Tag Archive: Pacific Ocean


Earth Watch Report  -  Storms

Tropical Storm ALVIN NHC 5-Day Cone Tropical Storm 01E (ALVIN) JTWC ATCF Track
Tropical Storm
ALVIN
NHC 5-Day Cone
Tropical Storm
01E (ALVIN)
JTWC ATCF Track

Active tropical storm system(s)
Alvin (01E) Pacific Ocean – East 14.05.2013 16.05.2013 Tropical Depression 290 ° 74 km/h 93 km/h 3.05 m NOAA NHC Details
Name of storm system Location Formed Last update Last category Course Wind Speed Gust Wave Source Details

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Tropical Storm data

Storm name: Alvin (01E)
Area: Pacific Ocean – East
Start up location: N 8° 12.000, W 103° 36.000
Start up: 15th May 2013
Status: Active
Track long: 166.53 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
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
16th May 2013 04:45:41 N 9° 0.000, W 105° 54.000 19 74 93 Tropical Depression 290 ° 10 1004 MB NOAA NHC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
17th May 2013 00:00:00 N 9° 30.000, W 108° 54.000 Hurricane I 102 120 NOAA NHC
17th May 2013 12:00:00 N 10° 0.000, W 110° 24.000 Hurricane I 120 148 NOAA NHC
18th May 2013 12:00:00 N 11° 30.000, W 113° 0.000 Hurricane II 130 157 NOAA NHC
19th May 2013 12:00:00 N 13° 0.000, W 115° 30.000 Hurricane I 120 148 NOAA NHC
20th May 2013 12:00:00 N 15° 30.000, W 117° 0.000 Hurricane I 102 120 NOAA NHC

 

Tropical Storm Alvin strengthens in eastern Pacific

By Ed Payne and Greg Botelho, CNN
updated 12:46 AM EDT, Thu May 16, 2013
STORY HIGHLIGHTS
  • Tropical Storm Alvin is centered about 700 miles south of Manzanillo, Mexico
  • It’s the first named storm of Eastern Pacific season, which opened Wednesday
  • It had maximum sustained winds of 45 mph
  • Alvin should strengthen and “is expected become a hurricane,” the hurricane center reports

(CNN) — The hurricane season opened Wednesday with a flourish, and more specifically, with the debut of its first named storm, Tropical Storm Alvin.

Tropical Depression 1-E was upgraded and named a tropical storm Wednesday, which happens to be the first day of the Eastern Pacific hurricane season, according to the National Hurricane Center.

The Atlantic hurricane season officially starts on June 1, and both seasons end November 30.

Read More Here

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Earth Watch Report  -  Earthquakes

 photo Russia-56MagEQMay12th2013_zps3add8c7c.jpg

M5.6 – 91km ENE of Shikotan, Russia 2013-05-12 22:42:45 UTC

 



Earthquake location 44.026°N, 147.811°E

Event Time

  1. 2013-05-12 22:42:45 UTC
  2. 2013-05-13 08:42:45 UTC+10:00 at epicenter
  3. 2013-05-12 17:42:45 UTC-05:00 system time

Location

44.026°N 147.811°E depth=53.4km (33.2mi)

Nearby Cities

  1. 91km (57mi) ENE of Shikotan, Russia
  2. 196km (122mi) ENE of Nemuro, Japan
  3. 219km (136mi) ENE of Shibetsu, Japan
  4. 283km (176mi) E of Abashiri, Japan
  5. 1156km (718mi) NE of Tokyo, Japan

 

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Tectonic Summary

Seismotectonics of the Kuril-Kamchatka Arc

The Kuril-Kamchatka arc extends approximately 2,100 km from Hokkaido, Japan, along the Kuril Islands and the Pacific coast of the Kamchatka Peninsula to its intersection with the Aleutian arc near the Commander Islands, Russia. It marks the region where the Pacific plate subducts into the mantle beneath the Okhotsk microplate, part of the larger North America plate. This subduction is responsible for the generation of the Kuril Islands chain, active volcanoes located along the entire arc, and the deep offshore Kuril-Kamchatka trench. Relative to a fixed North America plate, the Pacific plate is moving towards the northwest at a rate that increases from 75 mm/year near the northern end of the arc to 83 mm/year in the south.

