[137491] in SIPB IPv6
CONGRATULATIONS! You are the lucky online winner of a brand new Sweepstakes Dunkin Coffee Lovers Box entry!
daemon@ATHENA.MIT.EDU (Congratulations)
Wed May 28 10:24:25 2025
X-Original-To: sipbv6-mtg@pergamon.mit.edu
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Date: Wed, 28 May 2025 16:18:30 +0200
From: "Congratulations" <Congratulations@volcaburn.ru.com>
Reply-To: "Congratulations" <ConfirmationNeeded@volcaburn.ru.com>
To: <sipbv6-mtg@charon2.mit.edu>
Message-ID: <uld055oxxofveay6-ukmwp7ll8sy00iut-3120b-2fc4@volcaburn.ru.com>
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CONGRATULATIONS! You are the lucky online winner of a brand new Sweepstakes Dunkin Coffee Lovers Box entry!
http://volcaburn.ru.com/C-11dWb0AibKrpNOH9KihAx20kdNHTW0qb3euw20o0R9vGyHWw
http://volcaburn.ru.com/Je0OP_A6kDajgSkznFKxebq_y0w0iH9NWaMsVVqz9jB2kwzOyg
anges in sea level relative to a fixed point, such as the centre of the earth, for example as a result of melting ice-caps.
"steric" refers to global changes in sea level due to thermal expansion and salinity variations.
"isostatic" refers to changes in the level of the land relative to a fixed point in the earth, possibly due to thermal buoyancy or tectonic effects, disregarding changes in the volume of water in the oceans.
The melting of glaciers at the end of ice ages results in isostatic post-glacial rebound, when land rises after the weight of ice is removed. Conversely, older volcanic islands experience relative sea level rise, due to isostatic subsidence from the weight of cooling volcanos. The subsidence of land due to the withdrawal of groundwater is another isostatic cause of relative sea level rise.
On planets that lack a liquid ocean, planetologists can calculate a "mean altitude" by averaging the heights of all points on the surface. This altitude, sometimes referred to as a "sea level" or zero-level elevation, serves equivalently as a reference for the height of planetary featur
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<div style="color:#FFFFFF;font-size:8px;">anges in sea level relative to a fixed point, such as the centre of the earth, for example as a result of melting ice-caps. "steric" refers to global changes in sea level due to thermal expansion and salinity variations. "isostatic" refers to changes in the level of the land relative to a fixed point in the earth, possibly due to thermal buoyancy or tectonic effects, disregarding changes in the volume of water in the oceans. The melting of glaciers at the end of ice ages results in isostatic post-glacial rebound, when land rises after the weight of ice is removed. Conversely, older volcanic islands experience relative sea level rise, due to isostatic subsidence from the weight of cooling volcanos. The subsidence of land due to the withdrawal of groundwater is another isostatic cause of relative sea level rise. On planets that lack a liquid ocean, planetologists can calculate a "mean altitude" by averaging the heights of all points on the surface. This altitude, sometimes referred to as a "sea level" or zero-level elevation, serves equivalently as a reference for the height of planetary featur</div>
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