The disagreement between two climate scientists that will decide our future

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Robert Chris, The Open University and Hugh Hunt, University of Cambridge

Getting to net zero emissions by mid-century is conventionally understood as humanity’s best hope for keeping Earth’s surface temperature (already 1.2°C above its pre-industrial level) from increasing well beyond 1.5°C – potentially reaching a point at which it could cause widespread societal breakdown.

At least one prominent climate scientist, however, disagrees.

James Hansen of Columbia University in the US published a paper with colleagues in November which claims temperatures are set to rise further and faster than the predictions of the Intergovernmental Panel on Climate Change (IPCC). In his view, the 1.5°C target is dead.

He also claims net zero is no longer sufficient to prevent warming of more than 2°C. To regain some control over Earth’s rising temperature, Hansen supports accelerating the retirement of fossil fuels, greater cooperation between major polluters that accommodates the needs of the developing world and, controversially, intervening in Earth’s “radiation balance” (the difference between incoming and outgoing light and heat) to cool the planet’s surface.


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There would probably be wide support for the first two prescriptions. But Hansen’s support for what amounts to the deliberate reduction of sunlight reaching Earth’s surface has brought into the open an idea that makes many uncomfortable.

Michael Mann from the University of Pennsylvania in the US and another titan of climate science, spoke for many when he dismissed solar radiation management as “potentially very dangerous” and a “desperate action” motivated by the “fallacy … that large-scale warming will be substantially greater than current-generation models project”.

Their positions are irreconcilable. So who is right – Hansen or Mann?

Earth’s radiation balance

First, an explanation.

There are only two ways to reduce global warming. One is to increase the amount of heat radiated from Earth’s surface that escapes to space. The other is to increase the amount of sunlight reflected back to space before it lands on something – whether a particle in the atmosphere or something on Earth’s surface – and is converted to heat.

There are many ways to do both. Anything that reduces the amount of greenhouse gas in the atmosphere will let more heat escape to space (replacing fossil fuels with renewables, eating less meat and tilling the soil less for example). Anything that makes the planet brighter will reflect more sunlight to space (such as refreezing the Arctic, making clouds whiter or putting more reflective particles in the atmosphere).

But the key difference between the two, in terms of their impact on global warming, is their response time. That is, the time it takes for a change in the factors that allow more heat to escape or sunlight to be reflected to appear as a change in Earth’s surface temperature.

Intervening to speed up the loss of heat from Earth’s surface cools the planet slowly, over decades and longer. Intervening to increase the sunlight Earth reflects back to space cools the planet more or less immediately.

The essence of the dispute between Mann and Hansen is whether reducing greenhouse gases, by a combination of reducing new emissions and permanently removing past emissions from the atmosphere, is now enough on its own to prevent warming from reaching levels that threaten economic and social stability.

Mann says it is. Hansen says that, while doing these things remains essential, it is no longer sufficient and we must also make Earth more reflective.

When will warming end?

Mann aligns with IPCC orthodoxy when he says that emissions reaching net zero will result, within a decade or two, in Earth’s surface temperature stabilising at the level it has then reached.

In effect, there is no significant warming in the pipeline from past emissions. All future warming will be due to future emissions. This is the basis for the global policy imperative to get to net zero.

In his new paper, Hansen argues that if the atmospheric concentration of greenhouse gases remains close to its current level, the surface temperature will stabilise after several hundred years between 8°C and 10°C above the pre-industrial level.

Of this, at least 2°C will emerge by mid-century, and probably a further 3°C a century from now. A temperature increase of this magnitude would be catastrophic for life on Earth. Hansen adds that to avoid such an outcome, brightening Earth is now necessary to halt the warming in the pipeline from past emissions.

Crevices in an ice sheet.
Bright surfaces, like ice sheets, reflect light to space.
Tobetv/Shutterstock

But at the same time, we must also largely eliminate emissions if we are to stop recreating this problem in the future.

