A comparison of multi-site daily rainfall downscaling techniques under Australian conditions

► We compare a range of multi-site rainfall downscaling models for hydrological purposes. ► Dynamic and stochastic models were compared using many rainfall statistics. ► A simple resampling scaling method performed well across a wide range of statistics. ► The more complex stochastic methods reprodu...

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Published inJournal of hydrology (Amsterdam) Vol. 408; no. 1; pp. 1 - 18
Main Authors Frost, Andrew J., Charles, Stephen P., Timbal, Bertrand, Chiew, Francis H.S., Mehrotra, R., Nguyen, Kim C., Chandler, Richard E., McGregor, John L., Fu, Guobin, Kirono, Dewi G.C., Fernandez, Elodie, Kent, David M.
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier B.V 30.09.2011
Elsevier
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Abstract ► We compare a range of multi-site rainfall downscaling models for hydrological purposes. ► Dynamic and stochastic models were compared using many rainfall statistics. ► A simple resampling scaling method performed well across a wide range of statistics. ► The more complex stochastic methods reproduced statistics that cannot be reproduced by scaling. ► Biases in GCM predictors are suggested as a possible cause of poor performance in GCM validation. Six methods of downscaling GCM simulations to multi-site daily precipitation were applied to a set of 30 rain gauges located within South-Eastern Australia. The methods were tested at reproducing a range of statistics important within hydrological studies including inter-annual variability and spatial coherency using both NCEP/NCAR reanalysis and GCM predictors, thus testing the validity of GCM downscaled predictions. The methods evaluated, all having found application in Australia previously, are: (1) the dynamical downscaling Conformal-Cubic Atmospheric Model (CCAM) of McGregor (2005); the historical data based (2) Scaling method applied by Chiew et al. (2009) and (3) Analogue method of Timbal (2004); and three stochastic methods, (4) the GLIMCLIM (Generalised Linear Model for daily Climate time series) software package ( Chandler, 2002), (5) the Non-homogeneous Hidden Markov Model (NHMM) of Charles et al. (1999), and (6) the modified Markov model–kernel probability density estimation (MMM–KDE) downscaling technique of Mehrotra and Sharma (2007). The results showed that the simple Scaling approach provided relatively robust results for a range of statistics when GCM forcing data was used, and was therefore recommended for regional water availability and planning studies (subject to certain limitations as mentioned in conclusion section). The stochastic methods better capture changes to a fuller range of rainfall statistics and are recommended for detailed catchment modelling studies. In particular, the stochastic methods show better results for daily extreme rainfall (e.g. flooding/low flow) as the simulations are not based purely on temporal/spatial rainfall patterns observed in the past, and a hybrid GLIMCLIM occurrence-KDE amounts model is recommended based on performance for individual statistics. For GCM downscaled simulations, biases in annual mean and standard deviation of ±5% and −30% were observed typically, and no single model performed well over all timescales/statistics, suggesting that the user beware of model limitations when applying downscaling methods for various purposes. A brief demonstration of predictor biases is presented, highlighting that biases observed in GCM predictors can cause poorer performance during GCM validation, and that investigation of these biases should inform choice of GCMs, GCM predictors, and the downscaling methods that use them.
AbstractList ► We compare a range of multi-site rainfall downscaling models for hydrological purposes. ► Dynamic and stochastic models were compared using many rainfall statistics. ► A simple resampling scaling method performed well across a wide range of statistics. ► The more complex stochastic methods reproduced statistics that cannot be reproduced by scaling. ► Biases in GCM predictors are suggested as a possible cause of poor performance in GCM validation. Six methods of downscaling GCM simulations to multi-site daily precipitation were applied to a set of 30 rain gauges located within South-Eastern Australia. The methods were tested at reproducing a range of statistics important within hydrological studies including inter-annual variability and spatial coherency using both NCEP/NCAR reanalysis and GCM predictors, thus testing the validity of GCM downscaled predictions. The methods evaluated, all having found application in Australia previously, are: (1) the dynamical downscaling Conformal-Cubic Atmospheric Model (CCAM) of McGregor (2005); the historical data based (2) Scaling method applied by Chiew et al. (2009) and (3) Analogue method of Timbal (2004); and three stochastic methods, (4) the GLIMCLIM (Generalised Linear Model for daily Climate time series) software package ( Chandler, 2002), (5) the Non-homogeneous Hidden Markov Model (NHMM) of Charles et al. (1999), and (6) the modified Markov model–kernel probability density estimation (MMM–KDE) downscaling technique of Mehrotra and Sharma (2007). The results showed that the simple Scaling approach provided relatively robust results for a range of statistics when GCM forcing data was used, and was therefore recommended for regional water availability and planning studies (subject to certain limitations as mentioned in conclusion section). The stochastic methods better capture changes to a fuller range of rainfall statistics and are recommended for detailed catchment modelling studies. In particular, the stochastic methods show better results for daily extreme rainfall (e.g. flooding/low flow) as the simulations are not based purely on temporal/spatial rainfall patterns observed in the past, and a hybrid GLIMCLIM occurrence-KDE amounts model is recommended based on performance for individual statistics. For GCM downscaled simulations, biases in annual mean and standard deviation of ±5% and −30% were observed typically, and no single model performed well over all timescales/statistics, suggesting that the user beware of model limitations when applying downscaling methods for various purposes. A brief demonstration of predictor biases is presented, highlighting that biases observed in GCM predictors can cause poorer performance during GCM validation, and that investigation of these biases should inform choice of GCMs, GCM predictors, and the downscaling methods that use them.
