Close-up of a flooded river. Credit: Tomasz Zajda

Severe flash floods in Mallorca

9 October 2018 09:55 UTC–10 October 02:40 UTC

Close-up of a flooded river. Credit: Tomasz Zajda
Close-up of a flooded river. Credit: Tomasz Zajda

Overnight 9/10 October 2018 severe storms caused devastating flash floods on the Spanish island of Mallorca.

Last Updated

05 December 2022

Published on

09 October 2018

By Mária Putsay (Hungarian Meteorological Service), Ivan Smiljanic (SCISYS) and Sancha Lancaster (Pactum)

As the severe storm systems crossed the island more than 230 mm of rain fell in the area of Sant Llorenç in just two hours, according to the Spanish weather service AEMET. The resulting flash floods were reported to have been the most serious floods to hit Spain in the past 25 years. At least 10 people were reported to have died.

The weather situation is seen in the Meteosat-11 Airmass RGB image (Figure 1) and the animation, 9 October 09:55 UTC–10 Oct 02:40 UTC (Figure 2). The heavy rain was caused by an upper level low situated over the Iberian Peninsula and west of the Mediterranean Sea.

 Meteosat-11 Airmass RGB, 9 October, 17:10 UTC
Figure 1: Meteosat-11 Airmass RGB, 9 October 17:10 UTC
Figure 2: Meteosat-11 Airmass RGB, 9 October 09:55 UTC–10 October 02:40 UTC

As seen from the animation, below the stationary upper level low several intense convective storms formed and developed during the daytime hours.

The evaluation of the convective systems can be followed more closely on the HRV Cloud RGB imagery (Figure 3). Several cells formed, developed and propagated (some from a different direction to main flow, so-called 'left-movers') over the island.

Figure 3: HRV Cloud RGB
 Meteosat-11 IR10.8, 9 Oct, 17:40 UTC
Figure 4: Meteosat-11 IR10.8, 9 October 17:40 UTC

On the satellite imagery several factors indicated the possible severity of the storms:

  • Cold U and cold ring shapes on the infrared imagery.
  • Intense overshooting tops, gravity waves and above-anvil cirrus plume
  • Presence of small ice crystals on the cloud tops.

The cold U and cold ring shapes can be clearly seen in the IR10.8 imagery, see the Meteosat-11 IR10.8 image at 17:40 UTC (Figure 4).

Confirmation of the severity of the systems also comes via the following precipitation products: the MPEF Multisensor Precipitation Estimate (MPE) and the NWCSAF Convective Rainfall Rate (CRR) product (Figure 5).

Both products suggested very intense rain events associated with observed system, where MPE in particular depicted some very localised areas of intense rainfall rates (more than 35mm/h).

Precipitation Product comparison

Met-11 Water Vapour with NWCSAF CRR product compare1
compare2
 

Figure 5: Meteosat-11 Water Vapour images with Multi-sensor Precipitation Estimate and NWC SAF Convective Rainfall Rate products.

Cloud top features are even better seen in the higher resolution images of the polar orbiting satellites.

At 12:24 UTC (before the heavy rain hit Mallorca) overshooting tops, cold-U shapes and an over-anvil ice plume could be seen on the 750 m spatial resolution NPP/VIIRS Sandwich image (Figure 6). At that time the storm systems were south-west of the island.

 Suomi-NPP Sandwich product (VIS0.67/IR10.8 blended image), 09 October, 12:24 UTC.
Figure 6: Suomi-NPP Sandwich product (VIS0.67/IR10.8 blended image), 9 October 12:24 UTC.
 

The colour shades of the Suomi-NPP VIIRS Day Microphysics RGB (red-orange), Suomi-NPP VIIRS Cloud Phase RGB (bright cyan) and Metosat-11 SEVIRI Convection RGB (yellow) confirm the presence of small particles on the storm top (Figures 7, 8 and 9), associated with intense updraft activities.

 Suomi-NPP, 09 October, 12:24 UTC
Figure 7: Suomi-NPP VIIRS Day Microphysics RGB (created with NIR1.6 channel), 9 October, 12:24 UTC
 
 Suomi-NPP, 09 October, 12:24 UTC
Figure 8: Suomi-NPP VIIRS Cloud Phase RGB, 9 October 12:24 UTC
 Meteoesat-11 Severe Convection RGB, 09 October, 12:30 UTC
Figure 9: Meteoesat-11 Severe Convection RGB, 9 October 12:30 UTC

On the NOAA-19 AVHRR Sandwich image (Figure 10) and Cloud RGB (Figure 11) from 15:11 UTC, the systems which dropped 233mm of rain in Colònia de Sant Pere, can be clearly seen over the island.

 NOAA-19, 09 October, 15:11 UTC
Figure 10: NOAA-19 AVHRR sandwich product (VIS0.63/IR10.8 blended image), 9 October 15:11 UTC
 
 NOAA-19, 09 October, 15:11 UTC
Figure 11: NOAA-19 AVHRR Cloud RGB, 9 October 15:11 UTC

Five hours later, around 20:00 UTC, Metop-A IR10.8 image (Figure 12) shows that the more severe systems had moved towards the north-east, away from the island.

 Metop-A IR10.8, 9 October, 20:01 UTC
Figure 13: Metop-A IR10.8, 9 October 20:01 UTC
 

Additional content

Flooding in Mallorca – In pictures (El País)
Majorca flash flood kills at least eight on Spanish island (BBC News)