Biophysical considerations in integrated catchment management : a modelling system for Northern Thailand
Abstract
A trend in environmental modelling and policy making has been to move towards the
use of integrated assessment methodologies as a means of balancing what are most
usually multi-issue problems with multiple stakeholders. These methodologies are
particularly relevant for the management of water resources given the interdisciplinary
nature of water problems. This thesis presents a Biophysical Toolbox that integrates
models for assessment of the outcomes of biophysical scenarios of water and land use
options. Outcomes are measured in terms of environmental indicators that are outputs of
the models.
The Biophysical Toolbox is comprised of three modules - the CATCHCROP crop
model, a hydrologic module based on the IHACRES rainfall-runoff model, and a
modified Universal Soil Loss Equation (USLE) approach. The models were designed to
have the following features: basic data requirements with which to drive the models;
relatively low parameterisation requirements thus limiting problems with error
accumulation; physically plausible, and easily transferred to other catchments. The aim
with integrated models of this type is to be able to discriminate between, and be
confident about, the relative changes in indicator outputs.
The CATCHCROP crop model was applied to subcatchments of Mae Chaem in northern
Thailand to identify: the impact of land management options (irrigation, fertilisation and
bunding status) on model outputs; and the sensitivities of deep drainage, surface runoff,
and crop yield estimates to the values of CATCHCROP model parameters. Model
behaviour was shown to be plausible when the land management of the crop was varied.
Results of a sensitivity analysis demonstrated the considerable non-linearity in the
response of CATCHCROP outputs to parameter values, and identified which
parameters most influenced the behaviour of the model. Two parameters were found to
be substantially insensitive.
Estimates of potential erosion were sensitive to the choice of equations describing the
topographic and rainfall erosivity factors of the USLE. Despite this, the choice of
equations should not affect the utility of the Biophysical Toolbox where direction and relative values of indicators between scenanos are important. Similar values of the
erosion susceptibility term in the USLE were obtained for each land unit whether the
procedure was applied on each land unit or on a more detailed grid-basis.
Testing of the hydrologic model involved analysing: the performance of the
regionalisation methodology in predicting discharge; changes in hydrologic response
under forest cover changes; and sensitivities in the model outputs to changes in values
of CATCHCROP model parameters. The regionalisation procedure generally overestimated
annual discharge although is capable of capturing relative changes. As forest
cover decreases, the proportion of streamflow in the quick flow component increased,
annual and wet season discharge increased, and dry season discharge decreased. The
relative quick and slow flow volume components were strongly sensitive to changes in
forest cover. Six main parameters within the CATCHCROP model were identified as
greatly impacting the calculation of quick and slow flow components.
The Biophysical Toolbox was then used to examine deforestation, climate, and land
management scenarios for the Mae Uam subcatchment of the Mae Chaem catchment,
highlighting tradeoffs among indicators and raising questions about perceived impacts.
The main results of the scenarios can be summarised as: deforestation scenarios do not
greatly impact streamflow although increases in potential erosion are extreme; upland
rice and vegetable crops are particularly susceptible to 'unacceptable' rates of erosion
on steeply sloping lands; wet season crop yields are more dependant on plot fertility
than on irrigation or bunding status. Sensitivity analysis of the whole toolbox was also
performed. Despite potentially large impacts of CATCHCROP parameter changes on
the re-calculation of the hydrology parameters, this did not translate into large
differences in total seasonal discharge.
Comprehensive testing of the Biophysical Toolbox illustrated the potential, and the
plausible behaviour, of the toolbox for exploring aspects of land and water resource
management in catchments in northern Thailand. Most useful to improve confidence in
model performance would be further testing of the hydrologic module in instrumented
catchments that have undergone significant forest cover changes over the period of
hydrologic record.
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