Anna Ukkola
Anna Ukkola
ARC Centre of Excellence for Climate Extremes, Australian National University
Verified email at
TitleCited byYear
Reduced streamflow in water-stressed climates consistent with CO2 effects on vegetation
AM Ukkola, IC Prentice, TF Keenan, AIJM van Dijk, NR Viney, RB Myneni, ...
Nature Climate Change 6, 75–78, 2016
A worldwide analysis of trends in water-balance evapotranspiration
AM Ukkola, IC Prentice
Hydrology and Earth System Sciences 17 (10), 4177-4187, 2013
Land surface models systematically overestimate the intensity, duration and magnitude of seasonal-scale evaporative droughts
AM Ukkola, MG De Kauwe, AJ Pitman, MJ Best, G Abramowitz, V Haverd, ...
Environmental Research Letters 11, 104012, 2016
New turbulent resistance parameterization for soil evaporation based on a pore‐scale model: Impact on surface fluxes in CABLE
M Decker, D Or, A Pitman, A Ukkola
Journal of Advances in Modeling Earth Systems 9 (1), 220-238, 2017
Modelling evapotranspiration during precipitation deficits: identifying critical processes in a land surface model
AM Ukkola, AJ Pitman, M Decker, MG De Kauwe, G Abramowitz, J Kala, ...
Hydrology and Earth System Sciences 20, 2403-2419, 2016
Asymmetric responses of primary productivity to altered precipitation simulated by ecosystem models across three long-term grassland sites
D Wu, P Ciais, N Viovy, AK Knapp, K Wilcox, M Bahn, MD Smith, S Vicca, ...
Biogeosciences 15, 3421-3437, 2018
Vegetation plays an important role in mediating future water resources
AM Ukkola, TF Keenan, DI Kelley, IC Prentice
Environmental Research Letters 11 (9), 094022, 2016
Derived Optimal Linear Combination Evapotranspiration (DOLCE): a global gridded synthesis ET estimate
S Hobeichi, G Abramowitz, J Evans, A Ukkola
Hydrology and Earth System Sciences 22, 1317-1336, 2018
Hydrological evaluation of the LPX dynamic global vegetation model for small river catchments in the UK
AM Ukkola, SJ Murray
Hydrological Processes 28 (4), 1939-1950, 2014
Evaluating the contribution of land‐atmosphere coupling to heat extremes in CMIP5 models
AM Ukkola, AJ Pitman, MG Donat, MG De Kauwe, O Angélil
Geophysical Research Letters 45 (17), 9003-9012, 2018
FluxnetLSM R package (v1.0): a community tool for processing FLUXNET data for use in land surface modelling
A Ukkola, N Haughton, M De Kauwe, G Abramowitz, A Pitman
Geoscientific Model Development 10, 3379-3390, 2017
Examining the evidence for decoupling between photosynthesis and transpiration during heat extremes
MGD Kauwe, BE Medlyn, AJ Pitman, JE Drake, A Ukkola, A Griebel, ...
Biogeosciences 16 (4), 903-916, 2019
Intensification of precipitation extremes in the world’s humid and water-limited regions
MG Donat, O Angélil, AM Ukkola
Environmental Research Letters 14 (6), 065003, 2019
Evaluating CMIP5 Model Agreement for Multiple Drought Metrics
AM Ukkola, AJ Pitman, MG De Kauwe, G Abramowitz, N Herger, JP Evans, ...
Journal of Hydrometeorology 19, 969-988, 2018
Identifying regions of drought mortality risk for tree species: a case study focussed on SE Australia.
MG De Kauwe, B Medlyn, P Meir, LA Cernusak, AJ Pitman, VE Haverd, ...
AGU Fall Meeting 2019, 2019
Natural variability of multi-year droughts in Australia in Last Millennium simulations
N Wright, ML Roderick, N Abram, B Henley, A Ukkola
AGU Fall Meeting 2019, 2019
Exploring the stationarity of Australian temperature, precipitation and pan evaporation records over the last century
AM Ukkola, ML Roderick, A Barker, AJ Pitman
Environmental Research Letters 14 (12), 124035, 2019
The aridity Index under global warming
P Greve, ML Roderick, AM Ukkola, Y Wada
Environmental Research Letters 14 (12), 124006, 2019
Amplification of risks to water supply at 1.5° C and 2° C in drying climates: a case study for Melbourne, Australia
BJ Henley, M Peel, R Nathan, AD King, AM Ukkola, D Karoly, KS Tan
Environmental Research Letters, 2019
How representative are FLUXNET measurements of surface fluxes during temperature extremes?
SVJ van der Horst, AJ Pitman, MGD Kauwe, A Ukkola, G Abramowitz, ...
Biogeosciences 16 (8), 1829-1844, 2019
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