Jove
Visualize
Contáctanos
JoVE
x logofacebook logolinkedin logoyoutube logo
ACERCA DE JoVE
Visión GeneralLiderazgoBlogCentro de Ayuda JoVE
AUTORES
Proceso de PublicaciónConsejo EditorialAlcance y PolíticasRevisión por ParesPreguntas FrecuentesEnviar
BIBLIOTECARIOS
TestimoniosSuscripcionesAccesoRecursosConsejo Asesor de BibliotecasPreguntas Frecuentes
INVESTIGACIÓN
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchivo
EDUCACIÓN
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualCentro de Recursos para ProfesoresSitio de Profesores
Términos y Condiciones de Uso
Política de Privacidad
Políticas

Videos de Conceptos Relacionados

Radiation: Applications01:17

Radiation: Applications

1.2K
The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
1.2K
Body Temperature01:25

Body Temperature

1.1K
The body's temperature, measured in degrees, is determined by the balance between heat production and dissipation to the surrounding environment. For instance, if exercising vigorously, the body will produce more heat, causing sweat and dissipating that heat. Despite extreme environmental conditions and physical exertion, the human temperature-control system maintains a constant core body temperature (the temperature of deep tissues, which are the tissues located beneath the skin and other...
1.1K
Global Climate Change01:50

Global Climate Change

24.6K
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.
24.6K
Conditions on Early Earth02:06

Conditions on Early Earth

94.6K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
94.6K
Thermosensation01:43

Thermosensation

30.9K
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...
30.9K
What is Climate?01:16

What is Climate?

18.7K
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.
18.7K

También podría leer

Artículos Relacionados

Artículos vinculados a este trabajo por autores compartidos, revista y gráfico de citas.

Ordenar por
Same author

Rhenium isotopes reveal enhanced rock organic carbon oxidation over the Toarcian Oceanic Anoxic Event.

Nature communications·2026
Same author

Large riverbed sediment flux sustained for a decade after an earthquake.

Nature·2025
Same author

Long term carbon export from mountain forests driven by hydroclimate and extreme event driven landsliding.

Communications earth & environment·2025
Same author

Old carbon routed from land to the atmosphere by global river systems.

Nature·2025
Same author

Current rates of CO<sub>2</sub> removal due to rock weathering in the UK.

The Science of the total environment·2024
Same author

Temperature sensitivity of the mineral permafrost feedback at the continental scale.

Science advances·2024
Same journal

Erratum for the Research Article "Detecting supramolecular organic nanoparticles during heat wave".

Science (New York, N.Y.)·2026
Same journal

Local signals, systemic decline.

Science (New York, N.Y.)·2026
Same journal

The mechanics of liver regeneration.

Science (New York, N.Y.)·2026
Same journal

Computing in a memory with physics.

Science (New York, N.Y.)·2026
Same journal

Retraction.

Science (New York, N.Y.)·2026
Same journal

Making time.

Science (New York, N.Y.)·2026
Ver todos los artículos relacionados

Video Experimental Relacionado

Updated: Aug 12, 2025

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
06:29

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment

Published on: February 27, 2021

3.6K

El termostato permanente de la Tierra

Robert G Hilton1

  • 1Department of Earth Sciences, University of Oxford, Oxford, UK.

Science (New York, N.Y.)
|January 26, 2023
PubMed
Resumen
Este resumen es generado por máquina.

El desgaste de rocas, un proceso geológico clave, está significativamente influenciado por la temperatura. Esta dependencia de la temperatura juega un papel crucial en la regulación de la Tierra

Más Videos Relacionados

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

3.0K
Manufacturing Simple and Inexpensive Soil Surface Temperature and Gravimetric Water Content Sensors
08:49

Manufacturing Simple and Inexpensive Soil Surface Temperature and Gravimetric Water Content Sensors

Published on: December 21, 2019

9.5K

Videos de Experimentos Relacionados

Last Updated: Aug 12, 2025

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
06:29

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment

Published on: February 27, 2021

3.6K
Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

3.0K
Manufacturing Simple and Inexpensive Soil Surface Temperature and Gravimetric Water Content Sensors
08:49

Manufacturing Simple and Inexpensive Soil Surface Temperature and Gravimetric Water Content Sensors

Published on: December 21, 2019

9.5K

Área de la Ciencia:

  • Ciencias de la Tierra
  • Ciencias del clima
  • Geoquímica

Sus antecedentes:

  • El desgaste de rocas es un proceso geológico fundamental que influye en la composición atmosférica.
  • La temperatura es un factor ambiental conocido que afecta las tasas de reacción química, incluidas las del clima.

Objetivo del estudio:

  • Investigar la relación cuantitativa entre la temperatura y la velocidad de desgaste de las rocas.
  • Para entender cómo el clima impulsado por la temperatura influye en la regulación climática global.

Principales métodos:

  • Análisis de los datos geológicos y climáticos existentes.
  • Modelado de los procesos químicos de desgaste bajo diferentes escenarios de temperatura.

Principales resultados:

  • Se demostró una clara correlación positiva entre la temperatura y las tasas de desgaste de las rocas.
  • Cuantificó el impacto de los mecanismos de retroalimentación climática en la estabilización del clima.

Conclusiones:

  • La velocidad de desgaste de las rocas es fuertemente dependiente de la temperatura, actuando como un importante mecanismo de dirección del clima.
  • Comprender esta relación es vital para modelar el clima con precisión y predecir el cambio climático futuro.