Titlebook: Shock Waves @ Marseille I; Hypersonics, Shock T Raymond Brun,Lucien Z. Dumitrescu Conference proceedings 1995 Springer-Verlag Berlin Heidel

嬉耍

Computational Analysis on Generic Forms in European Hypersonic Facilities: Standard Model Electre ansymmetric generic form provided also the possibility to study the influence of real gas effects on flap efficiency and heating. An increase in flap efficiency resulting from the shrinking of the separated boundary layer region in front of the flap combined with an increase of the pressure recovery o

Cubicle

Shock Wave Interactions in Hypervelocity Flowas effects are seen to increase the range of shock impingement points for which enhanced heating occurs. They also reduce the type IV (Edney 1968 a,b) interaction supersonic jet width and influence the type II—III transition process.

dura-mater

Flirtatious

束以馬具

ution of stable high-pressure cells in the subtropics (e.g. Sahara and Arabian deserts); (2) the continentality, based on the distance to the oceans that constitute the main source of moisture (e.g. deserts in Central Asia); (3) orographic barriers that block the path of weather fronts creating rain

巫婆

John L. Stollery Rivers transport approximately 75,000 million tonnes of material each year, of which 20,000 million tonnes reaches the sea, around 80 % in solid form and 20 % in solution. Fluvial systems are frequently the main agents involved in landscape evolution and exert a prime influence on other interrelate

華而不實(shí)

Lucien Z. Dumitrescusoil, and time. This chapter is mostly illustrated with photography because the small-scale details of the weathering process are difficult to capture with images from space. Nevertheless, some large-scale weathering forms may well be detected from space as pictures of exfoliation patterns or corest

神圣不可

narcissism

normous erosive forces due to their weight and their ability to transport and use rock debris of different sizes that are frozen at the glacier’s base. Rock debris scratches the hard rock at the valley floor and creates typical striae or striations as well as polishing of rock surfaces where finer p

Saline