2012
DOI: 10.1029/2011wr011123
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Bayesian parameter uncertainty modeling in a macroscale hydrologic model and its impact on Indian river basin hydrology under climate change

Abstract: [1] Macroscale hydrologic models (MHMs) were developed to study changes in land surface hydrology due to changing climate over large domains, such as continents or large river basins. However, there are many sources of uncertainty introduced in MHM hydrological simulation, such as model structure error, ineffective model parameters, and low-accuracy model input or validation data. It is hence important to model the uncertainty arising in projection results from an MHM. The objective of this study is to present… Show more

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Cited by 55 publications
(28 citation statements)
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“…Investigation into the uncertainty introduced by (i) the climate driving data and (ii) the way the hydrological models were used revealed that "hydrological" errors attributable to the definition of input flow data in the tributaries are of less significance than those associated with the derivation and downscaling of climate model rainfall, air temperature and solar radiation variables. This is not the first study worldwide to draw such a conclusion and it corroborates the findings of Raje and Krishnan (2012) for example. Indeed, in formulating FFH, Prudhomme et al (2013) compared FFH with pre-2000 observations and identified the largest mismatches in dry conditions and in drier regions; these non-systematic departures were attributed in the main to climate rather than hydrological model uncertainty.…”
Section: Implications For the Models Underpinning The Predictionssupporting
confidence: 84%
“…Investigation into the uncertainty introduced by (i) the climate driving data and (ii) the way the hydrological models were used revealed that "hydrological" errors attributable to the definition of input flow data in the tributaries are of less significance than those associated with the derivation and downscaling of climate model rainfall, air temperature and solar radiation variables. This is not the first study worldwide to draw such a conclusion and it corroborates the findings of Raje and Krishnan (2012) for example. Indeed, in formulating FFH, Prudhomme et al (2013) compared FFH with pre-2000 observations and identified the largest mismatches in dry conditions and in drier regions; these non-systematic departures were attributed in the main to climate rather than hydrological model uncertainty.…”
Section: Implications For the Models Underpinning The Predictionssupporting
confidence: 84%
“…Considering also the wider impacts of changes in this region, and the research community's ability to project them, improvements in the representation of land surface hydrology in climate models are needed to decrease projection uncertainty. Limitations in this regard have likely contributed to highly uncertain projections in other major basins (Raje and Krishnan 2012;Bring et al 2015;Asokan et al 2016). …”
Section: Discussionmentioning
confidence: 99%
“…They concluded that modeled streamflow is sensitive to three parameters, allowing for a more parsimonious reduced set of model parameters. Raje and Krishnan (2012) extended this analysis with Markov Chain Monte Carlo methods to model uncertainty and eventually project future discharge with respect to climate change. They concluded that uncertainty resulting from a general circulation model (GCM) is larger than that from parameter uncertainties in VIC.…”
Section: Introductionmentioning
confidence: 99%