Thursday, May 7, 2026

Science has just discovered “oases” of clams and tube worms at a depth of 9,533 meters, where sunlight does not exist and yet life thrives in abundance


From Ecoticias

A last-minute detour nearly six miles down has led scientists to what they call the deepest known ecosystem on Earth, a long stretch of seafloor communities that don’t depend on sunlight at all.
Instead, clams and tube worms appear to survive on chemical energy from methane and other gases leaking out of cracks in the ocean floor.

The discovery, described in a new Nature study, comes from dives in two remote trenches in the northwest Pacific, including areas between Russia and Alaska.
It also adds a fresh twist to a big question in ocean science: how far down can life really go, and what keeps it going when there’s no light, little food, and crushing pressure?

A “one-more-look” moment in the hadal zone


The hadal zone is the deepest part of the ocean, starting around 6,000 meters down and running to the bottom of the deepest trenches.
Think of it as Earth’s underwater canyons, where pressure is so extreme that ordinary submarines cannot go.

During a 2024 expedition that ran from July 8 to August 17, researchers used the deep-diving submersible Fendouzhe to explore the Kuril-Kamchatka Trench and the western Aleutian Trench.
Geochemist Mengran Du, working with Xiaotong Peng, reported seeing dense groups of animals at depths from about 5,800 to 9,533 meters, spanning roughly 2,500 kilometers.

How methane replaces sunlight

Most life on Earth ultimately runs on sunlight, because plants and algae use it to make food.
In these trenches, there’s no light at all, so the system runs on chemosynthesis, which is basically “making food from chemicals” instead of from sunlight.

Here’s the simple version.
Cold seeps are cracks in the seafloor that leak chemicals like methane and hydrogen sulfide, and NOAA’s cold seep overview explains how bacteria can use those chemicals for energy.
Some of these bacteria live inside animals like clams and tube worms, feeding their hosts in a kind of built-in food factory.

A new clue about carbon cycling in the deepest ocean

What surprised the team wasn’t just the animals, but the chemistry under them.
The researchers reported unusually high methane in trench sediments, and they suggest microbes may be producing methane locally by processing buried organic material and recycling carbon on site.

In practical terms, that means the trenches may act less like a dead-end storage pit and more like a “recycling center” for carbon in the deep ocean.

That matters because methane and carbon dioxide are powerful greenhouse gases in the atmosphere, and understanding where carbon ends up, and how long it stays there, helps scientists build better climate and ocean models.

Why this matters beyond the trenches


Experts who were not part of the work say the size and depth of the communities stand out.
Johanna Weston of Woods Hole Oceanographic Institution has pointed out that deep trenches are remote, but they’re still connected to the surface, including through food pulses and pollution that sinks.

That connection keeps showing up in other research.
Weston’s team recently described a deep-sea scavenger that feeds on sinking seaweed in the Atlantic in a Woods Hole press release, and earlier work linked trench life to plastic pollution through an Eurythenes plasticus report.

Meanwhile, methane-based partnerships aren’t limited to trenches, as shown by a methane-powered sea spiders study that found deep-sea spiders hosting methane-eating microbes on their bodies.

What comes next for exploring the deepest ocean

The big takeaway is that these chemical-powered communities may be more widespread than scientists once thought.
If similar cold seep conditions exist in other trenches, there may be more “dark ecosystems” waiting, and some species may be new to science.

That’s one reason international efforts are ramping up, including the Global Hadal Exploration Programme, which aims to coordinate deep-ocean research across countries and disciplines.
It fits a broader surge in species discovery, highlighted by the Ocean Census announcement that reported hundreds of newly documented marine species.

Links :

Wednesday, May 6, 2026

NOAA releases first images of nodules from waters near American Samoa


Image of geological samples from the seafloor that were collected via box core on April 14, 2026, in U.S. waters off American Samoa. (Image credit: USGS)
Download Image

From NOAA
 
New images and samples were collected during 2026 efforts to map and characterize the seafloor in federal waters off American Samoa 

NOAA released today the first images of geologic seafloor samples from a hydrographic survey project to map and characterize more than 30,000 square nautical miles of federal waters in the U.S. exclusive economic zone (EEZ) beyond the territorial waters of American Samoa. The box core samples will allow for further analysis to understand the composition of deep sea resources and the environments in which they are found.

“NOAA’s mapping missions serve as a reminder that ocean exploration is a vital piece of our nation’s economic development,” said NOAA Administrator Neil Jacobs, Ph.D. “These images highlight the outstanding work of our NOAA team and partners to characterize the seafloor, and the data gathered during this historic project will enable science-based decision-making to support responsible development.”

The new images were collected as part of a Department of Commerce initiative to implement the U.S. Offshore Critical Minerals Mapping Plan as defined by President Trump’s Executive Order 14285: Unleashing America's Offshore Critical Minerals and Resources. In developing the mapping plan, NOAA, in consultation with the Department of Interior’s Bureau of Ocean Energy Management(BOEM) identified the federal waters near American Samoa as a priority area of the seabed for mapping and analyzing nodules that may contain critical minerals.

“NOAA’s work to map and characterize these areas reflects the strength of interagency collaboration under President Trump’s Executive Order to unleash America’s offshore critical minerals,” said BOEM Acting Director Matt Giacona. “For BOEM, NOAA’s high-resolution mapping and characterization are essential inputs that will provide the foundational data needed to assess resource potential, inform leasing and environmental reviews, and reduce uncertainty as we evaluate future offshore mineral activities in a responsible, science-based manner.”

As the mission remains underway, images of the seafloor and box core samples will be posted online on a rolling basis, serving as an initial indication of mineral resource potential and the deep-ocean marine environment in the federal waters off American Samoa. Scientists from the U.S. Geological Survey (USGS) will conduct analyses of the seafloor composition, which will enhance scientific understanding of the deep seabed in the region and inform future exploration and activities related to deep seabed minerals. USGS plans to release the initial analyses from this work early this summer.

Presumed polymetallic nodules on the seafloor off American Samoa at a depth of 5,498 meters (3.42 miles) prior to the collection of a box core. (Image credit: NOAA)
Download Image


“USGS is excited for the opportunity to study the composition of these unique mineral samples in U.S. waters within the Samoa Basin,” said Ned Mamula, director, USGS. “We will continue providing the actionable science our partner agencies need for decision-making.”

NOAA’s Office of Coast Survey is leading the project contract, with NOAA Ocean Exploration, BOEM, and USGS providing additional scientific expertise and guidance.

