Bruegge, C., Chrien, N., and Haner, D., 2001. A Spectralon BRF data base for MISR calibration applications. Remote Sensing of Environment, 76, 354–366.

Albedo - Etsy UK Overlord Albedo - Etsy UK

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.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.

Question paper (Modified A4 18pt) (Higher) : Paper 2 - June 2019

Constellation Level 1, Flower of Eden: "Transient Blossoms generated by Albedo's Abiogenesis: Solar Isotoma regenerate 1.2 Energy for Albedo." Damage from the environmental instead of the player (burning grass, fall damage, etc.) can generate Transient Blossoms. 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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Grenfell, T. C., and Perovich, D. K., 1984. Spectral albedos of sea ice and incident solar irradiance in the southern Beaufort Sea. Journal of Geophysical Research, 89, 3573–3580. 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. Mullen, P. C., and Warren, S. G., 1988. Theory of the optical properties of lake ice. J. Geophys. Res., 93(D7), 8403–8414.

Albedo: Wing Ver. - Museum collection Albedo: Wing Ver. - Museum collection

Dunkle, R. V., and Bevans, J. T., 1956. An approximate analysis of the solar reflectance and transmittance of a snow cover. Journal of Meteorology, 13, 212–216. Pegau, W. S., and Paulson, C. A., 2001. The albedo of arctic leads in summer. Annals of Glaciology, 33, 221–224. 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

GOOD SMILE RACING

Greuell, W., and de Ruyter de Wildt, M., 1999. Anisotropic reflection by melting glacier ice: measurements and parametrizations in Landsat TM Bands 2 and 4. Remote Sensing of Environment, 70, 265–277. Segelstein, D., 1981. The Complex Refractive Index of Water. M.S. Thesis, University of Missouri, Kansas City. Taylor, V. R., and Stowe, L. L., 1984. Reflectance characteristics of uniform earth and cloud surfaces derived from Nimbus-7 ERB. Journal of Geophysical Research, 89, 4987–4996.

Albedo Figure - Etsy UK

Warren, S. G., and Wiscombe, W. J., 1980. A model for the spectral albedo of snow, 2, Snow containing atmospheric aerosols. Journal of Atmospheric Sciences, 37, 2734–2745. Albedo is the amount of sunlight ( solar radiation) reflected by a surface, and is usually expressed as a percentage or a decimal value, with 1 being a perfect reflector and 0 absorbing all incoming light. When talking about albedo, the surface is almost always the surface of a planet like Earth. [2] White objects, such as a snowy hill have a high albedo. Conversely, dark objects, like pavement, have a low albedo. [3] The term can also refer to human made structures. In fact, energy efficient building design takes albedo into consideration whether a wall or ceiling warms the building or keeps it cool - resulting in a choice of a dark or light coating respectively. Fatal Blossom DMG will snapshot Albedo's stats when Abiogenesis: Solar Isotoma is cast and will not be affected by changes in his stats that occur afterwards. [5]

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.