The present application is related to U.S. patent application Ser. No. 14/465,753 filed on Aug. 21, 2014 by Breiholz et al., entitled “Weather Radar System and Method With Fusion of Multiple Weather Information Sources,” to U.S. patent application Ser. No. 14/162,035 filed on Jan. 23, 2014 by Kronfeld et al., entitled “Weather Radar System and Method With Path Attenuation Shadowing,” to U.S. patent application Ser. No. 14/086,844 filed on Nov. 21, 2013 by Breiholz et al., entitled “Weather Radar System and Method for Estimating Vertically Integrated Liquid Content,” to U.S. patent application Ser. No. 14/465,730 filed on Aug. 21, 2014 by Breiholz et al., entitled “Weather Radar System and Method With Latency Compensation for Data Link Weather Information,” to U.S. patent application Ser. No. 14/323,766 filed on Jul. 3, 2014 by Shimon et al., entitled “Efficient Retrieval of Aviation Data and Weather Over Low Bandwidth Links,” and to U.S. patent application Ser. No. 14/608,071 filed on Jan. 28, 2015 by Breiholz et al., entitled “Enhancement of Airborne Weather Radar Performance Using External Weather Data,” each of which is assigned to the assignee of the present application and incorporated herein by reference in its entirety.
The inventive concepts disclosed herein relate generally to the field of weather display systems, and more particularly to weather display systems and methods configured to provide multiple source weather data.
Aircraft weather radar systems are often used to alert operators of vehicles, such as aircraft pilots, of weather hazards in the area near the aircraft. Such weather radar systems typically include an antenna, a receiver transmitter, a processor, and a display. The system transmits radar pulses or beams and receives radar return signals indicative of weather conditions. Conventional weather radar systems, such as the WXR 2100 MULTISCAN radar system manufactured by Rockwell Collins, Inc., have Doppler capabilities and can measure or detect parameters such as weather range, weather reflectivity, weather velocity, and weather spectral width or velocity variation. Weather radar systems may also detect outside air temperature, winds at altitude, INS G loads (in-situ turbulence), barometric pressure, humidity, etc.
Weather radar signals are processed to provide graphical images to a radar display. The radar display is typically a color display providing graphical images in color to represent the severity of the weather. Some aircraft systems also include other hazard warning systems such as a turbulence detection system. The turbulence detection system can provide indications of the presence of turbulence or other hazards. Conventional weather display systems are configured to display weather data in two dimensions and often operate according to ARINC 453 and 708 standards. A horizontal plan view provides an overview of weather patterns that may affect an aircraft mapped onto a horizontal plane. Generally the horizontal plan view provides images of weather conditions in the vicinity of the aircraft, such as indications of precipitation rates. Red, yellow, and green colors are typically used to symbolize areas of respective precipitation rates, and black color symbolizes areas of very little or no precipitation. Each color is associated with radar reflectivity range which corresponds to a respective precipitation rate range. Red indicates the highest rates of precipitation while green represents the lowest (non-zero) rates of precipitation. Certain displays may also utilize a magenta color to indicate regions of turbulence.
While aircraft-based weather radar systems may typically provide the most timely and directly relevant weather information to the aircraft crew based on scan time of a few seconds, the performance of aircraft-based weather systems may be limited in several ways. First, typical radar beam widths of aircraft-based weather radar systems are 3 to 10 degrees. Additionally, the range of aircraft-based weather radar systems is typically limited to about 300 nautical miles, and typically most effective within about 80-100 nautical miles. Further, aircraft-based weather radar systems may be subject to ground clutter when the radar beam intersects with terrain, or to path attenuation due to intense precipitation or rainfall.
Information provided by aircraft weather radar systems may be used in conjunction with weather information from other aircraft or ground-based systems to, for example, improve range and accuracy and to reduce gaps in radar coverage. For example, the National Weather Service WSR-88D Next Generation Radar (NEXRAD) weather radar system is conventionally used for detection and warning of severe weather conditions in the United States. NEXRAD data is typically more complete than data from aircraft-based weather radar systems due to its use of volume scans of up to 14 different elevation angles with a one degree beam width. Similarly, the National Lightning Detection Network (NLDN) may typically be a reliable source of information for weather conditions exhibiting intense convection. Weather satellite systems, such as the Geostationary Operational Environmental Satellite system (GOES) and Polar Operational Environmental Satellite system (POES) are other sources of data used for weather analyses and forecasts.
