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Environmental Issues [Filtered, stifled & blocked by Google!]

Sarychev Peak Before and After Images

Posted by feww on July 5, 2009

Before and after images show impact of  the Sarychev Peak Volcano eruption on Matua Island.

Ostrov Matua, Kuril Islands

sarychev_ast_2009181
Image dated June 30, 2009

sarychev_ast_2007146
Image dated
May 26, 2007

Acquired by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite, these images of Ostrov Matua show the island shortly after the eruption on June 30, 2009 (top), and two years before on May 26, 2007 (bottom).

In these false-color images, vegetation appears red, water appears dark blue, and clouds, water vapor and ice all appear white. Volcanic rock, including old lava flows and debris from the recent eruption, ranges from gray to dark brown.

The most striking difference between these two images is the gray coating on the northwestern half of the island in June 2009. While vegetation on the rest of the island appears lush, volcanic debris—probably a mixture of pyroclastic flows and settled ash—covered virtually all the vegetation on the northwestern end. A close look at the top image also reveals that the recent volcanic activity appears to have expanded the island’s coastline on the northwestern end.

Another difference between the images relates to snow cover. In the image from May 2007, snow spreads over much of the island, although the snow alternates with snow-free ground. The vegetation is pinkish-gray, suggesting the spring thaw is still underway. The complete lack of snow in 2009 may result from a combination of a difference in season and volcanic activity having melted or covered any lingering snow.

NASA image created by Jesse Allen, using data provided courtesy of NASA/GSFC/METI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. Caption by Michon Scott.

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Posted in Earth’s Energy Budget, Sarychev Peak photos, Volcano Watch, active volcanoes, volcanism | Tagged: , , , , | Leave a Comment »

Travel Health Alert: Measles Outbreak in NZ

Posted by msrb on July 5, 2009

Measles Outbreak in Christchurch, NZ!

The following Travel Health Alert was relayed to FEWW by Blogger TEAA

New Zealand Travel Health Warning: Measles Outbreak in Christchurch!

Global Health Alert  Bulletin # 28  - Outbreak of potentially lethal measles infection in Christchurch!

Four Christchurch Boys’ High School students were found to have measles infection last week, with another case suspected.

Canterbury health officials have now identified an additional six likely cases of the measles in the region, said Medical Officer of Health Dr Cheryl Brunton.

No further information has been released.

See also:

More About Measles Infection:

The following information about Measles is from CDC website:

Measles Advisory- Measles is a highly infectious disease that can result in severe, sometimes permanent, complications. The disease is no longer common in the United States, but it remains widespread in most countries of the world. Recent outbreaks in the United States highlight the ongoing risk of measles importations from other countries by people who travel. These outbreaks also highlight the impact vaccination has in preventing measles. As the new school year begins, parents should consider the importance of vaccination in protecting their children, themselves, and others against this highly contagious disease. Further information regarding recent U.S. measles outbreaks is available in an April 2008 CDC Health Advisory and in an August 2008 Morbidity and Mortality Weekly Report, Update: Measles — United States, January–July 2008.

Measles Virus

This thin-section transmission electron micrograph (TEM) revealed the ultrastructural appearance of a single virus particle, or “virion”, of measles virus. The measles virus is a paramyxovirus, of the genus Morbillivirus. It is 100-200 nm in diameter, with a core of single-stranded RNA, and is closely related to the rinderpest and canine distemper viruses. Two membrane envelope proteins are important in pathogenesis. They are the F (fusion) protein, which is responsible for fusion of virus and host cell membranes, viral penetration, and hemolysis, and the H (hemagglutinin) protein, which is responsible for adsorption of virus to cells.

There is only one antigenic type of measles virus. Although studies have documented changes in the H glycoprotein, these changes do not appear to be epidemiologically important (i.e., no change in vaccine efficacy has been observed). See PHIL 8429 for a black and white version of this image.

Prior to 1963, almost everyone got measles; it was an expected life event. Each year in the U.S. there were approximately 3 to 4 million cases and an average of 450 deaths, with epidemic cycles every 2 to 3 years. More than half the population had measles by the time they were 6 years old, and 90 % had the disease by the time they were 15. This indicates that many more cases were occurring than were being reported. However, after the vaccine became available, the number of measles cases dropped by 98 % and the epidemic cycles drastically diminished. Measles virus is rapidly inactivated by heat, light, acidic pH, ether, and trypsin. It has a short survival time (<2 hours) in the air, or on objects and surfaces. Credit : CDC/ Courtesy of Cynthia S. Goldsmith; William Bellini, Ph.D.

What’s Measles?

A respiratory disease caused by a virus, which normally grows in the cells that line the back of the throat and in the cells that line the lungs.

Symptoms

Rash, high fever, cough, runny nose, and red, watery eyes (lasts about a week).

Complications

Diarrhea, ear infections, pneumonia, encephalitis, seizures, and death

Approximately 20% of reported measles cases experience one or more complications. These complications are more common among children under 5 years of age and adults over 20 years old.

Measles causes ear infections in nearly one out of every 10 children who get it. As many as one out of 20 children with measles gets pneumonia, and about one child in every 1,000 who get measles will develop encephalitis. (This is an inflammation of the brain that can lead to convulsions, and can leave your child deaf or mentally retarded.) For every 1,000 children who get measles, one or two will die from it. Measles can also make a pregnant woman have a miscarriage, give birth prematurely, or have a low-birth-weight baby.

In developing countries, where malnutrition and vitamin A deficiency are prevalent, measles has been known to kill as many as one out of four people. It is the leading cause of blindness among African children. Measles kills almost 1 million children in the world each year.

Transmission

Spread by contact with an infected person, through coughing and sneezing (highly contagious)

The disease is highly contagious, and can be transmitted from 4 days prior to the onset of the rash to 4 days after the onset. If one person has it, 90% of their susceptible close contacts will also become infected with the measles virus.

The virus resides in the mucus in the nose and throat of the infected person. When that person sneezes or coughs, droplets spray into the air. The infected mucus can land in other people’s noses or throats when they breathe or put their fingers in their mouth or nose after handling an infected surface. The virus remains active and contagious on infected surfaces for up to 2 hours. Measles spreads so easily that anyone who is not immunized will probably get it, eventually.

Vaccine

Measles vaccine (contained in MMR, MR and measles vaccines) can prevent this disease.

The MMR vaccine is a live, attenuated (weakened), combination vaccine that protects against the measles, mumps, and rubella viruses. It was first licensed in the combined form in 1971 and contains the safest and most effective forms of each vaccine.