About deep seabed mineral development

Deep seabed mining is the extraction of nodules containing critical minerals from the ocean floor. Some regions of the deep seabed contain an abundance of valuable resources like manganese, nickel, cobalt, copper and rare earth elements. Critical minerals are used in everything from defense systems and batteries to smartphones and medical devices and are increasingly important components for American manufacturing. Access to these minerals is a key factor in the resilience of U.S. supply chains. Learn more by visiting NOAA’s National Ocean Service website.

Tuesday, May 5, 2026

The seabed doctrine: when commercial infrastructure gets drafted

 
 
From Pulse by Dize Kandu
 
There is a sentence buried on page seventeen of the U.S. Strategic Subsea Cables Act of 2026 that I cannot stop thinking about.
It quotes NATO: undersea cables carry an estimated ten trillion dollars in transfers every day, and around ninety-five percent of global data flows are transmitted through them.
The number is doing the work of an argument.
You read it and you feel, viscerally, that something so vital must be protected and whatever protection looks like, it must be worth the cost.

That is how doctrine gets written now.
Not with tanks, not with treaties, but with statistics placed so precisely that the conclusion appears to arrive on its own.

I have been watching the subsea cable file for a while as a maritime security professional, but also as someone who lives in a country where several of the world's critical digital arteries surface.
What is happening in Washington right now is not, properly speaking, a cable protection bill.
It is the quiet legislative reclassification of a global commercial network into a strategic military asset, and it is being done through a door almost no one is watching: the door of narrative.

What the Act Actually Does

Let me walk through the legislation, because most of the summaries floating around have been written by people who read the press release and stopped there.

The Strategic Subsea Cables Act of 2026, introduced in March by Representatives Wilson and Meeks with Senate companions from Shaheen and Barrasso, pairs with H.R.2503, an export control bill that industry analysts have already started calling "the shield" to the Act's "sword."
The shield keeps subsea cable manufacturing and maintenance technology out of Chinese hands, accelerating what submarine industry observers describe as a formal split between "trusted" Western cable supply chains and "untrusted" Chinese ones.
The sword, this new Act, does four things.



It mandates sanctions against any foreign person who intentionally damages undersea infrastructure.
It creates ten full-time State Department positions dedicated to cable diplomacy, with instructions to work the International Cable Protection Committee harder and to build a multinational fleet of dedicated repair ships.
It establishes a presidential interagency committee to coordinate U.S.cable policy across the Department of State, Homeland Security, the Department of War, the Department of Commerce, and others.
And it requires federal agencies to share threat information directly with private cable operators, who are, let us remember, commercial telecommunications companies.

Read those four elements together, and something becomes clear that the summaries do not state.
The Act is not designed to protect cables.
It is designed to enroll them.
A commercial fiber-optic line laid by a consortium of private carriers becomes, under this framework, a node in an American-led enforcement architecture, one whose operating concept is sanctions, whose intelligence-sharing moves in one direction, and whose legal theory rests on intentional state-sponsored sabotage.

And here is where the architecture starts to show its seams.

Of the roughly six hundred active cables on the planet, around four private firms; SubCom (United States), Alcatel Submarine Networks (France), NEC (Japan), and HMN Technologies (China), manufacture and install the overwhelming majority.
Consortiums own most of the cables.
Landings are scattered across dozens of jurisdictions.
The repair fleet, such as it is, is chronically undersized and aging.
No single government commands this system.
No single government can.
The Act does not attempt to build shared governance; it attempts to install U.S. jurisdiction over the parts that can be reached through sanctions, licensing, and the threat of private litigation.
It is, functionally, a workaround for the fact that the actual system is bigger than any one state.
Juha Martelius and the Inconvenient Problem of Evidence

Which brings me to a name most people in the defense community outside Europe have never heard.

Juha Martelius is the director of Supo, Finland's Security and Intelligence Service, an agency whose sole job is to understand what is actually happening on and under the water between Finland and Russia.
In March of this year, Supo published its National Security Overview for 2026, and Martelius put something on the record that Washington has not yet fully absorbed.
Direct quote, publicly delivered: "Our understanding has been that there has been no deliberate Russian state activity in the background.
It is a very broadly shared view in the other European intelligence community."

Let that sit for a moment.

Source: Dmitri Fedotkin/ERR

The country that lost the Estlink 2 power cable on Christmas Day 2024.
The country that seized the Eagle S tanker, spent months investigating it, charged its officers with aggravated criminal mischief, and then watched its own courts struggle with the fundamental legal question of whether anchor drag outside territorial waters could even be prosecuted as sabotage under existing law.
The country that knows exactly how to run a cable incident to ground, because it has done it, that country, through the agency best positioned to know, is saying: slow down.
Not every cable fault is a hybrid warfare attack.
And labeling every incident as Kremlin-directed sabotage, Supo warns explicitly in its assessment, "may actually amplify the fear and perceived reach of Russian power, which serves Russian strategic interests."

In intelligence terms, this is a devastating observation.
Finland is essentially telling the rest of the Western alliance that the narrative around subsea cable incidents is running ahead of the evidence, and that the narrative itself is doing Moscow's work for it.

There is a deeper technical point embedded in Supo's caution that deserves attention.
The Baltic Sea, where most of the recent incidents have clustered, sees an enormous volume of commercial traffic through shallow, cable-dense waters.
Of the roughly 150 to 200 cable faults that occur worldwide every year, the overwhelming majority are caused by fishing trawlers and anchor drops in waters under two hundred meters.
Seven cable cuts in the Baltic between November 2024 and January 2025 sounds alarming, and it is.
But it is also statistically consistent with what happens when shadow fleet vessels, poorly maintained, crewed by people working under opaque ownership structures, operating tankers with documented equipment failures transit one of the world's most cable-dense shallow seas.
Some of those incidents are almost certainly deliberate.
Some are almost certainly not.
Distinguishing between the two requires forensic patience that a sanctions-driven policy framework actively discourages.



The Eagle S case is the case study nobody wants to talk about.
Finnish prosecutors could not prove intent.
They pivoted to a clever argument, that operating a vessel so poorly maintained that its windlass could malfunction constituted criminal recklessness but the court was unmoved on the jurisdictional question of damage occurring in the exclusive economic zone rather than territorial waters.
The tanker was eventually released.
The crew returned home.
The cable was repaired.
And Finland was left with a legal system that had tried, in good faith, to prosecute suspected cable sabotage under the rule of law and run aground on structural limitations that international maritime law never contemplated when it was written.

The Strategic Subsea Cables Act does not solve that problem.
It routes around it.
If the courts cannot prove intent, sanction the ship's beneficial owner.
If the flag state is useless, target the registry itself.
If the evidence is ambiguous, let the cable owner file a civil suit that does not require the same burden of proof.
This is not the rule of law being strengthened.
It is the rule of law being supplemented by the rule of unilateral economic pressure, and the supplement is quickly becoming the main instrument.

