2011 NHC Proving Ground Products Red-Green-Blue (RGB) Air Mass and Dust Products John Knaff 1.

Slides:



Advertisements
Similar presentations
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.
Advertisements

J.N. Kagenyi Senior Meteorologist RS/GIS IMTR-NAIROBI SWFDP NOV.2012.
APPLICATIONS OF METEOSAT SECOND GENERATION (Meteosat-8) AIRMASS RGB Jochen Kerkmann Satellite Meteorologist, Training Officer
Visible and Infrared (IR) Weather Satellite Interpretation 1. Visible satellite images are coded from black to white according to the amount of reflected.
 Bodies of air that bring distinctive weather features to the country.  A mass of air in air that is very uniform in temperature, pressure, and humidity.
Satellites and Radar – A primer ATMO 203. Satellites Two main types of satellite orbits – Geostationary Earth Orbiting Satellite is 35,786 km (22,236.
Water Vapour Imagery and
Air Masses Fronts Atmosphere map symbols Pressure.
Solar Energy and the Atmosphere. Earth-Sun Relationships Earth’s Motions Earth has two principal motions—rotation and revolution Earth’s Orientation (tilt)
Air Masses and Air Mass Weather
Canada’s Climate February 20,  Often defined as average weather, when weather means the current state of the atmosphere  Because of Canada’s size,
Satellite basics Estelle de Coning South African Weather Service
Weather Patterns.
Version 0.2, 16 January 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) SQUALL LINES Author:Jochen Kerkmann (EUMETSAT)
Chapter 8: Air Masses, Fronts Mid-Latitude Cyclones Air Masses  large body of air whose properties of temperature and humidity are fairly similar in any.
CLIMATE 5.8A.
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
Chapter 4 .1 What Causes Climate?
EARTH’S CLIMATE. Latitude – distance north or south of equator Elevation – height above sea level Topography – features on land Water Bodies – lakes and.
RGB Airmass and Dust products NASA SPoRT CIRA. RGB Air Mass RED (6.2 – 7.3) –vertical moisture distribution GREEN ( ) – tropopause height based.
DoD Center for Geosciences/Atmospheric Research at Colorado State University Annual Review April 17-19, Development of Satellite Products for the.
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,
RGB Activities for the GOES-R Proving Ground Gary Jedlovec, NASA / MSFC / SPoRT Mark DeMaria NOAA / NESDIS / STAR Tim Schmit NOAA / NESDIS / CIMSS and.
1 Air masses, Fronts, & Cyclones Extratropical Cyclone –Cyclone not in the tropics –Also known as Frontal Lows Frontal Cyclones Wave Cyclones Frontal Waves.
Cloud microphysics and precipitation through the eyes of METEOSAT SECOND GENERATION (MSG) Thomas Heinemann Meteorological Products Expert
Weather.
Version 1.0, 30 November 2004 Slide: 1 METEOSAT SECOND GENERATION (MSG) DUST DETECTION Author:Jochen Kerkmann Contributors:H.-J. Lutz.
Weather How do you determine the weather?. Weather Refers to the state of the atmosphere at a specific time and place. What does it look like outside.
This is because they would not be able to live in the hot sun and heat. They only come out in the night when it is a little cooler.
Air Masses and Fronts. What are air masses? Large Bodies of air Form when the air over a large region sits in one place for many days – The air gradually.
Purpose To deepen your knowledge of satellite images' interpretation  Preparation for the succeeding part about summer convection.
Air Masses and Fronts Meteorology. Air Masses Classified by temperature and humidity –Tropical: Warm, form in tropics, low pressure –Polar: cold, form.
Weather Patterns Air Masses and Fronts. Types of Fronts Cold front – a cold air mass overtakes a warm air mass ▫Type of Weather: clouds, possibly storms.
Next Week: QUIZ 1 One question from each of week: –5 lectures (Weather Observation, Data Analysis, Ideal Gas Law, Energy Transfer, Satellite and Radar)
EARTHS SYSTEMS. ATMOSPHERE Invisible layers of air primarily made up of Nitrogen (75%), Oxygen (20.9%), and Argon (.9%) gases.
WHAT IS WEATHER?  The weather is just the state of the atmosphere at any time, including things such as temperature, precipitation, air pressure and cloud.
Earth’s climate and how it changes
Version 1.0, 14 May 2004 Slide: 1 APPLICATIONS OF METEOSAT SECOND GENERATION (MSG) FOG DETECTION Author:Jochen Kerkmann (EUMETSAT)
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.
Introduction to atmosphere and weather
Shuddle and Atmosphere  Lego Shuttle reached an altitude of 35,000 meters. Which layers of the atmosphere did the shuttle reach before descending back.
METEOSAT SECOND GENERATION FROM FIRST TO SECOND GENERATION METEOSAT
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.
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.
TYPES OF AIR MASSES. TEMPERATURE TEMPERATURE HUMIDITY.
Lesson 26 What is an air mass?.
Air Masses. Air- What’s the Difference? Incoming solar radiation heats the air Not all places on Earth get the same amounts of solar radiation. Unequal.
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,
Divergent outflow from the convective cloud system in the airmass RGB, (WV6.2-WV7.3), WV6.2, WV7.3 images Mária Putsay and André Simon.
12010 McIDAS Users' Group Meeting Madison Wisc., October 2010 Using McIDAS-V to process data of EUMETSAT satellites for training and reach-out HansPeter.
Importance of the Atmosphere Earth's atmosphere is a mixture of gases that surrounds Maintains balance of heat Protects life forms from sun’s rays 1 1.
METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION
Best practices for RGB compositing of multi-spectral imagery
METEOSAT SECOND GENERATION (MSG) NIGHT-TIME CONVECTION
APPLICATIONS OF METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG)
devised by: D. Rosenfeld
Air Masses - Jet Stream - Pressure Systems
Air Masses - Jet Stream - Pressure Systems
METEOSAT SECOND GENERATION (MSG)
METEOSAT SECOND GENERATION (MSG) OVERVIEW MSG SEVIRI CHANNELS
METEOSAT SECOND GENERATION (MSG)
Presentation transcript:

2011 NHC Proving Ground Products Red-Green-Blue (RGB) Air Mass and Dust Products John Knaff 1

Red-Blue-Green (RGB) Products Air Mass MSG – Ch 5 (6.25µm), 6 (7.35µm), 8 (9.66µm), 9 (10.8µm) – R = WV WV7.35 (-25 to 0 K) – G = IR IR10.8 (-40 to +5 K) – B = WV6.25 (243 to 208 K) 1.Detect the position of jet streams and areas of dry descending stratospheric air with high PV (red areas) 2.Discriminate tropical air masses (i.e., rich-ozone tropical air mass vs. low- ozone polar air mass) 3.Discriminates subtropical air masses (dryer subtropics vs. moister tropics) 4.Detect typical WV features like cold lows, deformation zones and wave features 5.Clouds heights can also be inferred by brightness Dust/Microphysics MSG – Ch 7 (8.7µm), 8 (9.66µm), 9 (10.8µm), 10 (12.0µm) – R = IR10.8 – IR12.0 (-2 to 4 K) – G = IR10.8- IR8.7 (0 to +15 K, γ=2.5) – B = IR10.8 (261 to 289 K) 1.Dust appears as purple, pink or magenta 2.Generally thicker dust clouds appear as dark magenta or purple 3.Level, thickness, and phase (ice/water) can be inferred. 4.Animation helps to confirm moving features 2

RGB Airmass Product Interpretation of Colors Thick, high-level clouds Thick, mid-level clouds Thick, low-level clouds (warm airmass) Thick, low-level clouds (cold airmass) Jet (high PV) Cold Airmass Warm Airmass Warm Airmass Deeper Moisture Shallower Moisture Copyright EUMETSAT 3

Dust Microphysics:Interpretation of Colors for Low/Mid-level Clouds Ocean Warm Desert Cold Desert Warm Land Cold Land Thick, mid-level cloud Thin, mid-level cloud Low-level cloud (cold atmosphere, Europe) Low-level cloud (warm atmosphere, Africa) Dust Storm Night day Copyright EUMETSAT Day Cold, thick, high-level clouds Thin cirrus clouds / contrails over vegetated land/ocean over sand desert Ocean Warm Desert Cold Desert Warm Land Cold Land Dust Microphysics: Interpretation of Colors for High-level Clouds 4

Limb effects Warm moist Warm dryer Cooler airmass Hot Dry 5

DUST – hot background Low clouds Over ocean High cloud Mid-level clouds 6