It is made by taking the measles virus from the throat of an infected person and adapting it to grow in chick embryo cells in a laboratory. As the virus becomes better able to grow in the chick embryo cells, it becomes less able to grow in a child’s skin or lungs. When this vaccine virus is given to a child it replicates only a little before it is eliminated from the body. This replication causes the body to develop an immunity that, in 95% of children, lasts for a lifetime.

A second dose of the vaccine is recommended to protect those 5% who did not develop immunity in the first dose and to give “booster” effect to those who did develop an immune response.

Who Needs the Vaccine

Does my child need this vaccine?

The young boy pictured here, displayed the characteristic maculopapular rash indicative of rubella, otherwise known as German measles, or 3-day measles. Rubella is a respiratory viral infection characterized by mild respiratory symptoms and low-grade fever, followed by a maculopapular rash lasting about 3 days. In children there may be no significant respiratory prodrome and the illness may not be diagnosed since the rash may be mild and mimic other conditions. It is estimated that 20-50% of infections are subclinical. Complications occur more frequently in adult women, who may experience arthritis or arthralgia, often affecting the fingers, wrists and knees. These joint symptoms rarely last for more than a month after appearance of the rash.

The rubella vaccine is a live attenuated (weakened) virus. Although it is available as a single preparation, it is recommended that in most cases rubella vaccine be given as part of the MMR vaccine (protecting against measles, mumps, and rubella). MMR is recommended at 12-15 months (not earlier) and a second dose when the child is 4-6 years old (before kindergarten or 1st grade).

Rubella vaccination is particularly important for non-immune women who may become pregnant because of the risk for serious birth defects if they acquire the disease during pregnancy.

Birth defects if acquired by a pregnant woman: deafness, cataracts, heart defects, mental retardation, and liver and spleen damage (at least a 20% chance of damage to the fetus if a woman is infected early in pregnancy). Image and caption: CDC.

Children should get 2 doses of MMR vaccine:

  • The first dose at 12-15 months of age
  • The second dose at 4-6 years of age

These are the recommended ages. But children can get the second dose at any age, as long as it is at least 28 days after the first dose.

For additional details, consult the MMR Vaccine Information Statement {PDF}  and the Childhood Immunization Schedule.

As an adult, do I need this vaccine?

You do NOT need the measles, mumps, rubella vaccine (MMR) if:

  • You had blood tests that show you are immune to measles, mumps, and rubella.
  • You are a man born before 1957.
  • You are a woman born before 1957 who is sure she is not having more children, has already had rubella vaccine, or has had a positive rubella test.
  • You already had two doses of MMR or one dose of MMR plus a second dose of measles vaccine.
  • You already had one dose of MMR and are not at high risk of measles exposure.

You SHOULD get the measles vaccine if you are not among the categories listed above, and:

  • You are a college student, trade school student, or other student beyond high school.
  • You work in a hospital or other medical facility*.
  • You travel internationally, or are a passenger on a cruise ship.
  • You are a woman of childbearing age.

For additional details, consult the MMR Vaccine Information Statement and the Adult Immunization Schedule.

See also:  Healthcare Personnel Vaccination Recommendations

More on Vaccines Page

Posted in H protein, Rubella, infectious diseases, measles virus | Tagged: , , , , , | Leave a Comment »

Palin Told to Quit!

Posted by feww on July 4, 2009

Palin resigned as Alaska’s governor

Palin’s position became untenable when she failed to block beluga whale being listed as endangered species

See: Palin Fails to Block Beluga Whale Protection

palin - Robert DeBerry - AP
Sarah Palin announced her resignation as Alaska governor in Wasilla. Photo: Robert DeBerry/AP. Image may be subject to copyright.

Sarah Palin has resigned as Alaska’s governor.

“We know we can effect positive change outside government at this moment in time on another scale and actually make a difference for our priorities,” she said.

Palin will transfer authority to her deputy, lieutenant governor Sean Parnell by end of July 2009.

Palin was NOT expected to win the next gubernatorial election in Alaska due in 2010.

Related Links:

Posted in Endangered Species, Sean Parnell, big oil, moose, polar bear | Tagged: , , , , | Leave a Comment »

VolcanoWatch Weekly [2 July 2009]

Posted by feww on July 3, 2009

VoW: Yellowstone Volcano

Location: 44.43°N 110.67°W
Summit Elevation:  2,805 m
Volcano Alert Level: NORMAL
Aviation Color Code: GREEN

Yellowstone
Remote sensor imagery of Yellowstone Caldera. Source: a frame-freeze picture from Yellowstone Volcano Due To Erupt


The rim of the Yellowstone Caldera.  Source ESA (mirrored from http://www.yellowstonegis.utah.edu/home/home.html)

What’s brewing under the old rocks?

  • Earthquake swarms are common at Yellowstone.
  • Increased seismic activity at Yellowstone Lake in Yellowstone National Park  in late December 2008 decreasing  since January 8, 2009.
  • Seismic activity  could continue.
  • The recent swarm is well above typical activity at Yellowstone, but  not unprecedented.
  • Earthquake swarms within the Yellowstone caldera typically occur with magnitudes of about 4.0.
  • A swarm with about 3,000 events occurred in 1985 on the northwest rim of the caldera, lasting for three months, with largest earthquakes up to M4.9  recorded. (Source: Volcanoes USGS )


Yellowstone Lake showing location and times of the recent earthquakes from Dec. 27, 2008 (blue) to Jan. 8, 2009 (red). The M 3.0 and greater earthquakes are shown as stars, the smaller earthquakes are shown as circles. During the swarm, the earthquake locations appear to have moved north. For more information on the depths of the earthquakes, see the cross section from X to X’ below.
(Source: Volcanoes USGS/ YVO )


The depth versus location of the Yellowstone Lake earthquake swarm from X to X’ on the Yellowstone Lake map. Earthquakes are shown from Dec. 27, 2008 (blue) to
Jan. 8, 2009 (red). The M 3.0 and greater earthquakes are shown as stars, the smaller earthquakes are shown as circles.  (Source: Volcanoes USGS
/ YVO )


Number of reviewed Yellowstone Lake earthquakes in six-hour and three-hour intervals from 12/27/08 to 01/06/09. The green line on the left figure gives the cumulative
number of earthquakes; the steep slopes correspond to increase in earthquake number. The red line in the figure on the right gives the cumulative moment, or energy; its sharp increase in the first few days is due to a greater number of large earthquakes with their greater energy release. The total cumulative moment is equivalent in energy to about one M 4.5 earthquake. Click on the image for a full-size version.
(Source: Volcanoes USGS/ YVO )

What causes earthquakes at Yellowstone?

