R = Channel 02 (VIS0.8) G = Channel 04r (IR3.9, solar component) B = Channel 09 (IR10.8) Day Microphysics RGB devised by: D. Rosenfeld Applications: Applications:Cloud.

Slides:



Advertisements
Similar presentations
Sequence for a cyclonic storm over western Europe Comparison with weather radar maps The radar images were provided by the INM, Spain, Dr Miguel A. Martinez.
Advertisements

Version 1.0, 30 June 2004 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB IMAGES: PART 05 RGB COMPOSITES WITH CHANNEL 12 AND THEIR INTERPRETATION.
Slide: 1 Version 0.3, 20 January 2004 METEOSAT SECOND GENERATION (MSG) METEOROLOGICAL USE OF THE SEVIRI HIGH-RESOLUTION VISIBLE (HRV) CHANNEL Contact:Jochen.
Version 0.6, 30 June 2004 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB IMAGES: PART 04 RGB COMPOSITES WITH CHANNELS AND THEIR INTERPRETATION.
Slide: 1 Version 1.1, 30 June 2004 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) METEOROLOGICAL USE OF THE SEVIRI IR3.9 CHANNEL Author:Jochen Kerkmann.
Precipitation Products PPS Anke Thoss, SMHI User Workshop, February 2015, Madrid.
Precipitation development; Warm and Cold clouds >0 ° C
APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB COMPOSITES WITH CHANNEL 12 AND THEIR INTERPRETATION.
Version 1.0, 30 November 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) HURRICANES AND TROPICAL CYCLONES Author:Jochen Kerkmann (EUMETSAT)
APPLICATIONS OF METEOSAT SECOND GENERATION (Meteosat-8) AIRMASS RGB Jochen Kerkmann Satellite Meteorologist, Training Officer
2011 NHC Proving Ground Products Red-Green-Blue (RGB) Air Mass and Dust Products John Knaff 1.
Image Interpretation for Weather Analysis Part 2 26 October 2010 Dr. Steve Decker.
Image Interpretation for Weather Analysis Part 2 27 February 2008 Dr. Steve Decker.
Incorporating Meteosat Second Generation Products in Season Monitoring Blessing Siwela SADC Regional Remote Sensing Unit November
Satellite basics Estelle de Coning South African Weather Service
Also called fair weather clouds and look like floating cotton Have very flat bases and are not very tall When first formed from droplets, they have.
Version 0.2, 16 January 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) SQUALL LINES Author:Jochen Kerkmann (EUMETSAT)
Version 1.0, 30 June 2004 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB IMAGES: PART 1 OVERVIEW MSG SEVIRI CHANNELS Author:Jochen Kerkmann (EUMETSAT)
Meteorolojik Uzaktan Algılamaya Giriş Erdem Erdi Uzaktan Algılama Şube Müdürlüğü 7-8 Mayıs 2012, İzmir.
Jochen Kerkmann Satellite Meteorologist, Training Officer
Applications of the SEVIRI window channels in the infrared
Basics Satellite Meteorology ( An Introduction to RS of MSG) Joseph Kagenyi Kenya Meteorological Department.
Version 1.0, 20 April 2005 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB IMAGES: PART 04 RGB COMPOSITES WITH CHANNELS AND THEIR INTERPRETATION.
MSG Red-Green-Blue(RGB) combinations Estelle de Coning South African Weather Service Most slides taken from EUMETSAT training events, Jochen Kerkmann 1.
Version 1.0, 30 November 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) SQUALL LINES Author:Jochen Kerkmann (EUMETSAT)
R = Channel 03 (NIR1.6) G = Channel 02 (VIS0.8) B = Channel 01 (VIS0.6) Day Natural Colours RGB devised by: D. Rosenfeld Applications: Applications:Vegetation,
Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB COMPOSITES WITH CHANNELS AND THEIR INTERPRETATION Authors:J. Kerkmann, HP. Roesli,
Clouds and Cloud Formation. What is a cloud? A cloud is a collection of small water droplets or ice crystals suspended in the air. They are visible because.
Version 0.8, 03 February 2005 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB IMAGES: PART 03 CHANNEL SELECTION AND ENHANCEMENTS Author:Jochen Kerkmann.
Cloud microphysics and precipitation through the eyes of METEOSAT SECOND GENERATION (MSG) Thomas Heinemann Meteorological Products Expert
Version 1.0, 30 November 2004 Slide: 1 METEOSAT SECOND GENERATION (MSG) DUST DETECTION Author:Jochen Kerkmann Contributors:H.-J. Lutz.
Purpose To deepen your knowledge of satellite images' interpretation  Preparation for the succeeding part about summer convection.
A cloud is a visible aggregate of tiny water droplets and/or ice crystals suspended in the atmosphere They can exist in a variety of shapes and sizes.
Chapter 7 Clouds A cloud is a collection of small water droplets or ice crystals suspended in the air, which forms when the warm air is cooled and condensation.
Water Vapor in the air Clouds Water falling from the.
Water in the Atmosphere + Weather Chapter Latent heat – Evaporation (__  ___)& Condensation (__  ___) Sublimation – Deposition NO LIQUID PHASE!
Version 1.0, 14 May 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) FOG DETECTION Author:Jochen Kerkmann (EUMETSAT)
Clouds. Water is strange stuff! Gas - water vapour (invisible) Liquid - water droplets (visible) Solid - ice crystals, hail, snow Water can occur in 3.
Clouds and Precipitation
Science 10: Mr. Jean January 12 th, The plan: Video clip of the day Atmospheric Layers Aurora Clouds BBC – Deep Freeze.
METEOSAT SECOND GENERATION FROM FIRST TO SECOND GENERATION METEOSAT
Lecture 5 Precipitation (2) Clouds Weather Systems Global Precipitation Patterns Regional Precipitation Patterns.
Cloud Terminology Cumulus = heap Stratus = layer Cirrus = curl of hair
UNDERSTANDING CONVECTIVE CLOUDS THROUGH THE EYES OF METEOSAT SECOND GENERATION (MSG) Jochen Kerkmann Satellite Meteorologist, Training Officer
Cloud property retrieval from hyperspectral IR measurements Jun Li, Peng Zhang, Chian-Yi Liu, Xuebao Wu and CIMSS colleagues Cooperative Institute for.
Clouds Ice cloud detection using the 8.7  m channel: areas of ice clouds (in particular thin cirrus) are red (positive difference), clear ground and water.
Version 1.1, 02 February 2005 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) SNOW DETECTION Author:J. Kerkmann (EUMETSAT)
Detecting Lee and Barrage clouds using Meteosat 8 Contact person: Jarno Schipper Version August 2005.
Slide: 1 R = Difference WV6.2 - WV7.3 G = Difference IR3.9 - IR10.8 B = Difference NIR1.6 - VIS0.6 RGB 05-06, 04-09, ("Day Convective Storms") devised.
Version 0.3, 20 January 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) DAY-TIME CONVECTION Author:Jochen Kerkmann (EUMETSAT)
Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) RGB COMPOSITES WITH CHANNELS AND THEIR INTERPRETATION Authors:J. Kerkmann, HP. Roesli,
Cirrus Clouds : feathery, light, usually composed of Ice crystals High altitude where it is usually very dry and cold.
Day Convective Storm RGB Detection of Cumulonimbus Cloud
METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION
METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG)
Best practices for RGB compositing of multi-spectral imagery
METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION
METEOSAT SECOND GENERATION (MSG)
APPLICATIONS OF METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG)
devised by: D. Rosenfeld
devised by: D. Rosenfeld
METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG)
APPLICATIONS OF METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG) OVERVIEW MSG SEVIRI CHANNELS
APPLICATIONS OF METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG)
Presentation transcript:

