<i>tran</i>-SAS v1.0: a numerical model to compute catchment-scale hydrologic transport using StorAge Selection functions
This paper presents the <q><i>tran</i>-SAS</q> package, which includes a set of codes to model solute transport and water residence times through a hydrological system. The model is based on a catchment-scale approach that aims at reproducing the integrated response of the...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-04-01
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Series: | Geoscientific Model Development |
Online Access: | https://www.geosci-model-dev.net/11/1627/2018/gmd-11-1627-2018.pdf |
Summary: | This paper presents the <q><i>tran</i>-SAS</q> package, which
includes a set of codes to model solute transport and water residence times
through a hydrological system. The model is based on a catchment-scale
approach that aims at reproducing the integrated response of the system at
one of its outlets. The codes are implemented in MATLAB and are meant to be
easy to edit, so that users with minimal programming knowledge can adapt them
to the desired application. The problem of large-scale solute transport has
both theoretical and practical implications. On the one side, the ability to
represent the ensemble of water flow trajectories through a heterogeneous
system helps unraveling streamflow generation processes and allows us to make
inferences on plant–water interactions. On the other side, transport models
are a practical tool that can be used to estimate the persistence of solutes
in the environment. The core of the package is based on the implementation of
an age master equation (ME), which is solved using general StorAge Selection
(SAS) functions. The age ME is first converted into a set of ordinary
differential equations, each addressing the transport of an individual
precipitation input through the catchment, and then it is discretized using
an explicit numerical scheme. Results show that the implementation is
efficient and allows the model to run in short times. The numerical accuracy
is critically evaluated and it is shown to be satisfactory in most cases of
hydrologic interest. Additionally, a higher-order implementation is provided
within the package to evaluate and, if necessary, to improve the numerical
accuracy of the results. The codes can be used to model streamflow age and
solute concentration, but a number of additional outputs can be obtained by
editing the codes to further advance the ability to understand and model
catchment transport processes. |
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ISSN: | 1991-959X 1991-9603 |