A Return to Phanerozoic Average Sea Level?

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SUMMARY

The forum discussion centers on the potential return to average sea levels akin to those during the Phanerozoic era, with a focus on the implications of natural geological processes versus anthropogenic effects. Participants debate the origins of significant sea level changes, particularly the Meltwater Pulse 1A, and the contributions of various ice sheets, including the Antarctic and North American ice sheets. Key references include the work of Weaver et al. (2003) and discussions on isotopic evidence from benthic foraminifera, which suggest complexities in correlating sea level rise with historical climate events.

PREREQUISITES
  • Understanding of Meltwater Pulse 1A and its implications for sea level rise.
  • Familiarity with isotopic analysis in paleoclimatology, particularly benthic foraminifera.
  • Knowledge of the Phanerozoic geological time scale and its significance in earth sciences.
  • Awareness of the contributions of major ice sheets, including the Antarctic and Laurentide ice sheets, to historical sea level changes.
NEXT STEPS
  • Research the Meltwater Pulse 1A and its impact on global sea levels.
  • Study the isotopic composition of benthic foraminifera and its relevance to paleoclimate reconstructions.
  • Examine the geological history of the Phanerozoic era for insights into sea level fluctuations.
  • Investigate the role of various ice sheets in historical climate change, focusing on the Antarctic and North American contributions.
USEFUL FOR

Geologists, paleoclimatologists, environmental scientists, and anyone interested in understanding the historical dynamics of sea level changes and their implications for future climate scenarios.

  • #31
Interesting thread, thank you. Sadly I lack the ability to extract the information I think I need and suspect it may be in the energy graphs above. So, if I may, I would like to ask a very hypothetical question:

Assuming current global energy levels are in balance, would it be possible to calculate, as a "forcing", the amount of energy needed to melt 96,983.8 cubic miles of ice and what would be the shortest timescale to achieve this?

Apologies if this is off topic or the wrong thread. The reason I ask is the many predictions of sea level rise being touted in the media. The latest, I read today, claimed the WWF is forecasting a 1 meter sea level rise in the next 10 years.

The ice figure above is my calculation ignoring the extra that would be required to fill low coastal areas. I am also assuming that ice already in the sea is not included. The melt must come from continental ice on Greenland and Antarctica. This also means the melt energy is provided by the atmosphere only.

I attempted to use the following:

The isothermal melting of ice requires some 334 kilojoules per kilogram at 273.16 K. At lower temperatures, it requires an average of some 2 kilojoules per degree more.

I calculated the total energy required and divided by ten to get the annual energy then divided that into the area of the planet to get watts per square meter. Problem is I am not sure I am going about this correctly. Also air melts ice from the top down, there is a limited contact area which I feel would have some effect on slowing down the energy transfer into the ice. How this would effect the timescale is beyond me.

Any thoughts or advice welcome.

Richard
 
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  • #32
Okay then. Here are the results of my calculations. I use the timescale of 10 years as this was the forecast from the WWF.

Using the value of 334 kilojoules per kilogram at 273.16 K to melt 96,983.8 cubic miles of ice I arrive at a figure of
382,216,079,803,280.4 joules per second to melt the ice over ten years.

This equates to a "forcing" of 0.75 watts per square meter. How this energy will be delivered to the ice in the required timescale I have no idea.
 

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