𝔖 Bobbio Scriptorium
✦   LIBER   ✦

A verification of an analytical formula for estimating the height of the stable internal boundary layer

✍ Scribed by S. A. Hsu


Publisher
Springer
Year
1989
Tongue
English
Weight
219 KB
Volume
48
Category
Article
ISSN
0006-8314

No coin nor oath required. For personal study only.


πŸ“œ SIMILAR VOLUMES


An examination of methods to estimate th
✍ Akula Venkatram πŸ“‚ Article πŸ“… 1986 πŸ› Springer 🌐 English βš– 446 KB

This paper examines the assumptions and derivations that govern commonly used methods of estimating the height of the thermal internal boundary layer (TIBL) that occurs near shorelines. We show that nearly all these methods require inputs that can be defined only in the very limited context of the d

A model for the height of the internal b
✍ Sven-Erik Gryning; Ekaterina Batchvarova πŸ“‚ Article πŸ“… 1996 πŸ› Springer 🌐 English βš– 760 KB

A model for the time and space variation of the internal boundary-layer height over a land area with an irregular coastline is presented. It is based on the analytical model of the boundary-layer height proposed by Gryning and Batchvarova (1990) and Batchvarova and Gryning (199 1). The model account

Comments on deriving the equilibrium hei
✍ G. J. Steeneveld; B. J. H. van de Wiel; A. A. M. Holtslag πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 98 KB

## Abstract Recently, the equilibrium height of the stable boundary layer received much attention in a series of papers by Zilitinkevich and co‐workers. In these studies the stable boundary‐layer height is derived in terms of inverse interpolation of different boundary‐layer height scales, each rep

Analytical model for the growth of the c
✍ Sven-Erik Gryning; Ekaterina Batchvarova πŸ“‚ Article πŸ“… 1990 πŸ› John Wiley and Sons 🌐 English βš– 868 KB

## Abstract A model of near‐neutral and convective steady‐state internal boundary layer evolution is presented. the model deals with the internal boundary layer that forms over land in coastal and lake areas during onshore winds. Near the ground, the growth of the internal boundary layer is control