ตัวอย่าง albedo

• Effective albedo for gap feeding upper pinch in doublepinch at peak temperature !

• The effect of perceived surface orientation on perceived surface albedo in binocularly viewed scenes.

• This energy balance depends on, among other factors, the planetary albedo.

• At the same time, the albedo differences themselves are likely to be related to differences in surface mineralogy and dust coverage.

• However, it is important to note that the global albedo pattern can change within only a few decades.

• The principal factors influencing soil temperatures are surface albedo and surface cooling.

• The amount of ice and snow is larger when the temperature is lower, so the lower the temperature the higher albedo.

• The figure shows the zonal-mean distribution, so the albedo and thermal inertia have been zonally averaged in the calculation.

• Information on the albedos and densities of those giants showing transits will be obtained.

• The difference in albedo is a factor of y10.

• Balancing the ice-albedo cooling and the greenhouse warming gives rise to two stable climate states.

• These high-albedo zones could be the remnant of sabkha or dusty materials composed of iron oxides, sulphates and other evaporates.

• It represents major gradients in key climatological parameters such as carbon flux, water flux and albedo.

• The planetary albedo is not a constant factor : it depends on the state of the climate itself, through the amount of clouds and ice.

• The red band was the least effective because of the in-uence of soil albedo and image vignetting.