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Earth Watch Report – Friday September 28th,2012

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Earthquakes

USGS

MAG UTC DATE-TIME
y/m/d h:m:s
LAT
deg
LON
deg
DEPTH
km
 Region
MAP  3.2 2012/09/27 23:59:40   18.546   -68.963 101.0  DOMINICAN REPUBLIC
MAP  6.0   2012/09/27 23:53:49   -8.825   157.557 10.0  SOLOMON ISLANDS
MAP  4.8   2012/09/27 22:18:21  -22.905   -68.620 86.1  ANTOFAGASTA, CHILE
MAP  3.3 2012/09/27 21:06:05   19.631   -64.225 62.0  VIRGIN ISLANDS REGION
MAP  5.0   2012/09/27 16:54:44  -24.893  -179.256 515.1  SOUTH OF THE FIJI ISLANDS
MAP  4.8   2012/09/27 16:39:00  -20.066   -69.068 94.3  TARAPACA, CHILE
MAP  4.2 2012/09/27 15:36:08   24.693  -110.239 14.8  GULF OF CALIFORNIA
MAP  4.5   2012/09/27 13:14:30   15.442   -91.632 228.7  GUATEMALA
MAP  4.5   2012/09/27 12:38:43   37.629   95.888 32.9  NORTHERN QINGHAI, CHINA
MAP  4.0 2012/09/27 11:24:11   24.419  -110.135 10.2  GULF OF CALIFORNIA
MAP  3.5 2012/09/27 10:41:15   61.984  -154.418 36.4  SOUTHERN ALASKA
MAP  4.8   2012/09/27 10:28:41   -9.422   123.543 98.1  TIMOR REGION, INDONESIA
MAP  2.6 2012/09/27 09:44:48   19.410  -155.304 4.0  ISLAND OF HAWAII, HAWAII
MAP  3.2 2012/09/27 08:36:34   36.890  -117.414 7.6  CENTRAL CALIFORNIA
MAP  2.5 2012/09/27 08:04:29   63.355  -151.197 10.6  CENTRAL ALASKA
MAP  4.5   2012/09/27 07:16:10   51.653  -177.636 35.7  ANDREANOF ISLANDS, ALEUTIAN IS., ALASKA
MAP  2.7 2012/09/27 05:58:59   38.827  -122.851 2.7  NORTHERN CALIFORNIA
MAP  2.6 2012/09/27 05:39:23   39.417  -123.535 3.2  NORTHERN CALIFORNIA
MAP  2.5 2012/09/27 05:21:53   39.467  -123.110 3.9  NORTHERN CALIFORNIA
MAP  2.8 2012/09/27 05:02:20   59.693  -152.430 67.9  SOUTHERN ALASKA
MAP  3.2 2012/09/27 04:23:58   19.694   -64.231 50.0  VIRGIN ISLANDS REGION
MAP  3.7 2012/09/27 04:12:45   62.877  -150.522 92.1  CENTRAL ALASKA
MAP  3.1 2012/09/27 04:03:04   19.676   -64.369 36.0  VIRGIN ISLANDS REGION
MAP  2.7 2012/09/27 03:50:39   18.045   -66.858 22.0  PUERTO RICO
MAP  2.6 2012/09/27 03:45:04   61.149  -150.911 50.8  SOUTHERN ALASKA
MAP  4.5   2012/09/27 03:28:52   51.728  -177.860 44.5  ANDREANOF ISLANDS, ALEUTIAN IS., ALASKA
MAP  4.7   2012/09/27 01:36:29  -23.208   -66.655 190.3  JUJUY, ARGENTINA
MAP  4.7   2012/09/27 01:08:24   41.218   15.026 5.0  SOUTHERN ITALY
MAP  4.5   2012/09/27 00:56:04   38.412   46.709 10.0  NORTHWESTERN IRAN

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6.0 magnitude quake hits off Solomon Islands: USGS

Agencies : Sydney,

A quake measuring magnitude 6.0 hit off the Solomon Islands today, but Australian seismologists said there was little risk of a tsunami.

The US Geological Survey put the quake at 6.0-magnitude some 272 kilometres west-northwest of the capital Honiara. With a depth of about 9 kilometres, it was about 112 kilometres southeast of the western city of Gizo.

Geoscience Australia measured the quake at about 6.2-magnitude but said it was unlikely to create a tsunami or cause serious damage in the capital.

“It’s just off the plate boundary so it’s a normal-sized earthquake and positioning for the area,” seismologist Hugh Glanville told AFP.

“It’s not too close to Honiara. There’s a local city with a population of about 6,000 or so that might get a bit of damage,” he said in reference to Gizo.

“But the majority of the population is a bit too far away to suffer more than a bit of shaking. And the population in the area is pretty sparse really.”

Glanville also said the quake was too small to generate a tsunami.

“Generally a local tsunami starts at about 6.5 (magnitude). It’s always possible, but it’s just extremely rare that it would generate a tsunami,” he said.

“It’s just one of the plate boundary earthquakes along the Ring of Fire that normally happens in this area.”

The Solomon Islands form part of the Ring of Fire, a zone of tectonic activity around the Pacific Ocean that is subject to earthquakes and volcanic eruptions.

In 2007 a tsunami following an 8.1-magnitude earthquake killed at least 52 people in the Solomons and left thousands homeless.

Matt Burrows Reporting
    The San Andreas, Calaveras, and Hayward fault lines -which run underneath Silicon Valley – could set off tremors and aftershocks globally, according to a new study.
Researchers at UC Berkeley and the U.S. Geological Survey found that fault lines of the “strike-slip” type, where plates of land slide past each other, were more likely to set off the worldwide aftershocks.
As an example, the researchers found the 8.6 earthquake in Indonesia this April set off 16 earthquakes with a magnitude of 5.5 or greater within days.
Not only could these “strike slip” faults like the San Andreas, Calaveras, and Hayward faults set off worldwide aftershocks, but the researchers indicate the faults could also be set off if another earthquake’s tremors struck when the fault was ready to rupture.
However, the study indicates a quake powerful enough to do that only happens once every 50 years or so.

Sumatran quakes in April were part of tectonic plate breakup

Scientists document an episode in the breakup of the Indo-Australian plate into two pieces, an epic process that began roughly 50 million years ago and isn’t done yet.

 Sumatran earthquakeA woman and her baby evacuate to higher ground after a strong earthquake in Sumatra in April. (Heri Juanda / Associated Press / April 11, 2012)

By Monte Morin, Los Angeles Times

Planet Earth may be 4.5 billion years old, but that doesn’t mean it can’t serve up a shattering surprise now and again.

Such was the case on April 11 when two massive earthquakes erupted beneath the Indian Ocean off the coast of the Indonesian island of Sumatra, far from the usual danger zones. Now scientists say the seafloor ruptures are part of a long suspected, yet never before observed, event: the slow-motion splitting of a vast tectonic plate.

The first of the quakes, a magnitude 8.7, was 20 times more powerful than California’s long anticipated “big one” and tore a complex network of faults deep in the ocean floor. The violence also triggered unusually large aftershocks thousands of miles away, including four off North America’s western coast.