R = Channel 02 (VIS0.8) G = Channel 04r (IR3.9, solar component) B = Channel 09 (IR10.8) Day Microphysics RGB devised by: D. Rosenfeld Applications: Applications:Cloud Analysis, Convection, Fog, Snow, Fires Area: Area:Full MSG Viewing Area Time: Time:Day-Time

Recommended Range and Enhancement: BeamChannelRangeGamma Red02 (VIS0.8)0 …+100 %1.0 Green04r (IR3.9r) %2.5 Blue09 (IR10.8) K1.0 Day Microphysics RGB devised by: D. Rosenfeld

R = Difference VIS0.8 Optical Thickness, Viewing Geometry G = Difference IR3.9r Optical Thickness, Phase, Particle Size, Viewing Geometry B = Channel IR10.8 Top Temperature Physical Interpretation (for dust/ash/water/ice clouds)

Interpretation of Colours for High-level Clouds Deep precipitating cloud (precip. not necessarily reaching the ground) - bright, thick - large ice particles - cold cloud Deep precipitating cloud (Cb cloud with strong updrafts and severe weather)* - bright, thick - small ice particles - cold cloud *or thick, high-level lee cloudiness with small ice particles Thin Cirrus cloud (large ice particles) Thin Cirrus cloud (small ice particles) Ocean Veg. Land Fires / Desert Snow

Interpretation of Colours for Mid-level Clouds Supercooled, thick water cloud - bright, thick - large droplets Supercooled, thick water cloud - bright, thick - small droplets Supercooled thin water cloud with large droplets Supercooled, thin water cloud with small droplets * * or, in rare occasions, thin Ci cloud with small ice particles Ocean Veg. Land Fires / Desert Snow

Interpretation of Colours for Low-level Clouds Thick water cloud (warm rain cloud) - bright, thick - large droplets Thick water cloud (no precipitation) - bright, thick - small droplets Thin water cloud with large droplets Thin water cloud with small droplets Ocean Veg. Land Fires / Desert Snow

Example 1: Severe Convection MSG-1, 13 June 2003, 12:00 UTC

Example 2: Ship Trails MSG-1, 17 January 2006, 13:00 UTC

Example 3: Fires MSG-1, 27 April 2004, 14:15 UTC

MSG-1, 8 October 2003, 12:00 UTC ice mixed water ice Example 4: Ice vs Water Clouds

MSG-1, 26 August 2005, 12:00 UTC ice water Example 5: Ice vs Water Clouds

0.8  m 3.9r  m 10.8  m Cb -32C Fog St AC Snow 10.8  m Cb -32C Fog St AC Snow Ci 10.8  m Cb -32C Fog St AC Snow 10.8  m Cb -32C Fog St AC Snow Ci 10.8  m Cb -32C Fog St AC Snow 10.8  m Cb -32C Fog St AC Snow Ci Example 6: Cloud Analysis

Maputo MSG-1, 6 November 2004, 12:00 UTC Thin Ice Cloud (small ice) Thick Ice Cloud (small ice) Thick Ice Cloud (large ice) Thin Ice Cloud (large ice) Example 7: Small vs Large Ice Particles

MSG-1, 19 March 2007, 08:00 UTC Very cold clouds (lee cloudiness) with small ice particles Example 8: Lee Cloudiness

MSG-1, 8 November 2005, 12:00 UTC Example 9: Frontal Clouds

Example 9: Comparison with Dust RGB MSG-1, 8 November 2005, 12:00 UTC

MSG-1, 26 May 2007, 16:29 UTC Example 10: Low Light Conditions