ASKiIMAN™ ARCHIVE / PHYSICAL GEOGRAPHY
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OCEAN TIDES (NCERT CH 14) SPRING VS NEAP
1. GRAVITY BULGE
LUNAR GRAVITY (FRONT)
CENTRIFUGAL (BACK)
2. SPRING TIDE
SYZYGY ALIGNMENT
MAXIMUM TIDAL RANGE
3. NEAP TIDE
QUADRATURE (90°)
MINIMUM TIDAL RANGE
LUNAR DAY = 24 HRS 50 MINS (MOON ADVANCES IN ORBIT) BAY OF FUNDY: HIGHEST TIDES ON EARTH (15-16 METERS)
WORLD R TO T · HYDROLOGY, OCEANS & BIOGEOGRAPHY · NODE 91 OF 106

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.

1. LUNAR & SOLAR GRAVITY → 2. CENTRIFUGAL COUNTER-FORCE → 3. SYZYGY (SPRING TIDES) → 4. QUADRATURE (NEAP TIDES) → 5. FLOOD & EBB CURRENTS

I. Definition, Forces & The Twin Bulges (NCERT Core)

MICRO-REALM 01

Tide Definition (NCERT)

PERIODICAL RISE & FALLOF SEA LEVEL
  • 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.
MICRO-REALM 02

Tide vs. Surge (NCERT)

TIDE:
GRAVITY
SURGE:
METEOROLOGY
  • Movement of water caused by meteorological effects (winds and atmospheric pressure changes) are called surges.
  • Surges are not regular like tides.
MICRO-REALM 03

The Primary Driver (Moon)

← GRAVITY
  • 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.
MICRO-REALM 04

The Secondary Driver (Sun)

GRAVITY →
  • To a lesser extent the sun's gravitational pull is a major cause for the occurrence of tides.
MICRO-REALM 05

Mass vs. Distance Rule

DISTANCE MATTERS MORETHAN MASS IN TIDAL FORCE
  • 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.
MICRO-REALM 06

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.
MICRO-REALM 07

The Twin Tidal Bulges

CENTRIFUGAL
  • 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

MICRO-REALM 08

High Tide (Crest)

HIGH WATER
  • Occurs when a location rotates exactly under one of the two tidal bulges.
  • Maximum water level (High Water).
MICRO-REALM 09

Low Tide (Trough)

LOW WATER
  • Occurs when a location rotates into the "trough" exactly between the two bulges.
  • Minimum water level (Low Water).
MICRO-REALM 10

Tidal Range

DIFFERENCE
  • The difference between high water and low water.
  • Varies greatly depending on coastal geometry and lunar phase.
MICRO-REALM 11

The Lunar Day Delay

24 HOURS + 50 MINSMOON ADVANCES IN ORBIT
  • 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.
MICRO-REALM 12

Semi-Diurnal Tide

HIGH
LOW
HIGH
LOW
  • 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.
MICRO-REALM 13

Diurnal Tide

HIGH
↓ 12 HRS ↓
LOW
  • 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.
MICRO-REALM 14

Mixed Tide

VARIATIONS IN HEIGHTWEST COAST OF N. AMERICA
  • 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

MICRO-REALM 15

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.
MICRO-REALM 16

Spring Tide (Max Range)

MAXIMUM TIDAL RANGETWICE A MONTH (FULL/NEW MOON)
  • 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.
MICRO-REALM 17

Conjunction vs Opposition

CONJUNCTION (NEW MOON)
OPPOSITION (FULL MOON)
  • 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.
MICRO-REALM 18

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.
MICRO-REALM 19

Neap Tide (Min Range)

MINIMUM TIDAL RANGEFORCES COUNTERACT EACH OTHER
  • 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.
MICRO-REALM 20

Perigee (Moon Closest)

MOON AT CLOSEST POINTUNUSUALLY HIGH TIDES
  • 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.
MICRO-REALM 21

Apogee (Moon Farthest)

MOON AT FARTHEST POINTUNUSUALLY LOW TIDES
  • 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.
MICRO-REALM 22

Perihelion (Jan 3)

EARTH CLOSEST TO SUNSLIGHTLY HIGHER RANGE
  • 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)

MICRO-REALM 23

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.
MICRO-REALM 24

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.
MICRO-REALM 25

Slack Water

STANDSTILL PERIODBETWEEN FLOOD & EBB
  • The brief period at the exact peak of high tide or bottom of low tide.
  • Tidal currents completely stop before reversing direction.
MICRO-REALM 26

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).
MICRO-REALM 27

Bay of Fundy (Max Tides)

HIGHEST TIDES IN THE WORLD15 - 16 METERS (NOVA SCOTIA)
  • 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.
MICRO-REALM 28

Master Tide Matrix

GRAVITY vs CENTRIFUGALSPRING (SYZYGY)NEAP (QUADRATURE)FLOOD & EBB
  • Completes the gravitational mechanics of the ocean.
  • Locks the celestial alignments mapping.
  • Transitions to Realm 92 (Ocean Currents).

Core Distinctions

1. Spring Tide vs. Neap Tide (Alignment vs. Right Angle)

• 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.

2. Perigee vs. Apogee (Lunar Orbital Proximity)

• 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.

3. Tides vs. Surges (Gravity vs. Weather)

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

THE TWIN BULGESMoon Gravity (Front) · Centrifugal (Back)
SPRING TIDESyzygy Alignment · Max Range
NEAP TIDEQuadrature (90°) · Min Range
LUNAR DAY24 Hours 50 Minutes
MAX EXTREMESBay of Fundy (Canada) · 15-16 Meters