JAVA -  SARGASSO SEA

 

 

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SARGASSUM - The giant brown seaweed, having shown that it can spread from North to South Atlantic oceans, could spread to the Indian and Pacific oceans as a potentially invasive species. The proof of which (as a theory) is satellite pictures, and changing wind states. The spread witnessed here, could just as easily migrate between oceans, and thence to the bays and seas within those oceans.

 

 

 

 

 

We are concerned that with the oceans warming at a faster rate than predicted, and with the spill over of sargassum from the Sargasso Sea in the North Atlantic, to create an Atlantic Equatorial sargassum gyre, that it is almost inevitable, and we might expect to see a South Atlantic sargassum gyre in the not too distant future, in proportion to insolation, since photosynthesis is the propagator of plant life.

 

If that comes to pass, and with the Indian and Pacific oceans also warming at the same rate as the Atlantic, so generating faster currents and winds; spillage around the horns could become a distinct possibility. In which case, the Java Sea could be a prime contender for a micro sargassum gyre. Dependent on location current circulation conditions. Or at least may suffer a similar fate to the Caribbean Sea, where the islands therein suffer beaches strewn with mounds of sargassum, to ruin fishing, tourism and marine ecology.

 

ABOUT THE JAVA SEA

 

The Java Sea (Indonesian: Laut Jawa, Javanese: Segara Jawa) is an extensive shallow sea on the Sunda Shelf, between the Indonesian islands of Borneo to the north, Java to the south, Sumatra to the west, and Sulawesi to the east. Karimata Strait to its northwest links it to the South China Sea. It is a part of the western Pacific Ocean.

The Java Sea covers the southern section of the 1,790,000 km2 (690,000 sq mi) Sunda Shelf. A shallow sea, it has a mean depth of 46 m (151 ft). It measures about 1,600 km (990 mi) east-west by 380 km (240 mi) north-south and occupies a total surface area of 320,000 km2 (120,000 sq mi).

It formed as sea levels rose at the end of the last ice age. Its almost uniformly flat bottom, and the presence of drainage channels (traceable to the mouths of island rivers), indicate that the Sunda Shelf was once a stable, dry, low-relief land area (peneplain) above which were left standing a few monadnocks (granite hills that, due to their resistance to erosion, form the present islands).

The southern section of the seafloor has long been recognized as geologically similar to northern Java, where oil fields occur and extend under the sea. Prospects are also favourable for oil fields in the waters off southeast Kalimantan. As the site of successful exploration for petroleum and natural gas, the Java Sea has become the basis of Indonesia's export program.

Fishing is an important economic activity in the Java Sea. Over 3,000 species of marine life are found in the area. A number of national parks exist in the area such as Karimunjawa. The Thousand Islands are located north of the national capital Jakarta, and are the city's only regency.

The area around the Java Sea is also a popular tourist destination. Scuba diving offers a chance to explore and photograph underwater caverns, wrecks, coral, sponges, and other marine life.

 

 

 

 

 

 

 

 

INDONESIA & CLIMATE CHANGE

Indonesia lies between latitudes 11°S and 6°N, and longitudes 95°E and 141°E. It is the world's largest Archipelagic state, extending 5,120 kilometres (3,181 mi) from east to west and 1,760 kilometres (1,094 mi) from north to south. The country's Coordinating Ministry for Maritime and Investments Affairs says Indonesia has 17,504 islands (with 16,056 registered at the UN) scattered over both sides of the equator, around 6,000 of which are inhabited. The largest are Sumatra, Java, Borneo (shared with Brunei and Malaysia), Sulawesi, and New Guinea (shared with Papua New Guinea).

Indonesia lies along the equator, and its climate tends to be relatively even year-round. Some regions, such as Kalimantan and Sumatra, experience only slight differences in rainfall and temperature between the seasons, whereas others, such as Nusa Tenggara, experience far more pronounced differences with droughts in the dry season and floods in the wet. Rainfall varies across regions, with more in western Sumatra, Java, Indonesia has two seasons - a wet season and a dry season - with no extremes of summer or winter. For most of Indonesia, the dry season falls between May and October, with the wet season between November and April. Indonesia's climate is almost entirely tropical, dominated by the tropical rainforest climate found in every large island of Indonesia.

