[137492] in SIPB IPv6
Say bye to your power bill if you own a home in these zip codes
daemon@ATHENA.MIT.EDU (Solar Savings)
Wed May 28 12:14:52 2025
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Date: Wed, 28 May 2025 17:42:18 +0200
From: "Solar Savings" <EnergyBillCruncherAdPartner@dreamease.ru.com>
Reply-To: "Solar Savings" <SaveonSolar@dreamease.ru.com>
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Say bye to your power bill if you own a home in these zip codes
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rring to geographic features such as mountains, on a topographic map variations in elevation are shown by contour lines. A mountain's highest point or summit is typically illustrated with the AMSL height in metres, feet or both. In unusual cases where a land location is below sea level, such as Death Valley, California, the elevation AMSL is negative.
Difficulties in use
Ocean
Reference ellipsoid
Local plumb line
Continent
Geoid
It is often necessary to compare the local height of the mean sea surface with a "level" reference surface, or geodetic datum, called the geoid. In the absence of external forces, the local mean sea level would coincide with this geoid surface, being an equipotential surface of the Earth's gravitational field which, in itself, does not conform to a simple sphere or ellipsoid and exhibits gravity anomalies such as those measured by NASA's GRACE satellites. In reality, the geoid surface is not directly observed, even as a long-term average, due to ocean currents, air pressure variations, temperature and salinity variations, etc. The location-dependent but time-persistent separation between local mean sea level and the geoid is referred to as (mean) ocean surface topography. It varies globally in a typical ran
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<div style="color:#FFFFFF;font-size:8px;">rring to geographic features such as mountains, on a topographic map variations in elevation are shown by contour lines. A mountain's highest point or summit is typically illustrated with the AMSL height in metres, feet or both. In unusual cases where a land location is below sea level, such as Death Valley, California, the elevation AMSL is negative. Difficulties in use Ocean Reference ellipsoid Local plumb line Continent Geoid It is often necessary to compare the local height of the mean sea surface with a "level" reference surface, or geodetic datum, called the geoid. In the absence of external forces, the local mean sea level would coincide with this geoid surface, being an equipotential surface of the Earth's gravitational field which, in itself, does not conform to a simple sphere or ellipsoid and exhibits gravity anomalies such as those measured by NASA's GRACE satellites. In reality, the geoid surface is not directly observed, even as a long-term average, due to ocean currents, air pressure variations, temperature and salinity variations, etc. The location-dependent but time-persistent separation between local mean sea level and the geoid is referred to as (mean) ocean surface topography. It varies globally in a typical ran</div>
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