Sentences with phrase «ocean basins for»

Then you can explain how a regional SST change can cause OHC to rise simultaneously in all major ocean basins for four decades (and counting).

Figure 7u - 12 describes the number of category 1 to 5 hurricanes that developed in the North Atlantic, northeast Pacific, and northwest Pacific Ocean basins for the period 1951 to 2002.

Not exact matches

Álvaro Corral of the Centre for Mathematical Research in Barcelona, Spain, and colleagues looked at records of hurricanes from four ocean basins around the world between 1966 and 2007.

They are derived from the idea that if the ice buttress for one of these big basins in East Antarctica were to go, you might get lots of ice sliding into the ocean very quickly, then sea level stabilizing after that most unbalanced ice is released.

«We need to do more studies to be able to determine if this new species, which we are yet to name, only lives in the shallow waters of the western Mediterranean or if it is also found in other deep water basins in the eastern Mediterranean or Atlantic Ocean, for example,» highlights Conxita Àvila.

The study shows that changes in heat distribution between the ocean basins is important for understanding future climate change.

Using supercomputers, the researchers found that this dense piece of ocean floor material (called a lithospheric slab) is slowly sinking into the Earth's mantle and is responsible for the formation of the Lake Eyre Basin, one of the Earth's largest internally drained basins and home to the lowest point in Australia at 15m below sea level, as well as the Murray - Darling Basin, home to the largest river system in Australia.

For scientific purposes, the Antarctic ice sheet is often divided into catchment basins so that comparative measurements can be taken to work out how the ice in each basin is changing and discharging ice to the oceans.

Newly developing ocean basins, formed by plate tectonics and continental rifting, provide just the right conditions for rapid burial in anoxic waters.

For much of the global ocean the coarser resolution is okay, but when you are studying a unique location like the Gulf of Maine, with its complex bathymetry of deep basins, channels, and shallow banks combined with its location near the intersection of two major ocean current systems, the output from the coarser models can be misleading.»

They found that across ocean basins, the ratio of human - generated mercury to human - generated CO2 tends to stay consistent among waters in the same layer of depth, because coal burning, for example, emits both mercury and CO2.

According to the researchers, to better understand if Matthew's intensification was aided by the warm - water eddies and the residing barrier layer in the Caribbean Sea's upper ocean, more ambient and in - storm upper ocean observations in this basin are needed to improve forecast models for the region.

The researchers found that organisms from each ocean basin had its own unique threshold for the level and type of stressor it could tolerate.

And the Reef Life Survey, begun in Tasmania by Stuart - Smith and marine ecologist Graham Edgar in 2007, has trait records for more than 5,000 species from all ocean basins.

«The Afar region provides a unique study area for continental breakup and formation of new ocean basins.»

The mountain ranges overlooking the Los Angeles basin that cradles the city, and the Pacific Ocean beyond, have served as the settings for cinematic fantasies ranging from Westerns to the classic detective stories of Raymond Chandler.

«Whereas the Pacific was previously considered the main driver of tropical climate variability and the Atlantic and Indian Ocean its slaves, our results document a much more active role for the Atlantic Ocean in determining conditions in the other two ocean baOcean its slaves, our results document a much more active role for the Atlantic Ocean in determining conditions in the other two ocean baOcean in determining conditions in the other two ocean baocean basins.

Prior to Sept. 1, Kilo was one of a trio of Category 4 hurricanes in the northeastern Pacific — a record clustering for any ocean basin.

El Niño is most widely known for how it shifts the location of warm ocean waters, leading to cooler - than - normal waters in the western tropical Pacific but warmer - than - normal in the central and eastern parts of the basin.

This current therefore is a major region for mixing water between different ocean basins.

Hovine, S., and T. Fichefet, 1994: A zonally averaged, three - basin ocean circulation model for climate studies.

The end of November means that both the Atlantic and East Pacific hurricane seasons have drawn to a close, and storm activity in the two ocean basins was quite different, indeed, but for the same reason.

Dr. Kevin Trenberth and his team have made a unique contribution through the investigation of climate variability and trends in the past, and through the use of models and other creative efforts to reconstruct river discharge into the oceans across the planet for almost 1000 river basins.

«The excrements of 80 billion land animals raised for food each year aren't» treated and go in to water basins and oceans».

It also said, for example, it missed both polar regions badly, had a 10 degree standard deviation over much of the land mass, missed significant portions of the eastern ocean basins, etc..

As for petroleum, while increased scarcity and demand will spur people to drive less, in smaller cars, it will also guarantee the expansion of drilling farther toward the ends of the Earth and deeper in ocean basins.

