Stable Boundary Layer Characteristics during Morning Transition Observed with a Tethered Lifting System during Perdigão 2017

In the spring of 2017, the Perdigão Program instrumented a unique, parallel ridge mountain in Perdigão, Portugal in unprecedented spatial and temporal resolution using traditional tower mounted sensors, instrumented aerial platforms, and remote sensing instrumentation. One of the unique aspects of Perdigão is that measurements of turbulence in the atmospheric boundary layer were not limited to ground based towers which typically restrict the phenomena that can be sampled, including low level jets, rotors, and entrainment. During Perdigão, the Army Research Laboratory and University of Colorado operated a Tethered Lifting System (TLS) equipped with an instrumentation package that includes a hot-wire anemometer and cold-wire to measure velocity and temperature fluctuations at 1 KHz, and temperature, pressure, humidity and wind speed measurements at lower frequencies for dynamic calibration of the hot-wire/cold-wire. Each TLS performed over 100 profiles of the atmospheric boundary layer during diverse background meteorological conditions which provided the unique opportunity to characterize the turbulent structure of the boundary layer.

Several TLS operations were conducted to sample boundary layer evolution during morning transition. Mean boundary layer characteristics are estimated through the morning transition relative to local sunrise. Regimes based on mean boundary layer wind direction will be created to evaluate how land surface heterogeneities upstream impact boundary layer characteristics.