base flow
drought flow

The reaches below the weir currently contain no base flow.

Low flows, sometimes called base flows, occur for the majority of the year.

A series of springs provide a continuous base flow to Deer Creek.

The operating rules require that a base flow immediately downstream in the creek must be maintained.

Thus the recharge can be calculated from this base flow if the catchment area is known.

This is significant because groundwater provides about 40% of the water needed to maintain normal base flow rates in our rivers and streams.

These include market based flows such as foreign direct investments and portfolio investments.

The sandstone outcrops in only a few places, and where it does, the springs provide the base flow for the river.

Substantial base flow in streams rounds the year.

Transfers are subject to a credit based flow control scheme, managed using flow frames.

Natural base flow is sustained largely by ground-water discharges.

However, in most other basins, the base flow is adequate to supply water and can be exploited through developments on the rivers.

Navier-stokes computations of projectile base flow with and without mass injection.

Because of the large private ownership and development potential, water diversions and low base flows are an important issue in this watershed.

The remaining 15 percent comes from a variety of sources, principally groundwater base flow and summer monsoon storms.

It consists of a base flow, the "noise", and a cocycle dynamical system on the "physical" phase space.

The term base flow may refer to:

The base flow is often ergodic.

Rain that falls on the north generally has a more gradual, longer-lasting effect, sustaining the base flow of the creek during dry periods.

Due to the urbanized nature of the watershed, the Don River experiences low base flows interspersed with high volume floods.

The measure-preserving dynamical system is known as the base flow of the random dynamical system.

Historically, much of the summer base flow of these rivers derived from the Fijeh and Barada springs.

Define the base flow as follows: for each "time" , let be a measure-preserving measurable function:

Density based flow, however, occurs when liquefaction of sediment during transport causes a change to the density of the fluid.

Historically, groundwater seepage from Tulare Lake maintained a significant base flow in the river during the dry months - some accounts suggest over 50 percent.