Modelling the interaction of sunlight with the Earth

View of Parque Nacional Patagonia, Chile, rendered using Eradiate Credit: Rayference

Radiative transfer models are computer programs that are used to help understand how energy from the sun interacts with the Earth’s surface and atmosphere. These vary in complexity and are often designed for a single task, meaning that comparing their outputs is difficult and few have been validated against the SI.

Challenge

Solution

Impact

Image showing polar bear on ice sheet

Metrology for SI traceable climate observations

Over half of the 55 Essential Climate Variables, used to predict how the Earth’s climate is evolving, has a space-based contribution. The MetEOC series of projects: • MetEOC (2011-2014) improved NMI calibration facilities, including ones used to calibrate instruments in the field. • MetEOC-2 (2014–2017) improved performance of an originally lab-based cryogenic solar radiometer to enable improvements of measurements of incoming solar radiation by a factor of 10 and developed standards and instrumentation for the characterisation of large areas of ocean, vegetation and desert, used to confirm satellite-borne instrumentation performance. • MetEOC-3 (2017-2021) integrated tuneable laser methods into calibration facilities such as STAR, to allow enhanced calibrations of spectroscopic instruments, for example, to retrieve localised measurements of CO₂. • MetEOC-4 (2020-2023) further improved the accuracy of calibration facilities, developing new instrumentation and standards to allow more comparable data on sky radiance from ground-based networks. These results will provide trustworthy evidence to policy makers and help timely and measured mitigation strategies to be implemented.

  • Category
  • EMPIR,
  • Environment,
  • EMN Climate and Ocean Observation,