Observations of the Australian summertime cool change have ranged over both the subsynoptic scale (200-2000 km) and the mesoscale (20-200 km). In this paper, the final in a series of three, a conceptual subsynoptic and mesoscale model is developed. -from Authors
CITATION STYLE
Ryan, B. F., & Wilson, K. J. (1985). The Australian summertime cool change. Part III: subsynoptic and mesoscale model. Monthly Weather Review, 113(2), 224–240. https://doi.org/10.1175/1520-0493(1985)113<0224:TASCCP>2.0.CO;2
Mendeley helps you to discover research relevant for your work.