In Southern Australia where water levels fluctuate and are naturally v
ariable, the importance of water regime, as distinct from water depth,
was shown and the difference between depth and elevation gradients wa
s verified. The water regimes at sites across an elevation gradient we
re described and quantified. The Sum Water Regime, an index of the hyd
rological past that plants had experienced, was a summary of depth and
duration of inundation. It was calculated over monthly intervals (1,
3, 6, 12 months) prior to plant harvests and on a daily scale (for eac
h record of water level: 1-30 days). It identified the response times
of two emergent species at the level of the population (live abovegrou
nd mass, g m(-2), and shoot density, number per m(2)). Triglochin proc
erum R.Br. had a rapid response time with population changes matching
changes in depth. In contrast, Baumea arthrophylla (Nees) Boeckeler ha
d a slower response time with its characteristics correlated to the pa
st water regime integrated over 6-12 months. At the level of photosynt
hetic organs, the change in the mean heights of T. placer um leaves ac
ross a spring depth gradient, paralleled the change in the maximum hei
ghts. Height and diameter also changed in proportion. For B. arthrophy
lla, the maximum height of its stems increased across the sampled grad
ient, but the mean heights fell at the deeper sites. Coupled with the
finding that increases in diameter did not keep pace with increases in
height, these results showed that T. procerum, unlike B. arthrophylla
, was well within its depth limits. Populations were sampled across th
e range of water regimes they experienced. This highlighted the signif
icant effect small changes in water regime have on the structure and p
erformance of aquatic plants. Measuring the range of characteristics,
not only identifies the upper and lower limits, but may be used to pre
dict the condition of other populations.