The Attribution Problem



Here is the gap that most Western defense commentary is refusing to address.
It is not a question of whether Russia has the capability and intent to damage subsea infrastructure.
It plainly does.
The GUGI fleet, Russia's Main Directorate for Deep Sea Research, maintains special-purpose vessels at Olenya Guba that are explicitly designed for seabed operations, including deep-diving submersibles, oceanographic surveillance ships, and nuclear-powered auxiliary submarines built for exactly this kind of work.
The reconnaissance patterns in the Baltic are real and have been documented for years.
No serious analyst disputes any of that.

The question is whether a legislative and sanctions architecture should be built on the assumption that every incident is confirmed sabotage, when the country with the most operational experience is telling us that sometimes a dragged anchor is a dragged anchor, and sometimes a windlass really does malfunction on a rusty tanker owned by a brass-plate company at a Dubai hotel address.
There is, of course, a middle category that deserves its own scrutiny: incidents that are not state ordered but are state tolerated, recklessness that Moscow neither commands nor prevents because the resulting chaos serves its interests regardless of who initiated it.
That distinction matters enormously, and it is precisely the kind of distinction that a sanctions first framework is structurally incapable of drawing.

This matters because attribution, once codified into policy, becomes self-reinforcing.
Every subsequent incident gets read through the attributed framework.
Every ambiguity resolves in favor of the conclusion already reached.
Supo has seen this before, in a different context, admittedly, but the institutional memory is relevant.
Finnish intelligence spent much of the Cold War learning how to distinguish between what Moscow was actually doing, what Moscow wanted Helsinki to think it was doing, and what Helsinki's allies were projecting onto the relationship.
That kind of analytical discipline is rare, and it is exactly what the current moment requires.

The American framework does not have that discipline built into it.
It has the opposite: a bipartisan consensus that adversary attribution is politically cheap and politically useful, combined with a legal architecture that rewards speed over accuracy.

The Classical Problem: What a Cable Actually Is

There is an older debate hiding underneath this new one.
In classical international law, subsea cables are commercial infrastructure, and their protection has been governed since 1884 by a convention whose enforcement mechanism is basically "the courts of the flag state will probably do something, eventually." 
UNCLOS adds some overlay but does not fundamentally change the commercial character of the assets.



The Strategic Subsea Cables Act does not amend either framework.
What it does instead is create a parallel, unilateral enforcement regime grafted onto commercial assets, one where the U.S.
government shares "threat information" with private operators, imposes sanctions on suspected saboteurs, and encourages cable owners to pursue private lawsuits against anonymous defendants in the style of Google's recent "Does 1 through 25" case, a civil action in which the company sued unnamed defendants operating fraudulent online advertising schemes linked to Chinese networks, using discovery mechanisms to unmask anonymous actors.
CSIS has been admirably candid about this framework, calling it "deterrence by detection" and "deterrence by punishment," and crediting it with a novel virtue: eliminating "plausible deniability."

I understand the appeal.
I really do.
Faced with a string of cable incidents in the Baltic and growing nervousness about Chinese behavior in the South China Sea, something has to be done.
But "deterrence by detection" is only as good as the attribution regime underneath it.
And if Finland, whose intelligence service is paid to be paranoid about exactly this question, is publicly saying the attribution is shakier than the headlines suggest, then what the Act is actually deterring may not be sabotage.
It may be deniability itself.

Which is a different, more interesting, and considerably more aggressive thing.

Deniability, in the grammar of international relations, is what allows states to act in the grey zone without triggering formal escalation.
Stripping it away sounds like a pure good, who, after all, is in favor of plausible deniability? The counter argument is not frivolous: deniability is also an enabler, the very mechanism that allows grey zone operations to continue without consequence, and reasonable analysts can disagree about which function predominates.
But in practice, deniability also functions as a shock absorber.
It creates space for quiet de-escalation, backchannel resolution, and the slow work of attribution that Finnish courts, for all their failures, have at least tried to do properly.
A regime that eliminates deniability through pre-attributed sanctions does not reduce hybrid warfare.
It simply relocates the escalation from the water to the courtroom, from the courtroom to the sanctions list, and from the sanctions list to wherever comes next.
What This Looks Like From Outside Washington



For countries positioned at the intersection of multiple cable corridors, Türkiye being one of them, with Mediterranean and Black Sea systems landing and transiting through our jurisdiction, a legislative architecture that converts commercial cables into strategic U.S.
assets is not a neutral development.
It is the extraterritorial extension of American maritime authority over infrastructure that touches our territorial waters, exclusive economic zones, and landing stations.

The Act does not ask Türkiye's permission to sanction a vessel that happens to drag its anchor near a cable running through our seabed.
It does not require coordination with the countries whose forensic intelligence services may have reached different conclusions about a given incident.
It simply installs Washington as the primary adjudicator of what counts as sabotage, what counts as accident, and what penalties attach to each.

Consider what this means in practice.
A Russian-linked tanker damages a cable in the Black Sea.
Under the Act, the U.S.
Treasury can move against the vessel's beneficial owner, freeze its assets, and pressure its insurers and classification society, all before a Turkish investigation has even begun.
Cable owners, many of them American companies, can file civil suits in U.S.
courts for damages that occurred in our waters.
Sanctions packages can be built on intelligence we did not participate in collecting and attribution judgments we did not review.
The enforcement architecture operates regardless of whether the coastal state agrees with the underlying analysis.

This is STRATCOM in legislative form, not the discipline of strategic communications as commonly understood, but its older sibling, the construction of an interpretive framework so dense, so pre-populated with conclusions, that disagreement sounds naive.
When every cable incident arrives with its attribution already attached, the policy response becomes automatic.
When the policy response becomes automatic, the policy framework becomes permanent.
When the policy framework becomes permanent, the cables themselves stop being commercial infrastructure in any meaningful sense.
They become something else.
They become a theatre.

And theatres, as anyone who has studied maritime security knows, are never neutral spaces.
What Can Be Done



What is to be done, then, by those of us who are not writing the legislation in Washington but who will have to operate inside its consequences?

First, build independent analytical capacity.
Every coastal state with significant cable exposure should develop its own forensic and attribution expertise, separate from whatever Washington's interagency committee decides to share.
Finland's Supo is a model precisely because it is willing to say "we do not see what you say you see." That kind of epistemic independence is now a strategic asset, not a diplomatic inconvenience.
For Türkiye specifically, with our existing maritime intelligence infrastructure and our geographic position at the chokepoints of two cable theatres, this capacity is achievable within a realistic timeframe if the institutional will exists to build it.

