CBCNEWS — Live CBC Newsroom With Marianne Dimain 20260920 100000 UTC 281 transcript segments Original Broadcaster Captioning (Enhanced) Data courtesy of The GDELT Project (https://www.gdeltproject.org/), from the Internet Archive TV News Archive. Machine transcription. Treat it as a searchable index of what was broadcast, not a verbatim quotation record. [00:00:28] Hey, I'm Johanna Wagstaff, a meteorologist and part of the [00:00:30] CBC News team covering stories on climate change. And we are [00:00:33] starting to feel the impacts of those changes in our daily [00:00:36] lives and see them in the world around us. In this episode, [00:00:39] we'll help make sense of it all, both what's already happening [00:00:42] and what could be coming in the future. Let's start by looking [00:00:46] at the effects of rising temperatures. [00:07:31] Just days before the Winter Olympics in Italy, [00:07:32] organizers were quietly panicking because of this green [00:07:36] slopes on the Dolomites, slopes that were supposed to [00:07:39] host the best skiers and snowboarders. But then, [00:07:42] right on cue, a series of storms moved [00:07:44] through, blanketing the venues just in [00:07:46] time. So officially, that crisis is over. But about [00:07:49] two Empire State Buildings worth of snow are part of the [00:07:53] backup plan. And this is how modern Winter Olympics operate [00:07:56] now. Not will it snow, but will technology come [00:07:59] through if it doesn't? [00:08:01] Because Italy is not an outlier. In Beijing 2020, two, [00:08:04] 100% of the snow was artificial. And of course, [00:08:06] in Vancouver 2010, snow was trucked in from the [00:08:09] interior for the local mountains. At the time, [00:08:12] the lack of snow felt like bad luck, [00:08:14] but in the end it was more of a preview for winters to come, [00:08:17] thanks to climate change. So what does that mean for the [00:08:21] future of Winter Olympics? For places that have built [00:08:24] their identities around winter, the International Ski and [00:08:27] Snowboard Federation has floated the idea of rotating [00:08:30] the games [00:08:32] between a small number of quote UN quote climate stable venues. [00:08:35] New research suggests that by the 20 fifties, [00:08:38] more than 70% of past and potential Olympic sites won't [00:08:42] be climate reliable. So does Whistler qualify? Well, for now, [00:08:45] yes, but it will mean some changes. [00:08:48] Whistler Blackcomb is still seen as safer than many [00:08:51] European resorts because of its elevation and sheer scale. But [00:08:55] even here the cracks are showing. Some are skiing on the [00:08:59] Horseman Glacier was suspended indefinitely [00:09:01] in 2025, and by mid century climate [00:09:04] models suggest that Whistler base could see about half of [00:09:07] its winter precipitation fall as rain. Keeping Whistler [00:09:10] Olympics ready would mean pushing finishing lines higher [00:09:14] up the mountain and leaning heavily on snow making. And the [00:09:17] village won't exactly feel like winter Wonderland with mainly [00:09:21] rain forecast at 600 meters 25 years on, [00:09:23] because snow making only works when temperatures are at or [00:09:27] just slightly above 0 and that window is shrinking by the 20 [00:09:31] fifties. The winter is [00:09:32] they currently think of as bad are expected to become average [00:09:36] lower elevation hills will have to adapt to year round resorts. [00:09:40] The true winter experience moves higher, [00:09:43] colder and farther inland. So Whistler and a few others like [00:09:47] Calgary, Salt Lake City, UT, and Sapporo, Japan, [00:09:50] may indeed be one of the last few places where Winter [00:09:54] Olympics still depend on winter, not just engineering. [00:10:03] Recent summers have been so hot in Japan, [00:10:06] they've invented a new word to describe it. For heat that tops [00:10:10] 40°C, the new word is Coco shobi. It [00:10:12] roughly translates to cruelly hot day. It's a move that makes [00:10:45] is different. It's a sobering, modern addition to the lexicon [00:10:49] by the Japan Meteorological Agency. It reflect not just the [00:10:54] temperature, but how the heat feels in their [00:10:57] daily life, like exhausting, overwhelming or even dangerous. [00:11:01] The word was chosen by the public via a national poll of [00:11:05] nearly half a million people. The reason? It's top of mind? [00:11:09] 2025 was the hottest summer in Japan since