Literatura científica selecionada sobre o tema "Mesospheric inversion layer"
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Artigos de revistas sobre o assunto "Mesospheric inversion layer"
Fadnavis, S., e G. Beig. "Mesospheric temperature inversions over the Indian tropical region". Annales Geophysicae 22, n.º 10 (3 de novembro de 2004): 3375–82. http://dx.doi.org/10.5194/angeo-22-3375-2004.
Texto completo da fonteLe Du, Thurian, Philippe Keckhut, Alain Hauchecorne e Pierre Simoneau. "Observation of Gravity Wave Vertical Propagation through a Mesospheric Inversion Layer". Atmosphere 13, n.º 7 (22 de junho de 2022): 1003. http://dx.doi.org/10.3390/atmos13071003.
Texto completo da fonteCollins, R. L., G. A. Lehmacher, M. F. Larsen e K. Mizutani. "Estimates of vertical eddy diffusivity in the upper mesosphere in the presence of a mesospheric inversion layer". Annales Geophysicae 29, n.º 11 (15 de novembro de 2011): 2019–29. http://dx.doi.org/10.5194/angeo-29-2019-2011.
Texto completo da fonteHozumi, Yuta, Akinori Saito, Takeshi Sakanoi, Atsushi Yamazaki e 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, n.º 22 (19 de novembro de 2018): 16399–407. http://dx.doi.org/10.5194/acp-18-16399-2018.
Texto completo da fonteSiva Kumar, V., Y. Bhavani Kumar, K. Raghunath, P. B. Rao, M. Krishnaiah, K. Mizutani, T. Aoki, M. Yasui e T. Itabe. "Lidar measurements of mesospheric temperature inversion at a low latitude". Annales Geophysicae 19, n.º 8 (31 de agosto de 2001): 1039–44. http://dx.doi.org/10.5194/angeo-19-1039-2001.
Texto completo da fonteRamesh, K., S. Sridharan, K. Raghunath, S. Vijaya Bhaskara Rao e Y. Bhavani Kumar. "Planetary wave-gravity wave interactions during mesospheric inversion layer events". Journal of Geophysical Research: Space Physics 118, n.º 7 (julho de 2013): 4503–15. http://dx.doi.org/10.1002/jgra.50379.
Texto completo da fonteRamesh, K., S. Sridharan e 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.
Texto completo da fonteQIAO Shuai, PAN Weilin, BAN Chao, CHEN Lei e YU Ting. "Characterization of Mesospheric Inversion Layer with Rayleigh Lidar Data over Golmud". Chinese Journal of Space Science 39, n.º 1 (2019): 84. http://dx.doi.org/10.11728/cjss2019.01.084.
Texto completo da fonteDuck, Thomas J., Dwight P. Sipler, Joseph E. Salah e John W. Meriwether. "Rayleigh lidar observations of a mesospheric inversion layer during night and day". Geophysical Research Letters 28, n.º 18 (15 de setembro de 2001): 3597–600. http://dx.doi.org/10.1029/2001gl013409.
Texto completo da fonteMcDade, Ian C., e Edward J. Llewellyn. "Satellite airglow limb tomography: Methods for recovering structured emission rates in the mesospheric airglow layer". Canadian Journal of Physics 71, n.º 11-12 (1 de novembro de 1993): 552–63. http://dx.doi.org/10.1139/p93-084.
Texto completo da fonteTeses / dissertações sobre o assunto "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.
Texto completo da fonteThe 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
Livros sobre o assunto "Mesospheric inversion layer"
Dunlop, Storm. 1. The atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0001.
Texto completo da fonteCapítulos de livros sobre o assunto "Mesospheric inversion layer"
"Pollution of the Atmosphere". In Environmental Toxicology, editado por Sigmund F. Zakrzewski. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195148114.003.0015.
Texto completo da fonteRelatórios de organizações sobre o assunto "Mesospheric inversion layer"
Wintersteiner, Peter P., e Edward Cohen. Observations and Modeling of the Upper Mesosphere: Mesopause Characteristics, Inversion Layers, and Bores. Fort Belvoir, VA: Defense Technical Information Center, outubro de 2005. http://dx.doi.org/10.21236/ada447582.
Texto completo da fonte