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View article: Positive low cloud feedback from increasing surface longwave radiation and parametrized convection in HadGEM3-GC3.1-LL.
Positive low cloud feedback from increasing surface longwave radiation and parametrized convection in HadGEM3-GC3.1-LL. Open
View article: The third Met Office Unified Model–JULES Regional Atmosphere and Land Configuration, RAL3
The third Met Office Unified Model–JULES Regional Atmosphere and Land Configuration, RAL3 Open
The third version of the Regional Atmosphere and Land (RAL3) science configuration is documented. Developed through international partnerships, RAL configurations define settings for the Unified Model atmosphere and Joint UK Land Environme…
View article: Sensitivity of near‐surface marine winds and wind stress in coastal Antarctica to regional atmospheric model configuration
Sensitivity of near‐surface marine winds and wind stress in coastal Antarctica to regional atmospheric model configuration Open
Near‐surface marine winds in coastal Antarctica have global importance, as they affect ocean circulation and sea‐ice variability. We test the sensitivities of simulated near‐surface winds and wind stress in coastal Antarctica to uncertain …
View article: The Met Office Unified Model Global Atmosphere 8.0 and JULES Global Land 9.0 configurations
The Met Office Unified Model Global Atmosphere 8.0 and JULES Global Land 9.0 configurations Open
We describe Global Atmosphere 8.0 and Global Land 9.0 (GA8GL9) that are science configurations of the Met Office Unified Model and JULES land surface model developed for use across weather and climate timescales. GA8GL9 builds upon GA7GL7.…
View article: Rolling <scp>DICE</scp> to advance knowledge of land–atmosphere interactions
Rolling <span>DICE</span> to advance knowledge of land–atmosphere interactions Open
The Diurnal Land–Atmosphere Coupling Experiment (DICE) aims to explore the complex interactions between the land surface and atmospheric boundary layer, which are generally not well understood and difficult to isolate in models. The projec…
View article: Supplementary material to "The third Met Office Unified Model-JULES Regional Atmosphere and Land Configuration, RAL3"
Supplementary material to "The third Met Office Unified Model-JULES Regional Atmosphere and Land Configuration, RAL3" Open
View article: The third Met Office Unified Model-JULES Regional Atmosphere and Land Configuration, RAL3
The third Met Office Unified Model-JULES Regional Atmosphere and Land Configuration, RAL3 Open
The third version of the Regional Atmosphere and Land (RAL3) science configuration is documented. Developed through international partnership, RAL configurations define settings for the Unified Model atmosphere and Joint UK Land Environmen…
View article: The hectometric modelling challenge: Gaps in the current state of the art and ways forward towards the implementation of 100‐m scale weather and climate models
The hectometric modelling challenge: Gaps in the current state of the art and ways forward towards the implementation of 100‐m scale weather and climate models Open
For a number of years research has been carried out in several centres which has demonstrated the potential benefits of 100‐m scale models for a range of meteorological phenomena. More recently, some meteorological services have started to…
View article: Impacts of the new UM convection scheme, CoMorph-A, over the Indo-Pacific and Australian regions
Impacts of the new UM convection scheme, CoMorph-A, over the Indo-Pacific and Australian regions Open
A new convection scheme, ‘CoMorph-A’, has been introduced into the latest UK Met Office coupled (GC4) and atmosphere-only (GA8) models. In this study, the impact of CoMorph-A is assessed in atmosphere-only Atmospheric Model Intercomparison…
View article: Impacts of free tropospheric turbulence parametrisation on a sheared tropical cyclone
Impacts of free tropospheric turbulence parametrisation on a sheared tropical cyclone Open
The turbulent transport of momentum, heat, and moisture can impact tropical cyclone intensity. However, representing subgrid‐scale turbulence accurately in numerical weather prediction models is challenging due to a lack of observational d…
View article: The use of idealised experiments in testing a new convective parametrization: Performance of <scp>CoMorph‐A</scp>
The use of idealised experiments in testing a new convective parametrization: Performance of <span>CoMorph‐A</span> Open
CoMorph is a new mass‐flux convection parametrization under development at the Met Office designed for use within the Unified Model and its successor model, LFRic. Use of a three‐dimensional idealised model enables controlled tests of the …
View article: What Are the Main Causes of Positive Subtropical Low Cloud Feedbacks in Climate Models?
What Are the Main Causes of Positive Subtropical Low Cloud Feedbacks in Climate Models? Open
We investigate positive subtropical low cloud feedback mechanisms in climate models which have performed the CMIP6/CFMIP‐3 AMIP and AMIP uniform +4K experiments while saving CFMIP‐3 process diagnostics on model levels. Our analysis focuses…
View article: Positive Low Cloud Feedback Primarily Caused by Increasing Longwave Radiation from the Sea Surface in Two Versions of a Climate Model
Positive Low Cloud Feedback Primarily Caused by Increasing Longwave Radiation from the Sea Surface in Two Versions of a Climate Model Open
Low cloud feedback in global warming projections by climate models is characterized by its positive sign, the mechanism of which is not well understood. Here we propose that the positive sign is primarily caused by the increase in upward l…
View article: Positive Low Cloud Feedback Primarily Caused by Increasing Longwave Radiation From the Sea Surface in Two Versions of a Climate Model
Positive Low Cloud Feedback Primarily Caused by Increasing Longwave Radiation From the Sea Surface in Two Versions of a Climate Model Open
Low cloud feedback in global warming projections by climate models is characterized by its positive sign, the mechanism of which is not well understood. Here we propose that the positive sign is primarily caused by the increase in upward l…
View article: Irrigation contrasts through the morning transition
Irrigation contrasts through the morning transition Open
The Land surface Interactions with the Atmosphere over the Iberian Semi‐arid Environment (LIAISE) campaign was conducted in July 2021, primarily to investigate the role of irrigation in modulating the boundary‐layer evolution in the Catala…
View article: The Met Office Unified Model GA7.2GL8.1 and GA7.2.1GL8.1.1 configurations: Developments from GA7GL7
The Met Office Unified Model GA7.2GL8.1 and GA7.2.1GL8.1.1 configurations: Developments from GA7GL7 Open
The Unified Model and JULES are used in defined Global Atmosphere and Global Land configurations to simulate the global atmosphere-land system at the Met Office and at other UM partners. GA7.0GL7.0 was frozen in 2016. However, the NWP perf…
View article: Confronting the Convective Gray Zone in the Global Configuration of the Met Office Unified Model
Confronting the Convective Gray Zone in the Global Configuration of the Met Office Unified Model Open
In atmospheric models with kilometer‐scale grids the resolution approaches the scale of convection. As a consequence the most energetic eddies in the atmosphere are partially resolved and partially unresolved. The modeling challenge to rep…
View article: What physical mechanisms cause positive subtropical low cloud feedbacks in climate models?
