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Structure of Convective Turbulence and Turbulent Fluxes over Complex Terrain during VERTIKATOR Ch. Kottmeier, M. Hasel, U. Corsmeier, N. Kalthoff Institut für Meteorologie und Klimaforschung, Universität Karlsruhe.
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Structure of Convective Turbulence and Turbulent Fluxes over Complex Terrain during VERTIKATOR Ch. Kottmeier, M. Hasel, U. Corsmeier, N. Kalthoff Institut für Meteorologie und Klimaforschung, Universität Karlsruhe Ch. Kottmeier et al., ICAM 2003
Structure of Convective Turbulence and Turbulent Fluxes over Complex Terrain during Vertikator Ch. Kottmeier, M. Hasel, U. Corsmeier, N. Kalthoff Institut für Meteorologie und Klimaforschung, Universität Karlsruhe • Vertical Exchange and Orography • Coordinator: Franz Fiedler, Karlsruhe • 2 Experiments in Alpine and Prealpine Mountains in 2002 • 6 Agencies, 8 Subprojects Ch. Kottmeier et al., ICAM 2003
Convection over mountains such as Black Forest is found most variable Ch. Kottmeier et al., ICAM 2003
KA Hornisgrinde Freudenstadt Convection over mountains such as Black Forest is found most variable Ch. Kottmeier et al., ICAM 2003
Hornisgrinde Murgtal KAMM 1 Simulation (H. Noppel, IMK, 2003) Ch. Kottmeier et al., ICAM 2003
Convection over mountains such as Black Forest controlled by: • all factors affecting local surface heating • induced mesoscale flows KAMM Model Simulation H. Noppel, 2003 Ch. Kottmeier et al., ICAM 2003
Convection over mountains such as Black Forest controlled by: • all factors affecting local surface heating • induced mesoscale flows • synoptic scale flow and orographic flow interaction Alps Ch. Kottmeier et al., ICAM 2003
thermo/hydro control deeply potentially unstable | | deep convection mesoscale circulations/ lifting inversions present | | | forced lifting shallow convection inhibiting factors: weak surface heating no convection dynamical control weak ---------------- synoptic flow ------- strong Ch. Kottmeier et al., ICAM 2003
Questions adressed • Heating and height of the mountaineous convective layer • Structure of convective turbulence Ch. Kottmeier et al., ICAM 2003
14 Ground stations • 2 radiosondes • 1 tethered balloon • 1 Radar-RASS • 2 SODARs • 1 Aerosol-LIDAR • 2 surface energy balance stations • 4 turbulence measurements • 5 aircraft • flight pattern of DO-128, D-IBUF Ch. Kottmeier et al., ICAM 2003
sawpattern flights of RF5 + 2-hourly radiosondes to get boundary layer heights Ch. Kottmeier et al., ICAM 2003
Mixing heights from T und q Ch. Kottmeier et al., ICAM 2003
Height of convectively mixed layer previous (glider record) day: hmix differs by 1200 m h differs by 1000 m Ch. Kottmeier et al., ICAM 2003
Height of convectively mixed layer morning flight: hmix differs by 2000 m h differs by 1000 m previous (glider record) day: hmix differs by 1200 m h differs by 1000 m Ch. Kottmeier et al., ICAM 2003
Height of convectively mixed layer afternoon flight: hmix differs by 1800 m morning flight: hmix differs by 2000 m h differs by 1000 m previous (glider record) day: hmix differs by 1200 m h differs by 1000 m Ch. Kottmeier et al., ICAM 2003
Turbulent heat fluxes above flight sections at different heights, morning flight Ch. Kottmeier et al., ICAM 2003
Turbulent heat fluxes above flight sections at different heights, afternoon flight Ch. Kottmeier et al., ICAM 2003
Turbulent latent heat fluxes above flight sections at different heights, afternoon flight Ch. Kottmeier et al., ICAM 2003
Selection of thermals, lead series:w‘ Ch. Kottmeier et al., ICAM 2003
2000 m MSL Total numbers of classified up- and downdrafts, afternoon flight 1000 m MSL Ch. Kottmeier et al., ICAM 2003
z/zi = 0.2 Composite structure of thermals and contribution to covariances (fluxes of heat and moisture) Ch. Kottmeier et al., ICAM 2003
z/zi = 0.54 z/zi = 0.2 Composite structure of thermals and contribution to covariances (fluxes of heat and moisture) Ch. Kottmeier et al., ICAM 2003
Wachstum der Murgtalzelle 1 June 19, 2002, afternoon: Cell development observed by Radar and aircraft data. (I. Bertram, IMK, 2002) Ch. Kottmeier et al., ICAM 2003 ulrich.corsmeier@imk.fzk.de