Tag Archive: India


Earth Watch Report  -  Biological Hazards

12.06.2013 Biological Hazard India State of Odisha, Angul Damage level Details

Biological Hazard in India on Wednesday, 12 June, 2013 at 03:28 (03:28 AM) UTC.

Description
Anthrax scare has gripped Angul district in Odisha with more than 35 people falling ill with suspected symptoms of the disease at Suleipal village under Kaniha block. Fifteen persons have been rushed to the SCB Medical College Hospital while the rest are being treated at the local hospital at Kaniha. All the affected persons are from the same village and are displaying symptoms of cutaneous anthrax infections, like severe lesions or wounds on the skin. “They have been admitted to the isolation ward of the hospital and are under the treatment of a special team of doctors. Though anthrax is yet to be confirmed, the symptoms are typical”, emergency medical officer of the SCBMCH, Dr B M Moharana, said. According to sources, the people are suspected to have contracted the infection from dead animals. The villagers are reported to have consumed meat of about three dead goats. While the cause of the death of the animals could not be ascertained, the people who had partaken the meat have begun to fall ill. The suspected outbreak has become a cause of serious concern because Angul district is known to be non-endemic to the disease.
Biohazard name: Anthrax
Biohazard level: 4/4 Hazardous
Biohazard desc.: Viruses and bacteria that cause severe to fatal disease in humans, and for which vaccines or other treatments are not available, such as Bolivian and Argentine hemorrhagic fevers, H5N1(bird flu), Dengue hemorrhagic fever, Marburg virus, Ebola virus, hantaviruses, Lassa fever, Crimean-Congo hemorrhagic fever, and other hemorrhagic or unidentified diseases. When dealing with biological hazards at this level the use of a Hazmat suit and a self-contained oxygen supply is mandatory. The entrance and exit of a Level Four biolab will contain multiple showers, a vacuum room, an ultraviolet light room, autonomous detection system, and other safety precautions designed to destroy all traces of the biohazard. Multiple airlocks are employed and are electronically secured to prevent both doors opening at the same time. All air and water service going to and coming from a Biosafety Level 4 (P4) lab will undergo similar decontamination procedures to eliminate the possibility of an accidental release.
Symptoms:
Status: confirmed

The Global Dispatch

India: At least 35 people sickened with suspected anthrax in Odisha

Some 35 people in Angul district in Odisha have presented with symptoms consistent with cutaneous anthrax sending fear into the community, according to the New Indian Express today.

Anthrax image/Janice Carr-CDC

Anthrax image/Janice Carr-CDC

All the affected persons are from the same village and are suspected to have consumed meat of about three dead goats. It has not yet been determined if the goats were infected.

Fifteen persons have been rushed to the SCB Medical College Hospital while the rest are being treated at the local hospital at Kaniha.

“They have been admitted to the isolation ward of the hospital and are under the treatment of a special team of doctors. Though anthrax is yet to be confirmed, the symptoms are typical”, emergency medical officer of the SCBMCH, Dr B M Moharana, said.

Anthrax is a pathogen in livestock and wild animals. Some of the more common herbivores are cattle, sheep, goats, horses, camels and deers.

It infects humans primarily through occupational or incidental exposure with infected animals of their skins.

Anthrax is caused by the bacterium, Bacillus anthracis. This spore forming bacteria can survive in the environment for years because of its ability to resist heat, cold, drying, etc. this is usually the infectiousstage of anthrax.

Read Full Article Here

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Reblogged  from   :  Champions for Cetaceans

By Kirsten Massebeau

Ocean day is a day to celebrate our oceans, understand more about them, and take action to help the very bodies of water that give our world life. Part of the amazing underwater world of the oceans are the inhabitants which include dolphins. Highly intelligent with brains as large as mans dolphins remain at the top of the food chain in the ocean. They can easily be categorized as the people of the sea. Dolphin families stay together for a lifetime living in socially complex societies. They recognize themselves in the mirror, and call each other by name. Many scientists today believe that cetaceans deserve status as non-human persons: “They believe dolphins – and their whale cousins – are sufficiently intelligent and self-aware to justify the same ethical considerations given to humans. Recognizing cetaceans’ rights would mean an end to whaling and the captivity of dolphins and whales, or their use in entertainment ”. (source).

Bruges Dolphinarium by Frederich Clemente

Bruges Dolphinarium by Frederich Clemente

Sadly despite the scientific data that deems dolphins unsuitable for captivity the practice continues. Bruges Dolphinarium in Europe is just one example of the terrible dolphin suffering that takes place in Europe and worldwide. Trapped in cement tanks filled with chlorinated water dolphins are forced to spend their lives in suffering for human entertainment, forced to perform tricks for dead fish something that would have never been part of their diet in the wild. In 2005 Toni Frohoff, Ph.D. prepared a report entitled, Report on Observations and Preliminary Assessment at Boudewijn Seapark Dolphinarium in Brugges, Belgium:

Bruges dolfinarium is considered as “substandard”. The fate of our 6 dolphins (more than 30 died Under the Dark Dome) is a good example of cruelty, as Morgan is a good example of commercial cynism of Industry. Dr Toni Frohoff said : “The facility itself appears to be sub-standard compared to many facilities around the world that a) provide a more naturalistic environment for dolphins and b) adhere to international governmental regulations This is especially notable due to the extreme noise and reverberation that is characteristic of an indoor facility (and in particular this one that plays such loud music and encourages loud sounds from the audience as well). In fact, this was the loudest facility of the many that I have visited – and in my opinion, is completely unacceptable and constitutes cruelty to these animals who are well-known for their exquisitely sensitive hearing. Further, the ambient and reverberating noises of the indoor facility pumps and maintenance systems may produce continuous noise from which the dolphins cannot escape” (source)

Many died in the nets as the capture process continued.  By SSCS Cove Guardians December 13th, 2012

Many died in the nets as the capture process continued. Those dolphins unwanted for

captivity were  slaughtered for pet food and human consumption.
By SSCS Cove Guardians December 13th, 2012

Read More Here

18 Signs That Massive Economic Problems Are Erupting All Over The Planet

Volcano Eruption - Mount Redoubt

In fact, a whole bunch of recent polls and surveys show that the American people are starting to feel much better about how the U.S. economy is performing.  Unfortunately, the false prosperity that we are currently enjoying is not going to last much longer.  Just look at what is happening in Europe.  The eurozone is now in the midst of the longest recession that it has ever experienced.  Just look at what is happening over in Asia.  Economic growth in India is the lowest that it has been in a decade and the Japanese financial system is beginning to spin wildly out of control.  One of the only places on the entire planet where serious economic problems have not already erupted is in the United States, and that is only because we have “kicked the can down the road” by recklessly printing money and by borrowing money at an unprecedented rate.  Unfortunately, the “sugar high” produced by those foolish measures is starting to wear off.  We are going to experience a massive amount of economic pain along with the rest of the world – it is just a matter of time.

