When the mercury rises in the UAE during the summer, the last things residents expect to see falling from the sky are hailstones – but they have appeared this week.
Social media users in Al Ain have posted videos of hailstones that appear to be sized somewhere between a pea and a golf ball.
The sudden flurry created an unlikely winter wonderland at the height of another sizzling summer in the UAE desert.
It came amid a spell of cloudy weather and rain that primarily affected Abu Dhabi and Al Ain.
Why are we seeing hail in the summer and why are updrafts important?
Crucial to the formation of hail are updrafts of air, which keep ice particles suspended in the atmosphere and allow them to grow into hailstones before they fall to Earth.
Surprisingly, the conditions that are ideal for hailstone formation are more likely to be seen in summer in the UAE.
“With warmer temperatures, the updrafts are stronger and sustained in time,” said Dr Diana Francis, an assistant professor and head of the Environmental and Geophysical Science (Engeos) Lab at Khalifa University in Abu Dhabi.
“That’s why the UAE witnesses hailstones when convective clouds occur during summer, when the temperatures are very high.
“The warm air naturally rises up, which fuels and maintains strong updrafts within the convective clouds.”
David Schultz, a professor of synoptic meteorology at the University of Manchester in the UK, said a number of factors, including a weather front or a sea breeze, could create an updraft capable of keeping ice particles in the atmosphere to form hail.
“What you need to start that updraft is usually a convergence of air coming from various locations. There are a number of ways that could happen,” he said.
The terrain could also cause an updraft, he said, with mountains able to cause the air movement required.
How do hailstones form and grow?
According to US space agency Nasa, the starting point for hailstones can be aggregated ice particles, known as graupel, or frozen raindrops.
The water exists in frozen form because temperatures 5km or 6km up in the atmosphere are below freezing, said Prof Schultz.
“Any cloud producing rain or snow at the surface of the middle or high latitudes … will start out as ice or snow,” he said.
“The conditions that form hail – you will have very strong updrafts into these clouds.”
“You can imagine that [hailstones] several centimetres across require even stronger [updrafts] in the atmosphere to keep [them] suspended in the air,” Prof Schultz said.
Dr Francis said that large hailstones were the result of several down-and-up movements of the hail that had initially formed within a cloud.
“They get tossed back up to the top of the storm by another updraft,” Dr Francis said. “Each trip above and below freezing adds another layer of ice until the hail becomes heavy enough to fall down to the surface.”
Nasa notes that each hailstone can experience both dry growth, when their surface remains dry, or wet growth, when a water-ice mesh forms. The combination creates a layered internal structure.
Why don't hailstones melt as they fall to Earth?
Eventually the hailstones become so large and heavy that the updrafts cannot keep them suspended any longer and they fall to Earth.
“Because they're falling quite rapidly, several metres per second, they can fall relatively quickly before they have time to melt,” Prof Schultz said.
He said hailstones could fall even in equatorial regions, as long as there was a strong enough updraft and they fell too fast to melt on the way down.
According to Nasa, hailstones are typically about 1cm in diameter, but some as large as 15cm in diameter have been recorded.
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The biog
Nickname: Mama Nadia to children, staff and parents
Education: Bachelors degree in English Literature with Social work from UAE University
As a child: Kept sweets on the window sill for workers, set aside money to pay for education of needy families
Holidays: Spends most of her days off at Senses often with her family who describe the centre as part of their life too
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This article is part of a guide on where to live in the UAE. Our reporters will profile some of the country’s most desirable districts, provide an estimate of rental prices and introduce you to some of the residents who call each area home.
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A comparison of sending Dh20,000 from the UAE using two different routes at the same time - the first direct from a UAE bank to a bank in Germany, and the second from the same UAE bank via an online platform to Germany - found key differences in cost and speed. The transfers were both initiated on January 30.
Route 1: bank transfer
The UAE bank charged Dh152.25 for the Dh20,000 transfer. On top of that, their exchange rate margin added a difference of around Dh415, compared with the mid-market rate.
Total cost: Dh567.25 - around 2.9 per cent of the total amount
Total received: €4,670.30
Route 2: online platform
The UAE bank’s charge for sending Dh20,000 to a UK dirham-denominated account was Dh2.10. The exchange rate margin cost was Dh60, plus a Dh12 fee.
Total cost: Dh74.10, around 0.4 per cent of the transaction
Total received: €4,756
The UAE bank transfer was far quicker – around two to three working days, while the online platform took around four to five days, but was considerably cheaper. In the online platform transfer, the funds were also exposed to currency risk during the period it took for them to arrive.
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- To encourage refugees to integrate the government will encourage them to out of the core protection route wherever possible.
- Under core protection there will be no automatic right to family reunion
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Notable salonnières of the Middle East through history
Al Khasan (Okaz, Saudi Arabia)
Tamadir bint Amr Al Harith, known simply as Al Khasan, was a poet from Najd famed for elegies, earning great renown for the eulogy of her brothers Mu’awiyah and Sakhr, both killed in tribal wars. Although not a salonnière, this prestigious 7th century poet fostered a culture of literary criticism and could be found standing in the souq of Okaz and reciting her poetry, publicly pronouncing her views and inviting others to join in the debate on scholarship. She later converted to Islam.
Maryana Marrash (Aleppo)
A poet and writer, Marrash helped revive the tradition of the salon and was an active part of the Nadha movement, or Arab Renaissance. Born to an established family in Aleppo in Ottoman Syria in 1848, Marrash was educated at missionary schools in Aleppo and Beirut at a time when many women did not receive an education. After touring Europe, she began to host salons where writers played chess and cards, competed in the art of poetry, and discussed literature and politics. An accomplished singer and canon player, music and dancing were a part of these evenings.
Princess Nazil Fadil (Cairo)
Princess Nazil Fadil gathered religious, literary and political elite together at her Cairo palace, although she stopped short of inviting women. The princess, a niece of Khedive Ismail, believed that Egypt’s situation could only be solved through education and she donated her own property to help fund the first modern Egyptian University in Cairo.
Mayy Ziyadah (Cairo)
Ziyadah was the first to entertain both men and women at her Cairo salon, founded in 1913. The writer, poet, public speaker and critic, her writing explored language, religious identity, language, nationalism and hierarchy. Born in Nazareth, Palestine, to a Lebanese father and Palestinian mother, her salon was open to different social classes and earned comparisons with souq of where Al Khansa herself once recited.
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