The temporal and spatial spectrum of the cloud-light environment can vary considerably depending upon the local, regional, and synoptic-scale climate. For example, within the subtropics, trade wind cumulus clouds dominate, and the cloud fraction distribution peaks at 0.5. In the mid-latitudes, clouds fraction tends toward a bi-modal distribution--most of the time, it is either clear or cloudy (although there are seasonal and regional exceptions).
To accurately depict the long-term time-space cloud environment, high quality, high frequency, and high density measurements of irradiance are a necessity. As such observational networks are virtually non-existent, sophisticated statistical and modeling techniques are required to create the needed data. The methods described here focus less on matching the absolute insolation at a site at a given time, but rather attempt to match the relative changes in insolation over time. Thus the statistical characteristics (i.e. ramp distributions, power spectral densities) are comparable. Here, we present methodologies used to create representative irradiance and power output data sets for the two distinct climate regimes referenced above, more specifically, Hawaii and Ontario, Canada.