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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

5.0K
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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Entropy01:18

Entropy

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The first law of thermodynamics is quantitatively formulated via an equation relating the internal energy of a system, the heat exchanged by it, and the work done on it. A quantitative formulation of the second law of thermodynamics leads to defining a state function, the entropy.
When an ideal gas expands isothermally, the disorder in the gas increases. From the molecular perspective, the gas molecules have more volume to move around in.
Consider an infinitesimal step in the expansion, which...
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Energy Conservation and Bernoulli's Equation01:16

Energy Conservation and Bernoulli's Equation

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Applying the conservation of energy principle or the work-energy theorem to an incompressible, inviscid fluid in laminar, steady, irrotational flow leads to Bernoulli's equation. It states that the sum of the fluid pressure, potential, and kinetic energy per unit volume is constant along a streamline.
All the terms in the equation have the dimension of energy per unit volume. The kinetic energy per unit volume is called the kinetic energy density, and the potential energy per unit volume is...
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Overview
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Prediction Intervals01:03

Prediction Intervals

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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. 
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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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Measuring Statistical Learning Across Modalities and Domains in School-Aged Children Via an Online Platform and Neuroimaging Techniques
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El Niño physics and El Niño predictability.

Allan J Clarke1

  • 1Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, Florida 32306-4320;

Annual Review of Marine Science
|January 11, 2014
PubMed
Summary

El Niño and the Southern Oscillation (ENSO) drives Earth's climate variability. Understanding ENSO's seasonal cycle and predicting its transitions are key for climate forecasting.

Area of Science:

  • Climate Science
  • Oceanography
  • Atmospheric Science

Background:

  • Year-to-year climate variability is largely influenced by El Niño and the Southern Oscillation (ENSO).
  • ENSO originates from ocean-atmosphere instability in the western equatorial Pacific warm pool.
  • The phenomenon exhibits phase locking to the seasonal cycle.

Purpose of the Study:

  • To elucidate the physics governing ENSO variability.
  • To explain the seasonal cycle and phase locking of ENSO events.
  • To discuss ENSO prediction challenges and precursors for transitions.

Main Methods:

  • Review of the physical mechanisms driving ENSO.
  • Analysis of ENSO's seasonal cycle and growth patterns.
  • Discussion of dynamical and statistical ENSO forecasting models.

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Main Results:

  • ENSO develops between April/May and November, with peak influence extending into the next year.
  • Predicting ENSO is straightforward from July to February.
  • Forecasting is more challenging during the April/May transition to a new ENSO event.

Conclusions:

  • The seasonal cycle significantly impacts ENSO predictability.
  • Understanding ENSO precursors is crucial for improving climate forecasts.
  • Dynamical and statistical models offer valuable tools for ENSO prediction.