nTo
ground validate AMSR-E measurements
nTo test
data assimilation of SM using AMSR-E or surrogate
nTo test
data assimilation of SM using discharge data (in heavily
vegetated areas)
nTo
understand scaling properties of SM from Ha to
100km2 scale in semi-arid
–To
better understanding C, P balance in semi-arid
catchments
–To
understand floodplain as a temp storage for sediment
from hillslope to river.