Source: https://patents.google.com/patent/US9720082B1/en
Timestamp: 2018-07-16 07:32:34
Document Index: 262066954

Matched Legal Cases: ['art 1300', 'art 1300', 'art 1300', 'art 1900', 'art 1900', 'art 1900', 'art 2000', 'art 2000', 'arts 1300', 'Application No. 13']

US9720082B1 - Weather radar system and method for detecting a high altitude crystal condition using two or more types of radar signals - Google Patents
Weather radar system and method for detecting a high altitude crystal condition using two or more types of radar signals Download PDF
US9720082B1
US9720082B1 US14206651 US201414206651A US9720082B1 US 9720082 B1 US9720082 B1 US 9720082B1 US 14206651 US14206651 US 14206651 US 201414206651 A US201414206651 A US 201414206651A US 9720082 B1 US9720082 B1 US 9720082B1
US14206651
The hazard warning system that included processing system for detecting a high altitude ice crystal (HAIC) condition. The aircraft warning system can use at least two types of radar returns to detect the HAIC condition. Warnings of high altitude ice crystal conditions can allow an aircraft to avoid threats posed by HAIC conditions including damage to aircraft equipment and engines.
The present application is related to U.S. application Ser. No. 14/086,844 filed on Nov. 21, 2013 now U.S. Pat. No. 9,244,166, U.S. application Ser. No. 13/919,406 filed on Jun. 17, 2013 now U.S. Pat. No. 9,244,157, U.S. application Ser. No. 13/841,893 filed Mar. 15, 2013 now U.S. Pat. No. 9,244,166, U.S. application Ser. No. 14/207,034 filed on an even date herewith invented by Koenigs, et al., U.S. application Ser. No. 13/246,769 filed Sep. 27, 2011 now U.S. Pat. No. 9,019,146 and U.S. application Ser. No. 14/206,239, filed on an even date herewith invented by Sishtla, et al., all incorporated herein by reference in their entireties and assigned to the assignee of the present application.
This specification relates generally to the detection of weather radar hazard. More particularly, this specification relates to the detection of a weather hazard warning related to ice crystals.
Conventional aircraft hazard weather radar systems, such as the WXR 2100 MultiScan™ radar system manufactured by Rockwell Collins, Inc., have Doppler processing and are capable of detecting at least four parameters: weather range, weather reflectivity, weather velocity, and weather spectral width or velocity variation. The weather reflectivity is typically scaled to green, yellow, and red color levels that are related to rainfall rate. The radar-detected radial velocity variation can be scaled to a turbulence level and displayed as magenta. Such weather radar systems can conduct vertical sweeps and obtain reflectivity parameters at various altitudes.
Radar reflectivity levels in and around the convective regions at high altitudes associated with high altitude, thin ice crystal formation have typically been very low and can be difficult to detect. Conventional X-band radar systems have insufficient energy on the target to detect and discriminate high altitude ice crystal clouds based upon reflectivity levels alone. It is difficult to distinguish low reflectivity precipitation areas from areas of high altitude ice crystal (HAIC) formation and HAIC clouds (HAIC2). Detection and display of high altitude ice crystallization areas is desirous because the icing events caused by HAIC and/or high altitude ice crystal cloud (HAIC2) conditions can have a direct impact on aircraft, crew and passengers depending on the severity of the accretion.
Thus, there is a need for an aircraft hazard warning system and method that senses high altitude ice crystal (HAIC) or high altitude ice crystal cloud (HAIC2) conditions. There is also a need for a hazard detection system that detects and displays high altitude associated threat (HAIC) or high altitude ice crystal cloud (HAIC2) warnings. There is also a need for a direct (non-inferred) HAIC or HAIC2 detection system and method. Yet further, there is a need for an aircraft hazard warning system that alerts a pilot to HAIC or HAIC2 conditions and can detect such conditions at a distance large enough to allow aircraft route changes.
An exemplary embodiment relates to an aircraft hazard warning system. The aircraft hazard warning system includes a processing system for detecting a high altitude ice crystal (HAIC) condition.
An exemplary embodiment relates to an aircraft hazard warning system. The aircraft hazard warning system includes comprising a processing system for detecting a high altitude ice crystal (HAIC) condition. The processing system uses at least two types of radar signals to detect the HAIC condition.