records began in [00:11:13] 1898. In fact, more than 1/3 of all the 40° [00:11:17] days ever recorded in the last 150 years have happened in just [00:11:21] the last three years. [00:11:23] The outlook for summer 2026 is also above normal. The IPCC and [00:11:27] local meteorologists are warning that the combined [00:11:30] effects of rising temps and humidity are increasingly [00:11:33] posing a severe risk of mortality. They need people to [00:11:37] take action. I think it's especially important for [00:11:40] elderly, which would be one in three [00:11:42] people over 65 years old in Japan, [00:11:44] and they really need to take heed in terms of caring for [00:11:47] their bodies and themselves. Parts of Canada can certainly [00:11:51] relate to this. Think of the sweltering, [00:11:53] heavy days in southern Ontario. [00:11:55] In Quebec, where the humidity makes it [00:11:58] nearly impossible for the body to cool itself through sweat. [00:12:02] These are the most dangerous days of the year. In Japan, [00:12:06] that humidity is relentless and months long, [00:12:09] amplified by the heat island effect of these massive urban [00:12:13] centres. Gradually, yearly, the temperature is rising up. [00:12:17] So maybe it's better to name the extreme hot day. It's a [00:12:21] it's kind of a warning. Japan is trying to ensure its [00:12:25] citizens know exactly what they're up against. [00:12:28] By the way, the word that came in second [00:12:30] place in that poll? Chomo shobi, which means super, [00:12:33] extremely hot day. But it seems extreme just doesn't cut it [00:12:37] anymore. [00:14:52] Welcome back. Our oceans and waterways are feeling the [00:14:54] impacts of climate change. Let's look at what those [00:14:57] changes could look like and the consequences they could have. [00:15:03] Imagine sea levels were up here instead of down there. This [00:15:06] isn't theoretical, it's happening. OK, [00:15:09] so not in a couple years, but over a couple centuries. [00:15:12] Which means now is exactly what we need to start planning. How [00:15:17] we build our cities, how we adapt our coastlines, [00:15:20] zoning laws, flood maps, sea walls, [00:15:22] wetlands. This is an abstract. It's about staying ahead of the [00:15:27] water. Because even if we cap warming at 1.5°C, [00:15:30] the oceans aren't done rising. [00:15:32] Scientists just rewound the numbers, [00:15:35] drawing on ancient coral sediment, fossil shorelines, [00:15:38] and found that the last time Earth was this warm, about 125, [00:15:42] 000 years ago, sea levels were four to 10 [00:15:44] meters higher. That's because ice takes time to melt, [00:15:48] but once it starts, it's hard to stop. Greenland [00:15:51] and Antarctica that ice won't collapse overnight, [00:15:54] but once they go, they don't quit. It's like [00:15:57] tipping a jug of water. You can't freeze it mid poor. Even [00:16:01] conservative projections show a 1m [00:16:03] sea level rise in 75 years, but it keeps going from there. [00:16:07] Right now, about 230 million people live [00:16:10] on land less than 1m above sea level, [00:16:12] about 1 billion within 10 meters. That's one in eight [00:16:16] people on Earth. So no, your entire city isn't going [00:16:20] underwater tomorrow. But this is coming, [00:16:22] and we've still got time to get ready. [00:19:56] Vancouver is one of the wettest cities on earth. Yet when it [00:19:59] comes to drinking water, [00:20:03] there is a crisis on the horizon. And the proposed [00:20:06] solutions are kind of wild. Like a giant straw pipes you [00:20:10] can drive through. Maybe even a new source lake. Stick with me. [00:20:14] Let's start by understanding the existing drinking water [00:20:17] system. I'm standing in front of one of them. This is [00:20:21] Capilano Lake, one of three reservoirs on the [00:20:23] North Shore Mountains that catch the runoff from 60, [00:20:27] 000 hectares of protected land. That means no hiking, [00:20:30] no camping, no human footprints. We lock [00:20:32] down these watersheds a century [00:20:34] ago to act as pristine catchment basins for Capilano, [00:20:38] Seymour and Coquitlam reservoirs. These giant holdy [00:20:42] lakes, if you will, provide the water to 3 million [00:20:46] people. That's about half of BC's entire population. The [00:20:50] genius of this system is the altitude. [00:20:55] The mountains do the heavy lifting using gravity as the [00:20:59] primary delivery method. So massive pumping