04/07/2021

(CA The Guardian) Canadian Inferno: Northern Heat Exceeds Worst-Case Climate Models

The Guardian

Scientists fear heat domes in North America and Siberia indicate a new dimension to the global crisis indicate a new dimension to the global crisis

A wildfire burning on a mountainside in Lytton, British Columbia, on Thursday.

If you were drawing up a list of possible locations for hell on Earth before this week, the small mountain village of Lytton in Canada would probably not have entered your mind.

Few people outside British Columbia had heard of this community of 250 people. Those who had were more likely to think of it as bucolic.

Nestled by a confluence of rivers in the forested foothills of the Lillooet and Botanie mountain ranges, the municipal website boasts: “Lytton is the ideal location for nature lovers to connect with incredible natural beauty and fresh air freedom.”

Over the past seven days, however, the village has made headlines around the world for a freakishly prolonged and intense temperature spike that turned the idyll into an inferno.

The US president, Joe Biden, and Canadian prime minister, Justin Trudeau, have warned worried populations to brace for more. Shocked climate scientists are wondering how even worst-case scenarios failed to predict such furnace-like conditions so far north.

Johan Rockström, the director of the Potsdam Institute for Climate Impact Research, said the recent extreme weather anomalies were not represented in global computer models that are used to project how the world might change with more emissions.

The fear is that weather systems might be more frequently blocked as a result of human emissions.

“It is a risk – of a serious regional weather impact triggered by global warming – that we have underestimated so far,” he said.

In Lytton, it felt as if the weather itself had stagnated. Trapped in a vast heat dome that enveloped western Canada and the north-western US, temperatures had nowhere to go but up.

In Lytton, the Canadian national heat record was broken on Monday, smashed on Tuesday and then obliterated on Wednesday when the local monitoring station registered 49.6C (121F).

After the insufferable heat came choking fire. First the forest burned, then parts of the town. On Wednesday evening, the mayor, Jan Polderman, issued the evacuation order.

“It’s dire. The whole town is on fire,” he said on TV. “It took, like, a whole 15 minutes from the first sign of smoke to, all of a sudden, there being fire everywhere.”

By Thursday, satellite images showed an eruption of blazes around the village and a widening smoke cloud across the region.

Canada heatwave: resident films escape from wildfire as flames engulf Lytton village – video 

Police stations and hospitals reported a surge in heat-related deaths – 486 in British Columbia, and dozens more south of the border. Roads buckled as asphalt expanded. At least one city suffered power cuts.

The psychological, political and economic impacts are harder to quantify, but for many, along with the horror came a sense of bewilderment that these northern territories were hotter than the Middle East.

David Phillips, the Canadian government’s senior climatologist, summed it up in an interview with CTV. “I mean, it’s just not something that seems Canadian.”

A woman and her cat rest inside a tent at the Oregon Convention Center cooling station in Portland. US. Photograph: Kathryn Elsesser/AFP/Getty Images

More people in more countries are feeling that their weather belongs to another part of the world.

Across the border, in Washington state, the maximum heat measured at Olympia and Quillayute was 6C higher than the previous all-time record, according to the Weather Prediction Centre. 

In Oregon, the town of Salem hit 47C, smashing the previous record by 9C. Several areas of California and Idaho also saw new highs.

The previous week, northern Europe and Russia also sweltered in an unprecedented heat bubble. June records were broken in Moscow (34.8C), Helsinki (31.7C), Belarus (35.7C) and Estonia (34.6C).

Further east, Siberia experienced an early heatwave that helped to reduce the amount of sea ice in the Laptev Sea to a record low for the time of year.

The town of Oymyakon, Russia, widely considered to be the coldest inhabited place on Earth, was hotter (31.6C) than it has ever been in June.

This followed a staggeringly protracted hot spell in Siberia last year that lasted several months.

Carlo Buontempo, director of the Copernicus Climate Change Service, said there was a clear human fingerprint on this “very freakish” event.

Without emissions from cars, farms and industry, he said, the record temperatures in the western north Americas would be expected only once in tens of thousands of years, but the probability rises along with the levels of the greenhouse gas. 

“In the present-day climate, getting an extremely hot June is common and is likely to occur twice in three decades. However, an analysis from many computer models suggests that by the end of the century these extreme temperatures are more likely than not. Human influence is estimated to have increased the likelihood of a new record several thousand times.”

How a heat dome forms and its effect on the jet stream

                  
Rising temperatures can be seen across the world. Even in the Middle East, temperatures of 50C plus were once outliers, but parts of Pakistan, India, Australia, the US and Canada are now regularly approaching or passing that mark.

But the intensity of the heat in the north-west Americas this year and Siberia last year has taken many scientists by surprise and suggested extra factors may be involved in northern latitudes.

One theory is that the recent temperature spike might have been caused not just by global heating, but by slowing weather systems that get stuck in one place for an extended period, which gives them time to intensify and cause more damage.

This was an important factor in the devastation in Texas caused by Hurricane Harvey in 2018, which sat above Houston for several days rather than blowing inland and weakening.

