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Status:
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Finalized Material from: Ivan
Discussed in the following Daily reports:
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Maximum CAPE during the specified period is shown as well as maximum CAPE in case the convective inhibition (CIN) is less than 200 J/kg and therefore convection can be triggered. When CIN is greater than 200 j/kg the cap is so strong that it prevents convection from happening.
The tephigram for Varna, the city affected by flash floods, shows that the atmosphere was unstable, humidity quite high coming from the Black Sea with easterly winds at the surface. The black curve in the analysis is drawn taking the maximum temperature in Varna on that day which was close to 23C. The 12-hour forecast profile was a little bit different with a deep saturated layer from the surface implying rainfall at that time.
Tephigrams for Varna: analysis (left), 12-h forecast (right).
3.3 ENS
The flash floods occurred on 19 June in the evening and in early morning on the 20 June when just in few hours more than 100 mm of rainfall were recorded in NE part of the country. Flash floods occurred there. The analyses show that 99th model climate percentile for 24h total rainfall was exceeded in many places in the east of Bulgaria. Some local heavy showers were observed in far western regions of the country as well. If we compare observations with the 95th model climate (M-climate) percentile, we'll notice areas of local torrential downpours in many parts of Northern Bulgaria as well. The shortest range EFI forecast matches quite well the areas affected by heavy rain but the EFI has never reached extremely high values close to 1 over NE Bulgaria. This is more likely due to the convective nature of the rain and the large uncertainty in the forecast that we might expect in such cases. Note that there is 6-hour shift between the validity of the EFI forecast and the accumulations represented by the observations: EFI is valid from 00 to 00UTC whilst accumulations are for periods starting from 06UTC.
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Longer lead time EFI/SOT forecasts for 72- and 120-hour total precipitation. Green triangles denote observations that exceed 99th model climate percentile.
The extended-range EFI, for T+240-360 gives a hint of wet weather.
EFI for total precipitation, forecast for T+240-360h. Yellow/red colours mean wetter than normal conditions.
Cyclonic features according to 12-hour maximum precipitation (-6/+6h) in different forecast valid for 19/06/2014 12UTC and 20/06/2014 00UTC.
3.4 Monthly forecasts
Exceptionally wet weather in the Balkans has been predicted well in the medium range by the ENS. Positive precipitation anomalies appeared even in the far medium range for days 8 to 14. For longer ranges in the monthly forecast there is no signal.
Precipitation anomalies from ECMWF monthly forecast compared with the analysis.
3.5 Comparison with other centres
Four control forecast of total precipitation from TIGGE: ECMWF, UKMO, NCEP and LAM Aladin Austria. Having different resolution and different model characteristics they all forecast significant rainfall in the eastern part of Bulgaria.
Forecasts of 24-h accumulated rainfall valid for 19 June 06UTC to 20 June 06UTC from ECMWF HRES (~16 km) and COSMO LEPS control (~10 km). Black numbers denote observed rainfall accumulations. COSMO LEPS is a non-hydrostatic limited-area ensemble which uses initial and boundary conditions from ECMWF ENS. It comprises 16 perturbed members and a control forecast with a horizontal resolution of about 10 km. To obtain initial and boundary conditions an extended ensemble of 2 consecutive ECMWF ENS runs is used (51+51 members) and a cluster analysis is applied to these 102 members. For each of the 16 clusters a representative member is selected to provide initial and boundary conditions. The ensemble is run up to T+132h.
Forecasts of 24-h accumulated rainfall valid for 19 June 06UTC to 20 June 06UTC from ECMWF HRES and UKMO global model.
Probability of rain above 50 mm/24h from ECMWF ENS (~32 km) and COSMO LEPS (~10 km) in the short range. Numbers in the brackets show the horizontal resolution of each ensemble.
Probability of rain above 20 and 50 mm/24h from ECMWF ENS and COSMO LEPS in the medium-range.
4. Experience from general performance/other cases
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5. Good and bad aspects of the forecasts for the event
- The EFI/SOT gave a signal of abnormal rainfall well in advance - 4 to 5 days before the event on 19 June.
- Convective nature of the rainfall makes forecasts of its location and intensity quite difficult. Forecasts vary a lot from one run to another considerably altering the location of the most intense rainfall. This increases the uncertainty of the forecast and makes the localisation of the heavy rain extremely difficult even in the short range. The cyclogenesis over the Black Sea is well captured by IFS.