“It was jaw-dropping,” said Thorne Lay, a professor of Earth and planetary sciences at UC Santa Cruz. “It was like nothing we’d ever seen.”

At first, Lay wondered whether the computer code he used to analyze earthquakes was wrong. Eventually, he and other scientists realized that they had documented the breakup of the Indo-Australian plate into two pieces, an epic process that began roughly 50 million years ago and will continue for tens of millions more. Lay and other scientists reported their findings online Wednesday in the journal Nature.

Most great earthquakes occur along plate borders, where one plate dives beneath the adjoining plate and sinks deep into Earth’s mantle, a process called subduction. The April 11 quakes, however, occurred in the middle of the plate and involved a number of strike-slip faults, meaning the ground on one side of the fault moves horizontally past ground on the other side.

Scientists say the 8.7 main shock broke four faults. The quake lasted 2 minutes and 40 seconds — most last just seconds — and was followed by a second main shock, of magnitude 8.2, two hours later.

Unlike the magnitude 9.1 temblor that struck in the same region on Dec. 26, 2004, and created a deadly tsunami, the April 11 quakes did not cause similar destruction. That’s because horizontally moving strike-slip faults do not induce the massive, vertical displacement of water that thrust faults do on the borders of plates.

The type of interplate faults involved in the Sumatran quakes are the result of monumental forces, some of which drove the land mass of India into Asia millions of years ago and lifted the Himalayan Mountains. As the Indo-Australian plate continues to slide northwest, the western portion of the plate, where India is, has been grinding against and underneath Asia. But the eastern portion of the plate, which contains Australia, keeps on moving without the same obstruction. That difference creates squeezing pressure in the area where the quakes occurred.

The study authors say that over time, as more quakes occur and new ruptures appear, the cracks will eventually coalesce into a single fissure.

“This is part of the messy business of breaking up a plate,” said University of Utah seismologist Keith Koper, senior author of one of the studies. “Most likely it will take thousands of similar large quakes for that to happen.”

The quakes were also notable for triggering powerful aftershocks thousands of miles away. Though major quakes have been known to trigger aftershocks at great distance, they are usually less than 5.5 in magnitude. The April earthquakes triggered 11 aftershocks that measured 5.5 or greater in the six days that followed, including a magnitude 7. Remote shocks were felt 6,000 to 12,000 miles from the main quakes.

Fred Pollitz, a geophysicist with the U.S. Geological Survey in Menlo Park, Calif., and lead author of one of the studies, said the quakes were extremely effective in transmitting seismic wave radiation around the world. Though Pollitz said the magnitude of the larger Sumatran quake is No. 10 on the list of quakes since 1900, no other temblor has triggered so many strong aftershocks so far away.

“It’s the most powerful earthquake ever in terms of capability of putting stress on other fault zones around the world,” he said.

Pollitz said the quakes were likely to teach seismologists about the physics of earthquakes, particularly those along strike-slip faults. That knowledge, he said, would certainly apply to California’s San Andreas fault, which is also a strike-slip fault.

Lay said that the Sumatran quakes were most surprising in that they were completely unanticipated by seismologists and that he did not expect the event to repeat any time soon.

monte.morin@latimes.com

Big quake was part of crustal plate breakup

by Staff Writers
Salt Lake City UT (SPX)


This map of the Indian Ocean region shows boundaries of Earth’s tectonic plates in the area, and the epicenters (red stars) of two great earthquakes that happened April 11, 2012. A new study from the University of Utah and University of California, Santa Cruz, says the main shock measured 8.7 in magnitude, about 40 times larger than the previous estimate of 8.6. An 8.2-magnitude quake followed two hours later.The scientists explain how at least four faults ruptured during the 8.7 main shock, and how both great quakes are likely part of the breakup of the Indo-Australian Plate into separate subplates. The northeastward-moving plate is breaking up over scores of millions of years because the western part of the plate is bumping into Asia and slowing down, while the eastern part is sliding more easily beneath Sumatra and the Sunda plate. Credit: Keith Koper, University of Utah Seismograph Stations.

Seismologists have known for years that the Indo-Australian plate of Earth’s crust is slowly breaking apart, but they saw it in action last April when at least four faults broke in a magnitude-8.7 earthquake that may be the largest of its type ever recorded.

The great Indian Ocean quake of April 11, 2012 previously was reported as 8.6 magnitude, and the new estimate means the quake was 40 percent larger than had been believed, scientists from the University of Utah and University of California, Santa Cruz, report in the Sept. 27 issue of the journal Nature.

The quake was caused by at least four undersea fault ruptures southwest of Sumatra, Indonesia, within a 2-minute, 40-second period. It killed at least two people, and eight others died from heart attacks. The quake was felt from India to Australia, including throughout South Asia and Southeast Asia.

If the four ruptures were considered separate quakes, their magnitudes would have been 8.5, 7.9, 8.3 and 7.8 on the “moment magnitude” scale used to measure the largest quakes, the scientists report.

The 8.7 main shock broke three faults that were parallel but offset from each other – known as en echelon faults – and a fourth fault that was perpendicular to and crossed the first fault.

The new study concludes that the magnitude-8.7 quake and an 8.2 quake two hours later were part of the breakup of the Indian and Australian subplates along a yet-unclear boundary beneath the Indian Ocean west of Sumatra and southeast of India – a process that started roughly 50 million years ago and that will continue for millions more.

“We’ve never seen an earthquake like this,” says study co-author Keith Koper, an associate professor geophysics and director of the University of Utah Seismograph Stations.

“This is part of the messy business of breaking up a plate. … This is a geologic process. It will take millions of years to form a new plate boundary and, most likely, it will take thousands of similar large quakes for that to happen.”

All four faults that broke in the 8.7 quake and the fifth fault that ruptured in the 8.2 quake were strike-slip faults, meaning ground on one side of the fault moves horizontally past ground on the other side.

The great quake of last April 11 “is possibly the largest strike-slip earthquake ever seismically recorded,” although a similar size quake in Tibet in 1950 was of an unknown type, according to the new study, which was led by two University of California, Santa Cruz, seismologists: graduate student Han Yue and Thorne Lay, a professor of Earth and planetary sciences. The National Science Foundation funded the study.

The 8.7 jolt also “is probably the largest intraplate [within a single tectonic plate of Earth's crust] ever seismically recorded,” Lay, Yue and Koper add. Most of Earth’s earthquakes occur at existing plate boundaries.

The researchers cannot be certain the April great quake was the largest intraplate quake or the largest strike-slip quake because “we are comparing it against historic earthquakes long before we had modern seismometers,” says Koper.

Why the Great Quake Didn’t Unleash Major Tsunamis
Koper says the 2012 quakes likely were triggered, at least in part, by changes in crustal stresses caused by the magnitude-9.1 Sumatra-Andaman earthquake of Dec. 26, 2004 – a jolt that generated massive tsunamis that killed most of the 228,000 victims in the Indian Ocean region.

