|
OALib Journal期刊
ISSN: 2333-9721
费用：99美元
|
|
|
|
海雾形成机制的初步研究
, PP. 12-20
Abstract:
海雾是近海面层大气的水汽凝结现象.这种现象的发生是大气与海洋及大气内部热量和水汽交换的结果.Rodhe,B.[1]曾用湍流扩散方程讨论过湍流对雾形成的作用.Fisher,E.F.和Caplan[1]首次对雾和层云的形成进行数值试验.
| [1] | Barker,E,H.,Oceanic fog o numerical study,AD 16(1973).7934.
|
| [2] | Roach.W.T,and Slingo,A Quart.J.R,Met.Soc.,105(1979),603-613.
|
| [3] | Rodhe,B.,Tellus,14(1962),49-86.
|
| [4] | Fisher,E,L.and Caplan,.J.,Atmos.Sei,20(1963),5,425-437.
|
| [5] | Barker,E,H.,Bound,layer.Meteor.,11(1977),267-294.
|
| [6] | Brown,R.and Roach,W,T.,Quart.J.R,Met.Soc.,102(1976),336-854.
|
| [7] | Cox,S,K Weather Rev.,91(1969).637-651.
|
Full-Text
|
|
Contact Us
service@oalib.com QQ:3279437679 
WhatsApp +8615387084133
|
|
