throughflow

Some bases remain in the soil, though others may be lost by throughflow.

This helps to keep the driving atmosphere fresh and healthy by achieving a 'throughflow' of air.

This is called subsurface return flow or throughflow.

During dry weather, streamflow is maintained by the combination of throughflow and groundwater flow.

The Indonesian Throughflow at whoi.edu.

In such soils which have a high vegetation content water is able to travel along the 'pipes', allowing water to travel faster than throughflow.

The underground part of the station underwent extensive remodelling works to increase throughflow of passengers resulting from the opening of High Speed 1.

Perrault went on to develop the theory of the hydrologic cycle, correctly accounting for the roles of evaporation, transpiration, throughflow and surface runoff.

This means that any water falling in the catchment area would have been rapidly converted into channel flow by surface runoff and to a lesser extent by throughflow.

It is a major contributor to the Indonesian Throughflow that transports water from the Pacific Ocean to the Indian Ocean.

Groundwater flows down-slope towards the river channel, but the rate of groundwater flow is less than the rate of throughflow or of overland flow.

Effect of salinity on estimating geostrophic transport of the Indonesian Throughflow along the IX1 XBT section.

The Lombok Strait is notable as one of the main passages for the Indonesian Throughflow that exchanges water between the Indian Ocean and the Pacific Ocean.

If children approached schooling in this manner schools would have no wish to 'lose' their pupils, the throughflow of children with genuine adjustment problems in units would be assured and the 'moral order're-established.

It is of significant biodiversity value as it is in the flow of the Indonesian Throughflow ocean current from the Pacific Ocean through the Malay archipelago to the Indian Ocean.

In a throughflow evaporator, the inspiration flow is led through a warmed up water bath, in case of a surface evaporator however the inspiration flow is guided along the surface of the water level.

The actual rates of operation of the processes of precipitation, interception, evaporation, transpiration, overland flow, throughflow and groundwater flow depend upon climatic, vegetative, pedological, topographic and geological conditions peculiar to each drainage basin.

For example, the rates of infiltration and throughflow will depend on slope, soil type, vegetation cover, depth of soil and other factors while the volumes of water stored as depression storage will depend upon surface topography.

When the Indonesian Throughflow (through Lombok Strait, Ombai and the Timor Passages) enters the Indian Ocean it is advected towards Africa within the Indian South Equatorial Current.

Interflow is sometimes used interchangeably with throughflow; however, throughflow is specifically the subcomponent of interflow that returns to the surface, as overland flow, prior to entering a stream or becoming groundwater.

In oceanographic, Bali Sea is concerned with the Indonesian Throughflow coming from Pacific Ocean to the Indian Ocean, the flow of which are mostly passing through Bali Strait and Lombok Strait.

Soil drying is promoted both by tree roots, which create large pores that are not characteristic of soils under grassland and moorlands, and the reduction of throughflow that occurs due to greater interception of precipitation by a tree canopy.

The Indonesian throughflow (ITF) is important to global climate since it provides a low-latitude pathway for warm, fresh water to move from the Pacific to the Indian Ocean and this serves as the upper branch of the global heat conveyor belt.

Thus a better understanding of the possible links between El Niño, Western Pacific Warm Pool, Indonesian Throughflow, wind pattern off western Australia, and ice volume expansion and contraction can be obtained by studying the behaviour of the LC during Quaternary at close stratigraphic intervals.

An important feature of the Indonesian Throughflow is that because the water in the western equatorial Pacific Ocean has a higher temperature and lower salinity than the water in the Indian Ocean, the Throughflow transports large amounts of relatively warm and fresh water to the Indian Ocean.