TY - JOUR
T1 - Advances in the subseasonal prediction of extreme events
T2 - relevant case studies across the globe
AU - Domeisen, Daniela I.V.
AU - White, Christopher J.
AU - Afargan-Gerstman, Hilla
AU - Muñoz, Ángel G.
AU - Janiga, Matthew A.
AU - Vitart, Frédéric
AU - Wulf, C. Ole
AU - Antoine, Salomé
AU - Ardilouze, Constantin
AU - Batté, Lauriane
AU - Bloomfield, Hannah C.
AU - Brayshaw, David J.
AU - Camargo, Suzana J.
AU - Charlton-Pérez, Andrew
AU - Collins, Dan
AU - Cowan, Tim
AU - del Mar Chaves, Maria
AU - Ferranti, Laura
AU - Gómez, Rosario
AU - González, Paula L.M.
AU - González Romero, Carmen
AU - Infanti, Johnna M.
AU - Karozis, Stelios
AU - Kim, Hera
AU - Kolstad, Erik W.
AU - LaJoie, Emerson
AU - Lledó, Llorenç
AU - Magnusson, Linus
AU - Malguzzi, Piero
AU - Manrique-Suñén, Andrea
AU - Mastrangelo, Daniele
AU - Materia, Stefano
AU - Medina, Hanoi
AU - Palma, Lluís
AU - Pineda, Luis E.
AU - Sfetsos, Athanasios
AU - Son, Seok-Woo
AU - Soret, Albert
AU - Strazzo, Sarah
AU - Tian, Di
N1 - © Copyright [2022] AMS, https://www.ametsoc.org/PUBSCopyrightPolicy
PY - 2022/6/1
Y1 - 2022/6/1
N2 - Extreme weather events have devastating impacts on human health, economic activities, ecosys tems, and infrastructure. It is therefore crucial to anticipate extremes and their impacts to allow for preparedness and emergency measures. There is indeed potential for probabilistic subseasonal prediction on timescales of several weeks for many extreme events. Here we provide an overview of subseasonal predictability for case studies of some of the most prominent extreme events across the globe using the ECMWF S2S prediction system: heatwaves, cold spells, heavy precipitation events, and tropical and extratropical cyclones. The considered heatwaves exhibit predictability on timescales of 3-4 weeks, while this timescale is 2-3 weeks for cold spells. Precipitation extremes are the least predictable among the considered case studies. Tropical cyclones, on the other hand, can exhibit probabilistic predictability on timescales of up to 3 weeks, which in the presented cases was aided by remote precursors such as the Madden-Julian Oscillation. For extratropical cyclones, lead times are found to be shorter. These case studies clearly illustrate the potential for event - dependent advance warnings for a wide range of extreme events. The subseasonal predictability of extreme events demonstrated here allows for an extension of warning horizons, provides advance information to impact modelers, and informs communities and stakeholders affected by the impacts of extreme weather events.
AB - Extreme weather events have devastating impacts on human health, economic activities, ecosys tems, and infrastructure. It is therefore crucial to anticipate extremes and their impacts to allow for preparedness and emergency measures. There is indeed potential for probabilistic subseasonal prediction on timescales of several weeks for many extreme events. Here we provide an overview of subseasonal predictability for case studies of some of the most prominent extreme events across the globe using the ECMWF S2S prediction system: heatwaves, cold spells, heavy precipitation events, and tropical and extratropical cyclones. The considered heatwaves exhibit predictability on timescales of 3-4 weeks, while this timescale is 2-3 weeks for cold spells. Precipitation extremes are the least predictable among the considered case studies. Tropical cyclones, on the other hand, can exhibit probabilistic predictability on timescales of up to 3 weeks, which in the presented cases was aided by remote precursors such as the Madden-Julian Oscillation. For extratropical cyclones, lead times are found to be shorter. These case studies clearly illustrate the potential for event - dependent advance warnings for a wide range of extreme events. The subseasonal predictability of extreme events demonstrated here allows for an extension of warning horizons, provides advance information to impact modelers, and informs communities and stakeholders affected by the impacts of extreme weather events.
KW - atmospheric sciences
KW - subseasonal-to-seasonal
KW - predictability
KW - extreme events
KW - forecasting
KW - Madden-Julian oscillation
KW - severe storms
KW - ensembles
KW - forecast verification
KW - probability
KW - forecasts / models / distribution
KW - flooding
U2 - 10.1175/bams-d-20-0221.1
DO - 10.1175/bams-d-20-0221.1
M3 - Article
SN - 0003-0007
VL - 103
SP - E1473–E1501
JO - Bulletin of the American Meteorological Society
JF - Bulletin of the American Meteorological Society
IS - 6
ER -