Global energy and climate processes

dc.contributor.authorFitzharris, Blair
dc.contributor.editorSturman, A.P.
dc.contributor.editorSpronken-Smith, R.A.
dc.date.accessioned2010-04-19T20:52:20Z
dc.date.available2010-04-19T20:52:20Z
dc.date.issued2001en
dc.description.abstractThe global climate system is driven by energy, almost all of which comes from the Sun. In this chapter, variations in the Sun-Earth relationship, which create spatial and temporal variations in the receipt of solar radiation over Earth's surface, are examined. Imbalances in energy inputs and outputs lead to massive transfers of energy in both the atmosphere and oceans. These factors control the nature of climate and lead to very distinctive climates in different regions of the world. To understand New Zealand's climate, it is necessary to first take a global view of the climate system of Earth.en
dc.identifier.citationFitzharris, Blair (2001) Global energy and climate processes. In Sturman, A.P. and Spronken-Smith, R. A. (Ed.). The Physical Environment: A New Zealand Perspective (pp. 113-129). Melbourne: Oxford University Press.en
dc.identifier.isbn978-0-19-558395-3
dc.identifier.urihttp://hdl.handle.net/10092/3765
dc.language.isoen
dc.publisherOxford University Pressen
dc.publisherUniversity of Canterbury. Geographyen
dc.rights.urihttps://hdl.handle.net/10092/17651en
dc.subject.marsdenFields of Research::260000 Earth Sciencesen
dc.subject.marsdenFields of Research::260000 Earth Sciences::260600 Atmospheric Sciences::260602 Climatology (incl. palaeoclimatology)en
dc.titleGlobal energy and climate processesen
dc.typeChapters
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