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How is Mean Lower Low Water Determined for a Station?

Published in Tide Levels 2 mins read

Mean Lower Low Water (MLLW) for a tide station is calculated by averaging the lowest tide recorded each day over a specific 19-year period. This period is called the National Tidal Datum Epoch.

Understanding Mean Lower Low Water (MLLW)

MLLW is a crucial reference point for nautical charts and coastal management. It represents the average height of the lowest low tides experienced at a location. Because tides vary due to astronomical and meteorological influences, a long-term average is required for accuracy.

Calculation Process

The determination of MLLW involves these key steps:

  1. Data Collection: Tide gauges at the station continuously record water levels over a 19-year period (National Tidal Datum Epoch). This period is used because it accounts for the 18.6-year lunar nodal cycle, which significantly affects tidal ranges.
  2. Identification of Daily Lowest Low Tides: For each day of the 19-year period, the lowest tide is identified and recorded.
  3. Averaging: All the recorded lowest low tides from the 19-year period are then averaged together. The resulting value is the MLLW.

Example:

Imagine a tide station has recorded the following lowest low tides (simplified example):

Year Lowest Low Tide (feet)
1 -2.5
2 -2.0
3 -3.0
... ...
19 -2.2

To calculate the MLLW, you would sum all 19 values and divide by 19.

Importance of the 19-Year Epoch

Using a 19-year epoch ensures that the MLLW value is representative of long-term tidal patterns and minimizes the influence of short-term variations.

Practical Applications

  • Nautical Charting: MLLW is often used as the chart datum, which is the reference level for depths shown on nautical charts. This ensures that mariners have sufficient clearance when navigating.
  • Coastal Zone Management: MLLW is also used in coastal zone management for determining property boundaries and regulating coastal development.

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