Partitioning of evaporation into transpiration, soil evaporation and interception: A comparison between isotope measurements and a HYDRUS-1D model + Corrigendum

(1)

Hydrol. Earth Syst. Sci., 16, 3261, 2012 www.hydrol-earth-syst-sci.net/16/3261/2012/ doi:10.5194/hess-16-3261-2012

Hydrology and

Earth System

Sciences

Corrigendum to

“Partitioning of evaporation into transpiration, soil evaporation and

interception: A comparison between isotope measurements and a

HYDRUS-1D model” published in Hydrol. Earth Syst. Sci., 16,

2605–2616, 2012

S. J. Sutanto1,3,*, J. Wenninger1,2, A. M. J. Coenders-Gerrits2, and S. Uhlenbrook1,2

1_{UNESCO-IHE, Department of Water Engineering, P.O. Box 3015, 2601 DA, Delft, The Netherlands} 2_{Delft University of Technology, Water Resources Section, P.O. Box 5048, 2600 GA, Delft, The Netherlands} 3_{Research Center for Water Resources, Ministry of Public Works, Jl. Ir. H. Djuanda 193, Bandung 40135, Indonesia} *_{now at: Institute for Marine and Atmospheric Research Utrecht (IMAU), University of Utrecht, Princetonplein 5, 3584 CC,}

Utrecht, The Netherlands

Correspondence to: S. J. Sutanto (s.j.sutanto@uu.nl)

Equation (2) on page 2608 should be as follow (without “t ”):

αA−B=

RA

RB

Equation (18) on page 2610 should be as follow:

δi=δf= n X j =1 (δsj·Hj·SWCj) SWC · Htotal

For description, change “i” into “j ”:

Where n is number of layer, δsj is the δ value in the soil

layer j , Hjis a correspondence depth of layer j , SCWjis the

soil water content in layer j , SWC is average of soil water content and Htotalis total depth.