Climate swings and roundabouts
Carter, Robert M. (2008) Climate swings and roundabouts. In: A Continent on the Move: New Zealand geoscience into the 21st century. Geological Society of New Zealand, Wellington, New Zealand, pp. 249-278.
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Earth receives more solar radiation per unit area at the equator than at the poles. The resulting imbalance in heat energy results in a vigorous fluid circulation in both the atmosphere and oceans, redistributing the heat around the planet. Heat is transferred via the atmosphere, which mixes globally on a one-year timeframe, and via ocean circulation, which mixes globally on a thousand-year timeframe. Natural climate change, therefore, needs to be considered over timeframes of at least several thousand years. The longest useful series of instrumental weather measurements, from Europe, is only c. 200 years long, so researchers into past climate change must look to long term geological records which, fortunately, Zealandia has in abundance.
|Item Type:||Book Chapter (Research - B1)|
This publication does not have an abstract. The first paragraph of the Introduction is displayed as the abstract.`
|FoR Codes:||04 EARTH SCIENCES > 0406 Physical Geography and Environmental Geoscience > 040699 Physical Geography and Environmental Geoscience not elsewhere classified @ 100%|
|SEO Codes:||97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%|
|Deposited On:||28 Jan 2010 11:03|
|Last Modified:||01 May 2013 18:03|
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