The difference between the reef flat and reef slope data is also quite distinct, with the exception of the Kelso Reef data. The largest temperature variation is found on the reef flat, with the same period of variation occuring on the reef slope, but the magnitude has just been reduced. This is mainly due to the closer proximity to the surface, and the solar energy recieved from the sun causing more heating of the water body because it is distributed over a smaller water volume. In the case of Kelso Reef, located on the mid continental shelf, there is very little difference between the reef flat and reef slope temperatures and the cycle each follows. The localised heating of the water in the shallow water at Kelso Reef is off set by the input, displacement by, and mixing of deep ocean water currents, so that very little difference appears.
Seasonal variations in the daily temperature variation also is evident. During summer the highest temperature difference is higher than winter, 2.2oC to 2.5oC for Magnetic Island, 1.4oC to 1.2oC for Myrmidon Reef, and 0.6oC to 0.5oC for Kelso Reef. The seasonal variation in average temperature, as previously discussed, can also be see for all of the reefs.