A model is presented explaining changes in cometary brightness during
an outburst at large heliocentric distances. It is shown that a combin
ation of the following effects can explain the main characteristics of
outburst at large heliocentric distances: the specific exothermic pro
cesses in cometary nucleus (as the HCN polymerisation and the crystall
ization of the water amorphous ice, connected with the ejection of the
large quantities of dust) and the sublimation of CO or CO2 from the c
omet's nucleus. The obtained results are in good agreement with observ
ations.