Another exemplary embodiment relates to a method of detecting a high altitude ice crystal (HAIC) condition on an aircraft using an electronic processor. The method includes receiving radar reflectivity data associated with a first type radar signal and a second type radar signal, and processing the radar reflectivity data to determine the HAIC condition exists by using the radar reflectivity data associated with the first type radar signal with the radar reflectivity data from the second type radar signal.
Another exemplary embodiment relates to an aircraft weather radar system. The aircraft weather radar system includes a radar antenna for receiving radar returns; and means for determining a high altitude ice crystal (HAIC) condition in response to at least two types of radar returns.
FIG. 6 is a flow diagram showing a process performed by the weather radar system illustrated in FIG. 3 for HAIC detection, according to an exemplary embodiment.
FIG. 7 is a more detailed block diagram of a sequential dual polarization architecture with a passive antenna for the weather radar system illustrated in FIG. 3 in accordance with another exemplary embodiment.
FIG. 8 is a more detailed block diagram of a simultaneous dual polarization architecture with a passive antenna for the weather radar system illustrated in FIG. 3 in accordance with yet another embodiment.
FIG. 9 is more detailed schematic block diagram of a simultaneous dual polarization architecture with an active antenna for the weather radar system illustrated in FIG. 3 in accordance with another exemplary embodiment.
FIG. 10 is a schematic perspective view illustration of a passive dual polarization antenna illustrated in FIGS. 7 and 8 in accordance with another embodiment.
FIG. 11 is a perspective view schematic illustration of an active dual polarization antenna for the architecture illustrated in FIG. 9 in accordance with another exemplary embodiment.
FIG. 12 is a chart showing normalized radar cross section for oblate spheroids (horizontal incidence) versus normalized particle size.
FIG. 13 is a more detailed schematic block diagram of a simultaneous dual frequency architecture with a passive antenna for the weather radar system illustrated in FIG. 3 in accordance with another exemplary embodiment.
FIG. 14 is a more detailed schematic block diagram of a simultaneous dual frequency architecture with an active antenna for the weather radar system illustrated in FIG. 3 in accordance with another exemplary embodiment.
FIG. 15 is a planar view schematic illustration of a passive dual frequency antenna for the architecture illustrated in FIG. 13 in accordance with another exemplary embodiment.
FIG. 16 is a perspective view schematic drawing of a dual frequency active antenna for the architecture illustrated in FIG. 14 in accordance with another exemplary embodiment.
FIG. 17 is a chart showing reflectivity for a random particle size cloud (oblate spheroid Z) versus average particular size for the weather radar system illustrated in FIG. 3 in accordance with another exemplary embodiment.
FIG. 18 is a chart showing reflectivity for a fixed particle size cloud (oblate spheroid Z) versus particular size for the weather radar system illustrated in FIG. 3 in accordance with another exemplary embodiment.
Referring to FIG. 2, the front of an aircraft 101 is shown with aircraft control center 10 and nose 100, according to an exemplary embodiment. A radar system 300 (e.g., a weather radar system or other radar system) is generally located within nose 100 of aircraft 101 or within aircraft control center 10 of aircraft 101. According to various exemplary embodiments, radar system 300 may be located on the top of aircraft 101 or on the tail of aircraft 101 instead. Radar system 300 may include or be coupled to an antenna system. A variety of different antennas or radar systems may be used as part of system 300 (e.g., a split aperture antenna, a monopulse antenna, a sequential lobbing antenna, etc.). In certain embodiments, antenna 310 is a dual, or more than dual frequency antenna or a dual or more than dual polarization antenna.