USGS / YVO cite a combination of geological factors including:

  • Regional stress associated with normal faults such as the nearby Teton and Hebgen Lake faults
  • Magmatic movements at depth (>7 kms)
  • Hydrothermal fluid activity caused by boiling groundwater which is heated by magma.

However,  YVO has not reported any anomalous changes in hot springs discharges, gas emissions …

In 2004 the Yellowstone caldera underwent period of accelerated uplift, clocking 7 cm/yr, or three times  faster than  in the recorded history; however the movement has now slowed down to  a maximum rate of 4 cm/yr (or about 175 % of the pre-2004 records.)

The uplift is most noticeable at the White Lake GPS station, as has been discussed in our monthly YVO updates during the past year. As of late October 2007, the total uplift since 2004 at that location is about 17 cm. Chang and his colleagues credit the relatively rapid rise to recharge of magma into the giant magma chamber that underlies the Yellowstone Caldera. They also used numerical modeling to infer that the magma intruded about 10 km (6 miles) beneath the surface.


This interferogram provides a map view of ground movements at Yellowstone. Each color contour represents a line of equal uplift relative to the ENVISAT satellite between Sept. 2004 and Aug. 2006. The center of the uplift is an elliptical region stretching from the northeastern part of the Yellowstone Caldera (the dashed black line) to the southwest. This area of maximum uplift encompasses both Yellowstone’s resurgent domes, features long known for similar movements. During this time period, the north-rim uplift anomaly subsided (bullseye in the upper left part of the interferogram). The yellow lines are roads. The yellow triangles are locations of GPS stations with continuous data. The light blue lake within the caldera is Yellowstone Lake. Thin black lines are mapped faults. Figure courtesy of C. Wicks, USGS. Caption: USGS / YVO


Yellowstone caldera Map. USGS   Click Image to Enlarge.


Source: USGS


Source: Yellowstone National Park.

Conclusion:

USGS / YVO: “At this time, there is no reason to believe that magma has risen to a shallow level within the crust or that a volcanic eruption is likely. “

FEWW: Perhaps, a new mindset is needed to help understand the true nature, “utility function” and full range of  all possible scenarios that might occur at the super volcano site. Let’s start looking at Yellowstone in the Big Picture frame.


Volcanic Activity Report: 24 June-30 June 2009

Source: Global Volcanism program (GVP) – SI/USGS Weekly Volcanic Activity Report

New activity/unrest:

NOTE: A small explosive eruption of Cleveland on 25 June prompted AVO to raise the Volcano Alert Level to Watch and the Aviation Color Code to Orange. An ash cloud that detached from the volcano was seen on satellite imagery moving S at an estimated altitude of 4.6 km (15,000 ft) a.s.l. No further activity was reported. On 27 June, AVO lowered the Volcano Alert Level to Advisory and the Aviation Color Code to Yellow. (Source: GVP)

Ongoing Activity:

Latest U.S. Volcano Alerts and Updates for July 03, 2009 0040 UTC

  • Redoubt Activity – Color Code YELLOW : Alert Level ADVISORY

  • Kilauea Activity  -  Color Code ORANGE : Alert Level WATCH

  • Cleveland Activity – Color Code – YELLOW : Alert Level – ADVISORY

  • Mauna Loa Activity – Color Code YELLOW : Alert Level ADVISORY

Redoubt Volcano Latest Observations: Local time: June 24, 2009 1705 AKDT (June 25, 2009 0105 UTC)
The eruption of Redoubt continues. Seismic activity remains low but above background levels.

Related Links:

Posted in Kīlauea, Volcano Hazards, Volcano Status, volcanism, volcanoes | Tagged: , , , , | Leave a Comment »

Magnitude 6.7 quake strikes south of Crete

Posted by feww on July 1, 2009

Strong 6.7 Mw quake strikes south of Crete, Greece

Magnitude 6.7 mainshock followed by at least one aftershock measuring 4.9 Mw struck south of the island of Crete, Greece.

10-degree Map Centered at 35°N,25°E

us2009ina8
Location Map. Note location of Santorini. Original Map: USGS

greece seis haz map
Major Tectonic Boundaries: Subduction Zones -purple (Source: USGS)

historic seismicity crete area

7_legend seismicity
Major Tectonic Boundaries: Subduction Zones -purple (Source: USGS)

Details of the Mainshock:

  • Magnitude: 6.7
  • Date-Time:
    • Wednesday, July 01, 2009 at 09:30:12 UTC
    • Wednesday, July 01, 2009 at 12:30:12 PM at epicenter
  • Location:  34.188°N, 25.426°E
  • Depth:  38 km (23.6 miles)
  • Region CRETE, GREECE
  • Distances
    • 130 km (80 miles) S of Iraklion, Crete, Greece
    • 195 km (120 miles) SE of Chania, Crete, Greece
    • 270 km (165 miles) NNE of Tubruq, Libya
    • 450 km (280 miles) SSE of ATHENS, Greece
  • Location Uncertainty:  horizontal +/- 7.1 km (4.4 miles); depth +/- 12.8 km (8.0 miles)
  • Parameters:  NST= 51, Nph= 51, Dmin=131.6 km, Rmss=1.19 sec, Gp= 72°, M-type=teleseismic moment magnitude (Mw), Version=7
  • Source: USGS NEIC (WDCS-D)
  • Event ID:  us2009ina1

What’s happening at Santorini?

For Background Information See: Volcanoes, Santorini Eruption and Crops Failure in China

Santorini

Country: Greece
Subregion Name: Greece
Volcano Type: Shield volcanoes
Volcano Status: Historical
Last Known Eruption: 1950
Summit Elevation: 367 m 1,204 feet
Latitude: 36.404°N 36°24′13″N
Longitude: 25.396°E 25°23′47″E
Source: GVP

Renowned Santorini (Thera), with its steep-walled caldera rim draped by whitewashed villages overlooking an active volcanic island in the center of a caldera bay, is one of the scenic highlights of the Aegean. The circular island group is composed of overlapping shield volcanoes cut by at least four partially overlapping calderas. The oldest southern caldera was formed about 180,000 years before present (BP), followed by the Skaros caldera about 70,000 years BP, and then the Cape Riva caldera about 21,000 years BP. The youngest caldera formed about 3600 years BP during the Late-Bronze-Age Minoan eruption that forced abandonment of the thriving Aegean Sea island. Post-Minoan eruptions beginning in 197 BC constructed a series of lava domes and flows that form two islands near the center of the caldera. A submarine eruption took place in 1650 AD outside the caldera NE of Thera. The latest eruption at Santorini produced a small lava dome and flow in 1950, accompanied by explosive activity. Photo by Lee Siebert, 1994 (Smithsonian Institution). Caption: Global Volcanism Program.

