000153463 001__ 153463
000153463 005__ 20210129213737.0
000153463 0247_ $$2doi$$a10.1002/2013JD021385
000153463 0247_ $$2WOS$$aWOS:000338340400006
000153463 0247_ $$2Handle$$a2128/16102
000153463 037__ $$aFZJ-2014-03061
000153463 041__ $$aEnglish
000153463 082__ $$a550
000153463 1001_ $$0P:(DE-HGF)0$$aYue, Jia$$b0$$eCorresponding Author
000153463 245__ $$aConcentric gravity waves in polar mesospheric clouds from the Cloud Imaging and Particle Size experiment
000153463 260__ $$c2014
000153463 3367_ $$2DRIVER$$aarticle
000153463 3367_ $$2DataCite$$aOutput Types/Journal article
000153463 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1402410810_26093
000153463 3367_ $$2BibTeX$$aARTICLE
000153463 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000153463 3367_ $$00$$2EndNote$$aJournal Article
000153463 520__ $$aFive concentric atmospheric gravity wave (AGW) events have been identified in Polar Mesospheric Cloud (PMC) images of the summer mesopause region (~82–84 km) made by the Cloud Imaging and Particle Size (CIPS) instrument on board the Aeronomy of Ice in the Mesosphere satellite during the Northern Hemisphere 2007 and 2009 PMC seasons. The AGWs modulate the PMC albedo, ice water content, and particle size, creating concentric ring patterns. On only one occasion (13 July 2007), the concentric AGWs in PMCs were aligned with AGWs with similar shapes observed in 4.3 µm radiance in the lower stratosphere, as measured by Atmospheric Infrared Sounder (AIRS). Coincident AIRS and Infrared Atmospheric Sounding Interferometer nadir measurements of 8.1 µm radiance reveal a region of deep convection in the troposphere close to the estimated centers of the AGWs in the stratosphere, strongly suggesting that convection is the wave source. The AGWs in CIPS on 13 July 2007 were ~1000 km away from the observed deep convection. Three other concentric AGWs in PMCs were 500–1000 km away from deep convection in the troposphere, while no convection was observed related to the wave on 29 July 2009. We perform a 2-D ray tracing study for the AGW event on 13 July 2007. The calculated propagation distance is much shorter than the distance between the AGWs in PMCs and the observed convection. The 2-D ray tracing study indicates that the AGWs in PMCs and in the stratosphere are probably excited by different tropospheric convective systems.
000153463 536__ $$0G:(DE-HGF)POF2-411$$a411 - Computational Science and Mathematical Methods (POF2-411)$$cPOF2-411$$fPOF II$$x0
000153463 588__ $$aDataset connected to CrossRef, juser.fz-juelich.de
000153463 7001_ $$0P:(DE-HGF)0$$aThurairajah, Brentha$$b1
000153463 7001_ $$0P:(DE-Juel1)129125$$aHoffmann, Lars$$b2$$ufzj
000153463 7001_ $$0P:(DE-HGF)0$$aAlexander, Joan$$b3
000153463 7001_ $$0P:(DE-HGF)0$$aChandran, Amal$$b4
000153463 7001_ $$0P:(DE-HGF)0$$aTaylor, Michael J.$$b5
000153463 7001_ $$0P:(DE-HGF)0$$aRussell, James M.$$b6
000153463 7001_ $$0P:(DE-HGF)0$$aRandall, Cora E.$$b7
000153463 7001_ $$0P:(DE-HGF)0$$aBailey, Scott M.$$b8
000153463 773__ $$0PERI:(DE-600)2016800-7$$a10.1002/2013JD021385$$n9$$p5115–5127$$tJournal of geophysical research / Atmospheres$$v119$$x0148-0227$$y2014
000153463 8564_ $$uhttps://juser.fz-juelich.de/record/153463/files/FZJ-2014-03061.pdf$$yOpenAccess$$zPublished final document.
000153463 909CO $$ooai:juser.fz-juelich.de:153463$$pdnbdelivery$$pVDB$$pdriver$$popen_access$$popenaire
000153463 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129125$$aForschungszentrum Jülich GmbH$$b2$$kFZJ
000153463 9132_ $$0G:(DE-HGF)POF3-511$$1G:(DE-HGF)POF3-510$$2G:(DE-HGF)POF3-500$$aDE-HGF$$bKey Technologies$$lSupercomputing & Big Data $$vComputational Science and Mathematical Methods$$x0
000153463 9131_ $$0G:(DE-HGF)POF2-411$$1G:(DE-HGF)POF2-410$$2G:(DE-HGF)POF2-400$$3G:(DE-HGF)POF2$$4G:(DE-HGF)POF$$aDE-HGF$$bSchlüsseltechnologien$$lSupercomputing$$vComputational Science and Mathematical Methods$$x0
000153463 9141_ $$y2014
000153463 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000153463 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000153463 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS
000153463 915__ $$0StatID:(DE-HGF)0110$$2StatID$$aWoS$$bScience Citation Index
000153463 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000153463 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000153463 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000153463 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000153463 915__ $$0StatID:(DE-HGF)1060$$2StatID$$aDBCoverage$$bCurrent Contents - Agriculture, Biology and Environmental Sciences
000153463 915__ $$0StatID:(DE-HGF)0310$$2StatID$$aDBCoverage$$bNCBI Molecular Biology Database
000153463 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline
000153463 915__ $$0StatID:(DE-HGF)1020$$2StatID$$aDBCoverage$$bCurrent Contents - Social and Behavioral Sciences
000153463 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000153463 920__ $$lyes
000153463 9201_ $$0I:(DE-Juel1)JSC-20090406$$kJSC$$lJülich Supercomputing Center$$x0
000153463 980__ $$ajournal
000153463 980__ $$aVDB
000153463 980__ $$aUNRESTRICTED
000153463 980__ $$aI:(DE-Juel1)JSC-20090406
000153463 9801_ $$aFullTexts