Following on from my previous post looking at temperature and elevation I decided to use the climate data from the locations in and around the landholder sites to see what the correlation was between annual rainfall and elevation.
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In the accompanying graph you can see the results. The vertical axis represents both elevation in metres above sea level and mean annual rainfall in millimetres. The horizontal axis shows each of the locations – sorted by ascending elevation from left to right.
Whilst it would not be appropriate to conclude that what occurs in these locations could be expected to be experienced in locations in all regions the graph does show rainfall continuing to increase with elevation increase. At lower elevations the annual rainfall is a much higher multiple of elevation (roughly 3 times) whilst at the higher elevations the rainfall is a much lower multiple (roughly 1 to 1 at Crookwell). This suggests that the trend is likely to reverse at a certain point and a quick look at the data Guyra (elevation 1332 metres, annual rainfall 926 metres) tends to confirm this – although Guyra is in a totally different region.
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