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• W4200608439 endingPage "17951" @default.
• W4200608439 startingPage "17927" @default.
• W4200608439 abstract "Abstract. Events of very high concentrations of 7Be cosmogenic radionuclide have been recorded at low-elevation surface stations in the subpolar regions of Europe during the cold season. With an aim to investigate the mechanisms responsible for those peak 7Be events, and in particular to verify if they are associated with the fast descent of stratospheric air masses occurring during sudden stratospheric warming (SSW) events, we analyze 7Be observations at six sampling sites in Fennoscandia during January–March 2003 when very high 7Be concentrations were observed and the Arctic vortex was relatively unstable as a consequence of several SSW events. We use the GEOS-Chem chemistry and transport model driven by the MERRA-2 meteorological reanalysis to simulate tropospheric 7Be over northern Europe. We show that the model reasonably reproduces the temporal evolution of surface 7Be concentrations observed at the six sampling sites. Our analysis of model simulations, surface 7Be observations, atmospheric soundings of ozone and temperature and surface ozone measurements indicates that the 7Be peak observed in late February 2003 (between 20 and 28 February 2003) at the six sampling sites in Fennoscandia was associated with downward transport of stratospheric vortex air that originated during an SSW that occurred a few days earlier (between 18 and 21 February 2003)." @default.
• W4200608439 created "2021-12-31" @default.
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• W4200608439 creator A5068255176 @default.
• W4200608439 creator A5079989046 @default.
• W4200608439 date "2021-12-07" @default.
• W4200608439 modified "2023-10-04" @default.
• W4200608439 title "Observation and modeling of high-&lt;sup&gt;7&lt;/sup&gt;Be concentration events at the surface in northern Europe associated with the instability of the Arctic polar vortex in early 2003" @default.
• W4200608439 cites W1485504984 @default.
• W4200608439 cites W1586790202 @default.
• W4200608439 cites W1676711056 @default.
• W4200608439 cites W1835577090 @default.
• W4200608439 cites W1963576816 @default.
• W4200608439 cites W1965765914 @default.
• W4200608439 cites W1971828012 @default.
• W4200608439 cites W1972417965 @default.
• W4200608439 cites W1974652816 @default.
• W4200608439 cites W1979588280 @default.
• W4200608439 cites W1985204423 @default.
• W4200608439 cites W1985550815 @default.
• W4200608439 cites W1993317377 @default.
• W4200608439 cites W1998176560 @default.
• W4200608439 cites W2000334586 @default.
• W4200608439 cites W2000935886 @default.
• W4200608439 cites W2001592871 @default.
• W4200608439 cites W2004326514 @default.
• W4200608439 cites W2006451550 @default.
• W4200608439 cites W2007606522 @default.
• W4200608439 cites W2022548072 @default.
• W4200608439 cites W2025181463 @default.
• W4200608439 cites W2030565031 @default.
• W4200608439 cites W2032399408 @default.
• W4200608439 cites W2036873747 @default.
• W4200608439 cites W2045407173 @default.
• W4200608439 cites W2049313591 @default.
• W4200608439 cites W2052043577 @default.
• W4200608439 cites W2054169992 @default.
• W4200608439 cites W2059852281 @default.
• W4200608439 cites W2060060142 @default.
• W4200608439 cites W2060880581 @default.
• W4200608439 cites W2066432590 @default.
• W4200608439 cites W2066919485 @default.
• W4200608439 cites W2068553057 @default.
• W4200608439 cites W2070192517 @default.
• W4200608439 cites W2070548986 @default.
• W4200608439 cites W2075491821 @default.
• W4200608439 cites W2075671886 @default.
• W4200608439 cites W2077150157 @default.
• W4200608439 cites W2081486310 @default.
• W4200608439 cites W2082519451 @default.
• W4200608439 cites W2083538237 @default.
• W4200608439 cites W2084059271 @default.
• W4200608439 cites W2090094328 @default.
• W4200608439 cites W2098383830 @default.
• W4200608439 cites W2099558722 @default.
• W4200608439 cites W2101564561 @default.
• W4200608439 cites W2103112181 @default.
• W4200608439 cites W2116336472 @default.
• W4200608439 cites W2118739416 @default.
• W4200608439 cites W2118984328 @default.
• W4200608439 cites W2120464484 @default.
• W4200608439 cites W2121745948 @default.
• W4200608439 cites W2127592741 @default.
• W4200608439 cites W2127755761 @default.
• W4200608439 cites W2134573290 @default.
• W4200608439 cites W2137628452 @default.
• W4200608439 cites W2138017294 @default.
• W4200608439 cites W2138266040 @default.
• W4200608439 cites W2140961555 @default.
• W4200608439 cites W2141429989 @default.
• W4200608439 cites W2142741595 @default.
• W4200608439 cites W2157486648 @default.
• W4200608439 cites W2162909972 @default.
• W4200608439 cites W2166939475 @default.
• W4200608439 cites W2167315345 @default.
• W4200608439 cites W2170246412 @default.
• W4200608439 cites W2176254346 @default.
• W4200608439 cites W2177529417 @default.
• W4200608439 cites W2260089446 @default.
• W4200608439 cites W2295487937 @default.
• W4200608439 cites W2302890134 @default.
• W4200608439 cites W2320554369 @default.
• W4200608439 cites W2325950029 @default.
• W4200608439 cites W2336839330 @default.
• W4200608439 cites W2344772005 @default.
• W4200608439 cites W2389215025 @default.
• W4200608439 cites W2475015771 @default.
• W4200608439 cites W2477244287 @default.
• W4200608439 cites W2500132293 @default.
• W4200608439 cites W2555453528 @default.
• W4200608439 cites W2561327866 @default.
• W4200608439 cites W2611772571 @default.

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