1987
DOI: 10.1007/bf01624753
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Secular tidal and nontidal variations in the Earth's rotation

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Cited by 12 publications
(5 citation statements)
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“…The torque exerted by tidal friction is relatively small 10 16 N m (Burša 1987) and considering the mantle viscosity 10 19 Pa s (Cathles 1975) only two orders of magnitude lower than the viscosity of lithosphere, this force is considered as insufficient for the plate movement. Today's mantle viscosity estimation following from the post glacial uplift, relative sea level changes and GRACE secular changes in gravity give relatively high values of upper mantle viscosity 5.3 × 10 20 Pa s (Paulson et al 2007), which do not witness about easy movement of plates in mantle.…”
Section: Calculation Of Forces Driving Platesmentioning
confidence: 99%
“…The torque exerted by tidal friction is relatively small 10 16 N m (Burša 1987) and considering the mantle viscosity 10 19 Pa s (Cathles 1975) only two orders of magnitude lower than the viscosity of lithosphere, this force is considered as insufficient for the plate movement. Today's mantle viscosity estimation following from the post glacial uplift, relative sea level changes and GRACE secular changes in gravity give relatively high values of upper mantle viscosity 5.3 × 10 20 Pa s (Paulson et al 2007), which do not witness about easy movement of plates in mantle.…”
Section: Calculation Of Forces Driving Platesmentioning
confidence: 99%
“…2. The torques of tidal friction were calculated by Burša (1987aBurša ( ), (1987b on the basis of angular momentum balance in the Earth -Moon -Sun system. Nm = 4.2 × 10 35 kg m 2 cy -2 = 4.2 ×10 16 kg m 2 s -2 = 4.2 × 10 16 Nm Ns = 8.9 × 10 34 kg m 2 cy -2 = 8.9 × 10 15 kg m 2 s -2 = 8.9 × 10 15 Nm…”
mentioning
confidence: 99%
“…The tidal fiction decelerates the Earth's rotation (Lambeck, 1977) and therefore it can be also considered as the force causing the westward movement of plates (Ostřihanský 2012a(Ostřihanský , 2012b. The torque exerted by the tidal friction is relative low 10 16 N m. (Burša 1987a) and considering the mantle viscosity only 2 orders of magnitude lower than the lithosphere (Cathles 1975), this force is considered as insufficient for the plate movement. But considering variable force (ad 1), acting on Earth's flattening, and tidal friction (ad 2) acting semidiurnally, then the westward movement is possible, owing to the north-south varying force ad 1, acting on it perpendicularly.…”
mentioning
confidence: 99%
“…The torques of tidal friction were calculated by Burša (1987aBurša ( ), ( 1987b on the basis of angular momentum balance in the Earth -Moon -Sun system.…”
mentioning
confidence: 99%
“…The torque exerted by the tidal friction is relative low 10 16 N m. (Burša 1987a) and considering the mantle viscosity only 2 orders of magnitude lower than the lithosphere (Cathles 1975), this force is considered as insufficient for the plate movement. But considering variable force (ad 2), acting on Earth's flattening, and tidal friction (ad 3) acting semidiurnally, then the westward movement is possible, owing to the north-south varying force ad 2, acting on it perpendicularly.…”
mentioning
confidence: 99%