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METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION

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Presentation on theme: "METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION"— Presentation transcript:

1 METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION
APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION Author: Jochen Kerkmann (EUMETSAT) Contributors: A. Canessa (Meteo AM)

2 MSG SEVIRI CHANNELS USEFUL TO MONITOR CONVECTION
PART 1: MSG SEVIRI CHANNELS USEFUL TO MONITOR CONVECTION NIGHT-TIME

3 Recommended Channels WV6.2 upper-level moisture WV7.3 mid-level moisture, early convection IR10.8 top temperature

4 Click on the image to see the animation !
IR10.8 Top Temperature Click on the image to see the animation ! Squall Line over Western Africa causing violent rainfall and sandstorms MSG-1, 14 July 2003, 02:00-08:45 UTC, IR10.8

5 CHANNEL DIFFERENCES USEFUL TO MONITOR CONVECTION
PART 2: CHANNEL DIFFERENCES USEFUL TO MONITOR CONVECTION NIGHT-TIME

6 Recommended Differences
IR3.9 - IR10.8 particle size, phase IR8.7 - IR10.8 optical thickness IR IR10.8 optical thickness WV6.2 - IR10.8 overshooting tops WV6.2 - WV7.3 overshooting tops

7 RED-GREEN-BLUE (RGB) COLOUR COMPOSITES FOR MONITORING CONVECTION
PART 3: RECOMMENDED RED-GREEN-BLUE (RGB) COLOUR COMPOSITES FOR MONITORING CONVECTION NIGHT-TIME

8 Recommended RGBs Night-time
Red: Cloud optical depth, approximated by the mm or brightness temperature. Green: Cloud particle size and phase, approximated by the mm brightness temperature. Blue: Temperature, provided by 10.8 mm brightness temperature.

9 Typical Convective Development - Nighttime -
I. Very early stage white white white light grey (low, warm water cloud) opt thick opt thick low water warm II. First convection* white white light grey dark grey (first convective towers) opt thick supercooled supercooled cold water water III. First icing white grey b/w noise black (transformation in Cb) opt thick ice cloud very cold very cold IV. Large icing white grey b/w noise black (Cb anvils) opt thick ice cloud very cold very cold *This phase is more frequent in Africa, i.e. it is more easy to find examples for this phase in tropical convection

10 RGB 10-09 / 09-04 / 09 Red Green Blue 12.0-10.8 10.8-3.9 10.8 RGB
I. Very early stage white-light yellow II. First convection light brown III. First icing /255 0 red-yellow IV. Large icing /255 0 red-yellow

11 5 8 9 3 7 4 MSG-1 11 November 2003 03:00 UTC RGB Composite
1. Desert quartz sands. 2. Desert soil. 3. Sea surface. 4. Sc with small drops. 5. Supercooled water layer clouds, no precip. 6. Lightly precip. cu. 7. Cb with lightning. 8. Deep convection, growing zone. 9. Deep convection, dissipation zone. 10. Thick cirrus. 11. Thin cirrus. 5 8 9 3:13 3 7 4 MSG-1 11 November 2003 03:00 UTC RGB Composite R = IR12.0-IR10.8 G = IR10.8-IR3.9 B = IR10.8 6 5 5 11 2 1 2 10 1

12 MSG-1 23 April 2003 19:00 UTC RGB Composite R = IR12.0-IR10.8 G = IR10.8-IR3.9 B = IR10.8

13 MSG-1 8 June 2003 19:30 UTC RGB Composite R = IR12.0-IR10.8 G = IR10.8-IR3.9 B = IR10.8

14 PART 4: EUROPEAN EXAMPLES

15 Severe Hailstorm Padova-Treviso (I)
28 August 2003

16 MSG-1, 28 August 2003, RGB Composite
16:30 UTC :30 UTC MSG-1, 28 August 2003, RGB Composite R=IR12.0-IR10.8, G=IR10.8-IR3.9, B=IR10.8

17 MSG-1 28 August 2003 17:30 UTC RGB Composite R = IR12.0-IR10.8 G = IR10.8-IR3.9 B = IR10.8

18 PART 5: AFRICAN EXAMPLES

19 Convection Ghana 23 April 2003

20 Thin Cirrus MSG-1 23 April 2003 19:00 UTC Severe Convection
Channel 09 BT (IR10.8) Severe Convection BT [K]

21 Click on the image to see the animation !
MSG-1 23 April 2003 19: :30 UTC Channel 09 BT (IR10.8)

22 MSG-1 23 April 2003 19:00 UTC Difference Image IR3.9 - IR10.8

23 MSG-1 23 April 2003 19:00 UTC Difference Image IR8.7 - IR10.8

24 MSG-1 23 April 2003 19:00 UTC Difference Image IR IR10.8

25 MSG-1 23 April 2003 19:00 UTC RGB Composite R = IR12.0-IR10.8 G = (IR3.9-IR10.8)i B = IR10.8

26 MSG-1 23 April 2003 19:00 UTC RGB Composite R = IR10.8-IR8.7 G = (IR3.9-IR10.8)i B = IR10.8

27 MSG-1 23 April 2003 19:00 UTC RGB Composite R = IR3.9-IR10.8 G = IR8.7-IR10.8 B = IR12.0-IR10.8


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