Sprache: Englisch
Verlag: Berlin/Heidelberg, Springer, 2004
ISBN 10: 3540203532 ISBN 13: 9783540203537
Anbieter: Antiquariat Smock, Freiburg, Deutschland
Erstausgabe
Zustand: Sehr gut. Formateinband: illustrierter Pappband / gebundene Ausgabe XV, 304 S. (24 cm) 1st Edition; Sehr guter Zustand. Sprache: Englisch Gewicht in Gramm: 700 [Stichwörter: Computermodellierung in den Atmosphären- und Ozeanwissenschaften].
Anbieter: Ria Christie Collections, Uxbridge, Vereinigtes Königreich
EUR 115,13
Anzahl: Mehr als 20 verfügbar
In den WarenkorbZustand: New. In.
Anbieter: Revaluation Books, Exeter, Vereinigtes Königreich
EUR 153,59
Anzahl: 2 verfügbar
In den WarenkorbHardcover. Zustand: Brand New. 1st edition. 350 pages. 9.25x6.25x0.75 inches. In Stock.
Sprache: Englisch
Verlag: Springer Berlin Heidelberg, Springer Berlin Heidelberg, 2004
ISBN 10: 3540203532 ISBN 13: 9783540203537
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Computer modeling pervades today all fields of science. For the study of com plex systems, such as the environment, it has become an indispensable tool. But it is also a tool that is often misunderstood and misinterpreted. These dangers are particularly pronounced in the environmental sciences, an area of interest and concern not only to scientists, but also to the general public, the media, policy makers and powerful interest groups. We cannot experiment with our planet. The only quantitative tool available for the assessment of the impact of our actions today on the future environment and living conditions of later generations is numerical modeling. The better the general understanding of the potential and limitations of numerical models, the better the chances for a rational analysis and discussion of environmental problems and poli cies. But in addition to the more recent political issue of human impacts on the environment, numerical models play an important role for the forecasting of natural environmental variability, such as tides and storm surges or the weathcr, or for the interpretation of environmental changes in the past, such as the relation between the Late Maunder Minimum of the sunspot cycle from 1675 to 1710 and the winter half year cooling at the end of the 17th century. The reasons for misunderstandings and misinterpretations of numerical model results are manifold.