Weather pictures & report of August 23 2011

 

MCS thunderstorms along thermal troughs


Synopsis: at 500 hPa, east of a relaxing trough west of the British Isles, our area in a moderate SW'ly flow of warm and humid potentially unstable air. During the morning passage of the axis of a short wave upper trough. At surface a small depression over northwest France moving into the channel with related to it the passage of of several thermal trough lines triggering thundery showers. Especially central parts of Belgium were affected with local flooding. The consecutive passage of no less than four big multicell thunderstorms (of which 3 MCS) resulted in the highest amount of discharges of the entire summer season over Belgium, namely 87000. All pictures taken at Kampenhout (central Belgium) with hours in local time (CET).

 

Surface analysis of August 23 2011 at 0800 CET. Related to a depression over northwestern France, a thermal trough crossing Belgium during the morning - early forenoon. (Source chart: Belgocontrol)

 

Loop of 18 surface analyses of each hour starting from August 22 at 2300 CET with weather plots showing the thundery outbreaks in 4 waves. (Source: meteocentre.com)

 

Upper air analysis 500 hPa of August 23 2011 at 0200 CET. A relaxing upper trough west of Ireland as extension of the cold pool just south of Iceland with furthermore a relaxing shortwave trough over western France which crossed Belgium in the forenoon. On the eastern flank a ridge near Italy - Balkan. It resulted over our area in a moderate SW'ly flow. (Source chart: DWD via wetter3)

 

Upper air analysis 850 hPa of August 23 2011 at 0200 CET. Between the low near Iceland and anticyclone over the Balkan, our area in a weak to moderate S'ly flow of warm air. (Source chart: DWD via wetter3)

 

Loop of forecasted soundings for Brussels of August 23 2011 between 0830-2000 CET. During the morning hours a so called CAP (or inversion) was present below 3000ft. Nevertheless due to passage of some thermal troughlines instability was released in form of MCS thunderstorms during the previous night and morning - forenoon. Due to diurnal heating the CAP was cleared in the afternoon, but by then it turned out too dry in the upper levels to form deep showers. Also detectable before noon is a pronounced directional windshear in the lowest 3 km whereby supercells could not be excluded. (Source: RASP)

 

Another loop of forecasted soundings for a 15 hours period (in steps of three hours) of Brussels from August 23 2011, 0500 CET onwards. Included are some thunderstorms indices: surface based CAPE was during the night 0 J/kg, but the most unstable one went up to around 1000 J/kg (which could be released with a trigger), KI 35, TT 55, LI -5 = strong convective potential which may lead to frequent thunderstorms, isolated severe. Directional shear was moderate with 127 m²/s², low level shear was 25 kt, deep layer shear 35-40 kt. Due to the moderate CAPE and moderate shear, multicells (eventually MCS) and supercells could be expected. (Source: weatheronline.co.uk).

 

Forecasted vertical profile and surface temperature for Brussels Airport of August 22 from 2000 CET and the following 48 hours. Legend of upper map: green-brown-white is humidity in steps of 10% with darkest green being 90% or more, wind in kt, temperatures each 5°C. Humid air at the begin of the period well towards the upper levels (200 hPa). Furthermore a slight fall of the upper air temperatures in the morning with passage of short wave upper trough, repeated during the evening with passage of cold front, and much drier air behind (above 13000 ft). Also clearly detectable is a rather strong wind shear first 12-15 hours in the lowest 6000ft. (Source: Belgocontrol)

 

Satellite image of 22/08/2011 at 2121 CET in the infra-red channel with the formation of some big multi-cells over western and northwestern France. The first one entered western parts of Belgium just after midnight.  (Source sat picture: NOAA and University of Bern)

 

Satellite image of 23/08/2011 at 0318 CET in the infra-red channel with the first MCS now over Holland, but more cells on its way to Belgium.  (Source sat picture: NOAA and University of Bern)

 

23/08/2011 0315-0700 CET. Satellite loop in the infra-red channel. Three multi-cell thunderstorms (of which two MCS) over Benelux and surrounding area. (Source sat picture: Eumetsat via Sat24.com)

