CENTRIFUGAL (BACK)
MAXIMUM TIDAL RANGE
MINIMUM TIDAL RANGE
Ocean Tides
Sun-Moon-Earth Gravity · Spring & Neap Magnitudes · Diurnal & Semi-Diurnal · Flood, Ebb & Tidal Bores (28 Micro-Realms)
The Periodical Rise and Fall of the Sea (NCERT Chapter 14)
The periodical rise and fall of the sea level, once or twice a day, mainly due to the attraction of the sun and the moon, is called a Tide. The moon's gravitational pull to a great extent, and to a lesser extent the sun's pull, are the major causes. Centrifugal force is the other factor, acting to counterbalance gravity; together they create two tidal "bulges" on Earth. When the Sun, Moon, and Earth align in a straight line (Syzygy), their forces combine to create maximum Spring Tides. When at a right angle (Quadrature), the forces counteract, creating minimum Neap Tides. The time between the high tide and low tide, when the water level is falling, is called the Ebb, while the rising phase is the Flood.
I. Definition, Forces & The Twin Bulges (NCERT Core)
Tide Definition (NCERT)
- The periodical rise and fall of the sea level, once or twice a day.
- Mainly due to the attraction of the sun and the moon.
Tide vs. Surge (NCERT)
GRAVITY
METEOROLOGY
- Movement of water caused by meteorological effects (winds and atmospheric pressure changes) are called surges.
- Surges are not regular like tides.
The Primary Driver (Moon)
- The moon's gravitational pull to a great extent is the major cause for the occurrence of tides.
- Because the Moon is much closer to Earth than the Sun.
The Secondary Driver (Sun)
- To a lesser extent the sun's gravitational pull is a major cause for the occurrence of tides.
Mass vs. Distance Rule
- Sun is 27 million times more massive than the Moon.
- But the Moon is ~390 times closer.
- Tidal force is inversely proportional to the CUBE of distance, making lunar pull 2.2x stronger.
Centrifugal Force
- Centrifugal force is the other factor which acts to counterbalance gravity.
- Generated by the Earth-Moon system revolving around their common center of mass.
The Twin Tidal Bulges
- Together, the gravitational pull and the centrifugal force are responsible for creating the two major tidal bulges on the earth.
- One faces the moon (gravity), one faces away (centrifugal).
II. Tide Frequencies, The Lunar Day & Tidal Range
High Tide (Crest)
- Occurs when a location rotates exactly under one of the two tidal bulges.
- Maximum water level (High Water).
Low Tide (Trough)
- Occurs when a location rotates into the "trough" exactly between the two bulges.
- Minimum water level (Low Water).
Tidal Range
- The difference between high water and low water.
- Varies greatly depending on coastal geometry and lunar phase.
The Lunar Day Delay
- A tidal day is 24 hours and 50 minutes.
- Because while Earth rotates, the Moon also advances slightly in its orbit.
- Earth takes 50 extra minutes to "catch up" to face the Moon again.
Semi-Diurnal Tide
- The most common tidal pattern.
- Featuring two high tides and two low tides each day.
- The successive high or low tides are approximately of the same height.
Diurnal Tide
- There is only one high tide and one low tide during each day.
- The successive high and low tides are approximately of the same height.
Mixed Tide
- Tides having variations in height are known as mixed tides.
- These tides generally occur along the west coast of North America and on many islands of the Pacific Ocean.
III. Magnitudes: Spring vs. Neap Tides & Orbital Anomalies
Syzygy (Straight Line)
- The position of both the sun and the moon in relation to the earth has direct bearing on tide height.
- When the sun, the moon and the earth are in a straight line.
Spring Tide (Max Range)
- When the sun, the moon and the earth are in a straight line, the height of the tide will be higher.
- These are called spring tides and they occur twice a month, one on full moon period and another during new moon period.
Conjunction vs Opposition
- Conjunction: Sun and Moon are on the SAME side of Earth (New Moon).
- Opposition: Sun and Moon are on OPPOSITE sides of Earth (Full Moon).
- Both produce Spring Tides.
Quadrature (Right Angle)
- When the sun and moon are at right angles to each other.
- Occurs during the first quarter and third quarter moon phases.
Neap Tide (Min Range)
- Normally, there is a seven day interval between the spring tides and neap tides.
- At this time the sun and moon are at right angles to each other and the forces of the sun and moon tend to counteract one another.
Perigee (Moon Closest)
- Once in a month, when the moon's orbit is closest to the earth (perigee), unusually high and low tides occur.
- During this time the tidal range is greater than normal.
Apogee (Moon Farthest)
- Two weeks later, when the moon is farthest from earth (apogee), the moon's gravitational force is limited.
- The tidal ranges are less than their average heights.
Perihelion (Jan 3)
- When the earth is closest to the sun (perihelion), around 3rd January each year.
- Tidal ranges are also much greater, with unusually high and unusually low tides.
- (Conversely, Aphelion on July 4th produces slightly lower ranges).
IV. Tidal Currents, Bores & Global Extremes (NCERT)
Flood Tide (Incoming)
- The time between the low tide and high tide, when the tide is rising, is called the flow or flood.
- Creates a strong landward current in coastal estuaries.
Ebb Tide (Outgoing)
- The time between the high tide and low tide, when the water level is falling, is called the ebb.
- Creates a strong seaward current dragging sediment out to sea.
Slack Water
- The brief period at the exact peak of high tide or bottom of low tide.
- Tidal currents completely stop before reversing direction.
Tidal Bore
- A steep, surging wave created when an incoming flood tide is funneled into a narrow, shallow river mouth.
- Famous in the Hooghly river (India) and Qiantang river (China).
Bay of Fundy (Max Tides)
- The highest tides in the world occur in the Bay of Fundy in Nova Scotia, Canada.
- The tidal bulge is 15 - 16 m.
- Because there are two high tides and two low tides every day (roughly a 24 hour period); then a tide must come in within about a six hour period.
Master Tide Matrix
- Completes the gravitational mechanics of the ocean.
- Locks the celestial alignments mapping.
- Transitions to Realm 92 (Ocean Currents).
Core Distinctions
• Spring Tide (Syzygy): When the sun, the moon and the earth are in a straight line, the height of the tide will be higher. Occurs on full moon and new moon periods.
• Neap Tide (Quadrature): The sun and moon are at right angles to each other and the forces of the sun and moon tend to counteract one another. Occurs during the first and third quarter moon.
• Perigee: When the moon's orbit is closest to the earth... unusually high and low tides occur.
• Apogee: When the moon is farthest from earth... the tidal ranges are less than their average heights.
Tides are strictly regular and predictable, driven purely by the gravitational attraction of the sun and the moon. Movement of water caused by meteorological effects (winds and atmospheric pressure changes) are called surges. Surges are completely irregular.
Tidal Dynamics Matrix
NCERT Chapter 14 Reference Guide