Abstract: Smooth vertical coordinate levels in atmospheric models can considerably reduce numerical errors in the simulation of flow past complex topography. In this paper we propose a new Smooth LEvel VErtical (SLEVE) coordinate formulation with a modified vertical decay of topography, leading to a more uniform level thickness near the ground while preserving the fast transition to smooth levels in the upper atmosphere. Using numerical simulations of flow past complex topography, we demonstrate the feasibility of this approach. As a result, the new formulation allows for generally thinner near-surface levels of almost constant thickness and thus a better resolution of the boundary layer compared to the SLEVE coordinate, while retaining its...
[[abstract]]A fundamental issue for describing gravity-driven flows over general topography is the s...
Summary. — A new approximate analysis is presented for stably stratified flows at low Froude number ...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weather predic...
There are great conceptual advantages in the use of an isentropic vertical coordinate in atmospheric...
Abstract The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weath...
A new vertical remapping scheme is proposed. The scheme is being implemented into a Locally Mass Con...
The primary research goal of CMMAP is to better understand the effect of cloud processes on the glob...
Many numerical weather prediction models employ terrain-following vertical coordinates. As a consequ...
Vita.A numerical model which gives improved vertical resolution in regions of interest by employing ...
In the terrain following coordinate, Gal-Chen and Somerville and other proposed a vertical coordinat...
A new geopotential based vertical coordinate, named View the MathML source, is presented, that treat...
The Louis scheme for calculating the vertical eddy fluxes within the atmospheric surface layer is im...
Even though the basic problem of the terrain-following vertical coordinates has been in a step-by-st...
The height (h) of the stable boundary layer (SBL) is of major importance to understand the relevant ...
[[abstract]]A fundamental issue for describing gravity-driven flows over general topography is the s...
Summary. — A new approximate analysis is presented for stably stratified flows at low Froude number ...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weather predic...
There are great conceptual advantages in the use of an isentropic vertical coordinate in atmospheric...
Abstract The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weath...
A new vertical remapping scheme is proposed. The scheme is being implemented into a Locally Mass Con...
The primary research goal of CMMAP is to better understand the effect of cloud processes on the glob...
Many numerical weather prediction models employ terrain-following vertical coordinates. As a consequ...
Vita.A numerical model which gives improved vertical resolution in regions of interest by employing ...
In the terrain following coordinate, Gal-Chen and Somerville and other proposed a vertical coordinat...
A new geopotential based vertical coordinate, named View the MathML source, is presented, that treat...
The Louis scheme for calculating the vertical eddy fluxes within the atmospheric surface layer is im...
Even though the basic problem of the terrain-following vertical coordinates has been in a step-by-st...
The height (h) of the stable boundary layer (SBL) is of major importance to understand the relevant ...
[[abstract]]A fundamental issue for describing gravity-driven flows over general topography is the s...
Summary. — A new approximate analysis is presented for stably stratified flows at low Froude number ...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...