Sentences with phrase «north sea currents»

Cold, active, north sea currents, three metre tides and other marine and climatic conditions, offer the advantage of a unique mix of minerals.

Not exact matches

Pursuing the current rout in world - wide crude prices, the market is praying George Osborned provides some tax breaks this week & #thirteen & #thirteen & # 13 & #thirteen & # 13 Image: Alamy & # 13 & # 13 The scenario has turn out to be so determined for some North Sea drilling operators that even the number of...

At the risk of pursuing your completely silly semantic tangent, but since I'm perfectly happy for people to say «Derry» or «Londonderry» as they prefer, and while I merrily concede that I doubt anyone will ever persuade me to call the «North Sea» the «German Sea», if you wish to replace my «mainland» with your «Great Britain», then go for it, but since only «Great Britain» was party to the Treaty of Versailles, might I then ask how you propose to continue to engage Mainland Shetland, Hoy, Anglesey etc. separately in the current war with Germany?

This cycle coincides with the natural rise and fall of sea surface temperatures in the North Atlantic, which fluctuate roughly 0.2 degree Celsius every 60 years as warm currents shift.

To that end, the United Kingdom in December signed a memorandum of understanding with nine other northern European states — Germany, France, Belgium, Denmark, the Netherlands, Ireland, Luxembourg and Norway — to study the possibility of building a $ 30 billion ($ 41.4 billion) grid in the North Sea that could be producing 100 GW of electricity within 20 years if all current plans come to fruition.

The U.K. - based oil company, BP, PLC, has signed a $ 17 - billion exploration deal with Russia in the hopes of replacing the declining output of its current fields in the North Sea.

«Examining surface currents suggests that the North Queensland Coastal Current in the Coral Sea, which would normally flush and cool the Northern Great Barrier Reef, actually did the opposite.

Examining the CyroSat - 2 sea ice thickness map for this spring, Stefan Hendricks further explained: «The Transpolar Drift Stream, a well - known current in the Arctic Ocean, will be carrying the majority of the thick, perennial ice currently located off the northern coasts of Greenland and Canada through the Fram Strait to the North Atlantic.

The melting and retreating of Arctic sea ice in the summer months also has allowed PWW to move further north than in the past when currents pushed it westward toward the Canadian archipelago.

The team, which includes Professor Baldwin, will lead innovative new research, which aims to advance current understanding of three key conditions that influence seasonal weather across the continent — the North Atlantic upper - ocean heat content, Arctic sea - ice, and the stratosphere.

Each year a million cubic metres of sediment has been dragged by the currents southwards down the coast or out into the North Sea.

The upper part of the modern Arctic Ocean is flushed by North Atlantic currents while the Arctic's deep basins are flushed by salty currents formed during sea ice formation at the surface.

«Summary of ocean current slowdowns, rapid sea level rise of east coast of North America, wavy jet streams and extreme weather events, Arctic and Antarctica connections and declining carbon sink in Amazon rainforests.

In the current situation, where the north is heating and the south is not, if the sea level rises that means the global ice quantity is INCREASING.

Melting sea ice will mean ocean currents can carry warmer water and nutrients into Arctic water, taking fish further north and potentially allowing them to mix between oceans.

A Japanese boy has been injured after a window fell off a US military helicopter and landed on a school playground - the second such incident in a week China has been staging military drills in the sea bordering North Korea, reportedly in response to the current US - South Korean joint exercise.

Today, if just the current Ross Ice Shelf of Antarctica melted, it is estimated that sea level would rise 20 to 251 If we melted all of the ice on Greenland, the North polar areas and the Antarctic in addition, sea level could rise 300» or so.

Current occurrences of the critically endangered North Pacific right whales and historically abundant Steller's sea lions in these areas are unknown.

Current occurrences, if still happen, of the critically endangered North Pacific right whales, and historically abundant Steller's sea lions in these areas are unknown.

Location: north, northeast of Boracay Access: about 25 minutes by boat from White Beach Experience: advanced divers and technical divers Depth: up to 70 meters Visibility: 10 - 30 meters Current: strong Characteristics: 3 dive sites - Yapak I and Yapak II, two different reef walls begin at 30 meters and drop down to 70 meters at Yapak III, wide diversity of fish, tuna, barracuda, snapper, jacks, sharks, and manta rays have been seen, sea turtles, sea snakes, sponges, nudibranchs, corals

The mingling of cool, nutrient - rich waters from the north with warm currents from the south form a dynamic transition zone that is home to a myriad of sea life from microscopic plankton to blue whales.

