An analytic solution for time-periodic thermally-driven slope flows

Author(s)
Dino Zardi, Stefano Serafin
Abstract

The article examines the flow generated by time-periodic variations in surface temperature along an infinite slope in an initially unperturbed, stably stratified atmosphere at rest. Uniform boundary conditions at the surface are conducive to an along-slope parallel flow, governed by a periodically reversing local imbalance between along-slope advection and slope-normal fluxes of momentum and heat. It is shown that solutions include both a transient part and a periodic regime and that three different flow regimes may occur. The properties of the solutions in each regime are examined and discussed, outlining novelties with respect to previously known results.

Organisation(s)
Department of Meteorology and Geophysics
External organisation(s)
Università degli Studi di Trento
Journal
Quarterly Journal of the Royal Meteorological Society
Volume
141
Pages
1968-1974
No. of pages
7
ISSN
0035-9009
DOI
https://doi.org/10.1002/qj.2485
Publication date
07-2015
Peer reviewed
Yes
Austrian Fields of Science 2012
105206 Meteorology
Keywords
ASJC Scopus subject areas
Atmospheric Science
Portal url
https://ucrisportal.univie.ac.at/en/publications/an-analytic-solution-for-timeperiodic-thermallydriven-slope-flows(a18c79fb-b347-4b57-9b99-fd9d29943578).html