Blocked high-pressure fronts were also blamed for the blistering heatwave in Europe in 2019.

Experts at the Potsdam Institute and elsewhere believe the rapid heating in the Arctic and decline of sea ice is making the jet stream wiggle in large, meandering patterns, so-called Rossby resonance waves, trapping high- and low-pressure weather systems in one location for a longer time.

This theory remains contested, but Michael Mann, director of the Earth System Science Center at Pennsylvania State University, said this week’s unexpectedly fierce heat at Lytton and elsewhere should prompt climatologists to consider additional impacts of human activity.

“We should take this event very seriously,” he wrote in an email. “You warm up the planet, you’re going to see an increased incidence of heat extremes. Climate models capture this effect very well and predict large increases in heat extremes.

"But there is something else going on with this heatwave, and indeed, with many of the very persistent weather extremes we’ve seen in recent years in the US, Europe, Asia and elsewhere, where the models aren’t quite capturing the impact of climate change.”

Regardless of which interactions are to blame, scientists are agreed that the simplest way to reduce the risk of further temperature jolts is to cut fossil fuel emissions and halt deforestation.

“It appears that this heatwave is still a rare phenomenon in the current climate, but whether it stays that way depends on our decisions,” Friederike Otto, associate director of the Environmental Change Institute at the University of Oxford, said.

“If the world does not rapidly eliminate fossil fuel use and other sources of greenhouse gas emissions like deforestation, global temperatures will continue to rise and deadly heatwaves such as these will become even more common.”

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(VICE) One Day After Setting Canada’s Heat Record, Town Burns To Ground

VICEMack Lamoureux

Officials said that most structures in Lytton, B.C., have been destroyed and multiple residents are still unaccounted for. 

A motorist watches from a pullout on the Trans-Canada Highway as a  wildfire burns on the side of a mountain in Lytton, B.C., Thursday, July 1, 2021. THE CANADIAN PRESS/Darryl Dyck

A small village in British Columbia burned to the ground one day after suffering through the hottest temperature ever recorded in Canada and several of its residents are still missing.

On Wednesday night, as a fire suddenly began boring down on the village of Lytton, which has a population of around 250 people, police went door to door and ordered the residents to evacuate their homes as soon as possible.

Michael Farnworth, B.C.’s public safety minister, said the blaze burned almost the entire town to the ground. 

"Most homes and structures in the village, as well as the ambulance station and the RCMP detachment, have been lost," Michael Farnworth said at a news conference on Thursday. "I also understand that some residents have not been accounted for and their location is currently being investigated by the RCMP."

“We got a phone call from emergency alert and I didn’t believe them,” evacuee Sharon Brown told Global News. “I looked out the door and there was fire everywhere. And my house burned down right after my daughter picked me up.”

The B.C. Coroners Service has yet to confirm if there have been any deaths, according to the Canadian Press

The number of residents unaccounted for is unknown.

The fire destroyed several cellular towers which has hampered the evacuees’ ability to contact loved ones.

The province has set up emergency reception centres and is urging residents to sign up. Because of the lack of cell service, officials do not even know if residents remain in the village. 

“Being without any cell service — that’s everybody’s lifeline. Nobody can contact each other,” an evacuee told Global News. “We’re going into Spence’s Bridge (a small B.C. community) to get some cell service and finally just get some relief, let everybody know we’re OK.”

Structures destroyed by wildfire are seen in Lytton, B.C., on Thursday, July 1, 2021. THE CANADIAN PRESS/Darryl Dyck

Several wildfires are ripping through the province at the moment, including one near Lytton, but B.C. Premier John Horgan said that the blaze was not caused by a nearby wildfire.


“We do not yet know what started the fire in Lytton,” said Horgan on Thursday. “There was little or no time to warn the community. In fact, it was the mayor himself that got the first whiff. Within minutes the city was engulfed.” 

Horgan said that he heard anecdotal information that the fire was sparked by a train going through the city but that a full investigation is underway. The Globe and Mail reported Friday that CN is actively investigating if the fire was started by one of their trains.

Shortly before the blaze, the little-known town became famous in Canada for breaking numerous heat records.

On Sunday, the town set a heat record with 46.6°C, then on Monday, it broke its own record after hitting 47.9°C. On June 29 it got even hotter, reaching 49.6°C (121.3°F), which beat out Las Vegas’ heat record of 47.2°C. It now stands as the hottest temperature ever recorded in Canada. 

The residents are now left to process the fact that not only have their homes been burned to the ground but that possible neighbours are missing.

Multiple GoFundMe campaigns have been started for the victims, several of which have raised over $100,000.

Canada Breaks Heat Record For Second Straight Day and Mountains Are Melting
In a press release about the shattered heat records, the World Meteorological Organization (WMO) said the heat experienced in Lytton is “more typical of summer temperatures in the Middle East than a province which is home to the Rocky Mountains and Glacier National Park.” 

British Columbia is not alone in experiencing severe spikes in temperature. 

