Auswahl der wissenschaftlichen Literatur zum Thema „Mesospheric inversion layer“
Geben Sie eine Quelle nach APA, MLA, Chicago, Harvard und anderen Zitierweisen an
Inhaltsverzeichnis
Machen Sie sich mit den Listen der aktuellen Artikel, Bücher, Dissertationen, Berichten und anderer wissenschaftlichen Quellen zum Thema "Mesospheric inversion layer" bekannt.
Neben jedem Werk im Literaturverzeichnis ist die Option "Zur Bibliographie hinzufügen" verfügbar. Nutzen Sie sie, wird Ihre bibliographische Angabe des gewählten Werkes nach der nötigen Zitierweise (APA, MLA, Harvard, Chicago, Vancouver usw.) automatisch gestaltet.
Sie können auch den vollen Text der wissenschaftlichen Publikation im PDF-Format herunterladen und eine Online-Annotation der Arbeit lesen, wenn die relevanten Parameter in den Metadaten verfügbar sind.
Zeitschriftenartikel zum Thema "Mesospheric inversion layer"
Fadnavis, S., und G. Beig. „Mesospheric temperature inversions over the Indian tropical region“. Annales Geophysicae 22, Nr. 10 (03.11.2004): 3375–82. http://dx.doi.org/10.5194/angeo-22-3375-2004.
Der volle Inhalt der QuelleLe Du, Thurian, Philippe Keckhut, Alain Hauchecorne und Pierre Simoneau. „Observation of Gravity Wave Vertical Propagation through a Mesospheric Inversion Layer“. Atmosphere 13, Nr. 7 (22.06.2022): 1003. http://dx.doi.org/10.3390/atmos13071003.
Der volle Inhalt der QuelleCollins, R. L., G. A. Lehmacher, M. F. Larsen und K. Mizutani. „Estimates of vertical eddy diffusivity in the upper mesosphere in the presence of a mesospheric inversion layer“. Annales Geophysicae 29, Nr. 11 (15.11.2011): 2019–29. http://dx.doi.org/10.5194/angeo-29-2019-2011.
Der volle Inhalt der QuelleHozumi, Yuta, Akinori Saito, Takeshi Sakanoi, Atsushi Yamazaki und Keisuke Hosokawa. „Mesospheric bores at southern midlatitudes observed by ISS-IMAP/VISI: a first report of an undulating wave front“. Atmospheric Chemistry and Physics 18, Nr. 22 (19.11.2018): 16399–407. http://dx.doi.org/10.5194/acp-18-16399-2018.
Der volle Inhalt der QuelleSiva Kumar, V., Y. Bhavani Kumar, K. Raghunath, P. B. Rao, M. Krishnaiah, K. Mizutani, T. Aoki, M. Yasui und T. Itabe. „Lidar measurements of mesospheric temperature inversion at a low latitude“. Annales Geophysicae 19, Nr. 8 (31.08.2001): 1039–44. http://dx.doi.org/10.5194/angeo-19-1039-2001.
Der volle Inhalt der QuelleRamesh, K., S. Sridharan, K. Raghunath, S. Vijaya Bhaskara Rao und Y. Bhavani Kumar. „Planetary wave-gravity wave interactions during mesospheric inversion layer events“. Journal of Geophysical Research: Space Physics 118, Nr. 7 (Juli 2013): 4503–15. http://dx.doi.org/10.1002/jgra.50379.
Der volle Inhalt der QuelleRamesh, K., S. Sridharan und K. Raghunath. „Rayleigh lidar observation of tropical mesospheric inversion layer: a comparison between dynamics and chemistry“. EPJ Web of Conferences 176 (2018): 03003. http://dx.doi.org/10.1051/epjconf/201817603003.
Der volle Inhalt der QuelleQIAO Shuai, PAN Weilin, BAN Chao, CHEN Lei und YU Ting. „Characterization of Mesospheric Inversion Layer with Rayleigh Lidar Data over Golmud“. Chinese Journal of Space Science 39, Nr. 1 (2019): 84. http://dx.doi.org/10.11728/cjss2019.01.084.
