100 degrees in Siberia? 5 ways the extreme Arctic heat wave follows a disturbing pattern



This Arctic heat wave has been unusually long-lived. The darkest reds on this map of the Arctic are areas that were more than 14 degrees Fahrenheit warmer in the spring of 2020 compared to the recent 15-year average.
Joshua Stevens/NASA Earth Observatory

Mark Serreze, University of Colorado Boulder

The Arctic heat wave that sent Siberian temperatures soaring to around 100 degrees Fahrenheit on the first day of summer put an exclamation point on an astonishing transformation of the Arctic environment that’s been underway for about 30 years.

As long ago as the 1890s, scientists predicted that increasing levels of carbon dioxide in the atmosphere would lead to a warming planet, particularly in the Arctic, where the loss of reflective snow and sea ice would further warm the region. Climate models have consistently pointed to “Arctic amplification” emerging as greenhouse gas concentrations increase.

Well, Arctic amplification is now here in a big way. The Arctic is warming at roughly twice the rate of the globe as a whole. When extreme heat waves like this one strike, it stands out to everyone. Scientists are generally reluctant to say “We told you so,” but the record shows that we did.

As director of the National Snow and Ice Data Center and an Arctic climate scientist who first set foot in the far North in 1982, I’ve had a front-row seat to watch the transformation.

Arctic heat waves are happening more often – and getting stuck

Arctic heat waves now arrive on top of an already warmer planet, so they’re more frequent than they used to be.

Western Siberia recorded its hottest spring on record this year, according the EU’s Copernicus Earth Observation Program, and that unusual heat isn’t expected to end soon. The Arctic Climate Forum has forecast above-average temperatures across the majority of the Arctic through at least August.

Arctic temperatures have been rising faster than the global average. This map shows the average change in degrees Celsius from 1960 to 2019.
NASA-GISS

Why is this heat wave sticking around? No one has a full answer yet, but we can look at the weather patterns around it.

As a rule, heat waves are related to unusual jet stream patterns, and the Siberian heat wave is no different. A persistent northward swing of the jet stream has placed the area under what meteorologists call a “ridge.” When the jet stream swings northward like this, it allows warmer air into the region, raising the surface temperature.

Some scientists expect rising global temperatures to influence the jet stream. The jet stream is driven by temperature contrasts. As the Arctic warms more quickly, these contrasts shrink, and the jet stream can slow.

Is that what we’re seeing right now? We don’t yet know.

Swiss cheese sea ice and feedback loops

We do know that we’re seeing significant effects from this heat wave, particularly in the early loss of sea ice.

The ice along the shores of Siberia has the appearance of Swiss cheese right now in satellite images, with big areas of open water that would normally still be covered. The sea ice extent in the Laptev Sea, north of Russia, is the lowest recorded for this time of year since satellite observations began.

The loss of sea ice also affects the temperature, creating a feedback loop. Earth’s ice and snow cover reflect the Sun’s incoming energy, helping to keep the region cool. When that reflective cover is gone, the dark ocean and land absorb the heat, further raising the surface temperature.

Sea surface temperatures are already unusually high along parts of the Siberian Coast, and the warm ocean waters will lead to more melting.

The risks of thawing permafrost

On land, a big concern is warming permafrost – the perennially frozen ground that underlies most Arctic terrain.

When permafrost thaws under homes and bridges, infrastructure can sink, tilt and collapse. Alaskans have been contending with this for several years. Near Norilsk, Russia, thawing permafrost was blamed for an oil tank collapse in late May that spilled thousands of tons of oil into a river.

Thawing permafrost also creates a less obvious but even more damaging problem. When the ground thaws, microbes in the soil begin turning its organic matter into carbon dioxide and methane. Both are greenhouse gases that further warm the planet.

In a study published last year, researchers found that permafrost test sites around the world had warmed by nearly half a degree Fahrenheit on average over the decade from 2007 to 2016. The greatest increase was in Siberia, where some areas had warmed by 1.6 degrees. The current Siberian heat wave, especially if it continues, will regionally exacerbate that permafrost warming and thawing.

