Tropical Savannas CRC > Publications > Savanna Links > Issue 36, Jan-June 2009

Issue 36, January-July 2009


GIS tool instrumental in river research

TRaCK—Tropical Rivers and Coastal Knowledge—has around 1.2 million square kilometres of land within its research area in tropical northern Australia, much of it remote and inaccessible. A new GIS tool promises a dynamic and flexible way for researchers and land managers to examine  river data. By Mary O’Callaghan

Figure 1. The GIS-based geomorphic classification tool highlights that there are major differences between rivers in the Southern Gulf country and in the Kimberley. In this example, streams that are similar to the selected section of river are shown in red. Streams that are dissimilar are shown in green.

With such a large research area, it is easy to see why scientists can’t visit each river reach. For this reason, TRaCK research focuses on four catchments: the Daly in the Northern Territory, the Fitzroy in Western Australia, and the Mitchell and Flinders in Queensland. But how do we know whether we can confidently apply the findings from field work in one catchment to other catchments across the north?

The Mitchell and the Daly, two very different rivers: The Mitchell (pictured left) has a 1.5 kilometre-wide channel in its lower reaches which flows through an alluvial floodplain. When it is choked with sand it can shift sideways by 50–100 metres in some years. Large pools (up to several kilometres in length) form one year and disappear the next. By contrast, the lower Daly (pictured right) has a relatively narrow (about 100 metres wide) and stable channel, largely bounded by bedrock. Pools in this river tend to ‘stay put’.
The Mitchell and the Daly, two very different rivers: 

The Mitchell (pictured above) has a 1.5 kilometre-wide channel in its lower reaches which flows through an alluvial floodplain. When it is choked with sand it can shift sideways by 50–100 metres in some years. 

Large pools (up to several kilometres in length) form one year and disappear the next. By contrast, the lower Daly (pictured below) has a relatively narrow (about 100 metres wide) and stable channel, largely bounded by bedrock. Pools in this river tend to ‘stay put’. 

The Mitchell and the Daly, two very different rivers: The Mitchell (pictured left) has a 1.5 kilometre-wide channel in its lower reaches which flows through an alluvial floodplain. When it is choked with sand it can shift sideways by 50–100 metres in some years. Large pools (up to several kilometres in length) form one year and disappear the next. By contrast, the lower Daly (pictured right) has a relatively narrow (about 100 metres wide) and stable channel, largely bounded by bedrock. Pools in this river tend to ‘stay put’.

“There are some fundamental differences between, for example, the Mitchell and the Daly Rivers,” says Dr Andrew Brooks from Griffith University (see pictures right).

“So, it’s important to get the message across that, just because we’ve done a lot of detailed work on the Daly, for example, this doesn’t necessarily mean that it’s applicable across Australia.”

Dr Brooks and his team set out to develop a method for describing the similarity, or dissimilarity, of the region’s riverine landscapes, as part of a method for legitimately extrapolating information from one segment of river to another.

What they’ve come up with is a way of classifying rivers that Dr Brooks believes could make other classification systems redundant.

Overcoming scale and subjectivity

In the field of geomorphology—understanding landscapes —there is a long history of classification systems.
“Just about every government program doing research over large scales uses some sort of classification,” explains Dr Brooks. “The problem is that any classification system has a lot of subjectivity; and they are often designed for specific purposes.”

Understanding that different people use classifications for different reasons, Dr Brooks and colleague John Spencer thought they could develop a better, more flexible approach using large spatial data sets.

Driven by the users’ needs

What John Spencer has developed is an interactive GIS-based tool where you select a specific segment of river, choose one or more variables—such as stream slope, valley width, catchment area, drainage density, geology—and you are presented with a measure of similarity between your river segment and all others.

For categorical data, such as geology, where there are no degrees of similarity, river segments that are the same show up in red on the map; those that are different show up in green. For data that is continuously variable, such as elevation, river segments that are similar are shown in varying shades of colour that reflect the degree of similarity.

From there you can define how many classes you want and, at the click of a button, the system will generate your user-defined classification.

And, unlike most GIS-based classifications, you can save the specification for how you made it, in case you ever want to run it again or compare it to another version. You can also download the underlying layers of data that the classification comprises.

Not just another classification

According to Dr Brooks, this is not just another classification.

“It’s dynamic and flexible, and allows people to explore the data. It really is a quantum leap from other classifications,” he said.

“To my knowledge this is the first time anyone’s developed such a system anywhere in the world. And you can build on it—that’s the beauty of it. It’s not set in time, which is the major constraint with a lot of other classifications. We can update it as new data becomes available.”

The system is already providing insights.

“It is obvious that there are major differences between the Southern Gulf country and the Kimberley—really fundamental differences that people need to understand,” says Dr Brooks (Figure 1).  ‘If you’ve got a study on the Flinders River floodplain, it’s probably not going to be a lot of use to someone in the Kimberley.”

Dr Mark Kennard, a fish ecologist and senior research fellow at Griffith University, says the system’s advantage is its flexibility. “There is no single correct classification as it really depends on the particular environmental features the user is interested in,” he said, “so being able to do things on the fly and then quickly try again with a different combination of variables is great.

“I think it’s a really useful tool for the public, for scientists and for people doing field surveys where they need to stratify sites, comparing like with like.”

Because it’s so flexible, Dr Brooks is keen for different groups with different objectives to try it out.  

“The plan is to make the system available on the web so that people can run it from anywhere,” explained Dr Brooks.

“We need to know it is meaningful on the ground, that we are not just generating pretty maps. It has to be able to usefully distinguish one type of river from another.”

Contact

Dr Andrew Brooks, Griffith University
Email: andrew.brooks@griffith.edu.au

John Spencer, Griffith University
Email: j.spencer@griffith.edu.au

Reprinted with permission from ON TRaCK newsletter, Issue 2
www.track.gov.au

TRaCK

TRaCK brings together leading tropical river researchers and managers from Charles Darwin University, Griffith University, University of Western Australia, CSIRO, James Cook University, Australian National University, Geoscience Australia, Environmental Research Institute of the Supervising Scientist, Australian Institute of Marine Science, North Australia Indigenous Land and Sea Management Alliance, and the Governments of Qld, NT and WA.