- Last updated
- July 16, 2020
- Terms of use
-
- Organization
- EnviDat: the Environmental Data Portal
- Categories
- Education, culture and sport
Description
Earth’s snow cover is very dynamic on diurnal time scales. The changes to the snow structure during this metamorphism have wide ranging impacts such as on avalanche formation and on the capacity of surface snow to exchange trace gases with the atmosphere. Here, we investigate the influence of dry metamorphism, which involves fluxes of water vapor, on the chemical reactivity of bromide in the snow. For this, the heterogeneous reactive loss of ozone at a concentration of 5-6E12 molecules cm-3 is investigated in artificial, shock-frozen snow samples doped with 6.2 uM sodium bromide and with varying metamorphism history. The oxidation of bromide in snow is one reaction initiating polar bromine releases and ozone depletions.
Resources
- SERVICE data list
- PDF Readme file
- SERVICE Ozone data
- SERVICE Matlab Script to view and plot data
- SERVICE Matlab Data
- SERVICE Data Figure 1
- SERVICE Acetone data
Additional information
- Identifier
- b6633dad-a0a5-497e-b393-d7c6ee018c0a@envidat
- Issued date
- February 20, 2020
- Modified date
- July 16, 2020
- Publisher
- EnviDat
- Contact points
- Languages
- English
- Further information
- -
- Landing page
- https://www.envidat.ch/#/metadata/labchemistrymetamorphism
- Documentation
-
- Temporal coverage
- -
- Spatial coverage
- -
- Update interval
- -
- Metadata Access
- API (JSON) Download XML