Six methods of downscaling GCM simulations to multi-site daily precipitation were applied to a set of 30 rain gauges located within South-Eastern Australia. The methods were tested at reproducing a range of statistics important within hydrological studies including inter-annual variability and spatial coherency using both NCEP/NCAR reanalysis and GCM predictors, thus testing the validity of GCM downscaled predictions. The methods evaluated, all having found application in Australia previously, are: (1) the dynamical downscaling Conformal-Cubic Atmospheric Model (CCAM) of McGregor (2005); the historical data based (2) Scaling method applied by Chiew et al. (2009) and (3) Analogue method of Timbal (2004); and three stochastic methods, (4) the GLIMCLIM (Generalised Linear Model for daily Climate time series) software package (Chandler, 2002), (5) the Non-homogeneous Hidden Markov Model (NHMM) of Charles et al. (1999), and (6) the modified Markov model-kernel probability density estimation (MMM-KDE) downscaling technique of Mehrotra and Sharma (2007). The results showed that the simple Scaling approach provided relatively robust results for a range of statistics when GCM forcing data was used, and was therefore recommended for regional water availability and planning studies (subject to certain limitations as mentioned in conclusion section). The stochastic methods better capture changes to a fuller range of rainfall statistics and are recommended for detailed catchment modelling studies. In particular, the stochastic methods show better results for daily extreme rainfall (e.g. flooding/low flow) as the simulations are not based purely on temporal/spatial rainfall patterns observed in the past, and a hybrid GLIMCLIM occurrence-KDE amounts model is recommended based on performance for individual statistics. For GCM downscaled simulations, biases in annual mean and standard deviation of +/-5% and -30% were observed typically, and no single model performed well over all timescales/statistics, suggesting that the user beware of model limitations when applying downscaling methods for various purposes. A brief demonstration of predictor biases is presented, highlighting that biases observed in GCM predictors can cause poorer performance during GCM validation, and that investigation of these biases should inform choice of GCMs, GCM predictors, and the downscaling methods that use them.
Six methods of downscaling GCM simulations to multi-site daily precipitation were applied to a set of 30 rain gauges located within South-Eastern Australia. The methods were tested at reproducing a range of statistics important within hydrological studies including inter-annual variability and spatial coherency using both NCEP/NCAR reanalysis and GCM predictors, thus testing the validity of GCM downscaled predictions. The methods evaluated, all having found application in Australia previously, are: (1) the dynamical downscaling Conformal-Cubic Atmospheric Model (CCAM) of McGregor (2005); the historical data based (2) Scaling method applied by Chiew et al. (2009) and (3) Analogue method of Timbal (2004); and three stochastic methods, (4) the GLIMCLIM (Generalised Linear Model for daily Climate time series) software package (Chandler, 2002), (5) the Non-homogeneous Hidden Markov Model (NHMM) of Charles et al. (1999), and (6) the modified Markov model–kernel probability density estimation (MMM–KDE) downscaling technique of Mehrotra and Sharma (2007). The results showed that the simple Scaling approach provided relatively robust results for a range of statistics when GCM forcing data was used, and was therefore recommended for regional water availability and planning studies (subject to certain limitations as mentioned in conclusion section). The stochastic methods better capture changes to a fuller range of rainfall statistics and are recommended for detailed catchment modelling studies. In particular, the stochastic methods show better results for daily extreme rainfall (e.g. flooding/low flow) as the simulations are not based purely on temporal/spatial rainfall patterns observed in the past, and a hybrid GLIMCLIM occurrence-KDE amounts model is recommended based on performance for individual statistics. For GCM downscaled simulations, biases in annual mean and standard deviation of ±5% and −30% were observed typically, and no single model performed well over all timescales/statistics, suggesting that the user beware of model limitations when applying downscaling methods for various purposes. A brief demonstration of predictor biases is presented, highlighting that biases observed in GCM predictors can cause poorer performance during GCM validation, and that investigation of these biases should inform choice of GCMs, GCM predictors, and the downscaling methods that use them.
