Abstract:
PROBLEM TO BE SOLVED: To provide a device where by detecting the presence of floating droplet and by measuring transverse scattering of the beam when laser beam penetrates clouds, information reflecting profile of the diameter of these droplets is provided. SOLUTION: An in-flight multiple field-of-view water droplet sensor includes an illumination portion and a detection portion. The illumination portion includes a first optical beam emitter configured to output a light beam. The detection portion includes a kaleidoscope configured to channel a first portion of the backscattered light towards an inner reflective surface of a circle-to-line converter, a multiple field-of-view subsystem having at least a first detector configured to receive light reflected by the circle-to-line converter, and a single field-of-view subsystem configured to receive a second portion of the backscattered light, the second portion not having been reflected by the circle-to-line converter. The single field-of-view subsystem may include a dual channel circular polarization detector for distinguishing between liquid water droplets and ice crystals based on information in the single field-of-view. COPYRIGHT: (C)2011,JPO&INPIT
Abstract:
PROBLEM TO BE SOLVED: To provide an apparatus for optically detecting and identifying liquid waterdrops and ice crystals in the air, including an irradiation part and a detection part. SOLUTION: The irradiation part outputs irradiated beams of circularly polarized light. The detection part receives back-scattered light of circularly polarized light from water content in clouds, in response to irradiation beam. The back-scattered light of circularly polarized light is passed through a circularly polarized light device and converted to the back scattered light of linearly polarized light, and the converted light is divided into two components. By an optional selection, each of the two components is subjected to further receiving a linearly polarized light for removing all orthogonally polarized light of leakage type. Next, two components are detected optically and by using the resulting detection signal, one or more parameters reflecting the presence/absence of ice crystal and/or waterdrops in the air are calculated. COPYRIGHT: (C)2010,JPO&INPIT
Abstract:
A device for optically detecting and distinguishing airborne liquid water droplets and ice crystals includes an illumination portion and a detection portion. The illumination portion (312) outputs a circularly polarized illuminating beam (318). The detection portion receives circularly polarized backscattered light from moisture in the cloud, in response to the illuminating beam. The circularly polarized backscattered light (322) is passed through a circular polarizer (333) to convert it into linearly polarized backscattered light, which is split into two components. Each of the two components is optionally subject to further linear polarization to filter out any leakage-type orthogonal polarization. The two components are then optically detected and the resulting detection signals are used to calculate one or more parameters reflective of the presence or absence of airborne ice crystals and/or water droplets.
Abstract:
In one aspect, methods of determining a size distribution of water droplets in a cloud are described herein. In some embodiments, a method of determining a size 5 distribution of water droplets in a cloud comprises sampling a depth of the cloud with a beam of electromagnetic radiation, measuring a scattering signal of the electromagnetic radiation returned from the cloud over a range of field of view angles to provide a measured scattering curve [proa,(O)], removing a portion of the measured scattering curve, replacing the removed portion with an extrapolation of the remaining measured scattering 10 curve to provide an estimated scattering curve, and determining a first estimate droplet size distribution [nt1)(D)] from the estimated scattering curve. r --- - gO) I ) 0) E -S* ' 0 uE E*1 = COD C) 0 =C ?=, ar :C 0 CD cEO) wa) a) M C E0 0 U =)~~~~ - )m II) 0i E >cJ - E) - n a) Z (0 (O!a)' a) )~ CW 0 J to 0- cu, :ZL a)U E~a ixL ) 0 6c' a) Ea E. 10 U) U n 0' u )c 3( 0) .0 C 0 0 0 M Ot cli ) m * = > E i0)0 33 1 ? E E L) -p- -c- .- )~ 0_ 00 -M c 0L :3 z 0 0~ Q) U ' L)Cl)0 0 o c'D -------
Abstract:
In one aspect, methods of determining a size distribution of water droplets in a cloud are described herein. In some embodiments, a method of determining a size distribution of water droplets in a cloud comprises sampling a depth of the cloud with a beam of electromagnetic radiation, measuring a scattering signal of the electromagnetic radiation returned from the cloud over a range of field of view angles to provide a measured scattering curve [P total(.theta.)], removing a portion of the measured scattering curve, replacing the removed portion with an extrapolation of the remaining measured scattering curve to provide an estimated scattering curve, and determining a first estimate droplet size distribution [n(1)(D)] from the estimated scattering curve.
Abstract:
In one aspect, methods of determining a size distribution of water droplets in a cloud are described herein. In some embodiments, a method of determining a size distribution of water droplets in a cloud comprises sampling a depth of the cloud with a beam of electromagnetic radiation, measuring a scattering signal of the electromagnetic radiation returned from the cloud over a range of field of view angles to provide a measured scattering curve [P total(.theta.)], removing a portion of the measured scattering curve, replacing the removed portion with an extrapolation of the remaining measured scattering curve to provide an estimated scattering curve, and determining a first estimate droplet size distribution [n(1)(D)] from the estimated scattering curve.
Abstract:
An airborne multiple field-of-view water droplet sensor includes an illumination portion and a detection portion. The illumination portion includes a first optical beam emitter configured to output a light beam. The detection portion includes a kaleidoscope configured to channel a first portion of the backscattered light towards an inner reflective surface of a circle-to-line converter, a multiple field of view subsystem having at least a first detector configured to receive light reflected by the circle-to-line converter, and a single field-of-view subsystem configured to receive a second portion of the backscattered light, the second portion not having been reflected by the circle-to-line converter. The single field-of-view subsystem may include a dual channel circular polarization detector for distinguishing between liquid water droplets and ice crystals based on information in the single field-of-view.
Abstract:
Methods of determining a size distribution of water droplets in a cloud are described herein. In some embodiments, a method of determining a size distribution of water droplets in a cloud comprises sampling a depth of the cloud with a beam of electromagnetic radiation, measuring a scattering signal of the electromagnetic radiation returned from the cloud over a range of field of view angles to provide a measured scattering curve [ p total (¸)], removing a portion of the measured scattering curve, replacing the removed portion with an extrapolation of the remaining measured scattering curve to provide an estimated scattering curve, and determining a first estimate droplet size distribution [ n (1) (D)] from the estimated scattering curve.
Abstract:
In one aspect, methods of determining a size distribution of water droplets in a cloud are described herein. In some embodiments, a method of determining a size distribution of water droplets in a cloud comprises sampling a depth of a cloud with a 5 beam of electromagnetic radiation, measuring echo intensities of the electromagnetic radiation returned from the cloud with a detector, determining a measured optical extinction coefficient from the measured echo intensities, determining a measured backscatter coefficient from the measured echo intensities, determining a lidar ratio from the measured optical extinction coefficient and the measured backscatter coefficient, 10 determining from the lidar ratio a value pair comprising a shape parameter (p) and median volume diameter (DMVD) of the water droplets, and determining a size distribution of the water droplets using the value pair (pt, DMVD). Qa) U) 0 ) c E o (D Z000 U)a C () or :t-- > ) 0 ) C C ) a) ~ a) Lcuf)l E 0 E E 0 a 0aa C) "0 Z0( E: E *Q 0-0 a)cu -0 0- C)- 0 0 a) 0a) C) I o- VZ 0 * 0M C U) 0,2)U)U aa a aD aa E m E E E E ff af C) a) a