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Bruegge, C., Chrien, N., and Haner, D., 2001. A Spectralon BRF data base for MISR calibration applications. Remote Sensing of Environment, 76, 354–366. Old: 더 많은 석화 고목을 알고 싶다고? 흠흠… 인근 비경에서 네가 봤다던 나무는 사실 그리 오래된 게 아니야. 잘 여문 나무는 보통 2 –3km 까지 자랄 수 있고, 뿌리에 큰 거미가 모이지. 그 거미를 치자와 레몬그라스에 묶고 백두구를 발라 몇 시간 동안 훈연하면 그 향기는 정말이지… 잊을 수가 없어

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Brandt, R. E., Warren, S. G., and O’Rawe Hinton, P., 1988. Effect of surface roughness on bidirectional reflectance of Antarctic snow. Journal of Geophysical Research, 103, 25789–25807. Pope, R. M., and Fry, E. S., 1997. Absorption specturm (380–700 nm) of pure water. II. Integrating cavity measurements. Applied Optics, 36(33), 8710–8723. Passive Talent 2, Homuncular Nature: "Using Rite of Progeniture: Tectonic Tide increases the Elemental Mastery of nearby party members by 125 for 10s."

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Nolin, A. W., and Dozier, J., 2000. A hyperspectral method for remotely sensing the grain size of snow. Remote Sensing of Environment, 74(2), 207–216. Hudson, S. R., and Warren, S. G., 2007. An explanation for the effect of clouds over snow on the top-of-atmosphere bidirectional reflectance. Journal of Geophysical Research, 112, D19202, doi:10.1029/2007JD008541. Painter, T. H., and Dozier, J., 2004. Measurements of the hemispherical-directional reflectance of snow at fine spectral and angular resolution. Journal of Geophysical Research, 109, D18115, doi:10.1029/2003JD004458. Aoki, Te., Aoki, Ta., Fukabori, M., Hachikubo, A., Tachibana, Y., and Nishio, F., 2000. Effects of snow physical parameters on spectral albedo and bidirectional reflectance of snow surface. Journal of Geophysical Research, 105, 10219–10236.

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Kato, S., and Loeb, N. G., 2005. Top-of-atmosphere shortwave broadband observed radiance and estimated irradiance over polar regions from Clouds and the Earth’s Radiant Energy System (CERES) instruments on Terra. Journal of Geophysical Research, 110, D07202, doi:10.1029/2004JD005308. Comments that are not in accordance with the Guidelines and/or that violate TOM’s Terms of Use and/or other policies are eligible to be reported or removed. Warren, S. G., and Brandt, R. E., 2008. Absorption spectrum of ice from the ultraviolet to the microwave: a revised compilation. Journal of Geophysical Research, 113, D14220, doi:10.1029/2007JD009744.

Grenfell, T. C., 1991. A radiative transfer model for sea ice with vertical structure variations. Journal of Geophysical Research, 96(C9), 16,991–17,001. The Earth's climate depends on a balance of incoming and outgoing energy from the sun, which is determined by albedo. The overall albedo of the Earth - measured to be 0.30 - has a significant effect on the equilibrium temperature of the Earth as it changes how much solar energy is reflected by the Earth as opposed to how much is absorbed. [5] This changes how Earth's energy budget balances and thus changes Earth's heat balance.