But for the moment, there are a lot of skeptics out there.

For the moment, there are a lot of people that are declaring that the problems of the past have been fixed and that we are heading for incredibly bright economic times ahead.

Unfortunately, those people appear to be purposely ignoring the economic horror that is breaking out all over the globe.

The following are 18 signs that massive economic problems are erupting all over the planet…

#1 The eurozone is now in the midst of its longest recession ever.  Economic activity in the eurozone has declined for six quarters in a row.

#2 Italy’s economy has now been contracting for seven quarters in a row.

#3 Industrial production in Italy has fallen for 15 months in a row.  It has now fallen to its lowest level in about 25 years.

#4 The number of people that are considered to be “seriously deprived” in Italy has doubled over the past two years.

#5 Consumer confidence in France has just hit a new all-time low.

#6 The number of unemployed workers seeking a job in France has hit a brand new all-time record high.  Many unemployed workers in France are utterly frustrated at this point…

“I’ve sent CVs everywhere, I come to the unemployment agency every day, for 3 or 4 hours to look for work as a truck driver and there’s never anything,” said 42-year old Djamel Sami, who has been unemployed for a year, leaving a job agency in Paris.

#7 Unemployment in the eurozone as a whole has just hit a brand new all-time record high of 12.2 percent.

#8 Youth unemployment continues to soar to unprecedented heights in Europe.  The following is from an article that was recently posted on the website of the Guardian that detailed how bad things are getting in some of the worst countries…

In Greece, 62.5% of young people are out of work, in Spain it’s 56.4%, then Portugal with 42.5%, and then Italy with 40.5%.

#9 Youth unemployment is being partially blamed for the worst rioting that Sweden has seen in many years.  The following is how the Daily Mail described the riots…

Sweden is reeling after a third night of rioting in largely run-down immigrant areas of the capital Stockholm.

In the last 48 hours violence has spread to at least ten suburbs with mobs of youths torching hundreds of cars and clashing with police.

It is Sweden’s worst disorder in years and has shocked the country and provoked a debate on how Sweden is coping with youth unemployment and an influx of immigrants.

#10 An astounding 10 percent of all banking deposits were pulled out of banks in Cyprus during the month of April alone.

#11 Economic growth in India is the slowest that it has been in an entire decade.

#12 Suddenly Australia is experiencing some tremendous economic challenges.  The following quotes are from a recent Zero Hedge article

Read Full Article Here

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Eurozone unemployment reaches new record high in April

The BBC’s Jamie Robertson says the employment figures show “disparity across Europe”

Unemployment in the eurozone has reached another record high, according to official figures.

The seasonally-adjusted rate for April was 12.2%, up from 12.1% the month before.

An extra 95,000 people were out of work in the 17 countries that use the euro, taking the total to 19.38 million.

Both Greece and Spain have jobless rates above 25%. The lowest unemployment rate is in Austria at 4.9%.

The European Commission’s statistics office, Eurostat, said Germany had an unemployment rate of 5.4% while Luxembourg’s was 5.6%.

The highest jobless rates are in Greece (27.0% in February 2013), Spain (26.8%) and Portugal (17.8%).

In France, Europe’s second largest economy, the number of jobless people rose to a new record high in April.

“We do not see a stabilisation in unemployment before the middle of next year,” said Frederik Ducrozet, an economist at Credit Agricole in Paris. “The picture in France is still deteriorating.”

‘Social crisis’

Youth unemployment remains a particular concern. In April, 3.6 million people under the age of 25 were out of work in the eurozone, which translated to an unemployment rate of 24.4%.

Figures from the Italian government showed 40.5% of young people in Italy are unemployed.

Europe’s already dismal jobs situation has deteriorated further. If we needed a reminder of the lingering effects of the eurozone financial crisis, it is to be seen in the jobs data.

The general pattern is that the largest increases in unemployment over the last year were in countries at the centre of the crisis – Greece, Cyprus, Spain and Portugal. There was also a sharp increase in Slovenia, a country seen as a possible future candidate for a financial rescue.

The main exception to the pattern was Ireland, another country receiving a bailout, where unemployment nonetheless fell by almost one and half percentage points in twelve months.

The figures also highlight the “lost generation” concern that is, or should be, causing some lost sleep for political leaders. Unemployment among young people is approaching one in four across the eurozone and it is 40% or higher in a few countries – Greece, Spain, Portugal and Italy.

“We have to deal with the social crisis, which is expressed particularly in spreading youth unemployment, and place it at the centre of political action,” said Italy’s President Giorgio Napolitano.

In the 12 months to April, 1.6 million people lost their jobs in the eurozone.

While the jobless figure in the eurozone climbed for the 24th consecutive month, the unemployment rate for the full 27-member European Union remained at 11%.

The eurozone is in its longest recession since it was created in 1999. At 1.4%, inflation is far below the 2% target set by the European Central Bank (ECB).

Consumer spending remains subdued. Figures released on Friday showed that retail sales in Germany fell 0.4% in April compared with the previous month.

Read Full Article Here

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Greece’s young: Dreams on hold as fight for jobs looms

Mark Lowen looks at the toughest equation Greece has to solve

Greece’s school exam season has arrived. But for many now facing the final-year tests known as the Panhellenics, the stress is twofold: last-minute cramming and the knowledge that they’ll soon enter the worst jobs climate in Europe.

