Using surface and TOA reflectance uncertainties and aerosol type uncertainties to constrain estimates of uncertainties in retrieved aerosol optical depth from AVHRR
Microwave sensors are used to measure upper tropospheric humidity, but the temperature of the on-board calibration target may drift slowly over time making long-term measurements difficult. To solve this, we employ a second reference for calibrating measurements – the moon
A synopsis of different algorithms for propagating uncertainty into the climate data record, including a link to a demonstrator of the powerful Algorithmic Differentiation method.