System and method for isolating inertial and non inertial velocities in the ocean

Patent metadata

Field	Value
Publication number	US-10274508-B2
Application number	US-201514731493-A
Country	US
Kind code	B2
Filing date	Jun 5, 2015
Priority date	Jun 10, 2014
Publication date	Apr 30, 2019
Grant date	Apr 30, 2019

Abstract

Embodiments relate to a system and methods for isolating the inertial and non-inertial components of a velocity field in a body of water, and further provides methods for predicting a path of an object in a body of water and for identifying an initial location in the water at which an object should be placed so that it travels to a desired location. The methods in some cases can partition a time series of velocity fields into inertial and non-inertial components in such a way that accounts for the variation of the inertial period over the range of latitudes within the field and maintains the fidelity of non-inertial variability over both shorter and longer time scales. The embodiments seperate the less-reliable inertial components from the more-reliable non-inertial background, enabling straightforward calculation of transport due to the non-inertial flow and evaluation of the superposition of inertial oscillations.

First claim

What is claimed is:

1. A method for navigating an object in a body of water, the method comprising:
(a) receiving data of a velocity field in a geographic area in a body of water, the velocity field comprising a plurality of water velocities at a corresponding plurality of associated locations in a two-dimensional (2D) geographic model representing the body of water, each velocity having an inertial component and a non-inertial component, the inertial component of each velocity corresponding to an inertial oscillation of the body of water at the location associated with the velocity, and each associated location being identified by its latitude and longitude;
(b) for each location in the 2D geographic model, determining a corresponding inertial period, the inertial period being a temporal period of the inertial oscillation of the body of water at the latitude of that location;
(c) receiving a specification of a specified time period over which the velocity data is to be analyzed, the specified time period comprising a series of specified time steps;
(d) receiving data of the velocity field for each time step, the data at each time step comprising data of the velocities in the velocity field at that time step;
(e) for each time step, calculating a weighted average of velocities within the inertial period of a specified location in the velocity field, the weighted average comprising an isolated non-inertial component of the velocities at the specified location at that time step,
wherein the weighted average at each time step is calculated by multiplying each of the velocities within the inertial period by at most a factor equal to a period of the time step,
each of the velocities at a beginning and/or an end of the inertial period being multiplied by a value corresponding to a prorated percentage of the time step, determined by an extent in the time step to which the inertial period encompassing those velocities extends beyond the beginning of the time step, and each of the remaining velocities within the inertial period being multiplied by a value corresponding to the entire time step;
summing the multiplied velocities, and dividing the summed velocities by the inertial period;

(f) repeating steps (b)-(e) for each location in the velocity field to obtain respective isolated non-inertial components of the velocities at each location in the velocity field;
(g) determining a path for the object in the 2D geographic model such that the determined path enables the object to decrease average fuel consumption, wherein the determined path is determined by integrating a motion of the object using the isolated non-inertial components of the velocities in the velocity field near to a trajectory of the object; and
(h) navigating the object in the body of water according to the determined path.

2. A method for identifying a location for placing an object in a body of water so that the object travels to a desired destination location, the method comprising:
(a) receiving data of a velocity field in a geographic area in a body of water, the velocity field comprising a plurality of water velocities at a corresponding plurality of associated locations in a two-dimensional (2D) geographic model representing the body of water, each velocity having an inertial component and a non-inertial component, the inertial component of each velocity corresponding to an inertial oscillation of the body of water at the location associated with the velocity, and each associated location being identified by its latitude and longitude;
(b) receiving data of the desired destination location for an object placed in the body of water;
(c) for each location in the 2D geographic model, determining a corresponding inertial period, the inertial period being a temporal period of the inertial oscillation of the body of water at the latitude of that location;
(d) receiving a specification of a specified time period over which the velocity data is to be analyzed, the specified time period comprising a series of specified time steps;
(e) receiving data of the velocity field for each time step, the data at each time step comprising data of the velocities in the velocity field at that time step;
(f) for each time step, calculating a weighted average of velocities within the inertial period of a specified location in the velocity field, the weighted average comprising an isolated non-inertial component of the velocities at the specified location at that time step,
wherein the weighted average at each time step is calculated by multiplying each of the velocities within the inertial period by at most a factor equal to a period of the time step,
each of the velocities at a beginning and/or an end of the inertial period being multiplied by a value corresponding to a prorated percentage of the time step, determined by an extent in the time step to which the inertial period encompassing those velocities extends beyond the beginning of the time step, and each of the remaining velocities within the inertial period being multiplied by a value corresponding to the entire time step;
summing the multiplied velocities, and dividing the summed velocities by the inertial period;

(g) repeating steps (c)-(f) for each location in the velocity field to obtain respective isolated non-inertial components of the velocities at each location in the velocity field;
(h) determining a path of the object in the 2D geographic model by integrating a motion of the object using the isolated non-inertial components of the velocities in the velocity field near to a trajectory of the object; and
(i) positioning the object in the body of water according to the determined path so that the object reaches the desired destination location.

3. A method for navigating an object in a body of water, the method comprising:
(a) receiving data of a velocity field in a geographic area in a body of water, the velocity field comprising a plurality of water velocities at a corresponding plurality of associated locations in a two-dimensional (2D) geographic model representing the body of water, each velocity having an inertial component and a non-inertial component, the inertial component of each velocity corresponding to an inertial oscillation of the body of water at the location associated with the velocity, and each associated location being identified by its latitude and longitude;
(b) for each location in the 2D geographic model, determining a corresponding inertial period, the inertial period being a temporal period of the inertial oscillation of the body of water at the latitude of that location;
(c) receiving a specification of a specified time period over which the velocity data is to be analyzed, the specified time period comprising a series of specified time steps;
(d) receiving data of the velocity field for each time step, the data at each time step comprising data of the velocities in the velocity field at that time step;
(e) for each time step, calculating a weighted average of velocities within the inertial period of a specified location in the velocity field, the weighted average comprising an isolated non-inertial component of the velocities at the specified location at that time step, wherein the weighted average at each time step is calculated by multiplying each of the velocities within the inertial period by at most a factor equal to a period of the time step, each of the velocities at a beginning and/or an end of the inertial period being multiplied by a value corresponding to a prorated percentage of the time step, determined by an extent in the time step to which the inertial period encompassing those velocities extends beyond the beginning of the time step, and each of the remaining velocities within the inertial period being multiplied by a value corresponding to the entire time step; summing the multiplied ve

Assignees

• Barron Charlie N
• Spence Peter L
• Smedstad Lucy F
• Us Navy

Inventors

• Barron Charlie N
• Spence Peter L
• Smedstad Lucy F

Classifications

• G01P5/001 Primary

  Full-field flow measurement, e.g. determining flow velocity and direction in a whole region at the same time, flow visualisation · CPC title