At 64.2%, youth unemployment in Greece is the highest in the continent. Those between the ages of 16 and 25 are now the crisis generation.

At the Spoudi school in Athens, dreams have been put on hold. The school leavers longed for a stable job, for a future full of opportunity. But instead, unemployment and uncertainty beckon.

 

The economy won’t recover because the educated ones will go abroad and only the older people will stay here”

Christina Zahagou Law graduate, 23

In a final maths class, students pore over complex algebra problems. But how to stay positive in today’s Greece might just be the most difficult equation to solve.

“I’m not sure about my future,” says Nathalie Scholden, an 18-year-old who hopes to study economics. “I think I won’t stay in Greece because there’s high unemployment and bad salaries. A lot of kids my age feel the same. If we’re here and nobody gets the life they want, why should we stay?”

Among the other students, few are optimistic. One thinks of leaving Athens for the countryside, another of going into farming because of a lack of opportunities.

“In Greece today you can’t do what you want,” says Alexandros Delakouras, 17. “It will be very difficult to get a job in my country but I will try hard.” He adds with a smile: “Maybe, with God’s help, I’ll succeed.”

Before Greece’s first bailout three years ago – and the spending cuts that ensued – unemployment in the country was under 12%. Now it’s at 27%.

And among the youth, it’s more than doubled from around 31% in May 2010. Recession has hit hard but it’s the austerity demanded by the country’s international lenders that has had such a devastating impact.

Brain drain

Doing the sums

Student studies maths

In Greece, 64.2% of 16 to 25-year olds are out of work

This has risen from 31.2% three years ago when Greece received its first international bailout

The economy is expected to stay in recession for the sixth consecutive year in 2013

Unemployment continues to rise and is not expected to start falling until 2015, the Greek central bank says

And so the brightest, like 23-year-old law graduate Christina Zahagou, are leaving. Greek emigration to Germany jumped by more than 40% last year. She is now following suit after failing to find work.

Read Full Article Here

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Sweden Riots Put Faces to Statistics as Stockholm Burns

A week of riots in Stockholm has torn a hole in Sweden’s image as a beacon of social harmony.

In Husby, a suburb north of the capital where 60 percent of residents were born outside Sweden and unemployment is twice the national average, youths torched cars, schools and other buildings in a show of anger that has unsettled one of Europe’s richest nations. The riots spread to more than 10 other suburbs in Stockholm.

A burning car set on fire in the Stockholm suburb of Kista after youths rioted in several different suburbs around Stockholm for a third executive night, late May 21, 2013. Photograph: Fredrik Sandberg via AP Photo/Scanipx Sweden

People exit Husby subway station to attend a demonstration against police violence and vandalism in the Stockholm suburb of Husby on May 22, 2013. Sweden’s youth unemployment rate was 23.6 percent last year– about three times the national average — according to the statistics office. Photographer: Jonathan Nackstrand/AFP/Getty Images

“Exclusion, poverty and unemployment” are the main causes of the riots, Yves Zenou, a professor at Stockholm University who has done research on urban economics and migration issues, said in a May 24 interview. “They feel excluded from Swedish society. Many are not in employment, many because of discrimination, and many have low education levels.”

The unrest has shocked Sweden, where the economic policies of Prime Minister Fredrik Reinfeldt helped the AAA rated nation emerge as a haven from the debt crisis raging across southern Europe. Yet Sweden’s aggregate wealth has hidden rifts in the economy as polices have failed to catch a demographic now taking to the streets to show its desperation.

Young people need “jobs as well as something to do in their spare time,” Iqra Siddiqui, a 16-year-old living in Hallunda, a suburb in south Stockholm, said yesterday in an interview outside the Skaerholmen subway station. “Another problem is that parents don’t know what their kids are up to.”

Police Detentions

Sweden’s youth unemployment rate was 23.6 percent last year — about three times the national average — according to the statistics office. A report this month by the Public Employment Services showed that about 77,000 people between 16 and 29 years haven’t studied or worked over the past three years, suggesting even larger hidden unemployment. By comparison, youth unemployment was about 153,000 last year, according to the agency.

Police, who as of May 24 had detained 29 people since the riots started on May 19, say most of those involved are about 20 years old. Their plight underscores how Europe’s economic pain is hitting young people hardest. According to Luxembourg-based Eurostat, youth unemployment in the 27-nation European Union reached 23.5 percent in March, versus 16.2 percent in the U.S.

Scenes outside Stockholm this week replayed images of youth unrest across Europe since the global economic crisis started. In 2011, riots that started in north London also spread to Manchester and the Midlands, in the worst youth unrest in the U.K. since the 1980s. Paris has seen similar violence.

‘Ordinary Night’

While unrest also spread to other towns over the weekend, including Oerebro and Linkoeping, violence in the Swedish capital have started to subside.

Last night was like “an ordinary night,” according to police spokesman Kjell Lindgren. Fewer than 10 cars were set on fire and there were no reports of stones being thrown at emergency services and no major vandalism. Between Saturday and Sunday, about 20 cars were set on fire and a school in a southern suburb was vandalized. Rocks were also thrown at police in the Vaarberg neighbourhood.

Reinfeldt, who gained power in 2006 on promises of bringing more people into the labor market, has struggled to carry that pledge over to immigrants and young adults. In Husby, an area dotted by concrete high rises, the number of people relying on state assistance is more than triple the average for Stockholm.

Sweden has suffered similar episodes of violence before, including in the southern city of Malmoe in 2008 as well as Gothenburg.

The Cause

Megafonen, a Husby advocacy group, traces the outbreak of Stockholm’s riots to the police shooting of a local 69-year-old man originally from Portugal. Police brutality and racist slurs have exacerbated tensions, the group says.

Dagens Nyheter, Sweden’s largest daily newspaper, has questioned those claims, as a columnist asked for specific examples of brutality and proof of racial insensitivity. The newspaper reported on May 24 that about half the people arrested on suspicion of rioting in Husby came from outside the neighborhood, and half of them had criminal records.

In response, the advocacy group posted witness accounts of police brutality and racism on its website.

