Presently
visiting NCAR/MMM, Boulder CO
Little is known at
present concerning the turbulence structure and the associated exchange
processes in highly complex terrain. In fact, what we essentially know
concerning the turbulence structure in, e.g., an Alpine valley, is that
commonly used approaches in boundary layer meteorology such as the validity of
scaling regimes cannot be expected to hold due to the violation of essentially all
prerequisites leading to their derivation. Nevertheless, and due to a lack of
better knowledge, numerical models of essentially all spatial resolutions
employ in one way or another boundary layer transfer schemes based on
idealized, flat and horizontally homogeneous conditions.
Therefore, during
the Special Observing Period (SOP) of the Mesoscale Alpine Programme (MAP)
boundary layer processes in highly complex topography were investigated in the Riviera
valley in southern Switzerland. In contrast to previous studies the main
focus was thereby on the turbulence structure and turbulent exchange
processes at the valley surfaces and with respect to the free troposphere. Due
to the anticipated spatial inhomogeneity a large number of turbulence probes
(sonic anemometers, fast-response hygrometers and scintillometers) were
deployed on a cross-section through the valley. Also a light research aircraft
with high temporal sampling resolution flew various patterns within the valley
to yield information on the turbulence structure within the bulk of the valley.
Additional instrumentation such as a radio acoustic sounding system, a
passive-microwave temperature profiler and a tethered balloon were operated
during selected periods. In this seminar, a short overview is given on the
measurements and observational strategies, as well as on specific problems
related to turbulence observations in highly complex terrain. Then, some
research highlights from the ongoing data analysis and numerical modeling are
presented and discussed.