Tectonically dominant surface denudation and topography in the Himalaya: Evidence from coupling between bedrock channel and valley hillslope processes

Drainage topographic and hydrological data used for channel and valley hillslope analysis. Each of the 16 table files share the same table head with 10 columns detailed in following: <b>Node</b>: Node number increasing downstream along trunk channel in the drainage analyzed. <b>Length/m</b>: Upstream channel length in meter at each node.<b>Ele/m</b>: Elevation in meter at each node.<b>Area/m^2</b>: Upstream drainagearea in m²at each node.<b>Sc</b>: Local channel gradient at each node.<b>Sh</b>: Average hillslope related to each node.<b>Q/m^3</b>: Upstream accumulated discharge in m³at each node.<b>lnQ</b>: Logarithmic value of upstream discharge at each node.<b>lnSc</b>: Logarithmic value of channel gradientat each node.<b>lnSh</b>: Logarithmic value of valley hillslope at each node.