Dynamic bias selection is often mentioned in relation to a continuous flow of training examples (data streams), where metalearning algorithms can be used for bias management and detecting concept drifts, as argued in Brazdil et al. (2009).
SATP works according to a simple request/reply scheme and must be used in addition to a connection-based network protocol that provides a reliable flow of data for example, TCP.
The workflow and data flow of this example is summarized in Fig. 2.
This encourages further use of the LES approach for this type of flow, for example by extension to scalar mixing predictions.
This theory on the pathogenesis of contrast-induced nephropathy resulted in the introduction of measures aimed at increasing renal blood flow, for example administration of theophylline (a selective renal adenosine antagonist) or of fenoldopam mesylate (a selective dopamine-1 receptor agonist that increases effective renal plasma flow without concomitant changes in glomerular filtration rate).
The rate of groundwater flow, for example, can be calculated from the breakdown of radioactive carbon-14 by measuring the time it takes for rainwater to pass through the ground, while numerical modeling is used to study heat and mass transfer in groundwater.
Measurement of blood flow, for example, cardiac output (CO), has traditionally been associated with the use of additional invasive monitoring, including the pulmonary artery catheter or using transpulmonary thermodilution, or less invasively, with the esophageal Doppler.
Several conditions such as redistribution of blood flow (for example, in shock, severe head injury, general anesthesia, and microcirculatory disorders) may affect the relationship between ScvO2 and SvO2 [ 9, 10].
Analysis of channel flow variation over the course of the experiments indicated that weirs change the relationship between transient storage parameters and flow, for example the trend of increasing α with flow without weirs was reversed in the presence of weirs.
The viscosity (i.e., internal resistance to flow) of seawater, for example, is higher than that of fresh water because of its higher salinity.
