LEADER 04547nam 22006495 450 001 996418446903316 005 20200706030044.0 010 $a981-13-9085-1 024 7 $a10.1007/978-981-13-9085-2 035 $a(CKB)4940000000158694 035 $a(DE-He213)978-981-13-9085-2 035 $a(MiAaPQ)EBC6005401 035 $a(PPN)242842828 035 $a(EXLCZ)994940000000158694 100 $a20200103d2020 u| 0 101 0 $aeng 135 $aurnn|008mamaa 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aDynamical Characteristics of Inertia-Gravity Waves in the Antarctic Mesosphere$b[electronic resource] $eAnalyses Combining High-Resolution Observations and Modeling /$fby Ryosuke Shibuya 205 $a1st ed. 2020. 210 1$aSingapore :$cSpringer Singapore :$cImprint: Springer,$d2020. 215 $a1 online resource (XVI, 92 p.) 225 1 $aSpringer Theses, Recognizing Outstanding Ph.D. Research,$x2190-5053 300 $a"Doctoral thesis accepted by The University of Tokyo, Tokyo, Japan." 311 $a981-13-9084-3 327 $aGeneral Introduction -- A new transformation method for a quasi-uniform and fine grid system in a circular region using the spring dynamics -- Quasi-12 h inertia-gravity waves in the lower mesosphere observed by the PANSY radar at Syowa Station (39.6?°E, 69.0 °S) -- Gravity wave characteristics in the winter Antarctic mesosphere by a long-term numerical simulation using a non-hydrostatic general circulation model -- Summary and concluding remarks -- Acknowledgements. . 330 $aThis book examines the origins and dynamical characteristics of atmospheric inertia-gravity waves in the Antarctic mesosphere. Gravity waves are relatively small-scale atmospheric waves with a restoring force of buoyancy that can transport momentum upward from the troposphere to the middle atmosphere. In previous studies, the dynamical characteristics of mesospheric gravity waves have not been fully examined using numerical simulations, since performing a numerical simulation with a high resolution and a high model-top requires considerable computational power. However, recent advances in computational capabilities have allowed us to perform numerical simulations using atmospheric general circulation models, which cover the troposphere to the mesosphere with a sufficiently fine horizontal resolution to resolve small-scale gravity waves. The book first describes the simulation of mesospheric gravity waves using a high-resolution non-hydrostatic atmospheric model with a high model top. The accuracy of the numerical results was confirmed by the first Mesosphere-Stratosphere-Troposphere/Incoherent Scattering (MST/IS) radar observation in the Antarctic. It also depicts the origins and propagation processes of mesospheric gravity waves on the basis of the results of the high-resolution numerical model. The behaviors of mesospheric gravity waves can be clearly explained using both fundamental and cutting-edge theories of fluid dynamics. 410 0$aSpringer Theses, Recognizing Outstanding Ph.D. Research,$x2190-5053 606 $aGeophysics 606 $aComputer simulation 606 $aAtmospheric sciences 606 $aFluids 606 $aGeophysics and Environmental Physics$3https://scigraph.springernature.com/ontologies/product-market-codes/P32000 606 $aGeophysics/Geodesy$3https://scigraph.springernature.com/ontologies/product-market-codes/G18009 606 $aSimulation and Modeling$3https://scigraph.springernature.com/ontologies/product-market-codes/I19000 606 $aAtmospheric Sciences$3https://scigraph.springernature.com/ontologies/product-market-codes/G36000 606 $aFluid- and Aerodynamics$3https://scigraph.springernature.com/ontologies/product-market-codes/P21026 615 0$aGeophysics. 615 0$aComputer simulation. 615 0$aAtmospheric sciences. 615 0$aFluids. 615 14$aGeophysics and Environmental Physics. 615 24$aGeophysics/Geodesy. 615 24$aSimulation and Modeling. 615 24$aAtmospheric Sciences. 615 24$aFluid- and Aerodynamics. 676 $a531 700 $aShibuya$b Ryosuke$4aut$4http://id.loc.gov/vocabulary/relators/aut$0887450 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a996418446903316 996 $aDynamical Characteristics of Inertia-Gravity Waves in the Antarctic Mesosphere$91982529 997 $aUNISA LEADER 01230nam 2200337Ia 450 001 996390914403316 005 20221108064619.0 035 $a(CKB)1000000000667928 035 $a(EEBO)2248517335 035 $a(OCoLC)09427761 035 $a(EXLCZ)991000000000667928 100 $a19830419d1680 uy | 101 0 $aeng 135 $aurbn||||a|bb| 200 00$aTo the King and both Houses of Parliament$b[electronic resource] $ehere are some of our sufferings and grievances laid before you in the wisdom of God to take into your consideration and to relieve us 210 $a[London $cs.n.$d1680] 215 $a1 broadside 300 $aReproduction of original in the Harvard University Library. 330 $aeebo-0062 606 $aDissenters, Religious$xLegal status, laws, etc$zEngland 606 $aDissenters, Religious$zEngland 615 0$aDissenters, Religious$xLegal status, laws, etc. 615 0$aDissenters, Religious 701 $aCharles$cKing of England,$f1630-1685.$0793293 712 02$aEngland and Wales.$bParliament. 801 1$bEEU 801 2$bWaOLN 906 $aBOOK 912 $a996390914403316 996 $aTo the King and both Houses of Parliament$92334557 997 $aUNISA LEADER 00750nam a2200229 i 4500 001 991000612139707536 005 20020506132859.0 008 990611s1976 it ||| | ita 035 $ab10725428-39ule_inst 035 $aEXGIL148610$9ExL 040 $aBiblioteca Interfacoltà$bita 100 1 $aRemond, René$0388552 245 13$aIl XIX secolo 260 $aMilano :$bRizzoli,$c1976 300 $a249 p. ;$c18 cm. 500 $aII volume 907 $a.b10725428$b02-04-14$c28-06-02 912 $a991000612139707536 945 $aLE002 Fondo Giudici M 1121$g1$iLE002G-1121$lle002$o-$pE0.00$q-$rn$so $t0$u0$v0$w0$x0$y.i10822859$z28-06-02 996 $aXIX secolo$9912708 997 $aUNISALENTO 998 $ale002$b01-01-99$cm$da $e-$fita$git $h3$i1