Monitoring the Rangelands - Photographic Sequences for Darling Riverine Plains
The Rangelands Information System Photographic Sequences is a tool which allows the user to view a photographic record of particular areas in the Rangelands. The photographs for Darling Riverine Plains has been provided by
The following photographic sequence products are available for the Darling Riverine Plains bioregion:
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Location 1
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April 1991
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
April 1992
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
May 1993
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
June 1994
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
April 1995
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
June 1996
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
August 1997
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
February 2000
Images show a northern floodplain site on the Culgoa River floodplain. While the canopy cover remains constant at around 7% throughout the period, the density of perennial chenopods (lignum (Muehlenbeckia florulenta) and golden goosefoot (Chenopodium auricomum)) fluctuates from 333 plants/ha in 1992 to 73 plants/ha in 1995. This is due to the dry condition from 1992-191995. These conditions are reflected also in the pasture biomass that is extremely low in 1992 and 1998. Biomass is highest in 2000 as a result of good seasonal rainfall. This site remains in good condition.
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