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Radar Meteorology Glossary
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Attenuation by precipitation
The equation
dBZc = dBZ + 2Cr
Σ
(Z
E
) is used for getting corrected values of
attenuation
by precipitation.
Example Image
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Radar Meteorology Glossary
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Dictionary of products
Dictionary of Dual Polarimetric products
Knobology of NRP 2.0
Guide to the Meteorological Use of URP 2.2
Canadian Radar Products (and some European)
A Note About Colours
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Radar Fundamentals
Radar Interpretation
Radar Applications
Technical Support Chat
Radar Introduction
Historical Development
International Weather Radar Distribution
Types of Radar
Radar Components
Radar Bands
The Radar Beam
Reflectivity and Precipitation Measurements
Measurement Issues
Radar Signatures
Pre-study Quiz
Radar Course Introduction
Recording of Presentation
Scan Strategies and Basic Products
Recording of Presentation
Polarimetric Radar
Interpretation Issues
Recording of Presentation
Non-Meteorological Returns
Recording of Presentation
Doppler Basics - Pre-study Notes
Doppler Basics - Power Point
Recording of Presentation
Radar Algorithms
Radar Algorithms - Powerpoint
Radar Algorithms - Recording
Warm Fronts
Warm Fronts - Powerpoint
Warm Fronts - Pure Snow Case - Recording
Powerpoint Presentation
Recording of Presentation
Cold Fronts
Powerpoint Presentation
Recording of Presentation
Principles of Convection I: Buoyancy and CAPE
Principles of Convection II: Using Hodographs
Principles of Convection III: Shear and Convective Storms
Powerpoint Presentation
Powerpoint Presentation
Recording of Presentation
Homework Assignment
Reflectivity Calculation
Reflectivity
Powerpoint Presentation
Recording of Presentation
Map to Hotel
Map from Hotel to Forecast Office
Restaurants in the Local Area
Around Edmonton
Edmonton Highlights
10 June 2008
Noel 2007
Fire Detection
Convective Storm and Frontal Systems
The use of profilers and VAD to study split cold fronts
Rain Rate Estimation from Dual-Polarisation Radar Observations
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