Recent studies have suggested that nitric acid uptake by ice clouds may dec
rease ice evaporation rates and thereby prolong the cloud lifetimes. To les
t this suggestion, ice desorption rates were studied as a function of HNO3
partial pressure (10(-6)-10(-5) Torr), relative humidity (28-92%), and temp
erature (192-204 K) using optical interference of a helium neon laser. Ice
evaporation rates in the presence of 1 x 10(-6) Torr HNO3 were indistinguis
hable from those of pure ice. Ln contrast, ice evaporation in the presence
of 8 x 10(-6) Torr HNO3 resulted in lower evaporation rates by 33% relative
to pure ice. Higher partial pressures of KNO3 result in a supercooled H2O/
HNO3 liquid layer over ice, which may freeze to form a sealed NAT coating.
This causes a lowering of the ice evaporation rate and prolongs the lifetim
e of ice. Ice exposed to lower partial pressures of HNO3 will not form a li
quid layer and will thus evaporate at the same rate as pure ice.