The average ocean temperature hovers around 73 degrees in August, making
it the warmest ocean water off the coast of California.
Not exact matches
From crab caught
off the coast of New England to the succulent salmon found in the cool
waters of the Northwest to the tender tuna from the
warm shores of Hawaii, there is no shortage of
ocean eats in the United States.
El Niño is an abnormal periodic
warming of surface
ocean water off the Pacific coast of South America.
But temperature measurements taken
off the continent's coast found
warm water brewing up from the
ocean depths.
Velicogna and her colleagues also measured a dramatic loss of Greenland ice, as much as 38 cubic miles per year between 2002 and 2005 — even more troubling, given that an influx of fresh melt
water into the salty North Atlantic could in theory shut
off the system of
ocean currents that keep Europe relatively
warm.
El Nino's mass of
warm water puts a lid on the normal currents of cold, deep
water that typically rise to the surface along the equator and
off the coast of Chile and Peru, said Stephanie Uz,
ocean scientist at Goddard Space Flight Center in Greenbelt, Maryland.
A new study by NOAA researchers suggests future
warming of
ocean waters off the Northeastern U.S. may be greater and occur at an even faster rate than previously projected.
A new study led by the University of Texas Institute for Geophysics has found that wind over the
ocean off the coast of East Antarctica causes
warm, deep
waters to upwell, circulate under Totten Ice Shelf, and melt the fringes of the East Antarctic ice sheet from below.
The one - two punch of
warming waters and
ocean acidification is predisposing some marine animals to dissolving quickly under conditions already occurring
off the Northern California coast, according to a study from the University of California, Davis.
That's because a current of cold
ocean water moves from north to south along the West Coast, cooling the coastal Pacific and removing the threat of hurricanes, which form only when low pressure systems siphon
off the energy from
warm ocean water.
A team of researchers from the GEOMAR Helmholtz Centre for
Ocean Research Kiel together with colleagues from Bergen, Oslo and Tromsø (Norway), have now discovered that large - scale sedimentation caused by melting of glaciers in a region off Norway has played a greater role in gas hydrate dissociation than warming ocean wa
Ocean Research Kiel together with colleagues from Bergen, Oslo and Tromsø (Norway), have now discovered that large - scale sedimentation caused by melting of glaciers in a region
off Norway has played a greater role in gas hydrate dissociation than
warming ocean wa
ocean waters.
There also was an assumption that many melting glaciers on the ice sheet's periphery eventually would retreat to higher ground on this flat bedrock, cutting
off contact with
warm ocean waters and slowing down the ice sheet's shedding.
If
water temperatures in the Atlantic are higher than normal, as they are now, hurricanes, which feed
off warm ocean water, are more likely to form.
In the Pacific and Indian
oceans, for example,
warming water has already kicked
off a coral bleaching event.
During normal conditions, trade winds blow to the west across the tropical Pacific
Ocean, piling up
warm surface
water in the western Pacific, and cold, deeper
water rises up, or upwells,
off the west coast of South America.
The Center for
Ocean Solutions writes: «Between 1951 and 1993 zooplankton biomass
off Southern California decreased by 80 % as a result of
warming surface
waters.»
Hurricanes feed
off warm water and the theory that rising
ocean temperatures are making them stronger than they would otherwise have been has been around for a long time.
As you cross over the border into Mozambique you'll load the boards onto 4x4s and get well
off the beaten track, tackling sand roads in search of
warm water perfection, enjoying evening yoga sessions by the
ocean and snorkelling with manta rays on an
ocean safari.
An area of
warm ocean water many scientists call «the blob» began forming
off the U.S. West Coast in 2013.
Snorkeling in the nearby
ocean offers hours of fun and enjoyment in the
warm gentle
waters off the coast.
Kick
off your shoes and feel the
warm, sensual sand massage your feet... dance along
water's edge, bathe them in the soothing surf... breathe deeply the fresh scent of
ocean spray... awaken your inner being
Always beckoning are the
warm waters of the Pacific
Ocean, where it's not uncommon to see dolphins join the surfers
off the rocky points.
About 500 km
off the southern tip of India, in the midst of the
warm and turquoise
waters of the Indian
Ocean lies the most fantastic paradise in the world, the beautiful and idyllic Maldives.
Bathing in the
warm waters of the Indian
Ocean off the east coast of Africa is a natural paradise: Madagascar has manged to keep its exotic appeal intact, becoming a luxury destination for those who love nature and simplicity, perfect for an unforgettable honeymoon.
The abundant
waters off the coast of Cabo San Lucas — located at the southern tip of the Baja Peninsula, where the calm and
warm waters of the Sea of Cortez mixes with the unfathomable cool currents of the Pacific
Ocean — offer the ideal conditions for plenty of sport - fish species, including (among others) Rooster Fish, Mahi Mahi (known locally as Dorado), varieties of Tuna, Sharks, Jacks, Groupers, and Billfish such as Sailfish, Swordfish, Black Marlin, Blue Marlin and Striped Marlin.
This isn't due to a
warming ocean (though the deep
water off the Antarctic coast line is indeed
warming), but to changes in the winds that have forced more circumpolar deep
water onto the continental shelf.
That'd be a hint that
warm water could indeed get in under the icecap once the edges melt
off, unblocking the deep channels and allowing
water to circulate in and out from the southern
ocean — wouldn't it?
