Related Experiment Video
Updated: Dec 26, 2025

06:10
Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
1.4K
Global lake thermal regions shift under climate change.
Stephen C Maberly1, Ruth A O'Donnell2, R Iestyn Woolway3
1UK Centre for Ecology & Hydrology, Lancaster Environment Centre, Lancaster, LA1 4AP, UK. scm@ceh.ac.uk.
Nature Communications
|March 8, 2020
Summary
Scientists defined nine global lake thermal regions using satellite data. Climate change may shift many lakes to warmer regions, impacting lake ecology and research.
Area of Science:
- * Limnology and climate science.
- * Global aquatic ecosystem analysis.
Background:
- * Lake temperature is a key ecological factor, but predicting its variations is difficult without a thermal classification system.
- * Existing global patterns do not fully capture lake thermal dynamics.
Purpose of the Study:
- * To establish an objective, globally applicable lake thermal classification system.
- * To project future shifts in lake thermal regions under different climate change scenarios.
Main Methods:
- * Objective analysis of seasonal surface temperature dynamics from satellite observations.
- * Application of a lake model driven by 21st-century climate projections (Representative Concentration Pathways 2.6, 6.0, and 8.5).
Main Results:
- * Identification of nine distinct, globally contiguous lake thermal regions.
- * Projected shifts in lake thermal regions by 2080-2099: 12% (low), 27% (medium), and 66% (high greenhouse gas scenarios).
- * A potential 79% reduction in the northernmost thermal region under high emissions.
Conclusions:
- * The new thermal region framework provides unique insights into global lake thermal patterns.
- * Climate change is projected to significantly alter lake thermal regimes worldwide.
- * This classification system can advance global lake research and ecological predictions.
Related Concept Videos
Global Climate Change
28.4K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
28.4K
What is Climate?
20.3K
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.
20.3K
Thermal Expansion
5.4K
The expansion of alcohol in a thermometer is one of many commonly encountered examples of thermal expansion, which is the change in size or volume of a given system as its temperature changes. The most visible example is the expansion of hot air. When air is heated, it expands and becomes less dense than the surrounding air, which then exerts an upward force on the hot air to, for example, make steam and smoke rise, and hot air balloons float. The same behavior happens in all liquids and gases,...
5.4K
Isothermal Processes
4.7K
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
4.7K
Temperature Dependent Deformation
327
In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added...
327
Effects of Temperature on Free Energy
27.8K
The spontaneity of a process depends upon the temperature of the system. Phase transitions, for example, will proceed spontaneously in one direction or the other depending upon the temperature of the substance in question. Likewise, some chemical reactions can also exhibit temperature-dependent spontaneities. To illustrate this concept, the equation relating free energy change to the enthalpy and entropy changes for the process is considered:
27.8K