Plate motion is predominantly convergent along the Kuril-Kamchatka arc with obliquity increasing towards the southern section of the arc. The subducting Pacific plate is relatively old, particularly adjacent to Kamchatka where its age is greater than 100 Ma. Consequently, the Wadati-Benioff zone is well defined to depths of approximately 650 km. The central section of the arc is comprised of an oceanic island arc system, which differs from the continental arc systems of the northern and southern sections. Oblique convergence in the southern Kuril arc results in the partitioning of stresses into both trench-normal thrust earthquakes and trench-parallel strike-slip earthquakes, and the westward translation of the Kuril forearc. This westward migration of the Kuril forearc currently results in collision between the Kuril arc in the north and the Japan arc in the south, resulting in the deformation and uplift of the Hidaka Mountains in central Hokkaido.

The Kuril-Kamchatka arc is considered one of the most seismically active regions in the world. Deformation of the overriding North America plate generates shallow crustal earthquakes, whereas slip at the subduction zone interface between the Pacific and North America plates generates interplate earthquakes that extend from near the base of the trench to depths of 40 to 60 km. At greater depths, Kuril-Kamchatka arc earthquakes occur within the subducting Pacific plate and can reach depths of approximately 650 km.

This region has frequently experienced large (M>7) earthquakes over the past century. Since 1900, seven great earthquakes (M8.3 or larger) have also occurred along the arc, with mechanisms that include interplate thrust faulting, and intraplate faulting. Damaging tsunamis followed several of the large interplate megathrust earthquakes. These events include the February 3, 1923 M8.4 Kamchatka, the November 6,1958 M8.4 Etorofu, and the September 25, 2003 M8.3 Hokkaido earthquakes. A large M8.5 megathrust earthquake occurred on October 13, 1963 off the coast of Urup, an island along the southern Kuril arc, which generated a large tsunami in the Pacific Ocean and the Sea of Okhotsk, and caused run-up wave heights of up to 4-5 m along the Kuril arc. The largest megathrust earthquake to occur along the entire Kurile-Kamchatka arc in the 20th century was the November 4, 1952 M9.0 event. This earthquake was followed by a devastating tsunami with run-up wave heights as high as 12 m along the coast of Paramushir, a small island immediately south of Kamchatka, causing significant damage to the city of Severo-Kurilsk.

On October 4,1994, a large (M8.3) intraplate event occurred within the subducted oceanic lithosphere off the coast of Shikotan Island causing intense ground shaking, landslides, and a tsunami with run-up heights of up to 10 m on the island.

The most recent megathrust earthquake in the region was the November 15, 2006 M8.3 Kuril Island event, located in the central section of the arc. Prior to this rupture, this part of the subduction zone had been recognized as a seismic gap spanning from the northeastern end of the 1963 rupture zone to the southwestern end of the 1952 rupture. Two months after the 2006 event, a great (M8.1) normal faulting earthquake occurred on January 13, 2007 in the adjacent outer rise region of the Pacific plate. It has been suggested that the 2007 event may have been caused by the stresses generated from the 2006 earthquake.

More information on regional seismicity and tectonics

 

 

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Russia  -  5 Earthquakes Ranging From 5.4 to 4.5 Magnitude,  May  10th , 2013 .  Total of  6 EQ’s in the last  2 days

 

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Russia  -  4.3  Magnitude Earthquake – 105km SE of Ozernovskiy

 

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CLIMATE SCIENCE

Pacific’s Marshall Islands facing drought emergency


by Staff Writers
Majuro (AFP) Marshall Islands (AFP) May 8, 2013

A drought has left areas of the Marshall Islands facing “dire” water shortages with aid agencies scrambling to ship relief to affected communities, officials in the Pacific nation said Wednesday.

With almost no rainfall since late last year on some of the northern islands, the government this week issued a disaster declaration as villages began rationing water to preserve supplies.

“We’ve got 3,700 people without drinking water, the situation is dire,” national water advisor Tom Vance said on Wednesday following a trip to Mejit Island.

Health officials said water tanks were running low and water from wells had turned brackish, making it unsafe to drink. Without rain, the only other source of liquid for the islanders is coconuts.

 

Read Full Article Here

 

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Marshall Islands face acute water shortage

Australia and US offer desalination and reverse-osmosis units as severe drought worsens in Pacific archipelago

  • Associated Press in Majuro
  • guardian.co.uk, Friday 10 May 2013 02.30 EDT
Marshall Islands

The Marshall Islands have declared a state of disaster in the north of the archipelago. Photograph: Doug Wilson/Corbis

About 6,000 people who live on the remote Marshall Islands in the Pacific are facing an acute shortage of fresh water as a severe drought worsens.