 

23/08/2011 0615-0745 CET. Satellite loop in the visual channel. A developing MCS thunderstorm affecting western parts Belgium. (Source sat picture: Eumetsat via Sat24.com)

 

23/08/2011 0815-1315 CET. Satellite loop in the visual channel. This MCS thunderstorm migrated further northeastwards with still some new but smaller cells building behind. (Source sat picture: Eumetsat via Sat24.com)

 

Radar loop (rain fall rate in mm) of August 23 2011 between 0315-1335 CET. Mainly the central parts of Belgium were affected by a lot of rain and lightning with the passage of no less than 4 multi-cell (MCS) thunderstorms. (Source radar picture: Belgocontrol)

 

Corresponding discharges of August 22 2011 from late evening onwards a first multi-cell reaching provinces Hainaut, Namur and Brabant-Walloon . (Source lightning picture: Buienradar)

 

Corresponding discharges of August 23 2011 with mainly the central & northeastern parts of Belgium and southeastern parts of Holland being affected by a lot of discharges during the first 1200 hours of the day. Total discharges of all storms was 87000 with around 12000 cloud-to-ground strikes. (Source lightning picture: Buienradar)

 

Main theme (besides the amount of lightning strikes) was the massive rain fall: Ukkel was the top with 42 mm, followed by Zaventem with 20 mm. My location at Kampenhout (5 km northeast of Zaventem) received 33 mm.

 

Metars of Brussels Airport (EBBR) (hours in UTC). Translation: copy paste each obs via metar-decoder
 

