Sentences with phrase «indian ocean basins»

But the warming is apparently confined to the North Atlantic and Indian ocean basins.

In the most recent case, waters in the Atlantic, Pacific, and Indian ocean basins began rising in mid-2014 and bleaching started in 2015.

This, even though over the Indian Ocean basin Ramanathan's team found that sooty brown clouds enhance heating by half of CO2's claimed effect, not masking it by half as had previously been thought.

This trend of poleward migration is evident in all ocean basins, except the North Indian Ocean basin, in homogenized satellite and so - called «best track» data.

Molnar, P., F. Pardo - Casas, and J. Stock, The Cenozoic and late Cretaceous evolution of the Indian Ocean basin: Uncertainties in the reconstructed positions of the Indian, African, and Antarctic plates, Basin Res., 1, 23 - 40, 1988.

Having said that, similar changes in tropical cyclone detection also seem to have occurred for each of the other basins, e.g., Hoarau et al., 2012 (Abstract) suggest that incomplete satellite coverage during the 1980s and early 1990s led to an underestimation of cyclone intensity in the northern Indian Ocean basin.

I am looking at ARGO data for the Indian Ocean basin.

Not exact matches

While there are regional differences in the poleward movement of cyclones, the fact that every ocean basin other than the northern Indian Ocean has experienced this change leads the researchers to suggest, in the paper, that this «migration away from the tropics is a global phenomenon.&rocean basin other than the northern Indian Ocean has experienced this change leads the researchers to suggest, in the paper, that this «migration away from the tropics is a global phenomenon.&rOcean has experienced this change leads the researchers to suggest, in the paper, that this «migration away from the tropics is a global phenomenon.»

Along one string of sites, or «stations,» that stretches from Antarctica to the southern Indian Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean baOcean, researchers have tracked the conditions of AABW — a layer of profoundly cold water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean baocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean baOcean and northward into all three of the major ocean baocean basins.

The research team found that deoxygenation caused by climate change could already be detected in the southern Indian Ocean and parts of the eastern tropical Pacific and Atlantic basins.

«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.

Presently, much of the Atlantic Ocean is well oxygenated (Figure 1) relative to the North Indian and Pacific Oceans, where bottom water O2 concentrations are lower because of the biological removal of O2 as thermohaline circulation moves deep waters across ocean basins from the North and South Atlantic towards the North Pacific, in isolation from the surface oOcean is well oxygenated (Figure 1) relative to the North Indian and Pacific Oceans, where bottom water O2 concentrations are lower because of the biological removal of O2 as thermohaline circulation moves deep waters across ocean basins from the North and South Atlantic towards the North Pacific, in isolation from the surface oocean basins from the North and South Atlantic towards the North Pacific, in isolation from the surface oceanocean.

In other major ocean basins, parts of the western North Atlantic, the Barents Sea in the Arctic, and much of the Indian Ocean were record ocean basins, parts of the western North Atlantic, the Barents Sea in the Arctic, and much of the Indian Ocean were record Ocean were record warm.

We do know that ocean basins produce this oscillatory behavior — the El Nino / Southern Oscillation, the Arctic Oscillation, the Pacific Decadal Oscialltion, the NAO, the Madden - Julian Oscillation (Indian Ocean), but they seem to have a bit of a random component, their forcing mechanisms are poorly understood, their «phase changes» appear impossible to predict very far in advance, and they must also be sensitive to the overall climate warocean basins produce this oscillatory behavior — the El Nino / Southern Oscillation, the Arctic Oscillation, the Pacific Decadal Oscialltion, the NAO, the Madden - Julian Oscillation (Indian Ocean), but they seem to have a bit of a random component, their forcing mechanisms are poorly understood, their «phase changes» appear impossible to predict very far in advance, and they must also be sensitive to the overall climate warOcean), but they seem to have a bit of a random component, their forcing mechanisms are poorly understood, their «phase changes» appear impossible to predict very far in advance, and they must also be sensitive to the overall climate warming.

The resulting Common Water, also called Antarctic Circumpolar water, flows northward at depth into the three ocean basins (primarily the Pacific and Indian Oceans).

The role of the Indian Ocean, the stationarity of teleconnections, the determination of the leader ocean basin in driving decadal variability, the anthropogenic role, the reduction of the model rainfall spread, and the improvement of some model components are among the most important remaining questions that continue to be the focus of current international projOcean, the stationarity of teleconnections, the determination of the leader ocean basin in driving decadal variability, the anthropogenic role, the reduction of the model rainfall spread, and the improvement of some model components are among the most important remaining questions that continue to be the focus of current international projocean basin in driving decadal variability, the anthropogenic role, the reduction of the model rainfall spread, and the improvement of some model components are among the most important remaining questions that continue to be the focus of current international projects.

Since the East Indian and West Pacific Oceans are not isolated by landmass, ocean currents spread this cumulative warming into the adjoining ocean basins.

Uses the International Best Track Archive for Climate Stewardship (IBTrACS, version v03r03) analysis during satellite era (1986 — 2010) and determines the trends of intensification of tropical cyclones (TC) over all the global basins, except the North Indian Ocean

The only two ocean basins with major increases in OHC during the ARGO era are the South Atlantic and the Indian Oceans, while the North Atlantic, Arctic, and South Pacific Oceans show significant declines in OHC.

Previous studies have considered mechanisms for the basin - scale ocean warming, but not the causes of the observed IPWP expansion, where expansion in the Indian Ocean has far exceeded that in the Pacific Oocean warming, but not the causes of the observed IPWP expansion, where expansion in the Indian Ocean has far exceeded that in the Pacific OOcean has far exceeded that in the Pacific OceanOcean.

The researchers examined data on the number and power of hurricanes making landfall in the five main hurricane basins: North Atlantic, northeastern Pacific, western North Pacific, northern Indian Ocean, and Southern Hemisphere.

The current bleaching event has affected reefs throughout the tropics — including much of the Pacific and parts of the Indian Ocean, the Atlantic and the Caribbean basin — and is largely thanks to the onset of a particularly severe El Niño event in 2015, which has resulted in unusually warm water temperatures in many regions.

Abstract: Mean - sea - level data from coastal tide gauges in the north Indian Ocean wereare used to show that low - frequency variability is consistent among the stations in the basin.

They identified regional differences, but found that every ocean basin except the northern Indian Ocean had experienced such a chocean basin except the northern Indian Ocean had experienced such a chOcean had experienced such a change.

Yet, the two data sets merrily follow each other in the basins of best data (e.g., the North Atlantic) and even in the worst (perhaps the South Indian Ocean).

After in fact stating the rising trend in Hurricane frequency in the Indian ocean Hoarau asks at the end of the article if there is a connection between global warming and the growing number of tropical cyclones in various ocean basins.

The researchers used statistical models and techniques from a field of mathematics called information theory to determine factors contributing to hurricane strength from 1970 to 2004 in six of the world's ocean basins, including the North Atlantic, Pacific and Indian oceans.

Three major ocean basins were examined; Atlantic, Indian and Pacific.

In this basin, significant inter-ocean exchange of heat and salinity from the Indian and Pacific Oceans serve as the main balance for the global meridional overturning circulation (MOC).