Current global convective information does not identify thunderstorm cores, overestimates the extent of thunderstorms, includes very little storm height information, results in poor predictions, is generally not very timely, and is difficult to interpret. Global convective weather information is conventionally derived from multiple sources. The first source is infrared satellite information that is 15 minutes to 1 hour old and only provides a coarse area where the highest clouds are located and not necessarily where the convective cells are located. The second source is global forecast models, which are used to identify and predict locations of convective activity using dew point and temperature information among other variables. The products derived from Global Forecast Models are very coarse and do not accurately identify the thunderstorm cores or the extent of the thunderstorm. Global lightning information is also available, but only shows the location of the strongest flashes and not the full extent of a thunderstorm core or whether the lightning flash is from a thunderstorm core or a non-threatening dissipating stratiform area. Existing products may derive a surrogate 2-D reflectivity or threat level from a lightning flash rate, however, such products are limited in usage in the United States and not globally. Moreover, global convective products are difficult to interpret by the operator, because the color codes do not correspond to threat levels pilots are accustomed to.
In one aspect, the inventive concepts disclosed herein are directed to a method of providing convective weather data. The method includes accessing lightning data, accessing statistical data representing a relationship between lightning flash rate data and at least one of reflectivity data and weather threat data, and accessing at least one of time of year data, geographic location data, temperature data, and altitude data. The method also includes generating a weather threat level map based on the accessed lightning data, the accessed statistical data, and the at least one of time of year data, geographic location data, temperature data, and altitude data. The weather threat level map indicates at least one of reflectivity and a weather threat. The method also includes providing the weather threat level map to an output port.
In a further aspect, the inventive concepts disclosed herein are directed to a weather processing device including a processor and an output port coupled to the at least one processor. The processor is configured to access lightning data, access statistical data representing a relationship between lightning flash rate data and at least one of reflectivity data and weather threat data, and access at least one of time of year data, geographic location data, temperature data, and altitude data. The processor is also configured to generate a weather threat level map based on the accessed lightning data, the accessed statistical data, and the at least one of time of year data, geographic location data, temperature data, and altitude data. The weather threat level map indicates at least one of reflectivity and a weather threat. The weather processing device also includes an output port coupled with the at least one processor and configured to provide the weather threat level map to at least one of a display, a weather avoidance decision support system, and an automated weather avoidance or rerouting system.
In a further aspect, the inventive concepts disclosed herein are directed to a weather processing system includes at least one processor and an output port coupled to the at least one processor. The processor is configured to access lightning data, access statistical data representing a relationship between lightning flash rate data and at least one of reflectivity data and weather threat data, access at least one of time of year data, geographic location data, temperature data, and altitude data, and access satellite data indicating convective activity. The processor is also configured to generate a weather threat level map based on the accessed lightning data, the accessed statistical data, the at least one of time of year data, geographic location data, temperature data, and altitude data, and the satellite data. The weather threat level map indicates at least one of reflectivity and a weather threat. The weather processing system also includes an output port coupled with the at least one processor and configured to provide the weather threat level map to at least one of a display, a weather avoidance decision support system, and an automated weather avoidance or rerouting system.
Embodiments of the inventive concepts disclosed herein will become more fully understood from the following detailed description, taken in conjunction with the accompanying drawings, wherein like reference numerals refer to like elements, in which:
Before turning to the figures, which illustrate exemplary embodiments of the inventive concepts disclosed herein in detail, it should be understood that the inventive concepts disclosed herein are not limited to the details or methodology set forth in the description or illustrated in the figures. It should also be understood that the terminology is for the purpose of description only and should not be regarded as limiting. As discussed below, systems and methods according to the inventive concepts disclosed herein can be utilized in a number of display devices for various types of applications or sensing systems. In some embodiments, the systems and methods of the inventive concepts disclosed herein may be used for a flight display of an aircraft. According to various exemplary embodiments, the systems and methods according to the inventive concepts disclosed herein may be used by any system in any embodiment that uses weather data or that renders computer graphics and displays an output (e.g., in another aircraft or spacecraft, a ground-based vehicle, a handheld device, in a non-vehicle application such as a ground-based weather radar system, a weather observation system, a situation awareness system, or a weather avoidance system).