Second, insist on the older framework.
Subsea cables are commercial infrastructure under the 1884 convention and under UNCLOS.
They are also strategic in effect, yes, but collapsing the distinction between commercial and military in legal terms is exactly the move that allows unilateral enforcement to masquerade as international law.
Countries with cable landings should resist the collapse, not because sabotage is fine, but because the legal categories still matter and because once they are collapsed, it will be very difficult to uncollapse them.
International maritime law evolves at the speed of consensus, and unilateral reclassification by the most powerful actor in the system is not consensus.

Third, and this is the part that defense sector LinkedIn will find uncomfortable: recognize that "deterrence by detection" is a narrative weapon before it is a technical one.
The AI, the predictive analytics, the cued satellite imagery, all of it is real and useful.
I have no quarrel with the technology, and the detection architecture has produced real operational value in tracking vessel movements and identifying suspicious transit patterns that would otherwise go unnoticed.
But what gets detected depends on what you are looking for, and what gets reported depends on who is writing the press release.
A maritime security architecture in which only Washington gets to name the saboteurs is not a security architecture.
It is a content strategy with sonar attached.

Fourth, invest in regional cooperation that does not run through Washington.
The Mediterranean cable cluster, the Black Sea landings, the Red Sea transit routes through Egypt, each of these is a theatre where coastal states have direct interest and insufficient coordination.
The European Union's 2025 cable security action plan is a start, but it remains overwhelmingly Atlanticist in its framing.
What is missing is a genuinely regional attribution and response framework that reflects the intelligence priorities and legal traditions of the states whose waters actually hold the cables.

The Argument, in the End



I will end with the sentence that started this piece.
Ten trillion dollars in transfers every day, ninety-five percent of global data.
Those numbers are real.
But they describe a commercial network that serves everyone, built mostly by four private companies, maintained by repair ships crewed by labour from a dozen countries, funded by consortiums that cross every geopolitical fault line on the planet.
It is one of the few genuinely shared pieces of infrastructure that the modern world still has.
The fact that my bank transaction and a Chinese financial transfer and a Russian diplomatic cable all ride the same fiber-optic strand for part of their journey is not a vulnerability to be eliminated.
It is a rare, dwindling piece of functional interdependence.

The question is whether we protect it as something shared, or whether we let it be drafted into somebody else's war.

Finland, quietly, is arguing for the former.
The Strategic Subsea Cables Act is quietly delivering the latter.
And the rest of us are going to have to decide, sooner than we think, which architecture we actually want to live inside.

Monday, May 4, 2026

Netherland (based on rasterized ENC NLHO) layer update in the GeoGarage platform

 
63 nautical charts updated

China establishes world's largest integrated maritime safety network

Vessels sail in a waterway in the Yangtze River in Hukou county, Jiujiang, east China's Jiangxi province.
(Photo/Zheng Feihua)

From People's Daily Online by Han Xin
 
China has developed the world's most comprehensive maritime safety and support infrastructure, creating a complete navigational assistance network covering coastal ports and shipping lanes, according to the Ministry of Transport.

In the first quarter of this year, China's coastal and inland ports handled 8.11 million vessel calls and 4.795 billion tons of cargo -- up 6.57 percent and 21.72 percent year on year, respectively.

Behind this busy shipping network lies an equally extensive support system.
"Maritime safety and support services provide technical backing for waterborne activities through spatial geographic information, navigation aids, communications, and environmental sensing, explained an official with the Maritime Safety Administration (MSA) under the Ministry of Transport.
"This ensures vessel safety, improves shipping efficiency, and supports marine economic development."

Maritime support serves as a "guardian" of navigation safety.

When a vessel collision occurred in the Pearl River estuary on Oct. 25, 2025, the MSA Southern Navigation Service Center promptly activated its emergency response mechanism and carried out efficient handling measures.

The Guangzhou Coast Radio Station issued navigational warnings in both Chinese and English; survey vessels located the sunken wreckage and surveyed temporary navigable channels; buoy vessels deployed emergency navigation marks in a timely manner, safeguarding smooth and orderly maritime traffic.

Cargo on an ocean-going vessel is handled in Xiamen, southeast China's Fujian province.
(Photo/Zeng Demeng)


Such rapid response is made possible by an efficient system that integrates navigation aids, hydrographic surveying, and communications.

In the South China Sea, all navigation aids in the Sansha waters have been equipped with the BeiDou navigation satellite system for remote monitoring and control, helping ensure the safe passage of more than 100,000 vessels annually.

In the East China Sea, China's first electronic nautical chart dedicated to fisheries was put into operation late last year, integrating key information such as high-risk zones for collisions between commercial and fishing vessels and major north-south coastal shipping routes, thereby enhancing safety in marine fishing operations.

A maritime support network spanning sea, land, and air now operates around the clock, quietly safeguarding waterways and vessels.
In 2025, the maritime system ensured the safe entry and exit of over 34.64 million vessels, while waterborne transport accidents fell by 36.7 percent year on year.

Data is another cornerstone.
China now conducts approximately 23,000 square kilometers (in converted units) of hydrographic surveying annually, and more than 5 million electronic charts are issued each year, providing high-precision foundational data for port planning, channel expansion, and improving navigational efficiency.

By the end of March this year, China managed 24,600 coastal navigation aids, an increase of 65 percent from a decade ago.
Annual public-service communications exceed 2.2 million instances, with over 1 million safety messages broadcast each year, forming a unified communication network that connects ports and vessels worldwide.

How has such a vast, multi-dimensional system been built? The answer lies in sustained technological innovation.

"As a technology-intensive sector, maritime support integrates a range of cutting-edge technologies, including artificial intelligence, big data, and satellite positioning and navigation," said Li Shigang, director of the Donghai Navigation Safety Administration under the Ministry of Transport.
He noted that the shipping industry is accelerating its transition toward greater intelligence and greener development.

In March 2024, the MSA launched an integrated map platform.
It consolidates marine charts, river charts and terrestrial geographic data onto one unified system and terminal, breaking long-standing data silos that separated maritime and land-based navigation services.

This innovation eliminates previous data barriers that prevented users from accessing multiple types of chart services simultaneously.
The platform has so far provided spatiotemporal data services to more than 50,000 vessels and over 20 ports, with annual service calls reaching into the tens of billions.
It has supported projects such as offshore wind power development and subsea oil pipelines.