The fact the 8.7 and 8.2 quakes were generated by horizontal movements along seafloor strike-slip faults – not by vertical motion along thrust faults – explains why they didn’t generate major tsunamis. The 8.7 quake caused small tsunamis, the largest of which measured about 12 inches in height at Meulaboh, Indonesia, according to the U.S. Geological Survey.

Without major tsunamis, the great earthquake caused “very little damage and death, especially for this size of an earthquake, because it happened in the ocean and away from coastlines,” and on strike-slip faults, says Koper.

The researchers studied the quake using a variety of methods to analyze the seismic waves it generated. Because the same data can be interpreted in various ways, Koper says it is conceivable that more than four fault segments broke during the 8.7 quake – conceivably five or even six – although four fault ruptures is most likely.

Breaking Up is Hard to Do
The Indo-Australian plate is breaking into two or perhaps three pieces (some believe a Capricorn subplate is separating from the west side of the Indian subplate). The magnitude-8.7 and 8.2 great quakes on April 11 occurred over a broad area where the India and Australian subplates are being sheared apart.

“What we’re seeing here is the Indo-Australian plate fragmenting into two separate plates,” says Lay.

The breakup of the northeast-moving Indo-Australian plate is happening because it is colliding with Asia in the northwest, which slows down the western part of the plate, while the eastern part of the plate continues moving more easily by diving or “subducting” under the island of Sumatra to the northeast. The subduction zone off Sumatra caused the catastrophic 2004 magnitude-9.1 quake and tsunami.

Seismic analysis shows the April 11 quakes “involve rupture of a very complex network of faults, for which we have no documented precedent in recorded seismic history,” the researchers write.

The analysis revealed this sequence for the faults ruptures that generated the 8.7 quake, and the estimated fault rupture lengths and slippage amounts:

+ The quake began with the 50-second rupture of a fault extending west-northwest to east-southeast, with an epicenter a few hundred miles southwest of Sumatra. The fault ruptured along a roughly 90-mile length, breaking “bilaterally” both west-northwestward and east-southeastward, and also at least 30 miles deep, “almost ripping through the whole plate,” Koper says. The seafloor on one side of the fault slipped about 100 feet past the seafloor on the fault’s other side.

+ The second fault, which slipped about 25 feet, began to rupture 40 seconds after the quake began. This rupture extended an estimated 60 miles to 120 miles north-northeast to south-southwest – perpendicular to the first fault and crossing it.

+ The third fault was parallel to the first fault and about 90 to the miles southwest of it. It started breaking 70 seconds after the quake began and ruptured along a length of about 90 miles. This fault slipped about 70 feet.

+ The fourth fault paralleled the first and third faults, but was to the northwest of both of them. It began to rupture 145 seconds after the quake began and continued to do so for 15 seconds until the quake ended after a total time of 2 minutes and 40 seconds. The fault rupture was roughly 30 miles to 60 miles long. The ground on one side of this fault slipped about 20 feet past ground on the other side.

Related Links
University of Utah
Tectonic Science and News

LISS – Live Internet Seismic Server

GSN Stations

These data update automatically every 30 minutes. Last update: September 28, 2012 10:49:03 UTC

Seismograms may take several moments to load. Click on a plot to see larger image.

CU/ANWB, Willy Bob, Antigua and Barbuda

 ANWB 24hr plot

CU/BBGH, Gun Hill, Barbados

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CU/BCIP, Isla Barro Colorado, Panama

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CU/GRGR, Grenville, Grenada

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CU/GRTK, Grand Turk, Turks and Caicos Islands

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CU/GTBY, Guantanamo Bay, Cuba

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CU/MTDJ, Mount Denham, Jamaica

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CU/SDDR, Presa de Sabaneta, Dominican Republic

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CU/TGUH, Tegucigalpa, Honduras

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IC/BJT, Baijiatuan, Beijing, China

 BJT 24hr plot

IC/ENH, Enshi, China

 ENH 24hr plot

IC/HIA, Hailar, Neimenggu Province, China

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IC/LSA, Lhasa, China

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IC/MDJ, Mudanjiang, China

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IC/QIZ, Qiongzhong, Guangduong Province, China

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IU/ADK, Aleutian Islands, Alaska, USA

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IU/AFI, Afiamalu, Samoa

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IU/ANMO, Albuquerque, New Mexico, USA

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IU/ANTO, Ankara, Turkey

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IU/BBSR, Bermuda

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IU/BILL, Bilibino, Russia

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IU/CASY, Casey, Antarctica

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IU/CCM, Cathedral Cave, Missouri, USA

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IU/CHTO, Chiang Mai, Thailand

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IU/COLA, College Outpost, Alaska, USA

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IU/COR, Corvallis, Oregon, USA

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IU/CTAO, Charters Towers, Australia

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IU/DAV,Davao, Philippines

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IU/DWPF,Disney Wilderness Preserve, Florida, USA

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IU/FUNA,Funafuti, Tuvalu

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IU/FURI, Mt. Furi, Ethiopia

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IU/GNI, Garni, Armenia

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IU/GRFO, Grafenberg, Germany

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IU/GUMO, Guam, Mariana Islands

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IU/HKT, Hockley, Texas, USA

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IU/HNR, Honiara, Solomon Islands

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IU/HRV, Adam Dziewonski Observatory (Oak Ridge), Massachusetts, USA

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IU/INCN, Inchon, Republic of Korea

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IU/JOHN, Johnston Island, Pacific Ocean

 JOHN 24hr plot

IU/KBS, Ny-Alesund, Spitzbergen, Norway

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IU/KEV, Kevo, Finland

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IU/KIEV, Kiev, Ukraine

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IU/KIP, Kipapa, Hawaii, USA

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IU/KMBO, Kilima Mbogo, Kenya

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IU/KNTN, Kanton Island, Kiribati

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IU/KONO, Kongsberg, Norway

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IU/KOWA, Kowa, Mali

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IU/LCO, Las Campanas Astronomical Observatory, Chile

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IU/LSZ, Lusaka, Zambia

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IU/LVC, Limon Verde, Chile

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IU/MA2, Magadan, Russia

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IU/MAJO, Matsushiro, Japan

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IU/MAKZ,Makanchi, Kazakhstan

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IU/MBWA, Marble Bar, Western Australia

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IU/MIDW, Midway Island, Pacific Ocean, USA

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IU/MSKU, Masuku, Gabon

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IU/NWAO, Narrogin, Australia

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IU/OTAV, Otavalo, Equador

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IU/PAB, San Pablo, Spain

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IU/PAYG Puerto Ayora, Galapagos Islands

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IU/PET, Petropavlovsk, Russia

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IU/PMG, Port Moresby, Papua New Guinea

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IU/PMSA, Palmer Station, Antarctica

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IU/POHA, Pohakaloa, Hawaii

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IU/PTCN, Pitcairn Island, South Pacific

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IU/PTGA, Pitinga, Brazil

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IU/QSPA, South Pole, Antarctica