Several studies consider Indonesia to be at severe risk from the projected effects of climate change. These include unreduced emissions resulting in an average temperature rise of around 1 °C (2 °F) by mid-century, raising the frequency of drought and food shortages (with an impact on precipitation and the patterns of wet and dry seasons, and thus Indonesia's agriculture system) as well as numerous diseases and wildfires. Rising sea levels would also threaten the majority of Indonesia's population who lives in low-lying coastal areas. Impoverished communities would likely be affected the most by climate change.

ORIGINS OF SARGASSUM

 

The North Atlantic Sargasso Sea is where sargassum originates and was contained for hundreds of years, until climate change and intensive farming. But should the unthinkable happen, and the invasive species take hold in the South Atlantic, from whence to spread it's biological advantage, one can imagine the dire consequences, perhaps mirroring that now ruining the Caribbean Sea. Make no mistake, the consequences of climate change and intensive, fertilizer based farming, could become a deadly world contagion, to make other epidemics seem insignificant, in terms of potential human tragedy.

 

An animal has a means to exhaust toxic waste, essential for a healthy lifestyle. The oceans have nowhere to dump the excrement we dump in it. They just get more polluted. Except for sargassum piling onto the shores, telling us that we have reached the limit.

 

So, what are the chances of it happening? Could there be a 'Java Sargasso Sea,' or belt, where the present welcoming waters are turned into a cesspit of foul smelling rotten seaweeds, as they release hydrogen sulphide gas to choke visitors to their shores.

 

COMPUTER SIMULATIONS & CONTAINMENT DEVICES

 

That all depends on temperature rise of seawater, combined with nutrient supply, and circulating currents, including winds. All of which is measurable, for variable algorithmic computer simulations. As has been performed on the influx to the Caribbean Sea, via the equatorial Atlantic gyre, by scientists at the University of South Florida in St. Petersburg's College of Marine Science, who used NASA satellite observations to discover and document the largest bloom of macroalgae. Others used Global Hybrid Coordinate Ocean Model surface currents (HYCOM) (Chassignet et al., 2007) and National Centers for Environmental Prediction Reanalysis (NCEP), in their simulations.

 

But nobody has yet created a computer model of a SeaVax Calypso or Sargasso, used in various (fleet SeaNet formations) to determine if such a concept could control volume escalation, before they grow to be profusely irrepressible. Indeed such simulations may help develop such concepts in terms of capacity and operations, that they may, or may not, contain the crisis, preventing a worldwide state of emergency - by nipping it in the bud.

 

THEORY DEVELOPMENT

 

At this stage of the formulation of his theory, the innovator is considering the awful prospect, based on the demonstrable and devastating spread of sargassum from the North Atlantic to the Equatorial South Atlantic, but not yet migrating to the more general south, due presumably, to temperatures not yet being to the liking of the buoyant seaweed.

 

The three major oceans are all interconnected via currents and driving winds. The main barrier to migration at present, is the temperature and level of nutrients, that is lower where the seaweed mats could pass from one to another. But that is by no means a hard point, as the melting of the polar caps indicates. We are living in changeable times, where the unthinkable is taking place, as a pace faster than previously supposed.

 

In other words, the impossible is rapidly becoming possible. And there is no containment system at present, to prevent that from happening; no international coordination, or action plan. A recipe for disaster you may think!

 

FACTUAL BACKGROUND

 

The sargassum crisis seen in the Caribbean Sea and Gulf of Mexico could be just the beginning of a worldwide plague, stemming from our inability to curb political insatiability for fossil fuels - to power failing economic strategies, based on growth, when we have already used up the planet twice over, in sustainable terms.

