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

Threats to Biodiversity01:50

Threats to Biodiversity

There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
What is Natural Selection?01:32

What is Natural Selection?

Natural selection is an evolutionary process in which individuals with survival-promoting traits reproduce at higher rates. These favorable traits become more common within a population or species. Naturally selected traits initially arise via random genetic mutations. In order for selection to occur, there must be variation within a population, the trait controlling the variation must be heritable, and there must be an evolutionary advantage for variation in the trait.The Theory of Natural...
Variation in Acceleration due to Gravity near the Earth's Surface01:20

Variation in Acceleration due to Gravity near the Earth's Surface

An object's apparent weight is its weight measured by a spring balance at its location. It is different from its true weight, the force with which the Earth pulls it, because of the Earth's rotation. Mathematically, an object's apparent weight equals its true weight minus the centripetal force that keeps it in a circular motion along with the Earth's surface every 24 hours.
The difference between the true and apparent weights is proportional to the square of the Earth's angular speed. Since the...
Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Carbon-dioxide Fixation01:28

Carbon-dioxide Fixation

Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
Deep Sea Microbial Ecology01:18

Deep Sea Microbial Ecology

The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...

También podría leer

Artículos Relacionados

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

Ordenar por
Same author

Problematic situations related to social media use and competencies to prevent them: results of a Delphi study.

Scientific reports·2024
Same author

Biologically derived epicardial patch induces macrophage mediated pathophysiologic repair in chronically infarcted swine hearts.

Communications biology·2023
Same author

Assessment of carbonaceous aerosols at Mukteshwar: A high-altitude (~2200 m amsl) background site in the foothills of the Central Himalayas.

The Science of the total environment·2023
Same author

Observed coupling between air mass history, secondary growth of nucleation mode particles and aerosol pollution levels in Beijing.

Environmental science: atmospheres·2022
Same author

Size-dependent influence of NO<sub>x</sub> on the growth rates of organic aerosol particles.

Science advances·2020
Same author

Ion-induced sulfuric acid-ammonia nucleation drives particle formation in coastal Antarctica.

Science advances·2018

Video Experimental Relacionado

Updated: Jul 6, 2026

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential
14:38

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential

Published on: April 20, 2012

Alta carga de aerosoles naturales sobre las selvas boreales.

P Tunved1, H-C Hansson, V-M Kerminen

  • 1Department of Applied Environmental Science (ITM), Air Pollution Laboratory, Frescativägen 54, SE-106 91, Stockholm, Sweden. peter.tunved@itm.su.se

Science (New York, N.Y.)
|April 15, 2006
PubMed
Resumen

El bosque boreal europeo contribuye significativamente a los aerosoles atmosféricos. Las emisiones forestales crean partículas climáticamente activas, lo que afecta las estimaciones del presupuesto de radiación y los ciclos de retroalimentación climática.

Más Videos Relacionados

Synthesis and Microdiffraction at Extreme Pressures and Temperatures
07:26

Synthesis and Microdiffraction at Extreme Pressures and Temperatures

Published on: October 7, 2013

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

Videos de Experimentos Relacionados

Last Updated: Jul 6, 2026

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential
14:38

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential

Published on: April 20, 2012

Synthesis and Microdiffraction at Extreme Pressures and Temperatures
07:26

Synthesis and Microdiffraction at Extreme Pressures and Temperatures

Published on: October 7, 2013

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

Área de la Ciencia:

  • Química de la atmósfera química de la atmósfera
  • Ciencias del clima Ciencias del clima Ciencias del clima
  • Ciencias del medio ambiente Ciencias del medio ambiente.

Sus antecedentes:

  • Los aerosoles influyen significativamente en el equilibrio de radiación de la Tierra.
  • Comprender las fuentes de aerosoles es crucial para el modelado climático.
  • La contribución de aerosoles de la región boreal europea requiere más investigación.

Objetivo del estudio:

  • Investigar la región boreal europea como fuente de masa y número de aerosoles atmosféricos.
  • Establecer una relación entre las emisiones de monoterpenos y la formación de aerosoles en áreas de bajo impacto antropogénico.
  • Para cuantificar la población climáticamente relevante de aerosoles generados por los bosques.

Principales métodos:

  • Análisis de las concentraciones de masa y número de aerosol.
  • Estudios de correlación entre las emisiones de monoterpenos y la formación de aerosoles.
  • Mediciones de campo en la región boreal europea.

Principales resultados:

  • La región boreal europea se identifica como una fuente sustancial de aerosoles atmosféricos.
  • Se encontró una relación directa entre las emisiones de monoterpenos y la conversión de gas a partícula.
  • Los bosques generan 1000-2000 partículas / cm3 de tamaños climáticamente activos durante la temporada de crecimiento.

Conclusiones:

  • Los bosques boreales son importantes fuentes naturales de aerosoles climáticamente relevantes.
  • Estos hallazgos son críticos para refinar los cálculos del presupuesto de radiación atmosférica.
  • El estudio destaca la importancia de las emisiones de aerosoles biogénicos en los mecanismos de retroalimentación climática.