Author Nguyen, Kim C.
Charles, Stephen P.
Chandler, Richard E.
Frost, Andrew J.
Mehrotra, R.
Fu, Guobin
Fernandez, Elodie
Chiew, Francis H.S.
Timbal, Bertrand
Kirono, Dewi G.C.
Kent, David M.
McGregor, John L.
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  surname: Frost
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  organization: Climate and Water Division, Australian Bureau of Meteorology, PO Box 413, Darlinghurst NSW 1300, Australia
– sequence: 2
  givenname: Stephen P.
  surname: Charles
  fullname: Charles, Stephen P.
  organization: CSIRO Water for a Healthy Country Flagship, CSIRO Land and Water, Private Bag 5, Wembley WA 6913, Australia
– sequence: 3
  givenname: Bertrand
  surname: Timbal
  fullname: Timbal, Bertrand
  organization: Centre for Australian Weather and Climate Research, Australian Bureau of Meteorology, PO Box 1289, Melbourne VIC 3001, Australia
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  givenname: Francis H.S.
  surname: Chiew
  fullname: Chiew, Francis H.S.
  organization: CSIRO Water for a Healthy Country Flagship, CSIRO Land and Water, PO Box 1666, Canberra ACT 2601, Australia
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  surname: Mehrotra
  fullname: Mehrotra, R.
  organization: School of Civil and Environmental Engineering, University of New South Wales, Sydney NSW 2052 , Australia
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  givenname: Kim C.
  surname: Nguyen
  fullname: Nguyen, Kim C.
  organization: Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Private Bag 1, Aspendale VIC 3195, Australia
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  givenname: Richard E.
  surname: Chandler
  fullname: Chandler, Richard E.
  organization: Department of Statistical Science, University College London, London WC1E 6BT, United Kingdom
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  givenname: John L.
  surname: McGregor
  fullname: McGregor, John L.
  organization: Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Private Bag 1, Aspendale VIC 3195, Australia
– sequence: 9
  givenname: Guobin
  surname: Fu
  fullname: Fu, Guobin
  organization: CSIRO Water for a Healthy Country Flagship, CSIRO Land and Water, Private Bag 5, Wembley WA 6913, Australia
– sequence: 10
  givenname: Dewi G.C.
  surname: Kirono
  fullname: Kirono, Dewi G.C.
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  givenname: Elodie
  surname: Fernandez
  fullname: Fernandez, Elodie
  organization: Centre for Australian Weather and Climate Research, Australian Bureau of Meteorology, PO Box 1289, Melbourne VIC 3001, Australia
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  givenname: David M.
  surname: Kent
  fullname: Kent, David M.
  organization: Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Private Bag 1, Aspendale VIC 3195, Australia
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Issue 1
Keywords CCAM
Scaling method
Hidden Markov model
GLM
Modified Markov model
Downscaling
Analogue method
software
Australasia
rain water
digital simulation
drainage basins
performances
flow
rainfall
atmospheric precipitation
probability density
testing
inundations
climate
linear models
planning
prediction
seasonal variations
standard deviation
statistics
Language English
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Hendon, Thompson, Wheeler (b0105) 2007; 20
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Chiew, Kirono, Kent, Frost, Charles, Timbal, Nguyen, Fu (b0055) 2010; 387
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Snippet ► We compare a range of multi-site rainfall downscaling models for hydrological purposes. ► Dynamic and stochastic models were compared using many rainfall...
Six methods of downscaling GCM simulations to multi-site daily precipitation were applied to a set of 30 rain gauges located within South-Eastern Australia....
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SubjectTerms Analogue method
Australia
CCAM
climate models
Computer simulation
computer software
Density
Downscaling
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
GLM
Hidden Markov model
Hydrology
Hydrology. Hydrogeology
linear models
Mathematical models
Modified Markov model
Natural hazards: prediction, damages, etc
prediction
probability
rain
rain gauges
Rainfall
Scaling method
Software packages
Statistics
Stochasticity
time series analysis
watersheds
Title A comparison of multi-site daily rainfall downscaling techniques under Australian conditions
URI https://dx.doi.org/10.1016/j.jhydrol.2011.06.021
https://www.proquest.com/docview/1365038577
https://www.proquest.com/docview/1671454009
https://www.proquest.com/docview/899166015
Volume 408
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