Thursday, May 10, 2012

Big rise in North Pacific plastic waste


Gyre  


 Debris tends to collect within the North Pacific Subtropical Convergence Zone. Ocean eddies and other small ocean circulation features will further aggregate material into more discrete "garbage patches"

From BBC


The quantity of small plastic fragments floating in the north-east Pacific Ocean has increased a hundred fold over the past 40 years.
Scientists from the Scripps Institution of Oceanography documented the big rise when they trawled the waters off California.
They were able to compare their plastic "catch" with previous data for the region.
The group reports its findings in the journal Biology Letters.
"We did not expect to find this," says Scripps researcher Miriam Goldstein.
"When you go out into the North Pacific, what you find can be highly variable. So, to find such a clear pattern and such a large increase was very surprising," she told BBC News.
All the plastic discarded into the ocean that does not sink will eventually break down.
Sunlight and the action of the waves will degrade and shred the material over time into pieces the size of a fingernail, or smaller.
An obvious concern is that this micro-material could be ingested by marine organisms, but the Scripps team has noted another, perhaps unexpected, consequence.
The fragments make it easier for the marine insect Halobates sericeus to lay its eggs out over the ocean.
These "sea skaters" or "water striders" - relatives of pond water skaters - need a platform for the task.
Normally, this might be seabird feathers, tar lumps or even pieces of pumice rock. But it is clear from the trawl results that H. sericeus has been greatly aided by the numerous plastic surfaces now available to it in the Pacific.


 The fragments are tiny - about 5mm in diameter, or less


 
The team found a strong association between the presence of Halobates and the micro-plastic in a way that was just not evident in the data from 40 years ago.
Ms Goldstein explained: "We thought there might be fewer Halobates if there's more plastic - that there might be some sort of toxic effect. But, actually, we found the opposite. In the areas that had the most plastic, we found the most Halobates.
"So, they're obviously congregating around this plastic, laying their eggs on it, and hatching out from it. For Halobates, all this plastic has worked out well for them."


The micro-plastic has been a boon to one marine invertebrate - Halobates sericeus

Ms Goldstein and colleagues gathered their information on the abundance of micro-plastic during the Scripps Environmental Accumulation of Plastic Expedition (Seaplex) off California in 2009. They then compared their data with those from other scientific cruises, including archived records stretching back to the early 1970s.
Plastic waste in the North Pacific is an ongoing concern.
The natural circulation of water - the North Pacific Gyre - tends to retain the debris in reasonably discrete, long-lived collections, which have popularly become known as "garbage patches".
In the north-eastern Pacific, one of these concentrations is seen in waters between Hawaii and California.
This Scripps study follows another report by colleagues at the institution that showed 9% of the fish collected during the same Seaplex voyage had plastic waste in their stomachs.
That investigation, published in Marine Ecology Progress Series, estimated the fish at intermediate ocean depths in the North Pacific Ocean could be ingesting plastic at a rate of roughly 12,000 to 24,000 tonnes per year.

Crabs, barnacles, sea anemones and hydroids make a home on a piece of discarded rope
 
Toxicity is the issue most often raised in relation to this type of pollution, but Ms Goldstein and colleagues say broader ecosystem effects also need to be studied.
The abundance of ocean debris will influence the success, or otherwise, of "rafting communities" - those species that are specifically adapted to life on or around objects floating in the water.
Larger creatures would include barnacles and crabs, and even fish that like to live under some kind of cover, but large-scale change would likely touch even the smallest organisms.
"The study raises an important issue, which is the addition of hard surfaces to the open ocean," says Ms Goldstein.
"In the North Pacific, for example, there's no floating seaweed like there is in the Sargasso Sea in the North Atlantic. And we know that the animals, the plants and the microbes that live on hard surfaces are different to the ones that live floating around in the water.
"So, what plastic has done is add hundreds of millions of hard surfaces to the Pacific Ocean. That's quite a profound change."
Ms Goldstein's co-authors were Marci Rosenberg, a student at the University of California Los Angeles, and Scripps research biologist emeritus Lanna Cheng.

Wednesday, May 9, 2012

New nautical chart inset makes for safer sailing in Norfolk Inner Harbor



 
From NOAA

NOAA’s Office of Coast Survey has released an updated chart of Norfolk Harbor in time for Virginia’s War of 1812 Bicentennial events, when boats of all shapes and sizes descend on the area for twelve days of maritime activities.
The updated chart includes a new inset of the Norfolk Inner Harbor, which provides updated depth measurements and more details than the current chart.



The new inset on existing NOAA chart 12253, Norfolk Harbor and Elizabeth River, is at a 1:10,000 scale.
The improvement incorporates data acquired by two hydrographic surveys: one last year by NOAA Ship Thomas Jefferson and another by a Coast Survey navigation response team in 2010.
The re-surveys of the Norfolk Inner Harbor updated more than 600 charted features and provided new bathymetry along the entire Norfolk waterfront.

