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Government Comments on the Final Draft of the SPM IPCC Working ...

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<str<strong>on</strong>g>Government</str<strong>on</strong>g> <str<strong>on</strong>g>Comments</str<strong>on</strong>g> <strong>on</strong> <strong>the</strong> <strong>Final</strong> <strong>Draft</strong> <strong>of</strong> <strong>the</strong> <strong>SPM</strong><br />

<strong>IPCC</strong> <strong>Working</strong> Group I Fourth Assessment Report<br />

Batch<br />

Page:line<br />

No.<br />

From To Comment<br />

is more than double <strong>the</strong> (9 cm) low estimate from <strong>the</strong> TAR.<br />

[Govt. <strong>of</strong> United States <strong>of</strong> America (Reviewer’s comment ID #: 2023-75)]<br />

<strong>SPM</strong>-734 A 11:29 11:30 Sentence that reads “Smaller assessed uncertainties in glacier and ice cap changes also c<strong>on</strong>tribute to a reduced upper bound” is<br />

awkwardly worded. Suggest instead something like “An improved knowledge base about glacier and ice cap changes have<br />

enabled uncertainties in this area to be reduced, which has also c<strong>on</strong>tributed to a reducti<strong>on</strong> in <strong>the</strong> upper bound for SLR<br />

projecti<strong>on</strong>s.”<br />

[Govt. <strong>of</strong> Canada (Reviewer’s comment ID #: 2004-52)]<br />

<strong>SPM</strong>-735 A 11:29 11:30 Suggest replacing <strong>the</strong> sentence "Smaller assessed uncertainties in glacier and ice cap7changes also c<strong>on</strong>tribute to a reduced<br />

upper bound" as it is not clear that it is correct. A possible expanded reformulati<strong>on</strong> would be: "Compared to <strong>the</strong> TAR a<br />

smaller estimate <strong>of</strong> <strong>the</strong> c<strong>on</strong>tributi<strong>on</strong> <strong>of</strong> glacier and ice caps has been made due to methodological improvements and changes,<br />

however large uncertainties remain in relati<strong>on</strong> to <strong>the</strong> global mass balance sensitivity, <strong>the</strong> total volume <strong>of</strong> ice and <strong>the</strong><br />

c<strong>on</strong>tributi<strong>on</strong> <strong>of</strong> glacier and ice caps around Greenland and Antarctica, which account for about half <strong>of</strong> <strong>the</strong> total ice volume <strong>of</strong><br />

G&IC. The c<strong>on</strong>tributi<strong>on</strong> <strong>of</strong> <strong>the</strong>se latter glaciers has been limited to a fixed fracti<strong>on</strong> (20%) <strong>of</strong> <strong>the</strong> calculated melting <strong>of</strong> G&IC<br />

outside <strong>of</strong> <strong>the</strong> ice sheet peripheries, although it is likely that melt and discharge rate from <strong>the</strong>se would increase with time<br />

during <strong>the</strong> 21st century as is already evidenced from <strong>the</strong> Antarctic Peninsula and fringing glaciers <strong>of</strong> <strong>the</strong> Greenland ice sheet”.<br />

Reas<strong>on</strong> 1) Global mass balance sensitivity: - this has been tuned since <strong>the</strong> SOD to fit observati<strong>on</strong>s as <strong>the</strong> model based<br />

estimates were far too low and remains static in <strong>the</strong> course <strong>of</strong> <strong>the</strong> 21st century. Model based estimates <strong>of</strong> this factor are 0.36 ±<br />

0.14 mm yr–1 K–1, regressi<strong>on</strong> against data to <strong>the</strong> 1990s gives 0.65 ± 0.40 mm yr -1 K-1 and over recent decade ~0.8 mm yr–1<br />

K–1 (Chapter 10 SOD pages 57-58) and final used is 0.80 ± 0.33 mm yr–1 K–1 .There is evidence <strong>of</strong> an increasing sensitivity<br />

in recent decades. It is noted in Chapter 10 that <strong>the</strong>re is a substantial difference between model based estimates and<br />

observati<strong>on</strong>s and that "The current state <strong>of</strong> knowledge does not permit a satisfactory explanati<strong>on</strong> <strong>of</strong> <strong>the</strong> difference" .<br />

Reas<strong>on</strong> 2) The total volume <strong>of</strong> ice in all G&IC appears to be more uncertain than in <strong>the</strong> TAR which estimated a total volume<br />

<strong>of</strong> 0.5m SLE about half <strong>of</strong> which was in <strong>the</strong> periphery <strong>of</strong> <strong>the</strong> two ice sheets. The SLE volume for G&IC not immediately<br />

associated with <strong>the</strong> ice sheets is 0.15-0.37m (Table 4.3) and around <strong>the</strong> ice sheets <strong>on</strong>e estimate is given <strong>of</strong> 0.25m, giving a<br />

total range <strong>of</strong> 0.4m-0.72m. The latter estimate does not include <strong>the</strong> ice volumes <strong>of</strong> <strong>the</strong> Antarctic Peninsula, nor <strong>the</strong> fringing<br />

glaciers <strong>of</strong> East Antarctica which are dynamically disc<strong>on</strong>nected from <strong>the</strong> ice sheet (4.5.1 page 17) and can be expected to, or<br />

are already, resp<strong>on</strong>d(ing) <strong>on</strong> different timescale than <strong>the</strong> ice sheet itself.<br />

Reas<strong>on</strong> 3) The melting <strong>of</strong> ice from <strong>the</strong> peripheral ice sheets and glaciers <strong>of</strong> <strong>the</strong> ice sheets was not estimated in <strong>the</strong> TAR and<br />

here is d<strong>on</strong>e by adding 20% to <strong>the</strong> n<strong>on</strong> ice sheet related G&IC SLR estimates. There is little or no observati<strong>on</strong>al or physical<br />

basis for applying this assumpti<strong>on</strong> throughout <strong>the</strong> 21st century. On <strong>on</strong>e estimate <strong>the</strong> glaciers <strong>of</strong> <strong>the</strong> Antarctic Peninsula (4-25)<br />

are presently discharging an ice volume equivalent to about 15% <strong>of</strong> <strong>the</strong> losses from G&IC not immediately associated with <strong>the</strong><br />

ice sheets in <strong>the</strong> 1993-2003 period. Even if 20% were an appropriate fracti<strong>on</strong> now it cannot be assumed to remain c<strong>on</strong>stant<br />

and most likely would increase as polar warming extends fur<strong>the</strong>r and changes ei<strong>the</strong>r <strong>the</strong> mass balance or <strong>the</strong> dynamics <strong>of</strong> <strong>the</strong><br />

G&IC immediately associated with <strong>the</strong> ice sheets. Hence this is very likely too low an estimate. (c<strong>on</strong>tinuati<strong>on</strong> comments<br />

combined by TSU)<br />

[Govt. <strong>of</strong> Germany (Reviewer’s comment ID #: 2011-34)]<br />

<strong>SPM</strong>-736 A 11:29 11:29 Add “small” before “ice cap” and delete <strong>the</strong> callout for footnote 7.<br />

Page 80 <strong>of</strong> 99

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