Convection-Permitting Models: Added Value and Advances in the Representation of Unresolved Physical Processes and Model Uncertainties

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Atmospheric Techniques, Instruments, and Modeling".

Deadline for manuscript submissions: 20 September 2024 | Viewed by 1026

Special Issue Editor


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Guest Editor
Faculty of Physics, Ludwig-Maximilians-Universität München, 80539 Munich, Germany
Interests: cloud-resolving models; convective scale processes; convection organization; cold pools; entrainment/detrainment

Special Issue Information

Dear Colleagues,

Convection-Permitting Models (CPMs) are numerical models designed to simulate the atmosphere using horizontal grid spacings sufficient (1 km < Δx < 4 km) to resolve at least part of the dynamics associated with moist convection. It is consequently possible to operate these models without specifically parameterising deep convection, although shallower cumulus clouds still need to be parameterised. Over the years, it has been demonstrated that CPMs, now used operationally by many national weather forecasting centres across the world, clearly improve the predictability of convection-related processes, such as the initiation and occurrence of deep convection, surface rainfall rates, as well as high-impact weather events. More recently, advances in computational capabilities have even permitted the development of global CPMs as well as CPM-based ensemble forecast systems.

In this special issue of Atmosphere, we invite scientific contributions presenting cutting-edge results that demonstrate the added value of CPMs over coarser resolution models. The main focus of this Special Issue is on the representation and predictability of convective-scale processes, including surface precipitation rates or extreme weather events. We also encourage contributions presenting advances that improve the predictive skills of CPMs, in particular concerning the representation of unresolved physical processes and model uncertainties using, for example, stochastic perturbation schemes.

Dr. Julien Savre
Guest Editor

Manuscript Submission Information

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Keywords

  • convection-permitting models
  • ensemble forecasting
  • convective-scale processes
  • predictability of convection
  • model uncertainties
  • physical parameterizations
  • stochastic perturbations

Published Papers (1 paper)

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Research

15 pages, 5387 KiB  
Article
On the Precursor Environments to Mountain Lee Wave Clouds in Central Iberia under CMIP6 Projections
by Javier Díaz-Fernández, Carlos Calvo-Sancho, Pedro Bolgiani, Juan Jesús González-Alemán, José Ignacio Farrán, Mariano Sastre and María Luisa Martín
Atmosphere 2024, 15(1), 128; https://doi.org/10.3390/atmos15010128 - 20 Jan 2024
Viewed by 721
Abstract
Mountain lee waves present significant hazards to aviation, often inducing turbulence and aircraft icing. The current study focuses on understanding the potential impact of global climate change on the precursor environments to mountain lee wave cloud episodes over central Iberia. We examine the [...] Read more.
Mountain lee waves present significant hazards to aviation, often inducing turbulence and aircraft icing. The current study focuses on understanding the potential impact of global climate change on the precursor environments to mountain lee wave cloud episodes over central Iberia. We examine the suitability of several Global Climate Models (GCMs) from CMIP6 in predicting these environments using the ERA5 reanalysis as a benchmark for performance. The dataset is divided into two periods: historical data (2001–2014) and projections for the SSP5–8.5 future climate scenario (2015–2100). The variations and trends in precursor environments between historical data and future climate scenarios are exposed, with a particular focus on the expansion of the Azores High towards the Iberian Peninsula, resulting in increased zonal winds throughout the Iberian Peninsula in the future. However, the increase in zonal wind is insufficient to modify the wind pattern, so future mountain lee wave cloud events will not vary significantly. The relative humidity trends reveal no significant changes. Moreover, the risk of icing precursor environments connected with mountain lee wave clouds is expected to decrease in the future, due to rising temperatures. Our results highlight that the EC-EARTH3 GCM reveals the closest alignment with ERA5 data, and statistically significant differences between the historical and future climate scenario periods are presented, making EC-EARTH3 a robust candidate for conducting future studies on the precursor environments to mountain lee wave cloud events. Full article
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