This book gives an account of certain observed irregularities on the rotation of the Earth, both in its rate of rotation (giving a variable length of day) and in the position of its axis. These irregularities are caused by events on and within the Earth and provide a means of studying a number of geophysical problems. Seasonal shifts in air masses and variable winds are causes of short-period fluctuations in the rotation. Climatic changes and their attendant sea levels are in part responsible for long-term fluctuations. Modern observations of the Moon and descriptions of ancient elipses both establish a secular increase in the length of day. The interpretation involves atmospheric, oceanic and bodily tides. The book provides a unified treatment of the rotation of the Earth, making this method of studying geophysical phenomena more readily accessible to geophysicists and others.
"synopsis" may belong to another edition of this title.
This book gives an account of certain observed irregularities on the rotation of the Earth, both in its rate of rotation (giving a variable length of day) and in the position of its axis. These irregularities are caused by events on and within the Earth and provide a means of studying a number of geophysical problems.
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Hardcover. Reprinted. Octavo; VG-/VG-; green spine with black and white text; reprinted with corrections; exterior to jacket has few slight smudges; only light wear to edges; price clipped front flap; blue cloth with gilt text to spine; titles blind stamped to front board; straight boards with clean exterior; text block edges have very mild tone; previous owner's name to ffep; frontispiece; clean interior; illustrated; pp 323. 1362896. FP New Rockville Stock. Seller Inventory # 1362896
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Hardcover. ed.1975. XIX, 323 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w10665 0521207789 Sprache: Englisch Gewicht in Gramm: 550. Seller Inventory # 2432512
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