The European macrohabitat river types (FCMacHT) is based on a number of physio-geographic factors associated with Expected Fish Communities (EFC). The 9 river types distinguished at a continental scale are however broad and various combinations of smaller habitat unit types may be recorded in each type. The habitat survey with help of MesoHABSIM modelling is a next step to more precise determination of the actual conditions for aquatic organisms at a given site under various hydrological conditions.
The purpose and background of the tool
Mesohabitat Simulation Model (MesoHABSIM) is an approach for modelling instream habitats. It consists of a data collection strategy and analytical techniques that allow the user to compute how much habitat is available for investigated fauna under specific environmental circumstances. It builds upon pre-existing physical habitat simulation models (e.g. PHABSIM) to predict an aquatic community's response to habitat modification. The model captures variations in stream morphology along the river into account and relates it to distribution of aquatic fauna. Mesohabitat types are defined by their hydromorphological units (HMUs), such as pools and rapids, geomorphology, land cover and other hydrological characteristics. Distribution of fish is observed in large number of HMU’s. Based on habitat characteristics of these units, mathematical functions describing relationship with fish abundance are calculated. The functions are used to predict the probability of species occurrence for each mapped mesohabitat.
Mesohabitats are mapped under multiple flow conditions at extensive sites along the river. This allows modelling of available fish habitat at a range of flows.
The results of MesoHABSIM create the framework for integrative analyses of many aspects of the ecosystem. It also allows managers to recreate reference conditions and evaluate possible instream and watershed restoration measures or alterations, such as dam removals or changes in water withdrawals. From the perspective of resource managers, it not only allows for quantitative measures of ecological integrity, but also creates a basis for making decisions where trade-offs between resource use and river restoration need to be considered.
Habitat modelling concept
Research has shown that the combination of streamflow variability and river mor¬phology (along with other factors such as water quality, energy inputs and biotic interactions) is a primary control on the processes that determine the composition and dynamics of stream ecosystems (KARR et al. 1986; STATZNER et al. 1988; MINSHALL 1988; HILDREW & TOWNSEND 1994; POFF & WARD 1989).
Following the development of the ecological niche theory (HURCHINTSON 1957), it became clear that living organisms can be affected by the variability of their whole environment. The observation that the aquatic animals respond to specific physical patterns in a stream, both at the population level over long periods of time and directly to patterns of physical habitat over a shorter timeframe, has provided the background for development of physical habitat models. Although physical variables are clearly not the only factors affecting abundance and health of organ¬isms in rivers (KARR et al. 1986), they provide effective assessment criteria due to their history of anthropogenic impact, predictability and ease of measurement (STALNAKER 1995).
In general, modelling of riverine physical habitat consists of two major procedures that together lead to an assessment of the impacts of various management options. Biological sampling is applied to determine habitat use by selected fish and/or invertebrate species. Spatial measurement provides a description of the morphologic/hydraulic habitat conditions in the studied water at a range of flows. Changes in these conditions with changing discharge can then be determined and variation in habitat suitability thus evaluated.
The selection of the variables used in physical habitat models arose from em¬pirical studies which demonstrated the association of fish (and invertebrates) with particular physical and chemical aspects of their available habitat (BININs & ElSERMANN 1979; JUNGWIRTH 1988; MILNER et al. 1985; RABENI & JACOBSON 1993: WRIGHT et al. 1993). The step was taken to link simple physical habitat use/description models to hydraulic models capable of predicting the variation of the key habitat variables in an incremental fashion (BOVEE 1982; GORE & NESTLER 1988). This allowed simulation of the relationship between stream discharge and an aggregate physical habitat quantity for life stages of a target aquatic species (e.g. fish). Thus, researchers simplified the analysis of anthropogenic changes (ORTH 1987) by modelling only the key habitat variables likely to change (which can also be measured relatively easily), and linking these with the preferences of aquatic species.
Data types
There are three major types of physical attributes that are incorporated in habitat modelling process: hydraulics, riverbed geometry and habitat dressing. Hydraulics includes the basic data on hydrology of the investigated river section, including characteristic multiannual average flows (average low flow, low flow threshold, medium flow threshold). The first step in preparation of a MesoHABSIM survey is to select the range of flows that will be closely analysed in the model. Field surveys are conducted usually at low flows, up to a low/medium flow threshold. These may vary with project objectives as well as with the investigation season. The MesoHABSIM surveys consist of multiple observations of at least three flows within the above range. This is the lowest number of observations necessary to develop habitat flow rating curves. At each flow condition, a set of measurements of water velocity and depth is taken in every HMU to assess the hydraulic parameters distribution.
Geometry of the river channel determines the number and distribution of HMU’s on investigated river section. This is assessed by HMU’s identification and measurements of water depth and substrate composition. In deep and narrow river beds runs, fast-runs, rapids and pools prevail, while in rivers with broad channel and flat banks glides, backwaters, riffles, or side arms are more frequent. Also, river slope is key factor for river channel geometry and habitat variability. Habitat dressing describes complexity and diversity of HMU, related to suitability for various groups of aquatic organisms. Features such as canopy shading, woody debris, water vegetation, boulder rocks, shallow margins, undercut banks, etc. are noted for each HMU in a simple scale (absent, present or abundant). Land use on both shores is also registered.
Flow chart
The flow diagram in Figure 2 and associated text in this section provide a step-by-step decision making guide.