Measuring cloud metrics using diverging quasi-optical radar

• US 10,444,368 B2
• Filed: 08/18/2016
• Issued: 10/15/2019
• Est. Priority Date: 08/18/2016
• Status: Active Grant

• Current Assignee: Rosemount Aerospace, Inc. (Raytheon Technologies Corporation d/b/a RTX)
• Original Assignee: Rosemount Aerospace, Inc. (Raytheon Technologies Corporation d/b/a RTX)
• Inventors: Ray, Mark, Anderson, Kaare Josef, Miller, Mark Sherwood
• Primary Examiner(s): Hellner, Mark
• Application Number:
  US15/240,438
• Publication Number:
  US 20180052237A1
• Time in Patent Office: 1,153 Days
• Field of Search: 356 401
• CPC Class Codes: B64D 15/20 Means for detecting icing or initiating de-icing
• CPC Class Codes: B64D 45/00 Aircraft indicators or protectors not otherwise provided for camouflage F41H3/00
• CPC Class Codes: G01S 13/865 Combination of radar systems with lidar systems
• CPC Class Codes: G01S 13/953 mounted on aircraft
• CPC Class Codes: G01S 17/95 for meteorological use
• CPC Class Codes: G01S 7/026 involving the transmission of elliptically or circularly polarised waves
• CPC Class Codes: G01S 7/28 Details of pulse systems
• CPC Class Codes: G01S 7/4818 using optical fibres
• CPC Class Codes: G01S 7/483 Details of pulse systems
• CPC Class Codes: G01S 7/499 using polarisation effects
• CPC Class Codes: H01P 1/161 sustaining two independent orthogonal modes, e.g. orthomode transducer combining or separating polarisations and frequencies H01P1/2131
• CPC Class Codes: H01P 1/173 using a conductive element
• CPC Class Codes: H01Q 13/02 Waveguide horns
• CPC Class Codes: H01Q 5/22 RF wavebands combined with non-RF wavebands, e.g. infrared or optical
• 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, based on a detected portion of a projected pulse of quasi-optical energy backscattered by water particles within a divergent projection volume of a cloud atmosphere, properties of the backscattering water particles. The pulse of quasi-optical energy is projected into the divergent projection volume of the cloud atmosphere. The divergent projection volume is defined by an axis of projection and an angle of projection about the axis of projection. The portion of the projected pulse of optical energy backscattered by water particles within the divergent projection volume of the cloud atmosphere is received and detected. Various properties of the backscattering water particles, which can be determined from the detected portion of the projected pulse backscattered by water particles can include particle density and/or particle size.

Claims

1. A system for measuring metrics of backscattering populations of water particles of a cloud atmosphere, the system comprising:

a quasi-optical transmitter configured to project a pulse of quasi-optical energy from a horn aperture into a first divergent projection volume of the cloud atmosphere, the first divergent projection volume defined by a first axis of projection and a first angle of projection about the first axis of projection, the first angle of projection based on a ratio of a transverse dimension of the horn aperture to a wavelength of the quasi-optical energy;

a quasi-optical receiver configured to detect a portion of the projected pulse of quasi-optical energy backscattered by a first backscattering population of water particles within the first divergent projection volume of the cloud atmosphere;

a cloud metric calculator configured to determine, based on a first detected portion of the projected pulse of quasi-optical energy backscattered by the first backscattering population of water particles within the first divergent projection volume of the cloud atmosphere, a first density of the first backscattering population of water particles within the first divergent projection volume of the cloud atmosphere;

an optical transmitter configured to generate a pulse of optical energy;

a transmitter fiber configured to receive the generated pulse of optical energy and to project the received pulse of optical energy from a transmission end of the optical fiber into a second divergent projection volume of the cloud atmosphere, the second divergent projection volume defined by a second axis of projection and a second angle of projection about the second axis of projection, the second angle of projection based on the numerical aperture of the fiber; and

a receiver fiber configured to receive a portion of the projected pulse of optical energy backscattered by a second backscattering population of water particles within the second divergent projection volume of the cloud atmosphere,

wherein the cloud metric calculator is further configured to determine, based on a detected portion of the projected pulse of optical energy backscattered by the second backscattering population of water particles within the second divergent projection volume of the cloud atmosphere, a second density of the second backscattering population of water particles within the divergent projection volume of the cloud atmosphere.

