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Herausgeber: 
  • Kevin E. Trenberth
  • Lennart Bengtsson
  • Robert Kandel
  • Claus Fröhlich
  • Roger-Maurice Bonnet
  • Jost Heintzenberg
  • Symeon Koumoutsaris
  • Brian Soden
  • Richard P. Allan
  • Paul Ingmann
  • Norman G. Loeb
  • Observing and Modeling Earth's Energy Flows 
     

    (Buch)
    Dieser Artikel gilt, aufgrund seiner Grösse, beim Versand als 3 Artikel!


    Übersicht

    Auf mobile öffnen
     
    Lieferstatus:   Auf Bestellung (Lieferzeit unbekannt)
    Veröffentlichung:  August 2016  
    Genre:  Naturwissensch., Medizin, Technik 
     
    Atmospheric Sciences / B / Climatology / Earth Sciences / Earth System Sciences / Electrical Engineering / Electrical Power Engineering / ENERGY / Energy technology & engineering / Energy, general / environmental science, engineering & technology / Geophysics / Geophysics/Geodesy / Meteorology & climatology / Physical geography / Physics and Astronomy / Solid Earth Sciences
    ISBN:  9789401779708 
    EAN-Code: 
    9789401779708 
    Verlag:  Springer Nature EN 
    Einband:  Kartoniert  
    Sprache:  English  
    Serie:  #41 - Space Sciences Series of ISSI  
    Dimensionen:  H 235 mm / B 155 mm / D  
    Gewicht:  1004 gr 
    Seiten:  484 
    Zus. Info:  Previously published in hardcover 
    Bewertung: Titel bewerten / Meinung schreiben
    Inhalt:
    This book provides a comprehensive presentation of Earth's energy flows and their consequences for the climate. The Earth's climate as well as planetary climates in general, are broadly controlled by three fundamental parameters: the solar irradiance, the planetary albedo and the planetary emissivity. Space measurements indicate that these three quantities are remarkably stable. A minor decrease in planetary emissivity is consistent with theoretical calculations. This is due to the ongoing increase of atmospheric greenhouse gases making the atmosphere more opaque to long wave terrestrial radiation. As a consequence radiation processes are slightly out of balance as less heat is leaving the Earth in the form of thermal radiation than the incoming amount of heat from the sun. Present space-based systems cannot yet satisfactorily measure this imbalance, but the effect can be inferred from the measurements of the increase of heat in the oceans. Minor amounts of heat are also used to melt ice and to warm the atmosphere and the surface of the Earth. 

    The book brings to fore the complexity of feedback processes of the Earth's climate system and in particular the way clouds and aerosols affect the energy balance both directly and indirectly through feed-back loops driven by the dynamics of atmospheric, ocean and land surface processes. The book highlights recent scientific progress as well as remaining challenges.

    Previously published in Surveys in Geophysics, Volume 33, Nos. 3-4, 2012

      



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