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IU/RAO, Raoul, Kermandec Islands

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IU/RAR, Rarotonga, Cook Islands

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IU/RCBR, Riachuelo, Brazil

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IU/RSSD, Black Hills, South Dakota, USA

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IU/SAML, Samuel, Brazil

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IU/SBA, Scott Base, Antarctica

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IU/SDV, Santo Domingo, Venezuela

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IU/SFJD, Sondre Stromfjord, Greenland

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IU/SJG, San Juan, Puerto Rico

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IU/SLBS, Sierra la Laguna Baja California Sur, Mexico

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IU/SNZO, South Karori, New Zealand

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IU/SSPA, Standing Stone, Pennsylvania USA

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IU/TARA, Tarawa Island, Republic of Kiribati

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IU/TATO, Taipei, Taiwan

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IU/TEIG, Tepich, Yucatan, Mexico

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IU/TIXI, Tiksi, Russia

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IU/TRIS, Tristan da Cunha, Atlantic Ocean

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IU/TRQA, Tornquist, Argentina

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IU/TSUM, Tsumeb, Namibia

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IU/TUC, Tucson, Arizona

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IU/ULN, Ulaanbaatar, Mongolia

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IU/WAKE, Wake Island, Pacific Ocean

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IU/WCI, Wyandotte Cave, Indiana, USA

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IU/WVT, Waverly, Tennessee, USA

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IU/XMAS, Kiritimati Island, Republic of Kiribati

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IU/YAK, Yakutsk, Russia

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IU/YSS, Yuzhno Sakhalinsk, Russia

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Volcanic Activity

Volcano erupts with smoke on Sumatra

A volcano has erupted on Indonesia’s Sumatra island, spewing thick grey smoke up to 1.5 kilometres into the sky.

Monitoring official Suparno says Mount Marapi’s eruption on Wednesday is its strongest since August last year, when its status was raised to level three out of four.

Suparno, who uses one name, says there is no plan for an evacuation because the nearest villages are far beyond the danger zone of three kilometres from the crater.

Marapi is among about 129 active volcanos in Indonesia, which is located on the Pacific Ring of Fire, an arc of volcanos and fault lines encircling the Pacific Basin.

Its last major eruption in 1992 killed a climber and injured several others, including two American tourists.

Today Volcano Activity China Baekdu Mountain, [Changbaishan Volcano] Damage level Details

Volcano Activity in China on Friday, 28 September, 2012 at 02:31 (02:31 AM) UTC.

Description
A volcano on the border of China and North Korea is showing signs of increasing activity and could erupt in the next few decades, Chinese researchers say. A massive eruption of Changbaishan around 1,100 years ago spread ash and volcanic gases for 30 miles and left a 3-mile-wide crater atop the volcano, scientists said. Three smaller eruptions have occurred since then, the most recent in 1903, they said. Seismic activity, ground deformation and gas emissions recorded in a period of heightened activity from 2002 to 2006 suggests the magma chamber beneath the volcano is growing. This activity suggests an explosion could occur in the next couple of decades, researchers said. “We need to upgrade our current monitoring system in order to be able to meet the need for the early warning system for Changbaishan,” Jiandong Xu, a vulcanologist at the China Earthquake Administration in Beijing. Of the dozen or so volcanoes located in mainland China Changbaishan is the most likely to experience an eruption with potential catastrophic effects, Xu said.
27.09.2012 Volcano Eruption Indonesia West Sumatra, [Mount Marapi Volcano] Damage level Details

Volcano Eruption in Indonesia on Wednesday, 26 September, 2012 at 18:03 (06:03 PM) UTC.

Description
A volcano has erupted on Indonesia’s Sumatra island, spewing thick grey smoke up to 1.5 kilometres into the sky. Monitoring official Suparno says Mount Marapi’s eruption on Wednesday is its strongest since August last year, when its status was raised to level three out of four. Suparno, who uses one name, says there is no plan for an evacuation because the nearest villages are far beyond the danger zone of three kilometres from the crater.
27.09.2012 Volcano Eruption Mexico States of Puebla and Mexico, [Popocatepetl Volcano] Damage level Details

Volcano Eruption in Mexico on Wednesday, 26 September, 2012 at 03:15 (03:15 AM) UTC.

Description
At least 26 eruptions accompanied by steam and gas, as well as a volcano tectonic quake were registered as a consequence of the Mexican volcano Popocatépetl activity during the last hours, it was reported Tuesday. The National Center of Disaster Prevention (Cenapred) said eruptions were of low and medium intensity with no ash expulsion in any of them. According to the institution, the volcano tectonic quake was registered at 11.54 local time (16:54 GMT). At this moment, the alert light of volcano activity remains yellow phase 2 and the surrounding population to keep informed as to alerts on the activity of the volcano also known as Don Goyo. Traffic between Santiago Xalitzintla and San Pedro Nexapa, via the Cortes passage, is under control. The Popo is located at the center of the country, in the territorial limits of the Morelos, Puebla and Mexico states. Located 55 kilometers Southeast of the Federal District, the Popocatépetl is the second highest volcano in Mexico, with a maximum height of five thousand 458 meters above sea level, only second to the Pico de Orizaba (Veracruz) with five thousand 610 meters.

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Storms / Flooding / Tornadoes

 Active tropical storm system(s)
Name of storm system Location Formed Last update Last category Course Wind Speed Gust Wave Source Details
Nadine (AL14) Atlantic Ocean 11.09.2012 27.09.2012 Tropical Depression 240 ° 93 km/h 111 km/h 4.88 m NOAA NHC Details

