与 «TIDE-GENERATING FORCE»相关的英语书籍
在以下的参考文献中发现
tide-generating force的用法。与
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1
An Introduction to Atmospheric Physics
The resultant of the two forces, called the tide generating force, is illustrated in Fig
. 1.7b. To formulate the tide generating force, we may replace the centrifugal
force per unit mass by the gravitational force acting at the distance (D) of the
center ...
Robert G. Fleagle, Joost A. Businger, 1981
2
Oceanography: An Invitation to Marine Science
We can calculate the strength of the tide-generating force as follows: Let the
distance between the center of Earth and that of the moon be R, let the radius of
Earth be r, and let m be the mass of the moon divided by the mass of Earth.
3
Oceanography of Asian Marginal Seas
The difference of co-tidal lines between Figure 7(b) and 8(b) is obvious in the
results of the East Sea where without tide-generating force the amphidromic point
in the Tartary Bay disappears while the amphidromic point just above the Korea ...
4
Descriptive Physical Oceanography
The most important constituents of the tide generating force are: M2 (Main lunar,
semi-diurnal constituent) with period 12.42 h; S2 (main solar, semi-diurnal
constituent) with period 12.00 h; N2 (lunar constituent due to monthly variation in
...
M. Affholder, F. Valiron, 2001
5
CK-12 Earth Science for High School
In this exercise you will use an equation to calculate the tide generating force.
Like the force of gravity, the pull of the tide generating force is directly related to
the masses of the astronomical objects involved and inversely related to the
square ...
6
Introduction to Coastal Processes and Geomorphology, Second ...
This is the tide-generating force Ft and it is the resultant vector addi- tion of Fc
and Flg Ft= (± r)2Gm E m M –––––––––––– R3 (3.4) On the Moon-facing side of
the Earth, the resultant tide-generating force is positive, which means it is
directed ...
Gerd Masselink, Michael Hughes, Jasper Knight, 2014
7
Hydrodynamics of Free Surface Flows: Modelling with the ...
The tide-generating force is extremely weak but is applied over enormous
distances. The waves produced are, moreover, deformed and amplified by
oceanic basins; thus variations in water levels of 13 m are observed while a static
theory ...
Jean-Michel Hervouet, 2007
8
Descriptive Physical Oceanography: An Introduction
Thus, the tide-generating force at Earth's surface has a component toward the
moon on the side of Earth facing the moon, and also away from the moon on the
other side of Earth. This is simply because the force at the ocean's surface on the
...
Lynne D. Talley, George L. Pickard, William J. Emery, 2011
It is this slight deviation which is called the tide-generating force. The larger
constant gravitational force is counterbalanced by the centrifugal force of the
Earth in its orbital rotation around the centre of the mass system represented by
Earth and ...
10
Earth Surface Processes
The horizontal tide-generating force is balanced by a horizontal pressure
gradient in the ocean water. The balance of the tide-generating force and the
horizontal pressure gradient is achieved by the water surface assuming a slope.
It can be ...
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Explained: The Supertide that Swallowed a French Abbey
Tide forces are also enhanced when the sun and the moon are directly over the ... Just as with the sun, the tide-generating forces are at their greatest when the ... «Scientific American, 三月 15»
Scientists Reveal the Cause of French Abbey Super Tide
Tide forces are also enhanced when the sun and the moon are directly over the ... Just as with the sun, the tide-generating forces are at their greatest when the ... «American Live Wire, 三月 15»