“Megafonen doesn’t start fires, we don’t believe this is the right method for long-term change,” said the group. “But we know that it’s a reaction to deficiencies in society. Unemployment, inadequate schools and structural racism are reasons behind what we are seeing today.”

Small Group

The largest immigrant group in Sweden is from Finland, followed by Iraq and Poland. In Husby, of residents with a foreign background, those who were born abroad or have two non-Swedish parents, 80 percent have heritage from either Asia or Africa, according to city statistics.

Residents are quick to point out that the violence is being carried out by a small group that doesn’t speak for most people living there. Community groups have taken to the streets to help ease tensions and restore calm, which was successful over the weekend.

Read Full Article Here

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Earth Watch Report  -  Earthquakes

 

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Today Earthquake India State of Jammu and Kashmir, [Bhaderwah area] Damage level Details

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Earthquake in India on Wednesday, 29 May, 2013 at 02:49 (02:49 AM) UTC.

Description
Fresh tremors last midnight shook Bhaderwah belt of Doda district causing more cracks in various buildings and one three-storey building collapsed at Sadar Bazaar. However, no causality or injuries were reported in the house collapse as occupants were in their relative’s house. The owner of the collapsed building has been identified as Jahangir Choudhary son of Zaffarullah Choudhary of Haveli Mohalla, Bhaderwah. The loss is estimated to be at around Rs 10 lakh and belongings worth of thousands were also destroyed. The rear side of the house completely collapsed included 10 rooms and 4 shops. Luckily there were no injuries to the occupants as they were out in the home due to cracks in the house. Choudhary family has urged for financial help from the government to repair the house. Jahangir Choudhary owner of the collapsed house alleged that despite damage to their house during earthquake of May 1 they were living in the said unsafe house only due to the apathetic attitude of the administration and state government, as till day they had not received any relief. When the house collapsed during midnight all the family members were in the house of their relatives. He further alleged that no one from the administration visited them to know about their well beings and to assess damaged to their house. Due to the house collapse, the road from Takia Chowk to Idgah remained closed for the whole day.

Soon after receiving the report of collapse of building, cops rushed to the spot and started removing the debris of building from the main Eidgah road near Sadar Bazaar and traffic for the whole day remained disrupted. SDM Bhaderwah Dr Ravi Bharti informed media that said building was already declared as unsafe by the administration as it had developed maximum cracks during May 1 quake and today it was completely damaged due to aftershocks. He advised people not to use unsafe buildings and houses keeping in view the continuous aftershocks to avoid any untoward incident. Two aftershocks shook Bhaderwah valley and adjoining areas in Doda-Kishtwar belt triggering fresh panic among the people. The fresh intensity tremors of 2.8, 5.3 and 2.9 on the Richter Scale shook Baderwah valley and adjoining areas of Doda-Kishtwar belt at 12.28 AM and 1.30 AM today, officials further said. The tremors were followed by aftershocks. A total of 43 tremors have been recorded in the Bhaderwah-Doda-Kishtwar belt during the past fortnight with maximum 11 on May 1. “We were very afraid, all the people went out into the streets and many took shelter in their cars, but fortunately the damage was fairly limited,” said Sheikh Masood Ahmed a local of Bhaderwah town, alleging that people are living in unsafe structures only due to negligence of administration as tents are provided “only to those who have political influence and poor people are still at the mercy of God”. Another citizen Neeraj Manhas also said that this is second incident within two days when already damaged structure due to earth quake has collapsed due to aftershocks and if as soon as possible no concrete steps are taken by government for the rehabilitation of affected people then no one can avoid human loss in near future at Bhaderwah. Manhas demanded special package for people so that they can reconstruct their structures before winter comes. It is notable to mention here that in Doda district, quakes and aftershocks caused damage to 494 schools, 12 primary health centers and 273 community centers. Government property worth Rs 80 crore and Rs 8 crore was damaged in Doda and Kishtwar respectively. Two persons were killed and 69, including 26 students, were injured in tremors that rattled the region on May 1.

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Fresh tremors in Bhaderwah, building collapses

KT NEWS SERVICE

BHADERWAH, May 28: Fresh tremors last midnight shook Bhaderwah belt of Doda district causing more cracks in various buildings and one three-storey building collapsed at Sadar Bazaar.
However, no causality or injuries were reported in the house collapse as occupants were in their relative’s house. The owner of the collapsed building has been identified as Jahangir Choudhary son of Zaffarullah Choudhary of Haveli Mohalla, Bhaderwah. The loss is estimated to be at around Rs 10 lakh and belongings worth of thousands were also destroyed. The rear side of the house completely collapsed included 10 rooms and 4 shops. Luckily there were no injuries to the occupants as they were out in the home due to cracks in the house.
Choudhary family has urged for financial help from the government to repair the house. Jahangir Choudhary owner of the collapsed house alleged that despite damage to their house during earthquake of May 1 they were living in the said unsafe house only due to the apathetic attitude of the administration and state government, as till day they had not received any relief. When the house collapsed during midnight all the family members were in the house of their relatives. He further alleged that no one from the administration visited them to know about their well beings and to assess damaged to their house. Due to the house collapse, the road from Takia Chowk to Idgah remained closed for the whole day.
Soon after receiving the report of collapse of building, cops rushed to the spot and started removing the debris of building from the main Eidgah road near Sadar Bazaar and traffic for the whole day remained disrupted.
SDM Bhaderwah Dr Ravi Bharti informed media that said building was already declared as unsafe by the administration as it had developed maximum cracks during May 1 quake and today it was completely damaged due to aftershocks. He advised people not to use unsafe buildings and houses keeping in view the continuous aftershocks to avoid any untoward incident.
Two aftershocks shook Bhaderwah valley and adjoining areas in Doda-Kishtwar belt triggering fresh panic among the people. The fresh intensity tremors of 2.8, 5.3 and 2.9 on the Richter Scale shook Baderwah valley and adjoining areas of Doda-Kishtwar belt at 12.28 AM and 1.30 AM today, officials further said. The tremors were followed by aftershocks. A total of 43 tremors have been recorded in the Bhaderwah-Doda-Kishtwar belt during the past fortnight with maximum 11 on May 1.

