Sentences with phrase «ocean basins over»

In the new study, scientists simulated the movement of Earth's tectonic plates and changes in the resonance of ocean basins over millions of years.

Since the tropical West Pacific is already warmer on average than the East, this trend led to a substantial increase in the west - to - east temperature differential across the Pacific Ocean basin over a 15 year period.

Not exact matches

However, ENSO also increased the mean and variability of MHW duration in the northeast Pacific Ocean (Supplementary Fig. 1E, F), the variability of intensity off Western Australia and California (Supplementary Fig. 1D) and the variability of frequency over much of the Tropics in all ocean basins as well as the mid - and high - latitudes in the Pacific Ocean (Supplementary Fig.Ocean (Supplementary Fig. 1E, F), the variability of intensity off Western Australia and California (Supplementary Fig. 1D) and the variability of frequency over much of the Tropics in all ocean basins as well as the mid - and high - latitudes in the Pacific Ocean (Supplementary Fig.ocean basins as well as the mid - and high - latitudes in the Pacific Ocean (Supplementary Fig.Ocean (Supplementary Fig. 1B).

MHW intensity between 1982 — 1998 and 2000 — 2016 increased in over 65 % of the global ocean, most notably in all five western boundary current regions, where the mean warming has been considerably faster than the global average39, and most mid-latitude ocean basins (Fig. 1e).

Sunrise views over the blue ocean from the large private balcony, bathroom with 2 vanity basins, rain shower, Thann bathroom amenities, double walk - in wardrobes, LCD TV, DVD player, free WiFi internet.

When Santa Ana conditions prevail, with winds in the lower two to three kilometers (1.25 - 1.8 miles) of the atmosphere from the north through east, the air over the coastal basin is extremely dry, and this dry air extends out over offshore waters of the Pacific Ocean.

Equally palatial is the bathroom with twin basins on a marble countertop, ceramic bathtub, WC enclosure, wall of well - designed wardrobes and both indoor and outdoor rain showers looking over the ocean.

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..

I agree the OHC data are incompatible with a predominately internal contribution (although I'm sure Judith would argue those data are too uncertain, though I don't think anyone has argued OHC decreasing over the last half - century, at least not at the ocean basins / depths that communicate with the atmosphere on the relevant timescales).

«The rapid warming of the Atlantic Ocean created high pressure zones in the upper atmosphere over that basin and low pressure zones close to the surface of the ocean,» said Prof Axel Timmermann, co-lead and corresponding author from the University of HaOcean created high pressure zones in the upper atmosphere over that basin and low pressure zones close to the surface of the ocean,» said Prof Axel Timmermann, co-lead and corresponding author from the University of Haocean,» said Prof Axel Timmermann, co-lead and corresponding author from the University of Hawaii.

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.

Ocean basin temperature, according to best Bedwetter Bandwagon estimate of energy imbalance at top of atmosphere, is only going to rise by 0.2 C over the next century.

Of course, this is not true of mean ocean heat capacity nor the world's mean temperature, however it may be substantial true over a 5 x 5 degree section of ocean or even a region as large as a single ocean basin.

Elevated pb signals are observed over deep extratropical regions (e.g., Southern Ocean basins) and shallow or semi-enclosed areas (e.g., Indonesian and Nordic seas).

«Nevertheless, neither data set supports the model result of Meehl et al. that the heat uptake in this layer (300 - 700m) in the Pacific dominates over other ocean basins during hiatus periods.»

«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.

The negative AO phase is characterized by a high - pressure center anomaly over the entire Arctic basin or polar cap and low - pressure center anomalies in each ocean basin in the mid-latitudes.

The positive AO phase is characterized by a low - pressure center anomaly over the entire Arctic basin or polar cap (the region poleward of 60 ° N) and high - pressure center anomalies in each ocean basin in the mid-latitudes.

We show that the influx of water into the volume created by this subsidence produces a sea - level fall at locations distant from these margins — indeed over the major ocean basins — that is comparable in amplitude to the syphoning mechanism isolated by Mitrovica and Peltier (1991).»

CO2 does not explain any of the ocean basin responses over the satellite era.

In La Nina years, more rain fell away from oceans, including over the Amazon, the Congo basin and Australia, she said.

The suggested hypothesis, is that in regions devoid of dust (e.g., over the large ocean basins), the formation of cloud condensation nuclei takes place from the growth of small aerosol clusters, and that the formation of the latter is governed by the availability of charge, such that charged aerosol clusters are more stable and can grow while neutral clusters can more easily break apart.

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

However the additional over burden of water, fresh and salt to each part of any ocean or extremely large body of water causes the deflection of the bottom of that basin to some extant as well as presenting as a rise in seal level at that area.

one might be able to forecast things over the scale of ocean basins, but one can not really expect much more detailed skill than that.

Runoff is collected over geographically realistic river basins and mixed into the ocean at the appropriate river mouths.

Variations in tropical cyclones, hurricanes and typhoons are dominated by ENSO and decadal variability, which result in a redistribution of tropical storm numbers and their tracks, so that increases in one basin are often compensated by decreases over other oceans.

Even though the temperature increases are small, because they are spread over huge ocean basins in layers a few kilometers thick, they quickly add up.

Many of these circulation patterns are thought to be driven by geographical features, such as the strong heating near the tropics nd over parts of the ocean basin, such as the Walker cell (see here).

The SST is all of the ocean basins has shown a steady and statistically significant trend over the last 30 - 40 years (e.g., see Hoyos et al 2006).

The activity does vary year to year and over multidecadal periods as ocean cycles including El Nino / La Nina, multidecadal cycles in the Pacific (PDO) and Atlantic (AMO) favor some basins over others.

In some ocean basins, the intensification of hurricanes over time has been linked to rising ocean temperatures.

Breaking internal waves in the vicinity of topography can reach heights of over 100 m and are thought to enhance basin - wide energy dissipation and mixing in the ocean.