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He was still chuckling when he spoke, sage from much experience of ocean travel. The Antarctic Circumpolar Current encircles that continent, influencing the area’s climate and connecting currents in several oceans. Early ancestors of the ocean’s biggest animals once walked on land. Follow their extraordinary journey from shore to sea.  The ocean is not only home to dolphins and jellyfish, whales, and sharks. It’s also a museum where stories about life on the sea, not recorded in the books, are discovered. Uncover the human stories behind shipwrecks, including some of the most famous ones, including the Titanic. Are you ready to go back in time? Tune in to Ocean Today’s latest “Full Moon” video collection! It is often stated that the thermohaline circulation is the primary reason that the climate of Western Europe is so temperate. An alternate hypothesis claims that this is largely incorrect, and that Europe is warm mostly because it lies downwind of an ocean basin, and because atmospheric waves bring warm air north from the subtropics.[39][40] “It’s estimated that 95 percent of the livable space on our planet is in the ocean, yet only a fraction of that space has been explored,” said study lead author Carole Baldwin of the NMNH. There, we might find something to eat; of which there was little hope, out on the ocean. Supercritical fluids, although not liquids, do share various properties with liquids. Underneath the thick atmospheres of the planets Uranus and Neptune, it is expected that these planets are composed of oceans of hot high-density fluid mixtures of water, ammonia and other volatiles.[86] The gaseous outer layers of Jupiter and Saturn transition smoothly into oceans of supercritical hydrogen.[87][88] The atmosphere of Venus is 96.5% carbon dioxide, which is a supercritical fluid at its surface. Puffer fish and tropical fish spawn in lukewarm and warm oceans. hello@oceanobservations.com A zone of rapid salinity increase with depth is called a halocline. The temperature of maximum density of seawater decreases as its salt content increases. Freezing temperature of water decreases with salinity, and boiling temperature of water increases with salinity. Typical seawater freezes at around −1.9 °C at atmospheric pressure. If precipitation exceeds evaporation, as is the case in polar and temperate regions, salinity will be lower. If evaporation exceeds precipitation, as is the case in tropical regions, salinity will be higher. Thus, oceanic waters in polar regions have lower salinity content than oceanic waters in temperate and tropical regions.[55] Theoretical models have been used to predict with high probability that GJ 1214 b, detected by transit, is composed of exotic form of ice VII, making up 75% of its mass,[70] making it an ocean planet. Oceana Canada, an ocean research charity, is hoping citizen scientists in Halifax armed with DNA kits will help them sniff out seafood fraud. (Elaine Thompson/Associated Press) A global layer of liquid water thick enough to decouple the crust from the mantle is thought to be present on the natural satellites Titan, Europa, Enceladus and, with less certainty, Callisto, Ganymede[62][63] and Triton.[64][65] A magma ocean is thought to be present on Io. Geysers have been found on Saturn’s moon Enceladus, possibly originating from about 10 kilometers (6.2 mi) deep ocean beneath an ice shell.[57] Other icy moons may also have internal oceans, or may once have had internal oceans that have now frozen.[66] GCOS Implementation Plan 2016   !NEW! Publications GOOS webinar on OceanSITES’ Unique Role in the Observing System Available here OceanSITES poster at EGU2015 Poster 1 Poster 2 Deep-Ocean T/S Challenge: Contribute a deep-ocean T/S Sensor! More information How: Develop a mobile app that unlocks ocean data for public and/or private benefit, ideally while supporting responsible use and protection of our ocean. In fact, getting to the deepest reaches of the ocean is so expensive that some people – like Oscar-winning director James Cameron – take it upon themselves to explore underwater spaces rarely visited by humans. New studies show complex effects of carbon dioxide on fish population. Many studies have shown that larvae of various fish species can be negatively affected by ocean acidification. Acidification is caused by large amounts of carbon dioxide (CO2) entering the seawater from the atmosphere. But CO2 can also influence the food supply for the fish … more Oregon’s year-round fishing spans the state from native redband trout in eastern deserts to rockfish and halibut in ocean waters – with lots of salmon, steelhead, trout and warmwater fishing in between. Whether your plans take you to a nearby neighborhood pond or to one of the state’s premiere fishing destinations, there will be a place for you to fish in Oregon every day of the year. This scientific research informs debates on issues including climate change, ocean acidification and plastics in the sea. A new ocean cleanup prototype is being deployed on the North Sea today. It is one of the last steps as we prepare to launch the first cleanup system in the Great Pacific Garbage Patch this summer. To understand how we arrived at this point, here is a brief history of the North Sea prototypes, and the reasons why we’re deploying another… We must know the value of our ocean to ensure conservation has a voice in ocean development. „Życie to podróż, to ocean” to zapis rozmowy jaką Artur Cieślar odbył z Julią Hartwig, poetką, tłumaczką, eseistką. To niezwykle miła pogawędka dwojga wyważonych, pogodzonych z losem ludzi, którzy ową harmonią, spokojem i ciepłą atmosferą czarują czytelnika od pierwszych słów. Julia Hartwig początkowo nie chciała się zgodzić na ten wywiad. Jest skromna, nie lubi zamieszania wokół siebie i nie przepada za opowiadaniem o swojej osobie. Na tę publikację namówił ją dopiero jej wieloletni przyjaciel, Jerzy Illg. Powstała w ten sposób niewielkich rozmiarów książeczka, w której pani Julia robi wszystko, byle pozostać w cieniu. Żałuję ogromnie, iż autoryzując tekst, usunęła najbardziej intymne zwierzenia i pozbawiła swoich czytelników możliwości głębszego poznania. “Najważniejsze jest to, czy mam coś do przekazania. Jeśli nie, to szkoda sobie i innym zabierać czas”, wyznaje autorka. Widocznie jej przekaz nie musi być pokaźnych rozmiarów, by robił wrażenie. Czy zatem mamy szansę natrafić w… Some planets and natural satellites outside the Solar System are likely to have oceans, including possible water ocean planets similar to Earth in the habitable zone or “liquid-water belt”. The detection of oceans, even through the spectroscopy method, however is likely extremely difficult and inconclusive. Join the next generation taking the ocean crisis into their own hands.  The partnership spans fisheries, aquaculture, oil and gas, marine bio products, transportation, defence, marine renewables, and ocean technology. Companies are collaborating to define a shared innovation roadmap based on common challenges and requirements. A team at Massachusetts Institute of Technology has unveiled their own solution—an ultrasound-controlled, soft robotic fish. It’s not the only fish robot out there, but it could be the first that can swim in three dimensions, untethered, in the open ocean. Such a robot has the potential to transform the way biologists study the ocean. The deepest point in the ocean is the Mariana Trench, located in the Pacific Ocean near the Northern Mariana Islands. Its maximum depth has been estimated to be 10,971 meters (35,994 ft) (plus or minus 11 meters; see the Mariana Trench article for discussion of the various estimates of the maximum depth.) The British naval vessel Challenger II surveyed the trench in 1951 and named the deepest part of the trench the “Challenger Deep”. In 1960, the Trieste successfully reached the bottom of the trench, manned by a crew of two men. Oceanographers divide the ocean into different vertical zones defined by physical and biological conditions. The pelagic zone includes all open ocean regions, and can be divided into further regions categorized by depth and light abundance. The photic zone includes the oceans from the surface to a depth of 200 m; it is the region where photosynthesis can occur and is, therefore, the most biodiverse. Because plants require photosynthesis, life found deeper than the photic zone must either rely on material sinking from above (see marine snow) or find another energy source. Hydrothermal vents are the primary source of energy in what is known as the aphotic zone (depths exceeding 200 m). 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