A theoretical framework for conditionally unstable flows over a mountain ridge is provided by means of numerical simulations performed with a cloud-resolving model. Three nondimensional parameters are identified, which explain most of the solution features. The role of wind shear is also addressed.
Idealized simulations of conditionally unstable flows over a mountain ridge
2015
Abstract
A theoretical framework for conditionally unstable flows over a mountain ridge is provided by means of numerical simulations performed with a cloud-resolving model. Three nondimensional parameters are identified, which explain most of the solution features. The role of wind shear is also addressed.File in questo prodotto:
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