Tidal Front Estimation via Numerical Mixing Discriminant

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Solution Overview

Problem

Current methods for identifying tidal fronts are time-consuming and costly, requiring direct observations of water temperatures at whole water depth in sea areas.

Innovation Solution

An apparatus and method using a tidal current numerical model derived from the relationship between tidal current flow velocities and water depths, combined with past observation data, to estimate whole water depth mixing sea areas and tidal fronts.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Measurement precision

If direct observations of water temperatures at whole water depth are performed to identify tidal fronts, then measurement precision is improved, but loss of time and cost increase significantly

Engineering Contradiction:
Improveidentification accuracy of tidal frontVSAvoidtime for temperature observation
Core Design Contradiction:
Measurement precisionVSLoss of time

Solution Approach 1:

The patent creates a numerical model that copies and simulates the physical ocean environment, allowing virtual observation of tidal front characteristics without actual field measurements. The model replicates water temperature distribution, current velocity, and mixing conditions to identify tidal fronts computationally, eliminating the need for time-consuming in-situ temperature profiling.

Inventive Principle:
Principle #26Copying

Solution Approach 2:

The patent replaces the mechanical/physical observation system (temperature sensors, CTD instruments, and manual sampling) with a computational numerical model. The model uses governing equations of fluid dynamics and heat transfer to simulate ocean conditions, substituting physical measurement infrastructure with mathematical computation to achieve the same identification goal.

Inventive Principle:
Principle #28Mechanics substitution (Replace mechanical system)

2Measurement precision

If direct observations of water temperatures at whole water depth are performed to identify tidal fronts, then measurement precision is improved, but cost increases significantly

Engineering Contradiction:
Improveidentification accuracy of tidal frontVSAvoidobservation cost
Core Design Contradiction:
Measurement precisionVSQuantity of substance

Solution Approach 1:

The numerical model creates a virtual copy of the ocean environment, allowing repeated simulations and analyses without the need for expensive field expeditions, specialized equipment, and trained personnel required for actual temperature observations. The model can be executed multiple times with different parameters at minimal computational cost.

Inventive Principle:
Principle #26Copying

Solution Approach 2:

The patent employs a computational model that can be executed repeatedly at very low cost compared to field observations. The numerical simulations use standard computer hardware and mathematical algorithms, representing a form of disposable, low-cost analysis tool that can be run as many times as needed without incurring additional observational costs.

Inventive Principle:
Principle #27Cheap short-living objects (Disposable)

3Reliability

If whole water depth temperature observations are conducted to identify mixing sea areas, then reliability of tidal front identification is improved, but device complexity and operational difficulty increase

Engineering Contradiction:
Improvereliability of mixing sea area identificationVSAvoidcomplexity of temperature observation system
Core Design Contradiction:
ReliabilityVSDevice complexity

Solution Approach 1:

The patent substitutes complex physical observation systems with a numerical model that solves governing equations computationally. The model incorporates conservation of mass, momentum, and energy equations along with boundary conditions to simulate ocean mixing processes, providing reliable identification without requiring complex in-situ measurement infrastructure.

Inventive Principle:
Principle #28Mechanics substitution (Replace mechanical system)

Solution Approach 2:

The numerical model acts as an intermediary between the complex physical ocean processes and the analysis requirements. It mediates by translating physical conditions (current velocity, water depth, friction coefficients) into simulated temperature distributions and mixing characteristics, simplifying the observation process while maintaining reliability through physically-based equations.

Inventive Principle:
Principle #24Intermediary (Mediator)

Applied Scientific Principles

This section explains which scientific principles are used to turn an abstract innovation direction into a practical engineering solution.

Function Achieved in This Case

Enables rapid and efficient estimation of tidal fronts without the need for direct ocean observations, facilitating the identification of areas with high fishery productivity.

Implementation Method 1

a tidal current numerical model derived from the relationship between flow velocities of tidal currents and water depths

Methodology Applied
Scientific EffectTidal current flow velocity relationship:

Implementation Method 2

The obtained past observation data includes a coefficient of friction of a seafloor in the sea area to be estimated

Methodology Applied
Scientific EffectFriction: Friction

Implementation Method 3

a rate of change of a quantity of heat absorbed per unit area

Methodology Applied
Scientific EffectHeat absorption: Absorption (physical)

Implementation Method 4

a specific heat

Methodology Applied
Scientific EffectSpecific heat:

Implementation Method 5

a reference density before a temperature change

Methodology Applied
Scientific EffectGravitation: Gravitation

Implementation Method 6

a reference density before a temperature change

Methodology Applied
Scientific EffectDensity:

Data Source

PatentUS20250123102A1Apparatus and method for estimating tidal fronts
Publication Date: 2025.04.17 KOREA INSTITUTE OF OCEAN SCIENCE & TECHNOLOGY
  • US20250123102A1 patent drawing

AI summary

Disclosed is an apparatus and method for estimating tidal fronts. The method for estimating tidal fronts includes obtaining past observation data of a sea area to be estimated, substituting and calculating the obtained past observation data into a preset whole water depth mixing discriminant for a plurality of points in the sea area to be estimated, and as a result of the calculation, regarding an area of points where a calculated value is less than or equal to a preset reference value as a whole water depth mixing sea area, regarding an area of points where the calculated value exceeds the preset reference value as a stratified sea area, and estimating a boundary between the regarded whole water depth mixing sea area and stratified sea area as a tidal front.