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A Sample Form of a Manuscript for the Atmosphere
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Yeo-Jin Ma1), Sun-Sin Lee1),*, Hye-Sung Jang1), and Ok-Jung Jang2)
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School of Earth and Environmental Sciences, Seo-Woon National University, Seoul, Korea
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Korea Institute of Atmospheric Forecast Systems, Daegu, Korea
(Division, Institute, City, (province), Country)
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*Corresponding Author: Sun-Sin Lee, School of Earth and Environmental Sciences, Seo-Woon
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National University, 1 Gwanak-ro, Gwanak-gu, Seoul 111-222, Korea.
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(complete mailing address)
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Phone : +82-2-111-1111, Fax : +82-2-111-1112
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E-mail : sslee@snu.ac.kr
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Abstract(new page)
Abstract A parameterization for the scattering of longwave radiation by ice clouds has
been developed
……………………………………………………………………………………………
…………………………………………………………………………………………………...
(Abstract should not exceed 250 words. Citation references should not appear)
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Key words: Longwave radiation, ice cloud, single scattering property, parameterization
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andcooling rate
(equal or less than 5 words. Keywords should be provided in English.)
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1. Introduction(primary heading, 1st page of main text, new page)
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About 16% or more of the whole earth is covered with thin clouds (Patterson,
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2001), which include a great amount of ice crystals. The radiative effects of cirrus
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clouds should be treated carefully, since the flux density change in the atmosphere and
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at the surface according to the sizes and shapes of these clouds…………………………
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……………………………………………………………………………………………………
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1.1 Data and methods (secondary heading)
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1.1.1 Choosing one model(tertiary heading)
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Let us consider the plane parallel atmosphere, the upward and downward flux (Chou et
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al., 2002b) at level p can be computed from following Eqs. (1) and (2).
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……………………………………………………………………………………………
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…………………………………………………………………..
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.
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1.1.1.1 Station-measured precipitation data(quaternary heading)
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Figures 4-6 show regression curves of scattering properties according to the effective
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sizes and the nine spectral bands (Table 1) for the mixture of ice crystals (Chou et al.,
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2002b) with Eqs…………………………………………………………………………
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……………………………………………………………………………………………
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2. Results(primary heading)
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The flux and cooling rates were calculated with the optical thickness and the effective
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size of ice crystals, applying the six-stream discrete ordinate algorithm to estimate the
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effectsof…………………………………………………………………………………
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………………………………………………………………………………………….
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3. Conclusions(primary heading)
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In the existing GCM or numerical model, the calculation of longwave flux considers
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only the absorption of ice clouds by a simple experience formula, leaving the scattering
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properties of clouds out of co……………………………………………………………..
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Acknowledgments
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This research is supported by…………………………………………………………
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Appendix(optional)
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REFERENCES (new page, Should be for authors to provide English references)
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Chou, M. D., K. T. Lee, and P. Yang, 2002a : Parameterization of shortwave cloud
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optical properties for a mixture of ice particle habits for use in atmospheric models. J.
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Geophys. Res., 107, 4600, doi:2002JD002061.
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______, M. J. Suarez, X. Z. Liang, and M. M.-H Yan, 2002b: A Thermal Infrared
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Radiation Parameterization for Atmospheric Studies. NASA Technical Memorandum,
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19(104606), 55 pp.
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Table 1. (new page)Locations of Ieodo Ocean Research Station (IORS) and Array for Real-time
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Geostrophic Oceanography (ARGO), water depths at the position, and ID numbers of ARGO.
Data Type
Longitude (oE)
Latitude (oN)
Depth (m)
ID number
IORS
125.17
32.11
65
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G1
137.08
21.96
2000
2900432
G2
127.43
20.90
1400
2900518
G3
127.38
16.79
2000
2900435
G4
127.88
12.37
1500
2900516
G5
132.05
12.61
1500
2900523
ARGO
Float
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Fig. 1. (new page) Schematic diagram of model domain and experimental design.
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