“The surveys and the new chart inset will help ensure the navigational safety of the hundreds of boats coming in and out of the harbor during the War of 1812 Bicentennial events,” explained NOAA Captain Doug Baird, chief of the Office of Coast Survey Marine Chart Division. “But this serves a broader economic need as well. The downtown area of Norfolk has developed as a multi-purpose port area, which requires a larger chart scale to support it.”
The larger scale coverage of the inner harbor area was requested by the Virginia Marine Pilot Association, which works closely with the Office of Coast Survey to ensure the safety of ships and mariners.

NOAA’s nautical charts come in a variety of formats, to meet the needs of different navigational systems.
The updated chart is now available to all mariners as a traditional paper chart from vendors, or as a Print on Demand chart through OceanGrafix.
Additionally, recreational boaters are able to download and print free BookletCharts designed especially for small boats: the War of 1812 Commemorative BookletChart and the updated regular edition for chart 12253 will be released later this month. NOAA’s electronic navigational chart will also be available shortly.

NOAA’s Office of Coast Survey has been the nation’s nautical chartmaker for two centuries.
Coast Survey contributes nautical charts, hydrographic data, and navigational assistance to the full range of NOAA’s navigational services.

USA NOAA update in the Marine GeoGarage





30 charts have been updated in the Marine GeoGarage
(NOAA update March/April 2012) and 1 chart added


  • 11304 NORTHERN PART OF LAGUNA MADRA
  • 11309 CORPUS CHRISTI BAY
  • 11323 APPROACHES TO GALVESTON BAY
  • 11345 NEW ORLEANS TO CALCASIEU RIVER WEST SECTION
  • 11412 TAMPA BAY AND ST JOSEPH SOUND
  • 11424 LEMON BAY TO PASSAGE KEY INLET
  • 12253 NORFOLK HARBOR AND ELIZABETH RIVER  (see Blog)
  • 12327 NEW YORK HARBOR
  • 13236 CAPE COD CANAL AND APPROACHES MA
  • 13272 BOSTON INNER HARBOR
  • 16161 KOTZEBUE HARBOUR AND APPROACHES   ***NEW***
  • 16660 COOK INLET NORTHERN PART
  • 16700 PRINCE WILLIAM SOUND
  • 17339 HOOD BAY AND KOOTZNAHOO INLET / KILLISNOO HARBOR
  • 17341 WHITEWATER BAY AND CHAIK BAY
  • 18400 STRAIT OF GEORGIA AND STRAIT OF JUAN DE FUCA
  • 18445 POSSESSION SOUND TO VASHON ISLAND PAGE A
  • 18448 PUGET SOUND SEATTLE TO OLYMPIA
  • 18645 GULF OF THE FARALLONES
  • 11351 POINT AU FER TO MARSH ISLAND
  • 11371 LAKE BORGNE AND APPROACHES CAT ISL TO POINT AUX HERBES
  • 11411 TAMPA BAY - PORT RICHEY TAMPA BAY - CLEARWATER HBR
  • 11415 TAMPA BAY ENTRANCE
  • 11503 ST MARYS ENTRANCE-CUMBERLAND SOUND AND KINGS BAY
  • 11555 CAPE HATTERAS WIMBLE SHOALS TO OCRACOKE INLET
  • 12324 SANDY HOOK TO LITTLE EGG HARBOR NEW JERSEY
  • 12335 HUDSON AND EAST RIVERS-GOVERNORS ISLAND TO 67TH STREET
  • 13221 NARRAGANSETT BAY RI-MA
  • 16663 NORTH FORELAND
  • 17337 WARM SPRING BAY CHATHAM STRAIT
  • 17338 PERIL STRAIT HOONAH SND-CHATHAM STRAIT

Today 1021 NOAA raster charts (2166 including sub-charts) are included in the Marine GeoGarage viewer.




Note : NOAA updates their nautical charts with corrections published in:
  • U.S. Coast Guard Local Notices to Mariners (LNMs),
  • National Geospatial-Intelligence Agency Notices to Mariners (NMs), and
  • Canadian Coast Guard Notices to Mariners (CNMs)
While information provided by this Web site is intended to provide updated nautical charts, it must not be used as a substitute for the United States Coast Guard, National Geospatial-Intelligence Agency, or Canadian Coast Guard Notice to Mariner publications

Please visit the
NOAA's chart update service for more info.

