<p>A surprising phenomenon has emerged in the mighty Himalayas that might slow down the effects of the global climate crisis. Scientists have noted that when high temperatures hit high-altitude ice masses, ‘katabatic’ winds are triggered that blow cold air to lower-altitude areas.</p>

<p>The study, published in the journal Nature Geoscience, was conducted using data from the Pyramid International Laboratory/Observatory climate station on Mount Everest, the world’s tallest summit.</p>

<h2><strong>What are katabatic winds?</strong></h2>

<p>According to Francesca Pellicciotti, professor of glaciology at the Institute of Science and Technology Austria and lead author of the study, a temperature gap is created between the air flowing above the mountains and the cooler air directly in contact with ice masses.</p>

<p>“This leads to an increase in turbulent heat exchange at the glacier’s surface and stronger cooling of the surface air mass,” she said.</p>

<p>As the warm air gets cooler and denser, it sinks, triggering the katabatic winds in neighbouring areas down the slope.</p>

<p><strong>Watch:&nbsp;COP28 Summit: 200 countries to hash out solutions for climate change</strong></p>

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<p>While this phenomenon may slow down the effects of global warming in some areas, its sustainability is not guaranteed over the coming decades.</p>

<p>However, studying the impact of this phenomenon becomes vital and significant as the Himalayan mountain range feeds into 12 rivers that provide fresh water to nearly 2 billion people in 16 countries.</p>

<h2><strong>Concerns</strong></h2>

<p>Scientists noted that this phenomenon doesn’t stop the melting of the glaciers due to climate change.</p>

<p>A June report previously covered by CNN showed that glaciers in the Himalayas melted 65 per cent faster in the 2010s compared with the previous decade, a trend highly unlikely to change its course.</p>

<p>“The main impact of rising temperature on glaciers is an increase of ice losses, due to melt increase,” said Fanny Brun, a research scientist at the Institut des Géosciences de l’Environnement in Grenoble, France. She was not involved in the study.</p>

<p><a href="https://www.wionews.com/india-news/himalayas-are-not-alps-uttarkashi-tunnel-mishap-is-a-reminder-not-to-mess-with-worlds-youngest-mountains-660743"><strong>Also read:&nbsp;`Himalayas are not Alps`: Uttarkashi tunnel mishap is a reminder `not to mess` with world`s youngest mountains</strong></a></p>

<p>Thomas Shaw, who is part of the ISTA research group with Pellicciotti, said there are various complexities involved behind the reasons for ice melting.</p>

<p>“The cooling is local, but perhaps still not sufficient to overcome the larger impact of climatic warming and fully preserve the glaciers,” Shaw observes.</p>

<p><em>(With inputs from agencies)</em></p>


A surprising phenomenon has emerged in the mighty Himalayas that might slow down the effects of the global climate crisis. Scientists have noted that when high temperatures hit high-altitude ice masses, ‘katabatic’ winds are triggered that blow cold air to lower-altitude areas.

A surprising phenomenon has emerged in the mighty Himalayas that might slow down the effects of the global climate crisis. Scientists have noted that when high temperatures hit high-altitude ice masses, ‘katabatic’ winds are triggered that blow cold air to lower-altitude areas. The study, published in the journal Nature Geoscience, was conducted using data from the Pyramid International Laboratory/Observatory climate station on Mount Everest, the world’s tallest summit. What are katabatic winds? According to Francesca Pellicciotti, professor of glaciology at the Institute of Science and Technology Austria and lead author of the study, a temperature gap is created between the air flowing above the mountains and the cooler air directly in contact with ice masses. “This leads to an increase in turbulent heat exchange at the glacier’s surface and stronger cooling of the surface air mass,” she said. As the warm air gets cooler and denser, it sinks, triggering the katabatic winds in neighbouring areas down the slope. Watch: COP28 Summit: 200 countries to hash out solutions for climate change × While this phenomenon may slow down the effects of global warming in some areas, its sustainability is not guaranteed over the coming decades. However, studying the impact of this phenomenon becomes vital and significant as the Himalayan mountain range feeds into 12 rivers that provide fresh water to nearly 2 billion people in 16 countries. Concerns Scientists noted that this phenomenon doesn’t stop the melting of the glaciers due to climate change. A June report previously covered by CNN showed that glaciers in the Himalayas melted 65 per cent faster in the 2010s compared with the previous decade, a trend highly unlikely to change its course. “The main impact of rising temperature on glaciers is an increase of ice losses, due to melt increase,” said Fanny Brun, a research scientist at the Institut des Géosciences de l’Environnement in Grenoble, France. She was not involved in the study. Also read: `Himalayas are not Alps`: Uttarkashi tunnel mishap is a reminder `not to mess` with world`s youngest mountains Thomas Shaw, who is part of the ISTA research group with Pellicciotti, said there are various complexities involved behind the reasons for ice melting. “The cooling is local, but perhaps still not sufficient to overcome the larger impact of climatic warming and fully preserve the glaciers,” Shaw observes. (With inputs from agencies)

Scientists stunned as Himalayas get cooler despite global climate crisis

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