
A
strong western disturbance over the western Himalayan region caused cloudiness
over northwest and adjoining central India. If snowfall played truant in
Himachal Pradesh on Christmas and New Year's Eve, then it made up for the lapse
with a vengeance. Snow walloped Shimla, Kufri , Narkanda , Chail , Manali ,
Chamba and Dalhousie.
In
fact the entire tribal belt of Kinnaur, Lahaul and Spiti, Kullu and Chamba
districts witnessed heavy snowfall. Shahpur and parts of Hamirpur among other
places also experienced snowfall and sleet after a gap of more than three
decades. And it's snowing in 'Queen of Hills' Shimla as well. This after 8
years! The minimum temperature recorded in the hill station fell to minus 0.8
degree C.
Dharamsala
received snow after a gap of 35 long years. Located at a height of only 1,350
metre and the abode of Tibetan Buddhist spiritual leader the Dalai Lama, Dharamsala
was totally covered in white, making the town more picturesque. In fact the snowfall was unusually heavy with McLeodganj,
its tiny hamlet, known for its strong British heritage, receiving some of the
heaviest snowfall on record.
Even Nurpur experienced snow. This after 45 years.
But what really took weather forecasters by surprise was heavy snow lower down
in Kangra town. This was after a gap of a whopping 67 years! The peculiarity of
Kangra, Nupur and Dharmasala are that these are foothills where snowfall is not
normally expected because of their low elevation. But Himachal Pradesh is not
complaining. Good amount of snowfall has not only rejuvenated its glaciers, but
also proved beneficial for its tourism industry, with scores of tourists making
a beeline to the hill state. Hotel
accommodation and flights are reportedly fully booked.
It
gets even better. Probably for the first time in the recorded history of
Punjab, several villages of Pathankot and Hoshiarpur districts experienced
snowfall on Saturday morning. The two districts normally experience maximum
temperature of up to 45 degrees Celsius in summer. The Met office however dismissed the event as
a 'freak' happening due to change in wind directions.
Last
Friday, parts of New Delhi and Amritsar woke up to be greeted by a
hailstorm. It is not that hailstorms are
a rarity in these parts of the country. It usually takes place during the
transition period where winter gives way to spring. This is when temperature
rises initially in the southern parts of India, giving rise to thunderstorms
and squally weather, including hailstorms in Northern India. The problem is
that we are not in this transition period and in fact only now entering into
the peak winter season.
So
what could have triggered the hailstorms? My friend, Rajesh Kapadia who
administers the blog Vagaries of the Weather explain that conditions for snow
are a) surface temperatures are below freezing upto 2 deg C b) atmospheric temperatures are below freezing c) air contains a minimum moisture level. Atmospheric temperatures were below freezing
but conditions of surface temperature and minimum moisture levels for snowfall were
not meet to create snow and so the western disturbance impact on New Delhi and
Amritsar probably took the shape of hailstorms. This of course remains a
logical conjecture.

Meanwhile,
more than 3 feet snow received over the past two days closed down Kashmir's
main highway, stranding hundreds of travellers. The snowfall on either side of
the Jawahar tunnel, blocked the only road link, connecting Kashmir to rest of
the country, and traffic has been suspended. Trucks carrying supplies to
Kashmir haven't moved a bit in the past three days because the Jammu-Srinagar
highway that connects the Valley with the rest of India is closed due to heavy
snowfall and landslides.
The
heavy snowfall also knocked out power and telephone lines after the 220
KV-Kishanpur-Pampore and 400 KV Kishanpur-Wagoora transmission lines snapped on
other side of Jawhar Tunnel due to snowfall.
Against the required 950 MW of electric power being supplied to the
valley, the availability this time is pegged at 120-150 MW. Among the available
power, 40-50 MW is being supplied to consumers while rest is being used for
running essential services. The plight of residents made worse as J&K is
already facing shortage of fuel- LPG and kerosene- for cooking and heating
purposes.
Temperatures
at Srinagar plummeted to minus 5.5 degree C, the coldest night in the city this
winter. Due to the extreme cold, water taps in most areas of Srinagar were
frozen in the morning. Picturesque
tourist spot Gulmarg recorded a low of minus 16.5 degree C. Qazigund’s low
dipped to minus 8.4 degree C followed by Kokernag (minus 6.3 degree C), Pahalgam
(minus six degree C) and Kupwara (minus 5.6 degree C).
The
Dal Lake was frozen at many places too. Kulgam town in south Kashmir received 2
feet of snow while Srinagar, around 5
inches of snowfall since last evening. High-altitude areas including the ski
resort of Kupwara district which recorded night temperature of minus 0.3
degrees Celsius, had 14.4mm of fresh snow till early morning.
Pahalgam, received fresh snow of 8cms during
the time while the world famous hill resort in south Kashmir, recorded a low of
minus 1.8 degree C. Kargil district in
Ladakh witnessed the first heavy snowfall of the season with Kargil town
recording 2 inches of snow while Drass had about 3.5 inches on the ground this
morning. Taisuru and Rangdum also recorded 2 inches snowfall. In Leh,
temperatures plunged to minus 18.8 deg C.
India
is experiencing a harsh winter characteristic of a La Niña winter. So how does
rest of the world shape up this winter?
GLOBAL WINTER
Let’s
look at the latest satellite temperature imagery for today.
From
these temperature maps it is evident that most of the extreme cold is confined
to Canada, Russia and Northern China. Winter by and large had been mild in most other
areas within the Northern Hemisphere. So mild that huge swathes of Northern
India are currently colder or at comparable temperature to much of Western
Europe.
