Adaptation of Climate Model Projections of Streamflow to Account for Upstream Anthropogenic Impairments. Townsend, N. T. & Gutzler, D. S. JAWRA Journal of the American Water Resources Association, 2020. _eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/1752-1688.12851![Adaptation of Climate Model Projections of Streamflow to Account for Upstream Anthropogenic Impairments [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex A statistical procedure is developed to adjust natural streamflows simulated by dynamical models in downstream reaches, to account for anthropogenic impairments to flow that are not considered in the model. The resulting normalized downstream flows are appropriate for use in assessments of future anthropogenically impaired flows in downstream reaches. The normalization is applied to assess the potential effects of climate change on future water availability on the Rio Grande at a gage just above the major storage reservoir on the river. Model-simulated streamflow values were normalized using a statistical parameterization based on two constants that relate observed and simulated flows over a 50-year historical baseline period (1964–2013). The first normalization constant is a ratio of the means, and the second constant is the ratio of interannual standard deviations between annual gaged and simulated flows. This procedure forces the gaged and simulated flows to have the same mean and variance over the baseline period. The normalization constants can be kept fixed for future flows, which effectively assumes that upstream water management does not change in the future, or projected management changes can be parameterized by adjusting the constants. At the gage considered in this study, the effect of the normalization is to reduce simulated historical flow values by an average of 72% over an ensemble of simulations, indicative of the large fraction of natural flow diverted from the river upstream from the gage. A weak tendency for declining flow emerges upon averaging over a large ensemble, with tremendous variability among the simulations. By the end of the 21st Century the higher-emission scenarios show more pronounced declines in streamflow.
@article{townsend_adaptation_2020,
title = {Adaptation of {Climate} {Model} {Projections} of {Streamflow} to {Account} for {Upstream} {Anthropogenic} {Impairments}},
volume = {n/a},
copyright = {© 2020 American Water Resources Association},
issn = {1752-1688},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1111/1752-1688.12851},
doi = {10.1111/1752-1688.12851},
abstract = {A statistical procedure is developed to adjust natural streamflows simulated by dynamical models in downstream reaches, to account for anthropogenic impairments to flow that are not considered in the model. The resulting normalized downstream flows are appropriate for use in assessments of future anthropogenically impaired flows in downstream reaches. The normalization is applied to assess the potential effects of climate change on future water availability on the Rio Grande at a gage just above the major storage reservoir on the river. Model-simulated streamflow values were normalized using a statistical parameterization based on two constants that relate observed and simulated flows over a 50-year historical baseline period (1964–2013). The first normalization constant is a ratio of the means, and the second constant is the ratio of interannual standard deviations between annual gaged and simulated flows. This procedure forces the gaged and simulated flows to have the same mean and variance over the baseline period. The normalization constants can be kept fixed for future flows, which effectively assumes that upstream water management does not change in the future, or projected management changes can be parameterized by adjusting the constants. At the gage considered in this study, the effect of the normalization is to reduce simulated historical flow values by an average of 72\% over an ensemble of simulations, indicative of the large fraction of natural flow diverted from the river upstream from the gage. A weak tendency for declining flow emerges upon averaging over a large ensemble, with tremendous variability among the simulations. By the end of the 21st Century the higher-emission scenarios show more pronounced declines in streamflow.},
language = {en},
number = {n/a},
urldate = {2020-05-13},
journal = {JAWRA Journal of the American Water Resources Association},
author = {Townsend, Nolan T. and Gutzler, David S.},
year = {2020},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/1752-1688.12851},
keywords = {climate, drought, streamflow, water management},
}
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The normalization is applied to assess the potential effects of climate change on future water availability on the Rio Grande at a gage just above the major storage reservoir on the river. Model-simulated streamflow values were normalized using a statistical parameterization based on two constants that relate observed and simulated flows over a 50-year historical baseline period (1964–2013). The first normalization constant is a ratio of the means, and the second constant is the ratio of interannual standard deviations between annual gaged and simulated flows. This procedure forces the gaged and simulated flows to have the same mean and variance over the baseline period. The normalization constants can be kept fixed for future flows, which effectively assumes that upstream water management does not change in the future, or projected management changes can be parameterized by adjusting the constants. At the gage considered in this study, the effect of the normalization is to reduce simulated historical flow values by an average of 72% over an ensemble of simulations, indicative of the large fraction of natural flow diverted from the river upstream from the gage. A weak tendency for declining flow emerges upon averaging over a large ensemble, with tremendous variability among the simulations. 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