Other Names
ClONO2, ClNO3
Definition
Chlorine Nitrate (ClONO2) is of importance as a
reservoir species (more abundant stable compound) for reactive chlorine and
nitrogen in the lower and middle stratosphere.
It is formed in the molecular reaction of ClO with NO2 and is destroyed via
photolysis by near-UV solar radiation. ClONO2 reacts rapidly with HCl on polar stratospheric
clouds and aerosol particles during polar night and provides active chlorine, which depletes local ozone.
Applications
(1)
Atmospheric Chemistry Models |
(3)
Polar Atmospheric Processes |
(2)
Monitoring of Ozone Layer |
(4)
Tropospheric-Stratospheric Exchanges |
GES DISC Datasets