Canada CHS update in the Marine GeoGarage


15 charts have been updated (Apr 27, 2012) :

  • 1311    SOREL-TRACY TO VARENNES
  • 1313    BATISCAN TO LAC SAINT-PIERRE
  • 1314    DONNACONA TO BATISCAN
  • 1315    QUEBEC TO DONNACONA
  • 1510A    LAC DES DEUX MONTAGNES
  • 1510B    LAC DES DEUX MONTAGNES
  • 2085    TORONTO HARBOUR
  • 3462    JUAN DE FUCA STRAIT TO STRAIT OF GEORGIA
  • 3545    JOHNSTONE STRAIT PORT NEVILLE TO ROBSON BIGHT
  • 4367    FLINT ISLAND TO CAPE SMOKEY
  • 4416    HAVRE DE GASPE
  • 4452    HARBOURS AND ANCHORAGES / NORTH SHORE
  • 4454    POINTE CURLEW  TO BAIE WASHTAWOUKA
  • 4460    CHARLOTTETOWN HARBOUR
  • 4498    PUGWASH HARBOUR AND APPROACHES
  • 4909    BUCTOUCHE HARBOUR


So 790 charts (1677 including sub-charts) are available in the Canada CHS layer. (see coverage)

Note : don't forget to visit 'Notices to Mariners' published monthly and available from the Canadian Coast Guard both online or through a free hardcopy subscription service.
This essential publication provides the latest information on changes to the aids to navigation system, as well as updates from CHS regarding CHS charts and publications.
See also written Notices to Shipping and Navarea warnings : NOTSHIP

GPS on commercial ships could improve tsunami warnings



While in transit from Hawaii to Guam, the research vessel Kilo Moana detected the February 2012 Chilean tsunami. (Photo courtesy of University of Hawaii, School of Ocean and Earth Science and Technology)

From SOEST

Commercial ships travel across most of the globe and could provide better warnings for potentially deadly tsunamis, according to a study published May 5 by scientists at the University of Hawaii – Manoa (UHM) and the National Oceanic and Atmospheric Administration's Pacific Tsunami Warning Center. (see AGU)

James Foster, lead author and Assistant Researcher at the UH School of Ocean and Earth Science and Technology (SOEST), and colleagues were able to detect and measure the properties of the tsunami generated by the magnitude 8.8 earthquake in Maule, Chile (February 2010), even though, out in the open ocean, the wave was only about 4 inches (9.4 cm) high.
The UH research vessel Kilo Moana was on its way from Hawaii to Guam at the time of the tsunami, and was equipped with geodetic GPS system recording data as the tsunami passed by.

 Position of R/V Kilo Moana during 2010 Chile tsunami

Careful analysis of this data showed that the researchers were able to detect changes in the sea-surface height very similar to the Pacific Tsunami Warning Center predictions.
This finding came as a surprise because tsunamis have such small amplitudes in the deep water, in contrast to their size when they reach the coastline, that it seemed unlikely that the tsunami would be detected using GPS unless the ship was very close to the source and the tsunami was very big.
"Our discovery indicates that the vast fleet of commercial ships traveling the ocean each day could become a network of accurate tsunami sensors," Foster said.

Although the initial warning for a tsunami is based on seismic data from the earthquake, the details about whether a tsunami was actually generated, how big it is, and where the energy is directed are currently provided by tide gauges and deep ocean pressure sensors (DART system).
This is the information that is needed to accurately predict how big the tsunami will be for specific locations, and whether or not an evacuation, and the associated cost, is necessary.
Tide gauges are restricted to land and therefore are sparsely distributed, while the DART systems are very expensive and hard to maintain.
Consequently, during the 2010 Chilean earthquake, the DART sensor closest to Hawaii was out of order. In fact, nearly 30% of that network was down at the time.

Commercial shipping lines, however, run all around the Pacific basin and provide great coverage globally around tsunamigenic regions (areas of the Earth that produced tsunamis).
"If we could equip some fraction of the shipping fleet with high-accuracy GPS and satellite communications, we could construct a dense, low-cost tsunami sensing network that would improve our detection and predictions of tsunamis -- saving lives and money," Foster commented.
Foster and co-authors estimate that this sort of ship-based system would have been able to detect the 2004 Indian Ocean tsunami within an hour, potentially save thousands of lives.
"There are so many ships out there that if you've got enough of them instrumented with the GPS systems there is always going to be some ships in the neighborhood of the region that produces the tsunami," said Foster.
Much more advanced than a handheld GPS, the unit on a ship would include a round antenna to help measure and transmit even the slightest wave height changes from a tsunami that would likely go unnoticed in the open ocean.
The difference being measured in length of time.
"An open ocean swell has a period of maybe 15 seconds, 20 seconds. A tsunami takes maybe 20 minutes, half an hour to pass," said Foster.

At $15,000 to $20,000 per unit, the GPS is cheaper than the current deep ocean buoys that provide tsunami data.

 GPS Tsunami Meter utilizes floating buoy as observation instrument, in which Real-Time Kinematic GPS antenna is attached on the top of the buoy body

The challenge will be getting the commercial shipping lines to jump on board to create a mobile tsunami detection system.

Foster and fellow SOEST researchers plan to deploy a demonstration system which will stream GPS data from one or two ships, thus generating accurate real-time heights and confirming that this approach can achieve the accuracy needed for tsunami detection.
As a bonus, the same processing system will generate data that meteorologists can use to improve weather forecasts.

Links :