Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert
Semiarid to arid regions located in north of China are known as one of the largest sources of dust aerosols in the globe. Previous studies demonstrated direct and indirect effects of atmospheric dust loading on climate. The surface and meteorological properties are known to be affecting dust entrain...
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IOP Publishing
2024-01-01
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Series: | Environmental Research Communications |
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Online Access: | https://doi.org/10.1088/2515-7620/ad19f3 |
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author | Yeonsu Park Si-Wan Kim Young-Min Yang Kyoung-Min Kim Mi-Kyung Sung Soon-Il An |
author_facet | Yeonsu Park Si-Wan Kim Young-Min Yang Kyoung-Min Kim Mi-Kyung Sung Soon-Il An |
author_sort | Yeonsu Park |
collection | DOAJ |
description | Semiarid to arid regions located in north of China are known as one of the largest sources of dust aerosols in the globe. Previous studies demonstrated direct and indirect effects of atmospheric dust loading on climate. The surface and meteorological properties are known to be affecting dust entrainment process. In this study, we found decadal variations of dust occurrence in Gobi Desert with the period of ∼24 years, utilizing the data acquired at the surface meteorological stations. An analysis of reanalysis datasets shows significant correlations between February North Atlantic Sea Surface Temperature (NASST) and precipitation in Gobi Desert and Mongolia in the following summer, causing a decadal variation of dust event frequency in the subsequent spring over the region. Strong time-lagged correlation is shown to be linked to an atmospheric wave train pattern that initiated from the NASST region, affecting large-scale circulation, ultimately causing surface drought over Gobi Desert. |
first_indexed | 2024-03-07T22:10:11Z |
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id | doaj.art-6e0d08eb86494b9b99b41ccbaa5dbffa |
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issn | 2515-7620 |
language | English |
last_indexed | 2024-03-07T22:10:11Z |
publishDate | 2024-01-01 |
publisher | IOP Publishing |
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series | Environmental Research Communications |
spelling | doaj.art-6e0d08eb86494b9b99b41ccbaa5dbffa2024-02-23T15:41:38ZengIOP PublishingEnvironmental Research Communications2515-76202024-01-016101100310.1088/2515-7620/ad19f3Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi DesertYeonsu Park0https://orcid.org/0009-0005-1200-2470Si-Wan Kim1https://orcid.org/0000-0002-7889-189XYoung-Min Yang2https://orcid.org/0000-0002-3048-6430Kyoung-Min Kim3Mi-Kyung Sung4https://orcid.org/0000-0002-7659-6571Soon-Il An5https://orcid.org/0000-0002-0003-429XIrreversible Climate Change Research Center, Yonsei University , Seoul, Republic of Korea; Department of Atmospheric Sciences, Yonsei University , Seoul, Republic of KoreaIrreversible Climate Change Research Center, Yonsei University , Seoul, Republic of KoreaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology , Nanjing, People’s Republic of ChinaDepartment of Atmospheric Sciences, Yonsei University , Seoul, Republic of KoreaKorea Institute of Science and Technology , Seoul, Republic of KoreaIrreversible Climate Change Research Center, Yonsei University , Seoul, Republic of Korea; Department of Atmospheric Sciences, Yonsei University , Seoul, Republic of KoreaSemiarid to arid regions located in north of China are known as one of the largest sources of dust aerosols in the globe. Previous studies demonstrated direct and indirect effects of atmospheric dust loading on climate. The surface and meteorological properties are known to be affecting dust entrainment process. In this study, we found decadal variations of dust occurrence in Gobi Desert with the period of ∼24 years, utilizing the data acquired at the surface meteorological stations. An analysis of reanalysis datasets shows significant correlations between February North Atlantic Sea Surface Temperature (NASST) and precipitation in Gobi Desert and Mongolia in the following summer, causing a decadal variation of dust event frequency in the subsequent spring over the region. Strong time-lagged correlation is shown to be linked to an atmospheric wave train pattern that initiated from the NASST region, affecting large-scale circulation, ultimately causing surface drought over Gobi Desert.https://doi.org/10.1088/2515-7620/ad19f3gobi desertdustnorth atlantic sea surface temperaturedecadal variability |
spellingShingle | Yeonsu Park Si-Wan Kim Young-Min Yang Kyoung-Min Kim Mi-Kyung Sung Soon-Il An Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert Environmental Research Communications gobi desert dust north atlantic sea surface temperature decadal variability |
title | Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert |
title_full | Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert |
title_fullStr | Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert |
title_full_unstemmed | Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert |
title_short | Possible impact of North Atlantic sea surface temperature on decadal variability of dust activity in Gobi Desert |
title_sort | possible impact of north atlantic sea surface temperature on decadal variability of dust activity in gobi desert |
topic | gobi desert dust north atlantic sea surface temperature decadal variability |
url | https://doi.org/10.1088/2515-7620/ad19f3 |
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