Physics – Geophysics
Scientific paper
Dec 1967
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1967papge..68..214v&link_type=abstract
Pure and Applied Geophysics PAGEOPH, Volume 68, Issue 1, pp.214-228
Physics
Geophysics
3
Scientific paper
The present paper contains studies of the nocturnal radiation at some Indian Stations (Madras, Waltair, Nagpur, New Delhi and Poona) with the help of the Ångström compensation Pyrgeometer. The technique of measurement is also described briefly. A study of the mean monthly variation of sky radiation during clear as well as all nights has been discussed. A comparitive study of mean monthly values of sky and other nocturnal radiation components at these stations is also presented. Ångström, [4]2) expressed the dependence of sky radiation S—on water vapour pressure e (mm of mercury) at the earth's surface and air temperature T (degrees absolute), near the instrument to be given by S=σ T 4 (0.75 0.32×10-0.069 e ) cal/cm2/min. According to this semi-empirical relationship, the calculated values of sky radiation for clear nights are smaller than the observed values of sky radiation at all the above stations. It is for this reason the authors obtained a new formula with different constants using nine years observed data at all the stations. To investigate the value of the constant, the mean annual observations presented for nine years from clear skies were analysed for correlations between B (black body radiation) verses S (sky radiation), N (net radiation) and E (absolute error) and obtained a good correlation co-efficients 0.90, 1 and 0.98 respectively. The new suggested formula is S=σ T 4 (0.88 0.32×10-0.069 e ) cal/cm2/min, 267° A< T<313° A. It is also verified using with observed data of different years of the stations. The agreement between the computed values with the new formula of sky radiation and observed sky radiation is found to be good.
Ramanadham R.
Viswanadham Y.
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