Der volle Inhalt der QuelleDuck, Thomas J., Dwight P. Sipler, Joseph E. Salah und John W. Meriwether. „Rayleigh lidar observations of a mesospheric inversion layer during night and day“. Geophysical Research Letters 28, Nr. 18 (15.09.2001): 3597–600. http://dx.doi.org/10.1029/2001gl013409.
Der volle Inhalt der QuelleMcDade, Ian C., und Edward J. Llewellyn. „Satellite airglow limb tomography: Methods for recovering structured emission rates in the mesospheric airglow layer“. Canadian Journal of Physics 71, Nr. 11-12 (01.11.1993): 552–63. http://dx.doi.org/10.1139/p93-084.
Der volle Inhalt der QuelleDissertationen zum Thema "Mesospheric inversion layer"
Mariaccia, Alexis. „Interaction ondes-écoulement moyen et impact sur la variabilité de la moyenne atmosphère“. Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ025.
Der volle Inhalt der QuelleThe middle atmosphere spans from 10 to 90 km and comprises the stratosphere (10 to 50 km) and the mesosphere (50 to 90 km). The equilibrium in the middle atmosphere results from the vertical propagation of small- and large-scale atmospheric waves redistributing the angular momentum across the atmosphere. These waves notably perturb the mean flow when they break, depositing their momentum and energy impacting the general circulation. Moreover, this wave-mean flow interaction is responsible for phenomena governing the observed variability in the middle atmosphere. Notably, the two most dramatic are the sudden stratospheric warmings (SSWs) and the mesospheric inversion layers (MILs). Specifically, SSWs manifest in winter by increasing the polar cap temperature (40 to 60 K) and weakening the polar vortex, which can reverse the westerly winds for the most extreme cases. A perturbed polar vortex can then impact the tropospheric weather in the following months by generating, for instance, severe cold air outbreaks. MILs represent an unexpected increase in temperature (10 to 50 K) occurring in the mesosphere, lasting several days and spanning thousands of kilometers. Moreover, MILs can represent significant issues for the safe reentry of rockets, space shuttles, or missiles into the atmosphere, sparking more interest in this phenomenon. For many years, the scientific community has investigated these two phenomena to understand their mechanism of occurrence and their effects on the atmosphere. The emergence of LiDAR technology and improved reanalysis products archiving the past climate has made their study more accessible.In this thesis, the objective is to make advancements in the understanding and the description of SSW and MIL phenomena with new LiDAR observations acquired at the Observatoire of Haute-Provence (44°N, 6°E) and the last generation of reanalysis product, ERA5, lasting from 1940 until the present. To commence our study of these phenomena through ERA5 data, we initially evaluated the capability of ERA5 in replicating the variability in the middle atmosphere by comparing it with LiDAR observations. We found that the observed stratospheric variability during wintertime, including the one generated by SSWs, is accurately reproduced in ERA5 reanalysis. However, the model cannot replicate this accuracy in the summer stratosphere and mesosphere, regardless the season, due to either the absence or imprecise simulation of MIL events. Additionally, we present new co-located temperature-wind observations during MIL events and assess how ERA5 simulates wind in the presence of MIL. A deceleration in wind occurs in the same altitude range as the temperature enhancement, supporting the role of gravity waves in the apparition of this phenomenon. In light of these findings, the ERA5 reanalysis in the stratosphere and the troposphere was solely used to study the main winter stratosphere unfoldings modulated by the timing of SSWs and their vertical links throughout winter months. Interestingly, we discovered that during wintertime in the northern hemisphere, the stratosphere follows four separate scenarios with distinct stratosphere-troposphere couplings. We found notable surface precursors associated with these scenarios that could potentially have applications for seasonal prediction
Bücher zum Thema "Mesospheric inversion layer"
Dunlop, Storm. 1. The atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0001.
Der volle Inhalt der QuelleBuchteile zum Thema "Mesospheric inversion layer"
„Pollution of the Atmosphere“. In Environmental Toxicology, herausgegeben von Sigmund F. Zakrzewski. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195148114.003.0015.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Mesospheric inversion layer"
Wintersteiner, Peter P., und Edward Cohen. Observations and Modeling of the Upper Mesosphere: Mesopause Characteristics, Inversion Layers, and Bores. Fort Belvoir, VA: Defense Technical Information Center, Oktober 2005. http://dx.doi.org/10.21236/ada447582.
Der volle Inhalt der Quelle