Lifespan of mountain ranges scaled by feedbacks between landsliding and erosion by rivers.
about
Self-organization of river channels as a critical filter on climate signals.Climate and topography control the size and flux of sediment produced on steep mountain slopes.Dramatic undercutting of piedmont rivers after the 2008 Wenchuan Ms 8.0 Earthquake.Storm-triggered landslides in the Peruvian Andes and implications for topography, carbon cycles, and biodiversityCombined hillslope diffusion and sediment transport simulation applied to landscape dynamics modellingRapid post-seismic landslide evacuation boosted by dynamic river width
P2860
Lifespan of mountain ranges scaled by feedbacks between landsliding and erosion by rivers.
description
2013 nî lūn-bûn
@nan
2013 թուականի Յունիսին հրատարակուած գիտական յօդուած
@hyw
2013 թվականի հունիսին հրատարակված գիտական հոդված
@hy
2013年の論文
@ja
2013年論文
@yue
2013年論文
@zh-hant
2013年論文
@zh-hk
2013年論文
@zh-mo
2013年論文
@zh-tw
2013年论文
@wuu
name
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@ast
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@en
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@nl
type
label
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@ast
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@en
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@nl
prefLabel
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@ast
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@en
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@nl
P2860
P50
P356
P1433
P1476
Lifespan of mountain ranges sc ...... sliding and erosion by rivers.
@en
P2860
P2888
P304
P356
10.1038/NATURE12218
P407
P577
2013-06-01T00:00:00Z
P6179
1008841590