Still getting hotter…

We are scientists who study the feasibility and effectiveness of alternative responses to climate change, addressing both the engineering and political realities of enabling change at the scale and speed necessary.

We find Mann’s rebuttal of Hansen’s claims unconvincing. Crucially, Mann does not engage directly with Hansen’s analysis of new data covering the last 65 million years.

Hansen explains how the models used by IPCC scientists to assess future climate scenarios have significantly underestimated the warming effect of increased greenhouse gas emissions, the cooling effect of aerosols and how long the climate takes to respond to these changes.

Besides greenhouse gases, humanity also emits aerosols. These are tiny particles comprising a wide range of chemicals. Some, such as the sulphur dioxide emitted when coal and oil are burned, offset the warming from greenhouse gases by reflecting sunlight back to space.

Others, such as soot, have the opposite effect and add to warming. The cooling aerosols dominate by a large margin.

Hansen projects that in coming months, lower levels of aerosol pollution from shipping will cause warming of as much as 0.5°C more than IPCC models have predicted. This will take global warming close to 2°C as early as next year, although it is likely then to fall slightly as the present El Niño wanes.

Underpinning Hansen’s argument is his conviction that the climate is more sensitive to greenhouse gases than previously reported. The IPCC estimates that doubling atmospheric CO₂ raises Earth’s temperature by 3°C. Hansen calculates it to be 4.8°C.

This, and the much longer climate response time that Hansen calculates from the historical record, would have a significant impact on climate model projections.

Time for reflection

The differences between Mann and Hansen are significant for the global response to climate change.

Mann says that allowing emissions to reach net zero by mid-century is sufficient, while Hansen maintains that on its own it would be disastrous and that steps must now be taken in addition to brighten the planet.

Brightening Earth could also reverse the reductions in reflectivity already caused by climate change. Data indicates that from 1998 to 2017, Earth dimmed by about 0.5 watts per square metre, largely due to the loss of ice.

Given what’s at stake, we hope Mann and Hansen resolve these differences quickly to help the public and policymakers understand what it will take to minimise the likelihood of imminent massive and widespread ecosystem destruction and its disastrous effects on humanity.

While 1.5°C may be dead, there may still be time to prevent cascading system failures. But not if we continue to squabble over the nature and extent of the risks.


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Robert Chris, Honorary Associate, Geography, The Open University and Hugh Hunt, Professor of Engineering Dynamics and Vibration, University of Cambridge

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

Roger Hallam was involved in starting the climate activism groups Extinction Rebellion and Just Stop Oil. He is still involved with Just Stop Oil and often gets arrested and imprisoned. [22/3 Apologies had a typo calling Roger Roget]

https://rogerhallam.com/starmers-treason/

I used to be a social science researcher at King’s College, London. The name of the game in that trade is to look at everything in context. So I will provide some context. There is overwhelming evidence that the climate science industry is structurally underestimating the realities we face. “Worst than expected” is the standard phrase of just about every article as new stats are published. A few years ago we were going to pass 1.5C around 2050 – now it is already happening. I remember reading reports that the Arctic will melt in the summer around 2100. Papers now predict 2035, if not before. AMOC – the ocean current that stops the 60 million people on these islands from starving to death – was going to collapse at some point next century. Now a recent paper tells us the odds are it will collapse by 2050. If you have not been paying attention, this will create a collapse of temperatures overnight of 3-8C across Europe. So don’t be surprised if it happens before your pension comes due. 

I’m like you. I don’t like to believe things are true if they conflict with my baseline beliefs – like “we will muddle through”. But then it becomes more difficult when it actually comes true. Scientists have been telling us privately and then publicly for years that staying under 1.5C was bollocks – and now here we are. For two decades or more the best kept secret of the climate space has been that aerosols (pollution from burning fossil fuel emissions) have been holding down temperatures by .5C-1C. As we passed 1.8C last September the pretence started to collapse as scientists raged about each other on a dark corner of Twitter. It’s the start of the exposure of the world’s biggest cover up. That they knew we were fucked a decade or more ago. Not that the media is interested. Everyone is still in on the pretence, it seems.

