gesjGEOGRAPHY, ENVIRONMENT, SUSTAINABILITYGEOGRAPHY, ENVIRONMENT, SUSTAINABILITY2071-93882542-1565Russian Geographical Society10.24057/2071-9388-2010-3-1-16-24gesj-262Research ArticleGEOGRAPHYГеографияCLIMATOLOGY OF THE BRUNT-VÄISÄLÄ FREQUENCY OVER MILAN, ITALYGrandoniGiovanniMammarellaMaria CristinaFavaronMauriziomafavaron@mac.com201001032010311624Copyright © Grandoni G., Mammarella M., Favaron M., 20102010Grandoni G., Mammarella M., Favaron M.Grandoni G., Mammarella M., Favaron M.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://ges.rgo.ru/jour/article/view/262Brunt-Vaisala frequencyfree atmospherestatic stabilityReferencesEsau I.N., Zilitinkevich S.S. (2006) Universal dependences between turbulent and meanEsau I.N., Zilitinkevich S.S. (2006) Universal dependences between turbulent and meanflow parameters in stably and neutrally stratified planetary boundary layers. Nonlinearflow parameters in stably and neutrally stratified planetary boundary layers. NonlinearProcesses in Geophysics, 13, 135–144Processes in Geophysics, 13, 135–144Holton J.R. (2004) An introduction to Dynamic Meteorology, 4th edition, Elsevier AcademicHolton J.R. (2004) An introduction to Dynamic Meteorology, 4th edition, Elsevier AcademicPress, Burlington MA, 535 pp.Press, Burlington MA, 535 pp.Hutchinson M.F. (1986) ALGORITHM 642: a fast procedure for calculating minimum cross-validationHutchinson M.F. (1986) ALGORITHM 642: a fast procedure for calculating minimum cross-validationcubic smoothing splines, ACM Transactions on Mathematical Software, 12, 2, 150–153cubic smoothing splines, ACM Transactions on Mathematical Software, 12, 2, 150–153Jacobson M. (2005) Fundamentals of Atmospheric Modeling, 2nd edition, CambridgeJacobson M. (2005) Fundamentals of Atmospheric Modeling, 2nd edition, CambridgeUniversity Press, Cambridge, 813 pp.University Press, Cambridge, 813 pp.R Development Core Team (2008) R: A Language and Environment for StatisticalR Development Core Team (2008) R: A Language and Environment for StatisticalComputing, R Foundation for Statistical Computing, Vienna, Austria. ISBN 3-900051-07-0,Computing, R Foundation for Statistical Computing, Vienna, Austria. ISBN 3-900051-07-0,URL http://www.R-project.orgURL http://www.R-project.orgSozzi R., Georgiadis T., Valentini M. (2002) Introduzione alla Turbolenza Atmosferica,Sozzi R., Georgiadis T., Valentini M. (2002) Introduzione alla Turbolenza Atmosferica,Pitagora Editrice, Bologna, 525 pp.Pitagora Editrice, Bologna, 525 pp.Stull R.B. (1988) An Introduction to Boundary Layer Meteorology, Kluwer AcademicStull R.B. (1988) An Introduction to Boundary Layer Meteorology, Kluwer AcademicPublishers, Dordrecht, 670 pp.Publishers, Dordrecht, 670 pp.Zilitinkevich S.S., Baklanov A. (2002) Calculation of the height of the stable boundary layerZilitinkevich S.S., Baklanov A. (2002) Calculation of the height of the stable boundary layerin practical applications, Boundary Layer Meteorology, 105, 389–409in practical applications, Boundary Layer Meteorology, 105, 389–409Zilitinkevich S.S., Esau I.N. (2003) The effect of baroclinicity on the equilibrium depth ofZilitinkevich S.S., Esau I.N. (2003) The effect of baroclinicity on the equilibrium depth ofneutral and stable planetary boundary layers, Q. J. R. Meteorol. Soc., 129, 3339–3356neutral and stable planetary boundary layers, Q. J. R. Meteorol. Soc., 129, 3339–3356Zilitinkevich S.S., Esau I.N., Baklanov A. (2007) Further comments on the equilibrium heightZilitinkevich S.S., Esau I.N., Baklanov A. (2007) Further comments on the equilibrium heightof neutral and stable planetary boundary layers. Quart. J. Roy. Met. Soc., 133, 265–271.of neutral and stable planetary boundary layers. Quart. J. Roy. Met. Soc., 133, 265–271.
The authors declare that there are no conflicts of interest present.