Processing electronics 304 are further shown as connected to aircraft sensors 314 which may generally include any number of sensors configured to provide data to processing electronics 304. For example, sensors 314 could include temperature sensors, humidity sensors, infrared sensors, altitude sensors, a gyroscope, a global positioning system (GPS), or any other aircraft-mounted sensors that may be used to provide data to processing electronics 304. It should be appreciated that sensors 314 (or any other component shown connected to processing electronics 304) may be indirectly or directly connected to processing electronics 304. Processing electronics 304 are further shown as connected to avionics equipment 312 and include a high altitude ice crystal (HAIC) or HAIC cloud (HAIC2) module 340 and a high altitude associated threat (HAAT) module 334. Modules 340 and 334 advantageously detect and locate HAIC, HAIC2 and HAAT conditions and cause display 20 to provide a visual and/or audio warning of such conditions. Modules 334 and 340 process data associated with weather radar reflectivity levels and/or data from other sensors (e.g., temperature, altitude, etc.) to determine HAIC, HAIC2 and HAAT conditions. Avionics equipment 312 can be or include a flight management system, a navigation system, a backup navigation system, or another aircraft system configured to provide inputs to processing electronics 304. The HAIC or HAIC2 condition can be sensed via a dual frequency or dual polarization process as explained below according to various exemplary embodiments.
Memory 320 is further shown to include HAAT module 334 which includes logic for using radar returns (e.g., data) in memory buffer 324 to make one or more determinations or inferences regarding high altitude associated threats (e.g., threats related to a blow off or anvil region of a weather cell). HAAT conditions can be associated with high severity threat conditions such as hail, lightning, turbulence, etc. For example, HAAT module 334 may be configured to use wind speed, wind direction, and size of a weather cell to predict the presence of an anvil region downwind of a weather cell that may contain lightning, hail, and/or turbulence. HAAT module 334 may be configured to cause a pattern (e.g., a red speckled region) to be displayed on an aviation display 20. For example, HAAT module 334 and module 338 can be configured to output a signal to display control module 338 indicating the existence, location, and severity or risk of the anvil region. HAAT module 334 can detect a HAAT condition based upon the presence of convective cells reaching high altitudes and having anvil shapes. Such conditions can be sensed using the techniques described in U.S. application Ser. Nos. 13/919,406 and 13/84,893. Ice crystals may be present in a HAAT region. A HAAT condition generally is a more significant threat than a HAIC or HAIC2 condition.
Memory 320 is further shown to include HAIC or HAIC2 module 340 which includes logic for using radar returns in memory buffer 324 to make one or more determinations or inferences regarding threats related to a HAIC or HAIC2 condition. Module 340 can be combined with module 338, be a hard wired ASIC, or programmable logic circuit in one embodiment. HAIC module 340 and weather radar system 300 can be configured to use dual frequency or dual polarization processes to detect presence of the HAIC or HAIC2 condition and its location in one embodiment. Dual frequency and dual polarization techniques advantageously allow for providing information on the nature of the scattering environment, thereby providing more accurate ice water content (IWC) estimates which aids discrimination of particle size and particle size distribution for HAIC detection. Alternatively, module 340 and weather radar system 300 can utilize an inferred or non-inferred process discussed in related U.S. patent application Ser. No. 14/206,239 incorporated herein by reference in one embodiment. In one embodiment, HAIC or HAIC2 module receives data associated with weather returns at high altitude and processes the data to determine existence of a HAIC or HAIC2 condition. The data can be processed by comparing the data representing returns of a first type (e.g., polarization or frequency) and returns of a second type (e.g., polarization or frequency) to known ice crystal return characteristics to determine a match and therefore a HAIC or HAIC2 condition. In one embodiment module 340 senses only one of a HAIC or HAIC2 condition.
Memory 320 is further shown to include a beam control module 336. Beam control module 336 may be an algorithm for commanding circuit 302 to sweep a radar beam. Beam control module 336 may be used, for example, to send one or more analog or digital control signals to circuit 302. The control signals may be, for example, an instruction to move the antenna mechanically, an instruction to conduct an electronic beam sweep (of a phased array or electronically scanned array antenna) in a certain way, (e.g., an instruction to move the radar beam to the left by five degrees, etc.). Beam control module 336 may be configured to control timing of the beam sweeps or movements relative to aircraft speed, flight path information, transmission or reception characteristics from weather radar system 300 or otherwise. Beam control module 336 may receive data from configuration data 326 for configuring the movement of the radar beam.