A state of disaster was declared in the north. Australia announced it would provide AU$100,000 (£65,335) for emergency desalination units. The US has also donated several reverse-osmosis machines, which convert salt water into fresh water.

There is no end in sight to the drought, with fine weather forecast for at least the next 10 days. The drought has also affected the food supply, hitting crops such as breadfruit, bananas and taro.

Casten Nemra, who chairs the national disaster committee, said many large families were surviving on as little as 4.5 litres of water a day.

 

Read Full Article Here

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2006-1130supernova

 

While there is, on average, only one supernova per galaxy per century, there is something on the order of 100 billion galaxies in the observable Universe. Taking 10 billion years for the age of the Universe (it’s actually 13.7 billion, but stars didn’t form for the first few hundred million), Dr. Richard Mushotzky of the NASA Goddard Space Flight Center, derived a figure of 1 billion supernovae per year, or 30 supernovae per second in the observable Universe. Now, scientists at the Technische Universitaet Muenchen have discovered the first proven biological evidence of a nearby supernova explosion on earth, finding hints of supernova iron in bacteria microfossils.

Researchers of the Cluster of Excellence Origin and Structure of the Universe at the Technische Universitaet Muenchen (TUM), found a radioactive iron isotope in fossils of iron-loving bacteria that they trace back to a supernova in our cosmic neighborhood. This is the first proven biological signature of a starburst on our earth. The age determination of the deep-drill core from the Pacific Ocean showed that the supernova must have occurred about 2.2 million years ago, roughly around the time when the modern human developed.

Most of the chemical elements have their origin in core collapse supernovae. When a star ends its life in a gigantic starburst, it throws most of its mass into space. The radioactive iron isotope Fe-60 is produced almost exclusively in such supernovae. Because its half-life of 2.62 million years is short compared to the age of our solar system, no supernova iron should be present on Earth. Therefore, any discovery of Fe-60 on Earth would indicate a supernova in our cosmic neighborhood. In the year 2004 scientists at TU Muenchen discovered Fe-60 on Earth for the first time in a ferromanganese crust obtained from the floor of the equatorial Pacific Ocean. Its geological dating puts the event around 2.2 million years ago.

 

Read Full Article Here

Earth Watch Report  -  Earthquakes

Russia  4.3 mag  May 9th  2013 photo Russia43magMay9th2013_zpsf0690007.jpg
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M4.3 – 105km SE of Ozernovskiy, Russia 2013-05-09 16:17:45 UTC

Earthquake location 50.946°N, 157.744°E

Event Time

  1. 2013-05-09 16:17:45 UTC
  2. 2013-05-10 03:17:45 UTC+11:00 at epicenter
  3. 2013-05-09 11:17:45 UTC-05:00 system time

Location

50.946°N 157.744°E depth=45.6km (28.3mi)

Nearby Cities

  1. 105km (65mi) SE of Ozernovskiy, Russia
  2. 225km (140mi) SSW of Vilyuchinsk, Russia
  3. 241km (150mi) SSW of Petropavlovsk-Kamchatskiy, Russia
  4. 253km (157mi) S of Yelizovo, Russia
  5. 2227km (1384mi) NE of Tokyo, Japan

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Tectonic Summary

Seismotectonics of the Kuril-Kamchatka Arc

The Kuril-Kamchatka arc extends approximately 2,100 km from Hokkaido, Japan, along the Kuril Islands and the Pacific coast of the Kamchatka Peninsula to its intersection with the Aleutian arc near the Commander Islands, Russia. It marks the region where the Pacific plate subducts into the mantle beneath the Okhotsk microplate, part of the larger North America plate. This subduction is responsible for the generation of the Kuril Islands chain, active volcanoes located along the entire arc, and the deep offshore Kuril-Kamchatka trench. Relative to a fixed North America plate, the Pacific plate is moving towards the northwest at a rate that increases from 75 mm/year near the northern end of the arc to 83 mm/year in the south.

Plate motion is predominantly convergent along the Kuril-Kamchatka arc with obliquity increasing towards the southern section of the arc. The subducting Pacific plate is relatively old, particularly adjacent to Kamchatka where its age is greater than 100 Ma. Consequently, the Wadati-Benioff zone is well defined to depths of approximately 650 km. The central section of the arc is comprised of an oceanic island arc system, which differs from the continental arc systems of the northern and southern sections. Oblique convergence in the southern Kuril arc results in the partitioning of stresses into both trench-normal thrust earthquakes and trench-parallel strike-slip earthquakes, and the westward translation of the Kuril forearc. This westward migration of the Kuril forearc currently results in collision between the Kuril arc in the north and the Japan arc in the south, resulting in the deformation and uplift of the Hidaka Mountains in central Hokkaido.