Roger Hallam https://rogerhallam.com/starmers-treason/ An interesting article. [22/3 Apologies had a typo calling Roger Roget]

Continue ReadingThe disagreement between two climate scientists that will decide our future

A heatwave in Antarctica totally blew the minds of scientists. They set out to decipher it – and here are the results

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DM Bergstrom, Author provided

Dana M Bergstrom, University of Wollongong

Climate scientists don’t like surprises. It means our deep understanding of how the climate works isn’t quite as complete as we need. But unfortunately, as climate change worsens, surprises and unprecedented events keep happening.

In March 2022, Antarctica experienced an extraordinary heatwave. Large swathes of East Antarctica experienced temperatures up to 40°C (72°F) above normal, shattering temperature records. It was the most intense heatwave ever recorded anywhere in the world.

So shocking and rare was the event, it blew the minds of the Antarctic climate science community. A major global research project was launched to unravel the reasons behind it and the damage it caused. A team of 54 researchers, including me, delved into the intricacies of the phenomenon. The team was led by Swiss climatologist Jonathan Wille, and involved experts from 14 countries. The collaboration resulted in two groundbreaking papers published today.

The results are alarming. But they provide scientists a deeper understanding of the links between the tropics and Antarctica – and give the global community a chance to prepare for what a warmer world may bring.

Head-hurting complexity

The papers tell a complex story that began half a world away from Antarctica. Under La Niña conditions, tropical heat near Indonesia poured into the skies above the Indian Ocean. At the same time, repeated weather troughs pulsing eastwards were generating from southern Africa. These factors combined into a late, Indian Ocean tropical cyclone season.

Between late February and late March 2022, 12 tropical storms had brewed. Five storms revved up to become tropical cyclones, and heat and moisture from some of these cyclones mashed together. A meandering jet stream picked up this air and swiftly transported it vast distances across the planet to Antarctica.

Below Australia, this jet stream also contributed to blocking the eastward passage of a high pressure system. When the tropical air collided with this so-called “blocking high”, it caused the most intense atmospheric river ever observed over East Antarctica. This propelled the tropical heat and moisture southward into the heart of the Antarctic continent.

Luck was on Antarctica’s side

The event caused the vulnerable Conger Ice Shelf to finally collapse. But the impacts were otherwise not as bad as they could have been. That’s because the heatwave struck in March, the month when Antarctica transitions to its dark, extremely cold winter. If a future heatwave arrives in summer – which is more likely under climate change – the results could be catastrophic.

Despite the heatwave, most inland temperatures stayed below zero. The spike included a new all-time temperature high of -9.4°C (15.1°F) on March 18 near Antarctica’s Concordia Research Station. To understand the immensity of this, consider that the previous March maximum temperature at this location was -27.6°C (-17.68°F). At the heatwave’s peak, 3.3 million square kilometres in East Antarctica – an area about the size of India – was affected by the heatwave.

The impacts included widespread rain and surface melt along coastal areas. But inland, the tropical moisture fell as snow – lots and lots of snow. Interestingly, the weight of the snow offset ice loss in Antarctica for the year. This delivered a temporary reprieve from Antarctica’s contribution to global sea-level rise.

An ice shelf before (left) and after (right) a collapse.
These images, acquired by the Copernicus Sentinel-2 satellites on January 30 2022 (left) and March 21 2022 (right), show the Conger ice shelf before and after the collapse, which was triggered by a shocking heatwave.
European Union, Copernicus Sentinel-2 satellite imagery, CC BY

Learning from the results

So what are the lessons here? Let’s begin with the nice bit. The study was made possible by international collaboration across Antarctica’s scientific community, including the open sharing of datasets. This collaboration is a touchstone of the Antarctic Treaty. It serves as a testament to the significance of peaceful international cooperation and should be celebrated.

