From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #16139 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Saturday, May 31 2025 Volume 14 : Number 16139 Today's Subjects: ----------------- Last day to Grab this BIG Promo! ["Chef Knives" Subject: Last day to Grab this BIG Promo! Last day to Grab this BIG Promo! http://coppersocks.click/DGHOdrewKkugIdD_Xn5mnLMSFjraBsNueaKFmrvKDNCCMcPk7Q http://coppersocks.click/f-qP9qqg_U_CBIXndghaR2K0WmHQbGfrqloc5IGdYG1TlaOVwA nchmark, averaged over a period of time long enough that fluctuations caused by waves and tides are smoothed out, typically a year or more. One must adjust perceived changes in LMSL to account for vertical movements of the land, which can occur at rates similar to sea level changes (millimetres per year). Some land movements occur because of isostatic adjustment to the melting of ice sheets at the end of the last ice age. The weight of the ice sheet depresses the underlying land, and when the ice melts away the land slowly rebounds. Changes in ground-based ice volume also affect local and regional sea levels by the readjustment of the geoid and true polar wander. Atmospheric pressure, ocean currents and local ocean temperature changes can affect LMSL as well. Eustatic sea level change (global as opposed to local change) is due to change in either the volume of water in the world's oceans or the volume of the oceanic basins. Two major mechanisms are currently causing eustatic sea level rise. First, shrinking land ice, such as mountain glaciers and polar ice she ------------------------------ End of alt.music.moxy-fruvous digest V14 #16139 ***********************************************