Thank you, Madam Chair.
First, I would like to thank Dr. John Pomeroy for being here today at the table with me.
Dr. Pomeroy is the Canada research chair in water resources and climate change. He is the inspiration behind this bill. He helped to draft this bill, and he patiently taught me about flood and drought forecasting.
Today, though, I will be concentrating on flood forecasting for simplicity, but I know that Dr. Pomeroy would be happy to take questions about drought conditions in Canada and the art of drought forecasting.
I would like you go back in your mind to when you were in high school, where you drew two-dimensional graphs consisting of the horizontal and the vertical axes, both of which are used in the flood forecasting process.
I will call the x-axis or the x-dimension the top-down process in flood forecasting. When I speak of the top-down process, I'm talking about weather forecasting now. It's top-down. It's not particularly democratic, but it's the technology that dictates that weather forecasting is a top-down process. Images come from satellites down to earth. They form the basis of weather forecasts that are fundamental to flood and drought forecasting.
Technology dictates this top-down process in weather forecasting. Weather forecasting is done by the Meteorological Service of Canada, whose main operations facility, the Canadian Meteorological Centre, is housed in a nondescript building covered with parabolic antennas situated along Autoroute 40 in Dorval, on Montreal Island. Should you ever drive by it, you will definitely see a mass of parabolic antennas on a roof, which you may readily, but incorrectly, think is a sports bar that requires all the antennas to receive signals from various sports events.
The horizontal axis represents the collaborative process that involves the provinces and territories. To forecast floods accurately, you have to do more than forecast the weather. You need data on water levels and flows in water bodies, lakes, rivers and brooks. Data collection necessarily requires the participation of the people closest to those phenomena on the ground, in other words, the people in the provinces and territories.
Water level and flow data are collected by water gauges and stations located in water bodies across the country, water bodies that are in provincial and territorial jurisdiction. As we know, water resources belong to the provinces and territories, and this is done under a collaborative and jointly financed federal-provincial program called the national hydrological service.
Climate change, as we all know, means more frequent and intense flooding and drought events. We therefore need a more accurate flood forecasting system, with greater lead times to allow communities to better prepare for floods and to better buttress against them.
Fortunately, flood forecasting methods and technologies are rapidly evolving. Technology now allows us to build more sophisticated flood forecasting models that cover larger geographic areas, to which we can attach probabilities of flood risk. Because these models cover larger areas, greater co-operation is required among jurisdictions—among provinces and between provinces and the federal government—because, as I said at the very start, the federal government is responsible for weather forecasting and has some in-house capabilities that are important to flood forecasting in terms of gauging water flows and water levels, etc. It's a collaborative process involving provincial, territorial and federal governments.
Because these models cover larger areas, greater computing power is required to run complex, dynamic models. We're talking here about supercomputers. Supercomputers are required for this kind of large-scale, complex probabilistic forecasting.
There are many benefits to this co-operation, which is, in fact, already a reality. There are many benefits when flood forecasters work together. As Dr. Pomeroy has pointed out, while some modellers in Canada may predict major floods every year, others may not be called on to predict even one flood in their entire career, so a national collaborative approach would create opportunities for shared experiences and professional development among flood forecasters in different provinces. There is already a community of forecasters who meet to discuss best practices, but we need a more formal, permanent structure to harness flood forecasting knowledge from jurisdictions across Canada and to better move forward together.
Some will say that this structure already exists within Environment and Climate Change Canada and that the department is already involved in flood forecasting. However, to quote Dr. Pomeroy, “ECCC has not established a national hydrological forecasting service. They have established a federal river flow forecasting system over part of the country that is exploratory and top down. But it does not have the participation of the provinces and territories.”
Nowhere in the Canadian Meteorological Service's published core mandate does one find a requirement to engage with provinces and territories on flood and drought forecasting. What is being developed currently is a federal system of stream-flow prediction, not a co-operative flood forecasting system that is national in scope. There is a difference.
At the moment, the Canadian Meteorological Service's stream-flow models help predict the volume of water passing through an area under different weather scenarios. This information is useful in decisions about irrigation and hydroelectricity generation. Stream-flow models are also being used to improve weather forecasts. For example, if the Canadian Meteorological Centre predicts that stream-flow will be high because the soil moisture in a basin is high, resulting in greater runoff because the land is not absorbing rain, this will be an indicator of greater expected evaporation from the soil. Evaporation, in turn, influences atmospheric dynamics. With high levels of soil moisture and evaporation, the energy and water in the atmosphere are greater. This, in turn, influences the weather and the weather forecast.
However, to forecast floods even more accurately, we need a far more refined approach and more local data.
True flood forecasting involves the added complexity of factoring in soil moisture, groundwater saturation, the state of glaciers and snowpack, the topology of the river network, river pinch points, and the state of river bank erosion. Human decisions pertaining to the regulation of dams and reservoirs must also be factored in.
In Canada, flood forecasting is further complicated by the fact that we are a northern country with mountainous regions and lots of ice. River ice jams can raise water levels many metres above the norm. These don't occur only during spring ice cover breakup; they can happen in the fall freeze-up and mid-winter breakup periods as well.
Another factor impacting flood risk that has been recently highlighted by Dr. Pomeroy is wildfires, which of course we've seen a lot of in the last couple of years. Wildfires destroy tree canopy, leading to much denser snowpack as more snow accumulates on the ground. Loss of canopy also translates into less shade and more direct sunlight hitting the snow, causing it to melt faster. The result is earlier and stronger spring runoff and a greater risk of downstream flooding.
The purpose of this bill isn't to reinvent the wheel but rather to urge the federal government to adapt and respond more effectively to the latest scientific developments and flood and drought forecasting methods at a time when floods and droughts have become more frequent and severe as a result of climate change.
If we look to Europe, we see that even independent states can achieve the unity of purpose required for accurate flood forecasting on a continental scale.
According to Dr. Pomeroy, and I'm sure he'll speak more about this, the prototype European flood forecasting—