Less heartwarmingly, the extraordinary heatwave shows how compounding weather events in the tropics can affect the vast Antarctic ice sheet. The heatwave further reduced the extent of sea ice, which was already at record lows. This loss of sea ice was exacerbated this year resulting in the lowest summer and winter sea ice ever recorded. It shows how disturbances in one year can compound in later years.

The event also demonstrated how tropical heat can trigger the collapse of unstable ice shelves. Floating ice shelves don’t contribute to global sea-level rise, but they acts as dams to the ice sheets behind them, which do contribute.

This research calculated that such temperature anomalies occur in Antarctica about once a century, but concluded that under climate change, they will occur more frequently.

The findings enable the global community to improve its planning for various scenarios. For example, if a heatwave of similar magnitude hit in summer, how much ice melt would there be? If an atmospheric river hit the Doomsday glacier in the West Antarctic, what rate of sea level rise would that trigger? And how can governments across the world prepare coastal communities for sea level rise greater than currently calculated?

This research contributes another piece to the complex jigsaw puzzle of climate change. And reminds us all, that delays to action on climate change will raise the price we pay.

This article has been amended to correct an error in converting a 40°C temperature difference from Celsius to Fahrenheit.The Conversation

Dana M Bergstrom, Honorary Senior Fellow, University of Wollongong

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

Continue ReadingA heatwave in Antarctica totally blew the minds of scientists. They set out to decipher it – and here are the results

On a climate rollercoaster: how Australia’s environment fared in the world’s hottest year

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An endangered yellow-footed rock wallaby. Joshua Bergmark

Albert Van Dijk, Australian National University; Shoshana Rapley, Australian National University, and Tayla Lawrie, The University of Queensland

Global climate records were shattered in 2023, from air and sea temperatures to sea-level rise and sea-ice extent. Scores of countries recorded their hottest year and numerous weather disasters occurred as climate change reared its head.

How did Australia’s environment fare against this onslaught? In short, 2023 was a year of opposites.

For the past nine years, we have trawled through huge volumes of data collected by satellites, measurement stations and surveys by individuals and agencies. We include data on global change, oceans, people, weather, water, soils, vegetation, fire and biodiversity.

Each year, we analyse those data, summarising them in an that includes an overall Environmental Condition Score and regional scorecards. These scores provide a relative measure of conditions for agriculture and ecosystems. Scores declined across the country, except in the Northern Territory, but were still relatively good.

However, the updated Threatened Species Index shows the abundance of listed bird, mammal and plant species has continued to decline at a rate of about 3% a year since the turn of the century.

Environmental condition indicators for 2023, showing the changes from 2000–2022 average values. Such differences can be part of a long-term trend or within normal variability.
Australia’s Environment 2023 Report.

Riding a climate rollercoaster in 2023

Worldwide, 77 countries broke temperature records. Australia was not one of them. Our annual average temperature was 0.53°C below the horror year 2019. Temperatures in the seas around us were below the records of 2022.

Even so, 2023 was among Australia’s eight warmest years in both cases. All eight came after 2005.

However, those numbers are averaged over the year. Dig a bit deeper and it becomes clear 2023 was a climate rollercoaster.

The year started as wet as the previous year ended, but dry and unseasonably warm weather set in from May to October. Soils and wetlands across much of the country started drying rapidly. In the eastern states, the fire season started as early as August.

Nonetheless, there was generally still enough water to support good vegetation growth throughout the unusually warm and sunny winter months.

Fears of a severe fire season were not realised as El Niño’s influence waned in November and rainfall returned, in part due to the warm oceans. Combined with relatively high temperatures, it made for a hot and humid summer. A tropical cyclone and several severe storms caused flooding in Queensland and Victoria in December.

As always, there were regional differences. Northern Australia experienced the best rainfall and growth conditions in several years. This contributed to more grass fires than average during the dry season. On the other hand, the rain did not return to Western Australia and Tasmania, which ended the year dry.

