Td. Sikora et Gs. Young, OBSERVATIONS AND APPLICATIONS OF THE HORIZONTAL PERTURBATION WIND-FIELD WITHIN CONVECTIVE STRUCTURES OF THE MARINE ATMOSPHERIC SURFACE-LAYER, Boundary - layer meteorology, 68(4), 1994, pp. 419-426
Studies involving radar remote sensing or modeling of the ocean/Marine
Atmospheric Surface Layer (MASL) interface demand a thorough descript
ion of how coherent convective structures couple the two mediums toget
her. The current analysis provides this information for the small-scal
e variability caused by boundary-layer convection. NCAR Electra 50 m a
bove mean sea level (MSL) turbulence data from Project FIRE (First ISS
CP [International Satellite Cloud Climatology Program] Regional Experi
ment) are conditionally sampled and composited to produce horizontal p
lanviews of the typical perturbation horizontal wind field within thes
e convective updrafts and downdrafts. Applications of these observatio
nal results, as well as similarly derived flux data from Sikora and Yo
ung (1993), to the above mentioned studies, are then discussed.