The Kuril-Kamchatka arc is considered one of the most seismically active regions in the world. Deformation of the overriding North America plate generates shallow crustal earthquakes, whereas slip at the subduction zone interface between the Pacific and North America plates generates interplate earthquakes that extend from near the base of the trench to depths of 40 to 60 km. At greater depths, Kuril-Kamchatka arc earthquakes occur within the subducting Pacific plate and can reach depths of approximately 650 km.

This region has frequently experienced large (M>7) earthquakes over the past century. Since 1900, seven great earthquakes (M8.3 or larger) have also occurred along the arc, with mechanisms that include interplate thrust faulting, and intraplate faulting. Damaging tsunamis followed several of the large interplate megathrust earthquakes. These events include the February 3, 1923 M8.4 Kamchatka, the November 6,1958 M8.4 Etorofu, and the September 25, 2003 M8.3 Hokkaido earthquakes. A large M8.5 megathrust earthquake occurred on October 13, 1963 off the coast of Urup, an island along the southern Kuril arc, which generated a large tsunami in the Pacific Ocean and the Sea of Okhotsk, and caused run-up wave heights of up to 4-5 m along the Kuril arc. The largest megathrust earthquake to occur along the entire Kurile-Kamchatka arc in the 20th century was the November 4, 1952 M9.0 event. This earthquake was followed by a devastating tsunami with run-up wave heights as high as 12 m along the coast of Paramushir, a small island immediately south of Kamchatka, causing significant damage to the city of Severo-Kurilsk.

On October 4,1994, a large (M8.3) intraplate event occurred within the subducted oceanic lithosphere off the coast of Shikotan Island causing intense ground shaking, landslides, and a tsunami with run-up heights of up to 10 m on the island.

The most recent megathrust earthquake in the region was the November 15, 2006 M8.3 Kuril Island event, located in the central section of the arc. Prior to this rupture, this part of the subduction zone had been recognized as a seismic gap spanning from the northeastern end of the 1963 rupture zone to the southwestern end of the 1952 rupture. Two months after the 2006 event, a great (M8.1) normal faulting earthquake occurred on January 13, 2007 in the adjacent outer rise region of the Pacific plate. It has been suggested that the 2007 event may have been caused by the stresses generated from the 2006 earthquake.

More information on regional seismicity and tectonics

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Earth Watch Report  -  Earthquakes

Mexico - 2 EQs  May 9th   2013 photo Mexico-2EQsMay9th2013_zpsc81f831a.jpg
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M4.1 – 44km SSW of Puerto Madero, Mexico 2013-05-09 05:25:11 UTC

Earthquake location 14.366°N, 92.617°W

Event Time

  1. 2013-05-09 05:25:11 UTC
  2. 2013-05-08 23:25:11 UTC-06:00 at epicenter
  3. 2013-05-09 00:25:11 UTC-05:00 system time

Location

14.366°N 92.617°W depth=35.1km (21.8mi)

Nearby Cities

  1. 44km (27mi) SSW of Puerto Madero, Mexico
  2. 47km (29mi) WSW of Suchiate, Mexico
  3. 60km (37mi) WSW of Ciudad Tecun Uman, Guatemala
  4. 69km (43mi) SSW of Tapachula, Mexico
  5. 228km (142mi) W of Guatemala City, Guatemala

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M4.5 – 10km SSW of Putla de Guerrero, Mexico 2013-05-09 19:30:11 UTC

Earthquake location 16.948°N, 97.970°W

Event Time

  1. 2013-05-09 19:30:11 UTC
  2. 2013-05-09 12:30:11 UTC-07:00 at epicenter
  3. 2013-05-09 14:30:11 UTC-05:00 system time

Location

16.948°N 97.970°W depth=21.7km (13.5mi)

Nearby Cities

  1. 10km (6mi) SSW of Putla de Guerrero, Mexico
  2. 46km (29mi) SW of Santa Maria Asuncion Tlaxiaco, Mexico
  3. 55km (34mi) ENE of Ometepec, Mexico
  4. 70km (43mi) N of Santiago Pinotepa Nacional, Mexico
  5. 300km (186mi) SSE of Mexico City, Mexico