Tropical Storm data

Share:
Storm name: Nadine (AL14)
Area: Atlantic Ocean
Start up location: N 16° 18.000, W 43° 6.000
Start up: 11th September 2012
Status: 22nd September 2012
Track long: 1,092.58 km
Top category.:
Report by: NOAA NHC
Useful links:
Past track
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave Pressure Source
12th Sep 2012 05:01:17 N 17° 48.000, W 45° 12.000 24 65 83 Tropical Storm 300 13 1004 MB NOAA NHC
12th Sep 2012 10:46:22 N 18° 36.000, W 46° 36.000 28 74 93 Tropical Storm 300 15 1001 MB NOAA NHC
13th Sep 2012 05:34:52 N 20° 42.000, W 50° 6.000 26 111 139 Tropical Storm 305 17 990 MB NOAA NHC
13th Sep 2012 11:12:43 N 21° 30.000, W 51° 18.000 26 111 139 Tropical Storm 305 17 990 MB NOAA NHC
14th Sep 2012 05:11:31 N 25° 0.000, W 53° 42.000 24 111 139 Tropical Storm 330 17 989 MB NOAA NHC
15th Sep 2012 06:55:17 N 30° 0.000, W 52° 48.000 22 120 148 Hurricane I. 25 17 985 MB NOAA NHC
15th Sep 2012 10:59:20 N 30° 42.000, W 51° 24.000 24 120 148 Hurricane I. 50 13 985 MB NOAA NHC
16th Sep 2012 05:13:53 N 30° 36.000, W 46° 36.000 28 130 157 Hurricane I. 95 15 983 MB NOAA NHC
17th Sep 2012 05:22:55 N 31° 24.000, W 38° 6.000 30 111 139 Tropical Storm 75 16 987 MB NOAA NHC
17th Sep 2012 10:47:47 N 32° 0.000, W 36° 24.000 28 111 139 Tropical Storm 65 15 985 MB NOAA NHC
18th Sep 2012 05:15:16 N 33° 54.000, W 34° 12.000 15 93 111 Tropical Storm 45 18 989 MB NOAA NHC
18th Sep 2012 10:46:51 N 34° 18.000, W 33° 36.000 13 93 111 Tropical Storm 45 14 990 MB NOAA NHC
19th Sep 2012 05:31:59 N 35° 48.000, W 32° 12.000 11 83 102 Tropical Storm 25 15 993 MB NOAA NHC
19th Sep 2012 11:00:20 N 36° 24.000, W 32° 6.000 7 83 102 Tropical Storm 360 9 993 MB NOAA NHC
20th Sep 2012 05:12:41 N 37° 6.000, W 31° 24.000 6 83 102 Tropical Storm 60 9 990 MB NOAA NHC
20th Sep 2012 11:02:24 N 36° 48.000, W 30° 36.000 15 83 102 Tropical Storm 120 18 983 MB NOAA NHC
21st Sep 2012 10:40:35 N 35° 6.000, W 27° 12.000 13 102 120 Tropical Storm 140 14 981 MB NOAA NHC
22nd Sep 2012 06:38:52 N 31° 54.000, W 26° 36.000 20 93 111 Tropical Storm 165 15 984 MB NOAA NHC
27th Sep 2012 04:58:41 N 29° 30.000, W 31° 24.000 9 83 102 Tropical Storm 220 15 993 MB NOAA NHC
27th Sep 2012 12:03:57 N 28° 54.000, W 31° 30.000 9 93 111 Tropical Storm 220 10 992 MB NOAA NHC
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
27th Sep 2012 16:47:10 N 28° 42.000, W 32° 24.000 11 93 111 Tropical Depression 240 ° 16 993 MB NOAA NHC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
29th Sep 2012 00:00:00 N 30° 0.000, W 35° 48.000 Hurricane I 102 120 NOAA NHC
30th Sep 2012 00:00:00 N 33° 0.000, W 36° 48.000 Tropical Depression 93 111 NOAA NHC
01st Oct 2012 00:00:00 N 35° 30.000, W 37° 30.000 Tropical Depression 93 111 NOAA NHC
02nd Oct 2012 00:00:00 N 36° 0.000, W 37° 30.000 Tropical Depression 83 102 NOAA NHC
Jelewat (18W) Pacific Ocean 20.09.2012 28.09.2012 SuperTyphoon 15 ° 232 km/h 278 km/h 4.27 m JTWC Details

Tropical Storm data

Share:
Storm name: Jelewat (18W)
Area: Pacific Ocean
Start up location: N 13° 42.000, E 132° 18.000
Start up: 20th September 2012
Status: Active
Track long: 805.87 km
Top category.:
Report by: JTWC
Useful links:
Past track
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave Pressure Source
22nd Sep 2012 06:41:44 N 11° 42.000, E 129° 54.000 6 93 120 Tropical Storm 200 9 JTWC
23rd Sep 2012 06:04:26 N 11° 48.000, E 128° 54.000 7 139 167 Typhoon I. 270 11 JTWC
24th Sep 2012 08:06:11 N 13° 36.000, E 128° 30.000 9 241 296 Typhoon IV. 350 10 JTWC
24th Sep 2012 10:43:47 N 14° 12.000, E 128° 12.000 13 232 278 Typhoon IV. 335 14 JTWC
25th Sep 2012 05:16:53 N 15° 42.000, E 127° 48.000 7 259 315 Super Typhoon 360 9 JTWC
25th Sep 2012 10:29:06 N 16° 24.000, E 127° 30.000 15 259 278 Super Typhoon 340 18 JTWC
26th Sep 2012 05:26:43 N 17° 18.000, E 126° 36.000 6 250 306 Typhoon IV. 305 17 JTWC
26th Sep 2012 10:56:11 N 18° 0.000, E 126° 6.000 15 250 306 Typhoon IV. 325 18 JTWC
27th Sep 2012 05:36:14 N 19° 42.000, E 124° 42.000 17 241 296 Typhoon IV. 310 19 JTWC
27th Sep 2012 10:57:01 N 20° 12.000, E 124° 24.000 15 250 306 Typhoon IV. 330 16 JTWC
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
28th Sep 2012 04:38:56 N 22° 24.000, E 124° 6.000 13 232 278 SuperTyphoon 15 ° 14 JTWC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
29th Sep 2012 12:00:00 N 27° 36.000, E 129° 0.000 Typhoon IV 176 213 JTWC
29th Sep 2012 00:00:00 N 25° 42.000, E 126° 48.000 Typhoon IV 204 250 JTWC
30th Sep 2012 12:00:00 N 32° 54.000, E 135° 18.000 Typhoon I 111 139 JTWC
01st Oct 2012 12:00:00 N 39° 6.000, E 144° 12.000 Tropical Depression 65 83 JTWC
Miriam (EP 13) Pacific Ocean – East 22.09.2012 27.09.2012 Tropical Depression 315 ° 65 km/h 83 km/h 4.57 m NOAA NHC Details

Tropical Storm data

Share:
Storm name: Miriam (EP 13)
Area: Pacific Ocean – East
Start up location: N 13° 42.000, W 107° 30.000
Start up: 22nd September 2012
Status: Active
Track long: 822.92 km
Top category.:
Report by: NOAA NHC
Useful links:
Past track
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave Pressure Source
22nd Sep 2012 06:35:22 N 13° 42.000, W 107° 30.000 19 56 74 Tropical Depression 275 10 1005 MB NOAA NHC
23rd Sep 2012 06:07:18 N 14° 54.000, W 108° 30.000 13 74 93 Tropical Storm 300 15 1002 MB NOAA NHC
24th Sep 2012 08:09:13 N 16° 48.000, W 111° 18.000 19 148 185 Hurricane I. 305 15 979 MB NOAA NHC
25th Sep 2012 05:19:32 N 18° 30.000, W 113° 54.000 13 167 204 Hurricane II. 305 14 968 MB NOAA NHC
25th Sep 2012 10:37:14 N 18° 42.000, W 114° 18.000 9 167 204 Hurricane II. 310 10 968 MB NOAA NHC
26th Sep 2012 05:24:31 N 19° 6.000, W 115° 12.000 7 130 157 Hurricane I. 310 9 983 MB NOAA NHC
26th Sep 2012 10:58:11 N 19° 30.000, W 115° 30.000 9 111 139 Tropical Storm 320 15 990 MB NOAA NHC
27th Sep 2012 05:38:27 N 21° 30.000, W 115° 42.000 11 74 93 Tropical Storm 345 12 999 MB NOAA NHC
27th Sep 2012 12:04:18 N 21° 48.000, W 116° 0.000 9 74 93 Tropical Storm 330 15 999 MB NOAA NHC
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
27th Sep 2012 16:46:34 N 22° 12.000, W 116° 18.000 9 65 83 Tropical Depression 315 ° 15 1000 MB NOAA NHC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
29th Sep 2012 00:00:00 N 22° 54.000, W 117° 18.000 Tropical Depression 37 56 NOAA NHC
30th Sep 2012 00:00:00 N 22° 54.000, W 117° 36.000 Tropical Depression 37 56 NOAA NHC
01st Oct 2012 00:00:00 N 22° 30.000, W 118° 0.000 Tropical Depression 28 37 NOAA NHC
Ewiniar (19W) Pacific Ocean 24.09.2012 28.09.2012 Tropical Depression 55 ° 83 km/h 102 km/h 4.57 m JTWC Details