A ground based system or an aircraft hazard warning system or other avionic system may integrate or combine convective weather data for displaying threat levels of the weather data on a display in one embodiment. The system can provide indications of convective threat levels using multiple sources including global lightning data, global weather model information, and satellite data for convective weather observation, prediction situation awareness, and weather threat avoidance in one embodiment. The system identifies convective weather cores using high update rate global lightning information to create a lightning flash rate map, where each flash over a predetermined interval (e.g., 10 minutes) is mapped to a memory map where each flash has an area of influence (e.g., 8 km) in one embodiment. The system uses weather model statistics (e.g., the Rockwell Collins global Tropical Rainfall Measurement Mission (TRMM) statistics) to identify 3-D global relationships between lightning flash rate and reflectivity or weather threat in one embodiment. The system considers time of year, geographic location, and temperature/altitude to select the appropriate flash rate to reflectivity function for reflectivity data in one embodiment. A weather threat level map or lightning flash rate map may be created, and successive maps can be compared using a trending and tracking algorithm to derive motion information that can be used for latency compensation and short-term predictions/nowcasts in one embodiment. In one embodiment, weather model statistics can be used to establish relationships between satellite infrared and visible channels and reflectivity and weather threat information.
Satellite information is typically between 15 minutes to 1 hour old based on regional satellite capabilities and therefore the location data of weather represented in the satellite information is generally relative to the current time. To compensate for this, the latent satellite data can be combined with wind information (e.g., 500 mb forcing level wind information) from meteorological model such as the Global Forecast System (GFS) to compensate for the age of satellite data in one embodiment. For example, the wind field may be combined with the infrared satellite data grid and each satellite grid value may be extrapolated to a predicted location based on the wind motion vector. The infrared satellite data indicates overall convective activity, but not necessarily where the convective cores are located. Combining the satellite with the estimated reflectivity/threat allows for a viable mid to long range convective threat assessment system, particularly if used in conjunction with an airborne weather radar according to some embodiments. The reflectivity threat information can also be turned into weather objects for use in weather avoidance decision support tools and automated weather avoidance or re-routing systems in some embodiments. Statistical information derived from the TRMM satellite or similar satellite may be used to derive an importance of each weather source in an overall weight or contribution in the weather threat level map.
Referring to
In some embodiments, the flight displays 20 may provide an output from an aircraft-based weather radar system, LIDAR system, infrared system or other system on the aircraft. For example, the flight displays 20 may include a weather display, a multifunction display, a weather radar map and a terrain display. Further, the flight displays 20 may include an electronic display of a synthetic vision system (SVS). For example, the flight displays 20 may include a display configured to display a two-dimensional (2-D) image, a three dimensional (3-D) perspective image of terrain and/or weather information, or a four dimensional (4-D) display of weather information or forecast information. Other views of terrain and/or weather information may also be provided (e.g., plan view, horizontal view, vertical view). The views may include monochrome or color graphical representations of the terrain and/or weather information. Graphical representations of weather or terrain may include an indication of altitude of the weather or terrain above sea level or the altitude relative to the aircraft.
The aircraft control center 10 may include one or more user interface (UI) elements 22. The UI elements 22 may include, for example, dials, switches, buttons, touch screens, keyboards, a mouse, joysticks, cursor control devices (CCDs) or other multi-function key pads certified for use with avionics systems, etc. The UI elements 22 may be configured to, for example, allow an aircraft crew member to interact with various avionics applications and perform functions such as data entry, manipulation of navigation maps, and moving among and selecting checklist items. For example, the UI elements 22 may be used to adjust features of the flight displays 20, such as contrast, brightness, width, and length. The UI elements 22 may also (or alternatively) be used by an occupant to interface with or change the displays of the flight displays 20. The UI elements 22 may additionally be used to acknowledge or dismiss an indicator provided by the flight displays 20. Further, the UI elements 22 may be used to correct errors on the electronic display. Other UI elements 22, such as indicator lights, displays, display elements, and audio alerting devices, may be configured to warn of potentially threatening conditions such as severe weather, terrain, obstacles, etc.