A buoy tender carries out buoy replacement operations in the main channel of Longkou Port, east China's Shandong province, Nov.
15, 2025.
(Photo/Tang Ke)


Infrastructure upgrades have also played a key role.

In the Bohai Sea, the MSA Northern Navigation Service Center has partnered with offshore oil companies and telecom operators to build multi-mode 5G base stations using offshore oil platforms.
As a result, the Liaoning-Shandong shipping route, which carries millions of passengers annually, has eliminated communication blackouts during its roughly seven-hour voyage.
Full coverage of communications and sensing across the Bohai Sea is expected by the end of this year.

In the South China Sea, the MSA has established the largest drone fleet within China's maritime system.
It has developed an "drone-plus" operational model for inspecting navigation facilities, collecting survey data, and responding to emergencies, enabling routine three-dimensional maritime support.

From traditional lighthouses and automatic identification systems to communication stations and the integrated map platform, continued investment in infrastructure is pushing China's maritime capabilities from "near-shore visibility" to "full-domain manageability."

Challenges remain.
China's maritime support system still faces gaps in advanced equipment, limited capabilities in distant and deep-sea areas, and insufficient sensing capacity in key waters.

"As China's maritime activities expand from near-shore and coastal areas to distant oceans and even polar regions, maritime support services must extend their reach accordingly," Li said.
"We need to broaden both geographic and functional coverage, strengthen capabilities in deep-sea areas, and better safeguard the stability of international logistics supply chains."

Looking ahead, efforts will focus on advancing the application of satellite internet at sea and enhancing communication and regulatory capabilities in key maritime zones, islands, and major straits, he added.
 

Sunday, May 3, 2026

Germany (based on rasterized ENC BSH) layer update in the GeoGarage platform

 
4 new nautical charts + 132 charts updated

Four waves crashing into each other


One of the rarest ocean phenomena wasn’t discovered by scientists—it was spotted by surfers.

Saturday, May 2, 2026

Sanderlings, fastest feet



Sanderlings rushing toward the water's edge

Friday, May 1, 2026

Portugal (based on rasterized ENC IHPT) layer update in the GeoGarage platform


24 nautical charts based on rasterized ENC (IHPT) updated


Croatia (based on rasterized ENC HHI) layer update in the GeoGarage platform

2 new charts added
 

 

Flamboyant sea slugs

Thursday, April 30, 2026

Spain (based on rasterized ENC IHM) layer update in the GeoGarage platform

56 ENC updated

Remembering Titanic: the tragedy behind SOLAS


From Safety4Sea

Claiming the title of the most high-level shipwreck in history, Titanic is far more than a famous tragic story as it redefined the concept of maritime safety and led to the adoption of SOLAS Convention.

The 𝗧𝗶𝘁𝗮𝗻𝗶𝗰 sank on the night of April 14 to 15, 1912.
Here, the images of its launch, in 1911.
Which required 22 tons of tallow, oil, and soap to make it slide.
 
The incident


The British luxury passenger ship RMS Titanic began its maiden voyage from Southampton, England to New York, US, on 10 April 1912.
After calling at Cherbourg in France and Queenstown (now Cobh) in Ireland on the same day, the ship headed west to New York, where it was expected to arrive on the morning of 17 April.

When the ship was about 375 miles south of Newfoundland, on 14 April, 11:40 p.m., lookout Frederick Fleet spotted an iceberg immediately ahead of Titanic and alerted the bridge.
First Officer ordered the ship to be steered around the obstacle and the engines to be reversed, but it was too late; the starboard side of Titanic struck the iceberg, rupturing five of its 16 supposedly watertight compartments below the waterline, while the ship could only survive four flooding.

Titanic began sinking bow-first, with water spilling from compartment to compartment as its angle in the water became steeper.
Meanwhile, distress signals were sent and passengers and some crew members were evacuated in lifeboats, many of which were launched only partially loaded.

At 2:20 am, the ship broke apart and foundered with more than 1,000 people still aboard.
Just under two hours after Titanic sank, the Cunard liner RMS Carpathia arrived and brought aboard an estimated 705 survivors.

Titanic: A timeline of events
14 April, 11:35 PM: Lookout spots an iceberg, rings the bell three times and calls the bridge.
First officer orders the Titanic “hard-a-starboard” (to the left) and the engines reversed.
He also closes the doors to the watertight compartments.
14 April, 11:40 PM: The starboard side of the Titanic hits the iceberg, Captain Smith arrives on deck and is informed that at least five of the ship’s compartments are flooded.
Designer Thomas Andrews surveys the damage, predicting that the ship has only about one to two hours before sinking.
15 April, 12:00 AM: Lifeboats begin to be readied for launch.
15 April, 12:15 AM: Distress signals are sent but most ships that respond are too far away.
15 April, 12:20 AM: The Carpathia receives the signal and immediately changes course to aid the ship, but it will need more than three hours to arrive.
Passengers’ embarkation on lifeboats is underway.
15 April, 12:45 PM: The ship unsuccessfully fires the first of eight distress rockets.
The first lifeboat is launched well below capacity, partially because of the crewmen’s worry that the davits would be unable to hold a fully loaded lifeboat.
15 April, 2:00 AM: The only lifeboats that remain on the Titanic are three of the collapsible boats.
The Titanic’s bow has sunk low enough that the stern’s propellers are now clearly visible above the water.
Captain Smith releases the crew, saying that “it’s every man for himself.” The Captain is reportedly seen on the bridge for the last time.
His body will never be recovered.
15 April, 2:17 AM: Wireless radio operator Jack Phillips sends a final distress signal.
He reportedly makes it to the overturned collapsible lifeboat B but succumbs to exposure.
His body will not be found.
15 April, 2:18 AM: The lights on the Titanic go out.
The ship breaks in two between the third and fourth funnels.
15 April, 2:20 AM: The stern disappears below the water, and the Titanic is gone.
15 April, 3:30 AM: The Carpathia arrives in the area, firing rockets.
15 April, 4:10 AM: The Carpathia begins picking up survivors from lifeboats.
15 April, 8:30 AM: The Californian arrives, searches the area for several hours but fails to find any survivors.
15 April, 8:50 AM: The Carpathia, carrying the 705 Titanic survivors, heads to New York City, where it will arrive on April 18.

Fatalities

All people who did not manage to get on lifeboats immersed in lethally cold water with a temperature of −2 °C (28 °F) and almost all died of cardiac arrest or other bodily reactions to freezing water, within 15–30 minutes.
Only five of them were helped into the lifeboats, though the lifeboats had room for almost 500 more people.

As a result, more than 1,500 people lost their lives, and about 705 were rescued, although theories on the exact numbers vary due to confusion over the passenger list, which included some names of people who canceled their trip at the last minute and some who were double-counted on the casualty lists.

