The real tragedy of cyclone ‘Thane’ which hit south west Tamil Nadu on 30 December is that it has already been forgotten by the media.Yet, over 50 lives have been lost, an estimated one million people (yes, one million) have been affected: a whopping 200,000 homes destroyed, hundreds of fishing boats lost and tens of thousands of hectares of crops damaged.The Development Promotion Group (DPG), a Chennai based NGO immediately sent out a team to assess what they could do to help. DPG blends an experience that combines long-term development work with quick and effective response to disasters. They are a well established NGO, having worked in South India since 1986 and on several occasions responded to disaster situations – including the tragic Tsunami of 2004. Today, DPG launched its appeal for long term rehabilitation work.
Wednesday, January 11, 2012
Our December 15th post Winter may have had a mild start but likely to be progressively harsh appears to be turning out prophetic. Big pattern changes in the global weather are on the way and we in India during the last few days got just a small taste of things to come during the last few days.
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 WINTERLet’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.”The Washington Post’s blog, Capital Weather blog reacting to these twitter posts:“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.taken from http://devconsultancygroup.blogspot.com
RT @sankararaman: Heavy rain between ambattur and ashok ngr
RT @raj_ab: Choolaimedu pa :) RT @weatherofindia: @raj_ab >> raining ! Where in chennai, pls update. Thanks
Nagercoil - Heavy rain now 1:20pm in town (Kanyakumari district, S. extreme Tamilnadu)
Day temperatures were below normal by 5 to 8 C over Haryana, Uttar Pradesh, W.Madhya Pradesh, Bihar, Gangetic Bengal, N.Orissa and Gujarat
Visibility would reduce to 200 m or less in dense fog in morning hours over some
parts of E. Uttar Pradesh and Bihar during next 2 days
parts of E. Uttar Pradesh and Bihar during next 2 days
As N-E Monsoon current has gone down, From today, No more easterlies will travel across Bay and reach Tamilnadu
Moisture is drifting South along S-E peninsula coast.. on 10-Jan, Vijayawada records 7cm !