Identifying threshold responses of Australian dryland rivers to future hydroclimatic change

Abstract Rivers provide crucial ecosystem services in water-stressed drylands. Australian dryland rivers are geomorphologically diverse, ranging from through-going, single channels to discontinuous, multi-channelled systems, yet we have limited understanding of their sensitivity to future hydroclima...

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Autores principales: Z. T. Larkin, T. J. Ralph, S. Tooth, K. A. Fryirs, A. J. R. Carthey
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Lenguaje:EN
Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/02d43724ba1a4c128778b979fd39bcd6
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spelling oai:doaj.org-article:02d43724ba1a4c128778b979fd39bcd62021-12-02T18:27:50ZIdentifying threshold responses of Australian dryland rivers to future hydroclimatic change10.1038/s41598-020-63622-32045-2322https://doaj.org/article/02d43724ba1a4c128778b979fd39bcd62020-04-01T00:00:00Zhttps://doi.org/10.1038/s41598-020-63622-3https://doaj.org/toc/2045-2322Abstract Rivers provide crucial ecosystem services in water-stressed drylands. Australian dryland rivers are geomorphologically diverse, ranging from through-going, single channels to discontinuous, multi-channelled systems, yet we have limited understanding of their sensitivity to future hydroclimatic changes. Here, we characterise for the first time the geomorphology of 29 dryland rivers with catchments across a humid to arid gradient covering >1,800,000 km2 of continental eastern and central Australia. Statistical separation of five specific dominantly alluvial river types and quantification of their present-day catchment hydroclimates enables identification of potential thresholds of change. Projected aridity increases across eastern Australia by 2070 (RCP4.5) will result in ~80% of the dryland rivers crossing a threshold from one type to another, manifesting in major geomorphological changes. Dramatic cases will see currently through-going rivers (e.g. Murrumbidgee, Macintyre) experience step changes towards greater discontinuity, characterised by pronounced downstream declines in channel size and local termination. Expanding our approach to include other river styles (e.g. mixed bedrock-alluvial) would allow similar analyses of dryland rivers globally where hydroclimate is an important driver of change. Early identification of dryland river responses to future hydroclimatic change has far-reaching implications for the ~2 billion people that live in drylands and rely on riverine ecosystem services.Z. T. LarkinT. J. RalphS. ToothK. A. FryirsA. J. R. CartheyNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 10, Iss 1, Pp 1-15 (2020)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Z. T. Larkin
T. J. Ralph
S. Tooth
K. A. Fryirs
A. J. R. Carthey
Identifying threshold responses of Australian dryland rivers to future hydroclimatic change
description Abstract Rivers provide crucial ecosystem services in water-stressed drylands. Australian dryland rivers are geomorphologically diverse, ranging from through-going, single channels to discontinuous, multi-channelled systems, yet we have limited understanding of their sensitivity to future hydroclimatic changes. Here, we characterise for the first time the geomorphology of 29 dryland rivers with catchments across a humid to arid gradient covering >1,800,000 km2 of continental eastern and central Australia. Statistical separation of five specific dominantly alluvial river types and quantification of their present-day catchment hydroclimates enables identification of potential thresholds of change. Projected aridity increases across eastern Australia by 2070 (RCP4.5) will result in ~80% of the dryland rivers crossing a threshold from one type to another, manifesting in major geomorphological changes. Dramatic cases will see currently through-going rivers (e.g. Murrumbidgee, Macintyre) experience step changes towards greater discontinuity, characterised by pronounced downstream declines in channel size and local termination. Expanding our approach to include other river styles (e.g. mixed bedrock-alluvial) would allow similar analyses of dryland rivers globally where hydroclimate is an important driver of change. Early identification of dryland river responses to future hydroclimatic change has far-reaching implications for the ~2 billion people that live in drylands and rely on riverine ecosystem services.
format article
author Z. T. Larkin
T. J. Ralph
S. Tooth
K. A. Fryirs
A. J. R. Carthey
author_facet Z. T. Larkin
T. J. Ralph
S. Tooth
K. A. Fryirs
A. J. R. Carthey
author_sort Z. T. Larkin
title Identifying threshold responses of Australian dryland rivers to future hydroclimatic change
title_short Identifying threshold responses of Australian dryland rivers to future hydroclimatic change
title_full Identifying threshold responses of Australian dryland rivers to future hydroclimatic change
title_fullStr Identifying threshold responses of Australian dryland rivers to future hydroclimatic change
title_full_unstemmed Identifying threshold responses of Australian dryland rivers to future hydroclimatic change
title_sort identifying threshold responses of australian dryland rivers to future hydroclimatic change
publisher Nature Portfolio
publishDate 2020
url https://doaj.org/article/02d43724ba1a4c128778b979fd39bcd6
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