Method of estimating cloud particle sizes using LIDAR ratio

• US 10,261,006 B2
• Filed: 07/21/2016
• Issued: 04/16/2019
• Est. Priority Date: 07/21/2016
• Status: Active Grant

• Current Assignee: Rosemount Aerospace, Inc. (Rtx Corporation)
• Original Assignee: Rosemount Aerospace, Inc. (Rtx Corporation)
• Inventors: Ray, Mark, Anderson, Kaare Josef
• Primary Examiner(s): Nguyen, Sang H
• Application Number:
  US15/216,340
• Publication Number:
  US 20180024036A1
• Time in Patent Office: 999 Days
• CPC Class Codes: G01N 15/0211 Investigating a scatter or diffraction pattern
• CPC Class Codes: G01N 2015/0046 in gas, e.g. smoke
• CPC Class Codes: G01S 17/95 for meteorological use
• CPC Class Codes: G01S 7/4812 transmitted and received beams following a coaxial path
• CPC Class Codes: G01S 7/499 using polarisation effects
• CPC Class Codes: G01W 1/00 Meteorology
• CPC Class Codes: Y02A 90/10 Information and communication technologies [ICT] supporting adaptation to climate change, e.g. for weather forecasting or climate simulation

Abstract

Apparatus and associated methods relate to determining sizes of water particles in a cloud atmosphere based on a detected portion of signals generated from a single monochromatic source and backscattered by water particles in a cloud atmosphere. A backscatter coefficient and an optical extinction coefficient are calculated, based on the detected portion of signals generated from the monochromatic source and backscattered by water particles in the cloud atmosphere. A LIDAR ratio—a ratio of the optical extinction coefficient to the backscatter coefficient, is calculated. Sizes of water particles in the cloud atmosphere are estimated based on the LIDAR ratio. An output signal indicative of the estimated sizes of water particles in the cloud atmosphere is generated. Estimating sizes of water particles using signals from a single monochromatic source advantageously can alert a pilot of an aircraft of cloud conditions, without requiring multi-chromatic sources.

Claims

1. A system for measuring an effective size of water particles in a cloud atmosphere, the system comprising:

a laser configured to generate a pulse of light of a wavelength and to direct the pulse of light into the cloud atmosphere;

an optical detector configured to detect a portion of the pulse of light backscattered by the water particles in the cloud atmosphere; and

a cloud metric calculator configured to determine, based on the detected portion of the pulse of light backscattered by the water particles in the cloud atmosphere, an optical extinction coefficient and a backscatter coefficient,

wherein the cloud metric calculator is further configured to estimate, based on a look-up table and a ratio of the determined optical extinction coefficient to the determined backscatter coefficient, the effective size of the water particles in the cloud atmosphere.

2. The system of claim 1, wherein the cloud metric calculator is further configured to calculate, based on the detected portion of the pulse of light backscattered by the water particles in the cloud atmosphere, a concentration of the water particles of the cloud atmosphere.

3. The system of claim 1, wherein the wavelength of the generate pulse of light is between 700 nano-meters and 2.0 micro-meters.

4. The system of claim 1, further comprising a polarizer configured to circularly polarize the pulse of light.

5. The system of claim 4, wherein the portion of the pulse of light is a first portion of the circularly polarized pulse of light, the first portion having a first polarization, wherein the signal detector is further configured to detect a second portion of the circularly polarized pulse of light backscattered by the cloud atmosphere, the second portion having a second polarization oppositely oriented to the first polarization.

6. The system of claim 5, wherein the cloud metric calculator is further configured to calculate, based on the detected first signal and the detected second signal, an ice/liquid phase ratio of the droplets in the cloud atmosphere.

7. A method for measuring an effective size of water particles in a cloud atmosphere, the method comprising:

generating a pulse of light of a wavelength;

directing the generated pulse of light into the cloud atmosphere;

detecting a portion of the pulse of light backscattered by the water particles in the cloud atmosphere;

determining, based on the detected portion of the pulse of light backscattered by the water particles in the cloud atmosphere, an optical extinction coefficient and a backscatter coefficient;

estimating, based on a look-up table and a ratio of the determined optical extinction coefficient to the determined backscatter coefficient, the effective size of the water particles in the cloud atmosphere; and

generating an output signal indicative of the estimated effective size of the water particles in the cloud atmosphere.

8. The method of claim 7, further comprising:

calculating, based on the detected portion of the pulse of light backscattered by the water particles in the cloud atmosphere, a concentration of the water particles in the cloud atmosphere.

9. The method of claim 7, wherein the wavelength of the generated pulse of light is between 700 nano-meters and 2.0 micro-meters.

10. The method of claim 7, further comprising:

polarizing the generated pulse of light, such that the pulse of light directed into the cloud atmosphere is polarized.

11. The method of claim 10, wherein the portion of the pulse of light backscattered by the water particles in the cloud atmosphere is a first portion of the pulse of the circularly polarized light backscattered by the water particles in the cloud atmosphere, the first portion having a first polarization, the method further comprising:

detecting a second portion of the circularly polarized pulse of light backscattered by the water particles in the cloud atmosphere, the second portion having a second polarization oppositely oriented to the first polarization.

12. The method of claim 11, further comprising:

calculating, based on the detected first portion and the detected second portion, an ice/liquid phase ratio of the droplets in the cloud atmosphere.

13. A system for measuring an effective size of water particles in a cloud atmosphere, the system comprising:

a laser;

a signal detector;

one or more processors; and

computer-readable memory encoded with instructions that, when executed by the one or more processors, cause the system to;

emit a pulse of light from the laser;

receive, from the signal detector, a signal indicative of a detected portion of the emitted pulse of light backscattered by the water particles in the cloud atmosphere;

determine, based on the received signal indicative of the detected portion of the emitted pulse of light backscattered by the water particles in the cloud atmosphere, an optical extinction coefficient and a backscatter coefficient;

estimate, based on a ratio of the determined optical extinction coefficient to the determined backscatter coefficient, the effective size of the water particles in the cloud atmosphere by using a look-up table in which the ratio of the determined optical extinction coefficient to the determined backscatter coefficient is correlated to the effective size of water particles; and

generate an output signal indicative of the estimated effective size of the water particles in the cloud atmosphere.

14. The system of claim 13, wherein the computer-readable memory further encoded with instructions that, when executed by the one or more processors, cause the system to:

calculate, based on the detected portion of the pulse of light backscattered by the water particles in the cloud atmosphere, a concentration of the water particles in the cloud atmosphere.

15. The system of claim 13, wherein the emitted pulse of light has a wavelength between 700 nano-meters and 2.0 micrometers.

16. The system of claim 13, further comprising a polarized configured to circularly polarize the pulse of light emitted from the laser.

17. The system of claim 16, wherein the portion of the pulse of light backscattered by the water particles in the cloud atmosphere is a first portion of the circularly polarized pulse of light backscattered by the water particles in the cloud atmosphere, the computer-readable memory is further encoded with instructions that, when executed by the one or more processors, cause the system to:

detect a second portion of the circularly polarized pulse of light backscattered by the water particles in the cloud atmosphere, the second portion having a second polarization oppositely oriented to the first polarization; and

calculate, based on the detected first portion and the detected second portion, an ice/liquid phase ratio of the droplets in the cloud atmosphere.