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Paul R. Field

Researcher at Met Office

Publications -  151
Citations -  10149

Paul R. Field is an academic researcher from Met Office. The author has contributed to research in topics: Ice crystals & Ice nucleus. The author has an hindex of 48, co-authored 147 publications receiving 8328 citations. Previous affiliations of Paul R. Field include University of Leeds & University of Southampton.

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Explicit Forecasts of Winter Precipitation Using an Improved Bulk Microphysics Scheme. Part II: Implementation of a New Snow Parameterization

TL;DR: In this article, a new bulk microphysical parameterization (BMP) was developed for use with the Weather Research and Forecasting (WRF) Model or other mesoscale models.
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Shattering and Particle Interarrival Times Measured by Optical Array Probes in Ice Clouds

TL;DR: In this article, it was shown that the interarrival times of particles measured by these probes can be bimodal and that the cloud probes are more affected than the precipitation probes.
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Observations and Parameterizations of Particle Size Distributions in Deep Tropical Cirrus and Stratiform Precipitating Clouds: Results from In Situ Observations in TRMM Field Campaigns

TL;DR: In this paper, the authors report on the evolution of particle size distributions (PSDs) and habits as measured during slow, Lagrangian-type spiral descents through deep subtropical and tropical cloud layers in Florida, Brazil, and Kwajalein, Marshall Islands, most of which were precipitating.
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Efficiency of the deposition mode ice nucleation on mineral dust particles

TL;DR: In this paper, the deposition mode ice nucleation efficiency of various dust aerosols was investigated at cirrus cloud temperatures between 196 and 223 K using the aerosol and cloud chamber facility AIDA (Aerosol Interaction and Dynamics in the Atmosphere).
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Studies of heterogeneous freezing by three different desert dust samples

TL;DR: In this article, the freezing of water by three different types of mineral particles at temperatures between −12°C and −33°C was investigated at the aerosol interactions and dynamics in the atmosphere (AIDA) chamber facility, and the results from the freezing experiments are consistent with the singular hypothesis of ice nucleation.