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5.2 Using Admiralty Tidal Curves for Height at Any Time

Key Takeaways

  • Admiralty Tidal Curves resolve non-sinusoidal shallow water distortions, estuarine friction, and asymmetric flood-ebb durations that invalidate the simplified Rule of Twelfths.

  • Read the actual curve’s height scales, spring/neap line styles and time reference. Many curves are HW-centred; some, including Cowes, are centred on LW. Join the predicted LW and HW heights on the transfer grid.

  • Problem 1 (forward calculation) finds the instantaneous height of tide at any specific clock time by projecting vertically from the time axis to the curve, horizontally to the diagonal line, and vertically to the height scale.

  • Problem 2 (reverse calculation) determines the safe passage time window over a shallow sill or drying bar by projecting from the required height to the diagonal, horizontally to both sides of the curve, and down to the time axis.

  • Required height of tide over a drying feature must always equal the charted drying height plus the vessel's static draught and a safe under-keel clearance margin.

Last updated: November 2026

5.2 Using Admiralty Tidal Curves for Height at Any Time

Note

Calculating High and Low Water only gives the turning points of the tide. Navigators frequently need the Height of Tide at an intermediate clock time (e.g., when anchoring) or the time window when depth exceeds a threshold (e.g., clearing a shallow sill or bar). Admiralty Tidal Curves provide the graphical method to solve both problems.


Limitations of the Rule of Twelfths

The Rule of Twelfths (1/12 in hour 1, 2/12 in hour 2, 3/12 in hour 3, 3/12 in hour 4, 2/12 in hour 5, 1/12 in hour 6) assumes a pure sinusoidal wave with equal 6-hour durations between HW and LW. In coastal navigation, this assumption frequently fails:

  1. Estuarine Friction: Narrow approaches delay flood waves, creating rapid floods (e.g., 4 hours) and sluggish ebbs (e.g., 8 hours).
  2. Shallow-Water Harmonics: In shallow waters (e.g., the English Channel and the Solent), interaction between primary frequencies generates overtides (M4,M6M_4, M_6), resulting in double high waters (Southampton) or extended stands (Weymouth, Saint-Malo).
  3. Empirical Profiles: Official Admiralty curves represent tidal observations at the port, representing its characteristic local profile.
AttributeRule of TwelfthsAdmiralty Tidal Curves
Wave ProfileAssumes pure sinusoidal waveReflects empirical coastal profile
Flood / Ebb DurationAssumes equal 6-hour durationsAccommodates asymmetrical durations
HarmonicsIgnores shallow-water harmonicsModels double high waters and stands
Curve DistinctionSingle theoretical ruleSeparate Mean Springs and Neaps curves
UseApproximate check where the profile is suitablePublished local method where available and applicable

Anatomy of the Admiralty Tidal Curve

Read the layout and instructions on the actual port curve. The following describes a common HW-centred format:

  1. High Water Height Scale (Top Axis): Graduated in metres across the port's High Water range.
  2. Low Water Height Scale (Bottom Axis): Graduated in metres across the port's Low Water range.
  3. The Diagonal Transfer Line: A straight pencil line drawn by the navigator directly connecting the plotted Low Water on the bottom scale to High Water on the top scale.
  4. The Central Curve Box: Contains the empirical profile curves:
    • Mean Springs Curve: Heavy solid line (red or black).
    • Mean Neaps Curve: Dashed line (blue or black).
    • On intermediate tides, the navigator interpolates between the curves based on tidal range.
  5. The Time Axis & Entry Boxes (Base Axis): Use the printed reference event and hour labels. HW-centred curves use HW as zero; a curve such as Cowes uses LW. Fill the boxes from that event, without assuming identical limits on both sides.

Problem 1: Height of Tide at a Specific Clock Time

HW-centred exercise: A skipper needs the height of tide at1530BST to check depth before anchoring.

Step-by-Step Graphical Protocol

  1. Extract Predictions: Obtain HW time (1300 BST, 5.2m) and LW time (1915 BST, 1.2m). For this hypothetical exercise, mean spring range is 4.0m and mean neap range 2.0m: the 4.0m range uses the spring curve. The supplied curve factor at HW +2h30m is 0.55.
  2. Plot Heights: Mark LW (1.2m) on the bottom scale and HW (5.2m) on the top scale. Join them with a straight pencil line (the diagonal line).
  3. Populate Time Boxes: Write HW time (1300) beneath the central 'HW' (0h) marker. Fill in adjacent hourly boxes:
    • Before HW: 1200 (-1h), 1100 (-2h), 1000 (-3h).
    • After HW: 1400 (+1h), 1500 (+2h), 1600 (+3h), 1700 (+4h).
  4. Locate Target Time: Find 1530 on the base axis (+2.5h after HW, midway between 1500 and 1600).
  5. Project to Curve: Project vertically straight UP from 1530 to intersect the Spring curve.
  6. Transfer to Diagonal: From the curve intersection, travel horizontally across to intersect the diagonal line.
  7. Read Height: Project vertically to the available height scale, following the printed layout. The supplied factor gives Height of Tide = 1.2 + (0.55 × 4.0) = 3.4 metres. A real calculation requires the actual port curve.

Problem 2: Safe Tidal Window for a Required Height

HW-centred exercise: Find the earliest and latest times when water level meets the stated drying-bar requirement.

