Wpływ cyrkulacji atmosferycznej na ilość całkowitego promieniowania słonecznego docierającego do powierzchni ziemi w Belsku (1971-2014)

Abstract

This paper analyses the amount of global solar radiation reaching the ground in Belsk, depending on the atmospheric circulation type. The study used daily sums of global solar radiation from 1971–2014 as well as the calendar of circulation types as developed by Lityński. The largest differences in the amount of solar radiation among the particular circulation types occur in the summer. The largest sums of solar radiation are observed during inflows of air masses from S and SW, and the smallest during the inflow from N, NE, and NW. On sunny days, the reduction of the incoming solar radiation is associated with the S and SW directions.