So how did scores change?

Every year we calculate an Environmental Condition Score that combines weather, water and vegetation data.

The national score was 7.5 (out of 10). That was 1.2 points lower than for 2022, but still the second-highest score since 2011.

Scores declined across the country except for the Northern Territory, which chalked up a score of 8.8 thanks to a strong monsoon season. With signs of drought developing in parts of Western Australia, it had the lowest score of 5.5.

The Environmental Condition Score reflects environmental conditions, but does not measure the long-term health of natural ecosystems and biodiversity.

Firstly, it relates only to the land and not our oceans. Marine heatwaves damaged ecosystems along the eastern coast. Surveys in the first half of 2023 suggested the recovery of the Great Barrier Reef plateaued.

However, a cyclone and rising ocean temperatures occurred later in the year. In early 2024, another mass coral bleaching event developed.

Secondly, the score does not capture important processes affecting our many threatened species. Among the greatest dangers are invasive pests and diseases, habitat destruction and damage from severe weather events such as heatwaves and megafires.

Threatened species’ declines continued

The Threatened Species Index captures data from long-term threatened species monitoring. The index is updated annually with a three-year lag, largely due to delays in data processing and sharing. This means the 2023 index includes data up to 2020.

The index showed an unrelenting decline of about 3% in the abundance of Australia’s threatened bird, mammal and plant species each year. This amounts to an overall decline of 61% from 2000 to 2020.

Line graph of Threatened Species Index
Threatened Species Index showing the abundance of different categories of species listed under the EPBC Act relative to 2000.
Australia’s Environment 2023 Report

The index for birds in 2023 revealed declines were most severe for terrestrial birds (62%), followed by migratory shorebirds (47%) and marine birds (24%).

A record 130 species were added to Australia’s threatened species lists in 2023. That’s many more than the annual average of 29 species over previous years. The 2019–2020 Black Summer bushfires had direct impacts on half the newly listed species.

Population boom adds to pressures

Australia’s population passed 27 million in 2023, a stunning increase of 8 million, or 41%, since 2000. Those extra people all needed living space, food, electricity and transport.

Australia’s greenhouse gas emissions have risen by 18% since 2000. Despite small declines in the previous four years, emissions increased again in 2023, mostly due to air travel rebounding after COVID-19.

Our emissions per person are the tenth-highest in the world and more than three times those of the average global citizen. The main reasons are our coal-fired power stations, inefficient road vehicles and large cattle herd.

Nonetheless, there are reasons to be optimistic. Many other countries have dramatically reduced emissions without compromising economic growth or quality of life. All we have to do is to finally follow their lead.

Our governments have an obvious role to play, but we can do a lot as individuals. We can even save money, by switching to renewable energy and electric vehicles and by eating less beef.

Changing our behaviour will not stop climate change in its tracks, but will slow it down over the next decades and ultimately reverse it. We cannot reverse or even stop all damage to our environment, but we can certainly do much better.The Conversation

Albert Van Dijk, Professor, Water and Landscape Dynamics, Fenner School of Environment & Society, Australian National University; Shoshana Rapley, Research Assistant, Fenner School of Environment & Society, Australian National University, and Tayla Lawrie, Project Manager, Threatened Species Index, The University of Queensland

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

Continue ReadingOn a climate rollercoaster: how Australia’s environment fared in the world’s hottest year

Tennis anyone? Bad news for skiers as snow season could shrink by 78% this century

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Adrian McCallum, University of the Sunshine Coast

As the days shorten, many of us, particularly in Australia’s south-east, are looking forward to cooler times, and perhaps the allure of snow on the horizon. In the past week many in this region experienced their warmest days for over a century. What does this bode for times to come?

