TY - JOUR
T1 - Interaction between atmospheric flows and obstacles
T2 - Experiments in a rotating channel
AU - Alessio, S.
AU - Briatore, L.
AU - Ferrero, E.
AU - Longhetto, A.
AU - Giraud, C.
AU - Morra, O.
PY - 1992/8
Y1 - 1992/8
N2 - We performed an experimental study using scale models in a hydrodynamic rotating channel, concerning the interactions between fluid flows and obstacles of different shapes. The study was meant to analyze the characteristics of the wakes observed on the lee side of quasi-bidimensional obstacles, in a neutral atmosphere. The obstacles were half-cylinders (with aspect ratio 0.87), placed transversally on the channel bottom and totally submerged in the fluid. We call them "quasi-bidimensional" since their width was a little smaller than the channel width, thus allowing the flow to partially go round their edges. The simulations were performed in the rotating hydraulic channel of ICG-CNR in Turin, and included various conditions of rotation period and flow speed. An interesting behaviour of the wakes was found on the lee side of subsynoptic-scale obstacles, modelled in conditions of Reynolds-Rossby similitude. More precisely, if a given threshold of flow velocity is exceeded, wake size is constant and is fully determined by the height of the obstacle.
AB - We performed an experimental study using scale models in a hydrodynamic rotating channel, concerning the interactions between fluid flows and obstacles of different shapes. The study was meant to analyze the characteristics of the wakes observed on the lee side of quasi-bidimensional obstacles, in a neutral atmosphere. The obstacles were half-cylinders (with aspect ratio 0.87), placed transversally on the channel bottom and totally submerged in the fluid. We call them "quasi-bidimensional" since their width was a little smaller than the channel width, thus allowing the flow to partially go round their edges. The simulations were performed in the rotating hydraulic channel of ICG-CNR in Turin, and included various conditions of rotation period and flow speed. An interesting behaviour of the wakes was found on the lee side of subsynoptic-scale obstacles, modelled in conditions of Reynolds-Rossby similitude. More precisely, if a given threshold of flow velocity is exceeded, wake size is constant and is fully determined by the height of the obstacle.
UR - http://www.scopus.com/inward/record.url?scp=0027008840&partnerID=8YFLogxK
U2 - 10.1007/BF00119377
DO - 10.1007/BF00119377
M3 - Article
SN - 0006-8314
VL - 60
SP - 235
EP - 241
JO - Boundary-Layer Meteorology
JF - Boundary-Layer Meteorology
IS - 3
ER -