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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

446
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...
446
What is Weather?01:07

What is Weather?

18.2K
Overview
18.2K
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

1.8K
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...
1.8K
Precipitation Gravimetry01:03

Precipitation Gravimetry

6.3K
Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
6.3K
Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

2.2K
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
2.2K
Types of Coprecipitation01:10

Types of Coprecipitation

611
Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
611

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Using Generative Art to Convey Past and Future Climate Transitions
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Generative emulation of weather forecast ensembles with diffusion models.

Lizao Li1, Robert Carver1, Ignacio Lopez-Gomez1

  • 1Google Research, Mountain View, CA, USA.

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Deep generative models can emulate costly weather forecasts, providing accurate probabilistic predictions and improving extreme weather event forecasting. This approach enhances decision-making and climate risk assessment.

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Area of Science:

  • Meteorology and Climate Science
  • Artificial Intelligence and Machine Learning

Background:

  • Uncertainty quantification is vital for decision-making, particularly in probabilistic weather forecasting.
  • Current methods rely on computationally expensive physics-based simulations to generate forecast ensembles.
  • This high computational cost limits the scale and efficiency of generating large ensembles.

Purpose of the Study:

  • To develop a computationally efficient method for generating probabilistic weather forecasts.
  • To leverage deep generative diffusion models for emulating physics-based weather simulations.
  • To improve the accuracy and reliability of weather and climate predictions.

Main Methods:

  • Utilized deep generative diffusion models trained on historical weather data.
  • Emulated operational ensemble weather forecasts using the learned models.
  • Assessed the statistical properties and predictive skill of generated ensembles compared to physics-based ones.
  • Evaluated the models' ability to correct biases in operational forecasting systems.

Main Results:

  • Generated ensembles exhibit similar statistical properties and predictive skill to traditional physics-based ensembles.
  • Emulated forecasts are produced at a significantly lower computational cost, enabling large-scale generation.
  • Bias-corrected generated ensembles demonstrate improved probabilistic forecast metrics and reliability.
  • Enhanced accuracy in forecasting probabilities of extreme weather events was observed.

Conclusions:

  • Deep generative diffusion models offer a scalable and cost-effective alternative for producing high-quality probabilistic weather forecasts.
  • This methodology shows promise for generating large climate projection ensembles for climate risk assessment.
  • The approach enhances the utility of weather forecasts for critical decision-making processes.