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dj1. Hey guys... some points to stir the pot a little.
2. ...look at these issues on a geological time scale then it appears quite different.
3. .... The media loves to sensationalize things and although sea levels have been predicted to rise by up to 10 meters, if we look a little further back in history at the Cretaceous period (144 – 65 million years ago) sea levels were 170 meters higher than today.
4. ......I think that even if humans do have some impact on the earths climate it has run its course in cycles for many millions of years before this and to try and sustain ourselves in a temperature range or sea level of what we “perceive” to be habitable is crazy. That is like trying to stop earthquakes and volcanoes from happening.
5. Thought I might add this for a balanced wholistic approach. Just a little food for thought.
Summary ;
1. stir indeed m8 lol
2. 145 million years ago to 65 million years ago - pretty difficult to compare Cretaceous and now ,
True there was (slightly) higher temp (5 deg) and (much) higher sea levels – but this needs qualification. (average ocean depth was damn all)
3. sensationalise ?
lol - you saying we might go back to the Cretaceous ? - lol - any comparison is pretty "strange" mate. eg Antarctica Australia and Africa were still joined lol. :eek3:
Also there was a massive amount of luxuriant flora – and no parking lots, nor roads
Only a few peaks of (now) Scotland were then land. Average depth of the ocean was much less. - absolutely no relevance to todays ocean floor or ocean shape.
4. The temperature then was only (about) 5 degrees hotter – about the same as IPCC scenario A1F1
5. balanced? - lol - no way we're going back to the dinosaurs ! - eg Johnny Howard
http://www.bbm.me.uk/portsdown/PH_130_Envmnt.htm
The world during the Cretaceous looked very different. Its continental arrangement was different, as was the 'flora and fauna' that survived in a very different climate.
The following discussion covers:
• The Appearance of the World
• The High Sea Level
• Climate and the High Temperature
The Appearance of the World
From space, the Cretaceous Earth looked markedly different. Although the continental arrangement was beginning to resemble that of today, an equatorial-seaway existed around the globe, dividing the land mass into Northern, and Southern, continents. Within this arrangement of continental separation by an oft-narrow seaway, Africa was still welded to South America, Antarctica and Australia were still attached to Africa, and North America and Eurasia was one.
Both the Atlantic and Indian Oceans were young and small, the Pacific = the "super-ocean"
Furthermore; there was little emergent land, little (or no) ice at the poles, and equatorial land was arid - unlike today's equatorial rainforests.
The biota was a mixture of the exotic and familiar - luxuriant green forests of now-extinct trees flourished within the Arctic Circle and dinosaurs roamed. However; flowering plants (angiosperms) were making their mark, and many marine animals, such as the crustaceans and crocodiles of the time, closely resemble those that thrive today.
The High Sea Level
Perhaps the most significant factor of the Cretaceous world was the very high sea levels. The global sea level was at its highest ever during the Cretaceous (though was very high in the preceding Jurassic, too), peaking during the Late Cretaceous around [86]Ma ago. Various estimates have suggested height increases (above today's level) of many 100's metres, and although it is now believed that many of these estimates are excessive, it is certain that the eustatic (global) sea level was well over 200m higher during the Cretaceous than it is today.
During the peak of the high sea levels, only isolated areas of the Highlands of Scotland, and possibly Wales, in the United Kingdom, were land. The rest of our island was under the warm, shallow, tropical sea that flooded much of the Eurasian continent.
…However; current estimates suggest that if all land ice were to melt (following our attempts to create another Greenhouse world), the sea levels would rise by 'only' about [80m]; so clearly other factors that affected the sea level were also at play in the Cretaceous.
The higher temperatures thus led to both more water in the oceans (dam all polar ice) , and a given mass of water occupying a greater volume; but even these could not account for the very high levels of water, for which a third explanation is required.
The third factor is the most important, and relates to tectonic processes, rather than atmospheric conditions.
During the Cretaceous, the great landmass of Pangea was breaking up,
… These new oceans were all shallow (as they resulted from land splitting apart), …
Thus, due to
• Tectonic activity and the geography of the Earth at the time reducing the capacity of the numerous but shallow ocean basins,
• The lack of polar ice because of a warmer climate, and
• thermal expansion of water in that warmer climate,
much oceanic water spilled out of the ocean basins to flood the adjacent shallow continental land.
Climate and the High Temperature
The higher temperature of the Cretaceous has already been referred to. Estimates suggest that at the beginning of the Cretaceous, the Global Mean Surface Temperature (GMST) was around 20 °C (about 5 ° hotter than today's value of 15 °C), and was about the same at the period's end - but peaked to a high of 25 °C in the Upper Cretaceous.
These high temperatures were due to the much higher level of carbon dioxide in the atmosphere at the time - which has been suggested as being 4 times as much as is in our air today.
The Cretaceous was thus an intense "Greenhouse world", and we have a long way to go before reaching those conditions.