Some of the many systematic effects in solar observations as sensed by a Davis VP2 solar sensor and logged by Cumulus may be reviewed in these images from the Cumulus history for my station in Albuquerque New Mexico.
Clear day near Winter solstice

Clear day near Summer solstice

Almost clear day near spring equinox

broken clouds in spring
Some of the effects and artifacts visible in these graphs include:
1. I have a mountain nearby to the East, so sunrise here does not include direct sunlight for up to an hour after nominal sunrise. This issue affects all the graphs.
2. There is a row of Arizona Cypress trees to the West of my detection station, so depending on time of year, there is a sudden drop in detected light even on very clear days. This issue is prominent in the summer graph, not a factor in the winter graph, and intermediate in the spring graphs.
3. I have a neighbor's house to the Southeast, which blocks morning light even after the mountain no longer blocks it, for a little while, depending on time of year. This issue is prominent in the winter graph.
4. I have guy wires to stabilize the weather station mounting pole. Even though there are very thin (80 pound test braided fishline), they make a visible dent on each side of noon. A guy working on my roof last summer broke one, which I have neglected to repair, so only one dent after mid-summer 2015.
5. The Cumulus "maximum" calculation overestimates the summer to winter difference at my location.
6. The Cumulus "maximum" calculation has very slightly the wrong shape for diurnal variation here.
7. Broken cloud conditions give very spiky graphs, which many early users think signal some sort of station problem. It is entirely possible for short periods that reflected light from broken clouds added to direct path sun shining through a hole in the clouds add to more light than would be present on a perfectly clear day.