2. The system of claim 1, wherein the quasi-optical transmitter is further configured to polarize the pulse of quasi-optical energy in a first polarization state.

3. The system of claim 1, wherein the quasi-optical receiver is further configured to filter the portion of the projected pulse of quasi-optical energy backscattered by the backscattering population of water particles of the cloud atmosphere, the filtered portion having a second polarization state.

4. The system of claim 1, wherein the quasi-optical transmitter and the quasi-optical receiver are components of an orthomode transducer.

5. The system of claim 4, wherein the orthomode transducer is a septum orthomode transducer.

6. The system of claim 1, wherein the ratio of the transverse dimension of the horn aperture to the wavelength of the projected quasi-optical energy is between 3.0 and 4.0.

7. The system of claim 1, wherein the angle of projection is greater than 15 degrees about the axis of projection.

8. The system of claim 1, wherein the wavelength of the projected pulse of quasi-optical energy is between 100 micrometers and 10 millimeters.

9. The system of claim 1, wherein the cloud metric calculator is further configured to estimate, based on the detected portion of the projected pulse of quasi-optical energy backscattered by the backscattering population of water particles within the divergent projection volume of the cloud atmosphere, an effective size of the backscattering population of water particles within the divergent projection volume of the cloud atmosphere.

10. The system of claim 1, wherein the second axis of projection is oriented within 10 degrees of the first axis of projection.

11. The system of claim 1, wherein the second angle of projection is within 10 degrees of the first angle of projection.

12. The system of claim 1, wherein the transmitter fiber runs longitudinally within a septum of an orthomode septum transducer.

19. The system of claim 1, wherein the wavelength of the generated pulse of optical energy is between 0.7 microns and 2.0 microns.

13. A method for measuring metrics of backscattering populations of water particles of a cloud atmosphere, the method comprising:

projecting a pulse of quasi-optical energy into a first divergent projection volume of the cloud atmosphere, the first divergent projection volume defined by a first axis of projection and a first angle of projection about the first axis of projection, the first angle of projection based on a ratio of a transverse dimension of a transmitting aperture to a wavelength of the quasi-optical energy;

receiving a portion of the projected pulse of quasi-optical energy backscattered by a first backscattering population of water particles within the first divergent projection volume of the cloud atmosphere;

determining, based on a detected portion of the projected pulse of quasi-optical energy backscattered by the first backscattering population of water particles within the first divergent projection volume of the cloud atmosphere, a first density of the backscattering population of water particles within the first divergent projection volume of the cloud atmosphere;

projecting a pulse of optical energy into a second divergent projection volume of the cloud atmosphere, the second divergent projection volume defined by a second axis of projection and a second angle of projection about the second axis of projection;

receiving a portion of the projected pulse of optical energy backscattered by a second backscattering population of water particles within the second divergent projection volume of the cloud atmosphere; and

determining, based on a detected portion of the projected pulse of optical energy backscattered by the second backscattering population of water particles within the second divergent projection volume of the cloud atmosphere, a second density of the second backscattering population of water particles within the second divergent projection volume of the cloud atmosphere.

14. The method of claim 13, wherein the angle of projection is greater than 15 degrees.

15. The method of claim 13, wherein the wavelength of the projected quasi-optical energy is between 100 micrometers and 10 millimeters.

16. The method of claim 13, further comprising:

estimating, based on a detected portion of the projected pulse of optical energy backscattered by the backscattering population of water particles within the divergent projection volume of the cloud atmosphere, an effective size of the backscattering population of water particles within the divergent projection volume of the cloud atmosphere.

17. The method of claim 13, wherein an intersection of the first and the second divergent projection volumes is at least 90% of each of the first and the second divergent projection volumes.

18. The method of claim 13, wherein the wavelength of the generated pulse of quasi-optical energy is between 1.0 mm and 2.7 mm.