Bigg, Grant and Hanna, Edward (2016) Impacts and effects of ocean warming on the weather. In: Explaining ocean warming : causes, scale, effects and consequences. IUCN (International Union for Conservation of Nature), pp. 359-372. ISBN 9782831718064
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Item Type: | Book Section |
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Item Status: | Live Archive |
Abstract
The heat content of the upper 700 m of the global ocean is ~ 120x1021 J higher than in 1995, the equivalent of
~ 240 times the human global energy consumption in 2013.
• Since the 1990s the atmosphere in the polar regions has been warming at about twice the average rate of
global warming.
• There is likely to be further major loss, and possibly the essential removal in some years, of summer Arctic sea
ice in the next 5-15 years.
• The extent of Antarctic sea ice has been growing at a rate of ~1.3% per decade, although there is strong
interannual variability.
• Over the last 20 years there has been a distinct change in the El Niño events, with a shift of the mean location
of sea surface temperature anomalies towards the central Pacific.
• There has been an increase in the number of severe hurricanes (Saffir-Simpson scale 3-5) at a rate of ~ 25-30%
per o
C of global warming.
• There has been an increase in storm surges along Arctic coasts, leading to more frequent inundation of fragile
coastal ecosystems.
• There have been significant increases in iceberg numbers in the ocean since the 1990s.
• There is likely to be an increase in mean global ocean temperature of 1-4o
C by 2100.
• Due to increased stratification of the ocean, the global Meridional Circulation is likely to decline over the next
century, although there is not a consensus as to the rate.
• Uncertainty about the future of most large-scale ocean-atmosphere teleconnections under greenhouse
warming is ubiquitous.
Keywords: | ocean, global warming, climate change |
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Subjects: | F Physical Sciences > F332 Marine Physics |
Divisions: | College of Science > School of Geography |
Related URLs: | |
ID Code: | 26479 |
Deposited On: | 01 Mar 2017 15:36 |
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