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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.
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Los contrails reducen el rango de temperaturas diarias.

David J Travis1, Andrew M Carleton, Ryan G Lauritsen

  • 1Department of Geography and Geology, University of Wisconsin-Whitewater, Whitewater, Wisconsin 53190, USA. travisd@uww.edu

Nature
|August 9, 2002
PubMed
Resumen
Este resumen es generado por máquina.

La ausencia de estelas de aeronaves durante un período de tres días en septiembre de 2001 condujo a un aumento inusual en el rango de temperatura diaria. Esto sugiere que las estelas de condensación tienen un impacto significativo en las temperaturas regionales de la superficie.

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Área de la Ciencia:

  • Ciencias de la atmósfera Ciencias atmosféricas.
  • Ciencias del clima Ciencias del clima Ciencias del clima Ciencias del clima
  • Impactos de la aviación en la aviación.

Sus antecedentes:

  • La influencia de las pistas de condensación de las aeronaves (contrails) en las temperaturas regionales ha sido una pregunta de larga data.
  • La verificación empírica fue un desafío debido al tráfico aéreo continuo.

Objetivo del estudio:

  • Para investigar el impacto de las estelas de condensación en el rango de temperatura diurna.
  • Para cuantificar el efecto de la ausencia de estelas de condensación en las temperaturas superficiales.

Principales métodos:

  • Análisis de los datos de temperatura de la superficie durante un período de reducción del tráfico aéreo.
  • Comparación del rango de temperatura diurna antes y después del evento.

Principales resultados:

  • Se observó un aumento anómalo en el rango de temperatura diurna promedio del 11 al 14 de septiembre de 2001.
  • Este aumento se atribuye, en parte, a la ausencia de estelas de condensación.

Conclusiones:

  • Los contrails de las aeronaves afectan de manera demostrable a las temperaturas regionales de la superficie.
  • La reducción de la contracción conduce a un rango de temperatura diurna más amplio al alterar la transferencia radiativa.