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3 LOCAL SCIENTIFIC KNOWLEDGE<br />
3.1 Introduction<br />
The following sections review the existing scientific information about the Oriners area,<br />
focusing on physical conditions and <strong>to</strong> a much smaller extent the biological conditions, which<br />
will <strong>be</strong> expanded on in the future as working knowledge improves. In certain cases, data from<br />
the station area is <strong>not</strong> available, but proxy data from other adjacent areas on Cape York have<br />
<strong>be</strong>en located and <strong>pre</strong>sented where applicable. Besides more regionalised surveys such as<br />
Cape York Peninsula Land Use Survey (CYPLUS), this is the first time that a scientific data<br />
synthesis has <strong>be</strong>en generated for the Oriners area specifically. This collation of data and<br />
additions over time will <strong>be</strong> useful for planning NRM and further scientific research for Oriners<br />
itself, as well as <strong>be</strong>ing of some use on adjacent stations. The relationships <strong>be</strong>tween the<br />
scientific data and the local observations <strong>pre</strong>sented in Section 2 will <strong>be</strong> considered further in<br />
Section 4. In general terms, the archival record confirms the general conditions <strong>not</strong>ed in the<br />
<strong>pre</strong>vious section and familiar <strong>to</strong> other parts of the Cape. It also provides evidence of the<br />
distinctiveness and unique value of this area compared <strong>with</strong> the broader Mitchell catchment.<br />
3.2 Physical conditions<br />
3.2.1 Climate<br />
The climate of the „forest country‟ surrounding Oriners Station 34 is tropical monsoonal and<br />
strongly seasonal, similar <strong>to</strong> other wet-dry tropic areas of Cape York and northern Australia<br />
(Hayden 1988; Stewart 1993; Petheram, McMahon et al. 2008; Ward, Pusey et al. 2011).<br />
Rainfall records from Oriners Station are brief (1963-1970), but additional rainfall data from<br />
nearby Dixie Station 55km away (1970-1974; 1988-2004) are useful in piecing <strong>to</strong> <strong>to</strong>gether<br />
climatic trends. In addition, longer rainfall records exist for nearby Koolatah Station 71 km<br />
away (1921-2011) and both rainfall and temperature records exist for the Musgrave <strong>to</strong>wnship<br />
95 km away (1887-1929; 1948-1978; 1984-2011). From these records, the strongly seasonal<br />
trends in monthly rainfall and temperature are apparent (Figure 44). Using the combined<br />
records from Oriners and Dixie Stations, >80% of the mean annual rainfall typically falls<br />
<strong>with</strong>in the wet season months of Decem<strong>be</strong>r <strong>to</strong> March inclusive. Monthly mean minimum<br />
temperatures are usually the highest during the summer wet season and lowest in the winter<br />
dry, while mean maximum temperatures are usually highest <strong>be</strong>tween Oct-Dec during the<br />
build-up <strong>to</strong> the wet season (Figure 44).<br />
34 Much of the data <strong>pre</strong>sented in this section refers <strong>to</strong> a broader area than the boundaries of Oriners<br />
Station, but Oriners (and <strong>to</strong> a lesser extent Sef<strong>to</strong>n Station) remain the primary focus.<br />
Working Knowledge at Oriners Station, Cape York<br />
131