Sentences with phrase «return flow of water»

Not exact matches

(27b)... and the sea returned to its wonted flow [the inference is clear: the wind abated and the water returned to its customary level] when the morning appeared... and the and LORD routed the Egyptians in the midst of the sea.

The increases were linked to return flows from the inundated Chowilla floodplain using The Living Murray environmental water, supported by the concurrent delivery of Commonwealth environmental water through the main channel.

Over 679,000 ML of Commonwealth environmental water was provided directly to the South Australian Murray (including over 284,000 ML of return flows from upstream Commonwealth environmental watering events in the Goulburn - Broken catchment, Campaspe River and Hattah Lakes).

This water was in addition to the 722 GL of Commonwealth environmental water delivered to maintain barrage flow to the Lower Lakes to 31 December 2015 as part of the River Murray Valley Flows and including return flows from watering events in Victorian tributaFlows and including return flows from watering events in Victorian tributaflows from watering events in Victorian tributaries.

In addition to the volume released from Hume Dam, return flows and the Commonwealth's 151 GL of held South Australian allocation were delivered directly to the South Australian border to meet environmental demands in the Lower River Murray, particularly for maintaining connectivity between the Lower Lakes and Coorong, and provide suitable habitat conditions (both salinity and water levels) in the Coorong for estuarine fish and vegetation species.

In addition to this volume released from Hume Dam and the volume approved for the Coorong, return flows and the Commonwealth's 134 GL of held South Australian allocation were delivered directly to the South Australian border for meeting environmental demands in the Lower River Murray, particularly for maintaining connectivity between the Lower Lakes Coorong and providing suitable habitat conditions (salinity and water levels) in the Coorong for estuarine fish and vegetation species.

Return flows from the use of Commonwealth water in Hattah Lakes also contributed to outcomes within the South Australian River Murray channel, Lower Lakes and Coorong.

Return flows from the use of Commonwealth environmental water in lower Broken Creek supported downstream actions throughout the Mid Murray, Lower Murray, Coorong and Lower Lakes, contributing to the protection, maintenance and improvement of the diversity and condition of water dependent native flora and fauna and ecosystem function.

Releases of environmental water (CEW and TLM) from Lake Victoria are providing refuge habitat from blackwater, with return flows contributing to outcomes in the Coorong.

The resulting organic soup flows into a flash vessel where pressure drops dramatically, liberating some of the water, which returns back upstream to preheat the flow into the first - stage reactor.

Return flows are an essential component of Colorado water accounting, and ranchers like to say their water is recycled four or five times by the time it gets all the way down to the main stem of the river.

Both fish species swim downstream during droughts and return during normal water flow, but the construction of dams, or stream fragmentation, prevents fish from returning upstream.

Each year, a huge amount of water evaporates from the ocean, then falls over land as rain or snow, and returns to the ocean through runoff and river flows.

Some plants, such as hickories and oaks, avoid freezing damage by dropping their leaves before the winter chill sets in - effectively shutting off the flow of water between roots and leaves - and growing new leaves and water transport cells when warmer weather returns.

That creates a return flow of warmer, saltier water toward Antarctica, where it's eroding ice shelves from beneath.»

But the two orbiters returned a wealth of scientific data in their own right, improving researchers» understanding of the Red Planet's topography and finding evidence that large amounts of water flowed across the Red Planet's surface long ago.

All too often, the return is placed under water, so it is difficult to detect any subtle diminution of flow.

However, these flows of water can be utilized by divers, who are able to drop down to the west and be effortlessly pulled along to east before rising and returning to the boat.

In particular, the very deepest part of the return flow (at around 3000 to 5000 m) has reduced and moved up in the water column compared to previous decades.

Thus it appears that disruption of deep water formation in the North Atlantic, via a blob of colder fresher water coming off of Greenland, would not «shut down» or even affect the Gulf Stream net mass transport at all, but instead would shift its northern return flow southwards, with many severe regional consequences.

There are those who appear to steadfastly maintain that all thermal radiation is from the surface and the and the convection return flow, which must heat at the dry adiabatic rate of 9.8 deg C per 1000 meters going down — unless it is gobbling up condensed water vapor on the way, and reach the surface before it can be cooled again.

If you pump water to this exceedingly remote, freezing place, said Levermann, then in 1,000 years, only about 20 percent of its equivalent will return to the ocean, through the gradual spreading and flow of Antarctic ice out toward the sea under its own massive weight.

That creates a return flow of warmer, saltier water toward Antarctica, where it's eroding ice shelves from beneath.»

As part of the planet's reciprocal relationship between ocean circulation and climate, this conveyor belt transports warm surface water to high latitudes where the water warms the air, then cools, sinks, and returns towards the equator as a deep flow.»

6 flow in opposite direction of wind - related currents return water taken away from one side of the ocean basin to the opposite side EX: Equatorial Countercurrents

This is the flow of warm water to the far north, which then dives to the sea bottom and returns to the south.

In principle, a large enough return flow of fresh water from rivers and glaciers could reduce the density of the surface waters sufficiently to stop them from sinking, in which case the whole AMOC would stop.

The return flow of warm water from the Pacific through the Indian ocean and the Caribbean to the North Atlantic, a distance of 40,000 km, takes from 13 to 130 years... Why do our Earthly model - makers believe they can deal with lag times like the example above?

These dense water masses spread into the full extent of the ocean and gradually upwell to feed a slow return flow to the sinking regions.