How low clouds shield the planet: and why we’re losing them

Fewer low clouds means lower albedo: the Earth reflects less energy back into space and warms up faster. The disappearance of these "white sentinels" anticipates the worst climate scenarios. This is revealed by a new study coordinated by the Alfred Wegener Institute

At most, it may have brought the world very close to exceeding the fateful threshold of +2.7°F relative to pre-industrial values during 2023-possibly even 2024-and outside the bounds identified for a tolerable Earth. Indeed, this is also often referred to as a ‘red line’ beyond which it has significant and devastating impacts on society and the ecology.

A new puzzle for climate science

With the enormous contribution factors of greenhouse gases build-up, El Niño, and glacial melting, for instance, these would still not fully explain the sudden and marked uprise in global temperatures.

According to a recent study by the Alfred Wegener Institute (AWI), there is suspicion of a previously overlooked culprit: the progressive decrease in certain types of clouds, especially low-altitude clouds. These clouds work like mirrors, reflecting solar radiation back into space. The Earth has apparently lost part of its natural “sunscreen,” causing it to absorb more and more solar energy and thus accelerate global warming.

Unexplained heat: a missing 0.36°F

The focus has traditionally been on increasing amounts of CO₂ and methane, fluctuations in El Niño, volcanic eruptions, and changes in solar output. While these account for a good deal of the warming, about 0.36°F (0.2°C) remains unaccounted for.

AWI researchers, working in cooperation with the European Centre for Medium-Range Weather Forecasts (ECMWF), compared satellite data and climate reanalyses going back to the mid-20th century. Their results indicate that 2023 will set a record low in the Earth’s albedo-the measure of how much sunlight the planet reflects. Though the steady drop in albedo has been attributed to the melting of Arctic and Antarctic ice, the accelerated decrease in the last few years is largely due to a decrease in low-altitude cloud cover-even at much lower latitudes.

Low altitude clouds

@Alfred Wegener Institute

The earth as an imperfect mirror

Consider the Earth as a big, imperfect mirror. Bright surfaces and clouds reflect part of the incoming solar energy back into space. But with fewer bright surfaces and fewer low-level clouds, more energy is retained, and this further feeds warming.

The decline in low-level clouds has been most pronounced over critical areas of the North Atlantic, where marine heatwaves and extreme climate events were off the charts in 2023. Scientists say these phenomena are linked. The decline in low cloud cover and the associated drop in albedo explain a great deal about the mysterious 0.36°F warming gap.

Low clouds: the planet’s cooling shield

While high-altitude clouds can act as a heat trap, they also reflect a significant amount of sunlight back into space, which balances the effect to a large degree. Low-altitude clouds cool the planet mainly by serving as a solar umbrella. Losing them weakens one of our most important buffers against global warming. If this trend represents a feedback loop—where global warming itself reduces low cloud formation, creating a vicious cycle—it’s a big problem.

Why are we losing low clouds?

Several reasons might contribute to the above-mentioned phenomena:

  • Fewer Aerosols: Stringent environmental controls on fuel for ships have resulted in fewer aerosol pollutants. Ironically, these particles facilitate cloud formation and reflect the sun.
  • Natural Variability: Natural variations on short- to medium-term time scales could be contributing to cloud formation.
  • Ocean Currents: Oceanic circulation patterns, which may be altered, are also a probable cause.

The most worrying explanation, however, is climate feedback: a warmer world can’t sustain its low cloud cover, and that accelerates the warming.

A new climate reality?

If these processes continue, the event of always staying above +2.7°F could happen decades earlier than expected, making it impossible to realize the goals of the Paris Agreement. Scientists emphasize the necessity of further research for separating temporary fluctuations from the new normal. Whatever the case, the message is clear: loss of low clouds badly cripples our ability to retard global warming.

Impacts on carbon budgets

The smaller albedo means that the “carbon budgets” of the world-representing the remaining amount of CO₂ we can emit without exceeding critical thresholds-must be recalculated. This dwindling budget shows the need to hasten the energy transition, forsake fossil fuels, and invest in sustainable technologies and practices.

A planet exposed

The Earth is ever more ‘naked’, without such reflecting clouds that block radiation from the Sun. Thus, this understated-yet-profound change tends to press heavy on planetary thermal balance. An atmosphere without these formations will leave its natural interplay of vapor and particles possibly being much more of a heat trap than it is presently.

But it does make a crucial point about one of the most under-discussed elements of climate science: low-altitude cloud cover plays a crucial cog in Earth’s climate system, and to see these clouds disappear is tantamount to removing a sponge that sops up excessive solar energy, accelerating an already dangerous trajectory.

The path forward

Faced with such evidence, the question is no longer whether to curb warming but how. If the skies become less reflective, humanity must compensate with greener solutions, acting swiftly and decisively.

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The world’s largest waterfall is hidden underwater

The largest waterfall in the world is not Niagara or Angel Falls, but is located in the Denmark Strait: a unique underwater phenomenon, unfortunately threatened by climate change

Not many people know that the biggest waterfall in the world lies deeply hidden beneath the ocean. The natural wonder, located in the Denmark Strait between Greenland and Iceland, dwarfs any terrestrial waterfall in height. Here, water tumbles over 10,000 feet from the Greenland Sea into the Irminger Sea—a drop that far surpasses Venezuela’s famed Angel Falls, which stands at around 3,900 feet (1.2 kilometers).

The science behind the Denmark Strait cataract

The unique underwater topography of the Denmark Strait—where the seafloor abruptly drops from 1,600 feet (500 meters) to more than 10,000 feet (3,000 meters) over a relatively short distance—accelerates deep ocean currents. This phenomenon gives rise to the massive underwater waterfall, which cascades into the vast trenches of the North Atlantic Ocean.

The Denmark Strait cataract stretches for an impressive 100 miles (160 kilometers) and carries an astonishing volume of 175 million cubic feet of water per second (5 million cubic meters), about 2,000 times the peak flow of Niagara Falls. When it was discovered in 1989, it stunned the scientific community. The waterfall forms due to differences in water density. Cold water from the northern seas, being denser, sinks beneath the warmer water of the Irminger Sea as the two currents meet. This sinking motion creates an enormous underwater cascade.

Invisible yet powerful

This Denmark Strait waterfall is not visible for the human eye because it happens in the ocean deep; instead, it can only be measured with the use of advanced instruments that show small changes in temperature and salinity. These gradients illustrate the powerful force behind shaping our ocean dynamics.

Climate change and its impact on underwater waterfalls

Underwater waterfall

@123rf

The underwater waterfall of the Denmark Strait is one of the rarest and amazing phenomena, impressive in both size and peculiar mechanism. Though invisible from above the sea, it plays a not-less-important role in keeping the balance of marine ecosystems and Earth’s climate conditions.

Unfortunately, this nature wonder is threatened by global warming. Global warming temperatures and shifts in ocean currents are reducing the volume of cold, dense water driving the waterfall. This change has severe ramifications for the marine ecosystems and the global climate.

 

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