Geographic setting

Santorini is an active volcano in the South Aegean Sea about 120 km north of
Crete, its location being 36.4oN, 25.4oE, and belongs to the Cycladic islands.
Santorini is a group of 5 islands:
1. The main island Thira (75,8 km², ca. 7000 inhabitants)
2. Thirasia (9,3 km², ca. 250 inhabitants)
3. Aspronisi (0,1 km², uninhabited)
4. Palea Kameni (0,5 km², 1 inhabitant)
5. Nea Kameni (3,4 km², uninhabited  (http://www.geophysicsonline.gr)

On June 13, 2009 GR Reporter (www.GRREPORTER.INFO) wrote:

columbusComputer generated image of Columbus. Source: GR Reporter

The submarine volcano, Columbus, located about 6.5 km south-east of Santorini in the Aegean Sea, is now the focus of “great interest” for Greek and German geologists.
“They have registered constant earthquakes of 4 Richter, hot air eruptions and continuous changes in the sea floor around the crater. The volcano is 470 meters high and reaches down to 17 meters beneath the sea floor. Its crater’s width is out of proportion- 1.5 kilometers. Complex submarine equipment has shown that Columbus’s volcanic activity never stops. It is the reason for the frequent earthquakes and constant changes in the surface around the crater.”

“The distortion of the sea floor is minor but it can be seen on the walls of the crater and in the 10-15-kilometers perimeter around it,” says Martin Heds from the Geology and Seismology institute to the Hamburg University.

According to Heds, “this does not indicate an eruption in near future.” The last known eruption of Columbus occurred in 1650.

“‘Reservoirs’” filled with hot water, reaching 200 degrees centigrade, resembling under-water fire places and releasing different kinds of gases- mostly carbon dioxide and hydrogen sulphide,” were discovered in the vicinity of Columbus.

A 5-km wide magma chamber is believed to be situated under the volcano. Lava is constantly spewed out of the chamber, GR Reporter suggested.

Tectonic Setting

The volcanic complex of Santorini is the most active part of the South Aegean Volcanic Arc. This volcanic arc is about 500 km long and 20 to 40 km wide and extends from the mainland of Greece through the islands of Aegina, Methana, Poros, Milos, Santorini, Kos, Yali, Nisyros and the Bodrum peninsula in Turkey. It is characterized by earthquakes at depths of 150-170 km that mark the subduction of the African underneath the Eurasian plate, more precisely the Aegean subplate, at a rate of up to 5 cm per year in a northeasterly direction.  (http://www.geophysicsonline.gr)

Hellenic Arc
The South Aegean Volcanic Arc and the tectonic setting of Santorini. (http://www.geophysicsonline.gr) Click Image to Enlarge.

Geology of Santorini

Non-volcanic rocks are exposed on Santorini at the Profitis Ilias Mountain, Mesa Vouno, the Gavrillos ridge, Pirgos, Monolithos and the inner side of the caldera wall between Cape Plaka and Athinios.

They represent a former non-volcanic island of about 9×6 km extension similar to neighboring Cycladic islands like Anaphe, Ios or Amorgos. The rocks consist of metamorphosed limestone and schist from Triassic to Tertiary time folded during the Alpine folding. The observed metamorphose grade is a blue-schist faciesresulting from tectonic deformation by the plate collision in the Oligocene to Miocene. At Athinios a 9.5 million year old Miocene granite intrusion has been found; it is part of the Cycladic Granitic Province and is the source of ore minerals including talc, chalcopyrite, chrysocolla, magnetite and others.(http://www.geophysicsonline.gr).

Santorini Geological setting
Simplified geologic map of Santorini. (http://www.geophysicsonline.gr  Sourced  From  http://www.geo.aau.dk/palstrat/tom/santorini_homepage/santorini_geology.htm).
Click Image to Enlarge.

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Posted in Aegean subplate, African Plate, Columbus volcano, Hellenic arc, South Aegean Volcanic Arc | Tagged: , , , , | Leave a Comment »

El Niño event almost certain: BOM

Posted by feww on July 1, 2009

El Niño event likely, says Australia’s Bureau of Meteorology

More evidence of a developing El Niño event has emerged during the past fortnight, and computer forecasts show there’s very little chance of the development stalling or reversing. —BOM

Equatorial sea-surface temperatures are currently more than 1°C above normal in the eastern Pacific, while the Southern Oscillation Index (SOI) remains below zero at around −2, says BOM.

A sustained negative SOI is often associated with El Nino conditions.

BOM hopes to provide a clear picture of the situation in the Pacific by next week when their final June data are analyzed.

El Niño events are usually (but not always) associated with below normal rainfall in the second half of the year across large parts of southern and inland eastern Australia.

Another adverse sign for southeastern Australian rainfall is the recent trend to positive values in the Indian Ocean Dipole (IOD), as measured by the Dipole Mode Index (DMI).

The next BOM update is available on July 8, 2009.

Last month FEWW reported US Climate Prediction Center as saying that conditions were favorable for a transition from ENSO-neutral to El Niño conditions during June – August 2009.

sst_wind_home_5day
Click image to update and enlarge.


Images from Tropical Atmospheric Ocean project: NOAA

Summary of BOM Weekly Update:

  • The Pacific Ocean sea surface is currently significantly warmer than the long-term average across most of the tropical Pacific, especially central to eastern areas.
  • A large amount of the sub-surface water of the tropical Pacific is also warmer than the long-term average, particularly in the east.
  • The latest 30-day SOI value is −2, while the monthly value for May was −5.
  • Trade winds remain weaker than normal across the central equatorial Pacific.
  • Cloudiness near the date-line is near-normal, and is yet to show a consistent trend towards El Niño conditions.
  • All international climate models predict the tropical Pacific to continue to warm and to be above El Niño thresholds throughout most of the second half of 2009.

“Australia is the world’s fourth-largest wheat exporter and its grain production is still recovering from the worst drought in more than 100 years that reduced the 2006/07 crop to just 10.6 million tonnes and the 2007/08 crop to 13.0 million tonnes.” Reuters reported.