Passengers traveling first class were significantly more likely to survive than other passengers, while women and children were more likely to survive than men, due to a “women and children first” protocol in lifeboats.
To put that into perspective, 387 of the 462 men in third class onboard perished in the disaster, and only 4 out of the 144 women in first class were lost.
Although unsurprisingly, third class suffered the greatest loss, subsequent claims that passengers in steerage were prevented from boarding lifeboats were largely dispelled.
The high death toll in third class was mostly attributed to the lack of a proper general alarm that did not permit passengers to realize the emergency until it was too late, while the difficulty of simply navigating the complex Titanic from the lower levels caused some to reach the top deck after most of the lifeboats had been launched, according to Britannica.

Probable causes

-Climate conditions: 
The immediate cause of the sinking was collision with an iceberg, which reminds us that, in every tragedy, there is human error along with bad luck.
In that time of that year, warmer-than-usual waters in the region made Atlantic waters a fruitful ground for corralling icebergs at the intersection of the Labrador Current and the Gulf Stream, while unusually high tides in January 1912 possibly dislodged icebergs of Labrador Sea sending them towards the Titanic route some months later.
In addition, the two lookouts onboard, Frederick Fleet and Reginald Lee, had a difficult job that night due to the fact that the ocean was unusually calm that night: As there would be little water breaking at its base, an iceberg would be more difficult to spot.
 
Neglecting warnings: 
Titanic received a series of warnings from other ships of drifting ice in the area of the Grand Banks of Newfoundland.
One of the ships to warn Titanic was the Atlantic Line’s Mesaba, a few hours before the tragedy, but the message was never relayed to the Titanic’s bridge.
Shortly after, the nearby Californian notified Titanic that it had stopped after becoming surrounded by ice, but wireless operator Phillips, who was handling passenger messages, scolded the Californian for interrupting him: “Shut up! Shut up! I am busy.”
 
Reversed engines: 
As soon as the bridge was notified of the iceberg, First Officer William Murdoch ordered a “hard-a-starboard”—a maneuver that would turn the ship to port (left)—and the engines reversed.
The Titanic began to turn, but it was too close to avoid a collision.
By reversing the engines, Murdoch actually caused the Titanic to turn slower than if it had been moving at its original speed.
Most experts believe the ship would have survived if it had hit the iceberg head-on, according to Britannica.
It has also been reported that, if the ship had stopped where it was hit, seawater would not have pushed into one interior compartment after another, and the ship might not have sunk as quickly.
 
Timekeeping:
Despite warnings on icebergs, the ship continued to steam at full speed, which was standard practice at the time.
Ice warnings were typically seen as advisories with reliance placed upon lookouts and it was generally believed that ice posed little danger to large vessels.
 
There were too few lifeboats: 
This did not cause the sinking but contributed to the high death toll.
The 20 lifeboats onboard were enough for 1,178 people—about half the number onboard, and one third of Titanic’s total capacity— which was still in excess of the 1,060-person capacity under the maritime safety regulations of those days.
Four of those boats were collapsible and proved hard to launch during the sinking.
Even worse, the lifeboats launched were eventually only about half-filled, because crewmen worried that the davits would not be able to support the weight of a fully loaded boat.
It is worth noting that the Captain had canceled the ship’s scheduled lifeboat drill earlier in the day of the sinking, and the crew was unaware that the davits had been tested in Belfast.
 
Poor practices onboard: 
Due to drill cancellation, the crew had not been trained adequately in carrying out an evacuation.
Those aboard Titanic were ill-prepared for such an emergency in accordance with accepted practices of the time, as ships were seen as largely unsinkable.
Furthermore, many passengers on the aftermath of the sinking testified to the general confusion on the ship: A general warning was never sounded, causing a number of passengers and even crew members to be unaware of the danger for some time.

The role of the SS Californian

The British steamship SS California has been scrutinized over its inaction as it was the closest ship near the accident area, received the distress signals but failed to respond to them in accordance with law.
After warning Titanic of the ice field, the wireless operator turned off his radio.
About an hour later, the crew of Californian see the rockets but fail to determine their source.
Following controversies, it was determined that the Californian could have saved many, if not all, of the lives that were lost.
However, as the true location of the Californian will likely never be conclusively known, some experts believe it was actually some 20 miles (37 km) away and would not have reached the Titanic before it sank.
 
 
The restaurant reception room of the RMS Titanic / Credit: Shutterstock

Liabilities

More than 60 survivors in US and Britain joined forces to sue the White Star Line for $16,804,112 (about $419 million in 2018 USD), which was far in excess of what White Star argued it was responsible for as a limited liability company under American law.

The company petitioned the US Supreme Court in 1914, which ruled in its favor finding that the causes of the ship’s sinking were largely unforeseeable, rather than due to negligence.
This limited the scope of damages survivors and family members were entitled to, prompting them to reduce their claims to some $2.5 million.
Eventually, White Star only settled for $664,000 ( $16.56 million in 2018),

The settlement was agreed to by 44 of the claimants in December 1915, with $500,000 set aside for the American claimants, $50,000 for the British, and $114,000 to go towards interest and legal expenses.

Lessons learned

The extended media coverage and the subsequent worldwide shock, due to the huge death toll, led to major improvements in maritime safety.
The most prevalent one was the establishment of the International Convention for the Safety of Life at Sea (SOLAS) in 1914, which still governs maritime safety.

The 1914 version was superseded by SOLAS 1929, SOLAS 1948, SOLAS 1960 (the first adopted under the auspices of the IMO) and SOLAS 1974.
SOLAS 1974 is still in force today, but it has been amended and updated many times.

The first International Conference for Safety of Life at Sea was called in London in 1913, drawing up rules requiring that every ship have lifeboat space for each person embarked; that lifeboat drills be held for each voyage; and, because the Californian had not heard the distress signals of the Titanic, that ships maintain a 24-hour radio watch.
In addition, the International Ice Patrol was established to warn ships of icebergs in the North Atlantic shipping lanes and to break up the ice.

Find an explanatory infographic here (Click to enlarge):



Did you know?
Titanic is the second largest ocean liner wreck in the world, only being surpassed by its sister ship HMHS Britannic, but is the largest sunk while in service as a liner, because Britannic was serving as a hospital ship at the time of its sinking.
Titanic sinking was the deadliest peacetime sinking of a superliner or cruise ship to date.
Two special survivors were the stewardess Violet Jessop and the stoker Arthur John Priest, who survived the sinkings of both Titanic and HMHS Britannic and were aboard RMS Olympic when she was rammed in 1911.
As passengers waited to enter lifeboats, they were entertained by the Titanic’s musicians, until shortly before the ship sank.
None of them survived the sinking.
 