Referring to
The radar system 50 may generally work by sweeping or casting a radar beam horizontally back and forth across the sky. For example, the radar system 50 may conduct a first horizontal sweep 52 directly in front of the aircraft 30 and a second horizontal sweep 54 downward at a tilt angle 56 (e.g., 20 degrees down). Returns from different tilt angles may be electronically merged to form a composite image for display on an electronic display, such as the flight display 20 in the aircraft control center 10. Returns may also be processed to, for example, distinguish among terrain, weather, and other objects, to determine the height of the terrain, or to determine the height of the weather.
The radar system 50 may also sweep a radar beam vertically back and forth at varying vertical tilt angles. Results from the different vertical tilt angles may be analyzed to determine the characteristics of weather. For example, the altitude, range, and vertical height of weather may be determined using the vertical scan results. The vertical scan results may be used to form an image for display on an electronic display (e.g., the flight display 20). For example, a vertical profile view of the weather may be generated. The profile may be used by a pilot to determine height, range, hazards and threats, and other relevant information that may be utilized by an aircraft crew member to change the course of the aircraft to avoid the detected weather condition.
Referring to
Additionally, the weather radar system 202 may perform multiple radar sweeps. The radar sweeps may include horizontal sweeps, vertical sweeps, or a combination of horizontal and vertical sweeps. Further, the radar sweeps can be performed such that they are substantially orthogonal to one another. According to some exemplary embodiments, the weather radar system 202 can be a monopulse radar system, a sequential lobing system, or a radar system with an aperture capable of switching modes. The weather radar system 202 may be a system for detecting weather patterns. Detected weather patterns may be communicated to the electronic display system 210 for display to the flight crew. In addition, data from the station 220 may be displayed on the display system 210. Detected weather patterns may instead or may also be provided to electronics or the processor 208 for further analysis or transmission to a station 220 or another aircraft 230, 240 via communication system 216. Communication system 216 may also receive weather radar data from other aircraft 230,240 or from the terrestrial station 220.
The aircraft sensors 203 may include, for example, one or more lightning sensors, turbulence sensors, pressure sensors, optical systems (e.g., camera system, infrared system), outside air temperature sensors, winds at altitude sensors, INS G load (in-situ turbulence) sensors, barometric pressure sensors, humidity sensors, or any other aircraft sensors or sensing systems that may be used to monitor weather and detect, for example, lightning, convective cells, or clear air turbulence. Data from the aircraft sensors 203 may be output to the processor 208 for further processing and display, or for transmission to a station 220 (e.g., a ground-based weather radar system or terrestrial station), to other aircraft 230, 240, or to a handheld device 222 (e.g., a laptop, a tablet, a smartphone, or any other portable computing device) via the communication system 216. The communications system 216 may be any wired (e.g., USB, parallel, serial, coaxial, fiber optic) and/or wireless (e.g., Bluetooth, WiFi, Zigbee, mesh, cellular, RF) communication system.
The station 220 may direct the aircraft 201, 230, 240 via the communication system 216 to scan in specific areas to improve detection accuracy of weather. Alternatively, the system 202 may request that the station 220 and the aircraft 230, 240 direct a scan towards weather of interest to the aircraft 201 (e.g., in the flight path) to improve weather detection accuracy. The scans performed by the radar system 202 and the requests may be transmitted to the station 220 or another aircraft 230, 240 via the communication system 216.
In some embodiments, the station 220 or the processor 208 may produce global convective weather information. For example, the station 220 may access or receive global lightning data from a network of lightning sensors, global weather model data, and satellite data. The station 220 may combine the data to produce a convective weather observation (e.g., a weather threat level map), as described in greater detail below, which can be used to predict situation awareness or for weather threat avoidance. In some embodiments, the station 220 may also access radar data from the aircraft 201, 230, 240 to assist in producing the convective weather observation. The station 220 can output the convective weather observation to the aircraft 201 via the communication system 216, to the handheld device 222 via the communication system 216 or via a direct connection (e.g., a USB connection or other wired connection; a Bluetooth, WiFi, or other wireless connection), or to the aircraft 230, 240 via the communication system 216 or via a direct connection. The display 210, a display on the handheld device 222, or a display on the aircraft 2304, 240 may display the convective weather observation. In some embodiments, the processor 208 may perform the steps described above with reference to the station 220.
