Radiation Protection Service University of Glasgow Lecture 2: Detecting Radiation Detecting Ionising Radiation James Gray University RPA.
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Figure 1: Using GERB and SEVIRI data to evaluate the Met Office NWP model in near-real time; example SINERGEE comparisons for 8 th March 2006 at 1200 UTC.
Robin Hogan, Julien Delanoë, Nicola Pounder, Nicky Chalmers, Thorwald Stein, Anthony Illingworth University of Reading Thanks to Alessandro Battaglia and.
SYSTEMATIC BIASES 3-hourly comparisons of top of atmosphere radiation from GERB and the Met Office global forecast model Systematic biases in model fluxes.
Robin Hogan Ewan OConnor Anthony Illingworth Nicolas Gaussiat Malcolm Brooks Cloudnet Evaluating the clouds in European forecast models.
THE ATMOSPHERE. Earths Atmosphere The Earths atmosphere is a thin layer of air that forms a protective covering around the planet. This layer of gas maintains.
Chapter 15 Section 2 Heating of the Atmosphere. Energy in the Atmosphere Radiation is the transfer of energy as electromagnetic waves 50% of the sun’s.
Chapter 3 Section 2 ppt
DKIST- Thermal Management 2015_Gorman_VFinal
1 EUMETSAT SAF NETWORK Lothar Schüller, EUMETSAT SAF Network Manager.
Remote Sensing Remote Sensing requires the following: 1. Electromagnetic Energy Source 2. Interaction with a Target 3. Sensor to Record Energy.