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Перевод: albedo

[существительное]
альбедо
[существительное]

Тезаурус:

1. At high latitudes there are positive feedbacks to warming, such as the melting of the snow and ice which decreases surface reflectivity (albedo), allowing more solar energy to be absorbed at the surface; the thinner sea ice, allowing a greater flow of heat through the ice from the ocean in winter to enhance the warming of the surface; and the increased evaporation, leading to an enhanced water vapour greenhouse effect.
2. a = albedo
3. A simultaneous thinning and shrinking of the sea ice lessens its albedo, or reflectivity, thereby allowing the oceans to absorb more heat from the sun.
4. Because an increase in poleward heat flow cools the tropics while heating the poles, such heat flow could by itself lower planetary albedo.
5. Pangaea at the end of the Palaeozoic must have experienced a climate of extreme continentality, not only because of its coherence (Valentine Moores, 1972) but because of the high albedo of extensive low-latitude deserts (Barron et al .,
6. If the former is the case, then a reduced vegetation cover due to mismanagement may lead, by affecting albedo and soil moisture, to reduced convective processes and therefore less rainfall; thus self-perpetuating drought becomes the norm.
7. It has recently been proposed that variations in albedo with respect to latitude (with considerable consequences for global climate) are a result of both the changing distribution of continents and sea-level oscillations.
8. This is because of the higher Bond albedo of Venus.
9. Shumskiy (1957) defines antarctic oases as substantial ice-free areas separated from an ice-sheet by an ablation zone, and kept free from snow by ablation due to low albedo and radiation.
10. One of the most advanced examples of development has been CLIMAP (Climate, Long Range Investigation, Mapping and Prediction, Hays and Moore, 1973) which has made a reconstruction of global sea surface, ice extent, ice elevation and continental albedo for the northern hemisphere summer at 18,000 years BP and this has provided the boundary conditions for global general circulation models to simulate the climate when the northern ice sheets were at their maximum extent (see Lockwood, 1983a).
11. Fast albedo feedbacks are too weak to change global temperature significantly without global mean radiative forcing.
12. We used reconstructions of ice sheets and compositions in ice cores to derive the albedo and greenhouse forcing of the LGM at zero solar mean forcing.
13. The UK Department of Environment (1979a) suggests the effect of ozone depletion on surface temperature would be barely detectable, while Reck (1976) suggests that the surface temperature would change by between -0.6 C and + 0.8 C, the sign depending upon the underlying surface albedo and the presence or absence of clouds and particulate pollution layers (warming when aerosol hazes are present, cooling when not present).