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Southwestern
Australia, July 1926
Rainfall in southwestern
Australia is strongly concentrated in the winter months, and thus flooding
tends to be mostly a winter phenomenon. There are exceptions, such as
in February 1955 and January 1982, when ex-tropical cyclones dumped
hundreds of millimetres over the area and triggered severe flooding
in local rivers. However most flooding, at least in the wetter areas
of southwestern Australia, occurs when a series of strong winter storms
produce prolonged heavy rainfall. In general these floods cause less
damage than their counterparts in the east, and loss of life is rare.
The winter of 1926
was exceptional for its persistent and sometimes heavy rainfall over
southwestern Australia. Following a rather wet April, the first half
of May was virtually dry. The rains returned with a vengeance just after
mid-month, and from then until September, seemed to be unrelenting.
At Collie, the 111-day period from 18 May to 5 September had only six
rain-free days. In mid-July, with the ground by now saturated., a low
pressure complex became established to the south of Western Australia.
This generated frequent heavy rains and fierce westerly gales: in some
coastal areas there was significant wind damage as well as flooding.
Over the week ending 22 July rainfall totals were widely in excess of
100mm, and even some of the drier inland wheatbelt centres such as Northam
and Beverley registered 80 to 90mm of rain.
Widespread flooding
resulted. Extensive areas of the southwest were under water, with large
portions of the towns of Northam, York, Beverley and Collie inundated.
Flooding was also severe in the Upper SwanGuildford and South
Perth areas around the Swan River, and in and around Bunbury. Flooding
extended as far east as Lake Grace, an uncommon event in winter. The
huge volume of water destroyed several bridges - including the Fremantle
railway bridge on 22 July, which collapsed soon after a passenger train
from Perth had made the crossing!
The events of 1926
were a noteworthy episode from a time when flooding in the southwest
was more common than it is today. This reflects the fact that, between
the turn of the century and the 1960s, the southwest was distinctly
wetter than it has been over the past 30 years. However it is worth
noting that floods were also less common in the 1880s and 1890s, whereas
in the 1860s and 1870s there were a number of severe events. Long-term
climate fluctuations of this kind can sometimes lull people into false
perceptions about the degree of risk from flooding.
On the other hand,
the decrease in rainfall over southwestern Australia during the late
20th century is generating concern for those people managing water resources
for the areas growing population, and for those involved in water-sensitive
activities such as agriculture and environmental conservation.
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