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Related Concept Videos

Prediction Intervals01:03

Prediction Intervals

3.0K
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. 
3.0K
End Point Prediction: Gran Plot01:07

End Point Prediction: Gran Plot

1.1K
A Gran plot is used to predict the equivalence volume or endpoint of a potentiometric or acid-base titration without reaching the endpoint. Typically, titration data is collected as a function of the titrant's volume up to a point less than the equivalence volume and then transformed into a linear format. The straight line is extended to the x-axis, indicating the necessary titrant volume to achieve the equivalence point.
For potentiometric titration, the Gran plot is created by plotting...
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Precipitation Processes01:12

Precipitation Processes

4.5K
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

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Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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Predicting Reaction Outcomes02:24

Predicting Reaction Outcomes

9.8K
Kinetics describes the rate and path by which a reaction occurs. In contrast, thermodynamics deals with state functions and describes the properties, behavior, and components of a system. It is not concerned with the path taken by the process and cannot address the rate at which a reaction occurs. Although it does provide information about what can happen during a reaction process, it does not describe the detailed steps of what appears on an atomic or a molecular level. On the other hand,...
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Determination of Expected Frequency01:08

Determination of Expected Frequency

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Suppose one wants to test independence between the two variables of a contingency table. The values in the table constitute the observed frequencies of the dataset. But how does one determine the expected frequency of the dataset? One of the important assumptions is that the two variables are independent, which means the variables do not influence each other. For independent variables, the statistical probability of any event involving both variables is calculated by multiplying the individual...
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Related Experiment Videos

Long-lead Prediction of ENSO Modoki Index using Machine Learning algorithms.

Manali Pal1, Rajib Maity2, J V Ratnam3

  • 1Department of Civil Engineering, Indian Institute of Technology Kharagpur, Kharagpur, 721302, West Bengal, India.

Scientific Reports
|January 17, 2020
PubMed
Summary

Machine Learning (ML) algorithms, Support Vector Regression (SVR) and Random Forest (RF), can forecast the El Niño (La Niña) Modoki index (EMI) phase up to 12 months ahead. SVR demonstrated superior performance over RF in these long-lead predictions.

Related Experiment Videos

Area of Science:

  • Climate Science
  • Machine Learning
  • Oceanography

Background:

  • El Niño (La Niña) Modoki (ENSO Modoki) index (EMI) is crucial for climate prediction.
  • Accurate long-lead prediction of EMI is challenging but vital for climate anomaly forecasting.
  • Machine Learning (ML) offers potential for improving ENSO prediction.

Purpose of the Study:

  • To evaluate the efficacy of non-linear ML algorithms for long-lead EMI prediction.
  • To compare the performance of Support Vector Regression (SVR) and Random Forest (RF) for EMI forecasting.
  • To identify key climate variables for predicting EMI using ML.

Main Methods:

  • Utilized Support Vector Regression (SVR) and Random Forest (RF) algorithms.
  • Forecasted the El Niño (La Niña) Modoki index (EMI) at 6, 12, 18, and 24-month lead times.
  • Identified predictors using Kendall's tau correlation and evaluated importance via Supervised Principal Component Analysis (SPCA) on sea surface temperature (SST), sea surface height (SSH), and soil moisture content (SMC).

Main Results:

  • Both SVR and RF accurately forecast the phase of the EMI at 6 and 12-month lead times.
  • The amplitude of strong EMI events was underestimated by both ML models.
  • Support Vector Regression (SVR) outperformed Random Forest (RF) in EMI forecasting accuracy.

Conclusions:

  • Machine Learning algorithms, particularly SVR, show significant promise for long-lead ENSO Modoki index prediction.
  • The study highlights the capability of SVR for reliable EMI phase forecasting up to a year in advance.
  • Further refinement is needed to improve the amplitude prediction of extreme EMI events.