Formulating Required Height of Tide

Required Depth=Vessel Static Draught+Under-Keel Clearance Margin (UKC)\text{Required Depth} = \text{Vessel Static Draught} + \text{Under-Keel Clearance Margin (UKC)} Required Height of Tide=Required Depth−Charted Depth\text{Required Height of Tide} = \text{Required Depth} - \text{Charted Depth}

Important

For a drying bank or sill with an underlined charted drying height (e.g., 1.4‾m\underline{1.4}\text{m}), Charted Depth is negative (−1.4m-1.4\text{m}). Subtracting a negative yields addition: Required Height of Tide=Vessel Draught+UKC Margin+Charted Drying Height\text{Required Height of Tide} = \text{Vessel Draught} + \text{UKC Margin} + \text{Charted Drying Height}

Worked Crossing Scenario

  • Vessel draught: 1.8 metres.
  • Prudent UKC margin: 0.8 metres.
  • Harbour entrance bar: Charted drying height of 1.4 metres (sounded as 1.4‾m\underline{1.4}\text{m}).
  • Required Height: 1.8m+0.8m+1.4m=4.0 metres1.8\text{m} + 0.8\text{m} + 1.4\text{m} = \mathbf{4.0\text{ metres}}.
  • Port predictions: HW 1400 BST (5.0m); LW 2015 BST (1.0m). For this hypothetical exercise, mean spring range is 4.5m and mean neap range 2.5m, giving (4.0−2.5)/(4.5−2.5) = 0.75. The supplied interpolated curve crosses factor 0.75 at HW −1h50m and HW +1h50m.

Reverse Plotting Protocol

  1. Plot Diagonal: Join LW (1.0m) on the bottom scale to HW (5.0m) on the top scale.
  2. Enter Required Height: Locate 4.0m4.0\text{m} on the horizontal height scale.
  3. Project to Diagonal: Project vertically from 4.0m4.0\text{m} to intersect the diagonal line.
  4. Transfer Horizontally to Curves: Required factor = (4.0−1.0)/(5.0−1.0) = 0.75. Draw the corresponding horizontal line across the curve box. For the supplied exercise readings:
    • Flood intersection (before HW): occurs at -1h 50m before HW.
    • Ebb intersection (after HW): occurs at +1h 50m after HW.
  5. Drop to Time Axis: Drop vertically down from both curve intersections to the time boxes:
    • HW time is 1400 BST.
    • Earliest Safe Arrival Time = 1400−0150=1210 BST1400 - 0150 = \mathbf{1210\text{ BST}}.
    • Latest Safe Departure Time = 1400+0150=1550 BST1400 + 0150 = \mathbf{1550\text{ BST}}.
  6. Conclusion: Safe crossing window spans 3 hours 40 minutes (from 1210 to 1550 BST).

Asymmetric Curves & Tidal Stands

In regions such as the Solent, Portland, and the Channel Islands, skippers encounter specialized curve features:

  1. Duration Corrections: When the time interval between LW and HW departs from 6 hours, some Admiralty curves provide auxiliary duration tables to scale the time axis.
  2. Dual High Waters & Stands: In Southampton Water and Portsmouth, overtides produce a secondary rise or prolonged stand. A horizontal line across the curve may intersect at multiple points, providing extended deep-water transit windows.
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Admiralty Tidal Curve Forward and Reverse Plotting Pathways
Test Your Knowledge

When using an Admiralty Tidal Curve to determine the height of tide at a specific clock time, what is the correct graphical procedure after plotting LW and HW and joining them with a diagonal line?

A

Enter the top scale at the target time, drop to the diagonal line, and read the height from the time axis at the bottom.

B

Find the target time on the base axis, project vertically to the Spring/Neap curve, travel horizontally to the diagonal line, and project vertically to read the height scale.

C

Project horizontally from the time axis to the diagonal line, move vertically to the curve, and project across to the height scale.

D

Connect the target time directly to the High Water mark on the top scale and read the intersection on the central vertical axis.

Test Your Knowledge

A yacht with a draught of 1.8m requires a minimum under-keel clearance of 0.7m to cross a harbour entrance bar with a charted drying height of 1.2m (drying bank, -1.2m depth). What is the minimum height of tide required, and how is it used on the tidal curve to find the crossing window?

A

2.5m; enter at 2.5m on the curve, move horizontally to the diagonal line, and read the base scale.

B

1.3m; enter at 1.3m on the diagonal line, drop to the bottom scale, and read the time window.

C

3.7m; enter at 3.7m on the height scale, drop to the diagonal line, move horizontally to intersect the curve on both flood and ebb, and drop to the time axis.

D

3.0m; enter at 3.0m on the time axis, project up to the curve, and measure the duration between high water and low water.

Test Your Knowledge

Why should a navigator use the published local tidal curve when shallow-water distortion makes the Rule of Twelfths unsuitable?

A

The Rule of Twelfths assumes a symmetrical 6-hour sinusoidal tide, whereas real coastal tides exhibit shallow-water distortions, asymmetrical flood/ebb durations, and prolonged stands.

B

The Rule of Twelfths is valid only for Neap tides and underpredicts tidal heights by exactly 50% during Spring tides.

C

Admiralty charts use imperial feet while the Rule of Twelfths is formulated exclusively for metric calculations.

D

The Rule of Twelfths cannot be calculated without an electronic tidal computer approved by the Maritime and Coastguard Agency.

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