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COLLABORATIVE EFFORTS BETWEEN THE UNITED STATES AND UNITED KINGDOM TO ADVANCE PREDICTION OF HIGH-IMPACT WEATHER

Bulletin of the American Meteorological Society, 2017-05, Vol.98 (5), p.937-948

2017

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The Surprising Role of Orography in the Initiation of an Isolated Thunderstorm in Southern England

Monthly weather review, 2009-09, Vol.137 (9), p.3026-3046

2009

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The impact of spin‐up and resolution on the representation of a clear convective boundary layer over London in order 100 m grid‐length versions of the Met Office Unified Model

Quarterly journal of the Royal Meteorological Society, 2019-04, Vol.145 (721), p.1674-1689

2019

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Convection‐permitting models: a step‐change in rainfall forecasting

Meteorological applications, 2016-04, Vol.23 (2), p.165-181

2016

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The use of 100m scale NWP models to understand differences between different measures of mixing height in a morning growing clear convective boundary layer over London

Quarterly journal of the Royal Meteorological Society, 2022-04, Vol.148 (745), p.1983-1995

2022

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The use of 100 m scale NWP models to understand differences between different measures of mixing height in a morning growing clear convective boundary layer over London

Quarterly journal of the Royal Meteorological Society, 2022-04, Vol.148 (745), p.1983-1995

2022

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Combination of Mesoscale and Synoptic Mechanisms for Triggering an Isolated Thunderstorm : Observational Case Study of CSIP IOP 1

Monthly weather review, 2007-11, Vol.135 (11), p.3728-3749

2007

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Methodology to evaluate numerical weather predictions using large‐aperture scintillometry sensible heat fluxes: Demonstration in London

Quarterly journal of the Royal Meteorological Society, 2024-10

2024

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Characteristics of Diagnostics for Identifying Elevated Convection over the British Isles in a Convection-Allowing Model

Weather and forecasting, 2023-07, Vol.38 (7), p.1079-1094

2023

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Does the Representation of Flow Structure and Turbulence at a Cold Front Converge on Multiscale Observations with Model Resolution?

Monthly weather review, 2017-11, Vol.145 (11), p.4345-4363

2017

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Evaluation of forward-modelled attenuated backscatter using an urban ceilometer network in London under clear-sky conditions

Atmospheric environment (1994), 2018-10, Vol.191, p.532-547

2018

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Convective-Scale Perturbation Growth across the Spectrum of Convective Regimes

Monthly weather review, 2018-01, Vol.146 (1), p.387-405

2018

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Does the Representation of Flow Structure and Turbulence at a Cold Front Converge on Multiscale Observations with Model Resolution?

Monthly weather review, 2017-11, Vol.145 (11), p.4345

2017

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Use of Z DR columns for early detection of severe convection within the operational radar network of the United Kingdom

Meteorological applications, 2024-01, Vol.31 (1)

2024

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Observed aerosol characteristics to improve forward-modelled attenuated backscatter in urban areas

Atmospheric environment (1994), 2020-03, Vol.224, p.117177, Article 117177

2020

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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

Quarterly journal of the Royal Meteorological Society, 2024-10

2024

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Integrated urban hydrometeorological, climate and environmental services: Concept, methodology and key messages

Urban climate, 2020-09, Vol.33, p.100623-100623, Article 100623

2020

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Effects of Initial and Boundary Conditions of Mesoscale Models on Simulated Atmospheric Refractivity

Journal of applied meteorology and climatology, 2012-01, Vol.51 (1), p.115-132

2012

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DEVELOPING A RESEARCH STRATEGY TO BETTER UNDERSTAND, OBSERVE, AND SIMULATE URBAN ATMOSPHERIC PROCESSES AT KILOMETER TO SUBKILOMETER SCALES

Bulletin of the American Meteorological Society, 2017-10, Vol.98 (10), p.ES261-ES264

2017

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Dynamical effects of ice sublimation in a frontal wave

Quarterly journal of the Royal Meteorological Society, 2000-07, Vol.126 (568), p.2405-2434

2000

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THE CONVECTIVE PRECIPITATION EXPERIMENT (COPE): Investigating the Origins of Heavy Precipitation in the Southwestern United Kingdom

Bulletin of the American Meteorological Society, 2016-06, Vol.97 (6), p.1003-1020

2016

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THE CONVECTIVE STORM INITIATION PROJECT

Bulletin of the American Meteorological Society, 2007-12, Vol.88 (12), p.1939-1955

2007

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The DYMECS project: a statistical approach for the evaluation of convective storms in high-resolution NWP models: the 3D structures of over 1,000 convective storms observed by the Chilboiton radar are used to constrain storm dynamics and microphysics in models with resolutions between 100 and 1,500 m

Bulletin of the American Meteorological Society, 2015-06, p.939

2015

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Improvements in Forecasting Intense Rainfall: Results from the FRANC (Forecasting Rainfall Exploiting New Data Assimilation Techniques and Novel Observations of Convection) Project

COLLABORATIVE EFFORTS BETWEEN THE UNITED STATES AND UNITED KINGDOM TO ADVANCE PREDICTION OF HIGH-IMPACT WEATHER

The Surprising Role of Orography in the Initiation of an Isolated Thunderstorm in Southern England

The impact of spin‐up and resolution on the representation of a clear convective boundary layer over London in order 100 m grid‐length versions of the Met Office Unified Model

Convection‐permitting models: a step‐change in rainfall forecasting

The use of 100m scale NWP models to understand differences between different measures of mixing height in a morning growing clear convective boundary layer over London

The use of 100 m scale NWP models to understand differences between different measures of mixing height in a morning growing clear convective boundary layer over London

Combination of Mesoscale and Synoptic Mechanisms for Triggering an Isolated Thunderstorm : Observational Case Study of CSIP IOP 1

Methodology to evaluate numerical weather predictions using large‐aperture scintillometry sensible heat fluxes: Demonstration in London

Characteristics of Diagnostics for Identifying Elevated Convection over the British Isles in a Convection-Allowing Model

Does the Representation of Flow Structure and Turbulence at a Cold Front Converge on Multiscale Observations with Model Resolution?

Evaluation of forward-modelled attenuated backscatter using an urban ceilometer network in London under clear-sky conditions

Convective-Scale Perturbation Growth across the Spectrum of Convective Regimes

Does the Representation of Flow Structure and Turbulence at a Cold Front Converge on Multiscale Observations with Model Resolution?

Use of Z DR columns for early detection of severe convection within the operational radar network of the United Kingdom

Observed aerosol characteristics to improve forward-modelled attenuated backscatter in urban areas

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

Integrated urban hydrometeorological, climate and environmental services: Concept, methodology and key messages

urbisphere-Berlin campaign: Investigating multi-scale urban impacts on the atmospheric boundary layer

Effects of Initial and Boundary Conditions of Mesoscale Models on Simulated Atmospheric Refractivity

DEVELOPING A RESEARCH STRATEGY TO BETTER UNDERSTAND, OBSERVE, AND SIMULATE URBAN ATMOSPHERIC PROCESSES AT KILOMETER TO SUBKILOMETER SCALES

Dynamical effects of ice sublimation in a frontal wave

THE CONVECTIVE PRECIPITATION EXPERIMENT (COPE): Investigating the Origins of Heavy Precipitation in the Southwestern United Kingdom

THE CONVECTIVE STORM INITIATION PROJECT

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