Another study presented in the symposium offered a new approach to forecasting the Colorado River's spring - summer «streamflow,» or
the volume of water flowing past a fixed point in the river.
The sheer
volume of water flowing over the falls amounts to 220,000 litres per second - enough to fill one Olympic sized swimming pool in 11 seconds!
During peak flow season,
the volume of water flowing over Niagara Falls averages a whopping 6,400 cubic meters per second.
The sheer
volume of water flowing over the falls amounts to 220,000 litres per second — enough to fill one Olympic sized swimming pool in 11 seconds!
Among these boundary currents are the Gulf Stream and the Kuroshio (off Japan), which rank next in
volume of water flow to the Antarctic Circumpolar Current.
Not exact matches
Now, with billions in new revenues
flowing out
of these deposits, a growing number
of oil - and - gas - field services firms have emerged with solutions to the problem
of how to remediate the huge
volumes of heavily polluted
water that comes out
of the ground.
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.
Commonwealth Environmental
Water Holder, David Papps said the multi-use event would see a large volume (up to 634 GLs) of Commonwealth environmental water made available to supplement a series of environmental water flows generated by the St
Water Holder, David Papps said the multi-use event would see a large
volume (up to 634 GLs)
of Commonwealth environmental
water made available to supplement a series of environmental water flows generated by the St
water made available to supplement a series
of environmental
water flows generated by the St
water flows generated by the States.
There are insufficient
volumes of environmental
water available anywhere in the system to replicate the types
of high
flows that occur naturally.
Commonwealth
water provided as barrage
flow exported significant
volumes of salt, nutrients and phytoplankton that supported ecosystem productivity in the Coorong and the export
of salt at the Murray Mouth.
During spring in 2016 - 17, a small
volume of Commonwealth environmental
water contributed to increasing river connectivity in the Mehi River and Carole Creek during a large natural
flow event.
This involves highly targeted and discrete environmental
watering actions such as maintaining low
flows to manage
water quality by flushing waterholes and directing small
volumes of water from the main river channels to providing refuges for plants and animals in wetlands and channel systems.
Features like giant gravel current ripples and displaced 65 - foot - wide boulders in the Scablands could not be explained by changes in the nearby Columbia River, he wrote — the
flow and
volume of whatever
water source formed them would have to be exponentially larger.
Over the course
of 30 days or so, possibly less, about 93,000 cubic kilometers
of water — almost 80 %
of the
volume of all free -
flowing fresh
water on Earth today — carved the 15 - km - wide, 2.5 - km - deep Aram Valley.
«These calcifying algae evidence two rapid decreases in the salt content, at approximately 8,400 and again 7,600 years ago, which can only be explained by the fact that a higher
volume of low - saline surface
water flowed from the Black Sea into the northern Aegean at these times.
If this scenario is accurate, Earth may today hold half as much
water in its depths as is currently
flowing in oceans on the surface, Panero said — an amount that would approximately equal the
volume of the Pacific Ocean.
Through the Lombok straits, between Bali and Lombok
flows the Indonesian through
flow, a massive
volume of water that passes from the pacific to the Indian Ocean.
The parking lot has been shifted so it is perpendicular to the ocean and the floodplain has been opened up, so that should a large rain event occur, the lagoon will be able to handle the heavy
volumes of water that
flow down Redwood Creek and out to the Pacific.
Even the most reluctant tyke will be amazed by the sheer
volume of water that hurtles over the Huka Falls - and when the
flow control gates open at Aratiatia the gorge is quickly flooded by the
waters of the Waikato River.
If we have a pool being filled from three different sources, each
of which varies substantially from minute to minute in its outflow, but the
volume of water in the pool increases steadilly, we know the net
flow into the pool is positive and the average
flow per minute even though we may be completely in the dark as to which source provides the greatest contribution in any given minute.
«Global warming causes the snow - caps
of the Himalayas to melt early and in bigger quantities, causing early and extra
volumes of water to
flow through the Ganges and the Brahmaputra rivers.
Measuring the distance apart and speed
of 2 satellites in space orbiting the earth to the width
of a human hair with no margin for error [damn those drift recalculations], and taking into account unknown factors with respect to the true values for
water depth,
water weight at different salt concentrations, ice depth magma
flows, volcanic activity etc [ie making a lot
of guesses], plus taking human motivation on board [like CO2 increase must melt ice surely] can give you an accurate measurement
of the
volume ice in Antarctica.