Memory 320 is further shown to include a display control module 338 which includes logic for displaying weather information on aviation display 20. For example, display control module 338 may be configured to display radar return information received from memory buffer 324 and to determine a gain level or other display setting for display of an inferred threat to aircraft 101 on a weather radar display. Display control module 338 may be configured to receive signals relating to threats to aircraft 101 from core threat module 328, overflight module 330, electrified region module 332, HAAT module 334, and HAIC or HAIC2 module 340. Display control module 338 may further be configured to cause, in response to one or more signals received from threat modules 328-334 and 340 and threshold values from configuration data 326, a change in color of a portion of an image on aviation display 20, a pattern (e.g., a speckled region) to be overlaid on an image on aviation display 20, and an icon to be shown on aviation display 20. Display control module 338 may be configured to cause a change in size, location, shape, or color of the colored regions, patterns, symbols, and/or icons in response to updated signals received from modules 328-336 and 340.
HAIC or HAIC2 module 340 and module 338 can be configured to cause a pattern (e.g., a yellow speckled region) to be displayed on an aviation display 20 to indicate a HAIC warning in one embodiment. HAIC or HAIC2 module 340 is configured to output a signal or data to display control module 338 indicating the existence, location, and severity or risk of the HAIC or HAIC2 condition or region in one embodiment. Module 338 can cause the appropriate video signal to be provided to display 20. An indication that the HAIC or HAIC2 warning is based on dual frequency or dual polarization analysis as described below or on an inferred processing or non-inferred processing as described in U.S. patent application Ser. No. 14/206,239, incorporated herein by reference according to various embodiments. Module 340 and module 338 can operate to provide the displays described in U.S. patent application Ser. No. 14/207,034, incorporated herein by reference in one embodiment.
With reference to FIG. 6, processing electronics 304 and module 340 (FIG. 3) can operate according to a process 650 for detecting a HAIC or HAIC2 condition. At a step 652, weather system 300 provides radar beams having a first characteristic to an area. The first characteristic can be a first frequency band (e.g., X band, W band, Ka band, etc.) or a first polarity type (e.g., horizontal, vertical, circular, etc.). At a step 653, system 300 provides radar beams having a second characteristic to the area. The second characteristic can be a second frequency different from the first frequency (e.g., X band, W band, Ka band, etc.), or a second polarity type different from the first polarity type (vertical, horizontal, circular, etc.). Steps 652 and 653 can be performed sequentially or simultaneously.
At a step 654, system 300 receives radar returns having the first characteristic from the area. In one embodiment, the radar returns are horizontally polarized returns from horizontally polarized beams ((HH) radar returns) or vertically polarized returns from vertically polarized beams ((VV) radar returns). At a step 656, weather radar system 300 receives radar returns having the second characteristic (e.g., VV or HH) from the area. In one embodiment, the second characteristic can be VV radar returns and the first characterized can be HH radar returns. In one embodiment, the first characteristic of the returns can be a first frequency band (e.g., X band) and the second characteristic of the returns can be a second frequency band (e.g., W, Ka, etc.) Steps 654 and 656 can be performed sequentially or simultaneously. At a step 658, the returns are analyzed to determine HAIC or HAIC2 characteristics by determining particle sizes and shapes and comparing to known particle sizes and shapes for HAIC or HAIC2 conditions in one embodiment. The returns can be compared to known returns for the different return characteristics for HAIC or HAIC2 conditions.
With reference to FIG. 7, weather radar system 300 can be configured to have an architecture 700 comprising a weather radar receiver (W×R) 702, a down converter 704, a dual polarization transmit/transmit duplexer 710, an interface 720, a passive antenna 718 and a power amplifier 712. Receiver 702, converter 704, power amplifier 712 and duplexer 710 can be part of circuit 302 (FIG. 3) or electronics 304. Power amplifier 712 operates to provide radar signals with a first polarization state and radar signals with a second polarization state sequentially. The radar signals are provided through duplexer 710 to antenna 718 for transmission. The frequency source may or may not be coherent for architecture 700.
Returns associated with the radar signals are received sequentially by antenna 718 and provided via interface 720 to duplexer 706. Duplexer 706 provides returns in a first polarization state to a first input of converter 704 and returns of a second polarization state at a second input of converter 704. The first polarization state can be horizontal (e.g., HH), and the second polarization state can be vertical (e.g., VV) in one embodiment. The returns received by down converter 704 are down converted and provided to receiver 702 and to input 355 of electronics 304 (FIG. 4) for processing. Electronics 304 and module 340 can process data associated with the radar returns to provide analysis for an HAIC or HAIC2 condition.
