Video Experimental Relacionado
Updated: Jun 14, 2026

10:28
Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
Cambios impulsados por la insolación en la circulación atmosférica durante los últimos 116.000 años en el Brasil
Francisco W Cruz1, Stephen J Burns, Ivo Karmann
1Department of Geosciences, University of Massachusetts, Amherst, 01002 Massachusetts, USA. fdacruz@geo.umass.edu
Nature
|March 4, 2005
Resumen
Los ciclos Dansgaard-Oeschger influyeron en el ciclo hidrológico tropical, impactando las precipitaciones en Brasil. Sin embargo, estos cambios climáticos a escala milenaria fueron menos dominantes que en el hemisferio norte.
Área de la Ciencia:
- Paleoclimatología Paleoclimatología
- La dinámica del clima La dinámica del clima La dinámica del clima
- Historia del clima en América del Sur Historia del clima en América del Sur
Sus antecedentes:
- Las oscilaciones de temperatura a escala milenaria, conocidas como ciclos de Dansgaard-Oeschger, fueron una señal climática dominante en el hemisferio norte durante el último período glacial.
- El alcance de la influencia del ciclo de Dansgaard-Oeschger en el hemisferio sur tropical y subtropical, en particular su ciclo hidrológico, sigue siendo incierto.
- Los cambios de insolación, impulsados por el ciclo de precesión de la Tierra, se consideran el principal forzamiento climático directo en el hemisferio sur.
Videos de Conceptos Relacionados
What is Climate?
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.
Global Climate Change
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.
Isothermal Processes
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...
Precipitation Processes
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...
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...
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...
Microbes and Climate Change
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...

