Matches in SemOpenAlex for { <https://semopenalex.org/work/W4304620008> ?p ?o ?g. }
- W4304620008 endingPage "13102" @default.
- W4304620008 startingPage "13087" @default.
- W4304620008 abstract "Abstract. Using European Centre for Medium-Range Weather Forecasts fifth-generation (ERA5) and second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) reanalysis and surface meteorological observation data, this study explores the possible impact of sudden stratospheric warming (SSW) events on air quality in the Beijing–Tianjin–Hebei (BTH) region. Major SSW events are divided into polar vortex displacement SSW and polar vortex split SSW. As the duration of split SSW events is longer and the stratospheric signal pulses propagate further downward than displacement SSWs, subseasonal variability of the atmospheric particulates in the BTH is larger during split SSWs. The air particulate concentration is light before the SSW onset due to the enhanced perturbation in the troposphere associated with strengthened planetary waves. The air particulate concentration around the SSW onset dates begins to rise due to weakening of the tropospheric disturbance as the enhanced planetary waves enter the stratosphere. In the decaying period of the SSW, the air particulate concentration decreases as the stratospheric negative northern annular mode (NAM) signal propagates downward. Specifically, in the pre-SSW period of displacement (split) SSW events, a wavenumber-1-like (wavenumber-2-like) anomaly pattern is strengthened. The East Asian winter monsoon intensifies as the East Asian trough is deepened, especially before the split SSW event onset, leading to a cleaning period. Around the SSW onset period as the tropospheric perturbation diminishes and the East Asian winter monsoon weakens, a surge of air particulate concentration is observed. After the SSW onset, due to the downward propagation of the stratospheric negative NAM signal, cold anomalies form in northeastern East Asia, especially for split SSWs, corresponding to a cleaning period in the BHT region. The local meteorological conditions during the SSWs are also discussed." @default.
- W4304620008 created "2022-10-12" @default.
- W4304620008 creator A5008200187 @default.
- W4304620008 creator A5031606363 @default.
- W4304620008 creator A5043091074 @default.
- W4304620008 creator A5049050520 @default.
- W4304620008 creator A5063660802 @default.
- W4304620008 creator A5073810224 @default.
- W4304620008 creator A5089572862 @default.
- W4304620008 date "2022-10-12" @default.
- W4304620008 modified "2023-10-17" @default.
- W4304620008 title "Possible influence of sudden stratospheric warmings on the atmospheric environment in the Beijing–Tianjin–Hebei region" @default.
- W4304620008 cites W1605302450 @default.
- W4304620008 cites W1965765914 @default.
- W4304620008 cites W1975434996 @default.
- W4304620008 cites W1997148915 @default.
- W4304620008 cites W2019594051 @default.
- W4304620008 cites W2088702514 @default.
- W4304620008 cites W2102906305 @default.
- W4304620008 cites W2103112181 @default.
- W4304620008 cites W2111954838 @default.
- W4304620008 cites W2130042267 @default.
- W4304620008 cites W2167315345 @default.
- W4304620008 cites W2292804962 @default.
- W4304620008 cites W2310212333 @default.
- W4304620008 cites W2371852352 @default.
- W4304620008 cites W2519497602 @default.
- W4304620008 cites W2528440629 @default.
- W4304620008 cites W2584213839 @default.
- W4304620008 cites W2594035764 @default.
- W4304620008 cites W2611772571 @default.
- W4304620008 cites W2617402157 @default.
- W4304620008 cites W2756959352 @default.
- W4304620008 cites W2793303697 @default.
- W4304620008 cites W2884477697 @default.
- W4304620008 cites W2885577621 @default.
- W4304620008 cites W2886845515 @default.
- W4304620008 cites W2887716294 @default.
- W4304620008 cites W2901434526 @default.
- W4304620008 cites W2903578514 @default.
- W4304620008 cites W2909413684 @default.
- W4304620008 cites W2913593218 @default.
- W4304620008 cites W2946245707 @default.
- W4304620008 cites W2961926878 @default.
- W4304620008 cites W2964421221 @default.
- W4304620008 cites W2970366149 @default.
- W4304620008 cites W2970481843 @default.
- W4304620008 cites W2971405396 @default.
- W4304620008 cites W2981436736 @default.
- W4304620008 cites W2984267390 @default.
- W4304620008 cites W3000049811 @default.
- W4304620008 cites W3001839736 @default.
- W4304620008 cites W3025949386 @default.
- W4304620008 cites W3026292362 @default.
- W4304620008 cites W3028399592 @default.
- W4304620008 cites W3036217958 @default.
- W4304620008 cites W3041160329 @default.
- W4304620008 cites W3113913879 @default.
- W4304620008 cites W3124246591 @default.
- W4304620008 cites W3128553283 @default.
- W4304620008 cites W3139731355 @default.
- W4304620008 cites W3172458608 @default.
- W4304620008 cites W3172858744 @default.
- W4304620008 cites W3178368669 @default.
- W4304620008 cites W3204989063 @default.
- W4304620008 cites W4211142008 @default.
- W4304620008 cites W4221042309 @default.
- W4304620008 cites W4229017145 @default.
- W4304620008 cites W4280506432 @default.
- W4304620008 doi "https://doi.org/10.5194/acp-22-13087-2022" @default.
- W4304620008 hasPublicationYear "2022" @default.
- W4304620008 type Work @default.
- W4304620008 citedByCount "5" @default.
- W4304620008 countsByYear W43046200082022 @default.
- W4304620008 countsByYear W43046200082023 @default.
- W4304620008 crossrefType "journal-article" @default.
- W4304620008 hasAuthorship W4304620008A5008200187 @default.
- W4304620008 hasAuthorship W4304620008A5031606363 @default.
- W4304620008 hasAuthorship W4304620008A5043091074 @default.
- W4304620008 hasAuthorship W4304620008A5049050520 @default.
- W4304620008 hasAuthorship W4304620008A5063660802 @default.
- W4304620008 hasAuthorship W4304620008A5073810224 @default.
- W4304620008 hasAuthorship W4304620008A5089572862 @default.
- W4304620008 hasBestOaLocation W43046200081 @default.
- W4304620008 hasConcept C125405218 @default.
- W4304620008 hasConcept C127313418 @default.
- W4304620008 hasConcept C136996986 @default.
- W4304620008 hasConcept C163861444 @default.
- W4304620008 hasConcept C178790620 @default.
- W4304620008 hasConcept C185592680 @default.
- W4304620008 hasConcept C24245907 @default.
- W4304620008 hasConcept C39432304 @default.
- W4304620008 hasConcept C49204034 @default.
- W4304620008 hasConcept C88582754 @default.
- W4304620008 hasConcept C9075549 @default.
- W4304620008 hasConcept C91586092 @default.
- W4304620008 hasConceptScore W4304620008C125405218 @default.
- W4304620008 hasConceptScore W4304620008C127313418 @default.