1 |
Yamada, T. and G. L. Mellor, 1983, A numerical simulation of the BOMEX data using a turbulence closure model coupled with ensemble cloud relations, Q. J. R. Meteor. Soc., 105, 95-944
|
2 |
Katayama, A, 1972, A simplified scheme for computing radiative transfer in the troposphere, Technical report No.6, Dept. of Meteorol., UCLA, 77pp
|
3 |
Businger, J. A, 1973, Turbulence transfer in the atmospheric surface layer, In Workshop on Micrometeorology(D. A Haugen, ed.), Amer. Meteor. Soc., 67-100pp
|
4 |
Monin, A.S., 1970, The atmospheric boundary layer, Annual Review of Fluid Mechanics, 2, 225-250
DOI
ScienceOn
|
5 |
Deardoff, J. W., 1978, Efficient prediction of ground surface temperature and moisture with inclusion of a layer of vegetation, Geophys. Res., 38, 659-661
|
6 |
Zangl, G., 2002, Stratified flow over a mountain with a gap, Linear theory and numerical simulations, Quart. J. Roy. Met. Soc., 128, 927-949
DOI
ScienceOn
|
7 |
Arya, S. P. S., 1988, Introduction to micrometeorology, Academic Press, 1-307pp
|
8 |
Palmer, T. N., G. J. Smith and R Swinbank, 1986, Alleviation of a systematic westerly bias in general circulation and NWP models through and orographic gravity wave drag parameterization, Q. J. R Meteor. Soc., 112, 1001-1039
DOI
|
9 |
Holton, J. R, 1992, Introduction to dynamic meteorology, Academic Press, 1-510pp
|
10 |
Bluestein, H. B., 1993, Synoptic-dynamic mete- orology in micllatitudes, Oxford Univ., 594pp
|
11 |
Segal, M., C. H. Yu, R. W. Arritt and R. A Pielke, 1988, On the impact of valley fridge thermally induced circulations on regional pollutant transport, Atmos. Environ., 22, 471-486
DOI
ScienceOn
|
12 |
Whiteman, C. D, 1990, Observations of thermally developed wind system in mountainous terrain, Atmospheric Processes over complex terrain, Meteor. Monogr., No. 40, Amer. Meteor. Soc., 5-42pp
|
13 |
Choi, H. and Y. H. Zhnag, 2005, Monthly variation of sea-air temperature differences in the Korean coast, J. Ocean., 61, 2, JO#818, in printed
|
14 |
Takahashi, S., 1997, Manual of LAS model reviced by Dr. J. Sato, 50pp
|
15 |
NFRI, 1995, SST Satellite pictures of GMS taken by National Fisheries Research & Development Institute
|
16 |
Klemp, J. B. and D. R. Durran, 1983, An upper condition permitting internal gravity wave radiation in numerical mesoscale models, Mon. Wea. Rev., 111, 430-440
DOI
|
17 |
Orlanski, I. A, 1976, Simple boundary condi- tion for unbounded hyperbolic flows, J. Comp. Phys., 21, 251-269
DOI
ScienceOn
|
18 |
Yamada, T., 1983, Simulation of nocturnal drainage flows by a q2-1 turbulence closure model, J. Atmos. Sci., 40, 91-106
DOI
|
19 |
Choi, H., Y. Zhang and S. Takahashi, 2004, Recycling of suspended particulates by the interaction of sea-land breeze circulation and complex coastal terrain, Meteor. and Atmos. Phys., 87, 109-120
|
20 |
Choi, H., J. Seo and J. Nam, 2002, Evolution of wind storm over coastal complex terrain, J. Environ. Sci., 11, 865-880
DOI
ScienceOn
|
21 |
Choi, H., 2004, Persistent high concentration of ozone during windstorm conditions in southern Korea, Meteor. and Atmos. Phys., 87, 93-107
|
22 |
Raynor, G. S., S. SethuRaman and R. M. Brown, 1979, Formation and characteristics of coastal internal boundary layer during onshore flows, Boundary Layer Meteor., 16, 4587-514
|
23 |
Pielke, R. A, 1984, Mesoscale meteorological modeling, Academic Press, 612pp
|