atmosphere.Basedon temperaturechanges,theatmospherecanbebrokenintofourmajorlayers,andanother threesmallintermediatelayersthatserveastransitionregionsfromonelayertothenext. Thereisthetroposphereandtropopause,thestratosphereandstratopause,themesosphere andmesopause,andthethermosphere. Thetroposphereisthelayeroftheatmosphere...
1 Introduction The ablation of a continuous flux of extraterrestrial dust in the atmosphere gives rise to per- manent layers of free neutral and ionized metal atoms in the 80–110 km altitude range. From the initial ground based observations of sodium at the end of the 1930s (Chapman 1938)...
Towards reconciling the large-scale structure of turbulent boundary layers in the atmosphere and laboratory Bound.-Lay. Meteorol., 145 (2) (2012), pp. 273-306 CrossrefView in ScopusGoogle Scholar [12] Stanislas Michel Near Wall Turbulence: an experimental view Phys. Rev. Fluids, 2 (10) (...
We have established the laws of formation of boride coatings in the course of saturation of titanium from different boron-containing media in the atmosphere of dynamic vacuum at a temperature of 900–1100°C. We have shown that the phase composition depends on the saturation temperature and the ...
A specimen was cut 600 mm×600 mm and marked with three pairs of datum marks. The specimen was allowed to reach equilibrium with the laboratory atmosphere and the distance between each set of datum marks was measured. The specimen was then placed in a tray under a head of 25 mm of water...
Ocean atmosphere systemMathematical-analysisIncompressible limitPenalization problemSingular limits3d eulerModelFlowIntegrabilityIn this paper we describe the weak solutions of the Navier-Stokes equations with a large Coriolis term as the Rossby and the Ekman numbers go to zero in a special domain with ...
The atmosphere is above the surface of Earth and is a thin gaseous layer that permits the existence of living things. Earth has many dramatic physical features. Landforms such The layer of Earth that we live on is the crust. This is the as teaus, mountains, ins, and valleys are all ...
The voltage was swept from −2 V to 2 V and the measured current was in the order of 10−7 A. We tested if liquid-exfoliated BP can be applied in other electrical devices. The sensitivity of BP to the sur- rounding atmosphere can be applied as vapor sensors. Previous study...
Keller, Direct statistical simulation of the near-surface layers of a cometary atmosphere. II: a nonspherical nucleus. Sol. Syst. Res. 40, 219-229 (2006)Skorov Yu. V., Markelov G. N., and Keller H. U., Direct statistical simulation of the near-surface layers of the cometary ...
It is well known that carbon films deposited by sputtering can degrade due to internal stresses and decomposition in the atmosphere. There are distinct visible differences in appearance and properties between intact carbon films and severely degraded ones. A carbon film that has undergone severe degrad...