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Tectonic Summary

Seismotectonics of Mexico

Located atop three of the large tectonic plates, Mexico is one of the world’s most seismologically active regions. The relative motion of these crustal plates causes frequent earthquakes and occasional volcanic eruptions. Most of the Mexican landmass is on the westward moving North American plate. The Pacific Ocean floor south of Mexico is being carried northeastward by the underlying Cocos plate. Because oceanic crust is relatively dense, when the Pacific Ocean floor encounters the lighter continental crust of the Mexican landmass, the ocean floor is subducted beneath the North American plate creating the deep Middle American trench along Mexico’s southern coast. Also as a result of this convergence, the westward moving Mexico landmass is slowed and crumpled creating the mountain ranges of southern Mexico and earthquakes near Mexico’s southern coast. As the oceanic crust is pulled downward, it melts; the molten material is then forced upward through weaknesses in the overlying continental crust. This process has created a region of volcanoes across south-central Mexico known as the Cordillera Neovolcánica.

The area west of the Gulf of California, including Mexico’s Baja California Peninsula, is moving northwestward with the Pacific plate at about 50 mm per year. Here, the Pacific and North American plates grind past each other creating strike-slip faulting, the southern extension of California’s San Andreas fault. In the past, this relative plate motion pulled Baja California away from the coast forming the Gulf of California and is the cause of earthquakes in the Gulf of California region today.

Mexico has a long history of destructive earthquakes and volcanic eruptions. In September 1985, a magnitude 8.1 earthquake killed more than 9,500 people in Mexico City. In southern Mexico, Volcán de Colima and El Chichón erupted in 2005 and 1982, respectively. Paricutín volcano, west of Mexico City, began venting smoke in a cornfield in 1943; a decade later this new volcano had grown to a height of 424 meters. Popocatépetl and Ixtaccíhuatl volcanos (“smoking mountain” and “white lady”, respectively), southeast of Mexico City, occasionally vent gas that can be clearly seen from the City, a reminder that volcanic activity is ongoing. In 1994 and 2000 Popocatépetl renewed its activity forcing the evacuation of nearby towns, causing seismologists and government officials to be concerned about the effect a large-scale eruption might have on the heavily populated region. Popocatépetl volcano last erupted in 2010.

More information on regional seismicity and tectonics

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Kyodo News, via Associated Press

Gray and silver storage tanks filled with radioactive wastewater are sprawling over the grounds of the Fukushima Daiichi plant.

TOKYO — Two years after a triple meltdown that grew into the world’s second worst nuclear disaster, the Fukushima Daiichi nuclear power plant is faced with a new crisis: a flood of highly radioactive wastewater that workers are struggling to contain.

Multimedia

Groundwater is pouring into the plant’s ravaged reactor buildings at a rate of almost 75 gallons a minute. It becomes highly contaminated there, before being pumped out to keep from swamping a critical cooling system. A small army of workers has struggled to contain the continuous flow of radioactive wastewater, relying on hulking gray and silver storage tanks sprawling over 42 acres of parking lots and lawns. The tanks hold the equivalent of 112 Olympic-size pools.

But even they are not enough to handle the tons of strontium-laced water at the plant — a reflection of the scale of the 2011 disaster and, in critics’ view, ad hoc decision making by the company that runs the plant and the regulators who oversee it. In a sign of the sheer size of the problem, the operator of the plant, Tokyo Electric Power Company, or Tepco, plans to chop down a small forest on its southern edge to make room for hundreds more tanks, a task that became more urgent when underground pits built to handle the overflow sprang leaks in recent weeks.

“The water keeps increasing every minute, no matter whether we eat, sleep or work,” said Masayuki Ono, a general manager with Tepco who acts as a company spokesman. “It feels like we are constantly being chased, but we are doing our best to stay a step in front.”

While the company has managed to stay ahead, the constant threat of running out of storage space has turned into what Tepco itself called an emergency, with the sheer volume of water raising fears of future leaks at the seaside plant that could reach the Pacific Ocean.

That quandary along with an embarrassing string of mishaps — including a 29-hour power failure affecting another, less vital cooling system — have underscored an alarming reality: two years after the meltdowns, the plant remains vulnerable to the same sort of large earthquake and tsunami that set the original calamity in motion.

There is no question that the Fukushima plant is less dangerous than it was during the desperate first months after the accident, mostly through the determined efforts of workers who have stabilized the melted reactor cores, which are cooler and less dangerous than they once were.