 

Read Full Article here

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Earth Watch Report  -  Extreme Weather

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20.05.2013 Heat Wave India Capital City, New Delhi Damage level
Details

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Heat Wave in India on Monday, 20 May, 2013 at 16:19 (04:19 PM) UTC.

Description
The heat wave will continue in Delhi and others parts of the country for the next two to three days. Dusty winds will hit north and northwest India during the period. In the first heat wave (about 45 degrees Celsius or above) of the summer in the capital, continuous sunshine for long daylight hours, stretching as much as 13 hours and 36 minutes, is driving up the temperature. The temperature in Delhi this week rose to 44.6 degrees Celsius and 46.2 degrees Celsius at the Safdarjang and Palam observatories respectively. It will not be surprising if the maximum temperature rises further to 45 degrees Celsius, a level observed on 31 May last year, the second time in a decade. The May record for Delhi, however, is 47.2 degrees Celsius, seen on 29 May 1944. Delhi wasn’t the hottest place in north India. Hisar in Haryana recorded 46 degrees Celsius on Sunday, five degrees above the average record of 40.7 degrees.

In Hisar, the maximum temperature may break last year’s record of 46.4 degrees registered on 31 May in the next two days. The highest maximum temperatures ever recorded in Hissar is 48.8 degrees on 21 May 1998. Winds from the Thar desert will continue to make life uncomfortable in most parts of northwest, central and east India in the coming two days. Some respite is possible at isolated pockets over northwest India if winds become southwesterly as they contain some moisture and are a bit cooler than the westerly winds. But most of the places in the region especially over Rajasthan, Punjab and Haryana will remain intense heat conditions. Hot and dry westerly winds will continue to hit central and east India in the coming two days so temperatures will remain in the mid-forties or above over interior Maharashtra. Nagpur, which registered 47.3 degrees as maximum could see a further rise in day temperature. The highest ever May temperature in Nagpur is 47.8 degrees registered on 26 May 1954. East Uttar Pradesh and adjoining areas of Bihar have temperatures in lower forties.

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Delhi reels under 44.5 degrees Celsius heat, no respite in sight

 

 

NEW DELHI: The mercury’s dreaded surge into the high forties has left vast swathes of north India sweltering under a severe heat wave spread across Delhi, Uttar Pradesh, Rajasthan, Punjab, Haryana, Madhya Pradesh and Bihar. Churu in Rajasthan continued to sizzle for the third day, recording a blistering 48.2 degrees Celsius.

Delhi sweated under 44.5 degrees Celsius, five degrees above normal, while Palam was the hottest in NCR at 46.2 degrees.

Met officials said there would be no respite till May 24. Even that would lower temperatures by just 1-2 degrees, after which high temperatures would return for the rest of the month, the Met office said. This would mark only the second instance of Delhi seeing such a prolonged heat wave in May in the last 10 years.

Mercury to stay high till Saturday

“The heat wave is the result of the absence of any western disturbance in Delhi and neighbouring areas, strengthening of hot northwesterly winds from the desert and subsidence of air in association with an anticyclone over Rajasthan and adjoining areas,” said O P Singh, deputy director of meteorology, Delhi Regional Meteorological Centre

“Such conditions are favourable for dust raising winds in northwest India and are likely to continue during the fourth week of May as well. There will be a small decrease in temperature during the coming weekend with the advent of a western disturbance,” Singh added.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Read Full Article Here

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No respite from heat for Delhi: Meteorological department

 

Watch  Video Here

 

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Natural disasters uprooted more than 32 million people in 2012

32,4 million people were forced to flee their homes last year due to natural disasters such as floods, storms and earthquakes, according to a report released by Internal Displacement Monitoring Centre on May 13, 2013. According to the report, 98% of those uprooted were displaced by climate- and weather-related events. Climate change is believed to play an increasingly significant role in global disasters. 2012 Special Report from the Intergovernmental Panel on Climate Change stated that, “disasters associated with climate extremes influence population mobility and relocation, affecting host and origin communities.”

This map shows internal displacement worldwide in 2012 by state and number of displaced people. CLICK ON IMAGE FOR LARGER VIEW (Credit: NRC/IDMC)

Floods in India and Nigeria were responsible for 41 % of displacement worldwide last year. Monsoon floods in India uprooted about 6.9 million people, while in Nigeria some 6.1 million were newly displaced. While Asia and Africa were hardest affected, some 1.3 million people were displaced in wealthy nations, especially the United States. Last year, the U.S. was among the 10 countries that experienced the most new displacement. Following Hurricane Sandy, most of those displaced were able to find refuge in adequate temporary shelter while displaced from their own homes.

The largest regional increase in the number of internally displaced people in 2012 was in the Middle East and North Africa, where 2.5 million people were forced to flee their homes. There were almost 6 million affected in the region at the end of 2012, a rise of 40 % on the 2011. Asia showed the second highest increase in new displacement after the Middle East and North Africa, with 1.4 million people forced to flee their homes during 2012.

 Read Full Article Here

Earth Watch Report  -  Earthquakes

 photo India-2EQsMay14th2013_zps7ec9e41f.jpg

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M4.2 – 17km S of Kishtwar, India 2013-05-14 19:58:25 UTC

 

Earthquake location 33.156°N, 75.780°E

Event Time

  1. 2013-05-14 19:58:25 UTC
  2. 2013-05-15 01:28:25 UTC+05:30 at epicenter
  3. 2013-05-14 14:58:25 UTC-05:00 system time

Location

33.156°N 75.780°E depth=50.6km (31.4mi)

Nearby Cities

  1. 17km (11mi) S of Kishtwar, India
  2. 20km (12mi) E of Doda, India
  3. 20km (12mi) NNE of Bhadarwah, India
  4. 65km (40mi) ENE of Udhampur, India
  5. 262km (163mi) ESE of Islamabad, Pakistan

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M4.7 – 19km SSE of Kishtwar, India 2013-05-14 20:00:02 UTC

 

Earthquake location 33.154°N, 75.837°E

Event Time

  1. 2013-05-14 20:00:02 UTC
  2. 2013-05-15 01:30:02 UTC+05:30 at epicenter
  3. 2013-05-14 15:00:02 UTC-05:00 system time

Location

33.154°N 75.837°E depth=10.9km (6.8mi)

Nearby Cities

  1. 19km (12mi) SSE of Kishtwar, India
  2. 22km (14mi) NNE of Bhadarwah, India
  3. 25km (16mi) E of Doda, India
  4. 70km (43mi) ENE of Udhampur, India
  5. 267km (166mi) ESE of Islamabad, Pakistan

 

….