A satellite image shows the Norilsk oil spill flowing into neighboring rivers. The collapse of a giant fuel tank was blamed on thawing permafrost.
Contains modified Copernicus Sentinel data 2020, CC BY

Wildfires are back again

The extreme warmth also raises the risk of wildfires, which radically change the landscape in other ways.

Drier forests are more prone to fires, often from lightning strikes. When forests burn, the dark, exposed soil left behind can absorb more heat and hasten warming.

We’ve seen a few years now of extreme forest fires across the Arctic. This year, some scientists have speculated that some of the Siberian fires that broke out last year may have continued to burn through the winter in peat bogs and reemerged.

A satellite images shows thinning sea ice in parts of the East Siberian and Laptev Seas and wildfire smoke pouring across Russia. The town of Verkhoyansk, normally known for being one of the coldest inhabited places on Earth, reported hitting 100 degrees on June 20.
Joshua Stevens/NASA Earth Observatory

A disturbing pattern

The Siberian heat wave and its impacts will doubtless be widely studied. There will certainly be those eager to dismiss the event as just the result of an unusual persistent weather pattern.

Caution must always be exercised about reading too much into a single event – heat waves happen. But this is part of a disturbing pattern.

What is happening in the Arctic is very real and should serve as a warning to everyone who cares about the future of the planet as we know it.

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Mark Serreze, Research Professor of Geography and Director, National Snow and Ice Data Center, University of Colorado Boulder

This article is republished from The Conversation under a Creative Commons license. Read the original article.

340,000 Melburnians have little or no parkland within 5km of their home


Ali Lakhani, La Trobe University; Dennis Wollersheim, La Trobe University; Elizabeth Kendall, Griffith University, and Prosper Korah, Griffith University

Under the stage 4 restrictions enforced throughout metropolitan Melbourne, residents can exercise for one hour each day, within five kilometres of their home.

While such restrictions are necessary to reduce the spread of COVID-19, they can potentially harm people’s physical and mental well-being.

Parks are great for exercising, getting fresh air, and getting close to nature, all of which boost our physical and mental health.

Unfortunately, some Melburnians have little or no access to parkland within their permitted 5km radius, meaning they are likely to miss out on these benefits.

Space to breathe

Our map analysis looked at mesh blocks, the smallest geographical area defined by the Australian Bureau of Statistics, typically containing 30-60 homes.

For each mesh block zoned as residential, we tallied up the total area zoned as parkland within a 5-kilometre radius. The results are shown in the interactive map below, in which darker greens indicate a larger area of available parkland (very light green: 0-4.5 sq km; light green: 4.5-9.2 sq km; mid-green: 9.2-13.2 sq km; dark green: 13.2-19 sq km; very dark green: more than 19 sq km).

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Of the 42,199 residential mesh blocks currently under stage 4 restrictions, 3,496 have between 0 and 4.5 square kilometres of parkland within 5km. This equates to about 135,000 homes or 340,000 people with little or no access to parks within their permitted area for exercising.

On average, residents in Cardinia, Mornington Peninsula and Melton have the least parkland within a 5km radius, whereas those in Knox, Yarra and Banuyle have the most.

Haves and have-nots

Our findings confirm that some Melburnians are more fortunate than others in their ability to access urban green space during stage 4 lockdown.

For those less fortunate, the state government should consider replacing the blanket 5km rule with a special provision that allows people to travel outside this radius if they would otherwise be unable to access a park.




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Bespoke rules could also help others, such as residents with a disability or older Melburnians who use a mobility aid. While many members of these groups might have plentiful parks within their 5km radius, they may have problems accessing them. Issues can include uneven pavements, kerbs without ramps, or steeply sloped paths.

The state government could help these people by auditing public spaces to establish where structural barriers exist, and then work to remedy them. Alternatively, once again, the blanket 5km rule could be amended with a special provision that allows older Melburnians, or those with a disability, to travel outside their 5km radius to get to the most suitable nearby park.The Conversation

Ali Lakhani, Senior Lecturer in Public Health, La Trobe University; Dennis Wollersheim, Lecturer, Health Information Management, La Trobe University; Elizabeth Kendall, Professor, The Hopkins Centre, Menzies Health Institute Queensland, Griffith University, and Prosper Korah, PhD Researcher, Urban Studies and Planning, Griffith University

This article is republished from The Conversation under a Creative Commons license. Read the original article.