definition
The act or process of flowing in or into
definition
Anything which flows in or into
example
The inflow of air
definition
Influence from outside.
definition
The act or process of flowing in or into
definition
Anything which flows in or into
example
The inflow of air
definition
Influence from outside.
definition
To flow in.
The principal time of inflow of North Sea water is during spring and summer.
Therefore the inflow waxes and wanes from season to season throughout the year, but it also varies in the same season in different years.
Where the evaporation is at a minimum, the inflow of rivers from a large continental area and the precipitation from the atmosphere at a maximum, there is necessarily the greatest dilution of the sea-water, the Baltic and the Arctic Sea being conspicuous examples.
The heat transmitted was measured by observing the difference of temperature between the inflow and the outflow, and the weight of water which passed in a given time.
On the contrary, the effect of the inflow of adult migrants is very marked, as is to be expected, in the returns for the new countries, such as the United States, Canada and Australasia.
Its outlet is through the Lacahahuira river into the Coipasa swamp, and it is estimated that the outflow is much less than the inflow, showing a considerable loss by evaporation and earth absorption.
Empirical rules have grown up assigning to each district, according to its average rainfall, a particular number of days' supply, independently of any inflow, as the contents of the reservoir necessary to secure a given yield throughout the driest seasons.
Many orifices through which water at first only dribbled were thus caused to discharge water with great force, and entirely free from sand, against the opposite side of the well, while the general result was to increase the inflow of water many times, and to entirely prevent the intrusion of sand.
But before this was accomplished the filtration of the effluent became defective, and brackish water was received, which rapidly increased nearly to the saltness of the inflow.
Update buoyancy after heat advection and freshwater inflow, if used.
We were also very successful in generating a significant cash inflow which benefits the whole Group.
Finance Again we achieved a good cash performance with operating cash inflow of 14.5p per share (2004 12.7p ).
The net cash inflow in 2003 primarily resulted from the proceeds from the exercise of the share options.
Direct foreign capital inflow will increase in comparison with last year.
There is no restriction from capital inflow into or outflow from Hong Kong.
Without applying external perturbations at the inflow boundary, large vortical structures develop naturally in the flow field due to buoyancy effects.
The most widely accepted reason for the Irish growth spurt is of course the large inflow of overseas direct investment, mainly American.
After the end of the war of 1895-1898 a large immigration from Spain began; the inflow from the United States was very small in comparison.
Most passages lack the inflow of seepage water, probably vital for the maintenance of cave populations.
Seasonal inflow may, for example, winnow out sediments from breccias and other areas, to redeposit them elsewhere.
In the sense of "flowing water," the word is applied to the inflow of the tide, as opposed to "ebb."
The museums, enriched by a constant inflow of works of art and inscriptions, have been carefully and scientifically arranged, and afford opportunities for systematic study denied to scholars of the past generation.
The dorsal skeletal elements of the thorax and of the anterior six abdominal segments unite with the wing-cases to form a large respiratory chamber, containing five pairs of tracheal gills, with lateral slits for the inflow and a posterior orifice for the outflow of water.
Tracing, then, the quantities of oil given per 1,000 fish from year to year, they seemed to establish a connexion between the variation in " condition " of the fish, the variation in the inflow of Atlantic water, and the variation in the number of sunspots from year to year.
To admit of the free inflow and outflow of currents of water necessary for respiration, which is effected by means of filamentous abdominal tracheal gills, the two ends of the tube are open.
The warmed air of summer produces an area of low pressure in the west-central United States, which interrupts the belt of high pressure that planetary conditions alone would form around the earth about latitude 30; hence there is a tendency of the summer winds to blow inward from the northern Pacific over the Cordilleras toward the continental centre, and from the trades of the torrid Atlantic up the Mississippi Valley; conversely in winter time, the cold air over the lands produces a large area of high pressure from which the winds tend to flow outward; thus repelling the westerly winds of the northern Pacific and greatly intensifying the outflow southward to the Gulf of Mexico and eastward to the Atlantic. As a result of these seasonal alternations of temperature and pressure there is something of a monsoon tendency developed in the winds of the Mississippi Valley, southerly infiowing winds prevailing in summer and northerly outfiowing winds in winter; but the general tendency to inflow and outflow is greatly modified by the relief of the lands, to which we next turn.
One of the best indications of actual winter weather, as apart from the arrival of winter by the calendar, is the development of cyclonic disturbances of such strength that the change frcm their warm, sirocco-like southerly inflow hi front of their centre, to the cold wave of their rear produces lion-periodic temperature changes strong enough to overcome the weakened diurnal temperature changes of the cold season, a relation which practically never occurs in summer time.
Meanwhile, till adequate means of transportation were provided, it was seen that city and prairie alike must wait for any large inflow of population.
Before this stage the converse process begins, the reduced column of fresh water is no longer capable of balancing the sea water in the sand, inflow occurs at c and e, resulting finally in the well water becoming saline.
The inflow to the deep basins is intermittent, probably with a long period of flux and reflux.
In some small and exceptional regions the water is very alkaline, and in the counties of the south-east it is so generally saline that it is difficult, below 150 ft., to avoid an inflow of salt water.
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