Referring to
The memory 206 may include any type of machine-readable storage device capable of storing radar returns, lightning data, satellite data, convective weather data, weather threat data, or associated weather data (shown in
The processor 208 may be implemented in hardware, firmware, software, or any combination of these methods. While a single processor 208 is shown in the Figures, in some embodiments, the processor 208 may include multiple processors that are located locally or remotely from the rest of the system. The aircraft 201 or the terrestrial station 220 may have one or more processors 208 that use the same or a different processing technology. Additionally, the processor 208 may be a separate component of the aircraft 201, the terrestrial station 220, or the handheld device 222 or may be embedded within another component of the aircraft 201, the terrestrial station 220, or the handheld device 222. The processor 408 may execute instructions that may be written using one or more programming languages, scripting languages, assembly languages, etc. The instructions may be carried out by, for example, a special purpose computer, logic circuits, or hardware circuits. The term “execute” is the process of running an application or the carrying out of the operation called for by an instruction. The processor 208 may process data and/or execute applications stored in the memory 206, such as the weather data and weather image application and/or other instructions.
The processor 208 may be included as part of a multi-scan, multi-tilt angle weather radar system and may perform the customary functions performed by a conventional weather radar return processing unit. The processor 208 may also perform several additional operations based upon the additional data and/or instructions provided in the memory 206, such as the convective weather methodology described herein. In general, the processor 208 may access data from various sources and integrate or combine them to generate convective weather observations and predictions in the form of data or weather threat level maps. The term “access,” as used herein, is understood to mean any type of data receipt or acquisition. For example, processor 208 may receive data pushed to it from other sources or may retrieve, poll, or pull data from a memory, a from communications system, or from other sources. The processor 208 may also merge or cross qualify portions, or ranges, of the radar returns of several different antenna sweeps at several different tilt angles, so that a single, relatively clutter-free image may be presented to the pilot based upon the several separate scans. The radar returns may be processed by the processor 208 to generate a 2-D, 3-D, or 4-D weather profile of the weather near the aircraft 201. In some embodiments, the processor 208 may merge or cross qualify portions, or ranges, of the radar returns or weather data of several different sources, including weather data from one or more remote sources via the terrestrial station 220 or the communications system 216, so that a composite or fused image may be presented to the pilot based upon the several weather data sources.
The processor 208 may process weather radar returns to identify or sense the presence of weather conditions in front of (e.g., in the flight path), in view of, or in proximity to the aircraft. In some embodiments, the processor 208 may utilize the altitude and range of the weather condition to generate a vertical profile associated with the weather. The processor 208 may scan across an array of azimuths to generate a 3-D weather profile of the weather near the aircraft, which may be stored for later presentation and/or displayed on the display 210 or a display of the handheld device 222. In some embodiments, additional visual indicators other than the representation of weather are provided on the display 210 or a display of the handheld device 222. In some embodiments, a range and bearing matrix having range markers indicating distance from a current location of the aircraft 201 and bearing markers indicating azimuths from a current flight path or bearing of the aircraft may be provided and may assist the pilot in cognitive recognition of weather features from the pilot's perspective.
Referring now to
The processor 208 generates the lightning flash map 320 based at least on statistical data 314 and lightning data 317b. Statistical data 314 provides a correlation of expected reflectivity for a given flash rate. The lightning flash map 320 may also be based on parameters 330, 332, 333, and 334 to determine a precise statistical correlation based on an expected temperature at a given altitude, based on a time of year and/or time of day, and based on a location. The lightning flash map 320 is configured to indicate a standard reflectivity color scheme through coloring, texturing, or associated data. In some embodiments, the processor 208 may store generated lightning flash maps 320 in the memory 206 for later reference or to derive motion for forecasting future lightning flash maps 320. Each lightning flash map 320 may be stored in memory as an image (e.g., color, grayscale, textured monochrome) or as data representative of an image.
