Sentences with phrase «need high ocean»

Not exact matches

Therefore, we don't need water high enough to cover Mount Everest, we just need some geological plate shifting so that mountains rise up and ocean floors drop.

A newly discovered reservoir of rare earths, which are needed for high - tech, automotive and renewable energy applications, may remain on the ocean floor for some time

«Any life emerging during the Hadean eon likely needed to be resistant to high temperatures, and could have survived such a violent period in Earth's history by thriving in niches deep underground or in the ocean's crust.»

«New international standards needed to manage ocean noise: Growing use of high - decibel seismic surveys to explore the ocean for resources poses increased risks to vulnerable marine life, experts say.»

Its Decadal Survey of Ocean Sciences, scheduled to be released in early 2015, is supposed to identify both high - priority research projects and the infrastructure needed to conduct them.

So the 10th grade honors student at Ocean City High School in New Jersey did what she normally does when she needs help with an assignment and doesn't have time to consult with teachers or classmates: She logged on to the Internet and linked to an online tutor.

Ocean rowers, like high altitude mountaineers, need to consume between 4,000 and 5,000 calories a day to avoid losing muscle mass.

But since intelligence can not be drawn from the void, subterfuge are resorted to, one of the most prevalent being the mania for «demystification», which allows an air of intelligence to be conveyed at small cost, for all one need do is assert that the normal response to a particular phenomenon is «prejudiced» and that it is high time it was cleared of the «legends» surrounding it; if the ocean could be made out to be a pond or the Himalayas a hill, it would be done.

With easy access to Ocean City, Washington, DC, and anywhere else you need to go, and high incomes with affordable housing prices, Columbia is a great place to make your home.

Coho fry remain in the creek for their first year, where they depend on slow - moving water, high oxygen levels in the water with adequate stream cover and abundant shelter to survive and develop the strength they will need for their migration into the ocean.

Perched high on a hilltop in the south of Bali, with breathtaking 200 degree views of the beautiful countryside and spectacular Indian Ocean, Villa Bayu offers a complete getaway experience for those in need of a real holiday...

The high - end kitchen and alfresco grill will meet your culinary needs, and the dining table for eight inspires memorable meals illuminated by large, ocean - view windows.

The two bedroom high ocean view apartments offer absolute luxury accommodation option on the Gold Coast with everything you need and more, including access to the exclusive rooftop terrace, resort swimming pool, gymnasium and guest lounge on level 27.

Atmos Sala Alcalá 31, Madrid (catalogue) Hemispheres and Continents Matthew Marks Gallery, New York 2012 All Things Pass Galerie Max Hetzler, Berlin (catalogue) Patricia Low Contemporary, Gstaad Fullmoon and Night + Fog Domaine de Chaumont - sur - Loire, Chaumont - sur - Loire 2011 Landscape with Path The High Line, New York Xippas, Montevideo L'Abbaye de la Chaise Dieu, Chaise Dieu Nocturne Villa Merkel, Esslingen (catalogue)... between here and the surface of the moon FRAC Auvergne, Clermont Ferrand; traveled to: FRAC Haute - Normandie, Sotteville - lès - Rouen 2010 As it is Alfonso Artiaco, Naples The Principle of Moments Whitecube, London Fullmoon@Eifel Weidingen, Eifel Matthew Marks Gallery, New York PKM Trinity Gallery, Seoul 2009 Sommer Gallery, Tel Aviv Xippas Gallery, Athens Sometimestill Galerie Max Hetzler, Berlin 2008 Nail to Nail David Patton, Los Angeles SCAI The Bathhouse, Tokyo In The Between Eye of Gyre, Omotesando Substitute Galleri K, Oslo Fire under snow Parasol unit, London (catalogue) Moons of the Iapetus Ocean White Cube, London (catalogue) 2007 Galleria Alfonso Artiaco, Naples Day Return Castle Ujazdowski — Center for Contemporary Art, Warsaw (catalogue) Night + Fog Galerie Max Hetzler, Berlin (catalogue) In the Between Musée d'art contemporain, Montreal SITE Santa Fe, Santa Fe Matthew Marks Gallery, New York 2006 Day Return Museum Folkwang, Essen (catalogue) Darren Almond and Janice Kerbel: Impossible Landscapes The Horticultural Society of New York, New York If I had you Domus Artium 2002 — Center for Contemporary Art, Salamanca Darren Almond / Albert Oehlen: Time 2 Kill Galerie Max Hetzler, Berlin 2005 Take Me Home Matthew Marks Gallery, New York Alfonso Artiaco, Naples Isolation K21 - Kunstsammmlung Nordrhein - Westfalen, Düsseldorf Only Sound Needs Echo and Dreads its Lack Galerie Chantal Crousel, Paris 2004 Live Sentence Lentos Kunstmuseum Linz, Linz (catalogue) If I Had You Galerie Max Hetzler, St. Johannes Evangelist Church, Berlin 2003 11 miles... from Safety White Cube, London (catalogue) If I Had You Fondazione Nicola Trussardi, Palazzo della Ragione, Milan Mine, A Galleri K, Oslo A Galerie Max Hetzler, Berlin Full Moon Sommer Contemporary Art, Tel - Aviv 2002 A National Theatre, London; Yorkshire Sculpture Park, commissioned by Public Art Development Trust, London at speed (with Sarah Morris) Galerie Max Hetzler, Berlin 2001 Coming up for air Matthew Marks Gallery, New York Kunsthalle Zürich, Zurich (catalogue) Night as Day Tate Britain, London (catalogue) De Appel Foundation - Center for Contemporary Art, Amsterdam Galerie Max Hetzler, E-Werk, Abspannwerk Buchhändlerhof, Berlin 2000 Mean Time Matthew Marks Gallery, New York Geisterbahn The Approach, London Traction Chisenhale Gallery, London 1999 Galerie Max Hetzler, Berlin The Renaissance Society, University of Chicago, Chicago 1997 ICA - Institute of Contemporary Arts, comissioned by Toshiba Art & Innovation, London Fan White Cube, London 1995 KN120 Great Western Studios, London 1991 Crawford Art College, Cork

