Related Experiment Video
Updated: May 1, 2026

08:20
In Situ Soil Moisture Sensors in Undisturbed Soils
Published on: November 18, 2022
8.3K
Uncertain dynamic response of mid-latitude winter precipitation
Lei Gu1,2, Dominik L Schumacher3, Sebastian Sippel4
1Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland. lei.gu@physics.ox.ac.uk.
Nature
|April 29, 2026
Summary
Climate models accurately simulate precipitation
Area of Science:
- Climate Science
- Atmospheric Science
- Meteorology
Background:
- Precipitation changes are critical for human societies and ecosystems.
- Observed and simulated precipitation trends show discrepancies, particularly in the Northern Hemisphere winter.
- Existing research suggests climate models may underestimate precipitation responses to human activities.
Purpose of the Study:
- To disentangle the thermodynamic and dynamic components of anthropogenic forcing and internal variability in winter precipitation trends.
- To investigate the contribution of these components to discrepancies between observed and simulated precipitation patterns.
- To assess the role of dynamic circulation changes in regional winter precipitation trends.
Main Methods:
- Analysis of winter precipitation trends from 1950-2022.
- Decomposition of precipitation trends into forced thermodynamic, forced dynamic, and internal variability components.
- Comparison of observed trends with climate model simulations, focusing on the Mediterranean region.
Main Results:
- Climate models broadly reproduce the thermodynamic component of precipitation changes but show substantial divergence in the dynamic component.
- In the Mediterranean, the simulated forced dynamic signal explains only about 10% of the observed dynamic trend, hindering detection.
- Projected circulation responses under continued emissions show intensified patterns that increasingly resemble observed trends.
Conclusions:
- While internal variability might play a role, the dynamic response of atmospheric circulation is an emerging factor in regional winter precipitation trends.
- Improving the representation of forced large-scale circulation responses in climate models is essential for enhancing confidence in regional precipitation projections.
- Further research is needed to fully understand and accurately model the dynamic drivers of precipitation change.
Related Concept Videos
Precipitation and Co-precipitation
4.8K
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...
4.8K
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...
5.0K
Types of Coprecipitation
5.5K
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...
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
5.5K
Precipitation Gravimetry
12.8K
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...
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...
12.8K
Precipitation Reactions
51.2K
In a precipitation reaction, aqueous solutions of soluble salts react to give an insoluble ionic compound – the precipitate. The reaction occurs when oppositely charged ions in solution overcome their attraction for water and bind to each other, forming a precipitate that separates out from the solution. Since such reactions involve the exchange of ions between ionic compounds in aqueous solution, they are also referred to as double displacement, double replacement, exchange reactions, or...
51.2K
What is Climate?
17.5K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
17.5K

