Land use, soils & climate | Understanding regional differences | Victoria's changing climate | Geomorphology land use and Victoria's bioregions | What impacts will the project have? | Contact | Publications

| Land use, soils and climate The Victorian landscape exhibits a rich variety of terrestrial ecosystems. This variety is a result of diverse terrain (from the mountains to the plains), climate (alpine to semi-arid), geology and soils. Over the last fifty years land use practices have become relatively finely-tuned to this diversity of climate and soil. Although climate over that period has been highly variable with respect to droughts, good years and wet years, models of the future climate are showing a general shift to drier and hotter conditions. There are many important questions for the future of Victorian agriculture and its adaptation to changing climatic conditions. For example:
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| Rainfall | ||
| The average annual rainfall, in millimetres (mm), has been derived from the average daily rainfall for each month for the period 1957 - 2005. This daily rainfall has been multiplied by the total number of days for that month, with the figure of 28.3 used for the month of February, thus incorporating three leap years. The rainfall figures for the 12 months are added together to obtain the total average rainfall volume for that period. The average annual rainfall periods derived include 1970-1995, 1996-2005 and the 2050 predicted values. | ||
1970-1995 | 1996-2005 | 2050 A1FI Prediction |
Temperature | ||
| The average annual temperature, in degree Celcius (ºC), has been derived from the monthly minimum and maximum temperatures for the period 1970 - 2005. For each month the minimum and maximum temperature range has been measured. By adding these together and dividing them by 24 (there are 12 minimum and 12 maximum levels), the average annual temperature can be calculated. The average annual temperature periods derived include 1970-1995, 1996-2005 and the 2050 predicted values. | ||
1970-1995 | 1996-2005 | 2050 A1FI Prediction |
| Evaporation | ||
| The average annual evaporation has been derived from the average daily evaporation for that period. This daily evaporation has been multiplied by the total number of days for that month, with the figure of 28.3 used for the month of February, thus incorporating three leap years. The 12 resulting figures are added together to get the average annual evaporation for the period. The average annual evaporation periods derived include 1970-1995, 1996-2005 and the 2050 predicted values. | ||
1970-1995 | 1996 - 2005 | |
Rainfall Evaporation | ||
| The average cumulative rainfall for April to December has been derived from the average monthly rainfall for the period 1957 – 2005, minus the average cumulative evaporation for April to December from the average monthly rainfall for the period 1957 – 2005. The average cumulative rainfall minus evaporation periods derived include 1970-1995 and 1996-2005. | ||
Geomorphology, land use and Victoria's bioregions | ||
| Geomorphology | Landuse | Bioregions | Soils Geomorphology | ||
| The map provided shows the Geomorphology of Victoria classified in 8 categories (zones), each comprising various geomorphological units. The units provide a framework that helps us to understand the vegetation type distribution as well as the soil type distribution and hence has some bearing on natural habitat distribution for fauna and flora. Further details are provided in Geomorphology Framework of Victoria on VRO. | ||
Landuse | ||
| The land use map for Victoria is based on the Australian Land Use and Management (ALUM) Classification. Five primary levels of land use are distinguished in order of increasing levels of intervention or potential impact on natural landscape systems. Water is also included in the classification as a sixth primary class because of its importance for natural resources management. The classification has a three-tiered hierarchical structure. Secondary classes represented include land management or practice variants. | ||
| Bioregions | ||
| Native flora and fauna are inherently diverse and exist within complex ecosystems. There is thus a need for a framework to address this complexity and connect us more directly to the biodiversity assets and challenges in our environments. Biogeographic regions, or bioregions, capture the patterns of ecological characteristics and the underlying environmental features in the landscape thus providing a natural framework for recognising and responding to biodiversity values. Five bioregions occur in Victorian waters; while the 12 national terrestrial bioregions have been broken down into 28 Victorian Bioregions. For further information on Victoria's Bioregions can be found on VRO. | ||
![]() Primary Production Landscapes of Victoria with representative Soil Profiles |
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