Architecture 700 advantageously only requires a single power amplifier 712 for providing power to both polarizations in one embodiment. Time multiplexing for both polarizations can degrade other radar scanning missions and can slow down HAIC and/or HAIC2 detection and discrimination in certain embodiments.
With reference to FIG. 8, an architecture 800 includes W×R receiver 702, down converter 704, a dual port transmit/receive duplexer 810, interface 720, a first type polarization power amplifier 812, a second type polarization amplifier 814, and passive antenna 718. Architecture 800 can simultaneously provide dual polarization radar signals (e.g., horizontal and vertical polarization signals) through duplexer 812 to antenna 718 to provide a radar beam with horizontal and vertical polarized energy. The polarizations can be dual orthogonal polarization in one embodiment. Returns are received by antenna 718 and returns of a first polarization type (e.g., HH) and a second polarization type (e.g., VV) are provided through down converter 704 to receiver 702 for processing.
Architecture 800 provides polarization agility and can utilize horizontal, vertical, linear polarization, circular polarization, elliptical polarization, horizontal transmit, horizontal/vertical receive/transmit and vice versa to provide additional information on particle shapes and sizes and ice water content for more accurate discrimination and fewer false alarms in one embodiment. Architecture 800 requires at least one additional power amplifier and associated connections in one embodiment.
With reference to FIG. 9, an architecture 900 includes W×R receiver 702, down converter 704, interface 720, duplexer 810, power amplifier 812, power amplifier 814, duplexer 810 and antenna 724. Antenna 724 is an active antenna in one embodiment. Radar signals of two polarization types can be simultaneously provided by amplifiers 812 and 814 through duplexer 810 to antenna 724. Antenna 724 can provide a dual polarization beam at a first time and a dual polarization time at a second time. Returns can be received through duplexer 810 and down converter 704 by W×R receiver 702 for processing for HAIC and HAIC2 condition detection. Architecture 900 advantageously allow regions of potential HAIC or HAIC2 conditions to be revisited almost instantaneously for verification and additional HAIC discrimination measurements.
With reference to FIG. 10, antenna 718 can be provided as a passive antenna with interspersed horizontal broad wall and vertical edge wall waveguide slots. Slots 723 can be used for horizontal polarization and slots 721 can be provided for vertical polarization in one embodiment. Antenna 718 can provide simultaneous dual channel returns or sequential single channel returns.
With reference to FIG. 11, antenna 724 is an active antenna and includes dual polarization elements. Antenna 724 can have simultaneous dual channels or a sequential single channel. Antenna 724 can be either mechanically or electronically scanned in either one or two dimensions in one embodiment.
With reference to FIG. 12, chart 1300 shows normalized radar cross section (RCS)
( σ π ⁢ ⁢ a 2 )
for an oblate spheroid having a dimension a in the X and Y directions and dimension b in the Z direction (See diagram 901). An X axis 1302 of chart 1300 provides normalized particle size in kD, where
and D=2a. λ is me wave length of the radar beam. A Y axis 1304 represents normalized radar cross section (RCS)
( σ π ⁢ ⁢ a 2 ) .
Generally, particles in a HAIC condition have various sizes and shape. For non-spherical particles, the radar cross section (RCS) depends on polarization. H polarization has an e-vector in the X-Y plane, and vertical polarization has an e-vector in the Z direction. Accordingly, polarization makes a difference in particle radar cross section. Chart 1300 assumes a particle shape having α=0.6, where α=b/a.
A curve 1306 and a curve 1308 demonstrate RCS differences due to polarization. The RCS differences can be utilized to discriminate particle shapes.
With reference to FIG. 13, an architecture 1350 includes weather radar receiver 702, down converter 704, dual port transmit/receiver duplexer 706 an interface 720, an X band power amplifier 752 and a W Band power amplifier 754 in one embodiment. X Band radar signals and W Band radar signals can be provided through duplexer 702 to a dual frequency antenna 760 in one embodiment. Antenna 760 can be a passive antenna in one embodiment.