After some short time, depending
of the
water volume in the bucket and the height
of flows RinH and RinB the red dye concentration gets in equilibrium.
The rate at which
water moves down a stream is the sole determinate
of the stream
flow volume?
Climate change separately brings in some desertification and loss
of river
volumes, as people remove that
flow in various ways to compensate for lack
of water elsewhere.
The above changes mean that the
volume of flow is reduced where partial pressure
of water vapor is low and is a little larger than that where we have more
water vapor.
So on condensation, under the still rising hotter lighter air carrying on doing its thing and perhaps adding new layers, there would be the accompanying
volume and temperature decrease
of that first previously rising lighter
volume now heavier liquid
water and added to by the adjacent
volumes of heavier colder air
flowing beneath the still rising lighter hotter and into the space now available on condensation
of its neighbour, which all now being heavier will increase the pressure at the surface as they all sink together displacing the lighter.
The amount
of water in the uplift reduces the
flow from the side because it adds to the
volume and because evaporation takes most
of the energy available reducing the overall
flow of air.
Observations suggest that variability in oceanographic conditions in the Arctic is very largely driven by the consequences
of the
flows through open passages to both Atlantic and Pacific Oceans, which themselves respond to the different and characteristic variability
of the circulation patterns
of each ocean: each inflow is not only variable in
volume of water transported but also in the temperature
of the
water imported.
-- under conditions that lead to adiabatic transition the pressure is also very close to hydrostatic pressure at every moment and every altitude — the loss
of water from the air does not affect the pressure, it reduces the
volume of the remaining air — the speed
of the convective
flow is reduced due to the reduced
volume of the gas.
A detailed and very accurate calculation
of the atmospheric
flows of moist air must take into account also the effects related to the
volume taken by
water vapor both when
water vapor is added by evaporation and when it's removed in condensation, but these effects are very minor corrections and not a source
of anything significant.
The outgoing
flow through Fram Strait carries with it large
volumes of fresh
water as fragmented pack ice, a
flow that is strongly episodic at decadal scale and is associated with the series
of so called Great Salinity Anomalies observed within the circulation
of the subarctic gyre and in the Nordic seas that were discussed in the previous chapter.
46 Hydroelectric Power Principle Potential Energy (PE)
of a mass
of water Physics for the IB Diploma 5th Edition (Tsokos) 2008 Hydroelectric Power Principle Potential Energy (PE)
of a mass
of water where h is the height
of the
water Mass (m) is given by Where ρ is the density
of the
water (1000kg / m3) And V is the
volume occupied Recall, the definition of power (P) Volume flow rate Q is So, Physics for the IB Diploma 5th Edition (Tsokos) 2
volume occupied Recall, the definition
of power (P)
Volume flow rate Q is So, Physics for the IB Diploma 5th Edition (Tsokos) 2
Volume flow rate Q is So, Physics for the IB Diploma 5th Edition (Tsokos) 2008 46
Ice - sheet
volume is controlled by the balance between mass input and mass loss; mass input is almost entirely due to snowfall, and mass loss is from iceberg calving supplied by
flow of the ice sheet, or runoff
of melt
water.
The direction and rate
of flow is determined by gravity and the
volume by the quantity
of water.
In the ocean and atmosphere interface the direction and rate
of flow is determined by pressure and the
volume by the phase changes
of water.
When one adds DLR it just behaves like a tributary joining a river because pressure having set the background upward rate
of flow (rather than gravity) the phase changes
of water ensure that only the
volume (quantity)
of the energy
flow changes from ocean skin upward.
By running that data with the amount
of water trawled (measured by the
flow meter), they can get an idea
of the density
of plastic in the gyres (amount
of plastic per unit
volume).
If, as seems plausible, the
volume of water involved was increased by the atmosphere's increased capacity to hold
water; then we can expect floods with peak
flows approaching 1.5 million cusecs by the end
of this century?
The biggest remaining question seems to be whether the circulating
water will quickly remove the heat from a small
volume of rock surrounding the larger fractures or whether it will
flow through many smaller fractures and efficiently remove the heat from a large
volume of rock over a much longer period.
However, the the study also found that measurements at the ice's edge show that climate models alone can overestimate the
volume of meltwater
flowing to the ocean because they fail to account for
water storage beneath the ice.
A common analogy is a garden hose: Volts are equivalent to the
water pressure in the hose; the current is equivalent to the
flow rate; and wattage is equivalent to the
volume of the spout's spray.