FEWW Moderators estimate that a new episode of El Niño, which would have devastating impact globally, could cause up to $500 billion in damages.

Related Links:


Posted in Australian drought, Australian rainfall, Indian Ocean Dipole, Southern Oscillation Index, drought and deluge | Tagged: , , , , | 1 Comment »

Redoubt Volcano settling down?

Posted by feww on July 1, 2009

Is Redoubt going back to sleep?

After Redoubt’s last explosive eruption about three month ago, the researchers at the Alaska Volcano Observatory say the volcano may be settling down. The aviation alert level has been lowered to code yellow (advisory), however, constant monitoring continues.

Redoubt has been oozing magma and ejecting steam since the last eruption on April 4, 2009.

“The last couple of months at Redoubt, we have been building a mountain,” said one of the researchers, referring to the colossal lava dome.

As of June 9, the giant dome had grown to approximately 67.5 million m3 in volume. the dome is unstable and can collapse  at any time, causing  explosions, and flooding the Drift River valley.


Redoubt from the east. Picture Date: July 01, 2009.  Image Creator: Cyrus Read. Image courtesy of AVO/USGS.


Redoubt photo taken by DFR Webcam. AVO. Camera is co-located with seismic station DFR, approximately 12.2 km NE of Redoubt.

ALASKA VOLCANO OBSERVATORY INFORMATION STATEMENT
Tuesday, June 30, 2009 4:38 PM AKDT (Wednesday, July 1, 2009 0038 UTC)

Redoubt Volcano
60°29′7″ N 152°44′38″ W, Summit Elevation 10197 ft (3,108 m)
Current Volcano Alert Level: ADVISORY
Current Aviation Color Code: YELLOW

Extended Information Statement

The 2009 eruption of Redoubt volcano began March 15th, 2009 with a steam explosion. Between March 22nd and April 4th, Redoubt produced multiple significant explosions that sent ash and gas clouds to as high as 65,000 feet (19.8 km) above sea level. After April 4th, the eruption continued with extrusion of a lava dome within the summit crater, eventually producing a blocky lava flow that currently extends ~0.6 miles (1 km) down the north flank of the volcano. Redoubt entered its 14th week of eruptive activity the week of June 22nd. More …

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Seagrass in Crisis

Posted by feww on June 30, 2009

Seagrass is disappearing from the world’s oceans at an accelerating rate

A new study finds that 29 percent of the world’s known seagrass has disappeared since 1879 and the losses were rising exponentially.

Seagrasses—a unique group of flowering plants that have adapted to exist fully submersed in the sea—profoundly influence the physical, chemical, and biological environments in coastal waters, acting as ecological engineers (sensuWright and Jones 2006) and providing numerous important ecological services to the marine environment (Costanza et al. 1997). Seagrasses alter water flow, nutrient cycling, and food web structure (Hemminga and Duarte 2000). They are an important food source for megaherbivores such as green sea turtles, dugongs, and manatees, and provide critical habitat for many animals, including commercially and recreationally important fishery species.—A Global Crisis for Seagrass Ecosystems

seagrasses
Examples of seagrass meadows and associated animals. (a) Seahorse (Hippocampus sp.) in temperate Cymodocea nodosa meadow,Mediterranean Sea. Photograph: Gérard Pergent. (b) School of zebrafish (Girella zebra) over a temperate Posidonia australis meadow, Western Australia. Photograph: Gary A. Kendrick. (c) Manatee (Trichechus manatus) feeding in a tropical Thalassia testudinum meadow, Puerto Rico. Photograph: James Reid. (d) Green sea turtle (Chelonia midas) feeding in a tropical T. testudinum meadow, Yucatán. Photograph: Robert P. van Dam. Source: A Global Crisis for Seagrass Ecosystems

Seagrasses, which are found in coastal waters are vanishing at the rate of about 110 sq km a year since 1980, Reuters reported the study as saying. The report is to be published in the U.S. journal Proceedings of the National Academy of Sciences.

Seagrasses as ecological service providers and biological sentinels Seagrass meadows have important ecological roles in coastal ecosystems and provide high-value ecosystem services compared with other marine and terrestrial habitats (figure below; Costanza et al. 1997). For example, primary production from seagrasses and their associated macro- and microepiphytes rivals or exceeds that of many cultivated terrestrial ecosystems (Duarte and Chiscano 1999). Seagrasses also provide an enormous source of carbon to the detrital pool, some of which is exported to the deep sea, where it provides a critical supply of organic matter in an extremely food-limited environment (Suchanek et al. 1985).Much of the excess organic carbon produced is buried within seagrass sediments, which are hotspots for carbon sequestration in the biosphere (Duarte et al. 2005). The structural components of seagrass leaves, rhizomes, and roots modify currents and waves, trapping and storing both sediments and nutrients, and effectively filter nutrient inputs to the coastal ocean (Hemminga and Duarte 2000).—A Global Crisis for Seagrass Ecosystems

Only about 177,000 sq km of seagrasses are left globally.

The study by Australian and American scientists compares the losses to that of coral reefs, tropical rainforests and mangroves. It says seagrass meadows are “among the most threatened ecosystems on earth,”  blaming the loss on population growth, development, climate change and ecological degradation of the oceans.

“Seagrasses are sentinels of change” and the loss of seagrass was an indicator of a deteriorating global marine ecosystem. “Mounting seagrass loss reveals a major global environmental crisis in coastal ecosystems,” the report said.

seagrass ecosystem services - major loss mechs

Moreover, seagrasses can be considered as biological sentinels, or “coastal canaries.” Changes in seagrass distribution, such as a reduction in the maximum depth limit (Abal and Dennison 1996) or widespread seagrass loss (Cambridge and McComb 1984), signal important losses of ecosystem services that seagrasses provide. Seagrasses are sessile, essentially integrating the relevant water quality attributes, such as chlorophyll and turbidity, that affect the light reaching their leaves. Several features of seagrasses and seagrass meadows result in their particular importance in this regard.The widespread distribution of seagrasses throughout tropical and temperate regions (figure 2) allows better assessment of larger-scale trends than do other comparable coastal habitats, such as mangrove, corals, or salt marsh plants, which are limited to only one of these broad geographic regions. Seagrasses also live in shallow, protected coastal waters, directly in the path of watershed nutrient and sediment inputs, and are therefore highly susceptible to these inputs (figure 4), unlike mangrove forests (which are largely unaffected by water quality) or coral reefs (which occur farther away from the imputs).—A Global Crisis for Seagrass Ecosystems

Some 70 percent of all marine life in the ocean directly depends on seagrass, U.S.-based Seagrass Recovery said.