Returns associated with the W beam and the X beam can be received through duplexer 706, down converter 704 by receiver 702 for processing for detection of HAIC or HAIC2 conditions. Alternatively, frequency bands can be utilized. Power amplifiers at higher frequencies are generally less efficient (e.g., 25% at X and 20% at Ka and 10% at W) in certain embodiments and noise figures can increase with frequency (e.g., 3 dB at X, 4 dB at Ka and 5 dB at W band).
Frequency diversity provides additional information on particle sizes and ice water content for more accurate discrimination and fewer false alarms in one embodiment. In addition, if W band is utilized with the same beamwidths as the X-band antenna, the new aperture is 1/100th of the area of the X band antenna, and the W band antenna can fit on the X band aperture without degradation of the X band signal in one embodiment. In addition, the W band portion of the antenna can use the same gimbal in one embodiment. Alternatively, other frequency bands besides X and W can be utilized including Ka bands, etc.
With reference to FIG. 14, an architecture 1400 includes weather radar receiver 702, down converter 704, dual port transmit/receive duplexer 706, power amplifier 752, interface 720 power amplifier 754 and an active antenna 762. X band and W band radar signals are provided through duplexer 706 to antenna 762 in one embodiment. Radar returns from the X band and W band radar signals are received through duplexer 706 and down converter 704. Receiver 702 receives the returns for processing to detect HAIC conditions.
Architecture 1400 advantageously provides little or no degradation to current weather radar missions in one embodiment. Architecture 1400 provides the advantage to revisit almost instantaneously regions of potential HAIC2 for verification and additional measurements in one embodiment.
With reference to FIG. 15, antenna 760 includes a W band aperture 768 ( 1/10th× 1/10th) antenna at the center of the X band aperture 770. Ka-band elements can also be interlaced with X band elements for Ka band isolation. Antenna 760 can be provided as the same size as an X band antenna with less than twice the weight and less than twice the cost in one embodiment. However, power required for antenna 706 can be increased by more than 2 times in one embodiment.
With reference to FIG. 16, antenna 762 is an active antenna including an antenna 780 inserted at the center corner of a lower frequency (e.g., X band) antenna 782. The relationship between sizes of the high frequency antenna to the lower frequency antenna is
Aperture ⁢ ⁢ Size ⁢ ⁢ Scale ⁢ ⁢ Factor = [ λ l ⁢ ⁢ high ⁢ ⁢ freq ⁢ ⁢ band λ low ⁢ ⁢ freq ⁢ ⁢ band ] 2
The higher frequency antenna can conceptually be placed anywhere within the lower frequency (e.g., X Band) AESA (Active Electronically Scanned Array) antenna. Additionally, multiple (e.g. W Band) antenna can be integrated into the lower frequency (X Band) AESA panels as system needs dictate, e.g. an, increase higher frequency sensitivity, or multiple higher frequency antennas can have polarization diversity, along with frequency diversity. The specific example herein is X/W B according to one embodiment and, however, other widely separated frequency band combinations may be used in other embodiments. A W Band antenna can be placed anywhere within the X Band AESA (Active Electronically Scanned Array) antenna in one embodiment. Additionally, a multiple W Band antenna can be integrated into two X Band AESA panels. Multiple band (W, X, etc.) antennas can have polarization diversity, along with X/W Band frequency diversity in some embodiments. The power is increased by greater than 2 times and the cost is increased by 2 times. Generally, current weather radar radomes are not wideband transmissive, and antenna 762 can compensate for randome distortion at high frequency.
With reference to FIG. 17, a chart 1900 of frequency diversity effect on particle reflectivity includes a Y axis 1904 representing reflectivity (Z, dB mm6/mm3), and an X axis 1902 representing average particle size in millimeters. Chart 1900 provides oblate spheroid reflectivity versus frequency for the gamma particle size distributions with μ=2. Chart 1900 assumes ice water content of one gram per meter cubed and a random particle size cloud.
A curve 1920 shows an X band response, a curve 1922 shows a Ka band response and a curve 1924 shows a W band response. Due to differences in scattering regimes such as Rayleigh and Mie scattering, particles have different radar reflectivities at different wavelengths as shown by curves 1920, 1922 and 1924. Comparison of reflectivity for two or more frequencies provides information on average particle size.
