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Talent Levels past 10 require Elemental Burst Level Increase methods, such as Constellations and Event bonuses. 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. Passive Talent 1, Calcite Might: "Transient Blossoms generated by Abiogenesis: Solar Isotoma deal 25% more DMG to opponents whose HP is below 50%." Release Date 2018/08 Specifications Painted 1/8th scale ABS&PVC figure with stand included. Approximately 250mm in height (stand included). Sculptor ehenmushi Paintwork Luu (Good Smile Shanghai) Oerlemans, J., and Knapp, W. H., 1998. A one-year record of global radiation and albedo from the ablation zone of the Morteratschgletscher, Switzerland. Journal of Glaciology, 44, 231–238.

term Global LAnd Surface Satellite (GLASS) data-set A long-term Global LAnd Surface Satellite (GLASS) data-set

Solar Isotoma is considered a Geo construct. Only one Solar Isotoma created by Albedo himself can exist at a time. 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 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.

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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. NASA Earth Observatory. (September 26, 2015). Albedo [Online]. Available: http://neo.sci.gsfc.nasa.gov/view.php?datasetId=MCD43C3_M_BSA 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. 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.

Kadokawa Overlord IV: Albedo (Wing Ver.) 1:7 Scale PVC Figure

KADOKAWA presents the figure brand KDcolle (KADOKAWA Collection), featuring figures with style only possible for KADOKAWA to create. With a charm unique to experienced publishing company KADOKAWA, we bring you a new series of figures sure to make your heart beat with excitement! Expect more from the KDcolle series coming soon! Measuring the Earth's Albedo, Accessed March 30th, 2019. https://earthobservatory.nasa.gov/images/84499/measuring-earths-albedo 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: The fraction of incident solar radiative energy flux, or irradiance, reflected and scattered upward from a surface integrated over the solar spectrum from 300 to approximately 3,000 nm.

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Constellation Level 1, Flower of Eden: "Transient Blossoms generated by Albedo's Abiogenesis: Solar Isotoma regenerate 1.2 Energy for Albedo." Active party members within the Solar Isotoma field who are protected by a shield created by Crystallize have their DMG increased by 17%. Andreassen, L. M., Van Den Broeke, M. R., Giesen, R. H., and Oerlemans, J., 2008. A five-year record of surface energy and mass balance from the ablation zone of Storbreen, Norway. Journal of Glaciology, 54(185), 245–258. 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.