Air Mass (solar Energy) - Accuracy Near The Horizon

Accuracy Near The Horizon

The above approximation overlooks the curvature of the Earth, and is reasonably accurate for values of up to around 75°. A number of refinements have been proposed to more accurately model the path thickness towards the horizon, such as that proposed by Kasten and Young (1989):

(A.2)

A more comprehensive list of such models is provided in the main article Airmass, for various atmospheric models and experimental data sets. At sea level the air mass towards the horizon ( = 90°) is approximately 38.

Modelling the atmosphere as a simple spherical shell provides a reasonable approximation:

(A.3)

where the radius of the Earth = 6371 km, the effective height of the atmosphere ≈ 9 km, and their ratio ≈ 708.

These models are compared in the table below:

Estimates of airmass coefficient
Flat Earth Kasten & Young Spherical shell
degree (A.1) (A.2) (A.3)
1.0 1.0 1.0
60° 2.0 2.0 2.0
70° 2.9 2.9 2.9
75° 3.9 3.8 3.8
80° 5.8 5.6 5.6
85° 11.5 10.3 10.6
88° 28.7 19.4 20.3
90° 37.9 37.6

This implies that for these purposes the atmosphere can be considered to be effectively concentrated into around the bottom 9 km, i.e. essentially all the atmospheric effects are due to the atmospheric mass in the lower half of the Troposphere. This is a useful and simple model when considering the atmospheric effects on solar intensity.

Read more about this topic:  Air Mass (solar Energy)

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