With reference to FIG. 18, a chart 2000 shows oblate spheroid reflectivity versus frequency for a fixed particle size cloud. The ice water content is assumed to be one gram per meter cubed. An X axis 2002 represents particle size in mm, and a Y axis 2004 represents reflectivity (Z dB mm6/mm3). Curve 2020 is associated with an X band radar signal, curve 2022 is associated with a Ka band, and curve 2024 is associated with a W band. As can be seen in chart 2000, transition from Rayleigh and Mie scattering depends on frequencies and particle shape to a minor extent. Comparison of reflectivity for two or more frequencies provides information on the particle size in a fixed particle size cloud.
System 300 can utilize data associated with charts 1300, 1900 and 2000 to determine particle size and shape. The identification of particle size and shape can be used to discriminate ice particles from non-ice particles. Accordingly, by comparing radar returns associated with two or more signal characteristics, system 300 can determine information about particles for discrimination of those particles being ice (being an HAIC and HAIC2 condition) or non-ice according to one embodiment. For example, dual polarization or dual frequency can allow discrimination between ice and super cooled water at high altitudes.
In one embodiment, returns can be compared to historical return characteristics at varying polarizations and frequencies to determine a match. The historical returns can be provided on a location by location or geographic type basis (e.g., continental, maritime, etc.). In one embodiment, ice particles in globe-like sphere form have a long dimension that is aligned in accordance with aerodynamic forces and/or electric fields associated with weather cells. Generally, a larger variation between horizontal and vertical polarization can mean a higher probability of ice presence. By comparing returns in horizontal or vertical polarizations, asymmetric particles can be distinguished from non-asymmetric particles or clouds containing asymmetrical particles can be distinguished from clouds not containing asymmetric particles.
Generally, larger particle sizes indicate a presence of ice as super cooled water tends to be small and spherical. Accordingly, the dual frequency technique provides information about size of particles for determination of a HAIC2 and HAIC condition. In one embodiment, the frequency difference between the two bands is large to provide better distinction between returns and particle sizes.
Although amplifiers 712, 812, 814, 752 and 754 are shown as a standalone module in FIGS. 7, 8, 9, 13, and 14, W×R receiver 702 can be an X Band or C Band weather radar receiver that is coherent to either the dual band or dual polarization in certain embodiments. The Tx and Rx chains can be derived from a common frequency source that is up-converted to the X Band Tx drive signal and the X Band Rx local oscillators to maintain coherency. An up converter tied to receiver 702 can be included in certain embodiments.
Although architectures 700, 800, 900, 1300, and 1400 include common components, entirely separate paths can be provided for different radar types (e.g., a separate path for a first polarization and a second polarization type and a separate path for X band and W band in one embodiment). Independent radar systems for dual polarization, or dual/tri-band frequency diversity, or both can be self-contained coherent systems in some embodiments.
In some embodiments, the ratio of phase can also be utilized for both dual polarization and/or dual frequency systems. Specific differential phase can be used to identify characteristics associated with HAIC and HAIC2 in certain embodiments. conditions.
a processing system associated with an active radar system configured to detect a high altitude ice crystal (HAIC) or high altitude ice crystal cloud (HAIC2) condition using at least two types of radar signals, wherein a first type of radar return and a second type of radar return are processed to: 1. determine a size of particles in a high altitude region for detecting at least one of the HAIC or HAIC2 condition where a larger size indicates the at least one of the HAIC or HAIC2 condition; or 2. determine a shape of the particles for detecting the at least one of the HAIC or HAIC2 condition where a less spherical shape indicates the at least one of the HAIC or HAIC2 condition, wherein the processing system causes a display to provide at least one of a HAIC or HAIC2 warning in response to detection of the at least one of the HAIC or HAIC2 condition;
an antenna system comprising an X band antenna having first elements for a first polarization signal in an X band and second elements for a second polarization signal in the X band and a W band antenna for a signal in the W band, the W band antenna being disposed in a face of the X band antenna;
a duplexer, wherein a first path and a second path is disposed between the downconverter and the duplexer, wherein the first path is for the first type of the return from a first type of radar signal of the two types of radar signals and the second path is for the second type of return from a second type radar signal of the two types of radar signals, wherein the first type of radar signal is the first polarization signal in the X band and the second type of radar signal is the second polarization signal in the X band or the first type of radar signal is in the X band and the second type of radar signal is the signal in the W band.
