Eager
to get in on all the hurricane action, the British tabloid press screamed of
“DOUBLE HURRICANE HELL” as weather models showed the remnants of Hurricanes
Maria and Lee merging to form a “Giant Atlantic SUPERSTORM.”
Apart
from the fact that, as you may suspect, this apocalyptic vision is somewhat
oversold – it’ll just be a tad windy and wet over the UK for a day or two – it
is actually possible for two hurricanes to merge.
There’s
not much point in worrying about Maria and Lee, though; right now, they’re
non-threatening Tropical Storms or just fairly insignificant depressions that
will peter out over the next few days. What does happen when hurricanes
collide, though?
Cyclonic
mergers are described by the Fujiwhara effect, named after the Japanese
meteorologist who first described such a phenomenon back in 1921, using water
vortices as an example.
When two cyclones get near each other, they will engage
in a bit of ballet, pirouetting around each other either in a counterclockwise
direction (in the Northern Hemisphere) or clockwise (in the Southern
Hemisphere).
Eventually,
they will begin to spiral in towards a central point. This happens for one of
two reasons: either diverging winds essentially push them together, or because
of something called positive vorticity advection, which describes how regions
of high spin (hurricanes, for example) migrate towards areas of low spin (the
space between the two).
Meteorological term-o-the-day: #Fujiwhara Effect - The tendency of two nearby tropical cyclones to rotate cyclonically about each other. pic.twitter.com/UCnsy0MGuc— NWS Spokane (@NWSSpokane) July 27, 2017
The
hurricane with a larger vortex – the more powerful one – will often dominate
proceedings, and the smaller hurricane will dance around it for a bit, before
falling into it. What happens afterwards, however, is uncertain.
Normally,
the chaotic interaction of two entirely different tropical storms – whose outer
winds are often going in different directions – means that the merger acts as a
breaker force. This tends to reduce the singular entity’s overall strength and
blasts it into weak remnants.
This
is what appeared to have happened in 2001, when Hurricane Gill interacted with
Hurricane Henriette; Gil was disrupted and broke up, but not before consuming
the remnants of Henriette.
On
other occasions, the hurricane merger can fail and ricochet both to completely
different directions to the paths they were originally on. Back in 1974,
Hurricanes Kristen and Ione met up, but resisted each other and ending up
bouncing apart, with the former being dragged northwest and the latter heading
northeast.
Infrequently,
you get a mix of both. Back in 1995, four tropical waves formed in the
Atlantic, which all eventually became storms – Humberto, Iris, Karen, and Luis.
To some extent, the first three interacted with each other and influenced their
formations and paths. Iris ultimately merged with Karen.
It’s
possible that two tropical cyclones can emerge to become briefly more powerful,
as their combined warm water vapor loads could fuel more precipitation
formation and lower the central pressure even more – but it’s unclear whether
this has ever happened in real life.
What’s
more likely is that a hurricane dances around a stronger one, fails to merge,
and as a result gets stronger itself. This took place in 2014, when TropicalStorm Karina spun around Hurricane Lowell and became a hurricane for some time
– before eventually being cannibalized by Hurricane Marie.
Meteorological term-o-the-day: #Fujiwhara Effect - The tendency of two nearby tropical cyclones to rotate cyclonically about each other. pic.twitter.com/UCnsy0MGuc— NWS Spokane (@NWSSpokane) July 27, 2017
In
any case, hurricane mergers are rare. It happens roughly once a year in the
Western Pacific, but once every few years in the Atlantic. This rarity, along
with the fact that they become far more unpredictable when they collide, makes
mergers potentially very dangerous – so it’s a good thing plenty of them result
in a disruptive, rather than an empowering, effect.
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