A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models

Abstract The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weather prediction (NWP) models. The Swiss Plateau experiences many days with FLS in winter. Most NWP models employ terrain‐following vertical coordinates. As a consequence, the typically flat cloud top is...

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Main Authors: Stephanie Westerhuis, Oliver Fuhrer
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2021-08-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
fog
Online Access:https://doi.org/10.1029/2020MS002437
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spelling doaj-b412d4f3dd5a4765b7fde3f9528b67662021-08-27T14:57:23ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662021-08-01138n/an/a10.1029/2020MS002437A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction ModelsStephanie Westerhuis0Oliver Fuhrer1ETH Zürich Zürich SwitzerlandMeteoSwiss Zürich SwitzerlandAbstract The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weather prediction (NWP) models. The Swiss Plateau experiences many days with FLS in winter. Most NWP models employ terrain‐following vertical coordinates. As a consequence, the typically flat cloud top is intersected by sloping coordinate surfaces above hilly terrain such as the Swiss Plateau. Horizontal advection across the sloping coordinate surfaces leads to spurious numerical diffusion which promotes erroneous FLS dissipation. To address this problem, we propose a new vertical coordinate formulation which features a local smoothing of the model levels. We demonstrate the positive impact of the new vertical coordinate formulation on a case study in detail and for a full month using the COSMO model. The improved vertical coordinate formulation is not yet sufficient to obtain perfect FLS forecasts, it is however a crucial aspect to consider on the way thereto.https://doi.org/10.1029/2020MS002437foglow stratusnumerical weather predictionvertical coordinate formulation
collection DOAJ
language English
format Article
sources DOAJ
author Stephanie Westerhuis
Oliver Fuhrer
spellingShingle Stephanie Westerhuis
Oliver Fuhrer
A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models
Journal of Advances in Modeling Earth Systems
fog
low stratus
numerical weather prediction
vertical coordinate formulation
author_facet Stephanie Westerhuis
Oliver Fuhrer
author_sort Stephanie Westerhuis
title A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models
title_short A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models
title_full A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models
title_fullStr A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models
title_full_unstemmed A Locally Smoothed Terrain‐Following Vertical Coordinate to Improve the Simulation of Fog and Low Stratus in Numerical Weather Prediction Models
title_sort locally smoothed terrain‐following vertical coordinate to improve the simulation of fog and low stratus in numerical weather prediction models
publisher American Geophysical Union (AGU)
series Journal of Advances in Modeling Earth Systems
issn 1942-2466
publishDate 2021-08-01
description Abstract The correct simulation of fog and low stratus (FLS) is a difficult task for numerical weather prediction (NWP) models. The Swiss Plateau experiences many days with FLS in winter. Most NWP models employ terrain‐following vertical coordinates. As a consequence, the typically flat cloud top is intersected by sloping coordinate surfaces above hilly terrain such as the Swiss Plateau. Horizontal advection across the sloping coordinate surfaces leads to spurious numerical diffusion which promotes erroneous FLS dissipation. To address this problem, we propose a new vertical coordinate formulation which features a local smoothing of the model levels. We demonstrate the positive impact of the new vertical coordinate formulation on a case study in detail and for a full month using the COSMO model. The improved vertical coordinate formulation is not yet sufficient to obtain perfect FLS forecasts, it is however a crucial aspect to consider on the way thereto.
topic fog
low stratus
numerical weather prediction
vertical coordinate formulation
url https://doi.org/10.1029/2020MS002437
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