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Source: The Conversation – USA (2) – By Rick Thoman, Alaska Climate Specialist, University of Alaska Fairbanks

Remnants of a powerful typhoon swept into Western Alaska’s Yukon-Kuskokwim Delta on Oct. 12, 2025, producing a storm surge that flooded villages as far as 60 miles up the river. The water pushed homes off their foundations and set some afloat with people inside, officials said. More than 50 people had to be rescued in Kipnuk and Kwigillingok, hundreds were displaced in the region, and at least one person died.

Typhoon Halong was an unusual storm, likely fueled by the Pacific’s near-record warm surface temperatures this fall. Its timing means recovery will be even more difficult than usual for these hard-hit communities, as Alaska meteorologist Rick Thoman of the University Alaska Fairbanks explains.

Disasters in remote Alaska are not like disasters anywhere in the lower 48 states, he explains. While East Coast homeowners recovering from a nor’easter that flooded parts of New Jersey and other states the same weekend can run to Home Depot for supplies or drive to a hotel if their home floods, none of that exists in remote Native villages.

What made this storm unusual?

Halong was an ex-typhoon, similar to Merbok in 2022, by the time it reached the delta. A week earlier, it had been a powerful typhoon east of Japan. The jet stream picked it up and carried it to the northeast, which is pretty common, and weather models did a pretty good job in forecasting its track into the Bering Sea.

But as the storm approached Alaska, everything went sideways.

The weather model forecasts changed, reflecting a faster-moving storm, and Halong shifted to a very unusual track, moving between Saint Lawrence Island and the Yukon-Kuskokwim Delta coast.

Unlike Merbok, which was very well forecast by the global models, this one’s final track and intensity weren’t clear until the storm was within 36 hours of crossing into Alaska waters. That’s too late for evacuations in many places.

Did the loss of weather balloon data canceled in 2025 affect the forecast?

That’s a question for future research, but here’s what we know for sure: There have not been any upper-air weather balloon observations at Saint Paul Island in the Bering Sea since late August or at Kotzebue since February. Bethel and Cold Bay are limited to one per day instead of two. At Nome, there were no weather balloons for two full days as the storm was moving toward the Bering Sea.

Did any of this cause the forecast to be off? We don’t know because we don’t have the data, but it seems likely that that had some effect on the model performance.

Why is the delta region so vulnerable in a storm like Halong?

The land in this part of western Alaska is very flat, so major storms can drive the ocean into the delta, and the water spreads out.

Most of the land there is very close to sea level, in some places less than 10 feet above the high tide line. Permafrost is also thawing, land is subsiding, and sea-level rise is adding to the risk. For many people, there is literally nowhere to go. Even Bethel, the region’s largest town, about 60 miles up the Kuskokwim River, saw flooding from Halong.

These are very remote communities with no roads to cities. The only way to access them is by boat or plane. Right now, they have a lot of people with nowhere to live, and winter is closing in.

These villages are also small. They don’t have extra housing or the resources to rapidly recover. The region was already recovering from major flooding in summer 2024. Kipnuk’s tribe was able to get federal disaster aid, but that aid was approved only in early January 2025.

What are these communities facing in terms of recovery?

People are going to have really difficult decisions to make. Do they leave the community for the winter and hope to rebuild next summer?

There likely isn’t much available housing in the region, with the flooding so widespread on top of a housing shortage. Do displaced people go to Anchorage? Cities are expensive.

There is no easy answer.

It’s logistically complicated to rebuild in places like Kipnuk. You can’t just get on the phone and call up your local building contractor.

Almost all of the supplies have to come in by barge – plywood to nails to windows – and that isn’t going to happen in winter. You can’t truck it in – there are no roads. Planes can only fly in small amounts – the runways are short and not built for cargo planes.

The National Guard might be able to help fly in supplies. But then you still need to have people who can do the construction and other repair work.

Everything is 100 times more complicated when it comes to building in remote communities. Even if national or state help is approved, it would be next summer before most homes could be rebuilt.

Is climate change playing a role in storms like these?

That will be another question for future research, but sea-surface temperature in most of the North Pacific that Typhoon Halong passed over before reaching the Aleutian Islands has been much warmer than normal. Warm water fuels storms.

