On statistics of the free-troposphere synoptic component: An evaluation of skewnesses and mixed third-order moments contribution to the synoptic-scale dynamics and fluxes of heat and humidity

dc.bibliographicCitation.firstPage11eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.volume60 Aeng
dc.contributor.authorPetoukhov, V.
dc.contributor.authorEliseev, A.V.
dc.contributor.authorKlein, R.
dc.contributor.authorOesterle, H.
dc.date.accessioned2020-08-03T06:36:52Z
dc.date.available2020-08-03T06:36:52Z
dc.date.issued2008
dc.description.abstractBased on the ERA40 data for 1976-2002 we calculated skewnesses and mixed third-order statistical moments (TOMs) for the synoptic variations [with (2.5-6) d timescales]of horizontal winds, temperature, vertical velocity and the specific humidity in Eulerian coordinates. All these variables show skewnesses which markedly deviate from zero, basically at the entries and the outlets of the mid-latitude storm tracks. In these regions, high values of skewness for vertical velocity, temperature and the specific humidity are revealed throughout the entire free troposphere, while the marked skewnesses for horizontal winds are traced in the lower free troposphere. We found a notable deviation of the synoptic-component statistics from the Gaussian statistics. We also made an estimate of the contribution from TOMs to the prognostic equations for the synoptic-scale kinetic energy and the meridional fluxes of sensible and latent heat, which appeared to be non-negligible, mainly in the storm tracks in winter. Our analysis attests that the most pronounced contribution of TOMs to the aforementioned equations comes from the self-advection by the horizontal synoptic-scale motions, while the TOMs induced by the metric terms in the original equations, and specifically the TOMs associated with the vertical self-advection by the synoptic-scale motions, are much less important.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5339
dc.identifier.urihttps://doi.org/10.34657/3968
dc.language.isoengeng
dc.publisherAbingdon : Taylor and Francis Ltd.eng
dc.relation.doihttps://doi.org/10.1111/j.1600-0870.2007.00276.x
dc.relation.ispartofseriesTellus, Series A: Dynamic Meteorology and Oceanography 60 A (2008), Nr. 1eng
dc.relation.issn0280-6495
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectadvectioneng
dc.subjectEulerian analysiseng
dc.subjectGaussian methodeng
dc.subjecthumidityeng
dc.subjectkinetic energyeng
dc.subjectlatent heat fluxeng
dc.subjectsensible heat fluxeng
dc.subjectskewnesseng
dc.subjectstorm trackeng
dc.subjectsynoptic meteorologyeng
dc.subjecttroposphereeng
dc.subject.ddc550eng
dc.titleOn statistics of the free-troposphere synoptic component: An evaluation of skewnesses and mixed third-order moments contribution to the synoptic-scale dynamics and fluxes of heat and humidityeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus, Series A: Dynamic Meteorology and Oceanographyeng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 2 of 2
Loading...
Thumbnail Image
Name:
Petoukhov et al 2008, On statistics of the free-troposphere synoptic component.pdf
Size:
5.52 MB
Format:
Adobe Portable Document Format
Description:
Loading...
Thumbnail Image
Name:
Petoukhov et al 2008, Lizenz.PNG
Size:
138.5 KB
Format:
Item-specific license agreed upon to submission
Description: