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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

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...
Uncertainty: Overview00:59

Uncertainty: Overview

In analytical chemistry, we often perform repetitive measurements to detect and minimize inaccuracies caused by both determinate and indeterminate errors. Despite the cares we take, the presence of random errors means that repeated measurements almost never have exactly the same magnitude. The collective difference between these measurements - observed values - and the estimated or expected value is called uncertainty. Uncertainty is conventionally written after the estimated or expected value.
Detection of Black Holes01:10

Detection of Black Holes

Although black holes were theoretically postulated in the 1920s, they remained outside the domain of observational astronomy until the 1970s.
Their closest cousins are neutron stars, which are composed almost entirely of neutrons packed against each other, making them extremely dense. A neutron star has the same mass as the Sun but its diameter is only a few kilometers. Therefore, the escape velocity from their surface is close to the speed of light.
Not until the 1960s, when the first neutron...
Boundary Layer Characteristics01:18

Boundary Layer Characteristics

When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
Uniform Depth Channel Flow: Problem Solving01:18

Uniform Depth Channel Flow: Problem Solving

To calculate the flow rate for a trapezoidal channel, first, identify the bottom width, side slope, and flow depth of the channel. The cross-sectional area (A) corresponding to the depth of flow (y), channel bottom width (B), and side slope (θ) is determined by:Next, calculate the wetted perimeter, which includes the bottom width and the sloped side lengths in contact with the water. Using the values of the cross-sectional area and the wetted perimeter, determine the hydraulic radius by...
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

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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Related Experiment Video

Updated: May 21, 2026

Trajectory Data Analyses for Pedestrian Space-time Activity Study
16:14

Trajectory Data Analyses for Pedestrian Space-time Activity Study

Published on: February 25, 2013

Spatiotemporal Detection and Uncertainty Visualization of Atmospheric Blocking Events.

Mingzhe Li, Peer Nowack, Bei Wang

    IEEE Transactions on Visualization and Computer Graphics
    |May 19, 2026
    PubMed
    Summary

    Atmospheric blocking events, which cause extreme weather, are now easier to detect and analyze using a new uncertainty visualization framework. This tool helps scientists understand blocking patterns and predict future climate risks.

    Related Experiment Videos

    Last Updated: May 21, 2026

    Trajectory Data Analyses for Pedestrian Space-time Activity Study
    16:14

    Trajectory Data Analyses for Pedestrian Space-time Activity Study

    Published on: February 25, 2013

    Area of Science:

    • Meteorology
    • Climate Science
    • Data Visualization

    Background:

    • Atmospheric blocking events are high-pressure systems causing prolonged extreme weather.
    • Accurate modeling and analysis of these events in long-term records are challenging.

    Purpose of the Study:

    • To introduce an uncertainty visualization framework for detecting and characterizing atmospheric blocking events.
    • To improve the analysis of historical blocking events and assess climate risks.

    Main Methods:

    • A geometry-based detection and tracking method was developed and tested on climate simulations (UKESM) and reanalysis data (ERA5).
    • Uncertainty-aware summaries including contour boxplots, frequency heatmaps, and 3D temporal stacks were proposed.
    • A case study of the 2003 European heatwave demonstrated the framework's application.

    Main Results:

    • The framework effectively maps the spatiotemporal occurrences of blocking events.
    • Visualizations reveal likely locations and evolving spatial footprints of blocking events.
    • Analysis of blocking frequency, duration, and intensity across regions and scenarios is supported.

    Conclusions:

    • The uncertainty visualization framework enhances the study of atmospheric blocking events.
    • It provides valuable insights for climate scientists and meteorologists in understanding extreme weather.
    • The tool aids in assessing climate risks associated with changes in blocking patterns.