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Albedo

Albedo of water surfacesAlbedo depends on the Sun altitude especially over water surface (roughness)90°2%20°45°5°5%12%35%Dependence on the Sun altitude causes well-defined diurnal and annual variations of albedoAnnual variation of albedoMinimal albedo –

Слайды и текст этой презентации

Слайд 1Albedo
The ratio of back-scattered from a surface radiation to the

incident radiation is known as reflectability or albedo of the

surface. This ratio is usually expressed in % or in decimal fractions.


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I

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Iref

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AlbedoThe ratio of back-scattered from a surface radiation to the incident radiation is known as reflectability or

Слайд 2Albedo of water surfaces
Albedo depends on the Sun altitude especially

over water surface
(roughness)

90°
2%
20°
45°

5%
12%
35%
Dependence on the Sun altitude causes well-defined

diurnal and annual variations of albedo

Annual variation of albedo

Minimal albedo – summer
Maximal albedo -- winter

Albedo of water surfacesAlbedo depends on the Sun altitude especially over water surface (roughness)90°2%20°45°5°5%12%35%Dependence on the Sun

Слайд 3Albedo of clouds
Albedo depends on cloud depth
Threshold
Albedo also depends on

cloud form. The largest albedo is at Ac and Sc

clouds. Ac – 73%; Sc – 64%; Cu – 52%

Cloud depth (∆h), albedo (r), and transmission function (P).

Albedo of cloudsAlbedo depends on cloud depthThresholdAlbedo also depends on cloud form. The largest albedo is at

Слайд 4Altocumulus (Ac) http://www.clouds-online.com/index.htm

Description:
Grey cloud bundles, sheds or rollers, compound like rough

fleecy cloud, which are often arranged in banks.

Origin:

By rise of

an expanded air layer at the border of a rising zone.

By convection or turbulence within an unstable layer of the middle cloud level.

By transformation from Altostratus und Nimbostratus at lability or Cumulus and Cumulonimbus at stability.
Altocumulus (Ac)  http://www.clouds-online.com/index.htmDescription:Grey cloud bundles, sheds or rollers, compound like rough fleecy cloud, which are often

Слайд 5Stratocumulus (Sc)
Description:
Cloud plaices, rollers or banks compound dark gray

layer cloud.

Origin:

By turbulence.

By convection in unstable air layers, which

are limited by a strong inversion upward.

By undulation in very damp air layers and usually at inversions.

From other clouds (Nimbostratus, Cumulus, Stratus)
Stratocumulus (Sc) Description: Cloud plaices, rollers or banks compound dark gray layer cloud.Origin:By turbulence. By convection in

Слайд 6Cumulus (Cu)

Description:
Heap cloud with flat basis in the middle

or lower level, whose vertical development reminds of the form

of towers, cauliflower or cotton.

Origin:
The Cumulus always indicates an instability to the layering of air with appropriate convection or turbulence.
Cumulus (Cu) Description: Heap cloud with flat basis in the middle or lower level, whose vertical development

Слайд 7Albedo of clouds
Albedo depends on cloud depth
Albedo also depends on

cloud form. The largest albedo is at Ac and Sc

clouds. Ac – 73%; Sc – 64%; Cu – 52%

Cloud depth (∆h), albedo (r), and transmission function (P).

Albedo of cloudsAlbedo depends on cloud depthAlbedo also depends on cloud form. The largest albedo is at

Слайд 8Dependence of albedo (r), transmission (P), and absorption (A) functions

on the Sun altitude.
Albedo, r%
Transmission function, P%
Absorption function, A%

Albedo of

clouds also depends on Earth’s surface albedo (re). The stronger the re value, the larger the cloud albedo
Dependence of albedo (r), transmission (P), and absorption (A) functions on the Sun altitude.Albedo, r%Transmission function, P%Absorption

Слайд 10Addition to albedo of clouds
Difference between albedo of a separate

cloud r and albedo of a cloud layer rl.

“n” is

cloud amount in decimal fractions, is albedo of cloud free atmosphere at the level of the possible cloud top.
From the experimental data the following formula has been obtained.


Here, rl%, and n in points.
Addition to albedo of cloudsDifference between albedo of a separate cloud r and albedo of a cloud

Слайд 11

The rate of separate cloud albedo, r(n), can be explained

by the fact that, at small cloud cover (n

the distance between clouds is rather big, and separated clouds act in each cloud own way (not interacting with each other).

As amount of clouds increasing, the clouds start interacting. Radiation scattered by a cloud side reaches some other clouds, resulting in increasing of reflection.

The rate of separate cloud albedo, r(n), can be explained by the fact that, at small cloud

Слайд 12Experimental data analysis has shown that albedo of cloud layer

depends only slightly on cloud depth. At n=4…6 points, correlation

coefficient is as low as 0,19±0,1. This fact can be explained in the same way as it was done in previous discussion.
The albedo of clouds can vary significantly as the initial depth is rather small (the cloudiness is thin).
Experimental data analysis has shown that albedo of cloud layer depends only slightly on cloud depth. At

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