Halong also brought lots of very warm air northward with it. East of the track on Oct. 11, Unalaska reached 68 degrees Fahrenheit (20 degrees Celsius), an all-time high there for October.

Rick Thoman retired from National Weather Service Alaska Region in 2018.

– ref. Typhoon leaves flooded Alaska villages facing a storm recovery far tougher than most Americans will ever experience – https://theconversation.com/typhoon-leaves-flooded-alaska-villages-facing-a-storm-recovery-far-tougher-than-most-americans-will-ever-experience-267423

Source: The Conversation – USA (2) – By Neal H. Hutchens, University Research Professor of Education, University of Kentucky

American colleges and universities are increasingly firing or punishing professors and other employees for what they say, whether it’s on social media or in the classroom.

After the Sept. 10, 2025, killing of conservative activist Charlie Kirk, several universities, including Iowa State University, Clemson University, Ball State University and others, fired or suspended employees for making negative online comments about Kirk.

Some of these dismissed professors compared Kirk to a Nazi, described his views as hateful, or said there was no reason to be sorry about his death.

Some professors are now suing their employers for taking disciplinary action against them, claiming they are violating their First Amendment rights.

In one case, the University of South Dakota fired Phillip Michael Cook, a tenured art professor, after he posted on Facebook in September that Kirk was a “hate spreading Nazi.” Cook, who took down his post within a few hours and apologized for it, then sued the school, saying it was violating his First Amendment rights.

A federal judge stated in a Sept. 23 preliminary order that the First Amendment likely protected what Cook posted. The judge ordered the University of South Dakota to reinstate Cook, and the university announced on Oct. 4 that it would reverse Cook’s firing.

Cook’s lawsuit, as well as other lawsuits filed by dismissed professors, is testing how much legal authority colleges have over their employees’ speech – both when they are on the job and when they are not.

For decades, American colleges and universities have traditionally encouraged free speech and open debate as a core part of their academic mission.

As scholars who study college free speech and academic freedom, we recognize that these events raise an important question: When, if ever, can a college legally discipline an employee for what they say?

Limits of public employees’ speech rights

The First Amendment limits the government’s power to censor people’s free speech. People in the United States can, for instance, join protests, criticize the government and say things that others find offensive.

But the First Amendment only applies to the government – which includes public colleges and universities – and not private institutions or companies, including private colleges and universities.

This means private colleges typically have wide authority to discipline employees for their speech.

In contrast, public colleges are considered part of the government. The First Amendment limits the legal authority they have over their employees’ speech. This is especially true when an employee is speaking as a private citizen – such as participating in a political rally outside of work hours, for example.

The Supreme Court ruled in a landmark 1968 case that public employees’ speech rights as private citizens can extend to criticizing their employer, like if they write a letter critical of their employer to a newspaper.

The Supreme Court also ruled in 2006 that
the First Amendment does not protect public employees from being disciplined by their employers when they say or write something as part of their official job duties.

Even when a public college employee is speaking outside of their job duties as a private citizen, they might not be guaranteed First Amendment protection. To reach this legal threshold, what they say must be about something of importance to the public, or what courts call a “matter of public concern.”

Talking or writing about news, politics or social matters – Kirk’s murder – often meets the legal test for when speech is about a matter of public concern.

In contrast, courts have ruled that personal workplace complaints or gossip typically does not guarantee freedom of speech protection.

And in some cases, even when a public employee speaks as a private citizen on a topic that a court considers a matter of public concern, their speech may still be unprotected.

A public employer can still convince a court that its reasons for prohibiting an employee’s speech – like preventing conflict among co-workers – are important enough to deny this employee First Amendment protection.

Lawsuits brought by the employees of public colleges and universities who have been fired for their comments about Kirk may likely be decided based on whether what they said or wrote amounts to a matter of public concern. Another important factor is whether a court is convinced that an employee’s speech about Kirk was serious enough to disrupt a college’s operations, thus justifying the employee’s firing.

Academic freedom and professors’ speech

There are also questions over whether professors at public universities, in particular, can cite other legal rights to protect their speech.

Academic freedom refers to a faculty member’s rights connected to their teaching and research expertise.

At both private and public colleges, professors’ work contracts – like the ones typically signed after receiving tenure – potentially provide legal protections for faculty speech connected to academic freedom, such as in the classroom.

