Carthey, A. J.R.

Fryirs, K. A.

Larkin, Z. T.

Ralph, T. J.

Tooth, S.

English

An amendment to this paper has been published and can be accessed via a link at the top of the paper.</p

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Aberystwyth UniversityAuthor CorrectionLarkin, Z. T.; Ralph, T. J.; Tooth, S.; Fryirs, K. A.; Carthey, A. J.R.Published in:Scientific ReportsDOI:10.1038/s41598-020-69597-5Publication date:2020Citation for published version (APA):Larkin, Z. T., Ralph, T. J., Tooth, S., Fryirs, K. A., & Carthey, A. J. R. (2020). Author Correction: Identifyingthreshold responses of Australian dryland rivers to future hydroclimatic change (Scientific Reports, (2020), 10, 1,(6653), 10.1038/s41598-020-63622-3). Scientific Reports, 10(1), [12525]. https://doi.org/10.1038/s41598-020-69597-5Document LicenseCC BYGeneral rightsCopyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) areretained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by thelegal requirements associated with these rights.            • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study orresearch.            • You may not further distribute the material or use it for any profit-making activity or commercial gain            • You may freely distribute the URL identifying the publication in the Aberystwyth Research PortalTake down policyIf you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediatelyand investigate your claim.tel: +44 1970 62 2400email: is@aber.ac.ukDownload date: 30. Aug. 20211Vol.:(0123456789)Scientific RepoRtS |        (2020) 10:12525  | https://doi.org/10.1038/s41598-020-69597-5www.nature.com/scientificreportsAuthor correction: identifying threshold responses of Australian dryland rivers to future hydroclimatic changeZ. t. Larkin , t. J. Ralph , S. tooth , K. A. fryirs  & A. J. R. carthey Correction to: Scientific Reports https ://doi.org/10.1038/s4159 8-020-63622 -3, published online 20 April 2020This Article contains errors in the in-text citations. In the Methods section, under the subheading ‘Climate data and future climate projections’,“To derive future precipitation and potential evapotranspiration, we used outputs from 16 downscaled global climate models (GCMs) that were part of the Intergovernmental Panel on Climate Change’s (IPCC) Fifth Coupled Model Intercomparison Project,  (CMIP558).”should read:“To derive future precipitation and potential evapotranspiration, we used outputs from 16 downscaled global climate models (GCMs) that were part of the Intergovernmental Panel on Climate Change’s (IPCC) Fifth Coupled Model Intercomparison Project,  (CMIP554).”And, in the same section,“Future projected precipitation is an output from the CMIP5 models. Mean annual temperature (Tmean) and annual temperature range (Trange) were the outputs used in conjunction with solar radiation (RA) to model future potential evapotranspiration (PET) using the Hargreaves-Samani equation (Eq. (1)59,60,61):The Hargreaves-Samani equation was used to calculate the modern AI used in this  study57 and therefore was also used for the future projections.”should read:“Future projected precipitation is an output from the CMIP5 models. Mean annual temperature (Tmean) and annual temperature range (Trange) were the outputs used in conjunction with solar radiation (RA) to model future potential evapotranspiration (PET) using the Hargreaves-Samani equation (Eq. (1)54,58–61):The Hargreaves-Samani equation was used to calculate the modern AI used in this  study57,58 and therefore was also used for the future projections.”Equation (1)PET = 0.0023RA(Tmean+ 17.8)Trange0.5Equation (1) PET = 0.0023RA(Tmean+ 17.8)Trange0.5open2Vol:.(1234567890)Scientific RepoRtS |        (2020) 10:12525  | https://doi.org/10.1038/s41598-020-69597-5www.nature.com/scientificreports/Open Access  This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creat iveco mmons .org/licen ses/by/4.0/.© The Author(s) 2020

Author Correction: Identifying threshold responses of Australian dryland rivers to future hydroclimatic change

