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criteria for the compasion of equations
criteria for the compasion of equations

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Document

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Volume Anomaly Detection in Data Networks: an Optimal Detection
Volume Anomaly Detection in Data Networks: an Optimal Detection

... based on the variance of the prediction error. The authors use the Kalman filter technique to achieve this goal, using SNMP measurements as the observation process and a linear state space model to capture the evolution of OD flows in time. Even though the approach is quite appealing, it presents a ...
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... Thad: “I just fit a line to the body fat percentage (y) versus weight data.” Fellow Statistician: “Tarpey, your model is wrong...under-specified – there are other variables that also predict body fat percentage; your estimated slope will be biased. You need more predictors” ...
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regional regression models of annual streamflow for the united states

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Bank of America and CCAR 2016 Stress Testing: A Simple Model

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Data assimilation

Data assimilation is the process by which observations are incorporated into a computer model of a real system. Applications of data assimilation arise in many fields of geosciences, perhaps most importantly in weather forecasting and hydrology. The most commonly used form of data assimilation proceeds by analysis cycles. In each analysis cycle, observations of the current (and possibly past) state of a system are combined with the results from a numerical model (the forecast) to produce an analysis, which is considered as 'the best' estimate of the current state of the system. This is called the analysis step. Essentially, the analysis step tries to balance the uncertainty in the data and in the forecast. The result may be the best estimate of the physical system, but it may not the best estimate of the model's incomplete representation of that system, so some filtering may be required. The model is then advanced in time and its result becomes the forecast in the next analysis cycle. As an alternative to analysis cycles, data assimilation can proceed by some sort of nudging process, where the model equations themselves are modified to add terms that continuously push the model towards observations.
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