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Incident solar radiation
at different
geographical latitudes

 

 

 

 

 

 

   

Sunīs Altitude Emden

 

alti-01.gif
S = Summer, 21.6.; hS= 90° - phi.gif + 23,45° = 60,067°   **

E = Equinox, 21.3., 23.9.; hE = 90° - phi.gif = 36,617°   **

W = Winter, 22.12., hW = 90° - phi.gif - 23,45° = 13,167°   **

phi.gif = 53,383°, Geographical latitude, Emden

N = North Pole

E = Equator

H = Horizon

SO = incident solar radiation

delta.gif = Declination = 23,45°

h = Sunīs altitude

** = 12 oīclock real solar time

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Sunīs Altitude Coxīs Bazar

 

alti-02.gif
S = Summer, 21.6.; hS= 90° - phi.gif + 23,45° = 92,032°   **

E = Equinox, 21.3., 23.9.; hE = 90° - phi.gif = 68,583°   **

W = Winter, 22.12., hW = 90° - phi.gif - 23,45° = 45,133°   **

phi.gif = 21,417°, Geographical latitude, Coxīs Bazar

N = North Pole

E = Equator

H = Horizon

SO = incident solar radiation

delta.gif = Declination = 23,45°

h = Sunīs altitude

** = 12 oīclock real solar time

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Sunīs Altitude Equator

 

alti-03.gif
S = Summer, 21.6.; hS= 90° - phi.gif + 23,45° = 113,45°   **

E = Equinox, 21.3., 23.9.; hE = 90° - phi.gif = 90°   **

W = Winter, 22.12., hW = 90° - phi.gif - 23,45° = 66,55°   **

phi.gif = 0°, Geographical latitude, Equator

N = North Pole

E = Equator

H = Horizon

SO = incident solar radiation

delta.gif = Declination = 23,45°

h = Sunīs altitude

** = 12 oīclock real solar time

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© K. H. Weiler   (June 10th, 2002)