Conceptual Model Modification and the Millennium Drought of Southeastern Australia
Long-term droughts observed in southern Australia have changed relationships between annual rainfall and runoff and tested some of the assumptions implicit in rainfall–runoff models used in these areas. Predictive confidence across these periods is when low using the more commonly used rainfall–runo...
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doaj-24d2055c8eb243b2956ae50b3d21ed662021-03-02T00:04:22ZengMDPI AGWater2073-44412021-03-011366966910.3390/w13050669Conceptual Model Modification and the Millennium Drought of Southeastern AustraliaJustin Hughes0Nick Potter1Lu Zhang2Robert Bridgart3CSIRO Land and Water, Canberra, ACT 2601, AustraliaCSIRO Land and Water, Canberra, ACT 2601, AustraliaCSIRO Land and Water, Canberra, ACT 2601, AustraliaCSIRO Land and Water, Clayton South, VIC 3169, AustraliaLong-term droughts observed in southern Australia have changed relationships between annual rainfall and runoff and tested some of the assumptions implicit in rainfall–runoff models used in these areas. Predictive confidence across these periods is when low using the more commonly used rainfall–runoff models. Here we modified the GR4J model to better represent surface water–groundwater connection and its role in runoff generation. The modified model (GR7J) was tested in 137 catchments in south-east Australia. Models were calibrated during “wetter” periods and simulation across drought periods was assessed against observations. GR7J performed better than GR4J in evaluation during drought periods where bias was significantly lower and showed improved fit across the flow duration curve especially at low flows. The largest improvements in predictive performance were for catchments where there were larger changes in the annual rainfall–runoff relationship. The predictive performance of the GR7J model was more sensitive to objective function used than GR4J. The use of an objective function that combined daily and annual error produced a better goodness of fit when measured against 80, 50 and 20 percent excedance flow quantiles and reduced evaluation bias, especially for the GR7J model.https://www.mdpi.com/2073-4441/13/5/669droughtrainfall–runoff modelnon-stationaritygroundwater–surface water connectionobjective functions |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Justin Hughes Nick Potter Lu Zhang Robert Bridgart |
spellingShingle |
Justin Hughes Nick Potter Lu Zhang Robert Bridgart Conceptual Model Modification and the Millennium Drought of Southeastern Australia Water drought rainfall–runoff model non-stationarity groundwater–surface water connection objective functions |
author_facet |
Justin Hughes Nick Potter Lu Zhang Robert Bridgart |
author_sort |
Justin Hughes |
title |
Conceptual Model Modification and the Millennium Drought of Southeastern Australia |
title_short |
Conceptual Model Modification and the Millennium Drought of Southeastern Australia |
title_full |
Conceptual Model Modification and the Millennium Drought of Southeastern Australia |
title_fullStr |
Conceptual Model Modification and the Millennium Drought of Southeastern Australia |
title_full_unstemmed |
Conceptual Model Modification and the Millennium Drought of Southeastern Australia |
title_sort |
conceptual model modification and the millennium drought of southeastern australia |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2021-03-01 |
description |
Long-term droughts observed in southern Australia have changed relationships between annual rainfall and runoff and tested some of the assumptions implicit in rainfall–runoff models used in these areas. Predictive confidence across these periods is when low using the more commonly used rainfall–runoff models. Here we modified the GR4J model to better represent surface water–groundwater connection and its role in runoff generation. The modified model (GR7J) was tested in 137 catchments in south-east Australia. Models were calibrated during “wetter” periods and simulation across drought periods was assessed against observations. GR7J performed better than GR4J in evaluation during drought periods where bias was significantly lower and showed improved fit across the flow duration curve especially at low flows. The largest improvements in predictive performance were for catchments where there were larger changes in the annual rainfall–runoff relationship. The predictive performance of the GR7J model was more sensitive to objective function used than GR4J. The use of an objective function that combined daily and annual error produced a better goodness of fit when measured against 80, 50 and 20 percent excedance flow quantiles and reduced evaluation bias, especially for the GR7J model. |
topic |
drought rainfall–runoff model non-stationarity groundwater–surface water connection objective functions |
url |
https://www.mdpi.com/2073-4441/13/5/669 |
work_keys_str_mv |
AT justinhughes conceptualmodelmodificationandthemillenniumdroughtofsoutheasternaustralia AT nickpotter conceptualmodelmodificationandthemillenniumdroughtofsoutheasternaustralia AT luzhang conceptualmodelmodificationandthemillenniumdroughtofsoutheasternaustralia AT robertbridgart conceptualmodelmodificationandthemillenniumdroughtofsoutheasternaustralia |
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