“Seagrass losses decrease primary production, carbon sequestration and nutrient cycling in the coastal zone. If the current rate of seagrass loss is sustained or continues to accelerate, the ecological losses will also increase, causing even greater ill-afforded economic losses,” said the study.

In addition to the well-documented causes of seagrass declines, other threats to these species are emerging. Over the last 20 years, introductions of nonnative marine species have arisen as a major environmental challenge for the world’s oceans (Carlton 1989). Such introductions are accelerating worldwide (Ruiz et al. 2000), a trend that will continue as the pathways for introductions widen and proliferate and as intervention lags (figure 6b; Naylor et al. 2001, Levine and D’Antonio 2003, Padilla and Williams 2004). At least 28 nonnative species have become established in seagrass beds worldwide, of which 64% have documented or inferred negative effects (figure 6b). The concern about this emerging threat to seagrass beds is that, whereas it is possible to reverse eutrophication or cease dredge-and-fill activities, it is virtually impossible to remove a nonnative species after establishment and spread (Lodge et al. 2006). Lastly, the rapid expansion of fish farming and other aquaculture practices (e.g., shellfish culture) can have serious consequences on local populations of seagrasses through physical disturbance or increased deposition of organic matter and nutrients (Marbà et al. 2006).—A Global Crisis for Seagrass Ecosystems

The preservation of seagrasses and their associated ecosystem services—in particular, biodiversity, primary and secondary production, nursery habitat, and nutrient and sediment sequestration—should be a global priority.We believe that the crisis facing seagrass ecosystems can be averted with a global conservation effort, and this effort will benefit not just seagrasses and their associated organisms but also the entirety of coastal ecosystems. —A Global Crisis for Seagrass Ecosystems

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Posted in Primary production, coastal zone, natural carbon sequestration, nutrient cycling, seagrass meadows | Tagged: , , , , | Leave a Comment »

Shiveluch spewes large plumes of ash

Posted by feww on June 30, 2009

Shiveluch volcano on the Kamchatka Peninsula ejects ash to a height of 7km

Shiveluch volcano on the Kamchatka Peninsula, Russia’s northernmost active volcano,  spewed out ash to a height of some 7,000 meters (23,000 feet), the local geophysics service reported on Monday.

The service had registered about 60 tremors within the area in the previous 24 hours.

“Some of them were followed by powerful ash bursts and avalanches,” a spokesman for the service said.

Shiveluch volcano erupted in December 2006. Local scientists expect the volcano to erupt explosively soon.

“Volcanic activity over the past two-three years has significantly altered the contour of the volcano, with the crater increasing in size by 50% and the slopes becoming far steeper.” RiaNovosti reported.

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Previous Comments by FEWW

FEWW Volcanic Activity Forecast

Posted in Explosive Eruption, Kamchatka peninsula, Kamchatka volcanoes, Koryakski volcano, Russian volcano | Tagged: , , , , | Leave a Comment »

Airbus Crashes in Comoros

Posted by feww on June 30, 2009

Yemenia Airbus A310 with 153 People Crashes in Comoros

Yemenia-Airbus-A310A Yemen Airways (Yemenia) Airbus A310 with 153 people onboard crashed in the Indian Ocean near the archipelago of Comoros earlier today, according to an airline official.

Most of the 142 passengers  (total of 153 people onboard) were Comoran or French. There are no report of  survivors.


Yemenia Airbus A310. Source:  aviationexplorer.com. Image may be subject to copyright.


The downed Yemenia Airbus A310 passenger jet was flying from Sanaa, Yemen,  to Moroni, in the Comoros, carrying also a 11-strong crew, Reuters reported an official as saying.

The Comoros (Population of 800,000), which consists of four small volcanic islands (Anjouan, Grande Comore, Moheli and Mayotte) in the Mozambique channel, about 300 kilometers northwest of Madagascar, is not believed to have any sea rescue capabilities.

Comoros map

Map of the Comoros Islands. Original map: UN.

“We still do not have information about the reason behind the crash or survivors,” the deputy general manager for Yemenia operations, said.

“The weather conditions were rough; strong wind and high seas. The wind speed recorded on land at the airport was 61 kilometers an hour. There could be other factors.”

“Two French military aircraft have left from the islands of Mayotte and Reunion to search the identified zone, and a French vessel has left Mayotte,”the director general of Moroni International Airport was reported as saying.

“The plane has crashed and we still don’t know exactly where. We think it’s in the area of Mitsamiouli,” Comoros Vice-President Idi Nadhoim told Reuters.

“We think the crash is somewhere along its landing approach,” Mr Kassim a representative from regional air security body ASECNA said. “The weather is really not very favorable. The sea is very rough.”

Reuters sketch showing the flight path of downed Yemenia Airbus. Image may be subject to copyright.

Who owns Yemenia?

Yemenia is 51 percent owned by the Yemeni government and 49 percent by the Saudi Arabian government. Yemenia’s fleet includes four Airbus A310-300s, two Airbus A330-200s and four Boeing 737-800s, according to the airline site.

Airbus Crash Stats

If you really have to fly because your life depends on it [sic,] and if you are flying an Airbus, then fly on odd days of the month because the Airbus is statistically twice more likely to crash on even days!

The Next Airbus Crash?

The probability that the next major air disaster would involve an Air New Zealand Airbus has now increased to 0.78.

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Posted in air new zealand, airline disasters, airline safety, comoros crash, french connection | Tagged: , , , , | 4 Comments »

Chaitén: A New Phase of Activity?

Posted by feww on June 29, 2009

Magnitude 5.3 quake strikes off the coast of Isen, Chile

A magnitude 5.3 quake struck off coast of Isen, Chile, at a depth of 10km on Monday. FEWW believes that the quake could be followed by more shocks, a number of which could be larger in magnitude, along the Chile Ridge, near the coast of Chile and about the subducting Nazca Plate. Additional seismic activity in the region could result in a new, more intense phase of activity in Chaitén, or prime other regional volcanoes for eruption.

Chaitén volcano as seen from the city of Chaitén (May 5, 2008)


Chaitén volcano ejects a plume of ash as seen from the city of Chaitén, 1,200km south from Santiago, Chile, on May 5, 2008. (ALVARO VIDAL/AFP/Getty Images). Image may be subject to copyright.

Earth’s Tectonic Plates with their movement vectors.


