Warm
ocean currents make surrounding areas warmer and rainy.
Cool
ocean currents make surrounding areas cooler and drier Warmer and Rainy Warm Ocean Current Cooler and Drier Cool Ocean Current
The underwater landscape structure, tropical latitude and sea
ocean currents make Belize the proud home of the largest living coral reef in the Western Hemisphere.
The varied formations and mixed
ocean currents make for great snorkeling opportunities.
Not only do the vagaries of weather patterns and
ocean currents make it hard to see climate changes, but the variability in what are often termed the Earth System components complicates the picture enormously.
Not exact matches
What they've found is a country with pretty colonial towns and cities, miles of golden - sand beaches, an equatorial climate tempered by offshore
ocean currents and the mountain terrain to
make it spring - like year - round, and an incredibly low cost of living.
One possible scenario is that rising temperatures may alter
ocean currents, depriving Europe of the Gulf Stream and
making it more like Labrador or Siberia.
Oceans, lakes, and rivers can all have strong
currents and waves that could
make it difficult for you to hold onto your baby.
His
current work involves writing software to help detect whales in the
ocean as part of an effort to
make whales more «visible» to humans, partly so that people will be invested in saving whales from boat traffic and other dangers.
One thing scholars know for certain is that the very nature of the
ocean trade made prolonged periods of interaction necessary: The currents of the Indian Ocean change seasonally, and traders had to wait for months until currents shifted in favor of the return vo
ocean trade
made prolonged periods of interaction necessary: The
currents of the Indian
Ocean change seasonally, and traders had to wait for months until currents shifted in favor of the return vo
Ocean change seasonally, and traders had to wait for months until
currents shifted in favor of the return voyage.
Map of
current land and ice separating the Weddell and Ross seas, courtesy of Wikimedia Commons / Wutsje / CIA Octopuses have
made themselves at home in most of the world's
oceans — from the warmest of tropical seas to the deep, dark reaches around hydrothermal vents.
The waters probed during this study, known as the California
Current, are a hot spot of
ocean acidification because of coastal upwelling, which brings naturally acidic waters to the surface, where they are
made even more acidic by greenhouse gas pollution.
More than 13 years in the
making, the center is designed to be the U.S. government's nerve center for a range of activities, including predicting hurricane tracks and forecasting
ocean currents.
That may mean
making politically unpalatable choices like retreat from
current ocean shorelines, an effort actually under way in New York via buyouts of some coastal residents.
The thickness of the remaining, multi-year ice, along with its geographic location, will
make it more difficult to melt than the ice that was spread across the Arctic, and exposed to Pacific and Atlantic
ocean currents, along with runoff from fresh water rivers.
There are some farming techniques that may
make be viable options in the future, especially for those on a budget, but
current methods have a drastic impact on native seafood species and on the
ocean ecosystem.
According to Doug Armstrong,
Ocean Beach Patrol Supervisor,
Ocean Beach's exposure to multiple swell directions coupled with its proximity to the tidal exchange at the mouth of the Golden Gate Strait
make it subject to a tremendous amount of rip
currents — and the rip
currents change every day.
Mexico Rocks & Tres Cocos is protected from
ocean swells and
currents, so it
makes for easier snorkeling, perfect for beginners.
Balinese Hindu purification ceremonies are held beside the
ocean at the sacred Pura Segara sea temple, and the glistening black sandy stretch of coastline is popular with surfers and beachcombers, but swirling
currents and a lack of lifeguards
make it unsuitable for swimming.
The islands of Komodo and Rinca act as a bottleneck between the Indian and Pacific
Ocean,
making the Komodo National Park sea a rollercoaster of
currents and waves.
The strong winds and
currents where the two
oceans meet around Cape Horn
make these seas tempestuous and extremely unpredictable, hence the hundreds of shipwrecks to its name.
This area is protected from
ocean swells and
currents, so it
makes for easier snorkeling.
The
currents and choppy conditions as well as the open
ocean nature of Socorro islands
make it an ideal dive destination for large pelagics not only for mantas but also for Humpback whales.
Also, this area is protected from
ocean swells and
currents, so it
makes for easier snorkeling.
