Concept · Ch 14
The rain shadow (the dry side of the hills)
Sea winds are forced up and over the Mount Lofty Ranges and lose most of their rain doing it, so the country just beyond the crest gets what is left over — and tips straight into mallee, the last and driest habitat of the gulf-to-range gradient.
First, meet: The Mediterranean bargain (two seasons, not four)The mesic refugium (a wet island in a dry land)
Stand on the eastern crest of the Mount Lofty Ranges and look back the way you came, and you have just watched a weather system get robbed. All winter, moist westerly air blows in off Gulf St Vincent and the ranges take it apart: forcing it upward, cooling it, wringing the water out of it as rain, long before it ever reaches the ridge you are standing on. Squeeze a cloud like that over a few hundred vertical metres and you get the drenched, ferny side of the range behind you — catching well over a thousand millimetres a year in the high country, against the few hundred the plains below make do with (Gill, McKenna & Wouters 2014). But whatever the cloud has left by the time it finally clears the summit is spent. It rolls down the far slope already wrung dry, and the country on that side gets whatever is left over, which is not much.
That is a rain shadow, and it is not a metaphor; it is the same plain physics that plays out behind every mountain range on Earth standing across a prevailing wind. The Mediterranean engine that hands the western, seaward slopes their wet winters and killing-dry summers (Cowling et al. 1996) hands the eastern lee an even harder bargain: a summer just as dry, stacked on a winter that was thin to start with. Drive over the crest and down the eastern side and you can watch the vegetation do the arithmetic within a few kilometres — tall wet stringybark forest thinning, then giving out altogether, into a low, grey-green scrub of multi-stemmed, lignotuber-rooted eucalypts standing over saltbush or spinifex. That is the mallee, the driest and toughest community on the whole gulf-to-range transect, and its extent and its inhabitants were counted, quadrat by quadrat, across a landscape most people only ever cross at highway speed (Foulkes & Gillen 2000).
It helps to think of the rain shadow as a mirror. Everything the wet side of the range does with its surplus — fern gully, swamp, tall forest, a refuge for species the baking plain cannot support — the dry side does in reverse, building an entirely different, equally specialised community out of scarcity. Read the rain shadow correctly and you are reading the same mountain twice: once as a gift, and once, a few kilometres further on, as a debt still being paid.
Go deeper — the mechanism & the evidence
The mechanism is orographic: prevailing moist westerlies are forced to rise over the Mount Lofty Ranges' spine, cool as they climb, and drop the bulk of their moisture as rain on the windward slopes and summits, where annual rainfall climbs above 1,100 mm against well under 500 mm on the plains at the range's foot (Gill, McKenna & Wouters 2014). Air that has already cleared the ridge has lost most of that water, so the eastern, lee side of the very same range receives a further, separate shortfall on top of it — the classic rain-shadow deficit — and the same Mediterranean summer-drought rhythm that dries the whole region then stacks a killing-dry season on top of that (Cowling et al. 1996). The vegetation answers within a short drive: tall wet sclerophyll forest along the range front gives way, over the crest, to the multi-stemmed, lignotuber- rooted mallee eucalypts and their chenopod- or spinifex-floored understorey, documented plot by plot across hundreds of survey quadrats in the country immediately behind the ranges (Foulkes & Gillen 2000) — proof that a rain shadow is not a folk description but a measurable line in the vegetation.
Sources & further reading
Every claim here is traceable. Each citation links to its entry in the bibliography.
- Gill, A.M., McKenna, D.J. & Wouters, M.A. (2014). Landscape fire, biodiversity decline and a rapidly changing milieu: a microcosm of global issues in an Australian biodiversity hotspot. Land 3(3): 1091–1136. DOI: 10.3390/land3031091. https://www.mdpi.com/2073-445X/3/3/1091 — The Mount Lofty Ranges' rainfall gradient — over 1,100 mm in the high hills against under 500 mm on the plains at their foot.
- Cowling, R.M., Rundel, P.W., Lamont, B.B., Arroyo, M.K. & Arianoutsou, M. (1996). Plant diversity in mediterranean-climate regions. Trends in Ecology & Evolution 11(9):362-366. https://doi.org/10.1016/0169-5347(96)10044-6 — The Mediterranean summer-drought mechanism the rain shadow compounds on the lee side of the range.
- Armstrong, D.M., Croft, S.J. & Foulkes, J.N. (2003). A Biological Survey of the Southern Mount Lofty Ranges, South Australia, 2000–2001. Department for Environment and Heritage, South Australia. https://data.environment.sa.gov.au/Content/Publications/Southern-Mount-Lofty-Ranges-BioSurvey.pdf — The mallee vegetation and fauna surveyed, quadrat by quadrat, in the rain-shadow country behind the ranges.
- Haslem, A., Kelly, L.T., Nimmo, D.G., Watson, S.J., Kenny, S.A., Taylor, R.S., Avitabile, S.C., Callister, K.E., Spence-Bailey, L.M., Clarke, M.F. & Bennett, A.F. (2011). Habitat or fuel? Implications of long-term, post-fire dynamics for the development of key resources for fauna and fire. Journal of Applied Ecology 48(2): 247–256. DOI: 10.1111/j.1365-2664.2010.01906.x. https://doi.org/10.1111/j.1365-2664.2010.01906.x — How long unburnt spinifex and mallee habitat needs to rebuild after fire — the rain shadow's fire-shaped aftermath.
See it in the country
The mallee emu-wrenThe mallee eucalyptsMount Lofty summitNgarkat — the great mallee reserveThe rain-shadow malleeSpinifex (Triodia)The gulf-to-range transect
Grounded in A Coast Running Out of Water. Every figure is stated once in the book's canonical facts register and cited to a published source.