But many experts warn that safety systems and fixes at the plant remain makeshift and prone to accidents.

The jury-rigged cooling loop that pours water over the damaged reactor cores is a mazelike collection of pumps, filters and pipes that snake two and a half miles along the ground through the plant. And a pool for storing used nuclear fuel remains perched on the fifth floor of a damaged reactor building as Tepco struggles to move the rods to a safer location.

The situation is worrisome enough that Shunichi Tanaka, a longtime nuclear power proponent who is the chairman of the newly created watchdog Nuclear Regulation Authority, told reporters after the announcement of the leaking pits that “there is concern that we cannot prevent another accident.”

A growing number of government officials and advisers now say that by entrusting the cleanup to the company that ran the plant before the meltdowns, Japanese leaders paved the way for a return to the insider-dominated status quo that prevailed before the disaster.

Even many scientists who acknowledge the complexity of cleaning up the worst nuclear disaster since Chernobyl fear that the water crisis is just the latest sign that Tepco is lurching from one problem to the next without a coherent strategy.

“Tepco is clearly just hanging on day by day, with no time to think about tomorrow, much less next year,” said Tadashi Inoue, an expert in nuclear power who served on a committee that drew up the road map for cleaning up the plant.

But the concerns extend well beyond Tepco. While doing a more rigorous job of policing Japan’s nuclear industry than regulators before the accident, the Nuclear Regulation Authority has a team of just nine inspectors to oversee the more than 3,000 workers at Fukushima.

And a separate committee created by the government to oversee the cleanup is loaded with industry insiders, including from the Ministry of Trade, in charge of promoting nuclear energy, and nuclear reactor manufacturers like Toshiba and Hitachi. The story of how the Fukushima plant ended up swamped with water, critics say, is a cautionary tale about the continued dangers of leaving decisions about nuclear safety to industry insiders.

Read  Full Article Here

Related

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Nuclear power plant stricken in 2011 tsunami now leaking radioactive groundwater: report

The water contains strontium, a byproduct of nuclear fission, and the Fukushima Dai-ichi plant is leaking it at a rate of 75 gallons per minute.

Wednesday, May 1, 2013, 2:35 PM
1K
43
1
http://assets.nydailynews.com/polopoly_fs/1.1332272.1367432781%21/img/httpImage/image.jpg_gen/derivatives/landscape_635/japan-fukushima.jpg” width=”635″ height=”423″ />

© Issei Kato / Reuters/REUTERS

Members of the media wear protective suits at the tsunami-crippled Fukushima Daiichi nuclear power plant in Fukushima prefecture in March. Two years after the disaster, contaminated groundwater containing radioactive strontium, a byproduct of nuclear fission, is leaking from the damaged reactor.

The Japanese nuclear plant stricken by a deadly tsunami two years ago is facing the dire issue of containing radioactive waste water, as operators rush to repair yet another possible disaster.

The March 11, 2011 earthquake and tsunami left the Fukushima Dai-ichi plant stricken, badly damaging its reactors, which serve to cool nuclear cores.

Now contaminated groundwater containing radioactive strontium, a byproduct of nuclear fission, is leaking from damaged reactor structures at an alarming rate of 75 gallons per minute.

PHOTOS: TOP 20 PHOTOS OF JAPAN TSUNAMI

Tanks of radiation-contaminated water are stored onsite at Fukishima.

© KYODO Kyodo / Reuters/REUTERS

Tanks of radiation-contaminated water are stored onsite at Fukishima.

The Dai-Ichi plant is owned by the Tokyo Electric Power Company, also known as Tepco, which has struggled to handle the plant’s meltdown and subsequent recovery.

The nuclear incident has been described as one of the most devastating in history, second only to Russia’s Chernobyl incident of the 1980s.

As the New York Times notes, news of the leaking groundwater comes at an embarrassing time for Tepco, which experienced a 29-hour power outage last month which affected another of the plant’s cooling systems.

