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Harvard: This common household toxin triggers memory loss
daemon@ATHENA.MIT.EDU (Struggling to remember)
Wed Apr 9 10:57:32 2025
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Date: Wed, 9 Apr 2025 16:57:30 +0200
From: "Struggling to remember" <Neverforgetanything@miraclesheet.za.com>
Reply-To: "Never forget anything" <Strugglingtoremember@miraclesheet.za.com>
Subject: Harvard: This common household toxin triggers memory loss
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Harvard: This common household toxin triggers memory loss
http://miraclesheet.za.com/yxbFkqCeqtwiTYOo9H2meeNS6fSPYhM7bpa5KIhcz5gfF2cH-A
http://miraclesheet.za.com/BimeJC95qxVRY2P8eKVzkBltCgaVbwtmfIGxpwPDClXCXKqL
me of its losses are offset by the growth of the East Antarctic ice sheet, Antarctica as a whole will most likely lose enough ice by 2100 to add 11 cm (4.3 in) to sea levels. Further, marine ice sheet instability may increase this amount by tens of centimeters, particularly under high warming. Fresh meltwater from WAIS also contributes to ocean stratification and dilutes the formation of salty Antarctic bottom water, which destabilizes Southern Ocean overturning circulation.
In the long term, the West Antarctic Ice Sheet is likely to disappear due to the warming which has already occurred. Paleoclimate evidence suggests that this has already happened during the Eemian period, when the global temperatures were similar to the early 21st century. It is believed that the loss of the ice sheet would take place between 2,000 and 13,000 years in the future, although several centuries of high emissions may shorten this to 500 years. 3.3 m (10 ft 10 in) of sea level rise would occur if the ice sheet collapses but leaves ice caps on the mountains behind. Total sea level rise from West Antarct
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<div style="color:#F7F7F7;font-size:8px;">me of its losses are offset by the growth of the East Antarctic ice sheet, Antarctica as a whole will most likely lose enough ice by 2100 to add 11 cm (4.3 in) to sea levels. Further, marine ice sheet instability may increase this amount by tens of centimeters, particularly under high warming. Fresh meltwater from WAIS also contributes to ocean stratification and dilutes the formation of salty Antarctic bottom water, which destabilizes Southern Ocean overturning circulation. In the long term, the West Antarctic Ice Sheet is likely to disappear due to the warming which has already occurred. Paleoclimate evidence suggests that this has already happened during the Eemian period, when the global temperatures were similar to the early 21st century. It is believed that the loss of the ice sheet would take place between 2,000 and 13,000 years in the future, although several centuries of high emissions may shorten this to 500 years. 3.3 m (10 ft 10 in) of sea level rise would occur if the ice sheet collapses but leaves ice caps on the mountains behind. Total sea level rise from West Antarct</div>
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