Editing Talk:1379: 4.5 Degrees
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:::::Having just re-read the explanation after posting my comment, I can see that the article attempts to do just that. But the link provided says 110 to 770 <b>mm</b>. Isn't the millimeters? [[Special:Contributions/108.162.238.134|108.162.238.134]] 15:44, 9 June 2014 (UTC) | :::::Having just re-read the explanation after posting my comment, I can see that the article attempts to do just that. But the link provided says 110 to 770 <b>mm</b>. Isn't the millimeters? [[Special:Contributions/108.162.238.134|108.162.238.134]] 15:44, 9 June 2014 (UTC) | ||
:::::But the sea level ''would'' rise more than 60m if the expansion of the sea is taken into account. If the earth became as hot as the graph indicates, then logically the seas would expand considerably. [[User:Calebxy|Calebxy]] ([[User talk:Calebxy|talk]]) 16:04, 9 June 2014 (UTC) | :::::But the sea level ''would'' rise more than 60m if the expansion of the sea is taken into account. If the earth became as hot as the graph indicates, then logically the seas would expand considerably. [[User:Calebxy|Calebxy]] ([[User talk:Calebxy|talk]]) 16:04, 9 June 2014 (UTC) | ||
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:Cretaceous sea levels seem to have been that high, but this tends to be attributed to the shape of the ocean basins, in particular the mid-ocean ridges, rather than to the temperature. [[Special:Contributions/108.162.219.35|108.162.219.35]] 17:01, 9 June 2014 (UTC) | :Cretaceous sea levels seem to have been that high, but this tends to be attributed to the shape of the ocean basins, in particular the mid-ocean ridges, rather than to the temperature. [[Special:Contributions/108.162.219.35|108.162.219.35]] 17:01, 9 June 2014 (UTC) | ||
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:::No, it's not hyperbole at all, actually there were tropical-climate trees in polar latitudes in the northern hemisphere during parts of the Cretaceous. [[Special:Contributions/108.162.250.237|108.162.250.237]] 11:26, 15 June 2014 (UTC) | :::No, it's not hyperbole at all, actually there were tropical-climate trees in polar latitudes in the northern hemisphere during parts of the Cretaceous. [[Special:Contributions/108.162.250.237|108.162.250.237]] 11:26, 15 June 2014 (UTC) | ||
::::Citation please- everything I could find was Temperate Rain Forests (kind of like still exist in Washington State and British Columbia).[[User:Seebert|Seebert]] ([[User talk:Seebert|talk]]) 12:28, 16 June 2014 (UTC) | ::::Citation please- everything I could find was Temperate Rain Forests (kind of like still exist in Washington State and British Columbia).[[User:Seebert|Seebert]] ([[User talk:Seebert|talk]]) 12:28, 16 June 2014 (UTC) | ||
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Independent of everything else, I'm having a tough time reconciling the fact that sea level was apparently 6m or more higher during the Roman era. E.g. the roman settlements and their harbors in places like Caister and Burgh Castle in Norfolk, England? I'm not aware that England has risen 6m. Seems to me that if see levels were to rise as much as 6m we'd just be back to where things were 1600-1700 years ago. {{unsigned ip|103.22.201.239}} | Independent of everything else, I'm having a tough time reconciling the fact that sea level was apparently 6m or more higher during the Roman era. E.g. the roman settlements and their harbors in places like Caister and Burgh Castle in Norfolk, England? I'm not aware that England has risen 6m. Seems to me that if see levels were to rise as much as 6m we'd just be back to where things were 1600-1700 years ago. {{unsigned ip|103.22.201.239}} | ||
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Since I used to live next to Burgh Castle, can I point out that the castle is indeed now c6m higher than the current estuary level. The nearby town of Great Yarmouth is built on land that first appeared above the waves around 1100AD. In Roman times it was possible to sail from Burgh Castle to the castle at Caistor - that's why they were built, to defend the mouth of the estuary between them.If you look at [https://www.google.co.uk/maps/place/Acle,+Norwich,+Norfolk+NR13/@52.6213598,1.6099949,13z/data=!4m2!3m1!1s0x47d9ff1ac61e4df5:0x957c4241ca1f0de3 map] very roughly all the green was under water circa 300AD --[[Special:Contributions/141.101.98.251|141.101.98.251]] 19:04, 1 November 2014 (UTC) | Since I used to live next to Burgh Castle, can I point out that the castle is indeed now c6m higher than the current estuary level. The nearby town of Great Yarmouth is built on land that first appeared above the waves around 1100AD. In Roman times it was possible to sail from Burgh Castle to the castle at Caistor - that's why they were built, to defend the mouth of the estuary between them.If you look at [https://www.google.co.uk/maps/place/Acle,+Norwich,+Norfolk+NR13/@52.6213598,1.6099949,13z/data=!4m2!3m1!1s0x47d9ff1ac61e4df5:0x957c4241ca1f0de3 map] very roughly all the green was under water circa 300AD --[[Special:Contributions/141.101.98.251|141.101.98.251]] 19:04, 1 November 2014 (UTC) | ||
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