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Related Concept Videos

What is Weather?01:07

What is Weather?

Overview
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...
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...
Absolute and Local Extreme Values01:22

Absolute and Local Extreme Values

The highest and lowest values of a function, relative to a reference axis, are known as extreme values. These include absolute maximum and absolute minimum values, which represent the highest and lowest points the function reaches across its entire domain. Within a restricted portion of the function, the highest and lowest values are referred to as local maximum and local minimum values, respectively.Periodic functions, such as sine and cosine, show extreme values at infinitely many points due...
Types of Coprecipitation01:10

Types of Coprecipitation

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...
Precipitation Gravimetry01:03

Precipitation Gravimetry

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...

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Related Experiment Video

Updated: May 29, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

Extreme-range precipitation probability across global weather systems.

Suqin Q Duan1, Wei-Ming Tsai1, Fiaz Ahmed1

  • 1Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, CA 90095, USA.

Science Advances
|May 27, 2026
PubMed
Summary

This study examined how different weather systems contribute to extreme rainfall events. Using high-resolution data, the researchers found that the most intense parts of precipitation distributions across major systems share a common shape. Dynamic processes largely determine this shape, while thermodynamic factors influence its strength. The study also found that the intensity of extreme rainfall from major systems is similar to that of total precipitation, suggesting a universal pattern. However, in some regions, specific systems like tropical low-pressure systems or mesoscale convective systems have a greater impact on extreme rainfall. These findings could help improve risk assessments by reducing the need for detailed weather-type identification in most areas.

Keywords:
precipitation risk modelingweather system dynamicsextreme rainfall patternsclimate modeling

Frequently Asked Questions

Related Experiment Videos

Last Updated: May 29, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

Area of Science:

  • Atmospheric dynamics and climate modeling
  • Hydrological risk assessment
  • Meteorological data analysis

Background:

Extreme rainfall events pose significant risks to communities and infrastructure, yet their prediction remains challenging. Current weather and climate models often fail to accurately represent the dynamics of precipitating systems. While some progress has been made in understanding average rainfall patterns, the behavior of extreme precipitation remains less clear. Prior research has shown that models struggle to capture the full range of precipitation intensities. This gap motivated a closer examination of how different weather systems contribute to extreme rainfall. Researchers have explored various approaches to model precipitation, but the specific role of system types in shaping extreme rainfall distributions remains unclear. A key uncertainty is whether the structure of precipitation intensity distributions is consistent across different systems. That uncertainty drove the need for high-resolution observational studies to better understand the universal characteristics of extreme precipitation.

Purpose Of The Study:

This study aimed to investigate the shape and drivers of precipitation probability distributions at the hourly scale across major weather systems globally. The specific problem addressed was the lack of clarity on whether extreme precipitation tails share a common structure across different systems. The motivation was to determine if such a universal pattern exists, which could simplify risk assessments. The researchers focused on major system types to understand their contributions to extreme rainfall. They sought to identify whether dynamic or thermodynamic factors dominate in shaping these distributions. The study also aimed to explore exceptions where certain systems disproportionately influence extreme events. By analyzing high-resolution observational data, the researchers aimed to provide insights into the universality of extreme precipitation patterns. This approach could inform more robust risk modeling without requiring detailed weather-type identification.

Main Methods:

The researchers used high-resolution observational data to analyze precipitation probability distributions at the hourly timescale. They categorized major weather system types across the globe to assess their contributions to extreme rainfall. The study focused on the high-intensity tails of these distributions to identify common patterns. Dynamic and thermodynamic factors were analyzed to determine their relative influence on the shape and magnitude of the distributions. The researchers compared the intensity scales of different system types to those of total precipitation. They examined whether shared thermodynamic environments or dynamic processes explain the observed similarities. The study also identified regions where specific systems, such as tropical low-pressure systems, had a disproportionate impact on extreme rainfall. This approach allowed the researchers to distinguish between universal patterns and system-specific anomalies.

Main Results:

The study found that the high-intensity tails of precipitation distributions across major weather systems share a typical shape. This shape can be characterized by a consistent intensity scale, indicating a universal pattern. Dynamic processes were identified as the primary driver of this universal shape. Thermodynamic factors were found to modulate the magnitude but not the overall structure of the distributions. The intensity scales of major contributing systems closely matched those of total precipitation. This similarity was attributed to shared thermodynamic environments and the dominance of intense systems. The researchers observed only modest variations in dynamic scales across different systems. Exceptions were identified in regions where tropical low-pressure systems or mesoscale convective systems disproportionately influenced extreme rainfall.

Conclusions:

The findings suggest that the shape of extreme precipitation distributions is largely governed by dynamic processes. Thermodynamic factors modulate the magnitude but not the universal structure of these distributions. The similarity in intensity scales between major systems and total precipitation supports the use of simplified risk models. This universality implies that detailed weather-type identification may not be necessary for most regions. The study highlights exceptions where specific systems, such as tropical low-pressure systems, have a disproportionate impact on extreme rainfall. These exceptions indicate that some regions may require more detailed modeling approaches. The results provide a framework for understanding the drivers of extreme precipitation across different weather systems. The researchers propose that this approach can improve risk assessments by reducing reliance on complex weather-type identification.

The high-intensity tails of precipitation distributions across major weather systems share a typical shape, which can be characterized by a consistent intensity scale.

Dynamic processes largely govern the universal shape of extreme precipitation distributions, while thermodynamic factors modulate their magnitude.

The similarity is due to shared thermodynamic environments, dominance of intense systems, and modest variations in dynamic scales.

Tropical low-pressure systems can disproportionately affect extreme precipitation, leading to gray-swan-prone distributions in certain regions.

Mesoscale convective systems can co-occur with other systems to disproportionately affect extreme rainfall in some regions.

The study supports risk assessment without overly depending on weather-type identification for most regions, simplifying modeling approaches.