Insolation and earth's orbital periods

Details Insolation and earth's orbital periods Insolation and earth's orbital periods

Jun 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993jgr....9810341b&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 98, no. D6, p. 10,341-10,362.

Physics

32

Insolation, Orbital Velocity, Solar Orbits, Solar Radiation, Irradiance, Solstices

Scientific paper

Three kinds of insolation are computed both analytically and numerically: (1) the instantaneous insolation (irradiance) at noon, (2) the daily irradiation, and (3) the irradiations received during particular time intervals of the day defined by two constant values of the zenith distance (diurnal irradiations). Also computed are mean irradiances (irradiations divided by the length of the time interval over which they are calculated) for different time intervals (e.g. the interval between sunrise and sunset). Examples of these insolations are given for the equinoxes and the solstices.

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