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If the current in the sea moves along the meridian, the Coriolis force presses the water to the shores, with a constant force or force pulsing.
Why on the northern and southern coasts of the seas and oceans the tides are three times higher than on the eastern and western coasts, but it should be the other way around.
If the current moves along the meridian, the Coriolis force presses the water to the shores of the continent with a constant force or a pulsating force. (twice a day).
Quote from: Yusup Hizirov on 18/04/2019 09:50:52If the current moves along the meridian, the Coriolis force presses the water to the shores of the continent with a constant force or a pulsating force. (twice a day).The deflecting force of Coriolis depends on the speed of rotation of the earth both around the axis and around the sun.
We can't look at your calculations unless you post them.If you are saying you have not done the maths, what are you using as the basis of your post?
The physical properties of a conventional solid gyro today are not fully understood,
Today in the Bay of Fundy the amplitude of the tides can be 6 meters, and tomorrow 18 meters.What is the reason for such a sharp jump?
Quote from: Yusup Hizirov on 30/04/2019 06:20:31Today in the Bay of Fundy the amplitude of the tides can be 6 meters, and tomorrow 18 meters.What is the reason for such a sharp jump?Where does it show this? Please post tide tables that show this variance.
The amplitude of the tides on earth is almost the same every year, with the exception of the bays into which the rivers flow.The tide tables are for months ahead, and if an error occurs it is not corrected.And in the calendar you will not find a mistake.You can get this information from the gauging station on duty.