FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2560804913> ?p ?o ?g. }

• W2560804913 abstract "Abstract Signatures of multiple stratospheric intrusions were observed on simultaneous and collocated ozone and water vapor profiles retrieved by lidars and radiosondes at the Maïdo Observatory, Reunion Island (21°S, 55°E, 2160 m above sea level), during MAïdo LIdar Calibration CAmpaign in April 2013. A singular structure of the ozone vertical profile with three peaks (in excess of 90 ppbv, at ~8, ~10, and ~13 km altitude) embedded in a thick dry layer of air suggested stratospheric intrusions with multiple origins. The hypothesis is corroborated by a synoptic analysis based on re‐analyses. European Centre for Medium‐Range Weather Forecasts ERA‐Interim temporal series associated with 5 days Lagrangian back trajectories initialized on each ozone peak allows to capture their stratospheric origin. The ozone peak at the lowest altitude is associated with an irreversible tropopause folding process along the polar jet stream during an extratropical cutoff low formation. Simultaneous lidar water vapor profiles of this peak show that the anticorrelation with ozone has been removed, due to mixing processes. Back trajectories indicate that the two other ozone peaks observed at higher altitudes are associated with the dynamics of the subtropical jet stream and the lower stratosphere. The observations confirm the recent stratospheric origins. The highest ozone peak is explained by the horizontal distribution of the intrusion. Use of a Lagrangian Reverse Domain Filling model and of the Meso‐NH Eulerian mesoscale model with a passive stratospheric tracer allow to further document the stratosphere‐troposphere transport processes and to describe the detailed potential vorticity and ozone structures in which are embedded in the observed multiple stratospheric intrusions." @default.
• W2560804913 created "2016-12-16" @default.
• W2560804913 creator A5000845350 @default.
• W2560804913 creator A5008690804 @default.
• W2560804913 creator A5009859726 @default.
• W2560804913 creator A5035276799 @default.
• W2560804913 creator A5037946408 @default.
• W2560804913 creator A5040764190 @default.
• W2560804913 creator A5046413368 @default.
• W2560804913 creator A5060433678 @default.
• W2560804913 creator A5086701413 @default.
• W2560804913 date "2016-12-22" @default.
• W2560804913 modified "2023-09-25" @default.
• W2560804913 title "Multiple subtropical stratospheric intrusions over Reunion Island: Observational, Lagrangian, and Eulerian numerical modeling approaches" @default.
• W2560804913 cites W1714398495 @default.
• W2560804913 cites W1789501672 @default.
• W2560804913 cites W1888229659 @default.
• W2560804913 cites W1965046336 @default.
• W2560804913 cites W1969915103 @default.
• W2560804913 cites W1975460872 @default.
• W2560804913 cites W1978120968 @default.
• W2560804913 cites W1979735728 @default.
• W2560804913 cites W1981810010 @default.
• W2560804913 cites W1981821774 @default.
• W2560804913 cites W1985550815 @default.
• W2560804913 cites W1986350444 @default.
• W2560804913 cites W1988158420 @default.
• W2560804913 cites W1989015374 @default.
• W2560804913 cites W1992500776 @default.
• W2560804913 cites W1993784124 @default.
• W2560804913 cites W1995199709 @default.
• W2560804913 cites W1997434369 @default.
• W2560804913 cites W1998016723 @default.
• W2560804913 cites W2002083966 @default.
• W2560804913 cites W2002443593 @default.
• W2560804913 cites W2006711613 @default.
• W2560804913 cites W2014037096 @default.
• W2560804913 cites W2020871079 @default.
• W2560804913 cites W2021277000 @default.
• W2560804913 cites W2022375558 @default.
• W2560804913 cites W2022446745 @default.
• W2560804913 cites W2025408334 @default.
• W2560804913 cites W2027793630 @default.
• W2560804913 cites W2031865695 @default.
• W2560804913 cites W2036168723 @default.
• W2560804913 cites W2044693808 @default.
• W2560804913 cites W2046033964 @default.
• W2560804913 cites W2050651382 @default.
• W2560804913 cites W2051927302 @default.
• W2560804913 cites W2053471539 @default.
• W2560804913 cites W2053933236 @default.
• W2560804913 cites W2055258612 @default.
• W2560804913 cites W2063531178 @default.
• W2560804913 cites W2064668420 @default.
• W2560804913 cites W2065895941 @default.
• W2560804913 cites W2070243750 @default.
• W2560804913 cites W2072739065 @default.
• W2560804913 cites W2075281384 @default.
• W2560804913 cites W2076520289 @default.
• W2560804913 cites W2076877883 @default.
• W2560804913 cites W2083339292 @default.
• W2560804913 cites W2086016079 @default.
• W2560804913 cites W2089987564 @default.
• W2560804913 cites W2090974104 @default.
• W2560804913 cites W2091118387 @default.
• W2560804913 cites W2094294508 @default.
• W2560804913 cites W2096153306 @default.
• W2560804913 cites W2108673018 @default.
• W2560804913 cites W2111266914 @default.
• W2560804913 cites W2112429580 @default.
• W2560804913 cites W2113373139 @default.
• W2560804913 cites W2118984328 @default.
• W2560804913 cites W2121370050 @default.
• W2560804913 cites W2121625343 @default.
• W2560804913 cites W2121745948 @default.
• W2560804913 cites W2122743645 @default.
• W2560804913 cites W2123694264 @default.
• W2560804913 cites W2124854884 @default.
• W2560804913 cites W2127181198 @default.
• W2560804913 cites W2130905116 @default.
• W2560804913 cites W2133984221 @default.
• W2560804913 cites W2135149625 @default.
• W2560804913 cites W2135419069 @default.
• W2560804913 cites W2137099629 @default.
• W2560804913 cites W2137937857 @default.
• W2560804913 cites W2138266040 @default.
• W2560804913 cites W2143767038 @default.
• W2560804913 cites W2144985953 @default.
• W2560804913 cites W2147522776 @default.
• W2560804913 cites W2147595550 @default.
• W2560804913 cites W2148053635 @default.
• W2560804913 cites W2149357482 @default.
• W2560804913 cites W2150572267 @default.
• W2560804913 cites W2150874742 @default.
• W2560804913 cites W2153915842 @default.
• W2560804913 cites W2157473329 @default.
• W2560804913 cites W2160571426 @default.
• W2560804913 cites W2163283870 @default.
• W2560804913 cites W2165726594 @default.
• W2560804913 cites W2167475648 @default.

• next