North coast sites have minimal currents and calm seas, especially in summer months, and may be done as drifts or from a moored boat.

In October 2016, the floating 8 million kilos concrete structure was transported by a submersible barge over the North Sea Canal, on the River Thames and through the King George V lock to its current location.

The most likely explanation is that the sand drifted north along the Queensland coast, carried by prevailing sea currents, millions of years ago.

Use the tab navigation above to view DuckPool sea temperature, DuckPool photographs, DuckPool detailed swell predictions, wind and weather forecasts, DuckPool webcams, current wind from Cornwall (North) live weather stations and DuckPool tide predictions.

Use the tab navigation above to view Towan sea temperature, Towan photographs, Towan detailed swell predictions, wind and weather forecasts, Towan webcams, current wind from Cornwall (North) live weather stations and Towan tide predictions.

Use the tab navigation above to view Bedruthan Steps sea temperature, Bedruthan Steps photographs, Bedruthan Steps detailed swell predictions, wind and weather forecasts, Bedruthan Steps webcams, current wind from Cornwall (North) live weather stations and Bedruthan Steps tide predictions.

CA Spectral Hues, curated by Sharon Bliss, Palo Alto Art Center, Palo Alto, CA Art Market, with Chandra Cerrito Contemporary, San Francisco, CA Building the Art House, curated by Katherine Connell and Emma Spertus, Rosenberg Library, City College of San Francisco, San Francisco, CA Big Idea, curated by Sue Collier, Leslie Ford, Jack McWhorter and JoAnn Rothschild, The Painting Center, New York, NY Along the Lines, Harrington Gallery, curated by Julie Finegan, Pleasanton, CA 2016 Plus +1, Trestle Contemporary Art Gallery, Brooklyn, NY Group show, November - December 2016, Galleri Urbane, Dallas, TX Palette, curated by Kelly Inouye, Theodora Mauro and Lisa Solomon, ampersand international arts, San Francisco, CA Small Works, Trestle Gallery, Brooklyn, NY Art Market, with Chandra Cerrito Contemporary, San Francisco, CA 2015 Therely Bare Redux, Zeitgeist Gallery, Nashville, TN Therely Bare Redux, Clara M Eagle Gallery, University of Tennessee, Murray Territory of Abstraction, Pentimenti Gallery, Philadelphia, PA Out of Storage, Studio 110 Projects, Sausalito, CA Art Market San Francisco, (with Chandra Cerrito Contemporary), San Francisco, CA The Airplane Show, B Sakata Garo, Sacramento, CA 2014 un.bound.ed, curated by Brent Hallard and Don Voisine, Root Division, San Francisco, CA (edition) DOPPLER SHIFT, curated by Mary Birmingham, Visual Arts Center, Summit, NJ (catalogue) The Intuitionists, curated by Heather Hart, Steffani Jemison & Jina Valentine, The Drawing Center, New York, NY (catalogue) First / Last, curated by Heather Phillips, Park Life, San Francisco, CA 2013 DOPPLER, Parallel Art Space, Brooklyn, NY (catalogue) Generations IX: The Red / Pink Show, A.I.R. Gallery, Brooklyn, NY Made In Paint: 2012 Artists in Residence, The Sam & Adele Golden Gallery, New Berlin, NY Rituals of Exhibition II, Light Space Project, H Gallery, Chiang Mai, Thailand Rituals of Exhibition, curated by Giles Ryder and Gilbert Hsiao, Don't Be Selfish, Phayao, Thailand POSTE CONCRET II, curated by Richard van der Aa, ParisCONCRET, Paris, FR 2012 Soft Luminosity, curated by Guido Winkler and Iemke van Dijk, IS Projects, Leiden, NL (edition) Art On Paper 2012, The Weatherspoon Museum of Art, Greensboro, NC (brochure) Islands of Order in a Sea of Chaos, curated by Ruth van Veenen, de Vishal, Haarlem, NL Doppler Stop, Amsterdams Grafisch Atelier, Amsterdam, NL (catalogue) Doppler Stop, Kunst & Complex, Rotterdam, NL Doppler Stop, Fluctuating Images / General Public, Berlin, DE Doppler Stop, trenutak.39 / Museum of Contemporary Art, Zagreb, HR Trade - O - Mat, curated by Kathryn Kenworth, Kala Art Institute, Berkeley, CA 2011 A Romance of Many Dimensions, curated by Brent Hallard, Brooklyn Artists Gym, Brooklyn, NY POSTE CONCRET I, curated by Richard van der Aa, ParisCONCRET, Paris, FR BYO, IS Projects, Leiden, NL Stop & Go Rides Again, touring exhibition curated by Sarah Klein, Z Space, San Francisco, US; Kunst & Complex, Rotterdam, NL; Fluctuating Images / General Public, Berlin, DE; Fluctuating Images / Interventionstraum, Stuttgart, DE An Exchange with Sol Lewitt, Massachussetts Museum of Contemporary Art, North Adams, MA (catalogue) ReTrace, Cesar Chavez Art Gallery, San Francisco State University, San Francisco, CA 2010 TOUCH, curated by Brent Hallard, ParisCONCRET, Paris, FR (catalogue) Factor XX, curated by Jenny Balisle, Los Gatos Museum, Los Gatos, CA (catalogue) The Rule of Typical Things, Gregory Lind Gallery, San Francisco, CA 2009 TRANS: form color, Meridian Gallery, San Francisco, CA (catalogue) TRANSformal, Pharmaka, Los Angeles, CA (brochure) The Grid, curated by JT Kirkland, MP5, Portland, OR 2008 Calculated Color, curated by Jane Lincoln, Higgins Art Gallery, Cape Cod, MA (brochure) The Space Between, curated by Cathy Kimbell, San Jose Institute of Contemporary Art, San Jose, CA (brochure) Close Calls, Headlands Center for the Arts, Sausalito, CA (also 2005, 2004) TOUCH, curated by Brent Hallard, Busdori, Tokyo, Japan Out of the Fog: Artists from Headlands Center for the Arts, curated by Dianne Romaine and Holly Blake, Art works Downtown, San Rafael, CA 2007 TRANS: Abstraktion, Weltraum, Munich, DE (brochure) 7 - 07 Hung Liu curates 7 Women Artists in the year of the Pig, b.Sakata Garo, Sacramento, CA (brochure) Bay Area Currents, The Oakland Art Gallery, Oakland, CA Visual Noise, UMC Gallery, University of Colorado, Boulder, CO The Unknown Quantity, Gregory Lind Gallery, San Francisco, CA Systems & Transmutations, Root Division, San Francisco, CA (catalogue) Still, Contemporary Quarterly, curated by Chandra Cerrito, www.ContemporaryQuarterly.com (brochure) 2006 Suitcase: Bus - Dori, curated by Brent Hallard, Tokyo, JP Summertime, Judy Saslow Gallery, Chicago, IL microcosm, curated by Victoria Wagner, Richmond Art Center, Richmond, CA (brochure) Sketch, The Memorial Union Gallery, University of California at Davis, Davis, CA 2005 Contemporary Perspectives, Museum of Contemporary Art, Santa Rosa, CA 2004 and now they aren't.