  Tropical Storm data

Share:
Storm name: Ewiniar (19W)
Area: Pacific Ocean
Start up location: N 18° 30.000, E 139° 0.000
Start up: 24th September 2012
Status: Active
Track long: 927.85 km
Top category.:
Report by: JTWC
Useful links:
Past track
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave Pressure Source
24th Sep 2012 08:04:10 N 18° 30.000, E 139° 0.000 26 46 65 Tropical Depression 335 17 JTWC
24th Sep 2012 10:42:45 N 19° 36.000, E 138° 54.000 20 56 74 Tropical Depression 350 17 JTWC
25th Sep 2012 05:14:15 N 21° 48.000, E 138° 18.000 15 74 93 Tropical Storm 355 15 JTWC
25th Sep 2012 10:28:32 N 22° 48.000, E 138° 30.000 19 74 93 Tropical Storm 10 10 JTWC
26th Sep 2012 05:25:41 N 25° 24.000, E 141° 18.000 15 93 120 Tropical Storm 60 16 JTWC
26th Sep 2012 10:53:51 N 26° 24.000, E 142° 12.000 24 93 120 Tropical Storm 40 19 JTWC
27th Sep 2012 05:35:33 N 30° 18.000, E 142° 18.000 22 81 130 Tropical Storm 350 17 JTWC
27th Sep 2012 10:56:30 N 31° 18.000, E 142° 12.000 19 102 130 Tropical Storm 355 15 JTWC
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
28th Sep 2012 04:37:59 N 31° 36.000, E 142° 18.000 9 83 102 Tropical Depression 55 ° 15 JTWC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
29th Sep 2012 12:00:00 N 38° 48.000, E 150° 18.000 Tropical Depression 83 102 JTWC
29th Sep 2012 00:00:00 N 36° 0.000, E 146° 18.000 Typhoon I 93 120 JTWC
30th Sep 2012 12:00:00 N 43° 6.000, E 161° 36.000 Tropical Depression 74 93 JTWC

Taiwan issues warning against Typhoon Jelawat

by Staff Writers
Taipei (AFP)

Taiwan on Thursday issued a warning over a strong typhoon approaching the island which could bring torrential rains and trigger landslides, a month after another heavy storm left six dead.

Residents in the north and east of the island were asked to take precautions against Typhoon Jelawat which is gaining momentum and approaching the island, the Central Weather Bureau said in a statement.

As of 0900 GMT, Jelawat was 380 kilometres (236 miles) southeast of the island’s southern-most tip.

With a radius of 250 kilometres and packing winds of up to 191 kilometres an hour, the typhoon was moving north-northwest at 14 kilometres per hour.

Typhoon Saola pounded Taiwan with fierce winds and torrential rain in August that left six people dead and forced nearly the entire island to shut down.

Related Links
Bringing Order To A World Of Disasters
When the Earth Quakes
A world of storm and tempest

Storms deluge historic British city

by Staff Writers
London (AFP)

Britain’s most severe September storms for 30 years flooded homes and businesses in the historic city of York on Thursday and threatened chaos for much of northern England.

Residents took to boats to navigate the picturesque streets of the city dating from Roman times but officials said flood defences would cope as the River Ouse reached near record levels, three metres (10 feet) higher than normal.

City of York Council insisted the centre was “very much open for business” despite 80 properties being flooded while defences in the nearby village of Cawood were bolstered overnight by 4,000 sandbags.

“Loads of staff have been working through the night to protect the city,” said Sally Burns from the council, who said experts believed the river levels had peaked.

“We need to be careful and make sure we are giving (sandbags) to the people who are a priority, we can see on the monitors where the problems are.”

The Met Office issued more than 50 flood warnings — indicating flooding is expected — and 80 flood alerts – meaning flooding is possible — in England and Wales.

Further rain was forecast for Thursday, putting thousands of home in northern England at risk.

In Newburn, northeast England, a four-storey block of flats teetered on the brink of collapse after floodwaters destroyed its foundations.

Police arrested a man and a woman in connection with the looting of �20,000 ($32,300, 25,000 euros) worth of bicycles from a nearby shop.

Elsewhere, police were investigating the discovery of two bodies on the banks of the swollen River Clywedog in north Wales.

The body of a 27-year-old woman was found on Wednesday and the second body, believed to be male, was discovered on Thursday. Police believe they are linked.

An 11-year-old boy was fighting for his life after being struck by lightning in storms in Swindon, southwest England.

The storms have been caused by an unusually deep area of low pressure but conditions are expected to improve over the next 24 hours.

Related Links
Bringing Order To A World Of Disasters
When the Earth Quakes
A world of storm and tempest

……………………………….

Today Tornado Tonga [Island of Nuiatoputapu] Damage level Details

Tornado in Tonga on Friday, 28 September, 2012 at 10:05 (10:05 AM) UTC.

Description
A family that fled to Tonga’s main island Tongatapu after the devastating tsunami hit the northern island of Nuiatoputapu three years ago had its house destroyed by a tornado on Wednesday. The house in the village of Makaunga was wrecked but no one was hurt. Radio Tonga says the family is now living in tents provided by the Red Cross. The town officer, Siosifa Lamipeti, says the tornado also damaged five power poles affecting supply for about 24 hours. He says there was minor damage to four other houses.

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Epidemic Hazards / Diseases

Today Epidemic Hazard Democratic Republic of the Congo Eastern Province, Mangala Damage level Details

Epidemic Hazard in Democratic Republic of the Congo on Friday, 28 September, 2012 at 02:25 (02:25 AM) UTC.

