Taking up where we left off in the previous post, we are going to explore
the spatial and temporal resolution. I am going to summarize key points from Watts, 2010 .
2.
Spatial resolution
Models can cover different spatial scales from few centimeters to
hundreds of kilometers. Hence, depending on the hydrological problem of interest,
the spatial resolution can be chosen according to the details that are to be described.
For instance, global hydrological cycles
are of hundreds of kilometers in spatial resolution. Such models require to be
broken down into smaller geographical units. This is where distributed
models come into the picture. Spatially distributed models process the
geographical units and produce results for each of them. So the whole catchment
is divided into sub areas.
On the opposite side there are lumped models, where the
whole hydrological system is considered as a single unit. For example a lumped
model of a catchment might consider only one point flow into the system and
give an averaged values for parameters such as soil moisture content.
Semi-distributed models sit between the lumped and distributed
models. These models are usually a series of lumped models.
3.
Temporal resolution
Hydrological models can be considered with different time-steps that
could range from few seconds to years. Some other models give averaged values
over a long time period. Model formulation has an impact on the chosen time
resolution. For instance, complex numerical models may behave unstable when
considering long time-steps. So it is up
to the modellers to choose the appropriate time resolution for the problem being
addressed.
So as we saw from this post and the previous post, there are
different factors and scales that modellers should consider when making the
decision of choosing a modelling approach. Next we are going to see what the
tools of decision making are when choosing a modelling approach.
Till next time,




