dc.contributor.author |
Braathen, G |
en |
dc.contributor.author |
Rummukainen, M |
en |
dc.contributor.author |
Kyrö, E |
en |
dc.contributor.author |
Schmidt, U |
en |
dc.contributor.author |
Dahlback, A |
en |
dc.contributor.author |
Jørgensen, T |
en |
dc.contributor.author |
Fabian, R |
en |
dc.contributor.author |
Rudakov, V |
en |
dc.contributor.author |
Gil, M |
en |
dc.contributor.author |
Borchers, R |
en |
dc.date.accessioned |
2014-03-01T01:10:20Z |
|
dc.date.available |
2014-03-01T01:10:20Z |
|
dc.date.issued |
1994 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/11368 |
|
dc.subject |
Ozone |
en |
dc.title |
Temporal development of ozone within the Arctic Vortex during the winter of 1991/92 |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1029/93GL02436 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1029/93GL02436 |
en |
heal.publicationDate |
1994 |
en |
heal.abstract |
In this study we address the question of temporal ozone trends on isentropic surfaces within the Arctic polar vortex during EASOE. We have combined ozone sonde data from twelve campaign stations distributed throughout the European sector of the Arctic. The development of ozone at the 425, 475, 550 and 700K levels is presented, using analysed fields of isentropic potential vorticity |
en |
heal.journalName |
Geophysical Research Letters |
en |
dc.identifier.doi |
10.1029/93GL02436 |
en |