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From:Atmospheric Chemistry and Physics (Vol. 23, Issue 1) Peer-ReviewedOrographic gravity waves (i.e., mountain waves) can potentially lead to cross-isentropic fluxes of trace gases via the generation of turbulence. During the DEEPWAVE (Deep Propagating Gravity Wave Experiment) campaign in...
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From:Atmospheric Chemistry and Physics (Vol. 23, Issue 1) Peer-ReviewedThe estimation of daily variations in aerosol concentrations using meteorological data is meaningful and challenging, given the need for accurate air quality forecasts and assessments. In this study, a 3x50-layer...
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From:Atmospheric Chemistry and Physics (Vol. 23, Issue 1) Peer-ReviewedThe Henry's law solubility (H.sub.S) and liquid-phase loss rate constants (k.sub.l) of the tropospheric trace gas constituents peroxyacetic nitric anhydride (PAN; CH.sub.3 C(O)O.sub.2 NO.sub.2, commonly known as...
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From:Atmospheric Chemistry and Physics (Vol. 23, Issue 1) Peer-ReviewedCurrent chemical transport models fail to reproduce both the concentrations and temporal variations of organic aerosol (OA), especially the secondary organic aerosol (SOA), hindering the identification of major...
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From:Atmospheric Chemistry and Physics (Vol. 23, Issue 1) Peer-ReviewedWe utilized the global atmospheric reanalysis ERA5 and reconstructed sea surface temperature (SST) data from 1979 through 2020 to examine the stability of the relationship between the SST oscillations in the southern...