[44319] in linux-announce channel archive
Experience Perfection: YETI's 30 oz Travel Mug Unleashed
daemon@ATHENA.MIT.EDU (Travel Mug)
Tue Dec 5 04:25:10 2023
Date: Tue, 5 Dec 2023 10:13:53 +0100
From: "Travel Mug" <TravelMug@solutionz.shop>
Reply-To: "Travel Mug" <TravelMug@solutionz.shop>
To: <linuxch-announce.discuss@charon.mit.edu>
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Experience Perfection: YETI's 30 oz Travel Mug Unleashed
http://solutionz.shop/wr5Ipdt7iCmk_r0jDGxaU-hnZP-s9zmumnpoCXHJOpGy-GDg8A
http://solutionz.shop/fyTUwiMnX2ASJt5WTkESz5yRngFwcioxxmyZw5HmAmQKybckEQ
County, on 30 November 1944, and is from the Kissi ethnic group. He is married to Kartumu Boakai and they have four children. Boakai is a Baptist and a deacon of the Effort Baptist Church.
The most important reason for the 5.3 seconds of longitude offset between the IERS Reference Meridian and the Airy transit circle is that the observations with the transit circle were based on the local vertical, while the IERS Reference is a geodetic longitude, that is, the plane of the meridian contains the center of mass of the Earth.
The International Hydrographic Organization adopted an early version of the IRM in 1983 for all nautical charts. It was adopted for air navigation by the International Civil Aviation Organization on 3 March 1989. Tectonic plates slowly move over the surface of Earth, so most countries have adopted for their maps an IRM version fixed relative to their own tectonic plate as it existed at the beginning of a specific year. Examples include the North American Datum 1983 (NAD83), the European Terrestrial Reference Frame 1989 (ETRF89), and the Geocentric Datum of Australia 1994 (GDA94). Versions fixed to a tectonic plate differ from the global version by at most a few centimetres.
The IERS system is not quite fixed to any point attached to the Earth. For example, all points on the European portion of the Eurasian plate, including the Royal Observatory, are moving northeast at about 2.5 cm per year relative to it. The IRM is the weighted average (in the least squares sense) of the reference meridians of the hundreds of ground stations contributing to the IERS network. The network includes GPS stations, satellite laser ranging
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<p style="color:#FFFFFF;font-size:8px;">The most important reason for the 5.3 seconds of longitude offset between the IERS Reference Meridian and the Airy transit circle is that the observations with the transit circle were based on the local vertical, while the IERS Reference is a geodetic longitude, that is, the plane of the meridian contains the center of mass of the Earth. The International Hydrographic Organization adopted an early version of the IRM in 1983 for all nautical charts. It was adopted for air navigation by the International Civil Aviation Organization on 3 March 1989. Tectonic plates slowly move over the surface of Earth, so most countries have adopted for their maps an IRM version fixed relative to their own tectonic plate as it existed at the beginning of a specific year. Examples include the North American Datum 1983 (NAD83), the European Terrestrial Reference Frame 1989 (ETRF89), and the Geocentric Datum of Australia 1994 (GDA94). Versions fixed to a tectonic plate differ from the global version by at most a few centimetres. The IERS system is not quite fixed to any point attached to the Earth. For example, all points on the European portion of the Eurasian plate, including the Royal Observatory, are moving northeast at about 2.5 cm per year relative to it. The IRM is the weighted average (in the least squares sense) of the reference meridians of the hundreds of ground stations contributing to the IERS network. The network includes GPS stations, satellite laser ranging</p>
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