Research released overnight suggests ski areas in Australia and Aotearoa New Zealand will soon have much less snow due to climate change. German researcher Veronika Mitterwallner and her colleagues show average annual snow-cover days may decline by 78% in the Australian Alps and 51% in the Southern Alps of Aotearoa New Zealand (under a high-emissions scenario) by 2071–2100. Worldwide, they found 13% of ski areas will lose all natural snow cover by the end of the century.

It’s often said Australia gets more snow than Switzerland, though the evidence says otherwise. The fact remains that the Australian Alps cover a large area, more than 12,000km, with a third or more covered in snow at peak times. So these changes will have a broad impact on local economies and threaten fragile alpine ecosystems.

a panoramic view of the Australian Alps covered in snow
If Australia loses three-quarters of its snow-cover days, a surprisingly big area will be affected.
Greg Brave/Shutterstock

How did the study make these findings?

Mitterwallner’s team used a high-resolution climate data set for the global land surface area to identify the annual number of natural snow-cover days. Then, they projected those data under three emissions scenarios, and looked at historical (1950-2010), present (2011-2040), immediate future (2041-2070) and near future (2071-2100) data to examine changes over time.

Under most modelled emission scenarios, they found the annual number of snow-cover days will greatly decrease worldwide. For Australia and Aotearoa New Zealand, in particular, they found the average number will decrease by 78% and 51% respectively. These were the two regions with the greatest losses of snow.

However, under a low-emissions scenario, the good news is no regions will fall below an average of 100 snow-cover days a year. This is historically the minimum number of days a ski resort needs in seven out of ten winters to remain viable (cover must be at least 30–50cm).

How will we adapt to the loss of snow?

Will the way we use our alpine areas have to change permanently? Many resorts have already pivoted to activities such as mountain biking that don’t rely on snow. Skiing may be off the agenda – tennis anyone?

The prognosis of such research has driven the formation of groups such as Protect Our Winters. The mission of the Australian section is to help Australia’s outdoor community protect the integrity of our unique alpine environment and lifestyle from climate change.

Beyond Australia, New York recently had its highest snowfall in two years. Across the United States in general, though, they just experienced the warmest winter ever.

What is going on? And what might this new research mean, particularly for Australia and Aotearoa New Zealand?

These predictions, for almost all emissions scenarios, do not bode well for the skiers among us. More importantly, as many communities in the Himalaya are finding out, snow is not just a recreational “nice to have”. It’s a life-source for alpine communities, both human and non-human, and all those that depend on rivers sustained by snow melt around the globe.

Perhaps a greater concern in our region is the potential for ecological damage as resorts seek to increase ski slope metreage in areas that remain snow-covered. Expanding resort footprints is not a sustainable approach to a problem that probably won’t be going away.

A snow machine shoots out a plume of snow in the Snowy Mountains
Resorts can make artificial snow, but that doesn’t solve the problem of it melting if the alps get warmer.
Edward Atkin/Shutterstock

Is artificial snow an option?

So how might we support the goals of Protect Our Winters? What alternatives do we have? How about artificial snow, would that work?

As part of my PhD studies many years ago, at the University of Cambridge’s Scott Polar Research Institute, I made masses of “polar snow” in a cold room (while effectively destroying the air-conditioning units at the same time). Artificial snow can be created quite readily, assuming enough water is at hand.

Artificial snow will have a different form and its density and microstructure will differ, potentially affecting longevity. (You can read more about snow mechanics here.)

But once on the ground, artificial snow, like natural snow, is subject to the vagaries of our weather. If the sun is shining and the day is hot, snow won’t last long, regardless of whether it’s natural or artificial.

