Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Global Climate Change01:50

Global Climate Change

29.9K
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.
29.9K
Responses to Heat and Cold Stress02:45

Responses to Heat and Cold Stress

15.9K
Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
15.9K
Microbes and Climate Change01:27

Microbes and Climate Change

65
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
65
Effects of Temperature on Free Energy02:11

Effects of Temperature on Free Energy

30.9K
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:
30.9K
Thermosensation01:43

Thermosensation

35.6K
Peripheral thermosensation is the perception of external temperature. A change in temperature (on the surface of the skin and other tissues) is detected by a family of temperature-sensitive ion channels called Transient Receptor Potential, or TRP, receptors. These receptors are located on free nerve endings. Those detecting cold temperatures are closer to the surface of the skin than the nerve endings detecting warmth. These thermoTRP channels, while temperature selective, have relatively...
35.6K
The Carbon Cycle01:14

The Carbon Cycle

45.7K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
45.7K

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same authorSame journal

Adaptation and Response in Drylands: A Dryland Research Agenda and Campaign Strategy.

Global change biology·2026
Same author

An overview of the NASA Adaptation and Response in Drylands field experiment scoping study.

Cambridge prisms. Drylands·2026
Same author

Abiotic and biotic controls of non-native perennial plant success in drylands.

Nature ecology & evolution·2026
Same author

Overestimated natural biological nitrogen fixation translates to an exaggerated CO<sub>2</sub> fertilization effect in Earth system models.

Proceedings of the National Academy of Sciences of the United States of America·2025
Same author

Drought intensity and duration interact to magnify losses in primary productivity.

Science (New York, N.Y.)·2025
Same author

Experimental warming alters free-living nitrogen fixation in a humid tropical forest.

The New phytologist·2025

Related Experiment Video

Updated: Apr 18, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

3.8K

Urgent need for warming experiments in tropical forests.

Molly A Cavaleri1, Sasha C Reed, W Kolby Smith

  • 1School of Forest Resources & Environmental Science, Michigan Technological University, 1400 Townsend Dr., Houghton, MI, 49931, USA.

Global Change Biology
|February 3, 2015
PubMed
Summary

Tropical forests are crucial for global climate, but future warming brings high uncertainty. Prioritizing manipulative warming experiments and a network of studies is vital for improving climate models and predicting forest carbon balance.

Keywords:
CMIP5carbon fluxecosystem processesglobal warmingnet ecosystem productiontemperaturetemperature thresholdtipping pointtropicswarming manipulation

More Related Videos

Resurrection of Dormant Daphnia magna: Protocol and Applications
07:37

Resurrection of Dormant Daphnia magna: Protocol and Applications

Published on: January 19, 2018

19.6K
Temperature Response of Soil Organic Matter Decomposition Rates: Construction and Applications of a Temperature Gradient Block
07:46

Temperature Response of Soil Organic Matter Decomposition Rates: Construction and Applications of a Temperature Gradient Block

Published on: January 30, 2026

522

Related Experiment Videos

Last Updated: Apr 18, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

3.8K
Resurrection of Dormant Daphnia magna: Protocol and Applications
07:37

Resurrection of Dormant Daphnia magna: Protocol and Applications

Published on: January 19, 2018

19.6K
Temperature Response of Soil Organic Matter Decomposition Rates: Construction and Applications of a Temperature Gradient Block
07:46

Temperature Response of Soil Organic Matter Decomposition Rates: Construction and Applications of a Temperature Gradient Block

Published on: January 30, 2026

522

Area of Science:

  • Climate Science
  • Ecology
  • Earth System Science

Background:

  • Tropical forests significantly impact global carbon dioxide exchange with the atmosphere.
  • Imminent unprecedented warming in the tropics presents high uncertainty regarding forest responses.
  • Existing earth system models show substantial variability in tropical carbon projections.

Purpose of the Study:

  • To prioritize research approaches for resolving uncertainties in tropical forest function.
  • To improve the predictive capacity of earth system models for tropical regions.
  • To explore the benefits and trade-offs of large-scale manipulative field experiments.

Main Methods:

  • Analysis of Coupled Model Intercomparison Project Phase 5 (CMIP5) data.
  • Comprehensive review of current scientific literature on tropical forest responses.
  • Evaluation of large-scale manipulative field experiments, including warming studies.

Main Results:

  • Model variability in projected net ecosystem production is nearly three times greater in the tropics than other latitudes.
  • Manipulative warming experiments are crucial for accurate prediction of tropical forest carbon balance.
  • A network of comparable studies across environmental gradients is recommended.

Conclusions:

  • Long-term, single-factor warming experiments targeting key ecosystem components are advocated.
  • Hypothesis testing of underlying mechanisms and improved model parameterization are essential.
  • Multi-faceted research programs, considering logistical feasibility, are the most effective way forward to understand tropical forest responses to climate change.