GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale

Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley...
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Autor*in:	Ellis, C [verfasserIn] Roering, J J Sweeney, K E

Format:	Artikel
Sprache:	Englisch

Erschienen:	2015

Rechteinformationen:	Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science.

Übergeordnetes Werk:	Enthalten in: Science - Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883, 349(2015), 6243, Seite 51
Übergeordnetes Werk:	volume:349 ; year:2015 ; number:6243 ; pages:51

Links:	Link aufrufen

Katalog-ID:	OLC1969531916

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520			\|a Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.
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allfields	PQ20160211 (DE-627)OLC1969531916 (DE-599)GBVOLC1969531916 (PRQ)pubmed_primary_261389700 (KEY)0063888920150000349624300051geomorphologyexperimentalevidenceforhillslopecontr DE-627 ger DE-627 rakwb eng 500 DNB LING fid Ellis, C verfasserin aut GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes. Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science. Roering, J J oth Sweeney, K E oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 349(2015), 6243, Seite 51 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:349 year:2015 number:6243 pages:51 http://www.ncbi.nlm.nih.gov/pubmed/26138970 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2185 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4046 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 349 2015 6243 51
spelling	PQ20160211 (DE-627)OLC1969531916 (DE-599)GBVOLC1969531916 (PRQ)pubmed_primary_261389700 (KEY)0063888920150000349624300051geomorphologyexperimentalevidenceforhillslopecontr DE-627 ger DE-627 rakwb eng 500 DNB LING fid Ellis, C verfasserin aut GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes. Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science. Roering, J J oth Sweeney, K E oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 349(2015), 6243, Seite 51 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:349 year:2015 number:6243 pages:51 http://www.ncbi.nlm.nih.gov/pubmed/26138970 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2185 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4046 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 349 2015 6243 51
allfields_unstemmed	PQ20160211 (DE-627)OLC1969531916 (DE-599)GBVOLC1969531916 (PRQ)pubmed_primary_261389700 (KEY)0063888920150000349624300051geomorphologyexperimentalevidenceforhillslopecontr DE-627 ger DE-627 rakwb eng 500 DNB LING fid Ellis, C verfasserin aut GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes. Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science. Roering, J J oth Sweeney, K E oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 349(2015), 6243, Seite 51 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:349 year:2015 number:6243 pages:51 http://www.ncbi.nlm.nih.gov/pubmed/26138970 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2185 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4046 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 349 2015 6243 51
allfieldsGer	PQ20160211 (DE-627)OLC1969531916 (DE-599)GBVOLC1969531916 (PRQ)pubmed_primary_261389700 (KEY)0063888920150000349624300051geomorphologyexperimentalevidenceforhillslopecontr DE-627 ger DE-627 rakwb eng 500 DNB LING fid Ellis, C verfasserin aut GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes. Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science. Roering, J J oth Sweeney, K E oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 349(2015), 6243, Seite 51 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:349 year:2015 number:6243 pages:51 http://www.ncbi.nlm.nih.gov/pubmed/26138970 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2185 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4046 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 349 2015 6243 51
allfieldsSound	PQ20160211 (DE-627)OLC1969531916 (DE-599)GBVOLC1969531916 (PRQ)pubmed_primary_261389700 (KEY)0063888920150000349624300051geomorphologyexperimentalevidenceforhillslopecontr DE-627 ger DE-627 rakwb eng 500 DNB LING fid Ellis, C verfasserin aut GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes. Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science. Roering, J J oth Sweeney, K E oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 349(2015), 6243, Seite 51 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:349 year:2015 number:6243 pages:51 http://www.ncbi.nlm.nih.gov/pubmed/26138970 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2185 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4046 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 349 2015 6243 51
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title	GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale
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title_sort	geomorphology. experimental evidence for hillslope control of landscape scale
title_auth	GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale
abstract	Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.
abstractGer	Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.
abstract_unstemmed	Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.
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title_short	GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale
url	http://www.ncbi.nlm.nih.gov/pubmed/26138970
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Experimental evidence for hillslope control of landscape scale</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Landscape evolution theory suggests that climate sets the scale of landscape dissection by modulating the competition between diffusive processes that sculpt convex hillslopes and advective processes that carve concave valleys. However, the link between the relative dominance of hillslope and valley transport processes and landscape scale is difficult to demonstrate in natural landscapes due to the episodic nature of erosion. Here, we report results from laboratory experiments combining diffusive and advective processes in an eroding landscape. We demonstrate that rainsplash-driven disturbances in our experiments are a robust proxy for hillslope transport, such that increasing hillslope transport efficiency decreases drainage density. Our experimental results demonstrate how the coupling of climate-driven hillslope- and valley-forming processes, such as bioturbation and runoff, dictates the scale of eroding landscapes.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: Copyright © 2015, American Association for the Advancement of Science.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Roering, J J</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sweeney, K E</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Science</subfield><subfield code="d">Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883</subfield><subfield code="g">349(2015), 6243, Seite 51</subfield><subfield code="w">(DE-627)12931482X</subfield><subfield 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GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale

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