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	{{Infobox paper		{{Infobox paper
	\| title = Tidal Asymmetry		\| title = Tidal Asymmetry
	\| url = [http://www.naturalphilosophy.org/pdf/abstracts/~~abstracts_paperlink_7327~~.~~doc~~ Link to paper]		\| url = [http://www.naturalphilosophy.org/pdf/abstracts/abstracts_paperlink_7380.pdf Link to paper]
	\| author = [[Raymond H Gallucci]]		\| author = [[Raymond H Gallucci]]
	\| keywords = [[Tides~~]], [[~~Gravity~~]], [[Springs]], [[Earth]], [[~~Moon]]		\| keywords = [[Tides; Symmetry; Gravity; Barycenter; Moon]]
	\| published = ~~2015~~		\| published = 2016
	\| num_pages = 10		\| num_pages = 10
	}}		}}

	'''Read the full paper''' [http://www.naturalphilosophy.org/pdf/abstracts/~~abstracts_paperlink_7327~~.~~doc~~ here]		'''Read the full paper''' [http://www.naturalphilosophy.org/pdf/abstracts/abstracts_paperlink_7380.pdf here]

	==Abstract==		==Abstract==

	The Earth’s diametrically opposed, presumably symmetric, tides are due to the Moon’s differential gravitational force varying across the Earth. This is not intuitively obvious, but becomes clear when the physics is examined mathematically. The presumed symmetry is due to an approximation that holds when the radius of the affect<u>ed</u> body (e.g., the Earth) is much less than its center-to-center distance from the affect<u>ing</u> body (e.g., the Moon). The exact solution indicates an asymmetry, which becomes more pronounced as the assumption loses its applicability.		The Earth’s diametrically opposed, presumably symmetric, tides are due to the Moon’s differential gravitational force varying across the Earth. This is not intuitively obvious, but becomes clear when the physics is examined mathematically. The presumed symmetry is due to an approximation that holds when the radius of the affect<u>ed</u> body (e.g., the Earth) is much less than its center-to-center distance from the affect<u>ing</u> body (e.g., the Moon). The exact solution indicates an asymmetry, which becomes more pronounced as the assumption loses its applicability.

	[[Category:Scientific Paper]]		[[Category:Scientific Paper\|]]

	[[Category:Gravity]]		[[Category:Gravity]]
	~~[[Category:Cosmology]]~~

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2016-12-30T18:27:52Z

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{{Infobox paper
| title = Tidal Asymmetry
| url = [http://www.naturalphilosophy.org/pdf/abstracts/abstracts_paperlink_7327.doc Link to paper]
| author = [[Raymond H Gallucci]]
| keywords = [[Tides]], [[Gravity]], [[Springs]], [[Earth]], [[Moon]]
| published = 2015
| num_pages = 10
}}

'''Read the full paper''' [http://www.naturalphilosophy.org/pdf/abstracts/abstracts_paperlink_7327.doc here]

==Abstract==

The Earth’s diametrically opposed, presumably symmetric, tides are due to the Moon’s differential gravitational force varying across the Earth. This is not intuitively obvious, but becomes clear when the physics is examined mathematically. The presumed symmetry is due to an approximation that holds when the radius of the affect<u>ed</u> body (e.g., the Earth) is much less than its center-to-center distance from the affect<u>ing</u> body (e.g., the Moon). The exact solution indicates an asymmetry, which becomes more pronounced as the assumption loses its applicability.

[[Category:Scientific Paper]]

[[Category:Gravity]]
[[Category:Cosmology]]

Tidal Asymmetry - Revision history

Maintenance script: Imported from text file

Maintenance script: Imported from text file