What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures

The latest climate doom paper "Sea-level rise due to polar ice-sheet mass loss during past warm periods" uses inaccurate proxies of sea levels and temperatures of past periods to conclude that even without any further increase of temperatures we could have soon sea level rises of 6-9 metre...

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Main Author: Parker, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Institute of Science 2015
Subjects:
Online Access:https://researchonline.jcu.edu.au/42833/1/What%20If%20Sea%20Levels%20Could%20Have%20Been%206-9%20Metres.pdf
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spelling ftjamescook:oai:researchonline.jcu.edu.au:42833 2023-09-05T13:13:35+02:00 What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures Parker, A. 2015-11 application/pdf https://researchonline.jcu.edu.au/42833/1/What%20If%20Sea%20Levels%20Could%20Have%20Been%206-9%20Metres.pdf unknown American Institute of Science https://researchonline.jcu.edu.au/42833/ https://researchonline.jcu.edu.au/42833/1/What%20If%20Sea%20Levels%20Could%20Have%20Been%206-9%20Metres.pdf Parker, A. (2015) What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures. Physics Journal, 1 (3). pp. 281-289. open Article PeerReviewed 2015 ftjamescook 2023-08-22T20:15:54Z The latest climate doom paper "Sea-level rise due to polar ice-sheet mass loss during past warm periods" uses inaccurate proxies of sea levels and temperatures of past periods to conclude that even without any further increase of temperatures we could have soon sea level rises of 6-9 metres. The paper ignores the evidence that the global temperatures are not warming over this century, as the global sea levels are nor significantly rising nor accelerating, and the Antarctic sea ice growth has ultimately outpaced the Arctic sea ice shrinking, while the carbon and hydrocarbon fuel usage has been further escalating, suggesting a decoupling between the three parameters and the carbon emission. In soccer, the intergovernmental players inadvertently strike the ball into their own team's goal. If with temperatures claimed as of today and about same carbon dioxide concentrations of 1890 the sea levels have been 6-9 metres higher 125,000 years ago, because parts of the Antarctic and the Greenland ice sheets have melted for other reasons than global warming, this does not mean we should try harder to change the climate by supporting not working renewable energies and paying carbon taxes. Preferably, we should do just nothing different from using our natural resources without feeling guilty for something it does not depends on us to achieve about same result. Sea levels may rise of up to 6-13 metres, or even fall, and even if the science of climate is settled we haven't understood yet why. Article in Journal/Newspaper Antarc* Antarctic Arctic Global warming Greenland Ice Sheet Sea ice James Cook University, Australia: ResearchOnline@JCU Antarctic Arctic Greenland The Antarctic
institution Open Polar
collection James Cook University, Australia: ResearchOnline@JCU
op_collection_id ftjamescook
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description The latest climate doom paper "Sea-level rise due to polar ice-sheet mass loss during past warm periods" uses inaccurate proxies of sea levels and temperatures of past periods to conclude that even without any further increase of temperatures we could have soon sea level rises of 6-9 metres. The paper ignores the evidence that the global temperatures are not warming over this century, as the global sea levels are nor significantly rising nor accelerating, and the Antarctic sea ice growth has ultimately outpaced the Arctic sea ice shrinking, while the carbon and hydrocarbon fuel usage has been further escalating, suggesting a decoupling between the three parameters and the carbon emission. In soccer, the intergovernmental players inadvertently strike the ball into their own team's goal. If with temperatures claimed as of today and about same carbon dioxide concentrations of 1890 the sea levels have been 6-9 metres higher 125,000 years ago, because parts of the Antarctic and the Greenland ice sheets have melted for other reasons than global warming, this does not mean we should try harder to change the climate by supporting not working renewable energies and paying carbon taxes. Preferably, we should do just nothing different from using our natural resources without feeling guilty for something it does not depends on us to achieve about same result. Sea levels may rise of up to 6-13 metres, or even fall, and even if the science of climate is settled we haven't understood yet why.
format Article in Journal/Newspaper
author Parker, A.
spellingShingle Parker, A.
What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
author_facet Parker, A.
author_sort Parker, A.
title What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
title_short What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
title_full What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
title_fullStr What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
title_full_unstemmed What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
title_sort what if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures
publisher American Institute of Science
publishDate 2015
url https://researchonline.jcu.edu.au/42833/1/What%20If%20Sea%20Levels%20Could%20Have%20Been%206-9%20Metres.pdf
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genre Antarc*
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Global warming
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genre_facet Antarc*
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op_relation https://researchonline.jcu.edu.au/42833/
https://researchonline.jcu.edu.au/42833/1/What%20If%20Sea%20Levels%20Could%20Have%20Been%206-9%20Metres.pdf
Parker, A. (2015) What if sea levels could have been 6-9 metres higher 125,000 years ago with same global temperatures. Physics Journal, 1 (3). pp. 281-289.
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