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This raises two important questions: (1) How large are the potential conflicts between regions primarily concerned with rising sea levels19 and the rates of surface air temperature?
It is uncertain, however, whether SRM can reduce climate change stressors such as sea-level rise or rates of surface air temperature change1,4,5,6.
The highest rates of surface lowering in the grounded areas surrounding TG appear to coincide with the fastest flowing ice (Fig. 1a, inset).
Studies based on rates of surface weathering in the Appalachian valleys of Pennsylvania indicate that caves at the highest elevation in the residual hills may be 2,000,000 to 3,000,000 years old.
For complete results see Supplementary Figs 2 and 3. Nonlinear eco-geomorphic feedbacks can produce increases in the rates of surface elevation gain above the historic rates as sea-level rise rate increases7,12.
Such low rates of change in the surrounding areas of slow-moving ice mean that variation in local surface mass balance is insufficient to explain the high rates of surface lowering of the fast-flowing ice4.
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Less than first power dependence of rates of surface-photocatalyzed reactions on light intensity at high photon flux is known [4, 7].
It is hypothesized that this could be due to the relative rates of surface-initiated polymerization versus conformational mobility of polymer chains anchored by one end to the surface.
Conversion rates of surface-bound C3b were more than 100-fold higher than fluid-phase C3b, confirming the requirement of a surface.
Over the last 25 years, the rate of surface warming has accelerated, amounting to the equivalent of about 3.5 degrees a century.
The variable rate of surface elevation change formulation is combined with the accelerated rate of sea-level change.
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