aerosol size distributions at surface in Korean Peninsula. Our analysis of the episode suggests that the dust is possibly mixed with the aerosols of anthropogenic origins in the Asian region. Therefore, accurate simulations of both anthropogenic aerosols and dust are helpful for evaluating models in the downwind region of the dust sources.