However, at the same time, there's been the steady increase in subtropical
ocean surface temperatures in the Atlantic
Warm Pool, leading to record
water temperatures
off the US east coast in winter, which tends to fuel more extreme storms (via the increase in
water vapor pressure over the
warmer ocean).
In an article on Yale 360 Environment, Veron writes that the major issues include mass bleachings caused by
warmer water, which kills
off zooxanthellae, the algae with which coral have a symbiotic relationship, and
ocean acidification.
The entire North Atlantic is unusually
warm right now (+0.6 degrees Celsius) relative to the already - globally -
warmed late twentieth century (1971 - 2000) average, and there are large patches of
ocean water off the US East Coast that are 2 - 4 degrees Celsius above that average.
Meanwhile, in the Pacific
Ocean, there's a long, skinny blob of unusually
warm water off the West Coast, stretching from Mexico to Alaska.
El Ni o an irregular variation of
ocean current that, from January to February, flows off the west coast of South America, carrying warm, low - salinity, nutrient - poor water to the south; does not usually extend farther than a few degrees south of the Equator, but occasionally it does penetrate beyond 12 S, displacing the relatively cold Peruvian current; usually short - lived effects, but sometimes last more than a year, raising sea - surface temperatures along the coast of Peru and in the equatorial eastern Pacific Ocean, having disastrous effects on marine life and fi
ocean current that, from January to February, flows
off the west coast of South America, carrying
warm, low - salinity, nutrient - poor
water to the south; does not usually extend farther than a few degrees south of the Equator, but occasionally it does penetrate beyond 12 S, displacing the relatively cold Peruvian current; usually short - lived effects, but sometimes last more than a year, raising sea - surface temperatures along the coast of Peru and in the equatorial eastern Pacific
Ocean, having disastrous effects on marine life and fi
Ocean, having disastrous effects on marine life and fishing
From the article: A new study released Monday found that
warming temperatures in Pacific
Ocean waters off the coast of North America over the past century closely followed natural changes in the wind, not increases in greenhouse gases related to global
warming.
It can not account for the huge volume of leftover
warm water that's below the surface and returned to the West Pacific and into the eastern tropical Indian
Ocean via
off - equatorial slow - moving Rossby waves.
Researchers travelled to the Southern
Ocean off Antarctica — one of the most remote and inaccessible
oceans in the world — to investigate how
warm water is making its way to the ice sheets, causing them to melt.
These models predicted that the Northern Hemisphere Polar region would
warm fastest and first, that the Southern
Ocean would draw a greater portion of atmospheric heat into the ocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh water flows into the nearby ocean zones and set off localized coo
Ocean would draw a greater portion of atmospheric heat into the
ocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh water flows into the nearby ocean zones and set off localized coo
ocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh
water flows into the nearby
ocean zones and set off localized coo
ocean zones and set
off localized cooling.
Ever since the early 1990s, scientific reports have highlighted the vulnerability of West Africa to inundation, flooding and loss of key industries, food growing and infrastructure due to glacial melt, thermal expansion of
ocean waters set
off by
warming, and an increase in storm strength in the North Atlantic.
Corals have been dying due to
warmer waters and will continue to die -
off at faster rates as the
ocean temperature continue to rise.
For example, reductions in seasonal sea ice cover and higher surface temperatures may open up new habitat in polar regions for some important fish species, such as cod, herring, and pollock.128 However, continued presence of cold bottom -
water temperatures on the Alaskan continental shelf could limit northward migration into the northern Bering Sea and Chukchi Sea
off northwestern Alaska.129, 130 In addition,
warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If
ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.134
El Niño is a weather phenomenon where the Pacific trade winds inexplicably falter not just a few days, but for weeks or months causing a band of
warmer than usual
ocean water to develop
off the Pacific coast of South America, particularly around where Peru is.
I will continue to fight for the health of the
waters off of New England and the United States, and against the dangerous effects of global
warming on
oceans everywhere.
The «blob» is a giant patch of unusually
warm water off the West Coast in the northeast Pacific
Ocean.
Forecasters are increasingly confident in a particularly big El Niño this time around because, deep below the Pacific
Ocean's surface,
off - the - charts
warm water is lurking:
They are feeding
off ever -
warming ocean waters.
The theory that the thermohalene
ocean current would slow because of global
warming says that it would slow down because of massive melt -
off of ice in Greenland, and the Arctic Sea, that would add a lot of fresh
water to the North Atlantic.
The white areas
off the Tropical Western coasts of northern South and all Central America as well as along the Central - eastern equatorial and Southeastern Pacific
Ocean indicate the pool of
warm water.
Hurricanes can be thought of, to a first approximation, as a heat engine; obtaining its heat input from the
warm, humid air over the tropical
ocean, and releasing this heat through the condensation of
water vapor into
water droplets in deep thunderstorms of the eyewall and rainbands, then giving
off a cold exhaust in the upper levels of the troposphere (~ 12 km / 8 mi up).
Both hurricanes and typhoons are strong tropical cyclones, which are storms that form over
warm ocean waters, have a well defined center of circulation, and feed
off of heat energy from the
ocean.
When they saw a massive coral reef die -
off in the area in September 2010, the team suspected that a dead zone instead of
warm or acidic
ocean water could be the culprit.
Scientists like Mann have also linked
warm ocean temperatures
off New England to the dramatic snowfalls that Boston experienced earlier this year — noting that
warmer water means there is more moisture in the atmosphere above it.