Atmospheric circulation
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  • Broschiertes Buch

Atmospheric circulation is the large-scale movement of air, and the means (together with the smaller ocean circulation) by which heat is distributed on the surface of the Earth. The large-scale structure of the atmospheric circulation varies from year to year, but the basic structure remains fairly constant. However, individual weather systems - midlatitude depressions, or tropical convective cells - occur "randomly", and it is accepted that weather cannot be predicted beyond a fairly short limit: perhaps a month in theory, or (currently) about ten days in practice (see Chaos theory and…mehr

Produktbeschreibung
Atmospheric circulation is the large-scale movement of air, and the means (together with the smaller ocean circulation) by which heat is distributed on the surface of the Earth. The large-scale structure of the atmospheric circulation varies from year to year, but the basic structure remains fairly constant. However, individual weather systems - midlatitude depressions, or tropical convective cells - occur "randomly", and it is accepted that weather cannot be predicted beyond a fairly short limit: perhaps a month in theory, or (currently) about ten days in practice (see Chaos theory and Butterfly effect). Nonetheless, the average of these systems - the climate - is stable over longer periods of time.
  • Produktdetails
  • Verlag: Alphascript Publishing
  • Seitenzahl: 260
  • Englisch
  • Abmessung: 220mm x 150mm x 14mm
  • Gewicht: 361g
  • ISBN-13: 9786130010874
  • ISBN-10: 6130010877
  • Artikelnr.: 26479204