Preprints
https://doi.org/10.5194/nhess-2021-396
https://doi.org/10.5194/nhess-2021-396
 
04 Jan 2022
04 Jan 2022
Status: this preprint has been withdrawn by the authors.

The unusually long cold spell and the snowstorm Filomena in Spain in January 2021

Philipp Zschenderlein and Heini Wernli Philipp Zschenderlein and Heini Wernli
  • Institute for Atmospheric and Climate Science, ETH Zurich, Universitätstr. 16, 8092 Zurich, Switzerland

Abstract. In early January 2021, Spain was affected by two extreme events – an unusually long cold spell and a heavy snowfall event associated with extratropical cyclone Filomena. For example, up to 50 cm of snow fell in Madrid and the surrounding areas in 4 days. Already during 9 days prior to the snowfall event, anomalously cold temperatures at 850 hPa and night frosts prevailed over large parts of Spain. During this period, anomalously cold and dry air was transported towards Spain from central Europe and even from the Barents Sea. The storm Filomena, which was responsible for major parts of the snowfall event, developed from a precursor low-pressure system over the central North Atlantic. Filomena intensified due to interaction with an upper-level potential vorticity (PV) trough, which was the result of anticyclonic wave breaking over Europe. In turn, this wave breaking was related to an intense surface anticyclone and upper-level ridge, whose formation was strongly influenced by a warm conveyor belt outflow of a cyclone off the coast of Newfoundland. The most intense snowfall occurred on 09 January and was associated with a sharp air mass boundary with an equivalent potential temperature difference at 850 hPa across Spain exceeding 20 K. Overall, the combination of pre-existing cold surface temperatures, the optimal position of the air mass boundary, and the dynamical forcing for ascent induced by Filomena and its associated upper-level trough were all essential – and in parts physically independent – ingredients for this extreme snowfall event to occur.

This preprint has been withdrawn.

Philipp Zschenderlein and Heini Wernli

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2021-396', Anonymous Referee #1, 07 Jan 2022
  • RC2: 'Comment on nhess-2021-396', Anonymous Referee #2, 19 Jan 2022
  • RC3: 'Comment on nhess-2021-396', Anonymous Referee #3, 31 Jan 2022

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2021-396', Anonymous Referee #1, 07 Jan 2022
  • RC2: 'Comment on nhess-2021-396', Anonymous Referee #2, 19 Jan 2022
  • RC3: 'Comment on nhess-2021-396', Anonymous Referee #3, 31 Jan 2022

Philipp Zschenderlein and Heini Wernli

Philipp Zschenderlein and Heini Wernli

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This preprint has been withdrawn.

Short summary
In early January 2021, Spain was affected by two extreme events – an unusually long cold spell and a heavy snowfall event associated with extratropical cyclone Filomena. In the study, we analyse the synoptic-dynamic development of the two extreme events. Cold air from the north was advected towards Spain and between 07 and 10 January, cyclone Filomena was responsible for major parts of the snowfall event. During this event, temperature and moisture contrasts accross Spain were very high.
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