Description
Bas-Congo virus after the province where it was found just west of Kinshasa, the teeming capital of the Democratic Republic of Congo. The discovery was announced today in the journal PLoS Pathogens. So far only three people in the remote village of Mangala are known to have contracted Bas-Congo hemorrhagic fever, two of whom died. One was a health care worker who cared for the other two villagers, which means it can apparently be transmitted from person to person, although no one knows how easily. But the small number of known cases is actually one of the important things about this finding. It signifies that scientists may have found an emerging disease very soon after it made its jump from whatever species it came from into humans. We’ll come back to its most likely origins a little later. The reason for thinking Bas-Congo only recently began infecting humans is that researchers have run blood tests on people throughout the DRC and found no evidence of antibodies that would indicate any of them has been exposed to the new virus. “It doesn’t appear to be widespread throughout the Congo,” study co-author Charles Chiu of the University of California San Francisco told Shots. He says the team is planning to do more blood tests on people in the DRC and neighboring countries, such as Congo-Brazzaville right next to Bas-Congo province. “I would say we caught it fairly quickly,” said another study author, Joseph Fair, in a telephone interview from the other side of the DRC, where he’s helping to track down the origin of an ongoing outbreak of Ebola hemorrhagic fever that has so far afflicted 51 people and killed 20.

“This wasn’t HIV, where we’re 15 years into a pandemic before we actually find that we have a pandemic,” says Fair, who’s with a group called Metabiota that contracts with governments and health agencies to track disease outbreaks. The three known cases of Bas-Congo fever actually occurred three years ago. But tissue samples from the victims languished in a laboratory freezer in Kinshasa until an astute doctor called the cases to Fair’s attention. That time lag, along with the inability to keep some tissue samples from thawing out, has hampered the researchers’ ability to track the virus through other possible cases in Mangala village. There are some other striking things about the new virus. It doesn’t belong to any of the four families of previously known hemorrhagic viruses – Arenaviridae, Bunyaviridae, Filoviridae and Flaviviridae. These families harbor such notorious bugs as Ebola, Marburg, Lassa fever, Crimean-Congo hemorrhagic fever, dengue fever and Rift Valley Fever. Instead, Bas-Congo belongs to the Rhabdovirus family, which has never been known to include human hemorrhagic fever viruses, although it does contain one that affects fish. “That in itself is astonishing,” Chiu says, “but even within the rhabdovirus family, it’s very divergent.” That is, it doesn’t resemble any other rhabdovirus.

Biohazard name: Bas-Congo hemorrhagic fever
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

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Climate Change

Global Grain Production at Record High Despite Extreme Climatic Events

by Staff Writers
Washington DC (SPX)


File image.

Global grain production is expected to reach a record high of 2.4 billion tons in 2012, an increase of 1 percent from 2011 levels, according to new research conducted by the Worldwatch Institute’s Nourishing the Planet project (www.worldwatch.org) for the Institute’s Vital Signs Online service.

According to the United Nations Food and Agriculture Organization (FAO), the production of grain for animal feed is growing the fastest – a 2.1 percent increase from 2011. Grain for direct human consumption grew 1.1 percent from 2011, write report authors Danielle Nierenberg and Katie Spoden.

In 2011, the amount of grain used for food totaled 571 million tons, with India consuming 89 million tons, China 87 million tons, and the United States 28 million tons, according to the International Grains Council.

The world relies heavily on wheat, maize (corn), and rice for daily sustenance: of the 50,000 edible plants in the world, these three grains account for two-thirds of global food energy intake. Grains provide the majority of calories in diets worldwide, ranging from a 23 percent share in the United States to 60 percent in Asia and 62 percent in North Africa.

Maize production in the United States – the largest producer – was expected to reach a record 345 million tons in 2012; however, drought in the Great Plains has altered this estimate severely. Maize yields for the 2012-13 growing season are now expected to decrease 13 percent from 2011 production, for a total production of 274.3 million tons.

The reliance on grain crops for food security is threatened by more-extreme climatic events, especially droughts and floods. According to the United Nations International Strategy for Disaster Risk Reduction, the World Food Programme, and Oxfam International, some 375 million people will be affected by climate change-related disasters by 2015.

By 2050, the FAO notes, 10-20 percent more people will be subject to hunger based on the changing climate’s effects on agriculture, and 24 million more children are expected to be malnourished – 21 percent more than if there were no climate change.

“The relationship between food security, grain production, and climate change is especially important in 2012,” said Nierenberg, a Worldwatch senior researcher and Nourishing the Planet project director.

“The recent drought affecting the United States and the rest of the world show the need to reduce price volatility, move away from fossil fuel-based agriculture, and recognize the importance of women farmers to increase resilience to climate change.”

The drought taking place in the Midwest and Great Plains of the United States is considered the country’s worst in 50 years, coming close to matching the late-1930s Dust Bowl.

The drought is expected to cost many billions of dollars and could top the list as one of the most expensive weather-related disasters in U.S. history. The global market will be most affected by this drought, as so much of the developing world relies on U.S. corn and soybean production.

Food prices have already begun to increase due to lower yields, and price fluctuations will inevitably affect food security around the globe.

Further highlights from the report:

+ The FAO expects global maize production to increase 4.1 percent from 2011, reaching an estimated 916 million tons in 2012.

+ Global rice production achieved an all-time high of 480 million tons in 2011, a 2.6 percent increase from 2010.

+ World wheat production is projected to drop to 675.1 million tons in 2012, down 3.6 percent from 2011, with the largest declines in feed and biofuel utilization.

+ Since 1961, grain production has increased 269 percent and grain yield has increased 157 percent, while the grain harvest area has increased only 25 percent.

+ This is due largely to the Green Revolution and the introduction of high-yielding grain varieties.

Related Links
Worldwatch Institute
Farming Today – Suppliers and Technology

Loss of species makes nature more sensitive to climate change

by Staff Writers
Gothenburg, Sweden (SPX)


File image.

High biodiversity acts as an insurance policy for nature and society alike as it increases the likelihood that at least some species will be sufficiently resilient to sustain important functions such as water purification and crop pollination in a changing environment.

“It’s the same principle as an investment portfolio – you’d be mad to put all your eggs in one basket,” says researcher Johan Eklof.

Experiments with eelgrass meadows in shallow inlets on the west coast of Sweden are now showing that climate change can exacerbate the negative effects of losing sensitive species, and that the insurance effect of biodiversity may be weaker than what we typically assume.

Eelgrass meadows in shallow inlets are important nursery habitats for cod, for example. Since the early 1980s the prevalence of eelgrass has fallen dramatically along the Bohuslan coast.

This is thought to be due partly to eutrophication, which favours mats of filamentous “nuisance” algae which shade and suffocate the eelgrass, and partly to the loss of cod, which has resulted in a huge increase in numbers of smaller predatory fish.

These predatory fish, in turn, reduce numbers of Grammarus locusta, herbivorous crustaceans which are effective grazers that normally control the filamentous algae.

This type of cascade effect has become increasingly common both onshore and off as many types of predator have been wiped out by hunting or fishing. Worryingly, theory and observations would indicate that these effects could magnify the effects of global warming, which favours heat-tolerant but grazing-sensitive plants such as filamentous algae.

At the Sven Loven Centre for Marine Sciences’ Kristineberg research station on Gullmarsfjorden, researchers from the University of Gothenburg’s Department of Biology and Environmental Sciences have developed miniature ecosystems in outdoor aquariums and have been investigating how future ocean warming and ocean acidification could affect the balance between eelgrass and filamentous algae.

