Iqbal 1983 An Introduction To Solar Radiation Rapidshare

Iqbal 1983 An Introduction To Solar Radiation Rapidshare ===== https://urluss.com/2taAOT

The results of the estimation of the solar radiation components for the different sites during the period 2001 - 2010 are presented in Table 1. In this Table, the different solar radiation components are defined, and the models that were used to estimate them are indicated. Table 1. Values of the estimated solar radiation components.

Table 1: Values of the estimated solar radiation components.

Solar radiation components

Eta

Insolation

(W m−2)

Temporal variance (W m−2)

(W m−2)

Temporal variance (W m−2)

(W m−2)

Temporal variance (W m−2)

I0.9

W m−2

The estimated I0.9 is lower than the I0.9 estimated by the case study of the Beaufort d’Hèra d’Oran (BO) station. However, this is due to the specific conditions of the BO station which is located within the piedmont of the Algerian Plateau, which is characterized by a high altitude, a clear climate, and a very low air density. Indeed, the BO station is located in the western part of the Algerian Plateau at an altitude of 1,400 meters. As the meteorological station is located at a height of 1,800 meters, the influence of the local meteorological conditions of the Algerian Plateau decreases with the altitude of the station. Consequently, the BO station is located in a favorable environment for solar radiation estimation, and the data for the period 2001 to 2010 were selected. The data for the other sites are observed at a height of 1,000 m, where the influence of the local meteorological conditions is also the lowest.

The I0.9 component is defined as the total solar radiation reaching the ground within 1° of latitude [35, 39]. It is the main component of the radiation reaching the ground and, consequently, the most important for agriculture. It is estimated by the [14] and [1] models.

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