(Surely the presence or absence of glacial ice doesn't greatly affect the «piling up» of sea ice against the shore — or terminal ice shelf — by persistent wind and current out of the North?)

More ground turns from white reflective snow to black, heat absorbant dirt.The same effect occurs as sea ice is lost.The corals blanch, and, as I stated last year on this site, the shutdown of the north Atlantic current will occur, since the salinity level studies I spoke of last year, off Greenland, continue to show that the upwelling mechanisms driving the North Atlanic current are in severe jeapordy, because the change in salinity levels effects the driver of the current, the upwelling and downwelling of different salinity levels off Greennorth Atlantic current will occur, since the salinity level studies I spoke of last year, off Greenland, continue to show that the upwelling mechanisms driving the North Atlanic current are in severe jeapordy, because the change in salinity levels effects the driver of the current, the upwelling and downwelling of different salinity levels off GreenNorth Atlanic current are in severe jeapordy, because the change in salinity levels effects the driver of the current, the upwelling and downwelling of different salinity levels off Greenland.

The deep water masses formed in this way are then exported out of the area in deep currents that eventually make up «North Atlantic Deep Water» (which also contains contributions from the Labrador Sea and entrainment of other water masses).

Southern expansion into the North Atlantic and Bering Sea will encounter more heat exchange with the open ocean currents than the ice northward of Canada.

