COROBOR designs software for Aviation & Meteorology for 16 years.

Slides:



Advertisements
Similar presentations
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200.
Advertisements

$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500.
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
© Crown copyright Met Office WAFC CAT verification Objective verification of GRIB CAT forecasts Dr Philip G Gill, WAFC Science Meeting, Washington, 20.
Larry Burch, WAFC Washington Nigel Gait, WAFC London
GRIB Visualization of data
15th Septmeber 2009 Chart 0 WAFS Workshop – Paris 2009 MET Services, Hans-Rudi Sonnabend Application of WAFS Products Hans-Rudi Sonnabend Lufthansa System.
Chapter 13 – Weather Analysis and Forecasting
Pilots & Weather Considerations Federal Aviation Administration 1.
Jet Stream Compression Turbulence Mountain wave Icing IFR ceiling and visibility CWSU Products MIS CWA PIREPS Questions and Comments Created 9/14/2008.
Joseph Kagenyi IMTR-NAIROBI Adopted from MSG Interpretation guide.
WAFS Workshop on the Use and Visualisation of Gridded SIGWX Forecasts, Paris, New WAFC Gridded Products = New Visualisation Opportunities.
METEOROLOGICAL SERVICES FOR LOW LEVEL FLIGHTS IN ROMANIA
BASIC REGULATIONS OF METEOROLOGICAL SERVICE FOR LOW-LEVEL FLIGHTS IN THE RUSSIAN FEDERATION User Consultation Workshop Meteorological Service for Low Level.
History of IATA requirements for gridded ICE, TURB and CB Cloud Products.
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.
 nm)  nm) PurposeSpatial Resolution (km) Ozone, SO 2, UV8 3251Ozone8 3403Aerosols, UV, and Volcanic Ash8 3883Aerosols, Clouds, UV and Volcanic.
Accessing and Interpreting Web-based Weather Data Clinton Rockey National Weather Service Portland, Oregon.
ASII-NG: Developments and outlook NWCSAF 2015 Users Workshop.
Viewing and Depicting the Atmosphere MODIS 03 FEB UTC
1 Conceptual Models (CMs): Cold Air Cloudiness (CAC), Enhanced Cumulus (EC ) and Comma How to use MSG satellite images similarities to and improvements.
Visible and Infrared (IR) Weather Satellite Interpretation 1. Visible satellite images are coded from black to white according to the amount of reflected.
SCIENCE NEWS Magnitude CENTRAL ITALY Magnitude CENTRAL ITALY.
Hayden Oswald 1 and Andrew Molthan 2 NASA Summer Intern, University of Missouri, Columbia, Missouri 1 NASA SPoRT Center, NASA/MSFC, Huntsville, Alabama.
Forecasting Weather After completing this section, students will analyze weather maps and the resulting regional weather (Standard PI – 061)
The Do It Yourself Internet Weather Briefing With thanks to Sam Zimmerman Start with the Big Picture General Synoptic Situation Likely cloud cover Precip,
SkyScope: An Aviation Weather Visualization Tool CPSC 533C Final Report Wesley Coelho Bertrand Low April 21, 2004.
How do we measure and forecast the weather?. Radar images can detect areas of rainfall and how heavy it is. RAINFALL.
Verification of WAFS Global Icing Products Jennifer Mahoney 1 and Sean Madine 1,2 1 NOAA/Earth System Research Laboratory 2 Cooperative Institute for Research.
NOAA FAA-NWS Aviation Weather Weather Policy and Product Transition Panel Friends and Partners in Aviation Weather October 22, 2014.
Color. -Visual light -An integral part of the sculpture -Creates desired effect -Distinguish items -Strengthen interest.
Section 12.3 Gathering Weather Data
20.5 Forecasting Weather Objectives
Uses of Telecommunications & ICT Weather Forecasting.
Color and Resolution Introduction to Digital Imaging.
TOPTHERM TopTask TopTask Competition Modern meteorological forecasting tools for gliding activities.
Blended Course on the Principles of Satellite Meteorology 21 st April – 15 th July 2009 Classroom June 2009 Final Presentation – Convection – 09May2009.
Weather Briefings Wisconsin Balloon Group March 11, 2006 Brad Temeyer
Lesson 5 – Predicting the Weather © Brent Coley 2010 |
GOES IMAGERY APPLICATIONS at the AVIATION WEATHER CENTER Steverino Silberberg NOAA/NWS/NCEP/Aviation Weather Center Kansas City, MO January 24, 2008.
Severe turbulence cases NOMEK Aviation requirements ICAO Annex 3 – “The objective of meteorological service for international air navigation shall.
GOES-R ABI Synthetic Imagery at 3.9 and 2.25 µm 24Feb2015 Poster 2 Louie Grasso, Yoo-Jeong Noh CIRA/Colorado State University, Fort Collins, CO
Do Now: Do Not Log In. Take out your notebook and a pen. Good morning! Do Now: Do Not Log In. Take out your notebook and a pen. Good morning! Aim: Review.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Weather and meteorology npor. Tereza Holubova. CONTENT Meteorological phenomena influencing aviation turbulence wind precipitation, icing clouds visibility.
© Crown copyright Met Office GA Met provision, UK Met Office Jonathan Dutton, Operations Centre, Met Office, UK.
Color Web Design Professor Frank. Color Displays Based on cathode ray tubes (CRTs) or back- lighted flat-screen Monitors transmit light - displays use.
Weather and Meteorology
Modeling GOES-R µm brightness temperature differences above cold thunderstorm tops Introduction As the time for the launch of GOES-R approaches,
1 Conceptual Models (CMs): Cold Air Cloudiness (CAC), Enhanced Cumulus (EC ) and Comma How to use MSG satellite images similarities to and improvements.
An Examination Of Interesting Properties Regarding A Physics Ensemble 2012 WRF Users’ Workshop Nick P. Bassill June 28 th, 2012.
MeteoExpert workstation.Visualization of new gridded forecasts MeteoExpert workstation. Visualization of new gridded forecasts.
Exercise1 You will find; 1.Fog / Stratiform Cloud 2.Cb / Cg 3.Transverse Line 4.Upper level flow 5.Jet stream, upper level vortex… 6.Lower level flow 7.Tropical.
Methodology n Step 1: Identify MOG (EDR ≥ 0.25) observations at cruising altitude (≥ FL250). n Step 2: Account for ascending/descending flights by filtering.
Experience in numerical forecast verification in the Hydrometeorological Centre of Russia N. P. Shakina, E. N. Skriptunova, A. R. Ivanova Zürich 2005 COSMO.
Atmospheric Motion Vectors - CIMSS winds and products (
Clouds General Information Cloud types (Low, Medium & High) Special Clouds.
© 2009 Aviation Supplies & Academics, Inc. All Rights Reserved. The Pilot’s Manual – Ground School Weather Chapter 15 Clouds and Thunderstorms.
Add to table of Contents Atmosphere LayersPg. 76 AtmospherePg. 77.
Chapter 20 Section 5 Forecasting Weather Objectives: -Compare and contrast the different technologies used to gather weather data -Analyze weather symbols,
INDOOR SKATEBOARD PARK
“Friends/Partners in Aviation Weather” Forum NBAA Convention – Orlando
METEOROLOGICAL SERVICES FOR LOW LEVEL FLIGHTS IN ROMANIA
Forecasting the Weather for RU27’s Recovery Mission Justin Ash and Nilsen Strandskov Part of the preparation process for the recovery of RU27, The Scarlet.
Background Decisions leading to the development of gridded forecasts of CB clouds, icing and turbulence Olli Marius Turpeinen Chief MET/AIM Section, ICAO.
Yuliya Naryshkina METEOAGENCY OF ROSHYDROMET
Potential Temperature (K)
What Color is it?.
MODIS Polar Winds Forecast Impact (3DVAR) Northern Hemisphere
Weather Briefing for Pigeon Racing
Presentation transcript:

