Long-term trends of synoptic-scale breaking Rossby waves in the northern hemisphere between 1958 and 2001
dc.contributor.author
Isotta, Francesco
dc.contributor.author
Martius, Olivia
dc.contributor.author
Sprenger, Michael
dc.contributor.author
Schwierz, Cornelia
dc.date.accessioned
2024-09-19T11:46:15Z
dc.date.available
2024-09-19T11:37:42Z
dc.date.available
2024-09-19T11:46:15Z
dc.date.issued
2008-10
dc.identifier.issn
0899-8418
dc.identifier.issn
1097-0088
dc.identifier.other
10.1002/joc.1647
en_US
dc.identifier.uri
http://hdl.handle.net/20.500.11850/694973
dc.description.abstract
Breaking synoptic-scale Rossby waves are frequent features of the upper troposphere and lower stratosphere (UTLS) which affect both global- and regional-scale dynamics. Furthermore, they directly influence ozone distribution through meridional transport of ozone-rich air towards the south and ozone-poor air towards the north. Here, trends in the frequency of these breaking waves are assessed by analysing a 44-year climatology (1958–2002) of potential vorticity (PV) streamers on isentropic surfaces from 310 to 350 K. These streamers are viewed as breaking Rossby waves, whereby stratospheric (tropospheric) streamers indicate southward (northward) breaking waves. Two complementary techniques are used to analyse the trends. First, linear trends are computed using the least-squares regression technique. Statistically significant linear trends are found to vary in location and magnitude between isentropic levels and the four seasons. In winter significant trends are detected in the eastern Pacific between 340 and 350 K. A positive trend of stratospheric streamers in the Tropics is related to an increase of total column ozone, whereas the positive trend of tropospheric streamers in the mid-latitudes is associated with a decrease of total ozone. Secondly, a nonlinear trend analysis is performed using the seasonal-trend decomposition procedure based on Loess (STL). With this technique, the low-frequency variability of the time series is analysed during the 44-year period. For instance, over the eastern Atlantic on 350 K, a phase of decreasing PV streamer frequencies in the 1950s and 1960s is followed by a positive streamer tendency after the 1970s. Additionally, trends of the zonal wind are investigated. One prominent outcome of this analysis is the observation that equatorial easterlies over the Atlantic are weakening. A dynamically meaningful link exists between the trends observed in both wind velocity and PV streamers.
en_US
dc.language.iso
en
en_US
dc.publisher
Wiley
en_US
dc.subject
potential vorticity
en_US
dc.subject
streamer
en_US
dc.subject
trend
en_US
dc.subject
ozone
en_US
dc.subject
wind velocity
en_US
dc.subject
seasonal-trend decomposition
en_US
dc.subject
breaking Rossby waves
en_US
dc.title
Long-term trends of synoptic-scale breaking Rossby waves in the northern hemisphere between 1958 and 2001
en_US
dc.type
Journal Article
dc.date.published
2008-01-16
ethz.journal.title
International Journal of Climatology
ethz.journal.volume
28
en_US
ethz.journal.issue
12
en_US
ethz.journal.abbreviated
Int. j. climatol.
ethz.pages.start
1551
en_US
ethz.pages.end
1562
en_US
ethz.publication.place
Chichester
ethz.publication.status
published
en_US
ethz.leitzahl
03203 - Davies, Huw Cathan
en_US
ethz.leitzahl.certified
03203 - Davies, Huw Cathan
ethz.date.deposited
2017-06-08T17:57:26Z
ethz.source
ECIT
ethz.identifier.importid
imp59364bbc3f9b160874
ethz.identifier.importid
imp59364c33c138835795
ethz.ecitpid
pub:18509
ethz.ecitpid
pub:25409
ethz.eth
yes
en_US
ethz.availability
Metadata only
en_US
ethz.rosetta.installDate
2024-09-19T11:37:44Z
ethz.rosetta.lastUpdated
2024-09-19T11:37:44Z
ethz.rosetta.exportRequired
true
ethz.rosetta.versionExported
true
dc.identifier.olduri
http://hdl.handle.net/20.500.11850/7885
dc.identifier.olduri
http://hdl.handle.net/20.500.11850/162014
ethz.COinS
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