Strong
ocean currents continually mix and lift food and nutrients from the deep
ocean canyons,
making this the perfect feeding ground for all types of marine mammals.
A picture - perfect tropical paradise, Tortuga Island's clear turquoise waters teem with tropical fish and very little
ocean current, which
makes it ideal for swimming, snorkeling and scuba diving.
Entitled Littoral Drift, a geologic term describing the action of wind - driven waves transporting sand and gravel, her
current series consists of camera-less cyanotypes
made in collaboration with the landscape and the
ocean, at the edges of both.
2015
Current Location, Waiting Room, Minneapolis 10th Baltic Biennial of Contemporary Art, Szczecin Aquí hay dragones (Here be Dragons), La Casa Encendida, Madrid Regular Expressions, 221A, Vancouver
Ocean of Images: New Photography 2015, at MoMA, New York Bunting, Chemould Prescott Road, Mumbay Transparencies, Bielefelder Kunstverein and Kunstverein Nürnberg Triple Canopy presents Pattern Masters, Performance at Whitney Museum of American Art, New York HPSCHD 1969 > 2015 / Live Arts Week IV, Mambo, Bologna, Italy The Secret Life, Murray Guy, New York Night Begins the Day: Rethinking Space, Time, and Beauty, Contemporary Jewish Museum, San Francisco Im Inneren der Stadt, Künstlerhaus Bremen When we share more than ever, MKG Museum, Hamburg Cool / As a state of mind, MAMO, Marseille Group presentation at Art Cologne, with Chert, Berlin Good luck with your natural, combined, attractive and truthful attempts in two exhibitions, Crac Alsace, Altkirsch Mijn Vlakke Land, FoMu, Antwerp more Konzeption, Conception now, Museum Morsbroich, Leverkusen Tongue Stones, Pioneer Works, Brooklyn, New York 2014 Requiem for the Bibliophile, Museum of Contemporary Art Santa Barbara, CA Scars of Our Revolution, Yvon Lambert, Paris Kochi - Muziris Biennal, Fort Kochi, India Crossing Brooklyn, Brooklyn Museum, Brooklyn, New York Ways of Working, According to an Office Desk, Upominki, Rotterdam AGITATIONISM, EVA International 2014, curated by Bassam El Baroni, Ireland's Biennial, Limerick City Unseen Presence, IMMA, Dublin #nostalgia, Glasgow International 2014, CCA, Glasgow To Meggy Weiss Lo Surdo, Happy Hours, CO2 gallery, Turin Canceled: Alternative Manifestations & Productive Failures, The Orseman Gallery, Smith College, Northampton, Massachusetts Simultáneo, La Tallera, Cuernavaca, México And I laid Traps for the Troubadours who get killed before they reached Bombay, Clark House Initiative, Bombay Flag Stavanger, curated by Randi Grov Berger and co-presented by Entrée, Kunsthall Stavanger, Norway video screening 25, ZERO, Milan 2013 Only to Melt, Trustingly, Without Reproach, curated by Tevz Logar, Skuc Gallery, Ljubljana Editionshow, Chert, Berlin I've Lost My Marbles, Totàl, Athens And So On And So Forth, curated by Margit Sade Lehni, Centre for Contemporary Art Riga, Latvia The Space Between Us, Courtesy, St - Ouen Please Come to the Show: Part II (1980 — Now), organised by David Senior, MoMA Library, New York Canceled: Alternative Manifestations & Productive Failures, Freedman Gallery, Albright College, Reading, PA Stranded Travelers, Atelier 35, Bucharest Just what is it that
makes today so familiar, so uneasy?
The
currents flowing across the sill bring warm Atlantic water into the polar sea, and although the net gain each year is tiny, over thousands of years it is enough to
make the Arctic
Ocean very much warmer.
Water from the melting ice
makes the
oceans rise, only a fraction of an inch a year but, in the fullness of time, enough to let the
currents increase their flow over the northern sill, bringing ever more warm water into the gelid Arctic.
Now, this will
make many readers mad, but does a warming world with
ocean currents, acidification changes have anything to do with this?
