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Sökning: WFRF:(Palazzi E.) > (2010-2014) > Probability density...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003878naa a2200349 4500
001oai:research.chalmers.se:92f4a622-981e-490d-9486-7c218063f21b
003SwePub
008171008s2011 | |||||||||||000 ||eng|
024a https://doi.org/10.5194/acp-11-10579-20112 DOI
024a https://research.chalmers.se/publication/1477342 URI
040 a (SwePub)cth
041 a engb eng
042 9 SwePub
072 7a art2 swepub-publicationtype
072 7a ref2 swepub-contenttype
100a Palazzi, E.u Institute of Atmospheric Sciences and Climate, Bologna4 aut
2451 0a Probability density functions of long-lived tracer observations from satellite in the subtropical barrier region: data intercomparison
264 c 2011-10-26
264 1b Copernicus GmbH,c 2011
338 a electronic2 rdacarrier
520 a Past studies have shown that a clear relationship exists between the field of a passive tracer and the Probability Distribution Function (PDF) of tracer concentrations, which can be exploited to identify the position and variability of stratospheric barriers to isentropic mixing.In the present study, we focus on the dynamical barrier located in the subtropics. We calculate PDFs of the long-lived tracers nitrous oxide (N(2)O) and methane (CH(4)) from different satellite instruments: the Microwave Limb Sounder (MLS) on board Aura, the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board Envisat, the Sub-Millimetre Radiometre (SMR) on board Odin and the Halogen Occultation Experiment (HALOE) on board UARS, overall covering the time period of 1992-2009.An analysis of the consistency among the different sets of data and their capability of identifying mixing regions and barrier-to-transport regions in the stratosphere and the subtropical barrier location is a prime aim of the present study. This is done looking at the morphological structure of the one-and two-dimensional PDFs of tracer concentrations measured by the different instruments. The latter differ in their spatial and temporal sampling and resolution, and there are some systematic differences in the determination of the subtropical barrier position that have been highlighted. However, the four satellite instruments offer an overall consistent picture of the subtropical barrier annual cycle. There is a strong seasonality consistently represented, characterized by the wintertime shift of the subtropical edge toward the summer hemisphere. However, the influence of the Quasi Biennial Oscillation (QBO) on isentropic transport and mixing, and by consequence, on the position of the subtropical barrier, is not equally represented in all satellite data using the methodology proposed.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Meteorologi och atmosfärforskning0 (SwePub)105082 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Meteorology and Atmospheric Sciences0 (SwePub)105082 hsv//eng
700a Fierli, F.u Institute of Atmospheric Sciences and Climate, Bologna4 aut
700a Stiller, G. P.u Karlsruher Institut für Technologie (KIT),Karlsruhe Institute of Technology (KIT)4 aut
700a Urban, Joachim,d 1964u Chalmers tekniska högskola,Chalmers University of Technology4 aut0 (Swepub:cth)joaurb
710a Institute of Atmospheric Sciences and Climate, Bolognab Karlsruher Institut für Technologie (KIT)4 org
773t Atmospheric Chemistry and Physicsd : Copernicus GmbHg 11:20, s. 10579-10598q 11:20<10579-10598x 1680-7316x 1680-7324
856u http://publications.lib.chalmers.se/records/fulltext/local_147734.pdfx primaryx freey FULLTEXT
856u https://www.atmos-chem-phys.net/11/10579/2011/acp-11-10579-2011.pdf
8564 8u https://doi.org/10.5194/acp-11-10579-2011
8564 8u https://research.chalmers.se/publication/147734

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