Given the number of ways that things can go wrong with continued CO2 emissions (from ocean acidfication and sea level rise to simple warming, shifting precipitation patterns, release of buried carbon in perma - frost, and the possibility of higher climate sensitivities — which seem to be needed to account for glacial / inter-glacial transitions), crossing our fingers and carrying on with BAU seems nothing short of crazy to me.

Our mainstream press needs to make addressing AGW, not to mention the ocean acid catastrophe, a high priority — it's place on the public priority list will mirror it's place in the media consciousness.

and «Where was all the water going to come from» so I decided to have a go and try to work out how much water would be needed to allow the World Ocean to rise by just 1 meter, there are two variables that I can not solve, 1 is that the world is curved so as you go up then you need more water for the next meter than you needed for the preceding meter and this is an exponential issue as it gets worse the higher you go, the other is that even though there are many areas where you could get a large rise without any inland flooding, like the «White Cliffs of Dover» then there are also many areas where there would be massive inland flooding, like Holland, so I had to make two assumptions to kill off two variable issues that I can not solve, so assuming that the world is flat, which it's not, and that there would be no inland flooding, and there will be massive inland flooding then using them then I got an answer.

You just need to add that more zonal jets when the sun is active widen the subtropical high pressure cells and allow more energy into the oceans to skew Enso in favour of El Nino over and above the basic 60 year periodicity so as to get the observed millennial climate cycling.and the temperature stepping from one PDO positive or negative phase to the next.

Both Washington state and the entire country need strong champions on both sides of the aisle who can elevate ocean issues at the highest levels of government and help break the Congressional logjam,» said David Wilmot, Ph.D., Co-Founder and President of Ocean Champocean issues at the highest levels of government and help break the Congressional logjam,» said David Wilmot, Ph.D., Co-Founder and President of Ocean ChampOcean Champions.

For falsification we would need to observe events such as the mid latitude jets moving poleward during a cooling oceanic phase and a period of quiet sun or the ITCZ moving northward whilst the two jets moved equatorward or the stratosphere, troposphere and upper atmosphere all warming or cooling in tandem or perhaps an unusually negative Arctic Oscillation throughout a period of high solar activity and a warming ocean phase.

Self similarity in the temperature record (due to internal dynamics) coupled with ocean outgassing fully explains the geological data without any need to invoke high sensitivities to CO2 or any arm - waving about feedbacks.

One does not need an enormous ice sheet for sea level to be high, chiefly because the Earth's coastal zones and ocean basins may be more porous and capacious than one would imagine.

