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
Engineering 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
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.
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.
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
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.
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.
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
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.
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.
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
Implementation Method 2
The obtained past observation data includes a coefficient of friction of a seafloor in the sea area to be estimated
Implementation Method 3
a rate of change of a quantity of heat absorbed per unit area
Implementation Method 4
a specific heat
Implementation Method 5
a reference density before a temperature change
Implementation Method 6
a reference density before a temperature change
Data Source
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.
