Results 161 to 170 of about 11,342 (218)
Signature of a zonally symmetric semidiurnal tide during major sudden stratospheric warmings and plausible mechanisms: a case study. [PDF]
Sci RepMitra G, Guharay A, Paulino I.
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Transbronchial Microwave Ablation of Peripheral Lung Tumors: The NAVABLATE Study. [PDF]
J Bronchology Interv PulmonolLau KKW +4 more
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Modeling method for refraction error compensation in ground object detection. [PDF]
PLoS OneYu D, Chen Z.
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, 2008 The Earth is surrounded by a blanket of air, called the atmosphere. The atmosphere is a thin layer of gases that envelope the Earth. The gases are held close to the earth by gravity and the thermal movement of air molecules. Life on Earth is supported by the atmosphere, solar energy, and the magnetic fields.
Williams, Akan B.
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Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1956
Abstract The influence of thermal conductivity on the temperature distribution in the thermosphere is discussed. It is inferred that the temperature gradient probably falls off rapidly above the base of the F1 layer instead of remaining almost constant up to great altitudes, as is often assumed.
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Abstract The influence of thermal conductivity on the temperature distribution in the thermosphere is discussed. It is inferred that the temperature gradient probably falls off rapidly above the base of the F1 layer instead of remaining almost constant up to great altitudes, as is often assumed.
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Journal of Geophysical Research, 1976
Analysis of rocket-borne mass spectrometric thermospheric measurements of major and minor neutral species by coupled multicomponent equations of motion reveals the lower thermosphere to be in a nonequilibrium state. The individual species motion and thermal diffusion are significant factors in (1) the theoretical calculations of self-consistent species
S. P. Zimmerman, T. J. Keneshea
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Analysis of rocket-borne mass spectrometric thermospheric measurements of major and minor neutral species by coupled multicomponent equations of motion reveals the lower thermosphere to be in a nonequilibrium state. The individual species motion and thermal diffusion are significant factors in (1) the theoretical calculations of self-consistent species
S. P. Zimmerman, T. J. Keneshea
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Planetary and Space Science, 1961
The vertical distribution of the density in the thermosphere, deduced from satellite observations, must be explained by an increase of the scale height with altitude. A varying gradient of the scale heighht cannot be interpreted by assuming an increase of the temperature gradient with altitude.
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The vertical distribution of the density in the thermosphere, deduced from satellite observations, must be explained by an increase of the scale height with altitude. A varying gradient of the scale heighht cannot be interpreted by assuming an increase of the temperature gradient with altitude.
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From Lotosphere to Thermosphere
2017This paper reflects on the influential nature of some of the many scientific achievements linked to Ed Brinksma on the occasion of his 60th birthday. We in particular discuss pioneering contributions in the contexts of constraint-oriented specification, model-based testing, and cost-optimal timed reachability, as well as with respect to tools and ...
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2021
The Earth’s Ionosphere and Thermosphere (IT) is a highly dynamic system persistently driven by variable forcings both from above (Solar EUV and the magnetosphere) and the lower atmosphere. The forcing from below accounts for the majority of the variability at low- and mid-latitude IT region during geomagnetic quiet times.
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The Earth’s Ionosphere and Thermosphere (IT) is a highly dynamic system persistently driven by variable forcings both from above (Solar EUV and the magnetosphere) and the lower atmosphere. The forcing from below accounts for the majority of the variability at low- and mid-latitude IT region during geomagnetic quiet times.
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