However, the First Amendment does not apply to how a private college regulates its professors’ speech or academic freedom.

Professors at public colleges have at least the same First Amendment free speech rights as their fellow employees, like when speaking in a private citizen capacity.

Additionally, the First Amendment might protect a public college professor’s work-related speech when academic freedom concerns arise, like in their teaching and research.

In 2006, the Supreme Court left open the question of whether the First Amendment covers academic freedom, in a case where it found the First Amendment did not cover what public employees say when carrying out their official work.

Since then, the Supreme Court has not dealt with this complicated issue. And lower federal courts have reached conflicting decisions about First Amendment protection for public college professors’ speech in their teaching and research.

Future of free speech for university employees

Some colleges, especially public ones, are testing the legal limits of their authority over their employees’ speech.

These incidents demonstrate a culture of extreme political polarization in higher education.

Beyond legal questions, colleges are also grappling with how to define their commitments to free speech and academic freedom.

In particular, we believe campus leaders should consider the purpose of higher education. Even if legally permitted, restricting employees’ speech could run counter to colleges’ traditional role as places for the open exchange of ideas.

The authors do not work for, consult, own shares in or receive funding from any company or organization that would benefit from this article, and have disclosed no relevant affiliations beyond their academic appointment.

– ref. What the First Amendment doesn’t protect when it comes to professors speaking out on politics – https://theconversation.com/what-the-first-amendment-doesnt-protect-when-it-comes-to-professors-speaking-out-on-politics-266128

Source: The Conversation – USA (2) – By Alexandra A Phillips, Assistant Teaching Professor in Environmental Communication, University of California, Santa Barbara

As the planet warms, it risks crossing catastrophic tipping points: thresholds where Earth systems, such as ice sheets and rain forests, change irreversibly over human lifetimes.

Scientists have long warned that if global temperatures warmed more than 1.5 degrees Celsius (2.7 Fahrenheit) compared with before the Industrial Revolution, and stayed high, they would increase the risk of passing multiple tipping points. For each of these elements, like the Amazon rain forest or the Greenland ice sheet, hotter temperatures lead to melting ice or drier forests that leave the system more vulnerable to further changes.

Worse, these systems can interact. Freshwater melting from the Greenland ice sheet can weaken ocean currents in the North Atlantic, disrupting air and ocean temperature patterns and marine food chains.

With these warnings in mind, 194 countries a decade ago set 1.5 C as a goal they would try not to cross. Yet in 2024, the planet temporarily breached that threshold.

The term “tipping point” is often used to illustrate these problems, but apocalyptic messages can leave people feeling helpless, wondering if it’s pointless to slam the brakes. As a geoscientist who has studied the ocean and climate for over a decade and recently spent a year on Capitol Hill working on bipartisan climate policy, I still see room for optimism.

It helps to understand what a tipping point is – and what’s known about when each might be reached.

Tipping points are not precise

A tipping point is a metaphor for runaway change. Small changes can push a system out of balance. Once past a threshold, the changes reinforce themselves, amplifying until the system transforms into something new.

Almost as soon as “tipping points” entered the climate science lexicon — following Malcolm Gladwell’s 2000 book, “The Tipping Point: How Little Things Can Make a Big Difference” — scientists warned the public not to confuse global warming policy benchmarks with precise thresholds.

The scientific reality of tipping points is more complicated than crossing a temperature line. Instead, different elements in the climate system have risks of tipping that increase with each fraction of a degree of warming.

For example, the beginning of a slow collapse of the Greenland ice sheet, which could raise global sea level by about 24 feet (7.4 meters), is one of the most likely tipping elements in a world more than 1.5 C warmer than preindustrial times. Some models place the critical threshold at 1.6 C (2.9 F). More recent simulations estimate runaway conditions at 2.7 C (4.9 F) of warming. Both simulations consider when summer melt will outpace winter snow, but predicting the future is not an exact science.

Forecasts like these are generated using powerful climate models that simulate how air, oceans, land and ice interact. These virtual laboratories allow scientists to run experiments, increasing the temperature bit by bit to see when each element might tip.

Climate scientist Timothy Lenton first identified climate tipping points in 2008. In 2022, he and his team revisited temperature collapse ranges, integrating over a decade of additional data and more sophisticated computer models.