Because of the shifting currents beneath the North Pole, the sea ice there is only two to three meters thick.

Changes in SST distribution is what one gets from starting / stopping North Atlantic Current components in Labrador and Greenland Seas, capping with sea ice, etc. 4.

Drexel Environmental Science Graduate Student [ANDY REVKIN says: Some of the sea ice on the Arctic Ocean kind of circles in a gyre, like a slow turntable, and much of it is ejected perpetually past Greenland into the North Atlantic by winds and currents.

This is not necessarily a contradiction to the other data series, because the two sediment cores used are located in the area of the deep outflow of Labrador Sea Water — but this is only one of two deep currents that together make up the southward part of the overturning circulation of the Atlantic, and thus the heat transport to the north.

Britain has no choice given the current and increasing reliance on North Sea gas for electricity production.

«On the other hand, herring catches off the north coast of Iceland have greatly diminished in the last seven years, possibly because of changes in the sea currents connected with the present climatic fluctuation.

Most interesting is that the about monthly variations correlate with the lunar phases (peak on full moon) The Helsinki Background measurements 1935 The first background measurements in history; sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane measurements at the Scottish coast 370 ppmCO2 in winds from the sea; 355 ppm in air from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aversea; 355 ppm in air from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aversea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly avnorth (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aversea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly averSea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly avNorth Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aversea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly average

The AMO1 (compressed) time sequence is a bit perplexing, but it is to do with North Icelandic Jet current, major player in the Nordic Seas summer oceanic heat release into atmosphere.

In the North Sea, surface temperatures are projected to increase 3.6 - 6.3 ° F (2 - 3.5 ° C) by the end of the century, if our emissions continue to rise at current rates.14, 15 If we make significant efforts to reduce our emissions, the increase in North Sea temperatures could be limited to 2.7 - 3.6 ° F (1.5 - 2 ° C).14, 15

The explanation of the that «incongruous» sea ice decline is very simple: Arctic warming is not caused by an imaginary AGW but by warm Gulf Stream water carried into the Arctic Ocean by North Atlantic currents.

Some of the warm water would be subducted by Atlantic Meridional Overturning Circulation / Thermohaline Circulation, some would be carried by ocean currents into the Arctic Ocean where it would melt sea ice, and the remainder would be spun southward by the North Atlantic gyre toward the tropics so it could be warmed more by the effects of the slower - than - normal trade winds.

The Fram strait ice loss, storms, volcanoes (mostly Icelandic), GHG, North Atlantic climate cycles, current patterns etc. all affect sea ice

Here, we have shown that this warming was associated and presumably initiated by a major increase in the westerly to south - westerly wind north of Norway leading to enhanced atmospheric and ocean heat transport from the comparatively warm North Atlantic Current through the passage between northern Norway and Spitsbergen into the Barents Sea.&rnorth of Norway leading to enhanced atmospheric and ocean heat transport from the comparatively warm North Atlantic Current through the passage between northern Norway and Spitsbergen into the Barents Sea.&rNorth Atlantic Current through the passage between northern Norway and Spitsbergen into the Barents Sea.»

New work on regional projections and emergence of the anthropogenic signal suggests that the two commonly predicted features of future regional sea level change (the increasing tilt across the Antarctic Circumpolar Current and the dipole in the North Atlantic) are related to regional changes in wind stress and surface heat flux.

The geochemist Wallace Broecker, to whom we owe a number of the important ideas about abrupt climate change, speculates that there is a chain of causation starting with more far - northern winter sea ice and (because of the ice preventing the winds from stirring up waves and evaporation and salt excess) thereby fewer sinks for the Gulf Stream, which in turn diminishes the big conveyor loop of currents linking the North Atlantic to the Pacific.

214 My sketch of the Gulf Stream and the underlying return current (the North Atlantic Deep Water) is adapted from that of Stefan Rahmstorf, «Risk of sea - change in the Atlantic,» Nature 388:825 - 826 (28 August 1997).

Other factors, including greenhouse gases, also contributed to the warming and regional factors played a significant role in increasing temperatures in some regions, most notably changes in ocean currents which led to warmer - than - average sea temperatures in the North Atlantic.

This in turn is influenced by sea level pressure patterns in polar and subpolar regions — as more or less wind and currents are pushed north (Roemmich et al, 2007, Qiu, Bo et al 2006).