'Zombie'
Hurricane Leslie to finally unravel in Portugal, Spain this weekend
12
October, 2018
Leslie
has held on like a zombie in the Atlantic since September, but the
wandering in the ocean may come to an end well before Halloween.
Leslie
has been meandering the Atlantic since it first formed on Sept. 23.
Through
Friday, Oct. 12, Leslie has stayed between 30 and 65 degrees west
longitude well away from any land or island areas and has survived on
warm waters and moisture over the middle of the Atlantic.
The
tropical cyclone has been bumped around by weather systems passing by
over the North Atlantic but has not encountered a strong enough
system to thrust the storm toward land.
Now,
all of that may change as a non-tropical feature is forecast to pull
Leslie eastward and allow the storm to break out of the central
Atlantic region, where it has been trapped for weeks.
"The strong front moving through the United Kingdom could pull Leslie towards Europe by early next week," said AccuWeather Meteorologist Tyler Roys.
Seas
and surf in this area will build ahead of Leslie's approach starting
with the Azores, Canary Islands and the Island of Madeira.
Leslie
is interacting with some wind shear, likely bringing the storm down
to tropical storm criteria on Saturday as it pushes just north of the
island of Madeira.
Despite
the exact strength of Leslie, waves of heavy rain, as well as gusty
winds will be likely across Madeira, even if there is not direct
landfall.
Increasingly heavy rain and a uptick in wind gusts are expected to start as early as late Saturday in southern Portugal.
"Wind
gusts of 65 to 80 km/h (40-50 mph) are possible across southern
Portugal and southwestern Spain, especially near the coasts,"
added Roys.
Torrential
rainfall will also accompany Leslie as it moves from the coast to
inland locations of the Iberian Peninsula. Rainfall amounts of 25-50
mm (1-2 inches) are likely with an AccuWeather Local StormMax™ of
100 mm (4 inches).
The
cities likely to be most affected will be Lisbon to Lagos and Faro,
Portugal, and from Huelva and Seville, Spain, to the Strait of
Gibraltar.
There
is a remote chance that Leslie not only survives the hostile weather
zone but could also drift back to the southward toward the Canary
Islands and western Africa coast.
Should
this be the case, rough seas would still likely affect southern
Portugal and Spain, in addition to Morocco.
If
Leslie makes this southerly turn and avoids land, it could make a run
at the longest-lasting storm in the Atlantic Ocean.
In
order for Leslie to be the longest-lived tropical cyclone on record,
it would have to hold through the third week of October and into the
fourth week of the month. Pacific Hurricane/Typhoon John holds the
record for longevity with 31 days.
There is a chance that Leslie may rival the Atlantic tropical cyclone longevity record. That title is held by the San Ciriaco Hurricane in 1899. The 1899 storm killed thousands of people in Puerto Rico and lasted for nearly 28 days.
Leslie
first formed over the middle of the Atlantic and about 1,145 miles
(1,845 km) west-southwest of the Azores.
During
the first few days of its life, Leslie was a subtropical storm. A
subtropical storm has characteristics of a tropical storm and also a
non-tropical storm.
During
the late afternoon hours on Saturday, Sept. 29, Leslie had acquired
full tropical characteristics.
Early
on Wednesday, Oct. 3, Leslie became a hurricane. However, it would
not be the last time for Leslie to do so.
By
the late afternoon hours on Thursday, Oct. 4, Leslie had weakened to
a tropical storm and would remain as a tropical storm into Tuesday,
Oct. 9.
During
the late evening hours on Oct. 9, Leslie again garnered enough
strength to regain hurricane status.
Leslie
is not the only system tracking through the Atlantic, the lingering
circulation and moisture from Michael,
which caused catastrophic damage in the Florida Gulf Coast,
and Nadine will
be traversing the Atlantic through the weekend.
There is the chance that Michael as a tropical rainstorm may hit part of the same area of Spain and Portugal after Leslie's arrival.