There’s a lot to think on here as we contemplate what our world and our region might look like when skiing and snow-covered ground become no more than a memory in some areas. Yes, our recreational activities might change as we wonder whether it’s worth waxing up the skis this year – or is it time to break out the racquets? The ongoing survival of many communities might be jeopardised as a result.The Conversation

Adrian McCallum, Discipline Lead – Engineering, University of the Sunshine Coast

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

Continue ReadingTennis anyone? Bad news for skiers as snow season could shrink by 78% this century

Just Stop Oil confronts Emily Thornberry && Keir Starmer and UK ‘Likud’ Labour party accused of aiding and abetting genocide

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Just Stop Oil supporters have disrupted a public event featuring Emily Thornberry. As Thornberry was delivering her open remarks, the pair stood up to confront the Labour front-bencher and Shadow Attorney General for England and Wales. They threw orange confetti and addressed the assembly, remarking “We need you to make a commitment to revoke the Tory licences for oil and gas infrastructure which will lock us on to the worst pathways of global warming and climate catastrophe”, and “Labour needs to wake up and smell the coffee. Everyone else has clocked that new oil and gas means more floods, more fires, rising food prices… when are you going to get it?”. Members of the audience were repeatedly heard to say “hear, hear!” to these comments.

After the action takers were escorted from the room, Emily Thornberry addressed the audience, saying:

“I have had Just Stop Oil outside my house, I have had Gaza protests pretty much everywhere I go. I assumed it was Gaza then I saw the orange and thought ‘Oh, right! It’s Just Stop Oil’. The worst thing is that one becomes hardened to it… I’m happy to argue the issues, I’m not happy to be told I’m responsible for the murder of babies in Gaza, or I’m personally responsible for the boiling of the planet.”

One of those taking action today was Genevieve Shanahan, 33, a university lecturer in Management and Sustainability. She said:

“Today I’m approaching Emily Thornberry to implore her to stand up to fossil fuel extremists and use her influence within Labour to secure a commitment to cancel these licences. The Labour Party are poised to win the next general election, and rather than grabbing this opportunity to protect the British public from this violence they are instead – unbelievably – dropping their existing climate commitments.”

“As a lecturer in sustainability, I need to practise what I teach. In my classroom we examine how permitting investment in new fossil fuel infrastructure would lock in economic incentives that will, according to all reasonable models, make climate collapse inevitable. If the Tories’ new oil and gas licences go ahead then that’s it – it’s game over for all of us.”

Keir Starmer accused of aiding and abetting genocide

Zionist Keir Starmer supports Israel's Gaza genocide.
Zionist Keir Starmer supports Israel’s Gaza genocide.

Let’s look at Emily Thornberry’s response. She is shadow Attorney General for England and Wales and so should know the law.

From my quick and limited review of the law of genocide, there are 2 main crimes supporting genocide: aiding and abetting genocide and complicity in genocide although unfortunately there is not a clear distinction due to how the law has developed. Aiding and abetting is more serious since there is a greater involvement in the act of genocide. So it is plausible that Keir “I support Zionism without qualification” Starmer is aiding and abetting genocide when he says that Israel has the right to withold power and water: he is clearly helping and supporting Israel’s genocide in Gaza.

Where does this leave Emily Thornberry and other Labour shadow cabinet members and MPs? Thornberry said “… I’m not happy to be told I’m responsible for the murder of babies in Gaza …”. She’s supporting her glorious Zionist leader and certainly not diverging from his Zionist policy of aiding and abetting genocide. The cabinet has collective responsibility i.e. they’re all guilty, and the shadow cabinet should be held to the same standard. MPs? Do they depart from Starmer’s Zionist aiding and abetting?

Genocide is a most serious crime and it’s clear that Israel is committing war crimes and genocide. Responsible for the murder of babies in Gaza? I’d say complicit because there is no opposition to it and the electorate are very likely to regard it as such. There’s the further issue of course that these politician cnuts are supposed to represent their electorate who want an end to Israel massacring children and other Gazans.

I’m not happy to be toldI’m personally responsible for the boiling of the planet.” Thornberry doesn’t want to be held to account for any of her actions or inactions. It’s certainly aiding and abetting again. Doing nothing to oppose it? Then complicity.

Continue ReadingJust Stop Oil confronts Emily Thornberry && Keir Starmer and UK ‘Likud’ Labour party accused of aiding and abetting genocide