What physical mechanisms cause positive subtropical low cloud feedbacks in climate models? Open
We investigate positive subtropical low cloud feedback mechanisms in climate models which have performed the CMIP6/CFMIP-3 AMIP and AMIP uniform +4K experiments while saving CFMIP-3 process diagnostics on model levels. Our analysis focuses…
View article: The second Met Office Unified Model–JULES Regional Atmosphere and Land configuration, RAL2
The second Met Office Unified Model–JULES Regional Atmosphere and Land configuration, RAL2 Open
In this paper we define RAL2 – the second Regional Atmosphere and Land (RAL) science configuration for regional modelling. RAL2 uses the Unified Model (UM) as the basis for the atmosphere and the Joint UK Land Environment Simulator (JULES)…
View article: The second Met Office Unified Model-JULES Regional Atmosphere and Land configuration, RAL2
The second Met Office Unified Model-JULES Regional Atmosphere and Land configuration, RAL2 Open
Supporting data for figures in GMD draft paper: The second Met Office Unified Model-JULES Regional Atmosphere and Land configuration, RAL2
View article: The second Met Office Unified Model-JULES Regional Atmosphere and Land configuration, RAL2
The second Met Office Unified Model-JULES Regional Atmosphere and Land configuration, RAL2 Open
Supporting data for figures in GMD draft paper: The second Met Office Unified Model-JULES Regional Atmosphere and Land configuration, RAL2
View article: Kilometer‐Scale Simulations of Trade‐Wind Cumulus Capture Processes of Mesoscale Organization
Kilometer‐Scale Simulations of Trade‐Wind Cumulus Capture Processes of Mesoscale Organization Open
The EUREC 4 A (Elucidating the role of clouds–circulation coupling in climate) and ATOMIC (Atlantic Tradewind Ocean‐Atmosphere Mesoscale Interaction Campaign) joint field campaign gathered observations to better understand the links betwee…
View article: MetUM Simulations of 2nd February Case Study
MetUM Simulations of 2nd February Case Study Open
This repository contains data to support the publication "Kilometre-scale simulations of trade-wind cumulus capture processes of mesoscale organization" submitted to JAMES. The data is from Met Office Unified Model simulations of the 2nd F…
View article: MetUM Simulations of 2nd February Case Study
MetUM Simulations of 2nd February Case Study Open
This repository contains data to support the publication "Kilometre-scale simulations of trade-wind cumulus capture processes of mesoscale organization" submitted to JAMES. The data is from Met Office Unified Model simulations of the 2nd F…
View article: Comment on gmd-2022-209
Comment on gmd-2022-209 Open
Abstract. In this paper we define RAL2 â the second Regional Atmosphere and Land (RAL) science configuration for regional modelling. RAL2 uses the Unified Model (UM) as the basis for the atmosphere and the Joint UK Land …
View article: Comment on gmd-2022-209
Comment on gmd-2022-209 Open
Abstract. In this paper we define RAL2 â the second Regional Atmosphere and Land (RAL) science configuration for regional modelling. RAL2 uses the Unified Model (UM) as the basis for the atmosphere and the Joint UK Land …
View article: The second Met Office Unified Model/JULES Regional Atmosphere and Land configuration, RAL2
The second Met Office Unified Model/JULES Regional Atmosphere and Land configuration, RAL2 Open
In this paper we define RAL2 - the second "Regional Atmosphere and Land" (RAL) science configuration for regional modelling. RAL2 uses the Unified Model (UM) as the basis for the atmosphere and the Joint UK Land Environment Simulator (JULE…
View article: Confronting the convective gray zone in the global configuration of the Met Office Unified Model
Confronting the convective gray zone in the global configuration of the Met Office Unified Model Open
In atmospheric models with kilometer-scale grids the resolution approaches the scale of convection. As a consequence the most energetic eddies in the atmosphere are partially resolved and partially unresolved. The modeling challenge to rep…
View article: Kilometer-scale simulations of trade-wind cumulus capture processes of mesoscale organization
Kilometer-scale simulations of trade-wind cumulus capture processes of mesoscale organization Open
Earth and Space Science Open Archive This preprint has been submitted to and is under consideration at Journal of Advances in Modeling Earth Systems (JAMES). ESSOAr is a venue for early communication or feedback before peer review. Data ma…
View article: SINGV: A convective‐scale weather forecast model for Singapore
SINGV: A convective‐scale weather forecast model for Singapore Open
Numerical weather prediction (NWP) capabilities in the Maritime Continent are not as developed as in the midlatitudes. Countries in the region do not develop their own modelling systems; rather they adapt models primarily developed for the…