stations and [00:21:02] massive amounts of electricity are not needed, [00:21:05] just pipes guiding the flow down to your glass. It's a [00:21:08] perfect passive system for now. We're very lucky with the [00:21:12] system we have. But the system has its limitations. And when [00:21:15] the reservoirs are full and they're full and they need to [00:21:19] last us throughout the summer, which brings us to conflict [00:21:23] number one, climate change. This whole [00:21:25] system works because the snow we get in the mountains [00:21:28] in the winter slowly melts through the spring and summer, [00:21:32] keeping our reservoirs full when demand is the highest. [00:21:35] I've looked at the projections for Metro Vancouver snow. By [00:21:39] the 20 fifties, the average winter snowpack is [00:21:42] expected to decrease by almost 60%. By the twenty 80s, [00:21:45] that number is closer to 80%. We're already losing winter [00:21:49] snow as the season shifts, getting more of our snow as [00:21:52] rain, and we're seeing glimpses of [00:21:55] what that looks like when we get to the bottom of our lakes. [00:21:58] Too early, Tighter restrictions. [00:22:02] 2026 is the earliest. Metro Vancouver has introduced stage [00:22:05] 2 water restrictions on record. Basically no lawn watering [00:22:09] until the fall. And so we know we provide a billion liters in [00:22:13] winter, so 1 billion liters. It's the [00:22:16] size of BC Place. If you fill it up every day in winter, [00:22:20] but in summer that increases by 50%. [00:22:23] So how do we get more water when we need it? [00:22:26] The first wild plan is the giant straw by the mid twenty [00:22:29] 30s, Metro Vancouver is launching a [00:22:31] second water intake at Coquitlam Lake to double its [00:22:35] water withdrawal. The water is already there, [00:22:38] it's just physically out of reach of our current pipes. [00:22:41] We're tunneling a brand new lower intake to grab that cold, [00:22:45] high quality water from the depths. Think of it like [00:22:48] sticking a longer straw in your bubble tea to get the last few [00:22:52] curls at the bottom of the cup. So they currently [00:22:55] provides drinking water to about 1/3 of the region. And [00:22:59] with the upgrade, eventually it's going to be [00:23:01] able to provide more than half of the region. It's a very Big [00:23:05] Lake. It's also very deep. The deepest part is actually below [00:23:09] sea level. But even if we have all the water we need, [00:23:12] we have to move it. And we live in a major seismic zone [00:23:15] conflict #2 our water has to travel under massive bodies of [00:23:19] water like the Burrard Inlet to get to your tap. I've done a [00:23:22] deep dive into the liquification hazard maps. And [00:23:25] the big concern here is that during a large earthquake, [00:23:29] the ground, especially near the riverbanks, [00:23:31] turned to jello. So if a main pipe snaps 30 meters below the [00:23:34] water, you can't just send a scuba [00:23:36] diver down to patch it. We could be dry for weeks. [00:23:40] About 75% of our primary pipes have been upgraded to seismic [00:23:44] resilient joints designed to bend and stretch like this one [00:23:47] rather than snap if the earth cracks, [00:23:49] correct. This pipe here is 3.2 meters in diameter. So yes, [00:23:52] you could drive a small car through there. It's challenging [00:23:56] in the sense that, you know, we do have to make sure that [00:23:59] the pipes are the right size, right material. And it's going [00:24:02] to be able to withstand these large earthquakes that you know, [00:24:06] we're one day you're going to see unfortunately, right? [00:24:09] But engineering can't solve everything if our habits don't [00:24:12] change. That [00:24:13] leads us to conflict #3 rising demand. We're adding 35, [00:24:16] 000 new neighbors every year. Based on forecasted demand and [00:24:20] population growth, the region will likely need [00:24:23] additional water storage by the mid twenty 30s if relying [00:24:27] solely on the current systems capabilities. But it turns out [00:24:31] Vancouver also just straight up uses a lot of water. The [00:24:34] Vancouver region are the highest per capita water users [00:24:38] in in the country. So, you know, it's not a it's not a table we [00:24:42] want to be first on, I think. So it's definitely a [00:24:45] A2 pronged [00:24:47] approach. It's let's all use less and let's plan for the [00:24:50] second intake at