Dozenten: Prof. Dr. T. Leisner, Prof. Dr. P. Braesicke, Prof. Dr. A. Fink, PD Dr. M. Höpfner, Prof. Dr. C. Hoose, Prof. Dr. P. Knippertz, PD Dr. M. Kunz, Prof. Dr. J. Pinto
Veranstaltungskalender
Kolloquium
Transport and mixing in the Arctic UTLS: Lessons learned from in situ tracer measurements on board the M55 Geophysica
Dienstag, 09. Juli 2013, 15:00
KIT Campus Nord, IMK-ASF,
Geb. 435, Raum 2.05
Geb. 435, Raum 2.05
During winter and spring the Arctic stratosphere
is dominated by a stable polar vortex within
which halogen from anthropogenic sources leads to
rapid photochemical processing triggering
substantial loss of polar ozone over the course
of most winters. These processes are facilitated
by the dynamical isolation of the vortex whose
edge represents a transport barrier inhibiting
the exchange with midlatitude air. However, in
the Arctic, wave breaking associated with major
stratospheric warming events episodically
destabilizes the vortex sometimes leading to
large-scale transport of processed vortex air to
midlatitudes and to intrusions of midlatitude air
into the vortex with effects on chemical
composition in both regions. Subsequently
small-scale irreversible mixing determines the
fate of the transported air masses.
Observations of chemical tracers help to
investigate and quantify the transport and mixing
processes in question. In situ measurements of a
suite of long-lived tracers were made with the
University of Wuppertal's HAGAR instrument on
board the M55 Geophysica aircraft in the Arctic
UTLS (up to 20 km altitude) during January
through March 2003 and 2009 (EU campaigns EUPLEX
and RECONCILE). During both these winters the
polar vortex was dynamically very active,
splitting and reforming due to major warming
events. The tracer observations are used along
with simulations by the Lagrangian chemical
transport model CLaMS to analyze both large-scale
isentropic transport and small-scale irreversible
mixing. Furthermore the composition of the
Arctic lowermost stratosphere below the polar
vortex is assessed, quantifying fractions
originating from the vortex, the midlatitude stratosphere, and the troposphere.
Diese Veranstaltung ist Teil der Reihe Karlsruher Meteorologisches Kolloquium
Referent/in
Prof. Dr. C. Michael Volk
Bergische Universität Wuppertal
Prof. for Experimental Atmospheric - FB C - Department of Physics
Prof. Dr. C. Michael Volk
Bergische Universität Wuppertal
Prof. for Experimental Atmospheric - FB C - Department of Physics
Veranstalter
IMK-ASF
Karlsruher Institut für Technologie (KIT)
Eggenstein-Leopoldshafen
E-Mail: sekretariat ∂does-not-exist.imk-asf kit edu
IMK-ASF
Karlsruher Institut für Technologie (KIT)
Eggenstein-Leopoldshafen
E-Mail: sekretariat ∂does-not-exist.imk-asf kit edu
Zielgruppe
Wissenschaftliche Mitarbeitende
Wissenschaftliche Mitarbeitende
Hinweise
"CS" - KIT-Campus Süd (Universität), Gebäude 30.23 (Physikhochhaus), Seminarraum 13/2
"CN" - KIT-Campus Nord (Forschungszentrum), Gebäude 435 (IMK), Raum 2.05
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