While the dynamics of snowpack ozone and surface layer ozone should be correlated, the complex dynamical processes are not yet clearly identifiable. Nonetheless, these analyses showed that (a) snowpack ozone is depleted by either photochemical and/or physical processes and (b) atmospheric ozone above the snow surface possibly results from the peroxy-nitrogen cycle.At the elevation of about 3208 m, the study area, named the Summit Environmental Observatory (a.k.a. Summit) (Figure II-1), is located in central Greenland (72.34AdN, 38.29AdW) and is within the dry-snow zone, which means that no melting ofanbsp;...
|Title||:||Surface Layer Ozone Dynamics and Air-snow Interactions at Summit, Greenland. Spring and Summer Ozone Exchange Velocity and Snowpack Ozone: The Complex Interactions|
|Publisher||:||ProQuest - 2007|