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Related Concept Videos

Prediction Intervals01:03

Prediction Intervals

The interval estimate of any variable is known as the prediction interval. It helps decide if a point estimate is dependable.
However, the point estimate is most likely not the exact value of the population parameter, but close to it. After calculating point estimates, we construct interval estimates, called confidence intervals or prediction intervals. This prediction interval comprises a range of values unlike the point estimate and is a better predictor of the observed sample value, y. 
The...
Econometric Views (EViews)01:29

Econometric Views (EViews)

Econometric Views, often stylized as EViews, is a package that merges statistical analysis with econometric studies. It is designed to provide tools for time series analysis, forecasting, and econometric model simulation. The software originated from MicroTSP software and has evolved significantly since its inception in 1981. The history of EViews is marked by a continuous effort to enhance its computational speed and user interface. It was initially developed for large computing systems but...
Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving01:29

Mechanistic Models: Compartment Models in Algorithms for Numerical Problem Solving

Mechanistic models play a crucial role in algorithms for numerical problem-solving, particularly in nonlinear mixed effects modeling (NMEM). These models aim to minimize specific objective functions by evaluating various parameter estimates, leading to the development of systematic algorithms. In some cases, linearization techniques approximate the model using linear equations.
In individual population analyses, different algorithms are employed, such as Cauchy's method, which uses a...
Propagation of Uncertainty from Systematic Error01:10

Propagation of Uncertainty from Systematic Error

The atomic mass of an element varies due to the relative ratio of its isotopes. A sample's relative proportion of oxygen isotopes influences its average atomic mass. For instance, if we were to measure the atomic mass of oxygen from a sample, the mass would be a weighted average of the isotopic masses of oxygen in that sample. Since a single sample is not likely to perfectly reflect the true atomic mass of oxygen for all the molecules of oxygen on Earth, the mass we obtain from this particular...

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Related Experiment Videos

An Improved Procedure for EI Nino Forecasting: Implications for Predictability.

D Chen, S E Zebiak, A J Busalacchi

    Science (New York, N.Y.)
    |September 22, 1995
    PubMed
    Summary

    Improved El Niño forecasting is achieved by coupling ocean-atmosphere models and assimilating wind data. This method enhances predictability and overcomes the spring barrier, suggesting El Niño is more predictable than previously thought.

    Related Experiment Videos

    Area of Science:

    • Climate Science
    • Oceanography
    • Atmospheric Science

    Background:

    • El Niño forecasting traditionally faces challenges, including a 'spring barrier' to prediction.
    • Previous models often did not fully integrate ocean-atmosphere interactions for initialization.

    Purpose of the Study:

    • To develop and evaluate an improved data assimilation procedure for El Niño forecasting.
    • To assess the impact of coupled ocean-atmosphere interactions on forecast accuracy and predictability.

    Main Methods:

    • A coupled ocean-atmosphere data assimilation procedure was employed.
    • Only wind information was assimilated, without using oceanic data.
    • The model initialization explicitly considered air-sea interaction.

    Main Results:

    • The new procedure yielded improved El Niño forecasts for the 1980s compared to previous methods.
    • The explicit consideration of air-sea interaction was identified as the key factor for improvement.
    • The spring barrier to El Niño prediction was eliminated by this procedure.

    Conclusions:

    • El Niño may be more predictable than previously estimated.
    • Forecast predictability might vary on decadal or longer timescales.
    • The spring barrier may not be an intrinsic feature of the real climate system.