Coquitlam so we can access more of the the [00:24:53] high quality water source water that we have in this region. [00:24:57] Even with the longer straw and the bendy pipes, [00:25:00] the math still doesn't quite add up for the next century. [00:25:04] Metro Vancouver is evaluating 7 mega projects to get us through [00:25:08] to 2120. We're talking about entirely new source lakes [00:25:11] outside our current map, like Harrison Lake or Pit Lake [00:25:15] lakes, by the way, that haven't already been [00:25:18] earmarked for BC Hydro use in the future. We're also talking about [00:25:22] raising the Seymour Falls Dam by 53 meters. And these are [00:25:25] engineering hurdles on unseated territories. Altering these [00:25:29] waterways requires decades of engagement with local First [00:25:32] Nations. Our 100 year survival equation is a race move. Water [00:25:36] from mountains that are losing snow across an earthquake fault [00:25:39] line to a sprawling city with a growing number of taps. The [00:25:43] Metro Vancouver has planned for 100 years before, [00:25:46] so they're betting billions that we can out engineer the clock. [00:25:56] Coming up, we're taking a look at stories [00:25:58] focused on climate change. Stay with us. [00:28:10] And we're back. So how do these changing temperatures impact [00:28:13] wildlife? Well, just like humans, animals, [00:28:15] plants, insects are forced to adapt to [00:28:17] our changing world. For some it means shrinking habitats, [00:28:21] but for others new opportunities. [00:28:27] A colony of Penguins on an Antarctic island, [00:28:29] dramatically shifting their behaviour in the face of [00:28:32] climate change. We don't know whether to be [00:28:35] a happy or or very sad yet, but for now we're alarmed. The [00:28:39] big change? The birds are breeding earlier, [00:28:42] a shift that's happening at record speed. Ignacio Martinez [00:28:46] led a decade long study on three species of Antarctic [00:28:50] Penguins. The sweeping survey relied on time lapse cameras [00:28:54] monitoring 37 colonies of Penguins in a region warming [00:28:58] three times faster than the rest of the world. All three, [00:29:02] Gentoo, Chinstrap and Adelie, moved up their breeding seasons. [00:29:06] Gentoos had the biggest change 13 days earlier on average, [00:29:10] and up to 24 days for some colonies. When we looked at the [00:29:14] time series of 10 years one after the other, [00:29:17] we realized like oh damn, this is the fastest change in [00:29:21] any vertebrate ever. [00:29:23] Shifting breeding patterns could help some species adapt [00:29:26] to climate change and has been seen in other plants and [00:29:30] animals, but it's not good news for all. [00:29:33] And that could pit Penguin species against each other over [00:29:36] scarce food and land. Like we only have one species. The [00:29:40] chances that species survives is very scarce. [00:29:44] Martinez says the findings suggest there could be winners [00:29:48] and losers of climate change, but overall it paints A [00:29:51] concerning picture for the future of Antarctic Penguins. [00:29:55] In Ayat Singh, CBC News, Toronto. [00:29:59] Scientists have confirmed something that shouldn't have [00:30:01] happened. The first sighting of a mosquito in Iceland. The news [00:30:05] sent a buzz around the world. It was a surprise because it [00:30:08] was the only country in the world that was mosquito free. [00:30:11] But the story isn't really about Iceland, [00:30:14] it's about what it means for Canada. Canadian scientists are [00:30:17] already modeling what our mosquito future might look like [00:30:20] as the climate warms. There are roughly 80 different mosquito [00:30:24] species in Canada. Some have been here for centuries and [00:30:27] others are newcomers chasing the heat. [00:30:29] But Canada's north is warming four times faster than the rest [00:30:33] of the world, meaning some parts of the [00:30:36] country are entering into the perfect breeding temperature [00:30:39] range for mosquitoes. And many of the newcomers carry disease. [00:30:43] It is Kulick PNS, which is the vector for West [00:30:46] Nile virus, so it has spread geographically [00:30:49] from the east of Canada all the way out to the West, [00:30:52] most recently seeing it in Edmonton and in Calgary in 2022. [00:30:56] These are, this is a species of mosquito [00:30:59] that we have never seen previously in these parts of Canada. A species once limited by cold is