Numerical weather prediction (NWP) is in a period of transition. As resolutions increase, global models are moving towards fully nonhydrostatic dynamical cores, with the local and …
JH Jungclaus, SJ Lorenz, H Schmidt… - Journal of Advances …, 2022 - Wiley Online Library
This work documents the ICON‐Earth System Model (ICON‐ESM V1. 0), the first coupled model based on the ICON (ICOsahedral Non‐hydrostatic) framework with its unstructured …
A Two-Way Nested Global-Regional Dynamical Core on the Cubed-Sphere Grid in: Monthly Weather Review Volume 141 Issue 1 (2013) Jump to Content Jump to Main Navigation …
H Weller - Monthly Weather Review, 2012 - journals.ametsoc.org
Controlling the Computational Modes of the Arbitrarily Structured C Grid in: Monthly Weather Review Volume 140 Issue 10 (2012) Jump to Content Jump to Main Navigation …
TD Ringler, D Jacobsen, M Gunzburger… - Monthly Weather …, 2011 - journals.ametsoc.org
Exploring a Multiresolution Modeling Approach within the Shallow-Water Equations in: Monthly Weather Review Volume 139 Issue 11 (2011) Jump to Content Jump to Main Navigation Logo …
Higher-order finite-volume flux operators for transport algorithms used within Runge–Kutta time integration schemes on irregular Voronoi (hexagonal) meshes are proposed and …
C Liao, T Tesfa, Z Duan, LR Leung - Environmental Modelling & Software, 2020 - Elsevier
Spatial discretization is the cornerstone of all spatially-distributed numerical simulations including watershed hydrology. Traditional square grid spatial discretization has several …
H Weller, J Thuburn, CJ Cotter - Monthly weather review, 2012 - journals.ametsoc.org
Currently, most operational forecasting models use latitude–longitude grids, whose convergence of meridians toward the poles limits parallel scaling. Quasi-uniform grids might …
PA Ullrich, D Devendran… - Monthly Weather …, 2016 - journals.ametsoc.org
Arbitrary-Order Conservative and Consistent Remapping and a Theory of Linear Maps: Part II in: Monthly Weather Review Volume 144 Issue 4 (2016) Jump to Content Jump to Main …