Even if the model agreed well with respect to saline anomalies in the inflow region, it has not yet been established whether it provides representative values for the absolute salinity in the entire ocean basin.

Can we consider the ocean basin volume as static for the purpose of sea level change prediction because the speed of water inputs will far outstrip the speed of mantle movements?

The massive water system is thought to stretch for 3,700 miles across the Amazon basin with an average width of about 200 miles, flowing west to east into the Atlantic Ocean at a rate of 350 feet a year.

The best example I know tis the ~ 3.75 year Rossby / Kelvin wave in the North Pacific, for which that ocean basin is resonant at that period.

Sea level change based on satellite altimetry is measured with respect to the Earth's centre of mass, and thus is not distorted by land motions, except for a small component due to large - scale deformation of ocean basins from GIA.

Looking at each ocean basin, and the global data, the long - term variations for the three depths in each basin are basically the same, as are the variations in the global data for the three depths.

The reason for a lack of short term correlation is probably that, absent a volcanic eruption, the Atlantic is warmer during an El Nino BUT the wind shear is greater, thus destroying, on such occasions, the agreement you would normally get with multidecadal changes in SST in the Atlantic RELATIVE to other ocean basins.

There is evidence for human influence in some individual ocean basins.

Exactly what I have been saying for years in that the net effect of the various ocean oscillations in each basin (your «stadium wave») modulates the solar effects sometimes supplementing and sometimes offsetting them.

The US CLIVAR Eastern Tropical Oceans Synthesis (ETOS) Working Group was formed to promote collaboration in the southeast oceanic basins, coordinate a model assessment of surface flux errors for the equatorial Atlantic, identify recent model improvements and common and persistent model errors, and provide recommendations of cases for community simulation and evaluation using eddy - permitting ocean models.

SLR satellite data includes things such as the «GIA Adjustment» — which is the amount of SLR that there would have been if the ocean basin hadn't increased in volume and in the case of this new study, how much higher the sea surface would have been if it had not been suppressed by the Mount Pinatubo volcanic eruption, another correction for ENSO / PDO «computed via a joint cyclostationary empirical orthogonal function (CSEOF) analysis of altimeter GMSL, GRACE land water storage, and Argo - based thermosteric sea level from 2005 to present», as well as other additions and adjustments — NONE OF WHICH can actually be found manifested in any change to the physical Sea Surface Height.»

Figure 5.3 shows the linear trends (1955 to 2003) of zonally averaged temperature anomalies (0 to 1,500 m) for the World Ocean and individual basins based on yearly anomaly fields (Levitus et al., 2005a).

As for the variation in heat content gain in each basin; this is no great surprise, as there is an exchange of water masses between the ocean basins.

«We conclude that, if projections for an increasing frequency of extreme El Niño and La Niña events over the twenty - first century are confirmed, then populated regions on opposite sides of the Pacific Ocean basin could be alternately exposed to extreme coastal erosion and flooding, independent of sea - level rise,» the authors write.

Figure 1 - Ocean heating rates for the global ocean and individual ocean basins down to 1500 meOcean heating rates for the global ocean and individual ocean basins down to 1500 meocean and individual ocean basins down to 1500 meocean basins down to 1500 metres.

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.

One of the rationales given by Chen & Tung for dismissing the role of the IPO in deep ocean warming is the expectation that the Pacific Ocean basin should have warmed more during the current (2000 - to present) IPO negative pocean warming is the expectation that the Pacific Ocean basin should have warmed more during the current (2000 - to present) IPO negative pOcean basin should have warmed more during the current (2000 - to present) IPO negative phase.

Figure 7u - 11 describes the month frequency of storm formation in the three ocean basins found in the Northern Hemisphere for the period 1951 to 2002.

Of these three regions, the northwest Pacific Ocean basin produced the most hurricanes for this period, an average of 17.7 storms per year (Figure 8.36).

How a single overturning cirulation could be responsible for approximately simultaneous OHC increase 0 — 2000m in all major ocean basins is a mystery to me — and to oceanographers too.

That warm water, of course, served as the fuel for the 1997/98 El Niño and was then redistributed to adjoining ocean basins in the years that followed, initially during the 1998/99/00 / 01 La Nina.

Other simple methods for controlling sea level are almost as simple, using heavy equipment to move shoreline dirt inland, thus increasing the total volume of the ocean basin.

During epochs when El Niño events dominate, the SST anomalies of the North Atlantic rise more than the SST anomalies of the other ocean basins, and when La Niña events dominate, the North Atlantic SST anomalies drop more than the SST anomalies for the rest of the globe.

The depth vs. age signal dom - inates the topography of the ocean basins and provides a firm foundation for plate tectonic theory (Parsons and Sclater, 1977).