Tectonic Summary

Seismotectonics of the Himalaya and Vicinity

Seismicity in the Himalaya dominantly results from the continental collision of the India and Eurasia plates, which are converging at a relative rate of 40-50 mm/yr. Northward underthrusting of India beneath Eurasia generates numerous earthquakes and consequently makes this area one of the most seismically hazardous regions on Earth. The surface expression of the plate boundary is marked by the foothills of the north-south trending Sulaiman Range in the west, the Indo-Burmese Arc in the east and the east-west trending Himalaya Front in the north of India.

The India-Eurasia plate boundary is a diffuse boundary, which in the region near the north of India, lies within the limits of the Indus-Tsangpo (also called the Yarlung-Zangbo) Suture to the north and the Main Frontal Thrust to the south. The Indus-Tsangpo Suture Zone is located roughly 200 km north of the Himalaya Front and is defined by an exposed ophiolite chain along its southern margin. The narrow (<200km) Himalaya Front includes numerous east-west trending, parallel structures. This region has the highest rates of seismicity and largest earthquakes in the Himalaya region, caused mainly by movement on thrust faults. Examples of significant earthquakes, in this densely populated region, caused by reverse slip movement include the 1934 M8.1 Bihar, the 1905 M7.5 Kangra and the 2005 M7.6 Kashmir earthquakes. The latter two resulted in the highest death tolls for Himalaya earthquakes seen to date, together killing over 100,000 people and leaving millions homeless. The largest instrumentally recorded Himalaya earthquake occurred on 15th August 1950 in Assam, eastern India. This M8.6 right-lateral, strike-slip, earthquake was widely felt over a broad area of central Asia, causing extensive damage to villages in the epicentral region.

The Tibetan Plateau is situated north of the Himalaya, stretching approximately 1000km north-south and 2500km east-west, and is geologically and tectonically complex with several sutures which are hundreds of kilometer-long and generally trend east-west. The Tibetan Plateau is cut by a number of large (>1000km) east-west trending, left-lateral, strike-slip faults, including the long Kunlun, Haiyuan, and the Altyn Tagh. Right-lateral, strike-slip faults (comparable in size to the left-lateral faults), in this region include the Karakorum, Red River, and Sagaing. Secondary north-south trending normal faults also cut the Tibetan Plateau. Thrust faults are found towards the north and south of the Tibetan Plateau. Collectively, these faults accommodate crustal shortening associated with the ongoing collision of the India and Eurasia plates, with thrust faults accommodating north south compression, and normal and strike-slip accommodating east-west extension.

Along the western margin of the Tibetan Plateau, in the vicinity of south-eastern Afghanistan and western Pakistan, the India plate translates obliquely relative to the Eurasia plate, resulting in a complex fold-and-thrust belt known as the Sulaiman Range. Faulting in this region includes strike-slip, reverse-slip and oblique-slip motion and often results in shallow, destructive earthquakes. The active, left-lateral, strike-slip Chaman fault is the fastest moving fault in the region. In 1505, a segment of the Chaman fault near Kabul, Afghanistan, ruptured causing widespread destruction. In the same region the more recent 30 May 1935, M7.6 Quetta earthquake, which occurred in the Sulaiman Range in Pakistan, killed between 30,000 and 60,000 people.

On the north-western side of the Tibetan Plateau, beneath the Pamir-Hindu Kush Mountains of northern Afghanistan, earthquakes occur at depths as great as 200 km as a result of remnant lithospheric subduction. The curved arc of deep earthquakes found in the Hindu Kush Pamir region indicates the presence of a lithospheric body at depth, thought to be remnants of a subducting slab. Cross-sections through the Hindu Kush region suggest a near vertical northerly-dipping subducting slab, whereas cross-sections through the nearby Pamir region to the east indicate a much shallower dipping, southerly subducting slab. Some models suggest the presence of two subduction zones; with the Indian plate being subducted beneath the Hindu Kush region and the Eurasian plate being subducted beneath the Pamir region. However, other models suggest that just one of the two plates is being subducted and that the slab has become contorted and overturned in places.

Shallow crustal earthquakes also occur in this region near the Main Pamir Thrust and other active Quaternary faults. The Main Pamir Thrust, north of the Pamir Mountains, is an active shortening structure. The northern portion of the Main Pamir Thrust produces many shallow earthquakes, whereas its western and eastern borders display a combination of thrust and strike-slip mechanisms. On the 18 February 1911, the M7.4 Sarez earthquake ruptured in the Central Pamir Mountains, killing numerous people and triggering a landside, which blocked the Murghab River.

Further north, the Tian Shan is a seismically active intra-continental mountain belt, which extends 2500 km in an ENE-WNW orientation north of the Tarim Basin. This belt is defined by numerous east-west trending thrust faults, creating a compressional basin and range landscape. It is generally thought that regional stresses associated with the collision of the India and Eurasia plates are responsible for faulting in the region. The region has had three major earthquakes (>M7.6) at the start of the 20th Century, including the 1902 Atushi earthquake, which killed an estimated 5,000 people. The range is cut through in the west by the 700-km-long, northwest-southeast striking, Talas-Ferghana active right-lateral, strike-slip fault system. Though the system has produced no major earthquakes in the last 250 years, paleo-seismic studies indicate that it has the potential to produce M7.0+ earthquakes and it is thought to represent a significant hazard.

