Jesse Norris
University of Manchester
4 Papers
6 Citations
Jesse Norris is an academic researcher from University of Manchester. The author has contributed to research in topics: Precipitation & Cold front. The author has an hindex of 3, co-authored 4 publications.
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Papers
Cloud Banding and Winds in Intense European Cyclones: Results from the DIAMET Project
Geraint Vaughan,John Methven,D. Anderson,Bogdan Antonescu,Laura Baker,T. P. Baker,S. P. Ballard,Keith Bower,P. R. A. Brown,Jeffrey M. Chagnon,Thomas Choularton,J. Chylik,Paul Connolly,Peter G. Cook,Richard Cotton,Jonathan Crosier,Christopher Dearden,James Dorsey,Thomas Frame,Martin Gallagher,Michael Goodliff,Suzanne L. Gray,Ben Harvey,Peter Knippertz,Humphrey W. Lean,Dingmin Li,Gary Lloyd,O. Martinez Alvarado,John Nicol,Jesse Norris,E. Öström,J. S. R. Owen,Douglas J. Parker,Robert S. Plant,Ian A. Renfrew,Nigel Roberts,Philip D. Rosenberg,A. C. Rudd,David M. Schultz,Jonathan P. Taylor,Tomasz M. Trzeciak,R. Tubbs,A. Vance,P. J. van Leeuwen,A. Wellpott,A. Woolley +45 more
TL;DR: The Diabatic Influences on Mesoscale Structures in Extratropical Storms (DIAMET) project as mentioned in this paper aims to improve forecasts of high-impact weather in extropical cyclones through field measurements, high-resolution numerical modeling, and improved design of ensemble forecasting and data assimilation systems.
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Snowbands over the English Channel and Irish Sea during cold‐air outbreaks
TL;DR: In this paper, the English Channel and Irish Sea were investigated for the formation of snowbands over the winters of 2009-10 and 2010-11, with the resulting convection frequently organizing into snowbands.
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Precipitation Banding in Idealized Baroclinic Waves
TL;DR: In this paper, the development of precipitation bands from a zonally uniform initial midlatitude jet is analyzed for a frictionless lower boundary, and with no latent-heat release or surface heat and moisture fluxes, a bent-back warm front forms.
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Variability of precipitation along cold fronts in idealized baroclinic waves
TL;DR: In this paper, a three-dimensional primitive equation model is used to investigate along-front variability of precipitation in an idealized baroclinic wave, showing that along the poleward part of the cold front, a narrow line of precipitation develops.