Detailed world map in English showing the tectonic plates with their movement vectors. For licensing details see: Attribution and Share-Alike

World geologic provinces


Source: USGS

Magnitude 5.3 OFF COAST OF AISEN, CHILE

Magnitude: 5.3
Date-Time: Monday, June 29, 2009 at 03:07:32 UTC
Location:  45.619°S, 76.605°W
Depth: 10 km (6.2 miles) set by location program
Region:  OFF THE COAST OF AISEN, CHILE
Distances:

  • 355 km (220 miles) W of Coihaique, Chile
  • 385 km (240 miles) SW of Castro, Chile
  • 1440 km (900 miles) SSW of SANTIAGO, Chile

Location Uncertainty: horizontal +/- 13.5 km (8.4 miles); depth fixed by location program
Parameters: NST= 40, Nph= 40, Dmin=733.6 km, Rmss=1.54 sec, Gp=133°, M-type=body wave magnitude (Mb), Version=6
Source: USGS NEIC (WDCS-D)
Event ID: us2009ilah

Earthquake Location

us2009ilah

Major Tectonic Boundaries: Subduction Zones -purple, Ridges -red and Transform Faults -green. Source: USGS.

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Posted in COAST OF ISEN, Nazca Plate, Plate Tectonics, oceanic tectonic plate, orogeny | Tagged: , , , , | Leave a Comment »

Beef recall, E.coli O157:H7 suspected

Posted by feww on June 29, 2009

20 people sickened by E.coli O157:H7

About 1/2 million pounds of beef recalled, E.coli O157:H7 contamination suspected

JBS-Swift Beef Co based in Greeley, Colorado, is expanding its June 24 recall  to a total of about 421,000 lbs of assorted beef products, USDA and the company said.

The recall is due to possible contamination by E.coli O157:H7 bacteria after about 20 people were sickened.  The recall includes meat products that were  processed on April 21 -22, 2009 and that have been sold nationally and internationally.

“The contamination may have come from further processing by other companies,” JBS spokesman said on Sunday.


Transmission electron micrograph of E. coli O157:H7 showing flagella. Pseudoreplica technique. Date: 1995. Photo Credit: Elizabeth H. White, M.S. / CDC

The recalled products are roasts and steaks rather than ground beef; however, the company cannot ruled out that  some of the beef may have been processed into ground products by intermediary resellers.

The products were  shipped to Arizona, California, Colorado, Florida, Illinois, Michigan, Minnesota, Nebraska, Oregon, South Carolina, Tennessee, Utah, Wisconsin as well as overseas destinations.

A potentially deadly bacteria, Escherichia coli O157:H7 is a strain of the bacterium Escherichia coli which causes foodborne illness. The infection often leads to bloody diarrhea, dehydration and occasionally to kidney failure, especially in young children, the elderly and persons with weak immune system.

The infections are associated with

  • Eating undercooked, contaminated ground beef
  • Drinking unpasteurized milk
  • Swimming in  contaminated water
  • Eating contaminated vegetables

In the US consumers can call 1-800-685-6328 for further assistance.


A colorized version of PHIL 7137 depicting a highly magnified scanning electron micrographic (SEM) view of a dividing Escherichia coli bacteria, clearly displaying the point at which the bacteria’s cell wall was dividing; Magnification 21674x.

Escherichia coli is a Gram-negative bacterium that normally colonizes the digestive tract of most warm-blooded animals, including human beings. E. coli are facultative in nature, which means that they can adapt to their environments, switching between aerobic, and anaerobic metabolic growth depending environmental stresses. One strain of E. coli, O157:H7, causes an estimated 73,000 cases of infection, and 61 deaths in the United States each year. Infection often leads to bloody diarrhea, and occasionally to kidney failure. Most illness has been associated with eating undercooked, contaminated ground beef. Person-to-person contact in families and child care centers is also an important mode of transmission. Infection can also occur after drinking raw milk and after swimming in or drinking sewage-contaminated water. Content Providers: CDC/ Evangeline Sowers, Janice Haney Carr. Photo Date: 2005. Photo Credit: Janice Haney Carr

What is Escherichia coli?

Escherichia coli (abbreviated as E. coli) are a large and diverse group of bacteria. Although most strains of E. coli are harmless, others can make you sick. Some kinds of E. coli can cause diarrhea, while others cause urinary tract infections, respiratory illness and pneumonia, and other illnesses. Still other kinds of E. coli are used as markers for water contamination—so you might hear about E. coli being found in drinking water, which are not themselves harmful, but indicate the water is contaminated. It does get a bit confusing—even to microbiologists.

What are Shiga toxin-producing E. coli?

Some kinds of E. coli cause disease by making a toxin called Shiga toxin. The bacteria that make these toxins are called “Shiga toxin-producing” E. coli, or STEC for short. You might hear them called verocytotoxic E. coli (VTEC) or enterohemorrhagic E. coli (EHEC); these all refer generally to the same group of bacteria. The most commonly identified STEC in North America is E. coli O157:H7 (often shortened to E. coli O157 or even just “O157”). When you hear news reports about outbreaks of “E. coli” infections, they are usually talking about E. coli O157. (Source: CDC.)

Related Links

This latest outbreak comes amid ongoing investigation into another Outbreak of E. coli O157:H7

Multistate Outbreak of E. coli O157:H7 Infections Linked to Eating Raw Refrigerated, Prepackaged Cookie Dough

Updated June 25, 2009

States Where Persons Infected with the Outbreak Strain of E. coli O157:H7 Live, United States, by State, March 1, 2009 to June 25, 2009

A map of the United States displaying cases of E. coli as of March 1, 2009 to June 25, 2009Click map to view a larger image.

Infections with the Outbreak Strain of E. coli O157:H7 By Date of Report to PulseNet

a chart showing, by month, infections related to E. coli O157:H7 reported to PulseNet.Click map to view a larger image.

CDC is collaborating with public health officials in many states, the United States Food and Drug Administration (FDA), and the United States Department of Agriculture Food Safety and Inspection Service (FSIS) to investigate an outbreak of E. coli O157:H7 infections.