Links :

Wednesday, April 29, 2026

China publishes maps detailing minerals on the ocean floor

 
A Chinese submersible in the South China Sea in 2017 during exploration for seabed mineral resources.
Credit... Liu Shiping/Xinhua, via Alamy

From NY Times by  Sachi Kitajima Mulkey

The new deep-sea atlas underscores Beijing’s interest in ocean mining, its military ambitions and its claims to disputed waters.


A research arm of the Chinese government said it had published an atlas of deep-sea mineral deposits, highlighting Beijing’s ambitions to mine the ocean floor and underscoring its disputed claims to waters that neighboring nations consider theirs.

Experts say the maps, in addition to pinpointing mineral deposits found in the deep ocean, give China’s military a thorough understanding of the seafloor in strategically important waters, providing an advantage if submarine warfare were to break out.

The announcement this month by the China Geological Survey puts pressure on other countries that have been ramping up their own seabed mining efforts, in part to reduce their dependence on China for critical minerals and rare earth elements.
Ocean sediments are rich in valuable resources including cobalt, nickel, and manganese.

“China is pouring enormous resources in an effort to emerge as a world-leading oceanographic power,” said Bruce Jones, a naval affairs and foreign policy expert at the Brookings Institution.
The United States historically dominated in ocean-science fields, he said.
Now, China is closing the gap, increasing China’s military capabilities and equipping it with the knowledge needed to fight underwater, Dr. Jones said.

With mapping of this nature, “you can use it for science, and you can use it for warfare,” Dr. Jones said.
“It’s a rare-earth play, it’s a scientific play, and it’s a strategic play all at once,” he said.

The atlas, according to materials published on the China Geological Survey website, maps the locations and concentrations of dozens of resources, drawing from two decades of research and samplings at more than 10,000 locations.
The China Geological Survey said the atlas included the East China Sea and the Yellow Sea, where China claims territory that neighboring nations consider theirs.

China controls most of the world’s supply of key critical metals and rare earths, which are essential ingredients in modern weapons and technologies, and the Chinese government recently approved a five-year plan that lists the development of deep-sea minerals a priority.
China has used its dominance to political ends, for example by restricting exports to the United States and Japan during disputes with those countries.

Japan is developing its own seabed mining program, in part to reduce its reliance on Chinese supplies.
In February, the government said it had successfully retrieved mud rich in rare earths from depths of more than 6,000 meters, an achievement that Japan’s prime minister, Sanae Takaichi, hailed as a “world’s first.” Japan and the United States have made commitments to support each others’ seabed mining projects.

The Trump administration has made seabed mining a priority.
It hopes to issue mining leases near Pacific Ocean territories like American Samoa.
It is also plans to permit commercial miningoutside of U.S. territorial waters without international approval.
China’s mining atlas has strategic importance in bolstering its claim for disputed waters, according to Yun Sun, who leads a Chinese foreign policy program at the Stimson Center, a foreign affairs research organization in Washington.
There are a number of international law customs that determine national boundaries.
Consistently occupying and managing a territory can strengthen a country’s claim to it.
That means nonmilitary actions, like science and conservation, can be used to exert authority over an area, Dr.
Sun said.
Publicly announcing the atlas could be interpreted as China making a statement that it commands this maritime domain.

Chinese deep-sea exploration ships have been spotted in the territorial waters of other countries, such as near the Aleutian Islands in Alaska.
China has also reportedly tested seabed mining equipment in waters that Taiwan and the Philippines claim.

Detailed mapping also helps countries claim additional seafloor, said Larry Mayer, director of the Center for Coastal and Ocean Mapping at the University of New Hampshire.
The United Nations Convention on the Law of the Sea sets a boundary of 200 nautical miles from a nation’s coastline as an “exclusive economic zone” where it has special rights over resources, but a country can claim more seabed if it can prove that its continental shelf extends beyond this zone.
This has been a significant driver of ocean exploration efforts, Dr.
Mayer said.
In 2023, the United States made public detailed maps made over the previous decade claiming about 380,000 square miles of expanded continental shelf, including in the Arctic, the Gulf of Mexico, and the Atlantic and Pacific Oceans.
China has also presented proposals to the United Nations to extend its claim to the continental shelf, based on geological map evidence, drawing borders that Japan disputes as overlapping with its exclusive economic zone.

In the South China Sea (which the atlas does not cover), China has redrawn boundaries in waters also claimed by Taiwan, Vietnam and the Philippines and has taken other steps, including building artificial islands, to support its claims.
Seabed mining is controversial.
Critics say not enough is known about deep-sea environments to safely mine them.
Research shows that mining would reduce the abundance of deep-sea animals and that ecosystems are slow to recover.
Numerous countries as well as environmental organizations have called for moratoriums or an industry ban.
 
Links :

Tuesday, April 28, 2026

Korea-Japan 'East Sea' dispute enters new phase as IHO adopts Digital Standard Society

 
The Greenwich Observatory labels the body of water as the Sea of Japan rather than the East Sea.
Courtesy of Professor Seo Kyoung-duk's team


 
From Seoul Economic Daily by Kim Do-yeon
 
The International Hydrographic Organization (IHO) has adopted a digital standard that identifies seas by unique numerical codes rather than names, a move expected to weaken Japan's long-standing claim to the sole use of "Sea of Japan."

According to the Ministry of Oceans and Fisheries on Wednesday, the IHO officially adopted the digital nautical chart dataset "S-130" at its Fourth Assembly held in Monaco from November 19 to 23.
The decision follows the organization's 2020 resolution at its Second Assembly to develop S-130 as a revised version of the existing nautical chart collection "Limits of Oceans and Seas (S-23)."

S-130 is a new digital nautical chart standard that identifies sea areas by unique identification numbers instead of names.
The key change is a shift from a name-based system to a numerical system suited for electronic navigation and geographic information systems (GIS).
Each sea area will be assigned a unique number combining the latitude and longitude of its center point, meaning seas will be managed under what amounts to an "identification number system."

"This is currently in its early stage, and after the IHO lays the groundwork, the system will be gradually refined to become operational," a Ministry of Oceans and Fisheries official said.
As a result, the existing standard nautical chart collection S-23 will remain only as a reference material from before the digital transition.
A map uploaded on the Voluntary Agency Network of Korea (VANK) website shows the body of water between Korea and Japan labeled as the East Sea.
Captured from VANK
The adoption of the new standard is also the result of the Korean government's continuous efforts to raise the issue and engage in diplomatic outreach in response to the sole designation of "Sea of Japan" in S-23.
Korea and Japan have long been in conflict over the naming of the sea area east of the Korean Peninsula.
When the IHO compiled S-23 in 1929, Japan registered the sea area as the "Sea of Japan," but Korea, then under Japanese colonial rule, was unable to participate in the naming process.