Their nine core tipping elements include large-scale components of Earth’s climate, such as ice sheets, rain forests and ocean currents. They also simulated thresholds for smaller tipping elements that pack a large punch, including die-offs of coral reefs and widespread thawing of permafrost.

Some tipping elements, such as the East Antarctic ice sheet, aren’t in immediate danger. The ice sheet’s stability is due to its massive size – nearly six times that of the Greenland ice sheet – making it much harder to push out of equilibrium. Model results vary, but they generally place its tipping threshold between 5 C (9 F) and 10 C (18 F) of warming.

Other elements, however, are closer to the edge.

Alarm bells sounding in forests and oceans

In the Amazon, self-perpetuating feedback loops threaten the stability of the Earth’s largest rain forest, an ecosystem that influences global climate. As temperatures rise, drought and wildfire activity increase, killing trees and releasing more carbon into the atmosphere, which in turn makes the forest hotter and drier still.

By 2050, scientists warn, nearly half of the Amazon rain forest could face multiple stressors. That pressure may trigger a tipping point with mass tree die-offs. The once-damp rainforest canopy could shift to a dry savanna for at least several centuries.

Rising temperatures also threaten biodiversity underwater.

The second Global Tipping Points Report, released Oct. 12, 2025, by a team of 160 scientists including Lenton, suggests tropical reefs may have passed a tipping point that will wipe out all but isolated patches.

Corals rely on algae called zooxanthellae to thrive. Under heat stress, the algae leave their coral homes, draining reefs of nutrition and color. These mass bleaching events can kill corals, stripping the ecosystem of vital biodiversity that millions of people rely on for food and tourism.

Low-latitude reefs have the highest risk of tipping, with the upper threshold at just 1.5 C, the report found. Above this amount of warming, there is a 99% chance that these coral reefs tip past their breaking point.

Similar alarms are ringing for ocean currents, where freshwater ice melt is slowing down a major marine highway that circulates heat, known as the Atlantic Meridional Overturning Circulation, or AMOC.

The AMOC carries warm water northward from the tropics. In the North Atlantic, as sea ice forms, the surface gets colder and saltier, and this dense water sinks. The sinking action drives the return flow of cold, salty water southward, completing the circulation’s loop. But melting land ice from Greenland threatens the density-driven motor of this ocean conveyor belt by dilution: Fresher water doesn’t sink as easily.

A weaker current could create a feedback loop, slowing the circulation further and leading to a shutdown within a century once it begins, according to one estimate. Like a domino, the climate changes that would accompany an AMOC collapse could worsen drought in the Amazon and accelerate ice loss in the Antarctic.

There is still room for hope

Not all scientists agree that an AMOC collapse is close. For the Amazon rain forest and the North Atlantic, some cite a lack of evidence to declare the forest is collapsing or currents are weakening.

In the Amazon, researchers have questioned whether modeled vegetation data that underpins tipping point concerns is accurate. In the North Atlantic, there are similar concerns about data showing a long-term trend.

Climate models that predict collapses are also less accurate when forecasting interactions between multiple tipping points. Some interactions can push systems out of balance, while others pull an ecosystem closer to equilibrium.

Other changes driven by rising global temperatures, like melting permafrost, likely don’t meet the criteria for tipping points because they aren’t self-sustaining. Permafrost could refreeze if temperatures drop again.

Risks are too high to ignore

Despite the uncertainty, tipping points are too risky to ignore. Rising temperatures put people and economies around the world at greater risk of dangerous conditions.

But there is still room for preventive actions – every fraction of a degree in warming that humans prevent reduces the risk of runaway climate conditions. For example, a full reversal of coral bleaching may no longer be possible, but reducing emissions and pollution can allow reefs that still support life to survive.

Tipping points highlight the stakes, but they also underscore the climate choices humanity can still make to stop the damage.

Alexandra A Phillips does not work for, consult, own shares in or receive funding from any company or organization that would benefit from this article, and has disclosed no relevant affiliations beyond their academic appointment.

– ref. What are climate tipping points? They sound scary, especially for ice sheets and oceans, but there’s still room for optimism – https://theconversation.com/what-are-climate-tipping-points-they-sound-scary-especially-for-ice-sheets-and-oceans-but-theres-still-room-for-optimism-265183