Garratt J R.1992.The Atmospheric Boundary Layer[M].Corn-bridge:Cambridge University Press,320pp.
[2]
何云开,黄健,贺志刚,等.2008.南海北部近岸春季海雾的年际变化[J].热带海洋学报,27(5):6-11.He Yunkai,Huang Jian,He Zhigang,et al.2008.Inter-annual variability of spring sea fog over northern South China Sea[J].Journal of Tropical O-ceanography(in Chinese),27(5):6-11.
[3]
胡瑞金,董克惠,周发琇.2006.海雾生成过程中平流、湍流和辐射效应的数值试验[J].海洋科学进展,24(2):156-165.Hu Ruijin,Dong Kehui,Zhou Faxiu.2006.Numerical experiments with the advection,turbulence and radiation effects in the seafog formation process[J].Advance Marine Science (in Chinese),24 (2):156-165.
[4]
Koracin D,Leipper D F,Lewis J M.2005a.Modeling sea fog on the U.S.California coast during a hot spell event[J].Geofizika,22:59-82.
[5]
Koracin D,Businger J A,Dorman C E,et al.2005b.Formation,evolution,and dissipation of coastal sea fog[J].Bound.-Layer Meteor.,117:447-478.
[6]
Lamb H.1943.Haars or North Sea fogs on the coasts of Great Brit-ain[R].Meteorology Office Publication M.O.504
[7]
Leipper D.1945.Forecasting summer fog at Shemya,Alaska[R].Weather Central,Alaska,11th Weather Region.Air Weather Service Tech.Rep.105-45.45pp.
[8]
Leipper DF.1994.Fog on the U.S.West Coast:A review[J].Bull.Amer.Meteor.Soc.,75:229-240.
[9]
Lennartsson L.2005.Influence of fog on stratification and turbulent fluxes over the ocean[D].M.S.Thesis,Institute of meteorolo-gy at Uppsala University.
[10]
Lewis J M,Koracin D,Redmond K T.2004.Sea fog research in the United Kingdom and United States:A historical essay including outlook[J].Bull.Amer.Meteor.Soc,75:395-408.
[11]
Nicholls S.1984.The dynamics of stratocumulus:Aircraft observa-tions and comparisons with a mixed layer model[J].Quart.J.Roy.Meteor.Soc.,110:783-820.
[12]
Pepper D W,Lee S C.1975.Transport phenomena in thermally stratified boundary layers[J].J.Heat Transfer,2:60-65.
[13]
Pili(e) R,Mack E J,Rogers C W,et al.1979.The formation of ma-rine fog and the development of fog-stratus systems along the Cali-fornia coast[J].J.Appl.Meteor.,18:1275-1286.
[14]
Roach W T.1995.Back to basics,Fog,Part 3-The formation and dissipation of sea fog[J].Weather,50:80-84
[15]
Rodhe B.1962.The effect of turbulence on fog formation[J].Tel-lus,14:49-86
[16]
Rogers D P,Koracin D.1992.Radiative transfer and turbulence in the cloud-topped marine atmospheric boundary layer[J].J.At-mos.Sci.,49:1473-1486.
[17]
Schuepp P H,Leclerc M Y,MacPherson J I,et al.1990.Footprint prediction of scalar fluxes from analytical solutions of the diffusion equation[J].Bound.-Layer Meteor.,50:355-373.
[18]
Stull R B.1988.An Introduction to Boundary Layer Meteorology[M].Dordrecht:Kluwer Academic Publishers,670pp.
[19]
Taylor G I.1917.The formation of fog and mist[J].Quart.J.Roy.Meteor.Soc.,43:241-268.
周发琇,刘龙太.1986.长江口及济州岛邻近海域综合调查报告(海雾)[J].山东海洋学院学报,16(1):115-131.Zhou Faxiu,Liu Longtai.1986.The report of comprehensive investigation for the adjacent seas of the mouth of Changjiang River and Jeju Is-land:Sea fog[J].Acta Shandong Institute of Oceanography(in Chinese),16(1):115-131.
[22]
Crofoot R F.2004.Investigations of scalar transfer coefficients in fog during the Coupled Boundary Layers and Air-Sea Transfer experiment,a case study[D].M.S.Thesis,WHOI/MIT Joint Program.
[23]
Douglas C.1930.Cold fogs over the sea[J].Meteor.Mag.,65:133-135.
[24]
Edson J,Crawford T,Crescenti J,et al.2007.The coupled bound-ary layers and air-sea transfer experiment in low winds[J].Bull.Amer.Meteor.,Soc,88:341-356.
[25]
Filonczuk M K,Cayan D R,Riddle L G.1995.Variability of ma-rine fog along the California Coast[R].Report 95-2.Scripps In-stitution of Oceanography,La Jolla,CA,92093-0224.
[26]
Findlater J,Roach W,McHugh B.1989.The haar of north-east Scotland[J].Quart.J.Roy.Meteor.Soc.,115:581-608.
[27]
Finnigan J J,Clement R,Malhi Y.2003.A re-evaluation of long-term flux measurement techniques.Part I:Averaging and coordi-nate rotation[J].Bound.-Layer Meteor.,107:1-48.
[28]
Gao Shanhong,Lin Hang,Shen Biao,et al.2007.A heavy sea fog event over the Yellow Sea in March 2005:Analysis and numerical modeling[J].Adv.Atmos.Sci.,24:65-81.
[29]
Kaimal J C.1975.Sensors and techniques for direct measurement of turbulent fluxes and profiles in the atmospheric surface layer[R].Atmospheric Technology,Tech.,No.7.
