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Uncertainty information in climate data records from Earth observation

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Figure

Figure 1. The benefit of pixel-level uncertainties in assimilating aerosol optical depth (AOD) estimated at 550 nm into the MonitoringAtmospheric Composition and Climate (MACC) model
Figure 2. Contribution to the overall uncertainty from differenterror sources for different spatio-temporal scales of analysis of aclimate data record (CDR)
Figure 3. Distributions of single-pixel brightness temperature (BT) errors from a simulation for the detection and calibration system of anadvanced very high resolution radiometer (AVHRR) for channels of different wavelength (columns) and two scene tempera
Figure 4. Simulation of locally correlated errors in the retrieval ofsea surface temperature (SST) overlaid with surface pressure con-tours to indicate length scales of atmospheric variability
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