The
table illustrates that El Niño-Southern Oscillation (ENSO) by itself is
not sufficient conditions to determine the character of winters within the
Northern Hemisphere. More important is the Arctic Oscillation (AO) Index. The erratic AO can generate strong shifts in the climate patterns that
could overwhelm or amplify La Niña's or El Niño’s typical impacts.
Technically, the Arctic Oscillation is a measure
of atmospheric pressure variations at sea level north of 20N latitude. Whenever
an Arctic high or low develops, it affects weather thousands of miles away.
Last
year the so-called "Arctic
fence" that keeps cold air penned up in the north broke down, allowing
frigid air to spill south. So far that's not happening this winter which should
explain the mild winter at the mid latitudes. However, the AO is a fickle—not
seasonal—phenomenon and can switch erratically between the two modes.

As
seen in the NOAA graph, the AO has been in its positive phase for the last 4
months, being particularly very strong all through December and first week
January this year. The exception was a couple of days around the middle of
October and before Christmas when it briefly flipped to its weakly negative
mode. But each time it showed a strong streak of resilience - rebounding
quickly to its strongly positive mode again.
But
yesterday, it flipped back to its weakly negative mode again as that Northern
India and Pakistan received a snow packing wallop. At the same time, in Europe, Austria found
itself buried under 4 feet of snow, creating chaos and disruption of traffic
and power supply. Snowfall trapped some 15,000 tourists at ski resorts on the
Arlberg Mountain on Friday, and while some roads are open there, others remain
closed. High winds are also whipping the nation, and closed an important rail
line. Most snow has fallen in the western states of Tyrol and Vorarlberg. 52 people were rescued by an army helicopter
there. An important rail line that connects Vienna and Innsbruck with western
Austria and Switzerland was to be closed until Sunday. Two rail lines that
connect western Austria with Germany were also closed.
These
two events may look unconnected but they need not. They occurred the same time as the AO flipped
to it weakly negative mode. But the moot
question is whether a negative AO is just a blip or something longer in
duration?
So
what do weather ensemble models indicate? As seen in the above graph, some show the AO index rebounding and
going positive while others (the majority) have it trending negative and ending
below zero.
Two
weathermen think on similar lines. On Twitter, former Accuweather and now with WeatherBell,
legendary weatherman Joe Bastardi observed: “10mb [stratospheric] warming on
European [model] over the pole by 360 hrs reaches 50C!!!! This is a huge event
and will have [northern] hemisphere cold implications…By that I mean, something
major is about to happen.”
Henry
Margusity Accuweather also anticipating a major change similarly observed: “This
is such an amazing weather pattern evolving. I told all the [meteorologists]
that we have a lot of winter ahead of us.”
It
was left to Dave Tolleris of Wxrisk to make a more nuanced statement about a
possible pattern change. He stated: “All
this being said this does NOT mean the winter of 2011-12 is about to turn nasty
for everyone and or the Northeast is going to see big snows or noreasters. …It
might turn that way but we don’t know that yet. But the old winter pattern of
2011-12 that has featured sustained warm/ mild dry pattern is going to end
soon. And whatever the new pattern … won’t be the same as what the last 45-60
days have been.”
“Much of the excitement by Bastardi and
Margusity probably stems from a strong stratospheric warming event that is now
showing up on the model guidance and how it might lead to more blocking and a
negative Arctic Oscillation (AO). Remember, a negative AO means a cold and
sometimes snowy weather pattern over the eastern U.S...
The pattern change ideas stem from research by Baldwin
and Dunkerton published in a 2001 “Science” article which documents how there is
coupling between the stratosphere and troposphere and that sudden stratospheric
warming events can have an impact on the AO (by helping modulate the strength
of the polar vortex), flipping it negative...
That research notes that once the warming propagates
down sufficiently to produce a weather pattern favouring a negative AO (lots of
high latitude blocking), the pattern tends to last for about two months. That
probably explains why some forecasters think that if the AO goes negative it
might stay that way through much of the remainder or the winter....
The potent polar vortex event and positive AO
that has been going on for over two months already appears to be on the wane
with or without help from the stratosphere. This strong vortex event has lasted
longer than most such events so the forecasts of it weakening may have some
merit.”
What all this means is that a big pattern change in winter outlook is due in
the next 7-14 days and the odds favour a strong negative AO. If Europeans and Northern Americans have put
away their woollies and not stocked up on their heating oil, then it is time they
did so in a hurry as a harsh winter is speeding their way and when it does will probably
not go away for the next 2-3 months.
In
India, if you thought that winter would have peaked by month end, you could be
likely to be wrong. Instead, the cold
wave could turn even harsher. Much of the cold wave and snow in the country is
linked to what called western disturbance (WD), which is a term used in India,
Pakistan, Bangladesh and Nepal to describe an extra-tropical storm, originating
in the Mediterranean that brings sudden winter rain and snow to the
northwestern parts of the Indian subcontinent.
This
is a non-monsoonal precipitation pattern driven by the Westerlies. The moisture
in these storms usually originates over the Mediterranean Sea and the Atlantic
Ocean. Extra-tropical storms are a global, rather than a localized, phenomena
with moisture usually carried in the upper atmosphere (unlike tropical storms
where it is carried in the lower atmosphere). Once their passage is hindered by the Himalayas, they are unable to proceed further, and they release significant precipitation over the southern Himalayas. In winter it brings snow and sleet.
As a strong negative AO brings cooling to the Mediterranean Sea and the Atlantic Ocean,
this in turn creates stronger WDs that in turn create higher likelihood of
snow, sleet and plunging temperatures.
Then again, the AO is so unpredictable and could prove everyone wrong.
This place is the best to stay while spending holiday seasons.
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