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Global Climate Change01:50

Global Climate Change

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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.
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What is Climate?01:16

What is Climate?

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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.
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What is Weather?01:07

What is Weather?

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Overview
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Responses to Heat and Cold Stress02:45

Responses to Heat and Cold Stress

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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.
14.0K
Effects of Temperature on Free Energy02:11

Effects of Temperature on Free Energy

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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:
26.3K
Temperature Dependent Deformation01:12

Temperature Dependent Deformation

221
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...
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Simulating Temperature in a Soil Incubation Experiment
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Cambios generalizados en la persistencia de la temperatura superficial bajo el cambio climático

Jingyuan Li1, David W J Thompson2,3

  • 1Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA.

Nature
|November 18, 2021
PubMed
Resumen
Este resumen es generado por máquina.

El cambio climático altera significativamente la persistencia de la temperatura de la superficie, lo que afecta la duración de los eventos meteorológicos. Comprender estos cambios es crucial para los ecosistemas y la sociedad.

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Área de la Ciencia:

  • Ciencias del clima
  • Ciencias atmosféricas
  • Ciencias del medio ambiente

Sus antecedentes:

  • El cambio climático global está causando alteraciones generalizadas en los patrones de temperatura de la superficie, incluidos los aumentos medios y los cambios de variación regional.
  • El impacto de los fenómenos meteorológicos en los ecosistemas y la sociedad depende en gran medida de su duración, por lo que la persistencia de la temperatura es un factor clave.

Objetivo del estudio:

  • Investigar cómo cambia la persistencia de la temperatura superficial en respuesta al cambio climático a lo largo del siglo XXI.
  • Analizar la robustez y los factores físicos de estos cambios en la persistencia de la temperatura.

Principales métodos:

  • Utilizó la salida de 150 simulaciones en cuatro modelos distintos del sistema de la Tierra.
  • Simulaciones incorporadas de modelos simplificados con procesos radiativos variados y dinámicas a gran escala.

Principales resultados:

  • Las simulaciones de cambio climático muestran alteraciones generalizadas en la persistencia de la temperatura superficial.
  • Estos cambios son más pronunciados y robustos sobre las regiones oceánicas.
  • Un amplio espectro de procesos físicos parece impulsar estos cambios en la persistencia.

Conclusiones:

  • Los cambios generalizados en la persistencia de la temperatura de la superficie bajo el cambio climático son robustos.
  • Existe una necesidad crítica de una mejor comprensión, simulación y restricción de estos cambios de persistencia.