Stormwater Thermal Mitigation

Overview

Streams draining urban areas are often much warmer than those draining natural ones due to changes in surface cover and hydrology. Urbanization increases stream temperatures by decreasing riparian shading and replacing natural landscapes with hard, dark-coloured pavements and roofs that absorb and store heat from the sun. The added impervious cover increases the volume of heated runoff while at the same time reducing discharge of cool groundwater to streams. This heating effect is further exacerbated as runoff flows through stormwater management ponds or other impoundments, where detained water is exposed to solar warming for extended time periods between rain events. This page explores different techniques for mitigating the effects of urbanization on the stream thermal regime.

Thermal Load

Since stream warming is influenced by the runoff temperature and volume of runoff draining to streams, impacts are best assessed through an evaluation of thermal loads both in the stream and in runoff discharged to streams. The thermal load is a function of the flow rate, water temperature, water density and heat capacity of water (or the energy required to increase a kg of water by 1 degree C).

Thermal Load = Q x ρ x T x C

Where:

• Q = flow rate (m³/s)
• ρ = water density (1000kg/m³)
• T = water temperature (°C)
• C = heat capacity of water (4187J/kg°C)

Since urban runoff volumes often increase by 2 to 5 times after development, and stormwater pond effluent temperatures are between 4 and 11°C warmer than pond influent temperatures in the summer, the overall thermal load increases to streams can be very significant (Van Seters et al. 2019).

Temperature Target Selection

Setting a stream temperature threshold for the protection of aquatic life can be based on:

1. Matching the water temperature regime of either a known pre-development thermal condition or the thermal condition of an undisturbed stream with similar characteristics; and,
2. Meeting the upper tolerance of one or more target aquatic species.

Thermal Mitigation Techniques

Techniques for mitigating thermal impacts to streams can be implemented:

1. Within the catchment near the source of runoff,
2. Along the conveyance route to a treatment facility
3. Within the stormwater pond or other stormwater treatment facility; and/or,
4. Within the stream itself.

Upstream of the Pond

Any measure that decreases runoff volumes or temperatures or both can help mitigate thermal loads to streams or downstream treatment facilities. Examples include bioretention, infiltration trenches or chambers, enhanced swales, permeable pavements, absorbent landscaping and increased canopy cover. The temperature (event mean temperature) and thermal load benefits of the practices are shown in figures 1 to 3 below. The most effective practices were deeper systems such as trenches, some deep bioretention facilities, and practices that promote significant runoff volume reductions. Beyond reducing temperatures and runoff volumes, enhancing infiltration also helps re-establish the natural baseflow regime that existed prior to development.

Influent and effluent event mean temperatures (EMT) for common LID practices. Source: (Van Seters, et al. 2019).

Event mean temperature (EMT) reduction for common LID practices. Source: (Van Seters, et al. 2019).

Thermal load reductions for common LID practices. Source: (Van Seters, et al. 2019).

Within the Pond Block

There are several opportunities to mitigate thermal impacts both within the pond itself and/or implemented within the upstream drainage area (and the lands surrounding) of the pond. Options shown in past studies to provide appreciable thermal mitigation benefits include (Van Seters and Dougherty, 2019)

Subsurface Draw Outlets

A reverse sloped outlet pipe drains cooler water from below the pond surface to a control manhole that is accessible from the bank for ease of maintenance. Deeper outlets result in cooler outflows than shallow outlets because pond water temperatures decrease with depth. The figure below shows an example of thermal stratification during the summer in a deep pond using said subsurface outlets.

Schematic of a reverse sloped subsurface draw outlet to help ensure cooler outflows occur from stormwater ponds (MOE, 2003).

The changing of land cover and land uses from rural to urban; the growth of urban settlements.

A hard surface area (e.g., road, parking area or rooftop) that prevents or retards the infiltration of water into the soil.

The portion of water precipitated onto a catchment area, which then flows as surface discharge from the catchment area past a specified point.

Water from rain, snow melt, or irrigation that flows over the land surface.

The changing of land cover and land uses from rural to urban; the growth of urban settlements.

A body of water smaller than a lake, often artificially formed.

refers to the characteristics and functions of a system prior to urban development.

The land draining to a single reference point (usually a structural BMP); similar to a subwatershed, but on a smaller scale.

A body of water smaller than a lake, often artificially formed.

A shallow excavated surface depression containing prepared filter media, mulch, and planted with selected vegetation.

Low Impact Development. A stormwater management strategy that seeks to mitigate the impacts of increased urban runoff and stormwater pollution by managing it as close to its source as possible. It comprises a set of site design approaches and small scale stormwater management practices that promote the use of natural systems for infiltration and evapotranspiration, and rainwater harvesting.

The total surface area upstream of a point on a stream that drains toward that point. Not to be confused with watershed. The drainage area may include one or more watersheds.

Refers to the conditions in which an organism lives and survives or the conditions in which an organism resides. These conditions can be described as aspects of a “physical”, “social” or an “economic” environment, depending on the perspective perceived by the observer.