 

The answer to failed political policies is very often a jolly good war, (Russia Vs Ukraine). When all cock-ups get thrown to the wind in the media scrum, and a whitewash ensues, until the next band of post-war cutthroats is elected, each with their hands in the pockets of Lucifer's climate change deniers. That said, it would take a nuclear conflict to reduce earth's population significantly enough to brake global warming - but then the planet would be barren and unable to support human life. Hence, an unthinkable solution to all but the most desperate of homicidal kleptocrats: warmongers.

 

But, ignoring thermonuclear first strikes for now, even if we transition to renewables immediately, global warming will not reverse for 30-50 years at best, and that is with a fair political wind. Meaning that the conditions for sargassum to populate welcoming equatorial waters (rich in nutrients) around the globe, remains a distinct possibility. Such as the:

 

 

Arabian Sea

Atlantic - North & South Equatorial

Banda Ceram Molucca & Timor Seas

Bay of Bengal

Celebes Sea

Gulf of Guinea

Gulf of Thailand

Indian Ocean

Java Sea

Pacific Ocean - North & South, Equatorial Belt (Costa Rica, Ecuador, Panama regions)

Philippine Sea

South China Sea

 

 

Seas and oceans in these latitudes could become inundated with macro algae, if the rafts of floating seaweed manage to navigate less hospitable barriers, such as colder regions. Which at the moment, Cape Horn and the Cape of Good Hope appear to offer some protection from invasion.

 

THESIS

 

This is a theory proposed by Nelson Kay (as a volunteer) in August of 2022, based on his work with the SeaVax team from 2016 - 2020. Though that exertion was mostly concerning micro and macro plastic recovery and river containment, the ocean engineering and logistical challenges posed by SeaVax are kindred concepts, and may be sympathetically adapted or even interchangeable to some degree. And may one day inspire others to devise a practical resolution.

 

Academics and scientific institutions inclined to test such thesis, or otherwise wishing to provide data or technological assistance, positive or negative, should please contact the Cleaner Ocean Foundation in the first instance. The aim being to prove or disprove the concept, to advance our knowledge in this little understood area of Oceanology/Oceanography. Students at all levels are most welcome, as are degree level students and post graduates looking to higher level qualifications, or simply to gain experience.

 

There are a million reasons for not doing something, and only one for taking up a challenge. Most people will use manifold negatives to sit back in their armchairs, and postulate. But, every now and again, someone is foolhardy enough to roll their sleeves up - and experiment - because they feel they must. Despite the enormity of the task. And that is how this website came about, in support of the SeaVax project in 2017.

 

 

 

 

Honduras, Caribean island with a tide of plastic, pictures by Caroline Power    

 

 

PLASTIC TIDE - These amazing pictures of a giant plastic tide were taken by Caroline Power. Please note how plastic and sargassum intertwine, creating a separation problem.

 

 

 

 

 

 

CARIBBEAN ISLANDS UNDER THREAT A-Z

 

Anguilla

Antigua and Barbuda

Aruba (Netherlands)

Bahamas
Barbados

British Virgin Islands

Caribbean Netherlands

Cayman Islands (UK)

Cuba

Curaçao (Netherlands)

Dominica

Dominican Republic (Hispaniola)

Grenada

Guadeloupe (France) 
Haiti (Hispaniola)
Jamaica
Martinique (France) 
Montserrat
Puerto Rico (US) 

Roatán

Saint Barthélemy

Saint Kitts and Nevis

Saint Lucia 

Saint Martin 

Saint Vincent and the Grenadines
Sint Maarten (Netherlands)

Tortuga

Trinidad and Tobago

Turks and Caicos Islands
United States Virgin Islands 

 

 

 

 

 

 

 

 

LINKS & REFERENCE

 

http://www.

 

 

 

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 This website is provided on a free basis as a public information service. copyright © Cleaner Oceans Foundation Ltd (COFL) (Company No: 4674774) August 2022. Solar Studios, BN271RF, United Kingdom. COFL is a charity without share capital. The names AmphimaxRiverVax™ and SeaVax™ are trademarks.

 

 

 

 

 

WORLD PLAGUES GIANT SARGASSUM SEAWEED MIGRATIONS TO ALL OCEANS