Verlag: Ginn & Co., London, 1971
ISBN 10: 0602216729 ISBN 13: 9780602216726
Anbieter: Left On The Shelf (PBFA), Kendal, Vereinigtes Königreich
Verbandsmitglied: PBFA
EUR 5,97
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In den WarenkorbPamphlet. Zustand: Good. 63pp Manchester Economics Project.
Sprache: Englisch
Verlag: D. Reidel Publishing Company, 2013
ISBN 10: 9400969562 ISBN 13: 9789400969568
Anbieter: Revaluation Books, Exeter, Vereinigtes Königreich
EUR 91,59
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In den WarenkorbPaperback. Zustand: Brand New. 532 pages. 9.61x6.14x1.21 inches. In Stock.
Sprache: Englisch
Verlag: Dordrecht, Springer Netherlands, 1983
ISBN 10: 9027713642 ISBN 13: 9789027713643
Anbieter: Antiquariat Bookfarm, Löbnitz, Deutschland
Hardcover. 521 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. AB-8925 9027713642 Sprache: Englisch Gewicht in Gramm: 1550.
Taschenbuch. Zustand: Neu. Variations in the Global Water Budget | F. A. Street-Perrott (u. a.) | Taschenbuch | 532 S. | Englisch | 2011 | Routledge | EAN 9789400969568 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.
Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - R.E. Newell President, International Commission on Climate International Association of Meteorology and Atmospheric Physics Water is the active ingredient in the global climatic system, its physical properties ensuring that it plays a major role. Its high thermal capacity provides a mechanism for moderating mid latitude winter temperatures; solar energy is absorbed by the surface layers of the middle latitude oceans in summer and is released to the atmosphere in winter as the ocean cools. The variation of saturation vapour pressure with temperature is the factor which causes oceanic surface temperatures at low latitudes to be limited by evaporation to values near 29°C, thereby limiting tropical marine air temperatures to about the same value. The substantial amount of energy involved in phase changes - the latent heat - governs the passage of solar energy to the atmo sphere; visible solar radiation is absorbed at the Earth's surface, energy is supplied to evaporate water and the latent heat is released to the atmosphere when and where condensation occurs, which is often a considerable distance from the source of the moisture. The infrared radiative characteristics of water vapour, namely the broad vibration-rotation bands typical of a triatomic molecule, permit it to act as the principal agent of energy loss from the atmosphere, throu ,h infrared radiation to space.