The northern portion of the Tibetan Plateau itself is largely dominated by the motion on three large left-lateral, strike-slip fault systems; the Altyn Tagh, Kunlun and Haiyuan. The Altyn Tagh fault is the longest of these strike slip faults and it is thought to accommodate a significant portion of plate convergence. However, this system has not experienced significant historical earthquakes, though paleoseismic studies show evidence of prehistoric M7.0-8.0 events. Thrust faults link with the Altyn Tagh at its eastern and western termini. The Kunlun Fault, south of the Altyn Tagh, is seismically active, producing large earthquakes such as the 8th November 1997, M7.6 Manyi earthquake and the 14th November 2001, M7.8 Kokoxili earthquake. The Haiyuan Fault, in the far north-east, generated the 16 December 1920, M7.8 earthquake that killed approximately 200,000 people and the 22 May 1927 M7.6 earthquake that killed 40,912.

The Longmen Shan thrust belt, along the eastern margin of the Tibetan Plateau, is an important structural feature and forms a transitional zone between the complexly deformed Songpan-Garze Fold Belt and the relatively undeformed Sichuan Basin. On 12 May 2008, the thrust belt produced the reverse slip, M7.9 Wenchuan earthquake, killing over 87,000 people and causing billions of US dollars in damages and landslides which dammed several rivers and lakes.

Southeast of the Tibetan Plateau are the right-lateral, strike-slip Red River and the left-lateral, strike-slip Xiangshuihe-Xiaojiang fault systems. The Red River Fault experienced large scale, left-lateral ductile shear during the Tertiary period before changing to its present day right-lateral slip rate of approximately 5 mm/yr. This fault has produced several earthquakes >M6.0 including the 4 January 1970, M7.5 earthquake in Tonghai which killed over 10,000 people. Since the start of the 20th century, the Xiangshuihe-Xiaojiang Fault system has generated several M7.0+ earthquakes including the M7.5 Luhuo earthquake which ruptured on the 22 April 1973. Some studies suggest that due to the high slip rate on this fault, future large earthquakes are highly possible along the 65km stretch between Daofu and Qianning and the 135km stretch that runs through Kangding.

Shallow earthquakes within the Indo-Burmese Arc, predominantly occur on a combination of strike-slip and reverse faults, including the Sagaing, Kabaw and Dauki faults. Between 1930 and 1956, six M7.0+ earthquakes occurred near the right-lateral Sagaing Fault, resulting in severe damage in Myanmar including the generation of landslides, liquefaction and the loss of 610 lives. Deep earthquakes (200km) have also been known to occur in this region, these are thought to be due to the subduction of the eastwards dipping, India plate, though whether subduction is currently active is debated. Within the pre-instrumental period, the large Shillong earthquake occurred on the 12 June 1897, causing widespread destruction.

 

 

….

 

 

THE WATCHERS

WATCHING THE WORLD EVOLVE AND TRANSFORM

Tropical Cyclone Mahasen (01B) is now centered several hundred miles south of Kolkata, India, and will impact areas from northeastern India to Bangladesh and Myanmar over the next few days. The system is about to enter  into an area of warm sea surface temperatures and lower wind shear which will intensified the cyclone and give it opportunity to become even better organized. Landfall is expected to occur on May 16, 2013 with most forecast models putting the path between Chittagong (Bangladesh) and Maungdaw (Myanmar).

On May 13, 2013 the Suomi NPP satellite caught an interesting glimpse of the storm as it moved off the eastern coast of India. The VIIRS Day-Night Band was able to resolve lightning flashes towards the center of the storm, along with mesopheric gravity waves emanating outwards like ripples in a pond. These gravity waves are of particular interest to air traffic controllers so assist in identifying areas of turbulence. (Credit: NOAA/NASA/VIIRS)

TC Mahasen will bring life-threatening conditions to millions of people from northeastern India and into Bangladesh and Myanmar. Due the low elevations of this region (mostly shallower than 200 meters), flooding, mudslides and storm surge present the greatest threats. These areas have been hit by some of the deadliest cyclones across the globe.

According to GDACS, up to 22.3 million people people can be affected by wind speeds of tropical storm strength or above. In addition, 4.1 million people people are living in coastal areas below 5m and can therefore be affected by storm surge.

The highest impact, surge and rainfall predictions are for the Chittagong and Cox’s Bazaar areas of Bangladesh but there are serious concerns for Rakhine State where there are more than 140,000 IDPs. (Credit: OCHA/ReliefWeb)

Torrential rains caused floods and landslides across Sri Lanka, which are responsible for seven reported deaths. Several overcrowded boats carrying hundreds of evacuees capsized off the coast of western Myanmar after the lead boat crashed into rocks and more than 50 people are feared dead. Myanmar state television reported Monday that 5,158 people were relocated from low-lying camps in Rakhine state to safer shelters. But far more people are considered vulnerable.

Bathymetry of the Bay of Bengal (Credit: Geomap/MGDS)

Storm surge prediction model (Credit: IMD)

According to latest report by Joint Typhoon Warning Center (JTWC), TC Mahasen is located approximately 246 nm southward of Calcutta, India. The system is moving north-northeastward at speed of 12 knots. Upper level analysis indicates an anticyclone to the east of the system continues to move into better vertical alignment with the low level circulation center, leading to a decrease in vertical wind shear to low levels (10 knots).

Read Full Report  Here

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Del6217777.jpg

Rohingya women reinforce their tents at the Ohnedaw Internally Displaced Persons (IDP) camp on the outskirts of Sittwe on May 15, 2013, as Cyclone Mahasen heads towards landfall. Hundreds of thousands of people in Bangladesh and Myanmar were ordered to evacuate Wednesday as a cyclone bore down on coastal areas home to flood-prone refugee camps for victims of sectarian unrest. Soe Than WIN/AFP/Getty Images

Bangladeshi marine sailors stand on the banks of the Bay of Bengal sea, as they prepare for the coming of tropical cyclone Mahasen, in Chittagong, Bangladesh, Wednesday, May 15, 2013. People living in coastal areas in Bangladesh and Myanmar are being evacuated as cyclone Mahasen appears to make landfall late Thursday or early Friday, according to news reports. (AP Photo/A.M. Ahad)

See Additional Photos Here

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Tropical Storm in Bangladesh on Thursday, 16 May, 2013 at 08:40 (08:40 AM) UTC.