«As [Lindzen's] colleagues at MIT in the Program in Atmospheres,
Oceans and Climate, all of whom are actively involved in understanding climate, we write to
make it clear that this is not a view shared by us, or by the overwhelming majority of other scientists who have devoted their professional lives to careful study of climate science,» said the letter, signed by
current and retired MIT professors.
Extension of the
current synoptic capacity of 6 - 7 days to 14 days would be a great start, but the lack of sufficient weather in the
oceans would
make this difficult to achieve for vulnerable coastal communities.
19 Deep Water
Currents Make up about 90 % of
oceans» water Differences in density cause them to move.
11 Surface
Currents Make up 10 % of oceans» water Up to maximum depth of 400 m Surface ocean currents are caused by the surface wind p
Currents Make up 10 % of
oceans» water Up to maximum depth of 400 m Surface
ocean currents are caused by the surface wind p
currents are caused by the surface wind patterns.
Indeed it's just the variance either side of the attractor, but Earth's
current geometry (land -
ocean distribution) encrypts the simplicity,
making it unrecognizable to most.
For examples deep
ocean currents and clouds are not well modelled by any of the IPCC models, all of which employ fudge factors to
make the models fit.
Previous large natural oscillations are important to examine: however, 1) our data isn't as good with regards to external forcings or to historical temperatures,
making attribution more difficult, 2) to the extent that we have solar and volcanic data, and paleoclimate temperature records, they are indeed fairly consistent with each other within their respective uncertainties, and 3) most mechanisms of internal variability would have different fingerprints: eg, shifting of warmth from the
oceans to the atmosphere (but we see warming in both), or simultaneous warming of the troposphere and stratosphere, or shifts in global temperature associated with major
ocean current shifts which for the most part haven't been seen.
Rising surface temperatures in the last three decades of the 20th century were roughly half caused by man -
made global warming and half by the
ocean currents keeping more heat near the surface, it finds.
Based on
current rates of
ocean acidification, scientists predict
oceans will be much quieter in the future —
making it more difficult for baby fish, who rely on auditory cues as a primary method of navigation, to find their way home.
The swirling
makes it difficult for oxygen to be exchanged between the rotating
current and the surrounding
ocean, researchers said.
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
The paper being discussed here
makes the claim that the
current hiatus in warming is due to the heat going into the Atlantic
ocean as the Atlantic
ocean is currently in the 30 year cooling phase of it's ~ 60 year warming / cooling cycle.
Even if the temperature e.g. at the poles, the sink places, dropped 1 °C more than average, that doesn't
make much difference: the
current CO2 level at about 400 ppmv gives about the same partial pressure of 400 microatm everywhere over the
oceans (minus a few % due to water vapour).
Until climatologists can properly
make models that reflect the entire global history and take into account plate position and how high the plates ride, oceanic levels due to this and the position of
oceans, overall insolation, overall daylength and its effects on average global temperature and factor in known carbon dioxide levels over that time period, then they will be unable to give any correlation between
current carbon dioxide levels and global temperature.
http://illconsidered.blogspot.com/2006/04/historically-co2-never-causes.html 100 years of shift does not factor into the larger scale phenomena http://illconsidered.blogspot.com/2006/01/one-hundred-years-is-not-enough.html Until climatologists can properly
make models that reflect the entire global history and take into account plate position and how high the plates ride, oceanic levels due to this and the position of
oceans, overall insolation, overall daylength and its effects on average global temperature and factor in known carbon dioxide levels over that time period, then they will be unable to give any correlation between
current carbon dioxide levels and global temperature.
The only way we could get runaway warming would be to
make the
ocean currents as close to frictionless as we could.
I think it is time for a general update due to subsequent developments (especially the
current 2 year global cooling trend and a quieter sun with cooling
oceans after an 8 year temperature plateau which tends to show that my point about solar and oceanic influences on global temperatures has some merit) and the fact that I can
make the essential points more simply by condensing them into a series of bullet points as follows:
Further, account must be
made of non-eustatic dynamic changes in sea level due to tides, storm surges, tsunamis and large - scale
ocean currents.
For
current ocean composition, CO2 that is added to sea water is partitioned primarily into HCO3 with the net reaction resulting in the generation of H + and thus decreasing pH and
making sea water more acidic; adding CO2 thereby decreases the concentration of CO..