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Download e-book for iPad: Medium and High Temperature by Jan F. Kreider

By Jan F. Kreider

ISBN-10: 0124259804

ISBN-13: 9780124259805

ISBN-10: 0323141110

ISBN-13: 9780323141116

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14) w h e r e E T is e x p r e s s e d in minutes. Corrected standard time is standard clock time (not daylight savings time) corrected for differences b e t w e e n the standard meridian for a time zone and the local site m e r i d i a n — corrected standard time = standard clock time (in the 24-h system) + (time zone meridian - local site longitude)/15. 15) The longitude values are m e a s u r e d west of Greenwich and the units of time are h o u r s . 6 and shown graphically by the a n a l e m m a in Fig.

O n e m e t h o d of estimating average hourly, b e a m solar flux if the c o m m o n l y m e a s u r e d daily total (direct plus diffuse) is k n o w n , w a s developed by Collares-Pereira and Rabl (C9). 4767 s'm(h - 60). s s T h e ratio I& /H is the ratio of daily horizontal diffuse to daily horizontal total radiation, on the a v e r a g e , described in the Section V I I I . th VII. A. DAILY h SOLAR RADIATION Daily Extraterrestrial CALCULATIONS Radiation E q u a t i o n ( 2 . 42) Jh (a=Q) sr w h e r e sunrise and sunset times are given by E q .

A. Monthly Extraterrestrial Radiation Instead of using monthly totals of solar flux, the usual prac­ tice is to divide monthly totals by the actual n u m b e r of days in e a c h m o n t h to calculate monthly averaged, daily a m o u n t s usually called " m o n t h l y " for short. 48) can be used to calculate //o,h> the monthly hori­ zontal extraterrestrial radiation from 44 2. x Principles of Solar Radiation and Optics r/is. 48) s w h e r e N is t h e initial d a y n u m b e r for a m o n t h , N is t h e final d a y n u m b e r , dt' = rf/ig/15, a n d t h e declination 8 (A0 is given by E q .

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Medium and High Temperature by Jan F. Kreider


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