Like atmospheric rivers, but smaller and slower moving, the pools of water vapor bring much-needed rain from the Indo-Pacific to arid regions along the east African coast
16 December 2021
AGU press contact
Liza Lester, +1 (202) 777-7494, [email protected] (UTC-4 hours)
Contact information for the researchers:
Brain Mapes, University of Miami, [email protected] (UTC-4 hours)
NEW ORLEANS—A new meteorological phenomenon has been identified drifting slowly over the western Indian Ocean. Dubbed “atmospheric lakes,” these compact pools of moisture originate over the Indo-Pacific and bring water to dry lowlands along East Africa’s coastline.
Brian Mapes, an atmospheric scientist at the University of Miami who recently noticed and described the unique storms, will present his findings on Thursday, 16 December at AGU’s Fall Meeting 2021.
Like the better-known streams of humid, rainy air called atmospheric rivers that are famous for delivering large amounts of precipitation, atmospheric lakes start as filaments of water vapor in the Indo-Pacific. These phenomena are defined by the presence of water vapor concentrated enough to produce rain, rather than being formed and defined by a vortex, like most storms on Earth. Unlike the fast-flowing atmospheric rivers, the smaller atmospheric lakes detach from their source as they move at a sedate pace toward the coast.
Atmospheric lakes begin as water vapor streams that flow from the western side of the South Asian monsoon and pinch off to become their own measurable, isolated objects. They then float along ocean and coastal regions at the equatorial line in areas where the average wind speed is around zero.
In an initial survey to catalog such storms, Mapes used five years of satellite data to spot 17 atmospheric lakes lasting longer than six days and within 10 degrees of the equator, in all seasons. Lakes farther off the equator also occur, and sometimes those become tropical cyclones.
The atmospheric lakes last for days at a time and occur several times a year. If all the water vapor from these lakes were liquified, it would form a puddle only a few centimeters (a couple inches) deep and around 1,000 kilometers (about 620 miles) wide. This amount of water can create significant precipitation for the dry lowlands of eastern African countries where millions of people live, according to Mapes.
“It’s a place that’s dry on average, so when these [atmospheric lakes] happen, they’re surely very consequential,” Mapes said. “I look forward to learning more local knowledge about them, in this area with a venerable and fascinating nautical history where observant sailors coined the word monsoon for wind patterns, and surely noticed these occasional rainstorms, too.”
Weather patterns in this region of the world have received little attention from meteorologists, limited mostly to studies of rain and water vapor on a monthly rather than day-to-day scale according to Mapes. He is working to understand why atmospheric lakes pinch off from the river-like pattern from which they form, and how and why they move westward. This might be due to some feature of the larger wind pattern, or perhaps that the atmospheric lakes are self-propelled by winds generated during rain production.
These are questions that would need to be answered before Mapes and other researchers can begin to study how climate change could affect atmospheric lake systems. He plans to study these events more closely using satellite data and will look at into the possibility that these atmospheric lakes occur elsewhere in the world.
“The winds that carry these things to ashore are so tantalizingly, delicately near zero [wind speed], that everything could affect them,” Mapes said. “That’s when you need to know, do they self-propel, or are they driven by some very much larger-scale wind patterns that may change with climate change.”
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Notes for Journalists
Brian Mapes will present the results of this work at AGU Fall Meeting 2021. For information about Fall Meeting 2021, including the schedule of press events, visit the online Media Center. Neither the presentation nor this press release is under embargo.
A42B-04 – Long-lived vapor lakes over the Indian Ocean: closest outdoor phenomenon to the self-aggregation paradigm?
A42B – Coupling of Clouds, Convection, and Circulation From Meso- to Planetary Scales I Oral Thursday, 16 December, 9:45 – 11:00 CT.