RELATED: RADIOACTIVE WATER LEAK FEARED AT JAPAN NUKE PLANT

 

Read Full Article Here

Earth  Watch Report – Storms

Tropical Cyclone 23P (ZANE) ATCF Track

Tropical Cyclone
23P (ZANE)
JTWC ATCF Track

 Active tropical storm system(s)
Name of storm system Location Formed Last update Last category Course Wind Speed Gust Wave Source Details
Zane (23P) Pacific Ocean – South 29.04.2013 02.05.2013 Tropical Depression 310 ° 65 km/h 83 km/h 5.49 m JTWC Details

  Tropical Storm data

Storm name: Zane (23P)
Area: Pacific Ocean – South
Start up location: S 13° 54.000, E 150° 12.000
Start up: 30th April 2013
Status: 02nd May 2013
Track long: 395.34 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
30th Apr 2013 04:44:37 S 13° 54.000, E 150° 12.000 22 65 83 Tropical Storm 250 12 JTWC
30th Apr 2013 11:13:56 S 14° 6.000, E 149° 30.000 13 111 139 Tropical Storm 255 14 JTWC
01st May 2013 05:30:57 S 14° 12.000, E 148° 18.000 9 111 139 Tropical Storm 260 35 JTWC
01st May 2013 13:03:18 S 13° 48.000, E 146° 48.000 13 102 130 Tropical Storm 280 23 JTWC
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
02nd May 2013 05:42:19 S 12° 30.000, E 144° 30.000 19 65 83 Tropical Depression 310 ° 18 JTWC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
03rd May 2013 06:00:00 S 10° 48.000, E 136° 24.000 Tropical Depression 56 74 JTWC

 

Earth Watch Report  -  Earthquakes

6.1 269km ESE of Ozernovskiy, Russia 2013-03-24 04:18:34 50.718°N 160.155°E 9.7

M6.1 – 269km ESE of Ozernovskiy, Russia 2013-03-24 04:18:34 UTC

Earthquake location 50.718°N, 160.155°E

Event Time

  1. 2013-03-24 04:18:34 UTC
  2. 2013-03-24 15:18:34 UTC+11:00 at epicenter
  3. 2013-03-23 23:18:34 UTC-05:00 system time

Location

50.718°N 160.155°E depth=9.7km (6.0mi)

Nearby Cities

  1. 269km (167mi) ESE of Ozernovskiy, Russia
  2. 274km (170mi) SSE of Vilyuchinsk, Russia
  3. 278km (173mi) SSE of Petropavlovsk-Kamchatskiy, Russia
  4. 300km (186mi) SSE of Yelizovo, Russia
  5. 2341km (1455mi) NE of Tokyo, Japan

 

Tectonic Summary

Seismotectonics of the Kuril-Kamchatka Arc

The Kuril-Kamchatka arc extends approximately 2,100 km from Hokkaido, Japan, along the Kuril Islands and the Pacific coast of the Kamchatka Peninsula to its intersection with the Aleutian arc near the Commander Islands, Russia. It marks the region where the Pacific plate subducts into the mantle beneath the Okhotsk microplate, part of the larger North America plate. This subduction is responsible for the generation of the Kuril Islands chain, active volcanoes located along the entire arc, and the deep offshore Kuril-Kamchatka trench. Relative to a fixed North America plate, the Pacific plate is moving towards the northwest at a rate that increases from 75 mm/year near the northern end of the arc to 83 mm/year in the south.

Plate motion is predominantly convergent along the Kuril-Kamchatka arc with obliquity increasing towards the southern section of the arc. The subducting Pacific plate is relatively old, particularly adjacent to Kamchatka where its age is greater than 100 Ma. Consequently, the Wadati-Benioff zone is well defined to depths of approximately 650 km. The central section of the arc is comprised of an oceanic island arc system, which differs from the continental arc systems of the northern and southern sections. Oblique convergence in the southern Kuril arc results in the partitioning of stresses into both trench-normal thrust earthquakes and trench-parallel strike-slip earthquakes, and the westward translation of the Kuril forearc. This westward migration of the Kuril forearc currently results in collision between the Kuril arc in the north and the Japan arc in the south, resulting in the deformation and uplift of the Hidaka Mountains in central Hokkaido.

The Kuril-Kamchatka arc is considered one of the most seismically active regions in the world. Deformation of the overriding North America plate generates shallow crustal earthquakes, whereas slip at the subduction zone interface between the Pacific and North America plates generates interplate earthquakes that extend from near the base of the trench to depths of 40 to 60 km. At greater depths, Kuril-Kamchatka arc earthquakes occur within the subducting Pacific plate and can reach depths of approximately 650 km.

