... Atmospheric and Oceanic Boundary Layer Physics V. Lykossov 3.1 Introduction The globe of the earth is surrounded by a gaseous atmosphere which is always in motion. ... One of the most important problems is the parameterization of the turbulent uxes of momentum, latent and sensible heat at the sea surface. ... In the atmospheric surface layer, typically the lower 10 % of the boundary layer, the turbulent uxes of momentum, water vapor and sensible heat are nearly constant with height. ...

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... An extended set of observables of the nuclear quasi-free (p, d + ) reaction including the triple differential cross-section for coincidence measurements, its analyzing power in case of polarized proton beams and, also, the parameters of the polarization of the excited recoil nucleus and the produced deuteron are considered in the framework of the distorted-wave impulse approximation using the reaction 16 O(p, d + )15 N at a proton energy of 650 MeV as an example. ...

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... LEX _COLON ) throw curr_ lex ; else { gl (); if ( c_type == LEX _ INT ) { dec ( LEX _ INT ); gl(); } else _ lex ; LEX _SEMICOLON ) _ lex ; LEX _FIN ) _ lex ; 69 / if ( c_type == LEX _BOOL ) { dec ( LEX _BOOL ); gl(); } else throw curr_ lex ; } } } void Parser::B () { if ( c_type == LEX _BEGIN ) { gl(); S(); while ( c_type == ... LEX t hrow curr_lex; else { st_int.push ( c gl(); w hile (c_type = { gl(); if (c_type != throw curr_ e lse { st_int.push gl(); } } if (c_type !=...

284. BookLibrary

285. http://oc.cs.msu.su/smirnov/PPP/beameruserguide.pdf