FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1600278853> ?p ?o ?g. }

• W1600278853 endingPage "2521" @default.
• W1600278853 startingPage "2511" @default.
• W1600278853 abstract "Sudden stratospheric warming (SSW) in the winter of 2008/2009 is the strongest recorded SSW event. The enhancement in semidiurnal variation of ionospheric TEC (total electron content) with phase shift forward is shown during 22 to 27 January 2009, based on the TEC observations in Beijing (40.30°N, 116.19°E geographic, 39.73°N dip latitude). We focus on finding the reason for the TEC variation. Winds observed by an all‐sky meteor radar in the same observatory are used to study mesospheric variation. The semidiurnal solar tide in the mesosphere starts to increase before the SSW and maintains oscillation with period 16–20 days during the SSW. The semidiurnal lunar tides in TEC and wind start to increase on 17 and 15 January, respectively. Although the semidiurnal lunar tide in TEC over Beijing almost dies out on 1 February, that over equatorial ionospheric anomaly crest does not vanish until 15 February when lunar tide in wind tends to be very weak. The maximum of lunar tide in wind appears on 2 February at 96 km with amplitudes of 15 m/s and 21 m/s for zonal and meridional winds. The phase comparison shows that lunar tides in TEC and zonal wind reach their maxima at almost the same time, which is 2–4 h lag behind the meridional wind. The coupling between the mesosphere and ionosphere contributes to the semidiurnal variation of TEC through both solar and semidiurnal lunar tides. The enhancement in semidiurnal lunar tide is responsible for the TEC peak shift forward during the SSW." @default.
• W1600278853 created "2016-06-24" @default.
• W1600278853 creator A5016666868 @default.
• W1600278853 creator A5032269255 @default.
• W1600278853 creator A5035878905 @default.
• W1600278853 creator A5051729149 @default.
• W1600278853 creator A5071162598 @default.
• W1600278853 creator A5072737831 @default.
• W1600278853 date "2013-05-01" @default.
• W1600278853 modified "2023-10-10" @default.
• W1600278853 title "Coupling between mesosphere and ionosphere over Beijing through semidiurnal tides during the 2009 sudden stratospheric warming" @default.
• W1600278853 cites W1499883790 @default.
• W1600278853 cites W1534676683 @default.
• W1600278853 cites W1565576960 @default.
• W1600278853 cites W1610992028 @default.
• W1600278853 cites W1622980052 @default.
• W1600278853 cites W1648765989 @default.
• W1600278853 cites W1649229465 @default.
• W1600278853 cites W1683584956 @default.
• W1600278853 cites W1707430005 @default.
• W1600278853 cites W1970509591 @default.
• W1600278853 cites W1977627480 @default.
• W1600278853 cites W1978743970 @default.
• W1600278853 cites W1978907947 @default.
• W1600278853 cites W1980146037 @default.
• W1600278853 cites W1980605581 @default.
• W1600278853 cites W1995733125 @default.
• W1600278853 cites W2005047310 @default.
• W1600278853 cites W2006307772 @default.
• W1600278853 cites W2006346291 @default.
• W1600278853 cites W2009994297 @default.
• W1600278853 cites W2010436212 @default.
• W1600278853 cites W2011567275 @default.
• W1600278853 cites W2013287837 @default.
• W1600278853 cites W2019553525 @default.
• W1600278853 cites W2031839859 @default.
• W1600278853 cites W2035254610 @default.
• W1600278853 cites W2038204397 @default.
• W1600278853 cites W2042454698 @default.
• W1600278853 cites W2043171981 @default.
• W1600278853 cites W2046357769 @default.
• W1600278853 cites W2047562524 @default.
• W1600278853 cites W2054991871 @default.
• W1600278853 cites W2056451297 @default.
• W1600278853 cites W2063082995 @default.
• W1600278853 cites W2068882733 @default.
• W1600278853 cites W2071743696 @default.
• W1600278853 cites W2078951470 @default.
• W1600278853 cites W2080307468 @default.
• W1600278853 cites W2084489672 @default.
• W1600278853 cites W2085605336 @default.
• W1600278853 cites W2086511638 @default.
• W1600278853 cites W2088259272 @default.
• W1600278853 cites W2093337996 @default.
• W1600278853 cites W2093739581 @default.
• W1600278853 cites W2104718076 @default.
• W1600278853 cites W2132292049 @default.
• W1600278853 cites W2154825135 @default.
• W1600278853 cites W2155869147 @default.
• W1600278853 cites W2156354812 @default.
• W1600278853 cites W2171369339 @default.
• W1600278853 doi "https://doi.org/10.1002/jgra.50280" @default.
• W1600278853 hasPublicationYear "2013" @default.
• W1600278853 type Work @default.
• W1600278853 sameAs 1600278853 @default.
• W1600278853 citedByCount "40" @default.
• W1600278853 countsByYear W16002788532014 @default.
• W1600278853 countsByYear W16002788532015 @default.
• W1600278853 countsByYear W16002788532016 @default.
• W1600278853 countsByYear W16002788532017 @default.
• W1600278853 countsByYear W16002788532018 @default.
• W1600278853 countsByYear W16002788532019 @default.
• W1600278853 countsByYear W16002788532020 @default.
• W1600278853 countsByYear W16002788532021 @default.
• W1600278853 countsByYear W16002788532022 @default.
• W1600278853 countsByYear W16002788532023 @default.
• W1600278853 crossrefType "journal-article" @default.
• W1600278853 hasAuthorship W1600278853A5016666868 @default.
• W1600278853 hasAuthorship W1600278853A5032269255 @default.
• W1600278853 hasAuthorship W1600278853A5035878905 @default.
• W1600278853 hasAuthorship W1600278853A5051729149 @default.
• W1600278853 hasAuthorship W1600278853A5071162598 @default.
• W1600278853 hasAuthorship W1600278853A5072737831 @default.
• W1600278853 hasBestOaLocation W16002788531 @default.
• W1600278853 hasConcept C116403925 @default.
• W1600278853 hasConcept C125405218 @default.
• W1600278853 hasConcept C127313418 @default.
• W1600278853 hasConcept C131980223 @default.
• W1600278853 hasConcept C145025062 @default.
• W1600278853 hasConcept C163861444 @default.
• W1600278853 hasConcept C165391973 @default.
• W1600278853 hasConcept C176379880 @default.
• W1600278853 hasConcept C69976271 @default.
• W1600278853 hasConcept C8058405 @default.
• W1600278853 hasConcept C88582754 @default.
• W1600278853 hasConcept C91586092 @default.
• W1600278853 hasConceptScore W1600278853C116403925 @default.
• W1600278853 hasConceptScore W1600278853C125405218 @default.

• next