| Резюме: | Analysing satellite datasets over large regions may introduce spurious relationships between aerosol and cloud properties due to spatial variations in aerosol type, cloud regime and synoptic regime climatologies. Using MODerate resolution Imaging Spectroradiometer data, we calculate relationships between aerosol optical depth Ta, derived liquid cloud droplet effective number concentration Ne and liquid cloud droplet effective radius re at different spatial scales. Generally, positive values of dlnNe/dlnTa are found for ocean regions, whilst negative values occur for many land regions. The spatial distribution of dlnNe/dlnTa shows approximately the opposite pattern, with generally positive values for land regions and negative values for ocean regions. We find that for region sizes larger than 4°x4°, spurious spatial variations in retrieved cloud and aerosol properties can introduce widespread significant errors to calculations of dlnNe/dlnTa and dlre/dlnTa. For regions on the scale of 60°x60°, these methodological errors may lead to an overestimate in global cloud albedo effect radiative forcing of order 80%.
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