The earth's motion of rotation including the theory of precession and nutation |
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Side 15
... follows from the fact that the area conserved upon any plane is equal to the projection upon it of the area conserved upon the plane of maximum areas . ( Routh's Rigid Dynamics , Art . 174. ) hence our equations become kß , = L ...
... follows from the fact that the area conserved upon any plane is equal to the projection upon it of the area conserved upon the plane of maximum areas . ( Routh's Rigid Dynamics , Art . 174. ) hence our equations become kß , = L ...
Side 19
... follows : if we refer the motion to the fixed plane of reference , and suppose V expressed as a function of 0 , 4 , , since k cos y is the area conserved on this plane , we shall have d at ( k cos y ) : == - dv dy • Now ( Art . 10 ( ii ) ...
... follows : if we refer the motion to the fixed plane of reference , and suppose V expressed as a function of 0 , 4 , , since k cos y is the area conserved on this plane , we shall have d at ( k cos y ) : == - dv dy • Now ( Art . 10 ( ii ) ...
Side 32
... follows from this that C - B ω1 can never be greater than e A C - A w , can never be greater than e B 2 If we neglect the disturbing force , h , k and therefore e are constant , and the value of e will be found by substituting the ...
... follows from this that C - B ω1 can never be greater than e A C - A w , can never be greater than e B 2 If we neglect the disturbing force , h , k and therefore e are constant , and the value of e will be found by substituting the ...
Side 34
... follows that to the first order of the disturbing force e continues absolutely constant . When the approximation is carried to the order of the square of the disturbing force * , it is found that e2 can con- tain no term proportional to ...
... follows that to the first order of the disturbing force e continues absolutely constant . When the approximation is carried to the order of the square of the disturbing force * , it is found that e2 can con- tain no term proportional to ...
Side 35
Charles Hartwell H. Cheyne. It follows , as in the preceding Article , that to the same degree of approximation the plane of maximum areas may be regarded as coincident with the Earth's equator . 26. We have now to examine the effect of ...
Charles Hartwell H. Cheyne. It follows , as in the preceding Article , that to the same degree of approximation the plane of maximum areas may be regarded as coincident with the Earth's equator . 26. We have now to examine the effect of ...
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The Earth's Motion of Rotation: Including the Theory of Precession and Nutation Charles Hartwell Horne Cheyne Uten tilgangsbegrensning - 1867 |
The Earth's Motion of Rotation: Including the Theory of Precession and Nutation Charles Hartwell Horne Cheyne Uten tilgangsbegrensning - 1867 |
The Earth's Motion of Rotation: Including the Theory of Precession and Nutation Charles Hartwell Horne Cheyne Uten tilgangsbegrensning - 1867 |
Vanlige uttrykk og setninger
area conserved axis in space calculating Cambridge centre of gravity Church cloth cos² Crown 8vo denote determine the motion dh dt dh dV differential coefficient disturbing force dk dt dl dh ds dh dt 2n dt dk dt dt dt dv dt dy dV dg dv ds dv dt dV dv dv dy Earth's axis ecliptic Elementary Treatise English equations of Art Extra fcap Fcap fixed plane formulæ Fourth Edition Heir of Redclyffe Hence HENRY KINGSLEY Illustrations integration invariable plane JOSEPH BAYMA longitude M. A. Second Edition maximum areas Moon's orbit motion of translation Nutation obtained order of approximation plane of maximum plane of reference Planetary Theory Poems point of Aries preceding Article Precession principal axes revised Sermons preached sin'i Sir NOEL PATON Spherical substituting Sun's Third Edition tion undisturbed motion Vignette vis viva Vols w₁ w₂ Y₁
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