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Carbon Dioxide and Earth's Future Pursuing the ... - Magazooms

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4. Rising Sea Levels Inundating Coastal Lowl<strong>and</strong>s<br />

www.co2science.org<br />

P a g e | 43<br />

The claim: Anthropogenic-induced global warming will lead to rapidly melting polar ice sheets,<br />

rapidly rising sea levels <strong>and</strong> catastrophic coastal flooding.<br />

With respect to <strong>the</strong> melting of earth’s polar ice sheets, we begin in <strong>the</strong> Nor<strong>the</strong>rn Hemisphere<br />

with <strong>the</strong> review of Alley et al. (2005), who claimed that “<strong>the</strong> Greenl<strong>and</strong> Ice Sheet may melt<br />

entirely from future global warming,” which contention <strong>the</strong>y buttressed with <strong>the</strong> statement<br />

that “recently detected rapid ice-marginal changes contributing to sea-level rise may indicate<br />

greater ice-sheet sensitivity to warming than previously considered.” Between <strong>the</strong> periods of<br />

1993-94 <strong>and</strong> 1998-99, for example, <strong>the</strong>y report that “<strong>the</strong> ice sheet was losing 54 ± 14 gigatons<br />

per year (Gt/year) of ice, equivalent to a sea-level rise of ~0.15 mm/year,” adding that despite<br />

excess snowfall in <strong>the</strong> sou<strong>the</strong>ast in 2002 <strong>and</strong> 2003, “net mass loss over <strong>the</strong> 1997-to-2003<br />

interval was higher than <strong>the</strong> loss between 1993 <strong>and</strong> 1999, averaging 74 ± 11 Gt/year or ~0.21<br />

mm/year sea-level rise.”<br />

Just one day before Alley et al.’s paper appeared in print, however, Johannessen et al. (2005),<br />

working with satellite-altimeter data from Greenl<strong>and</strong>, reported in a Sciencexpress paper posted<br />

online that although below 1500 meters <strong>the</strong> mean change of <strong>the</strong> ice sheet height with time was<br />

a decline of 2.0 ± 0.9 cm/year over <strong>the</strong> 11-year period 1992-2003, above 1500 meters <strong>the</strong>re was<br />

a positive growth rate of fully 6.4 ± 0.2 cm/year due to snow accumulation; <strong>and</strong> averaged over<br />

<strong>the</strong> entire ice sheet <strong>the</strong> mean result was also positive, with a mean growth rate of 5.4 ± 0.2<br />

cm/year, which when adjusted for an isostatic uplift of about 0.5 cm/year yielded a mean<br />

growth rate of approximately 5 cm/year, for a total increase in <strong>the</strong> mean thickness of <strong>the</strong><br />

Greenl<strong>and</strong> Ice Sheet of about 55 cm over <strong>the</strong> 11-year period, a result that was just <strong>the</strong> opposite<br />

of that suggested by Alley et al.<br />

Then, like a pendulum changing direction yet again, came <strong>the</strong> study of Rignot <strong>and</strong><br />

Kanagaratnam (2005), who used satellite radar interferometry observations of Greenl<strong>and</strong> to<br />

detect “widespread glacier acceleration.” Calculating that this phenomenon had led to a<br />

doubling of <strong>the</strong> ice sheet’s mass deficit in <strong>the</strong> last decade <strong>and</strong>, <strong>the</strong>refore, to a comparable<br />

increase in Greenl<strong>and</strong>’s contribution to rising sea levels, <strong>the</strong>y went on to claim that as more<br />

glaciers accelerate, “<strong>the</strong> contribution of Greenl<strong>and</strong> to sea-level rise will continue to increase.”<br />

Hard on <strong>the</strong> heels of <strong>the</strong>ir paper, however, came <strong>the</strong> satellite radar altimetry study of Zwally et<br />

al. (2005), which once again sent <strong>the</strong> pendulum swinging in <strong>the</strong> opposite direction in response<br />

to <strong>the</strong>ir finding that “<strong>the</strong> Greenl<strong>and</strong> ice sheet is thinning at <strong>the</strong> margins (-42 ± 2 Gt/year below<br />

<strong>the</strong> equilibrium-line altitude) <strong>and</strong> growing inl<strong>and</strong> (+53 ± 2 Gt/year above <strong>the</strong> equilibrium-line<br />

altitude) with a small overall mass gain (+11 ± 3 Gt/year; -0.03 mm/year sea-level equivalent).”<br />

But Chen et al. (2006) soon after pushed <strong>the</strong> pendulum way back in <strong>the</strong> o<strong>the</strong>r direction with<br />

<strong>the</strong>ir Gravity Recovery <strong>and</strong> Climate Experiment (GRACE) study, wherein <strong>the</strong>y concluded that<br />

satellite-measured gravity variations suggested that <strong>the</strong> Greenl<strong>and</strong> Ice Sheet was currently<br />

disappearing at a rate of some 240 cubic kilometers per year. However, <strong>the</strong> many problems<br />

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