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ClimateRainfall
An obvious east to west gradient exists for annual mean precipitation, ranging from very dry to moderate. Areas located in the east of the province, lying in the foothills of the Great Dividing Range, receive the highest annual mean precipitation. Similarly, the driest quarter mean precipitation ranges from dry to wet along an east to west gradient. Rainfall erosivity, the potential for rainfall induced soil loss (Stein, 2005) is low throughout the province. Precipitation results in lateral runoff from the surrounding floodplains into rivers, supplying nutrients and debris (allochthonous inputs) to the system. In the Murray-Darling province this accounts for the majority of river flow. Low annual mean precipitation means a reduced incidence of such events. Inundation of the floodplain by overbank flows serves the same purpose, though flooding is also a result of precipitation occurring somewhere in the system. The low frequency of allochthonous inputs means that production within the channel, primarily by algae, is important. Production is also increased when the floodplain is inundated; therefore flooding events are significant for the organisms that utilise algae.
Murray-Darling FBP Rainfall Maps State Rainfall Map
Temperature
The annual mean temperature for the Murray-Darling FBP ranges from cool to cold, with the lowest temperatures recorded from the areas of the province at higher altitude. There is an extremely strong longitudinal gradient for the values of the highest weekly mean maximum temperature, ranging from cold to warm. The highest value for this statistic recorded in the province is 36.5°C. The Murray-Darling FBP is the coldest province in the state with the lowest value for the lowest weekly mean maximum temperature recorded for any province (0°C). Temperature values for this statistic range throughout the province from cool to cold, and it is obvious that the values are influenced by altitude: areas in the province at higher altitudes are cooler than those at lower altitudes. The ratio of the hottest weekly maximum to the coldest weekly minimum values was high throughout the province. This suggests that seasonality in temperature is pronounced, and that areas in the Murray-Darling FBP experiencing hot summers are experiencing cold winters. Sections of the province that experience a low hottest month mean maximum temperature support an array of cold adapted species that occur nowhere else in Queensland. Examples of these species are the river black fish (Gadopsis marmoratus) and mountain galaxias (Galaxias olidus). Both of these species are intolerant of warm water so they can only survive in streams that remain cool throughout the year. These cooler parts of the province may also lack species found elsewhere in the province that rely on warmer temperatures for some aspect of their life cycle, for example fish that rely on a rise in water temperature as a spawning cue. Diversity of temperature conditions may result in higher species richness as thermal requirements of more species may be met.
Summary Maps of Province Temperature State Temperature Map
Water balance
Annual mean runoff for the region is exceptionally low at 3 mm, displaying a slight north-south gradient, with greater run off in the southern regions of the province. While precipitation largely exceeds evaporation for most of the year (Thompson 1992; Walker et al. 1981), the dominance of sandy soils in the region results in high infiltration capacity, reducing the run-off associated with rainfall events (Laycock 1975b; Marshall, McGregor & Negus 2006; Walker et al. 1981).
Last updated: 21 February 2012 |
— Department of Environment and Resource Management
