Dernière mise à jour
16 juillet 2020
Conditions d'utilisation
Open use. Must provide the source.

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.

Ressources

Informations complémentaires

Identifier
b6633dad-a0a5-497e-b393-d7c6ee018c0a@envidat
Date de publication
20 février 2020
Date de modification
16 juillet 2020
Editeur
EnviDat
Points de contact
Langues
Anglais
Informations complémentaires
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Landing page
https://www.envidat.ch/#/metadata/labchemistrymetamorphism
Documentation
Couverture temporelle
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Couverture spatiale
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Intervalle d'actualisation
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Accès aux métadonnées
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Thorsten Bartels-Rausch