As of Thursday, June 25, 2009, 69 persons infected with a strain of E. coli O157:H7 with a particular DNA fingerprint have been reported from 29 states. Of these, 46 have been confirmed by an advanced DNA test as having the outbreak strain; these confirmatory test results are pending on the others. The number of ill persons identified in each state is as follows: Arizona (2), California (3), Colorado (5), Connecticut (1), Delaware (1), Georgia (1), Iowa (2), Illinois (5), Kentucky (3), Massachusetts (4), Maryland (2), Maine (3), Minnesota (6), Missouri (1), Montana (1), North Carolina (2), New Hampshire (2), New Jersey (1), Nevada (2), Ohio (3), Oklahoma (1), Oregon (1), Pennsylvania (2), South Carolina (1), Texas (3), Utah (2), Virginia (2), Washington (6), and Wisconsin (1).

Ill persons range in age from 2 to 65 years; however, 64% are less than 19 years old; 73% are female. Thirty-four persons have been hospitalized, 9 developed hemolytic uremic syndrome (HUS); none have died. Reports of these infections increased above the expected baseline in May and continue into June.

Investigation of the Outbreak

In an epidemiologic study, ill persons answered questions about foods consumed during the days before becoming ill and investigators compared their responses to those of persons of similar age and gender previously reported to State Health Departments with other illnesses. Preliminary results of this investigation indicate a strong association with eating raw prepackaged cookie dough. Most patients reported eating refrigerated prepackaged Nestle Toll House cookie dough products raw.

E. coli O157:H7 has not been previously associated with eating raw cookie dough. CDC, the state health departments, and federal regulatory partners are working together in this ongoing investigation.

Clinical Features

Most people infected with E. coli O157:H7 develop diarrhea (often bloody) and abdominal cramps 2-8 days (average of 3-4 days) after swallowing the organism, but some illnesses last longer and are more severe. Infection is usually diagnosed by culture of a stool sample. Most people recover within a week, but some develop a severe infection. A type of kidney failure called hemolytic uremic syndrome (HUS) can begin as the diarrhea is improving; this can occur in people of any age but is most common in children under 5 years old and the elderly.

Advice to Consumers

The Food and Drug Administration (FDA) and the Centers for Disease Control and Prevention are warning consumers not to eat any varieties of prepackaged Nestle Toll House refrigerated cookie dough due to the risk of contamination with E. coli O157:H7. If consumers have any prepackaged, refrigerated Nestle Toll House cookie dough products in their home they should throw them away. Cooking the dough is not recommended because consumers might get the bacteria on their hands and on other cooking surfaces. The recall does not include Nestle Toll House morsels, which are used as an ingredient in many home-made baked goods, or other already baked cookie products.

Individuals who have recently eaten prepackaged, refrigerated Toll House cookie dough and have experienced any of these symptoms should contact their doctor or health care provider immediately. Any such illnesses should be reported to state or local health authorities.

Consumers should be reminded they should not eat raw food products that are intended for cooking or baking before consumption. Consumers should use safe food-handling practices when preparing such products, including following package directions for cooking at proper temperatures; washing hands, surfaces, and utensils after contact with these types of products; avoiding cross contamination; and refrigerating products properly.
Advice to Retailers, Restaurateurs, and Food-service Operators

Retailers, restauranteurs, and personnel at other food-service operations should not sell or serve any Nestle Toll House prepackaged, refrigerated cookie dough products subject to the recall.

For additional information


Posted in Ecoli infection, Greenley, ecoli, ecoli bacteria, meat recall | Tagged: , , , , | 1 Comment »

House Passes Emissions Bill

Posted by feww on June 27, 2009

Posted in CO2 Emissions, Cap and Trade, Energy and Commerce Committee, pollution control, too little too late | Tagged: , , , , | Leave a Comment »

Eco-Terrorism and Dead Rare Sunfish

Posted by feww on June 27, 2009

Guilty of Eco-Terrorism: Tourists and Tour Operators

Eco-Tourists [sic] and Eco Tour Operators [sic] are systematically destroying the fragile marine environment in the south Pacific and Southern [Antarctic] oceans.

“Eco-tourists” love dead natural beauty, at least according to a short article in New Zealand Nelson Mail:

“Tourists being guided along Farewell Spit were mesmerised by more than just the area’s natural beauty yesterday.

“A large sunfish, about 2 metres long, and 2m wide from fintip to fintip, was spotted as Farewell Spit Eco Tours driver John Stevens was heading towards the spit with a busload of tourists.”

Dead Rare SunfishDo the eco-terrorists get a warm sensation rushing through their body knowing they are alive and can spot the dad rare sunfish, but the dead fish can’t see them?

Look What We Caught! [Original caption: STRANGE FIND.  Shelley Climo from the Farewell Spit Eco Tours office with the sunfish, found near Puponga township.] Photo: PADDY GILLOOLY/Farewell Spit Eco Tour (Via Nelson Mail). Image may be subject to copyright.

According to Farewell Spit Eco Tours owner Paddy Gillooly “the sunfish fascinated the tourists.”

“It was quite a good way to start the day. It’s one of the biggest ones I’ve seen.”

“The day before, tourists had seen a small dead minke whale that had washed up on the spit, and had since been washed away again.” The Nelson Mail said.

How very revealing!

“Mr Gillooly said he had seen about half a dozen sunfish washed up at the spit over the years. Because they could not manoeuvre easily, they could get washed into shallow water and stuck there.”

But do they all die of natural causes [sic]?

They were also a “very hard fish”, he said.

“Boaties and yachts sometimes [very often] run into them, and the yacht will [sometimes] come off second best.”

Source:  http://www.stuff.co.nz/environment/2542883/Sunfish-a-rare-sight

The world cannot survive with the impact of airline industry and tourism, but the “economy” can cope without the two!

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Posted in Farewell Spit, eco-terrorism, marine ecology, sunfish, tasman sea massacre | Tagged: , , , , | Leave a Comment »

How Sarychev Peak Moved from Russia to Japan!

Posted by feww on June 25, 2009

Better late than never mate, goes the Australian saying

As for the reporting accuracy, close but no shrimps!

better late than never mate
Sarychev Volcano moved to Japan (!) See section underlined in red.
A condensed screen dump of the news URL at Australia’s Melbourne Herald Sun site http://www.news.com.au/heraldsun/story/0,21985,25688161-24331,00.html

Even the Aussies should be entitled to accurate, prompt reporting!

Heaven knows we have criticized Earth Observatory often enough for holding on to images of public interest instead of releasing them instantly on Internet.  However it took the Australian broadcaster nearly two weeks and a major political shift, taking the Sarychev Peak out of the hands of Russians and handing it over to the Japanese, to report the eruption.

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Posted in Sarychev Peak erupted, Sarychev activity, reporting accuracy, volcanic eruption, volcanoes | Tagged: , , , , | Leave a Comment »