The effects were unexpectedly clear and unambiguous: it was the diversity of algal herbivores that determined the extent to which the ecosystem was affected by warming and acidification.

“High diversity meant that neither warming nor acidification had any real effect as the algae were eaten before they managed to grow and shade the eelgrass,” says researcher and biologist Johan Eklof, who headed up the study.

“But when we simultaneously simulated the effects of fishing and removed the effective but vulnerable herbivor Grammarus locusta, the algae took over the ecosystem – especially in the warmer conditions.”

The researchers believe that we should be concerned about the results.

“Most management is based on the assumption that we afford to lose the most sensitive species because other, more resilient species will take their place,” says Johan Eklof. “But this may not be the case with future climate changes, as it can reduce the net efficiency of the resilient species – without directly affecting them.”

However, the researchers are also careful to point out that there is still hope if society does decide to take action.

“If we protect the local biodiversity we still have, and restore the diversity we’ve lost, by for example protecting predatory fish stocks in coastal areas and reducing nutrient loading, then we’ll probably be able to increase the ecosystems’ resilience to climate change.”

Related Links
University of Gothenburg
Climate Science News – Modeling, Mitigation Adaptation

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Solar Activity

.

3MIN News Sept 27. 2012

Published on Sep 27, 2012 by

TODAY’S LINKS
Global Aftershocks: http://phys.org/news/2012-09-sumatra-earthquake-triggered-temblors-worldwide….
The Ripping Fault Lines: http://phys.org/news/2012-09-sumatra-quake-crustal-plate-breakup.html
[Old Article] Croatian Scientist says Earth Ripping Apart: http://www.croatiantimes.com/news/Around_the_World/2012-04-15/26423/Quake_Exp…
ISS Debris Threat: http://phys.org/news/2012-09-space-debris-threatens-iss.html
Russia Suspends Monsanto: http://phys.org/news/2012-09-russia-monsanto-corn-imports.html
100M Dead in 18 Years: http://www.weather.com/news/100-million-could-die-due-to-climate-20120926

REPEAT LINKS
Spaceweather: http://spaceweather.com/ [Look on the left at the X-ray Flux and Solar Wind Speed/Density]

HAARP: http://www.haarp.alaska.edu/haarp/data.html [Click online data, and have a little fun]

SDO: http://sdo.gsfc.nasa.gov/data/ [Place to find Solar Images and Videos - as seen from earth]

SOHO: http://sohodata.nascom.nasa.gov/cgi-bin/soho_movie_theater [SOHO; Lasco and EIT - as seen from earth]

Stereo: http://stereo.gsfc.nasa.gov/cgi-bin/images [Stereo; Cor, EUVI, HI - as seen from the side]

SunAEON:http://www.sunaeon.com/#/solarsystem/ [Just click it... trust me]

SOLARIMG: http://solarimg.org/artis/ [All purpose data viewing site]

iSWA: http://iswa.gsfc.nasa.gov/iswa/iSWA.html [Free Application; for advanced sun watchers]

NASA ENLIL SPIRAL: http://iswa.gsfc.nasa.gov:8080/IswaSystemWebApp/iSWACygnetStreamer?timestamp=…
NOAA ENLIL SPIRAL: http://www.swpc.noaa.gov/wsa-enlil/

US Wind Map: http://hint.fm/wind/

NOAA Bouys: http://www.ndbc.noaa.gov/

NOAA Environmental Visualization Laboratory: http://www.nnvl.noaa.gov/Default.php

RSOE: http://hisz.rsoe.hu/alertmap/index2.php [That cool alert map I use]

GOES Xray: http://www.swpc.noaa.gov/sxi/goes15/index.html

JAPAN Radiation Map: http://jciv.iidj.net/map/

LISS: http://earthquake.usgs.gov/monitoring/operations/heliplots_gsn.php

Gamma Ray Bursts: http://grb.sonoma.edu/ [Really? You can't figure out what this one is for?]

BARTOL Cosmic Rays: http://neutronm.bartol.udel.edu//spaceweather/welcome.html [Top left box, look for BIG blue circles]

TORCON: http://www.weather.com/news/tornado-torcon-index [Tornado Forecast for the day]

GOES Weather: http://rsd.gsfc.nasa.gov/goes/ [Clouds over America]

RAIN RECORDS: http://www.cocorahs.org/ViewData/ListIntensePrecipReports.aspx

EL DORADO WORLD WEATHER MAP: http://www.eldoradocountyweather.com/satellite/ssec/world/world-composite-ir-…

PRESSURE MAP: http://www.woweather.com/cgi-bin/expertcharts?LANG=us&MENU=0000000000&…

HURRICANE TRACKER: http://www.weather.com/weather/hurricanecentral/tracker

INTELLICAST: http://www.intellicast.com/ [Weather site used by many youtubers]

NASA News: http://science.nasa.gov/science-news/science-at-nasa/

PHYSORG: http://phys.org/ [GREAT News Site!]

QUAKES LIST FULL: http://www.emsc-csem.org/Earthquake/seismologist.php

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Space

  Earth approaching objects (objects that are known in the next 30 days)

Object Name Apporach Date Left AU Distance LD Distance Estimated Diameter* Relative Velocity
(2012 SY49) 28th September 2012 0 day(s) 0.0067 2.6 19 m – 42 m 15.84 km/s 57024 km/h
(2012 SJ32) 28th September 2012 0 day(s) 0.0297 11.6 26 m – 59 m 8.11 km/s 29196 km/h
(2012 SM50) 30th September 2012 2 day(s) 0.1074 41.8 36 m – 81 m 8.68 km/s 31248 km/h
(2012 RH10) 03rd October 2012 5 day(s) 0.1260 49.0 98 m – 220 m 12.90 km/s 46440 km/h
(2012 QE50) 09th October 2012 11 day(s) 0.0809 31.5 450 m – 1.0 km 11.47 km/s 41292 km/h
(1994 EK) 14th October 2012 16 day(s) 0.1356 52.8 230 m – 520 m 12.22 km/s 43992 km/h
(2012 PA20) 15th October 2012 17 day(s) 0.1502 58.5 100 m – 230 m 10.36 km/s 37296 km/h
(2012 RV16) 18th October 2012 20 day(s) 0.1270 49.4 310 m – 700 m 16.14 km/s 58104 km/h
1 AU = ~150 million kilometers,1 LD = Lunar Distance = ~384,000 kilometers Source: NASA-NEO

 

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Biological Hazards / Wildlife / Hazmat

HAZMAT in USA on Thursday, 27 September, 2012 at 18:30 (06:30 PM) UTC.

Description
Nine people were taken to the hospital following a chemical spill at West Knox Co. Veteran’s Home. All of the victims were suffering from respiratory problems, one of them was being treated as an emergency. Authorities called it a concentrated chlorine spill. They said it happened shortly after 9:30 a.m. at Ben Atchley State Veterans’ Home in Karns. The home was evacuated and the scene is being treated as a hazmat situation.

 

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