EBBR 222120Z 06005KT 040V100 7000 TS FEW035CB 17/15 Q1017 TEMPO VRB15G30KT 3000 TSRA=
EBBR 222150Z VRB02KT 5000 -TSRA SCT030CB 17/16 Q1018 TEMPO VRB15G30KT 3000 TSRA=
EBBR 222220Z 12009KT 4000 TSRA SCT006 BKN016CB 17/16 Q1017 TEMPO VRB15G30KT 2500 TSRA BKN007=
EBBR 222250Z 18005KT 140V200 4000 TSRA FEW006 SCT026CB BKN047 17/16 Q1018 TEMPO VRB15G30KT 2500 TSRA
EBBR 222320Z 11010KT 6000 TSRA FEW006 SCT026CB BKN047 16/15 Q1016 TEMPO VRB15G30KT 3000 TSRA
EBBR 222350Z 08015KT 6000 -RA FEW006 FEW024CB BKN047 16/15 Q1012 TEMPO VRB15G30KT 3000 TSRA
EBBR 230020Z 10010KT 070V130 8000 FEW010 17/16 Q1012 NOSIG 
EBBR 230050Z 16005KT 120V230 9999 FEW009 17/16 Q1013 NOSIG 
EBBR 230120Z 25004KT 200V290 9999 FEW009 SCT013 17/16 Q1015 TEMPO BKN012
EBBR 230150Z 29006KT 9999 FEW009 SCT013 17/16 Q1015 TEMPO BKN012
EBBR 230220Z 29008KT 5000 BR FEW007 BKN016 17/16 Q1016 TEMPO VRB15G30KT 2500 TSRA BKN006
EBBR 230250Z 31010KT 280V350 1500 +TSRA BR BKN007 BKN018CB 16/16 Q1016 TEMPO VRB15G30KT 1200 +TSRA 
EBBR 230320Z 07007KT 2000 BR SCT007 FEW018CB 16/16 Q1014 TEMPO VRB15G30KT 1200 TSRA BR 
EBBR 230350Z 08006KT 050V110 2000 BR BKN003 16/16 Q1013 TEMPO 1200 BR  
EBBR 230420Z 08003KT 040V130 2000 BR BKN003 16/16 Q1013 TEMPO 1200 BR  
EBBR 230450Z 09004KT 060V150 1800 BR SCT003 BKN004 16/16 Q1013 NOSIG
EBBR 230520Z 11006KT 070V150 2000 BR SCT003 BKN004 17/16 Q1012 NOSIG
EBBR 230550Z 28012KT 2200 BR SCT004 BKN006 17/16 Q1015 TEMPO VRB20G30KT 2000 SHRA TSRA BKN012CB
EBBR 230620Z 32008G18KT 290V030 2500 -TSRA SCT006 BKN011 SCT017CB 17/16 Q1015 TEMPO VRB20G30KT 2000 SHRA TSRA BKN012CB 
EBBR 230650Z 07009KT 030V100 2500 R25L/P2000N R25R/M0050VP2000U R02/P2000N BR FEW012 FEW020CB 17/16 Q1013 TEMPO VRB20G30KT 2000 SHRA TSRA BKN012CB 
EBBR 230720Z 10011KT 070V130 5000 R25L/P2000N R25R/M0050VP2000D R02/P2000N BR FEW014 18/16 Q1012 TEMPO VRB20G30KT 2000 SHRA TSRA BKN012CB  
EBBR 230750Z 24017KT 0900 R25L/0900VP2000D R25R/1400VP2000D R02/0550VP2000D TSRAGR BKN014CB 17/15 Q1014 TEMPO VRB20G35KT 1200 SHRA TSRAGR BKN012CB 
EBBR 230820Z VRB05G16KT 2000 R25L/0750VP2000U R25R/M0050VP2000U R02/0450VP2000U TSRA FEW009 BKN015CB 16/15 Q1014 TEMPO VRB20G35KT 1200 SHRA TSRAGR BKN012CB
EBBR 230850Z 13008KT 090V150 8000 -TSRA FEW010 SCT018CB 17/// Q1013 TEMPO VRB20G35KT 1200 SHRA TSRAGR BKN012CB 
EBBR 230920Z 09008KT 9999 FEW015 SCT018CB 17/16 Q1012 TEMPO VRB20G35KT 2000 SHRA TSRA BKN012CB 
EBBR 230950Z 11007KT 9999 -TSRA FEW017CB SCT034 17/16 Q1012 TEMPO VRB20G35KT 2000 SHRA TSRA BKN012CB
EBBR 231020Z 15006KT 9999 FEW017CB SCT034 18/17 Q1012 TEMPO 2500 SHRA TSRA BKN012CB
EBBR 231050Z 17008KT 140V200 9999 R25L/P2000N R25R/M0050VP2000D R02/P2000N FEW017CB SCT034 18/17 Q1013 TEMPO 2500 SHRA TSRA BKN012CB
EBBR 231120Z 15007KT 9999 R25L/P2000N R25R/M0050VP2000D R02/P2000N FEW026CB SCT044 19/18 Q1012 NOSIG
EBBR 231150Z 15008KT 120V180 9999 FEW028TCU SCT048 22/19 Q1012 NOSIG
EBBR 231220Z 17007KT 130V200 9999 FEW032TCU SCT048 22/19 Q1012 NOSIG
EBBR 231250Z 17009KT 140V200 9999 FEW042 23/18 Q1012 NOSIG 





23/08/2011 0854 NE. When the third thunderstorm (second MCS) moved towards the east edging my location, a typical chaotic sky belonging to a thundery weather was left behind.

 

23/08/2011 0954 W. When the fourth (and final) thunderstorm (third MCS) moved in it was preceded by a low rapid moving rolling cloud.

 

23/08/2011 0955 W. Wider view, sadly visibility was not that great and when approaching some cloud fragments in front of the roll began to form.

 

23/08/2011 0957 SW. View bit to the south when the roll cloud was almost overhead with very dark skies.

 

23/08/2011 1000 NNW. Roll cloud overhead.

 

23/08/2011 1002 N. Roll cloud overhead.

 

23/08/2011 1003 S. Opposite side where the sky was on its darkest.

 

23/08/2011 1012 N. Backside of the roll cloud.

 

The roll cloud with below very the dark skies was between 0954-1001 also captured on film and speeded up to 18 frames per second. 

 

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