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Since Pomeranian Phase - 17 - 16 ka BP (Marks, et al., 2016) up to Gardno Phase - 16.8 - 16.6 ka BP (Marks, 2002) ~ f4(x)
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Averaged pace:
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Averaged pace:
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"Development dynamics between SB - Słupsk Bank Phase - 16.2 - 15.8 ka BP ~ f5(x), and SMB - Southern Middle Bank Phase - 15.4 - 15.0 ka BP ~ f6(x)"
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Averaged pace:
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Inequalities defining the areas between the successive face of the ice sheet deglaciation phases / coastline locations.
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Averaged development pace between Southern Middle Bank Phase and Baltic Ice Lake
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Averaged development pace between Baltic Ice Lake and Yoldia Sea
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Averaged development pace between Yoldia Sea and Ancylus Lake
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Averaged development pace between Ancylus Lake and Littorina Sea 2
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Averaged development pace between Littorina Sea 2 and Littorina Sea
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Averaged development pace between Littorina Sea and current coastline
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Results in the form of an average rate of development dynamics between individual phases.
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Nested table of the shift dynamics in the time function [m/year].
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Forecast, +6m scenario, when i.e. 90% of the Greenland ice melts down.
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Adjustable time scale, GMSL rise may exceed 5m in ca. 3000 years time according to RCP8.5 scenario (Oppenheimer et al., 2019), or in ca. 4000 years based on 0.15 m rise during last 100 years (mareograph in Gdańsk, IMGW data).
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Forecast of the future morphodynamics rate [m/year] for + 6 m a.s.l. scenario.
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Area = [A_JG1 - B_JG1] + [C_JG1 - D_JG1]
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Erosion dynamics since 8000 b2k, 3600 m along the coast in Jastrzebia Góra region (S1)
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Erosion dynamics since 8000 b2k, 734 m along the coast in the Gdynia Orłowo Cliff (S2) area:
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Split functions for Gdynia ~8ka b2k [y25A, y25B]
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Split functions for Gdynia ~ b2k (-50 a BP) [y26A, y26B]
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Split functions ~ Gdynia Orlowo Cliff (GOC) ~ TRANSFORMED data
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GOC ~8ka b2k [y27A, y27B, y27C]
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GOC ~b2k (-50 a BP)
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split functions for GOC ~b2k (-50 BP)
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Dynamics of GOC since ~8000 b2k to ~btk
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C1
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C2
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C3
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C4
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(C1+C2+C3+C4)/4
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Erosion dynamics coefficient for GOC since ~8ka b2k to b2k equals 0.11 m/year.
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...as you've reached this far, perhaps you'd find a way to support my further research?
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