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Water vapour as an indicator of dynamical processes in the extratropical UTLS inferred from balloon observations Sergey Khaykin (1), A. Lukyanov(1), V.Yushkov.

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Presentation on theme: "Water vapour as an indicator of dynamical processes in the extratropical UTLS inferred from balloon observations Sergey Khaykin (1), A. Lukyanov(1), V.Yushkov."— Presentation transcript:

1 Water vapour as an indicator of dynamical processes in the extratropical UTLS inferred from balloon observations Sergey Khaykin (1), A. Lukyanov(1), V.Yushkov (1), R. Kivi (2), Karpechko (2), M. Maturilli (3) (1) Central Aerological Observatory of Roshydromet, Russian Federation (2) Arctic Research Centre of the Finnish Meteorological Institute, Finland (3) Alfred Wegener Institute for Polar and Marine Research, Germany The Extra-tropical UTLS: observations, concepts and future directions NCAR, Boulder, CO October 19-22, 2009

2 FLASH-B Fluorescent Advanced Stratospheric Hygrometer for Balloon
Central Aerological Observatory of Roshydromet Measurements and Methods FLASH-B Fluorescent Advanced Stratospheric Hygrometer for Balloon FLASH-B is a compact fast response stratospheric hygrometer using Lyman-alpha fluorescence technique for H2O measurements. Range of water vapour measurements Detection limit Response time Integration time Vertical resolution Measurement precision Total uncertainty Height range Weight ppmv 0.1 ppmv 0.2 sec 4 sec ~ 50 m (descent in UTLS) 5.5% <10 % (1σ) 350… 5 mBar 0.5 kg w/out batteries TRACAO trajectory photochemical model [Lukyanov et al., 2003] ECMWF T511L ° x 0.5° data

3 Central Aerological Observatory of Roshydromet
Measurements and Methods FLASH-B measurement locations Ny-Alesund, Norway Sodankyla, Finland Lindenberg, Germany Payerne, Switzerland 2008 Esrange, Sweden 2006, 2007

4 RDF reconstruction of PV field
Water vapour at the edge of Polar vortex 625 K 575 K 530 K 530 K 575 K 625 K RDF reconstruction of PV field

5 Variability of water vapour in the UTLS

6 Hygropause and tropopause Θ-level variations and H2O at hygropause
Climatology of the transition layer Alternative definition of transition layer: the region between thermal tropopause and hygropause. Hygropause and tropopause Θ-level variations and H2O at hygropause

7 Sodankyla 17.02.2004 7-day RDF 330 K Dynamics of the transition layer
lg(H2O) [ppmv] O3 [ppmv] PV [PV unit] 330 K

8 Flux through tropopause x 10-2 [kg/m2/s]
Cross-tropopause flux ( 18 Feb 2004, Sodankyla) Potential temperature of dynamical tropopause (3.5 pvu), [K] 06 UT 12 UT 18 UT Cross tropopause transport: Red – TST, Blue - STT Flux through tropopause x 10-2 [kg/m2/s]

9 Combined H2O/O3/aerosol flight, Sodankyla, 26 January 2009
Water vapour, ozone and aerosol in the LS Combined H2O/O3/aerosol flight, Sodankyla, 26 January 2009

10 Summary Various case studies based on high-resolution in-situ observations were presented. They highlight various dynamical processes influencing LS composition. High-resolution water vapour measurements are of great importance for case studies of UTLS dynamics. Laminated structure of stratospheric WV profile: indicator of vortex dynamics and troposphere-stratosphere exchange A case of STE at the anticyclone’s boundary was shown WV variability at the extratropical hygropause is shown related to vortex dynamics and transport from TTL


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