A boundary layer with a higher temperature requires the deeper ocean to have a higher temperature for it to sustain the same flux (deltaT) through the boundary layer to the atmosphere (the deeper ocean (< 1 mm) still needs to loose the solar energy or it would start boiling eventually).

«But the other thing I want to point out,» England added, «is that greenhouse gases in the atmosphere are at such high concentrations compared to what they were 100 years ago that you don't need to bring heat back up from the ocean to the surface to get future warming — you just need to slow down the heat uptake by the ocean, and greenhouse gases will do the rest.»

«Drilling in high - risk places like the freezing waters of the Arctic Ocean is a backwards - looking strategy when we need to look forward to meet energy needs and limit the effects of climate change.»

Open water in the Arctic Ocean during the winter allows heat to flow from the ocean to the atmosphere, creating the high pressure needed for a negative NAO to materiaOcean during the winter allows heat to flow from the ocean to the atmosphere, creating the high pressure needed for a negative NAO to materiaocean to the atmosphere, creating the high pressure needed for a negative NAO to materialize.

The research needs that have high priority in establishing the technical, environmental, and economic feasibility of large - scale capture and disposal of CO -LCB- sub 2 -RCB- from electric power plants are: (1) survey and assess the capacity, cost, and location of potential depleted gas and oil wells that are suitable CO -LCB- sub 2 -RCB- repositories (with the cooperation of the oil and gas industry); (2) conduct research on the feasibility of ocean disposal, with objectives of determining the cost, residence time, and environmental effects for different methods of CO -LCB- sub 2 -RCB- injection; (3) perform an in - depth survey of knowledge concerning the feasibility of using deep, confined aquifers for disposal and, if feasible, identify potential disposal locations (with the cooperation of the oil and gas industry); (4) evaluate, on a common basis, more» system and design alternatives for integration of CO -LCB- sub 2 -RCB- capture systems with emerging and advanced technologies for power generation; and prepare a conceptual design, an analysis of barrier issues, and a preliminary cost estimate for pipeline networks necessary to transport a significant portion of the CO -LCB- sub 2 -RCB- to potentially feasible disposal locations.

If we are to get a real idea of the rate of tropical convection that drives Hadley cell dynamics and the size of the subtropical high pressure cells we need to measure the rate of evaporation from the tropical ocean.

The oceans may or may not have been a net carbon sink but the extent to which they acted as a net carbon sink would have been reduced by the higher surface temperatures and that to me suggests that they must have contributed to higher CO2 in the air and since the oceans are magnitudes more important than human emissions in the natural carbon cycle that is where we need to look to explain observed changes.

«For example, to produce a six - foot flood, if the ocean is a foot higher, you only need as much storm surge as you would have previously needed to produce a five - foot flood,» said Robert Kopp, professor of earth and planetary science at Rutgers university, and one of the authors.

To know what these high numbers mean for local changes on the world's coastlines, you need a framework that accounts for all the key drivers: among them not just Antarctica, but also Greenland, mountain glaciers, the expansion of the warming ocean, changes in winds and current, shifts in Earth's gravitational field, and land motion.

For true falsification we would need to observe events such as the mid latitude jets moving poleward during a cooling oceanic phase and a period of quiet sun or the ITCZ moving northward whilst the two jets moved equatorward or the stratosphere, troposphere and upper atmosphere all warming or cooling in tandem or perhaps an unusually powerful Arctic Oscillation throughout a period of high solar turbulence and a warming ocean phase.

In case you need reminding, these higher than normal ocean temperatures fit solidly into the broader global trend towards warmer temperatures — though regionally they are much greater than the global average (as the chart at top shows, with the red areas being up to 5 °C above normal).

Coastal protection needs to account for higher storm surges, affected by storm strength, storm size and uneven SLR distribution and re-configuring of ocean flow.

I think there are several AGW factors & other natural factors that go into higher Mexican Gulf SST, and we need to consider all of them — more shallow waters being heated more, & more rapidly than deep seas; the slowing of the thermo - haline ocean conveyor from fresh water pouring into the North Atlantic, leaving hot waters more stuck in place in the south.

It was an incredibly humbling experience to watch the ocean's highest predator show exactly why it earned that moniker, and convincingly demonstrate why I needed to keep my hands close to my body.