Wet Tropics

The Wet Tropics Freshwater Biogeographic Province (FBP) consists of the Jeannie, Endeavour, Daintree, Mossman, Barron, Russell-Mulgrave, Johnstone, Tully, Murray, Hinchinbrook Island, Herbert, and Black drainage basins, and is located in the north-east of the State. The FBP covers the Wet Tropics, Cape York Peninsula, and Einasleigh Uplands Bioregions.

 

Key Ecosystem Drivers – Wet Tropics FBP

Wet season Temperature varies spatially with no gradient High relief ratio Convex and concurve bank shapes Percentage of water whioch is base flow (30%) Submerged and emergent vegetation Annual no-flow duration (1mo) Annual spate duration (1mo) Large woody debris cover (6%) Small, medium trees Sand High macroinvertebrate richness Fauna Fauna

Climate Geology & Topography Hydrology Water Quality Habitat

Rainfall

This province contains the highest precipitation value recorded in Queensland. The values for the driest quarter mean precipitation throughout the province are patchy.

Annual mean precipitation is high.

Rainfall erosivity is on average very high.

Temperature

Cold to moderate annual mean temperatures.

Seasonality in temperature is not pronounced.

The annual mean temperature for the Wet Tropics FBP ranges from cold to moderate, with the lowest temperatures recorded from the areas of the province at higher altitude.

Water balance

Mean Annual Runoff in the province is high (7.24 mm).

 

Terrain

Generally steep relief and high stream slopes.

Most of the Wet Tropics FBP has a high relief ratio, with a mean for the province of 0.06 . Low relief ratio values are confined to small patches within the province .

 

Base flow and flood flow

Groundwater ecosystem significance – 30% of flow is base flow, 70% flood flow from rainfall.

Gauges

Modelled pre-development data from 8 gauges within the Wet Tropics FBP were used for these analyses.

Magnitude of spates

Magnitude of spates averaged 3 to 4 Ml km2 day-1, but larger and smaller average values occur within the province at particular sites.

No flow spells

Flow can generally be considered to be perennial in the province.  The longest recorded no-flow spell was over 5 months.

Rise and fall of the hydrograph

For both the mean rate and greatest rate variables, the rate of rise is approximately double the rate of fall.

Wet and dry seasons

The wet season is January to April and the dry season May to December.

Seasonal patterns are relatively consistent and predictable: wet and dry periods follow long term trends.

Turbidity

Turbidity within the Wet Tropics province is generally very low.

 

 

Bank shape and slope

Convex and concave shaped banks are the most often present and most often dominant bank shape categories. All bank slope categories are present and all are the predominant category at some sites .

Riparian vegetation and macrophytes

The riparian zone is primarily dominated by medium and small trees, woody shrubs and grasses . Trees over 30 m tall, vines, herbs and forbs, rushes and sedges, tree ferns, mosses, palms, and ferns typically form minor components of riparian cover but all are typically present.

Substrate composition and heterogeneity

The number of substrate classes recorded from sites in the Wet Tropics province is high with respect to most other provinces in Queensland. Pool and edge habitats primarily consist of sand, whilst riffles mainly have cobble subtrates.

Woody debris and snags

Large Woody Debris (LWD) and snags are conspicuous components of many rivers in the province. Bed coverage by woody debris and leaf litter tends to be quite low (5.5 and 6.5% respectively). 

Last updated: 21 February 2012

Queensland Government
WetlandInfo   —   Department of Environment and Resource Management

                 

Monitoring and Assessment
Science and Research
Wetland Conceptual Models