Table A1 – 4. A flooding overlay checkInundation area <strong>for</strong> three flood events on <strong>the</strong> Gwydir River, 1975 to 1983. Agreement between flood events,indicated by <strong>the</strong> area <strong>of</strong> overlap and non-overlap, was low, and was not dependent on flood size. Reasons <strong>for</strong> thiswere not determined at <strong>the</strong> time <strong>the</strong> analysis was done, but this was a period <strong>of</strong> floodplain development (Roberts,unpublished data).Event size Area <strong>of</strong> overlap Area <strong>of</strong> non-overlap150 GL a month and 130 GL month 11,033 ha 6,0001 (35.2%) <strong>of</strong> smaller flood not flooded by larger flood150 GL month and 303 GL month 29,801 ha 7,935 ha (21.0%) <strong>of</strong> smaller flood not flooded by larger flood130 GL month and 303 GL month 13,580 ha 3,474 ha (20.4%) <strong>of</strong> smaller flood not flooded by larger flooda GL = gigalitre = 1,000,000,000 litresTable A1 – 5. Comparison <strong>of</strong> two methodsInundated area estimated <strong>for</strong> three floods using two methods <strong>of</strong> interpretation: Method 1, visual interpretation <strong>of</strong>flooded area on hard copy, measured by planimetry; Method 2, micro-BRIAN estimated flooded areas afterrectifying grey-scale images, using scanned and digitised hard copy (Roberts, unpublished data).Date <strong>of</strong> image Method 1 Method 2 Change as %, as area (ha)1 November 1975 37,500 37,736
Appendix 2:EvapotranspirationEvapotranspiration dataThis Appendix gives ‘best guess’ estimates <strong>of</strong> K c and K s (Table A2 – 1) <strong>for</strong>use in indirect estimates <strong>of</strong> evapotranspiration, as outlined in <strong>the</strong> thirdmethod in Section 6.Table A2 – 1.K c and K s <strong>for</strong> plant communities typical <strong>of</strong>south-eastern AustraliaPlant community(Structure + Dominant)TREE-dominated plant communitiesRiparian <strong>for</strong>est – mainly eucalypts eg. river red gum(Eucalyptus camaldulensis)Open woodlandeg. blackbox, coolibaheg. river coobah (Acacia stenophylla)SHRUB-dominated plant communitiesShrublands – contrasting <strong>for</strong>ms• Twiggy and deciduous eg. lignum (twiggy)• Succulent and salt-tolerant eg. chenopodseg. Atriplex, ChenopodiumGRASS-dominated plant communitiesGrasslands – dryish water regime, rapid responses onflooding, tussock perennialseg. Warrego summer grass and CanegrassGrasslands – trailing or mat <strong>for</strong>ming, aquatic typeseg. Moira grass (Pseudoraphis spinescens) and watercouch (Paspalum distichum)Grasslands – tall erect, including o<strong>the</strong>r grass-likeemergents growing in water 0.5–1.5 m deep.eg. Phragmites australis and cumbungi (Typha spp.)SEDGE-dominated plant communitiesSedgelands – medium-tall erect culms with no lamina,and low LAI: cover wide ecological range from nearpermanent to intermittenteg. EleocharisSedgelands – medium–tall, erect culms with bracts actingas leaveseg. Bolboschoenus, CyperusAQUATIC HERB-dominated plant communitiesAquatic herblands – dissected leaves, emerging through<strong>the</strong> water, and under water: milfoilsAquatic herblands – broad or large flat blade leaves onor just above <strong>the</strong> water surfaceeg. pondweeds (Potamogeton spp.) and water ribbons(Triglochin spp.)K c0.8To be confirmedK sOasis and saline water effectsunlikely0.4 <strong>for</strong> blackbox types 0.1–0.5 (saline groundwater,blackbox types)0.3 – 0.60.3 –0.6(Values <strong>for</strong> dry to wetconditions)0.8–1.0 when flooded andactively growing0.1–0.2 when droughted1.3–1.4 Not applicable1.3–1.4 when flooded 0.4–0.6 when senescent1.3–1.4 when flooded 0.4–0.6 when senescent1.3 Not applicable1.1–1.3 Not applicableContinued on next pageAppendix 2: Evapotranspiration 109
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Estimating the WaterRequirements fo
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ContentsPreface 7Acknowledgments 8G
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List of Tables1 Spatial variability
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Note that the guide is concerned pr
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ecomes a matter of how to use what
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Figure 1. Floodplain featuresThe fl
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Figure 4.Wanganella Swamps, souther
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Floodplain wetlands, being a mosaic
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Section 2:Introducing theVegetation
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size and vigour rarely reach their
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floodplains survive there because t
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The lagoon floor is then colonised
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Note 11Growth-formsField guides to
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identical conditions. PFTs differ f
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Note 13Changes in depthSome herbace
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Focusing on depthWater regime analy
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Note 15Internet dataEnvironmental d
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Step 3: Vegetation-hydrologyrelatio
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Note 19Modelling and time-stepsIn s
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Section 4: Old andNew DataOne of th
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see Figure 15), despite a three-fol
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frequency. This is rather limiting,
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Figure 13. Lippia, a floodplain wee
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single measure of the vegetation to
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Section 5:ObtainingVegetation DataW
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However, if the chosen species has
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Figure 15. Range of tree condition
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Figure 16. Spatial-temporal sequenc
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- Page 92 and 93: ReferencesPrefaceArthington AH and
- Page 94 and 95: Section 3Roberts J and Marston F (1
- Page 96 and 97: Kunin WE and Gaston KG (1993). The
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