4.6 Article

European West Coast atmospheric rivers: A scale to characterize strength and impacts

Journal

WEATHER AND CLIMATE EXTREMES
Volume 31, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.wace.2021.100305

Keywords

Atmospheric rivers; Scale; Precipitation; Impacts

Funding

  1. Spanish regional government Xunta de Galicia [ED481B 2018/069, ED481B 2018/062]
  2. Fulbright Commission (U.S. Department of State)
  3. Spanish Government (MINECO) [CGL2015-65141-R]
  4. National Science Foundation (NSF) CAREER Award [AGS 1454089]
  5. Ministerio de Ciencia, Innovacin y Universidades, Spain [RTI2018-095772-B-I00]
  6. Xunta de Galicia [ED431C 2017/64-GRC]
  7. Fundacao para a Ciencia e Tecnologia (Potugal) by project Weather Extremes in the Euro Atlantic Region: Assessment and Impacts-WEx-Atlantic [PTDC/CTA-MET/29233/2017]
  8. Scientific Employment Stimulus 2017 from Fundacao para a Ciencia e Tecnologia (FCT) [CEECIND/00027/2017]
  9. Fundação para a Ciência e a Tecnologia [PTDC/CTA-MET/29233/2017] Funding Source: FCT

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This study applies the newly-created atmospheric river intensity and impacts scale (AR Scale) to the European continent, finding remarkable variability in the distribution of AR events across Europe. AR1 and AR2 events are the most frequent, explaining most of the precipitation, but with a low probability of extreme rainfall, while AR3, AR4, and AR5 events, although less common, are associated with a high probability of extreme rainfall.
This manuscript applies the recently-created atmospheric river intensity and impacts scale (AR Scale) to the European continent. The AR Scale uses an Eulerian perspective based solely upon the time series of integrated vapor transport (IVT) over a given geographic location (often represented by a model or reanalysis grid cell). The scale assigns events with persistent, strong IVT at that location to one of five levels (AR1 to AR5), or if the IVT is too weak or short-lived it is determined not to be an AR. AR1 events are primarily beneficial, AR2, 3 and 4 include a mix of beneficial and hazardous impacts, while AR5s are primarily hazardous. The frequency of occurrence, the associated probability of anomalous precipitation and the amount of precipitation explained by each AR rank are provided across Europe for the extended winter season (from October through March). AR1 and AR2 events are the most frequent and explain most of the observed precipitation, but they are associated with a low probability of extreme rainfall. Although AR3, AR4 and AR5 events are much less frequent, and normally provide a smaller fraction of annual precipitation, they are associated with a high probability of extreme rainfall. These results show remarkable variability among the different regions of the European continent. This manuscript also provides an AR detection catalog over Europe for the period 1980-2019, and a simplified version of the algorithm used to rank the events from AR1 to AR5.

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