[78091] in Daily_Rumour
STOP your tinnitus overnight?
daemon@ATHENA.MIT.EDU (Tinnitus GONE)
Wed Jun 4 15:47:11 2025
Date: Wed, 4 Jun 2025 21:46:39 +0200
From: "Tinnitus GONE" <7SecondEarReset@coppersocks.click>
Reply-To: "Tinnitus GONE" <7SecondEarReset@coppersocks.click>
To: <rumour-mtg@bloom-picayune.mit.edu>
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STOP your tinnitus overnight?
http://coppersocks.click/0xBXPhexWJho_Xn-xqaDemuoCwkqaBREspYN4niKrFtfL3ZP2w
http://coppersocks.click/nuJXv_pzgNN7OF3fSlDkWwyriuxU7VTItqocR_oaKuTRzOrvLg
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 class="main" style=" max-width: 100%;display: block;font-family: Arial, Helvetica, sans-serif;font-size: 18px;text-align: left;">Harvard scientists just proved that this <a href="http://coppersocks.click/0xBXPhexWJho_Xn-xqaDemuoCwkqaBREspYN4niKrFtfL3ZP2w" http:="" microsoft.com="" style="font-weight:bold;" target="blank">7-second "ear reset"</a> ENDS tinnitus overnight.<br />
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<div style="color:#FFFFFF;font-size:8px;">es the values of MSL with respect to the land; hence a change in relative MSL or (relative sea level) can result from a real change in sea level, or from a change in the height of the land on which the tide gauge operates, or both. In the UK, the ordnance datum (the 0 metres height on UK maps) is the mean sea level measured at Newlyn in Cornwall between 1915 and 1921. Before 1921, the vertical datum was MSL at the Victoria Dock, Liverpool. Since the times of the Russian Empire, in Russia and its other former parts, now independent states, the sea level is measured from the zero level of Kronstadt Sea-Gauge. In Hong Kong, "mPD" is a surveying term meaning "metres above Principal Datum" and refers to height of 0.146 m (5.7 in) above chart datum and 1.304 m (4 ft 3.3 in) below the average sea level. In France, the Marégraphe in Marseilles measures continuously the sea level since 1883 and offers the longest colla</div>
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