“The Northwest Territories have recorded their all-time highest temperatures not just in June, but any point in the year,” Armel Castella, a meteorologist with Environment and Climate Change Canada, said in the press release. “ We are setting records that have no business in being set so early in the season.”

The WMO believes that heat records will continue to be broken as the summer carries on.

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(The Conversation) The North American Heatwave Shows We Need To Know How Climate Change Will Change Our Weather

The Conversation | 

NASA

Authors
  •  is Professor in Atmospheric Science, Monash University
  •  is Professor, School of Earth, Atmosphere and Environment, Monash University
Eight days ago, it rained over the western Pacific Ocean near Japan.

There was nothing especially remarkable about this rain event, yet it made big waves twice.

First, it disturbed the atmosphere in just the right way to set off an undulation in the jet stream - a river of very strong winds in the upper atmosphere - that atmospheric scientists call a Rossby wave (or a planetary wave).

Then the wave was guided eastwards by the jet stream towards North America.

Along the way the wave amplified, until it broke just like an ocean wave does when it approaches the shore. When the wave broke it created a region of high pressure that has remained stationary over the North American northwest for the past week.

This is where our innocuous rain event made waves again: the locked region of high pressure air set off one of the most extraordinary heatwaves we have ever seen, smashing temperature records in the Pacific Northwest of the United States and in Western Canada as far north as the Arctic.

Lytton in British Columbia hit 49.6℃ this week before suffering a devastating wildfire“.

What makes a heatwave?

While this heatwave has been extraordinary in many ways, its birth and evolution followed a well-known sequence of events that generate heatwaves.

Heatwaves occur when there is high air pressure at ground level. The high pressure is a result of air sinking through the atmosphere. As the air descends, the pressure increases, compressing the air and heating it up, just like in a bike pump.

Sinking air has a big warming effect: the temperature increases by 1 degree for every 100 metres the air is pushed downwards.

The North American heatwave has seen fires spread across the landscape. NASA

High-pressure systems are an intrinsic part of an atmospheric Rossby wave, and they travel along with the wave.

Heatwaves occur when the high-pressure systems stop moving and affect a particular region for a considerable time. When this happens, the warming of the air by sinking alone can be further intensified by the ground heating the air – which is especially powerful if the ground was already dry.

In the northwestern US and western Canada, heatwaves are compounded by the warming produced by air sinking after it crosses the Rocky Mountains.

How Rossby waves drive weather

This leaves two questions: what makes a high-pressure system, and why does it stop moving?

As we mentioned above, a high-pressure system is usually part of a specific type of wave in the atmosphere – a Rossby wave. These waves are very common, and they form when air is displaced north or south by mountains, other weather systems or large areas of rain.

Rossby waves are the main drivers of weather outside the tropics, including the changeable weather in the southern half of Australia. Occasionally, the waves grow so large that they overturn on themselves and break. The breaking of the waves is intimately involved in making them stationary.

Importantly, just as for the recent event, the seeds for the Rossby waves that trigger heatwaves are located several thousands of kilometres to the west of their location. So for northwestern America, that’s the western Pacific. Australian heatwaves are typically triggered by events in the Atlantic to the west of Africa.

Another important feature of heatwaves is that they are often accompanied by high rainfall closer to the Equator. When southeast Australia experiences heatwaves, northern Australia often experiences rain. These rain events are not just side effects, but they actively enhance and prolong heatwaves.

What will climate change mean for heatwaves?

Understanding the mechanics of what causes heatwaves is very important if we want to know how they might change as the planet gets hotter.

We know increased carbon dioxide in the atmosphere is increasing Earth’s average surface temperature. However, while this average warming is the background for heatwaves, the extremely high temperatures are produced by the movements of the atmosphere we talked about earlier.

So to know how heatwaves will change as our planet warms, we need to know how the changing climate affects the weather events that produce them. This is a much more difficult question than knowing the change in global average temperature.

How will events that seed Rossby waves change? How will the jet streams change? Will more waves get big enough to break? Will high-pressure systems stay in one place for longer? Will the associated rainfall become more intense, and how might that affect the heatwaves themselves?

Our answers to these questions are so far somewhat rudimentary. This is largely because some of the key processes involved are too detailed to be explicitly included in current large-scale climate models.

Climate models agree that global warming will change the position and strength of the jet streams. However, the models disagree about what will happen to Rossby waves.

From climate change to weather change

There is one thing we do know for sure: we need to up our game in understanding how the weather is changing as our planet warms, because weather is what has the biggest impact on humans and natural systems.

To do this, we will need to build computer models of the world’s climate that explicitly include some of the fine detail of weather. (By fine detail, we mean anything about a kilometre in size.)

This in turn will require investment in huge amounts of computing power for tools such as our national climate model, the Australian Community Climate and Earth System Simulator (ACCESS), and the computing and modelling infrastructure projects of the National Collaborative Research Infrastructure Strategy (NCRIS) that support it.

We will also need to break down the artificial boundaries between weather and climate which exist in our research, our education and our public conversation.

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