Aberystwyth UniversityAuthor CorrectionLarkin, Z. T.; Ralph, T. J.; Tooth, S.; Fryirs, K. A.; Carthey, A. J.R.Published in:Scientific ReportsDOI:10.1038/s41598-020-69597-5Publication date:2020Citation for published version (APA):Larkin, Z. T., Ralph, T. J., Tooth, S., Fryirs, K. A., & Carthey, A. J. R. (2020). Author Correction: Identifyingthreshold responses of Australian dryland rivers to future hydroclimatic change (Scientific Reports, (2020), 10, 1,(6653), 10.1038/s41598-020-63622-3). Scientific Reports, 10(1), [12525]. https://doi.org/10.1038/s41598-020-69597-5Document LicenseCC BYGeneral rightsCopyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) areretained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by thelegal requirements associated with these rights.            • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study orresearch.            • You may not further distribute the material or use it for any profit-making activity or commercial gain            • You may freely distribute the URL identifying the publication in the Aberystwyth Research PortalTake down policyIf you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediatelyand investigate your claim.tel: +44 1970 62 2400email: is@aber.ac.ukDownload date: 28. Oct. 20221Vol.:(0123456789)Scientific RepoRtS |        (2020) 10:12525  | https://doi.org/10.1038/s41598-020-69597-5www.nature.com/scientificreportsAuthor correction: identifying threshold responses of Australian dryland rivers to future hydroclimatic changeZ. t. Larkin , t. J. Ralph , S. tooth , K. A. fryirs  & A. J. R. carthey Correction to: Scientific Reports https ://doi.org/10.1038/s4159 8-020-63622 -3, published online 20 April 2020This Article contains errors in the in-text citations. In the Methods section, under the subheading ‘Climate data and future climate projections’,“To derive future precipitation and potential evapotranspiration, we used outputs from 16 downscaled global climate models (GCMs) that were part of the Intergovernmental Panel on Climate Change’s (IPCC) Fifth Coupled Model Intercomparison Project,  (CMIP558).”should read:“To derive future precipitation and potential evapotranspiration, we used outputs from 16 downscaled global climate models (GCMs) that were part of the Intergovernmental Panel on Climate Change’s (IPCC) Fifth Coupled Model Intercomparison Project,  (CMIP554).”And, in the same section,“Future projected precipitation is an output from the CMIP5 models. Mean annual temperature (Tmean) and annual temperature range (Trange) were the outputs used in conjunction with solar radiation (RA) to model future potential evapotranspiration (PET) using the Hargreaves-Samani equation (Eq. (1)59,60,61):The Hargreaves-Samani equation was used to calculate the modern AI used in this  study57 and therefore was also used for the future projections.”should read:“Future projected precipitation is an output from the CMIP5 models. Mean annual temperature (Tmean) and annual temperature range (Trange) were the outputs used in conjunction with solar radiation (RA) to model future potential evapotranspiration (PET) using the Hargreaves-Samani equation (Eq. (1)54,58–61):The Hargreaves-Samani equation was used to calculate the modern AI used in this  study57,58 and therefore was also used for the future projections.”Equation (1)PET = 0.0023RA(Tmean+ 17.8)Trange0.5Equation (1) PET = 0.0023RA(Tmean+ 17.8)Trange0.5open2Vol:.(1234567890)Scientific RepoRtS |        (2020) 10:12525  | https://doi.org/10.1038/s41598-020-69597-5www.nature.com/scientificreports/Open Access  This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creat iveco mmons .org/licen ses/by/4.0/.© The Author(s) 2020

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Author Correction:Identifying threshold responses of Australian dryland rivers to future hydroclimatic change (Scientific Reports, (2020), 10, 1, (6653), 10.1038/s41598-020-63622-3)

Author Correction:Identifying threshold responses of Australian dryland rivers to future hydroclimatic change (Scientific Reports, (2020), 10, 1, (6653), 10.1038/s41598-020-63622-3)

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