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 Status:Ongoing analysisFinalised Material from: Linus, Mohamed, Fernando, Ivan

 

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Discussed in the following Daily reports:

http://intra.ecmwf.int/daily/d/dreport/2014/10/31/sc/

http://intra.ecmwf.int/daily/d/dreport/2014/11/03/sc/

http://intra.ecmwf.int/daily/d/dreport/2014/11/04/sc/

http://intra.ecmwf.int/daily/d/dreport/2014/11/05/sc/

http://intra.ecmwf.int/daily/d/dreport/2014/11/06/sc/

http://intra.ecmwf.int/daily/d/dreport/2014/11/07/sc/


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1. Impact

During the first week of November the north-central Mediterranean coast and the southern Alps were hit by intense rainfall and showfall (in the Alps). The situation was caused by a developing trough. Also Morocco was affected by heay rain (see daily reports above).

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 The unstable situation continued during November, see http://intra.ecmwf.int/daily/d/dreport/2014/11/13/sc/ and http://intra.ecmwf.int/daily/d/dreport/2014/11/17/sc/ - http://intra.ecmwf.int/daily/d/dreport/2014/11/18/sc/.

2. Description of the event

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The plots above show the ongoing alert levels from EFAS where yellow is 2-5 years return period, red 5-20 and purple >20 years.

3. Predictability

  

3.1 Data assimilation

 

3.2 HRES

For the rainfall on 3 Nov 06UTC to 4 Nov 06UTC, the plots below show forecast from operational HRES (cy40r1), e-suite HRES (cy41r1) and experiment with TC1279 (8km) and cycle 41r1. The amount of rain the the worst affected area in France increased with about 20% in the e-suite as expected from the changes in cloud physics. With the increased resolution we find a significant increase for this case.

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3.3 ENS


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titleEFI for 3-day precipitation

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4. Experience from general performance/other cases

 

5. Good and bad aspects of the forecasts for the event

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