2. The aircraft hazard warning system of claim 1, wherein the two types of radar signals comprise the first polarization signal in the X band and the second polarization signal in the X band.
3. The aircraft warning system of claim 1, wherein the two types of radar signals comprise the first type radar signal being at a first polarization and the second type radar signal being at a second polarization.
4. The aircraft warning system of claim 3, wherein the HAIC condition is detected using the at least two types of radar signals after a region of interest is identified.
5. The aircraft warning system of claim 1, wherein the processing system determines a region of interest using an inferred process.
6. The aircraft hazard warning system of claim 5, wherein the inferred process uses a temperature anomaly detection.
7. The aircraft hazard warning system of claim 2, wherein the first type radar signal is an X band frequency and the second type radar signal is a millimeter Ka, or W band frequency.
8. The aircraft hazard warning system of claim 3, wherein the first polarization signal is an H polarization signal and the second polarization signal is a V polarization signal.
9. The aircraft hazard warning system of claim 8,
wherein the antenna system is an active scanning array antenna system.
10. The aircraft hazard warning system of claim 9, wherein the antenna system is electronically steerable.
11. A method of detecting a high altitude ice crystal (HAIC) condition or a high altitude ice crystal cloud (HAIC2) condition on an aircraft using an electronic processor associated with an active radar system, the method comprising:
providing a first type of radar signal to an antenna system, the antenna system comprising an X band antenna having first elements for a first polarization signal in an X band and second elements for a second polarization signal in the X band and a W band antenna for a signal in the W band, the W band antenna being disposed in a face of the X band antenna;
providing a second type of radar signal to the antenna system;
receiving a first type of radar return from the first type of radar signal on a first receive path and a second type of radar return from the second radar signal on a second receive path;
processing the first type of radar return and the second type of radar return to determine at least one of HAIC or HAIC2 condition, wherein the first type of radar return and the second type of radar return are processed to: 1. determine a size of particles in a high altitude region for detecting the HAIC or HAIC2 condition where a larger size indicates at least one the HAIC or HAIC2 condition; or 2. determine a shape of the particles for detecting at least one of the HAIC or HAIC2 condition where a less spherical shape indicates the at least one of the HAIC or HAIC2 condition; and
displaying at least one of a HAIC or HAIC2 warning in response to detection of the at least one of the HAIC or HAIC2 condition.
12. The method of claim 11, wherein the HAIC warning of the HAIC condition is provided on a weather radar display.
14. The method of claim 11, wherein the first type radar return is associated with a first frequency and the second type radar return is associated with a second frequency.
15. The method of claim 11, wherein the first type radar return is associated with a first polarization and the second type radar return is associated with a second polarization.
16. The method of claim 11, wherein the HAIC warning of the HAIC condition is provided as a speckled region on a plan view display.
17. An active aircraft weather radar system, comprising:
a radar antenna for receiving two types of radar return signals; and
means for determining a high altitude ice crystal (HAIC) condition in response to at least the two types of radar return signals, wherein the two types of radar return signals are processed to: 1. determine a size of particles in a high altitude region for detecting at least one of the HAIC condition where a larger size indicates the HAIC condition; or 2. determine a shape of the particles for detecting the HAIC condition where a less spherical shape indicates the HAIC condition, wherein the processing system causes the display to provide a HAIC warning in response to detection of the HAIC condition;
a duplexer, wherein a first path and a second path is disposed between the downconverter and the duplexer, wherein the first path is for a first type of return of the two types of radar return signals and the second path is for a second type of return of the two types of radar return signals, wherein the first type of radar signal is the first polarization signal in the X band and the second type of radar signal is the second polarization signal in the X band or the first type of radar signal is in the X band and the second type of radar signal is the signal in the W band.
18. The weather radar system of claim 17 wherein the display provides weather images.
20. The aircraft weather radar system of claim 19, wherein the warning of the HAIC condition is provided in response to a comparison of the two types of returns.
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