Major
heat wave for northern Europe and the Arctic this weekend
11
October, 2018
Models
agree: northern Europe and the Arctic are in for a major heat wave
this weekend. Temperatures are expected to be up to 10-15 °C above
the long term average for this period!
The
strong ridge and warm air advection ahead of the low pressure area
over the Atlantic (including the upcoming cyclone ‘Callum’) will
result in temperatures well above the long-term average for this
period. Temperatures are expected to soar
10-15 °C above the
1981-2010 average across large parts of northern Europe, as
well as
over northern parts of central Europe. Additional warming is expected
across fjords in western Norway as southeasterly winds produce
significant Foehn effect / warming of the airmass.
Temperature anomaly (2 m temperature) across Europe from Friday to Monday. GFS model. Map: Wxcharts.eu
Additionally,
the warm airmass will push far into the Arctic region, over eastern
Greenland and Svalbard, pushing almost all the way to the North Pole.
Temperature anomaly (2 m temperature) over the northern hemisphere on Sunday. GFS model. Map: Wxcharts.eu
Polar
jet circulation changes
bring Sahara dust to Arctic,
increasing
temperatures,
melting ice
10
October, 2018
Fast
Facts
- A new atmospheric mechanism by which dust travels from the Sahara Desert across the eastern side of the North Atlantic Ocean towards the Arctic has been discovered
- The dust emission was generated by a Saharan cyclone that was triggered by the intrusion of a trough emanating from the polar jet
- The poleward transport of warm dust was caused by a meandering polar jet stream
- Approximately half of the warming in the Arctic is being attributed to increased moisture and heat fluxes transported to the region from lower latitudes
A
new atmospheric mechanism by which dust travels from the Sahara
Desert across the eastern side of the North Atlantic Ocean towards
the Arctic has been discovered
The
dust emission was generated by a Saharan cyclone that was triggered
by the intrusion of a trough emanating from the polar jet
The
poleward transport of warm dust was caused by a meandering polar jet
stream
Approximately
half of the warming in the Arctic is being attributed to increased
moisture and heat fluxes transported to the region from lower
latitudes
Abu
Dhabi, October 10, 2018: Research scientists at NYU Abu Dhabi, along
with other global researchers, have identified a new mechanism by
which warm dust travels from the Sahara Desert to the Arctic Circle,
which has been proven to affect rising temperatures and ice melt in
Greenland.
Their
findings highlight the role that the polar jet and associated
atmospheric circulation plays in the transport of mineral dust from
the Sahara desert to the Arctic across eastern side of the North
Atlantic Ocean.
A
meandering polar jet was discovered as responsible for both the
emission and transport of dust from Northwest Africa to the Arctic.
The emission has been linked to an intense Saharan cyclone that
formed in early April 2011, which was caused by the intrusion of an
upper-level trough emanating from the polar jet.
The
study has found that atmospheric circulation of this nature enables
the transport of dust, warm and moist air masses from subtropics and
mid-latitudes to the Arctic, where approximately half of the warming
is now being attributed to increased
moisture and heat fluxes
transported to the region.
The
warm and moist air masses accompanying the Saharan dust caused a rise
in surface temperature of 10C for more than three consecutive days
upon reaching southeastern Greenland. Subsequent temperature
observations detected increased melting within the ice across this
same area.
"The
polar jet stream has been identified as the main driver for such
events leading
to the transport of large amount of dust to
high-latitudes," said Diana Francis, atmospheric scientist at
NYU Abu Dhabi and lead research scientist in this study.
"If
the polar jet is set to slow more frequently due to the changes in
the Arctic climate system and to the Arctic Amplification, such
events are expected to become more frequent," Francis added.
The
newly discovered poleward route is considered the most substantial in
terms of dust load import into the Arctic, due to the minimal
geographical distance between
the origin point and the destination.
'The
impact of dust deposition on ice in Greenland, such as darkening ice
and formation of algae on ice or cryoconite, as well as the link
between Saharan dust transport and the Arctic heat dome must be
investigated further in collaboration with scientists in UK and
Germany' Francis emphasized.
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