Since then, discussions have continued based on the principle of dual naming in the absence of agreement between the parties, but no consensus has been reached due to differences between the two countries.
However, with the introduction of S-130, sea names themselves will no longer be used in the future digital standard system, bringing the long-standing "East Sea dual naming" debate into a new phase.

Experts say the nature of the competition is fundamentally changing.
Under the previous S-23 system, the key question was which name to display.
Going forward, how a particular name is presented within the data structure has become the more important issue.

"The goal should now be to design a structure in which the East Sea is continuously exposed," said Park Chang-gun, a professor of Japanese Studies at the School of East Asian International Studies at Kookmin University.
"Rather than focusing on dual naming through diplomatic persuasion, the key task is to ensure that the East Sea naturally appears through data structures and standardization rules."

"We need to strengthen our capacity to participate in international standard governance in order to secure a position that can influence decision-making and design," Park added.
"Since the actual impact of place-name designation is determined on platforms such as Google Maps and marine information systems, cooperation with global platforms is also essential."

He also said, "We need to develop a strategy for taking the lead in standards and structures amid the low-intensity competition with Japan."
 
Links : 

Monday, April 27, 2026

British Isles & misc. (UKHO) layer update in the GeoGarage platform

26 new edition on nautical raster charts

Strongest El Niño in a century? What this rare phenomenon could bring.

 
Dramatic ocean warming expected across the Pacific could lead to one of the strongest El Niño events on record this year. (Ben Noll/The Washington Post; data source: ECMWF)
 
From WP by Ben Noll

This year’s potential super El Niño is looking increasingly likely to have wide-reaching climate impacts that last into 2027.

 The chances for a planet-warming super El Niño this year are rising, according to an updated model forecast issued Sunday.
The latest ECMWF outlook indicates there’s a high chance for a supercharged version of the climate pattern that affects regional-to-global weather patterns this summer or fall, doubling down on a super El Niño prediction from last month.

During a typical El Niño, a warming patch of water in the equatorial Pacific Ocean influences what regions experience droughts, floods, extreme heat, hurricanes and declining sea ice. During relatively rare super El Niño events, happening once every 10 to 15 years on average, the effects may be stronger, more persistent and more widespread.

That’s because sea temperatures in that key region of the Pacific Ocean warm more than 2 degrees Celsius (3.6 degrees Fahrenheit) above average, leading to a strong atmospheric response — typically peaking in December or January.

For example, the Western United States, parts of Africa, Europe and India could face a hotter-than-average summer, some tropical countries, such as those in the Caribbean and Indonesia could face worse drought and extreme heat, while more tropical cyclones could develop in the Pacific, with fewer in the Atlantic.
This possible super El Niño could also push global temperatures to record levels, particularly in 2027, and have agricultural impacts as weather patterns change.
“Real potential for the strongest El Niño event in 140 years,” wrote Paul Roundy, a professor of atmospheric science at the State University of New York at Albany.

 
A super El Niño event is forecast to develop by this fall, causing significant weather-related impacts across the planet. 
(Ben Noll/The Washington Post; data source: ECMWF)

Global impacts from a super El Niño
 
 SST anomalies

This year’s potential super El Niño seems increasingly likely to have wide-reaching climate impacts that last into 2027.

It could break the record for El Niño intensity set in December 2015, when sea temperatures in the central equatorial Pacific reached 2.8 degrees Celsius (5.04 degrees Fahrenheit) above average.
Still, even as some signs point to a potent event, including a rare triplet-cyclone pattern brewing in the Pacific, uncertainty remains as to how strong this year’s El Niño will become. Furthermore, no two El Niño events are alike — especially as the climate warms — but past experiences can be used to help plan and prepare.
Here are some of the weather impacts predicted to unfold through at least October, according to the newest model outlook.

 
El Niño will influence areas of drought and downpours across the planet later this year.
(Ben Noll/The Washington Post; data source: ECMWF)
  • Reduced hurricane activity in the Atlantic Ocean and possible drought in the Caribbean islands. Increased hurricane and typhoon risk in the Pacific Ocean, including Hawaii, Guam and much of eastern Asia.
  • Potential drought in central and northern India, suppressing rainfall from that region’s monsoon season, which could impact agricultural production.
  • Above-average summer temperatures and humidity in the Western United States, possibly coming with unusual downpours, which may reach into the Plains and extend severe thunderstorm season.
  • Developing droughts in portions of Central Africa, Australia, Indonesia, the Philippines, some South Pacific islands, Central America and northern Brazil, particularly later in the year. Flooding downpours in Peru and Ecuador, parts of northern and eastern Africa, the Middle East and near the equator in the Pacific.
  • Higher frequency of heat waves across large parts of South America, the southern United States, Africa, Europe, parts of the Middle East, India and eventually Australia.
  • New global temperature records — especially in 2027 — probably breaking records set in 2024.

 
Well above-average temperatures are forecast across swaths of the planet later this year while El Niño is forecast to intensify.
(Ben Noll/The Washington Post; data source: ECMWF)

The strongest El Niño events almost always cause a record-warm year. That’s because heat comes out of the ocean during El Niño, overspreads the tropics in the Pacific, then gets redistributed across the planet by changes in the jet streams.
This could contribute to milder winter temperatures in the United States — and big storms along the West Coast — as the impacts of El Niño reach a peak from the end of the year into early 2027.

As the planet warms, El Niño behaves differently

Strong El Niño periods often appear as an upward stairstep in long-term plots of global temperatures.
“Due to the increasing concentration of greenhouse gases, the climate system cannot effectively exhaust the heat released in a major El Niño event before the next El Niño comes along and pushes the baseline upward again,” Defense Department meteorologist Eric Webb said.
Therefore, a super El Niño in 2026-27 would disperse more heat than other events in 1982-83, 1997-98 and 2015-16.

 
Sea surface temperature anomalies during the formative stages of four El Niño events show how much more warm water there is in 2026 compared to past years.
(Ben Noll/The Washington Post; data source: NOAA/OISST)

Not only would a super El Niño spread unusual heat and humidity far and wide, but it may also spark record atmospheric moisture flows-, which drive downpours that raise the risk for floods. That’s because a warmer atmosphere has a higher moisture-carrying capacity.