COROBOR designs software for Aviation & Meteorology for 16 years. 480 MESSIR-AERO Workstations for Pilot Met Briefing are currently operational around the world. This presentation will show some MESSIR-AERO outputs for: Global Gridded Elements (wind direction, temperature...). The New Gridded Elements.

A SIGWX chart is based on information extracted from thinned GRIB information and data from WAFC regarding max wind speed, tropopause and geopotential.

Jet stream core position and height are extracted from WAFC GRIB data Jet stream core position and height are extracted from WAFC GRIB data. The same data source is used for tropopause level. The software determines jet core position, altitude and speed based on the max wind speed and associated heights.

The necessary information for users is available on single layer or multiple layers. In order to have a complete image, a multi-layer display is extremely suggestive and can be used at a glance. Maximum CAT potential

RGB overlaying is extremely easy to interpret and, based on users’ suggestions, some of the layers can be compacted in display in order to have a broad image.

In the example below, the five levels of icing potential are displayed in three colors: blue for 700hPa, green for cumulative 600 / 500hPa and red for 400/300hPa.

The final image is very easy to analyze, taking into account the combinations of colors and intensities. As examples, bright white involves a high risk of icing at all levels and light yellow is showing icing at medium and high levels i.e. between 600 and 300 hPa.

Areas of significant weather and CB clouds are delimitated using five different thinned GRIB data types: CB tops / base, EMBD CB tops / base and CB extension. One of the alternative display modes regarding CB is similar to a satellite visible imagery.

Color intensity is directly correlated with the risk of icing or turbulence In case of icing: Cumulated icing risk at 700, 400 and 300hPa Cumulated icing risk between 700 and 400hPa Cumulated icing risk only at 400 and 300hPa Cumulated icing risk only at 600 and 500hPa Icing risk only at 700hPa Cumulated icing risk between 600 and 300hPa Cumulated icing risk at all levels

Icing risk at all levels Icing risk only at 600 and 500hPa Cumulated icing risk at 700, 400 and 300hPa Icing risk between 600 and 300hPa Icing risk only at 700hPa

THANK YOU