Back

Updated: Thursday, 16 May, 2013 at 11:38 UTC
Description
Cyclone Mahasen has struck the southern coast of Bangladesh, lashing remote fishing villages with heavy rain and fierce winds that flattened mud and straw huts and forced the evacuation of more than 1 million people. The main section of the storm reached land on Thursday and immediately began weakening, according to Mohammad Shah Alam, director of the Bangladesh meteorological department. However, its forward movement was also slowing, meaning that towns in its path would have to weather the storm for longer, he said. Even before the brunt of the storm hit, at least 18 deaths related to Mahasen were reported in Bangladesh, Burma and Sri Lanka. The storm could bring life-threatening conditions to about 8.2 million people in Bangladesh, Burma and north-east India, according to the UN’s Office for the Co-ordination of Humanitarian Affairs. Danger was particularly high for tens of thousands of displaced Rohingya people living in plastic-roofed tents and huts made of reeds in dozens of refugee camps along Burma’s western coast.

Driven from their homes by violence, members of the Muslim minority group refused to follow evacuation orders. Many distrust officials in the majority-Buddhist country, where Rohingya have faced decades of discrimination. UN officials, hoping they would inspire greater trust, fanned out across the area to encourage people to leave. Early on Thursday, the cyclone battered the southern Bangladesh fishing village of Khepurpara along the Bay of Bengal with 62mph (100km/h) winds and was heading east toward the city of Chittagong and the seafront resort town of Cox’s Bazar. River ferries and boat services were suspended, and scores of factories near the Bay of Bengal were closed. The military said it was keeping 22 navy ships and 19 air force helicopters on alert. Tens of thousands of people fled their shanty homes along the coast and packed into cyclone shelters, schools, government office buildings and some of the 300 hotels in Cox’s Bazar to wait out the storm. Some brought their livestock, which took shelter outside.

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Tropical Cyclone Mahasen targets India, Bangladesh, Myanmar

Tropical Cyclone Mahasen (TC 01B) is getting better organized. Winds are predicted to increase to hurricane force as the system moves further northward into the Bay of Bengal. TC Mahasen is now located east-nort​heast of Sri Lanka and is expected to impact areas from northeast India to Bangladesh and Myanmar.

According to latest report by Joint Typhoon Warning Center (JTWC), TC Mahasen is located approximately 721 nm southward of Calcutta, India. The system is moving north-northwestward at speed of 6 knots. Maximum sustainable winds are 55 knots with gusts up to 70 knots.

Indian Ocean IR satellite image of the system on May 12, 2013 (Credit: METEOSAT-7/CIMSS)

The cyclone is beginning to round the western edge of the subtropical ridge to the east. It is expected to slow down over the next 24 hours as it makes the turn before recurving northeastward on the poleward side of the ridge axis. TC Mahasen will gradually intensify as the vertical wind shear relaxes along the ridge axis. Additionally, the poleward outflow is expected to open up as the system becomes exposed to the prevailing westerlies.

Animated infrared satellite imagery shows the system has regained a central dense overcast feature that has, once again, obscured the low level circulation center. Upper level analysis indicates the system is 7 degrees south of the ridge axis in an area of moderate (20 knot) easterly vertical wind shear. However, the vertical wind shear is offset by robust westward outflow.

After the next 72 hours, TC Mahasen will gradually weaken as vertical wind shear increases before making landfall near Chittagong, Bangladesh. Land interaction will rapidly erode and dissipate the system.

​TC Mahasen forecast track (Source: JTWC)

According to Indian Meteorological Department (IMD), under the influence of this system, rainfall at many places with isolated heavy rainfall would occur over Andaman and Nicobar Islands during next 48 hours. Squally winds speed reaching 40-45 km/h gusting to 60 km/h would prevail along Andaman and Nicobar Islands during next 48 hours. Sea condition will be rough to very rough along and off Andaman and Nicobar Islands during this period.

 

Read Full Article Here

Earth Watch Report  -  Hailstorm

09.05.2013 Hailstorm India State of Mizoram, [Mizoram-wide] Damage level Details

Hailstorm in India on Thursday, 09 May, 2013 at 13:06 (01:06 PM) UTC.

Description
Over 200 houses, especially tin- roofed and those with asbestos walls, were damaged in rain and hailstorm in different areas of Kolasib district in Mizoram, official sources said today. Sixty-three houses were damaged in Kolasib town and 100 others in nearby Thingdawl village in the rain and hailstorm yesterday, the sources said. Around 40 houses were also damaged in Bukpui village along the Serkhan-Bagha road and three houses were damaged in Sethawn village, they said. Several landslides, which occurred due to rains, also blocked a number of roads in Kolasib town, they said.

Eight killed, many injured; large damage in weather fury in Tripura, Mizoram

Friday – May 10, 2013, 04:13pm (GMT+5.5) 

IndiaVision NEWS

Agartala/Aizawl – Seasonal cyclonic storms accompanied by lightning and rain continued to create devastation in Tripura and Mizoram for the sixth day Friday, killing eight people so far injuring 40 others, an official said here.

Several thousand houses have been damaged in the cyclonic storms accompanied by lightning and incessant rains that also uprooted thousands of trees, telephone and electric poles both in Tripura and Mizoram.

Restoration work was on in both the northeastern states.

“Since Sunday, eight people, including five women, were killed in different parts of Tripura in house collapse and lightning. Over 40 people injured some of them seriously in these weather furies,” an official of the Tripura relief department told IANS.

“Sixty-year-old Ramani Debbarma and her 17-year-old-son Utpal died when huge landslides buried their home at Simna in western Tripura Wednesday night. Their bodies have been recovered late Thursday night,” he added.

The first nonstop rains in the pre-monsoon period also caused flooding and huge waterlogging in the low-lying areas of capital Agartala, its outskirts and other parts of Tripura. Several thousand people were forced to move to several makeshift relief camps.

The Tripura government has sanctioned from Rs.1,000 to Rs.10,000 as immediate relief assistance to each affected family.

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