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Deep convection 2 Wilfried Jacobs DWD Meteorological Training and Conference Centre.

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Presentation on theme: "Deep convection 2 Wilfried Jacobs DWD Meteorological Training and Conference Centre."— Presentation transcript:

1 Deep convection 2 Wilfried Jacobs DWD Meteorological Training and Conference Centre

2 Purpose To enable you to interpretate small and meso scale structures in radar images  identification of relevant structures  corresponding conceptual model  ( related weather)

3 Pre-requesites Pre-reading of material in relation to "Deep convection Part 2".

4 Content 1.Quiz based upon self study 2.Detailed investigations of radar images –(mainly super cells in relation to conceptual models and "weather") Intensities Doppler 3.Quiz (time depending) 4.Questions & answers

5 1. Quiz (self study)

6 Single cell: Please, mark the correct answer(s) ( )

7 Multi cell: Please, mark the correct answer(s) ( ) Blueish: high reflectivities

8 Super cell: Please, mark the correct answer(s) Blueish: high reflectivities

9 Please, mark the correct answer(s) ( ) Blueish: approaching Redish-pink: veering away

10 Please, mark the correct answer(s) ( ) Blueish: approaching Redish-pink: veering away

11 2. Examples  conceptual models (Many Images from Peter Lang (DWD))

12 Super cells

13 Radar Berlin: 03 July 2003, around 15 UTC 1 km 3 km + 15 Min R R 2 km

14 Weak meso cyclone (06 June 2002, around 15 UTC, Feldberg / Black forrest) Erroneous pixel?  animations! 2 km 1 km Ra Rotation about 12m/s 6 km Ra

15 18:25 Tornado of Wittenberg, 12.06.02, 18:15 No extreme dBz R 2 km Rotation about 20 m/s

16 Hail near Munich (23 June 2008, about 13 UTC)

17 Hail near Munich (23 June 2008, around 13 UTC) "tilted tower", hail in the upper part Tornado possible

18 Hail near Munich (23 June 2008, around 13 UTC) Anvil Prec, light at surface Storm motion WER

19 Fine structures in super cells (dBz) 2 km 3 km 6 km 12 km WER / inflow / strong echo gradient (horizontal) hook echo WER/ strong echo gradient (vertical) Updraft Outlow FL : flanking line RFD: rear-flank downdraft (often as Hook-echo) FFD: Forward flank downdraft Top: 12 km FFD RFD FL

20 Fine structures in super cells (Doppler) 2 km 4 km 6km 9 km 12 km RFD inflow RR partly folding

21 Mini Tornado (15 June 2007, 16:15 UTC) 2 km radar Munich R 2 km, radar HP No clear rotation, line orientated shear stronger R

22 Squall line

23 Hazardous weather over Southwest Germany (30 May 2008, 01 UTC) Gustline 3 km R R Folding Gusts at least: (please tick ): < 20 m/s < 30 m/s > 35 m/s 2 km

24 Single / multi cells

25 20:26 20:41 20:56 21:11 8 km CON (1 km)DIV (8 km) DIV 1 km Weakening of a convective cell

26 Quiz

27 Where do you expect a flanking line? (please mark ( )) 2 km 3 km

28 Where do you expect a WER ? (please mark ( )) 2 km 3 km WER

29 6 km FL : flanking line RFD: rear-flank downdraft (often as Hook-echo) FFD: Forward flank downdraft Where do you find the outflow with possibly precipitation hail (please mark ( ))?

30 Where do you expect the highest risk to tornado ? (please mark ( )) Tornado possible

31 Difficult: Where is the inflow (please mark ( ))? 2 km R

32 Where do you expect the outflow and possible precipitation (please mark ( )) 6km R

33 Comming next "My Part deep convection 3" –Practical nowcasting Potential and weaknesses of data types (NWP, satellite, obs, radar) during nowcasting process Case studies among other during class room part

34 Thank you! Question?


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