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Artykuły w czasopismach na temat "Mesospheric inversion layer"
Fadnavis, S., i G. Beig. "Mesospheric temperature inversions over the Indian tropical region". Annales Geophysicae 22, nr 10 (3.11.2004): 3375–82. http://dx.doi.org/10.5194/angeo-22-3375-2004.
Pełny tekst źródłaLe Du, Thurian, Philippe Keckhut, Alain Hauchecorne i 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.
Pełny tekst źródłaCollins, R. L., G. A. Lehmacher, M. F. Larsen i 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.
Pełny tekst źródłaHozumi, Yuta, Akinori Saito, Takeshi Sakanoi, Atsushi Yamazaki i 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.
Pełny tekst źródłaSiva Kumar, V., Y. Bhavani Kumar, K. Raghunath, P. B. Rao, M. Krishnaiah, K. Mizutani, T. Aoki, M. Yasui i 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.
Pełny tekst źródłaRamesh, K., S. Sridharan, K. Raghunath, S. Vijaya Bhaskara Rao i Y. Bhavani Kumar. "Planetary wave-gravity wave interactions during mesospheric inversion layer events". Journal of Geophysical Research: Space Physics 118, nr 7 (lipiec 2013): 4503–15. http://dx.doi.org/10.1002/jgra.50379.
Pełny tekst źródłaRamesh, K., S. Sridharan i 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.
Pełny tekst źródłaQIAO Shuai, PAN Weilin, BAN Chao, CHEN Lei i 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.
Pełny tekst źródłaDuck, Thomas J., Dwight P. Sipler, Joseph E. Salah i 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.
Pełny tekst źródłaMcDade, Ian C., i 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 (1.11.1993): 552–63. http://dx.doi.org/10.1139/p93-084.
Pełny tekst źródłaRozprawy doktorskie na temat "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.
Pełny tekst źródłaThe 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
Książki na temat "Mesospheric inversion layer"
Dunlop, Storm. 1. The atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0001.
Pełny tekst źródłaCzęści książek na temat "Mesospheric inversion layer"
"Pollution of the Atmosphere". W Environmental Toxicology, redaktor Sigmund F. Zakrzewski. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195148114.003.0015.
Pełny tekst źródłaRaporty organizacyjne na temat "Mesospheric inversion layer"
Wintersteiner, Peter P., i Edward Cohen. Observations and Modeling of the Upper Mesosphere: Mesopause Characteristics, Inversion Layers, and Bores. Fort Belvoir, VA: Defense Technical Information Center, październik 2005. http://dx.doi.org/10.21236/ada447582.
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