Pauline Grierson
0000-0003-2135-0272
University of Padova
80 papers found
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Megadroughts in the Common Era and the Anthropocene
Assessing temporal changes in groundwater recharge using spatial variations in groundwater ages
Diel cycles of δ13CDIC and ecosystem metabolism in ephemeral dryland streams
Geomorphic and hydrological controls on groundwater dolocrete formation in the semi‐arid Hamersley Basin, northwest Australia
Groundwater seepage controls salinity in a hydrologically terminal basin of semi-arid northwest Australia
Natural hazards in Australia: extreme bushfire
Interpreting vegetation change in tropical arid ecosystems from sediment molecular fossils and their stable isotope compositions: A baseline study from the Pilbara region of northwest Australia
Better planning outcomes require adequate data and ecological understanding to be successful and credible: A reply to Evans et al., 2015
Evidence for extreme floods in arid subtropical northwest Australia during the Little Ice Age chronozone (CE 1400-1850).
Cacao quality: Highlighting selected attributes
Evidence for climate-driven synchrony of marine and terrestrial ecosystems in northwest Australia
Inter-specific differences in the dynamics of water use and pulse-response of co-dominant canopy species in a dryland woodland
Drought variability in the eastern Australia and New Zealand summer drought atlas (ANZDA, CE 1500–2012) modulated by the Interdecadal Pacific Oscillation
Alluvial ground water influences dissolved organic matter biogeochemistry of pools within intermittent dryland streams
Linking stream ecology with morphological variability in a native freshwater fish from semi-arid Australia
Tree Rings Show Recent High Summer-Autumn Precipitation in Northwest Australia Is Unprecedented within the Last Two Centuries
Impacts of high inter-annual variability of rainfall on a century of extreme hydrologic regime of northwest Australia
Estimation of evaporative loss based on the stable isotope composition of water using “Hydrocalculator”
Evaluating recharge to an ephemeral dryland stream using a hydraulic model and water, chloride and isotope mass balance
Dissolved organic carbon biolability decreases along with its modernization in fluvial networks in an ancient landscape
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