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    Circulation Features Associated with the Winter Rainfall Decrease in Southwestern Australia 

    Source: Journal of Climate:;1993:;volume( 006 ):;issue: 007:;page 1356
    Author(s): Allan, Robert J.; Haylock, Malcolm R.
    Publisher: American Meteorological Society
    Abstract: A study of atmospheric and oceanic circulation features in the wider Australian region is undertaken in an attempt to establish the cause(s) of the observed decrease in austral winter (JJA) rainfall over the southwestern ...
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    Multidecadal Variability in the Climate System over the Indian Ocean Region during the Austral Summer 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 007:;page 1853
    Author(s): Allan, Robert J.; Lindesay, Janette A.; Reason, Chris J. C.
    Publisher: American Meteorological Society
    Abstract: Several independent historical studies of global atmospheric and oceanic parameters have identified low-frequency fluctuations in the global climate system. Much of this research has focused on Europe, the Atlantic Ocean, ...
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    Sea Level and Rainfall Correlations in Australia: Tropical Links 

    Source: Journal of Climate:;1990:;volume( 003 ):;issue: 008:;page 838
    Author(s): Allan, Robert J.; Beck, Karen; Mitchell, William M.
    Publisher: American Meteorological Society
    Abstract: A preliminary study is made of simultaneous and lagged seasonal cross correlations between northern Australian sea level and district rainfall anomalies. Zero-lagged patterns show strong links with the El Niño/Southern ...
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    A Further Extension of the Tahiti-Darwin SOI, Early ENSO Events and Darwin Pressure 

    Source: Journal of Climate:;1991:;volume( 004 ):;issue: 007:;page 743
    Author(s): Allan, Robert J.; Nicholls, Neville; Jones, Phil D.; Butterworth, Ian J.
    Publisher: American Meteorological Society
    Abstract: An extension of the Tahiti minus Darwin Southern Oscillation Index (SOI) from 1882 back to 1876 is reported following the recovery of early Darwin mean sea-level pressure data spanning the period 1865?81. As a result, we ...
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