This region has frequently experienced large (M>7) earthquakes over the past century. Since 1900, seven great earthquakes (M8.3 or larger) have also occurred along the arc, with mechanisms that include interplate thrust faulting, and intraplate faulting. Damaging tsunamis followed several of the large interplate megathrust earthquakes. These events include the February 3, 1923 M8.4 Kamchatka, the November 6,1958 M8.4 Etorofu, and the September 25, 2003 M8.3 Hokkaido earthquakes. A large M8.5 megathrust earthquake occurred on October 13, 1963 off the coast of Urup, an island along the southern Kuril arc, which generated a large tsunami in the Pacific Ocean and the Sea of Okhotsk, and caused run-up wave heights of up to 4-5 m along the Kuril arc. The largest megathrust earthquake to occur along the entire Kurile-Kamchatka arc in the 20th century was the November 4, 1952 M9.0 event. This earthquake was followed by a devastating tsunami with run-up wave heights as high as 12 m along the coast of Paramushir, a small island immediately south of Kamchatka, causing significant damage to the city of Severo-Kurilsk.

Instrumental Intensity

ShakeMap Intensity Image

Earth Watch Report  -  Storms

Severe Tropical Cyclone SANDRA (17F) (13U) (19P) Satellite Image Tropical Cyclone 19P (SANDRA) ATCF Track
Severe Tropical
Cyclone SANDRA
(17F) (13U) (19P)
Satellite Image
Tropical Cyclone
19P (SANDRA)
JTWC ATCF Track

  Active tropical storm system(s)
Name of storm system Location Formed Last update Last category Course Wind Speed Gust Wave Source Details
Sandra (19P) Pacific Ocean – South 06.03.2013 14.03.2013 Tropical Depression 180 ° 74 km/h 93 km/h 5.79 m JTWC Details

Tropical Storm data

Storm name: Sandra (19P)
Area: Pacific Ocean – South
Start up location: S 15° 24.000, E 156° 48.000
Start up: 07th March 2013
Status: 14th March 2013
Track long: 1,004.29 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
08th Mar 2013 04:55:13 S 14° 48.000, E 156° 30.000 9 83 102 Tropical Storm 35 15 JTWC
09th Mar 2013 05:40:58 S 15° 18.000, E 158° 18.000 7 120 148 Cyclone I. 105 24 JTWC
10th Mar 2013 06:16:15 S 15° 54.000, E 160° 30.000 9 157 194 Cyclone II. 100 28 JTWC
11th Mar 2013 05:05:45 S 17° 6.000, E 161° 42.000 9 194 241 Cyclone III. 130 35 JTWC
12th Mar 2013 05:13:19 S 20° 0.000, E 161° 54.000 17 157 194 Cyclone II. 180 28 JTWC
13th Mar 2013 04:51:53 S 23° 36.000, E 161° 30.000 15 102 130 Tropical Storm 200 23 JTWC
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
14th Mar 2013 05:19:39 S 29° 6.000, E 162° 6.000 37 74 93 Tropical Depression 180 ° 19 JTWC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
15th Mar 2013 00:00:00 S 32° 0.000, E 160° 36.000 Tropical Depression 56 74 JTWC

Tropical Cyclone 20P (TWENTY) ATCF Track

Tropical Cyclone
20P (TWENTY)
JTWC ATCF Track

20P Pacific Ocean – South 13.03.2013 14.03.2013 Tropical Depression 140 ° 65 km/h 83 km/h 6.10 m JTWC Details

Tropical Storm data

Storm name: Tim (20P)
Area: Pacific Ocean – South
Start up location: S 13° 0.000, E 146° 36.000
Start up: 14th March 2013
Status: Active
Track long: 0.00 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
Current position
Date Time Position Speed
km/h
Wind
km/h
Gust
km/h
Category Course Wave
feet
Pressure Source
14th Mar 2013 10:45:40 S 14° 54.000, E 149° 42.000 26 93 120 Cyclone I 120 ° 24 JTWC
Forecast track
Date Time Position Category Wind
km/h
Gust
km/h
Source
15th Mar 2013 18:00:00 S 17° 36.000, E 154° 42.000 Cyclone I 120 148 JTWC
15th Mar 2013 06:00:00 S 16° 42.000, E 153° 42.000 Cyclone I 111 139 JTWC
16th Mar 2013 06:00:00 S 18° 30.000, E 155° 0.000 Cyclone I 111 139 JTWC
17th Mar 2013 06:00:00 S 19° 18.000, E 154° 18.000 Tropical Depression 83 102 JTWC
18th Mar 2013 06:00:00 S 19° 24.000, E 152° 42.000 Tropical Depression 56 74 JTWC
19th Mar 2013 06:00:00 S 18° 30.000, E 150° 6.000 Tropical Depression 46 65 JTWC

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