Abstract
The 3-D complex topography effect on the surface solar radiative budget over the Tibetan Plateau is investigated by means of a parameterization approach on the basis of “exact” 3-D Monte Carlo photon tracing simulations, which use 90 m topography data as building blocks. Using a demonstrative grid size of 10 × 10 km2, we show that differences in downward surface solar fluxes for a clear sky without aerosols between the 3-D model and the conventional plane-parallel radiative transfer scheme are substantial, on the order of 200 W/m2 at shaded or sunward slopes. Deviations in the reflected fluxes of the direct solar beam amount to about +100 W/m2 over snow-covered areas, which would lead to an enhanced snowmelt if the 3-D topography effects had been accounted for in current climate models. We further demonstrate that the entire Tibetan Plateau would receive more solar flux by about 14 W/m2, if its 3-D mountain structure was included in the calculations, which would result in larger sensible and latent heat transfer from the surface to the atmosphere.
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References
Chen Y, Hall A, Liou KN (2006) Application of 3D solar radiative transfer to mountains. J Geophys Res 111:D21111. doi:10.1029/2006JD007163
Dozier J, Frew J (1990) Rapid calculations of terrain parameters for radiation modeling from digital elevation data. IEEE Trans Geosci Remote Sens 28:963–969. doi:10.1109/36.58986
Dubayah R, Rich P (1995) Topographic solar radiation models for GIS. Int J Geogr Inf Sci 9:405–419. doi:10.1080/02693799508902046
Dubayah R, Dozier J, Davis FW (1989) The distribution of clear-sky radiation over varying terrain. Proceedings IGARSS '89 vol. 2: 885–888, IEEE 89CH2768-0
Dubayah R, Dozier J, Davis FW (1990) Topographic distribution of clear-sky radiation over the Konza Prairie, Kansas. Water Resour Res 26:679–690. doi:10.1029/89WR03107
Essery R, Marks D (2007) Scaling and parameterization of clear-sky solar radiation over complex topography. J Geophys Res 112:D10122. doi:10.1029/2006JD007650
Fu Q, Liou KN (1992) On the correlated k-distribution method for radiative transfer in nonhomogeneous atmospheres. J Atmos Sci 49:2139–2156. doi:10.1175/1520-0469(1992) 049<2139:OTCDMF>2.0.CO;2
Govaerts YM, Verstraete MM (1998) Raytran: a Monte Carlo ray tracing model to compute light scattering in three-dimensional heterogeneous media. IEEE Trans Geosci Remote Sens 36:493–505
Gu Y, Farrara J, Liou KN, Mechoso CR (2003) Parameterization of cloud-radiation processes in the UCLA general circulation model. J Climate 16:3357–3370. doi:10.1175/1520-0442(2003) 016<3357:POCPIT>2.0.CO;2
Gu Y, Liou KN, Xue Y, Mechoso CR, Li W, Luo Y (2006) Climatic effects of different aerosol types in China simulated by the UCLA atmospheric general circulation model. J Geophys Res 111:D15201. doi:10.1029/2005JD006312
Iwabuchi H, Kobayashi H (2008) Modeling of radiative transfer in cloudy atmospheres and plant canopies using Monte Carlo methods. FRCGC Technical Report 8: pp 199
Jarvis A, Reuter HI, Nelson A, Guevara E (2008) Hole-filled seamless SRTM data V4, International Centre for Tropical Agriculture (CIAT), available from http://srtm.csi.cgiar.org
Lai Y-J, Chou M-D, Lin P-H (2010) Parameterization of topographic effect on surface solar radiation. J Geophys Res 115:D01104. doi:10.1029/2009JD012305
Lee W-L, Liou KN (2007) A coupled atmosphere–ocean radiative transfer system using the analytic four-stream approximation. J Atmos Sci 64:3681–3694
Lee W-L, Liou KN, Hall A (2011) Parameterization of solar fluxes over mountain surfaces for application to climate models. J Geophys Res 116:D01101. doi:10.1029/2010JD014722
Liou KN, Lee W-L, Hall A (2007) Radiative transfer in mountains: application to the Tibetan Plateau. Geophys Res Lett 34:L23809. doi:10.1029/2007GL031762
Mayer B, Hoch SW, Whiteman CD (2010) Validating the MYSTIC three-dimensional radiative transfer model with observations from the complex topography of Arizona’s Meteor Crater. Atmos Chem Phys 10:8685–8696
Molnar P, England P, Martinod J (1993) Mantle dynamics, uplift of the Tibetan Plateau, and the Indian monsoon. Rev Geophys 31:357–396
Preseindorfer RW, Mobley CD (1986) Albedos and glitter patterns of a wind-roughened sea surface. J Phys Oceanogr 16(7):1293–1316
Qiu J (2008) China: the third pole. Nature 454:393–396
Wang Q, Tenhunen J, Schmidt M, Otieno D, Kolcun O, Droesler M (2005) Diffuse PAR irradiance under clear skies in complex alpine terrain. Agric For Meteorol 128:1–15. doi:10.1016/j.agrformet.2004.09.004
Yang K, Pinker RT, Ma Y et al (2008) Evaluation of satellite estimates of downward shortwave radiation over the Tibetan Plateau. J Geophys Res 113:D17204. doi:10.1029/2007JD009736
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The research work presented in this paper was supported by the National Science Council, Taiwan under contracts NSC101-2111-M-001-001, NSC100-2119-M-001-029-MY5, and NSC98-2111-M-034-004-MY3, Academia Sinica, DOE Grant DE-SC0006742, and NSF Grant AGS-0946315.
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Lee, WL., Liou, K.N. & Wang, Cc. Impact of 3-D topography on surface radiation budget over the Tibetan Plateau. Theor Appl Climatol 113, 95–103 (2013). https://doi.org/10.1007/s00704-012-0767-y
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DOI: https://doi.org/10.1007/s00704-012-0767-y