In some embodiments, processor 208 may estimate reflectivity based on satellite data using statistical relationships between TRMM satellite radar and infrared or visible satellite features (including satellite trend data). Statistical data 314 may include statistics of a satellite related to the geographic location, time of year, time of day, temperature/altitudes parameters 330, 332, 333, 334. Processor 208 may access the statistical data 314 to derive reflectivity or threat information from the satellite statistics.
In some embodiments, the processor 208 may generate the weather threat map 324 based on the generated lightning flash map 320 and satellite data 316. The weather threat map 324 is configured to have a standard reflectivity color scheme including green, yellow, red, and optionally magenta. The weather threat map 324 may be provided to display 210 or a display of handheld device 222 via an output port for viewing by a pilot. Alternatively, the weather threat map 324 may be provided to a weather threat avoidance or re-routing system of the aircraft 201 via an output port. In some embodiments, the processor 208 may be further refined using weather data 317a. In some embodiments, satellite data 316 may be adjusted based on wind information and an expected latency in accessing the satellite data. Further details of the methodology behind the system 300 are provided below.
In some embodiments, the weather threat map 324 may be the lightning flash map 320 or the processor 208 may generate the weather threat map 324 based on the lightning flash map 320. In some embodiments, the weather threat map 324 may be omitted and the lightning flash map 320 may be provided by the system 300.
The data stored in the memory 206 may be data accessed from local or external sources. In one embodiment where the system 300 is on the aircraft 201, statistical data 314, satellite data 316, and lightning data 317b may be received from the terrestrial station 220 or the handheld device 222 via the communication system 216. Weather data 317a from returns received by the antenna 204 may be stored in the memory 206. Weather data 317a may, for example, be based on received horizontal and/or vertical radar scans. Weather data 317a may also be from another weather radar source or data from an onboard weather radar system operating at a different frequency, such as a Ka band frequency, a W band frequency, etc. Weather data 317a may be accessed via the communications unit 216 and/or from the terrestrial station 220 (e.g., NEXRAD weather data). In some embodiments, weather data 317a may be from a non-radar airborne source (a LIDAR source, an infrared source, etc.). Weather data 317a may include, for example, a time of sensing data, such as a time stamp, and motion vector data (e.g., individual weather cell and average motion vector data) for temporal and spatial correlation (e.g., NEXRAD data accessed from the terrestrial station 220).
In some embodiments where the system 300 is on the terrestrial station 220 or the handheld device 222, statistical data 314 may be preloaded from a statistical model (e.g., the TRMM model mentioned above, or another statistical weather model correlating lightning data to reflectivity or convective weather), satellite data 316 may be accessed from the NEXRAD system or another IR satellite data source, and lightning data 317b may be accessed from a global lightning network (e.g., the National Lightning Detection Network (NLDN) available from Vaisala, the World Wide Lightning Location Network (WWLLN) administered by the University of Washington and various other universities, Earth Networks Total Lightning Network (ENTLN) available from Earth Networks). Weather data 317a may be accessed via the communications unit 216 and/or from the aircraft 201, 230, 240, from a ground based radar system, or from a non-radar airborne source (a LIDAR source, an infrared source, etc.). In some embodiments, radar return data 317a may not be located in the memory 206, but the processor 208 may receive the data directly from the antenna or an external system via the communications system 216. Parameters 320, 322, 324, and 326 may be provided to the aircraft 201, which may optionally combine the data with the radar return data. In embodiments where the system 300 is on the terrestrial station 220, the provided weather threat map 324 and future updates to the weather threat map 324 may be provided to the aircraft 201 or the handheld device 222 at a predetermined interval. For example, an updated weather threat map 324 may be provided to the aircraft 201 or the handheld device 222 every minute, every 5 minutes, every 10 minutes, or at any other time interval depending on the bandwidth of the communications system 216.
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Proprietary studies have shown relationships between optically detected lightning flash rates and measured radar reflectivity. The studies have shown numerical correlation coefficients between areas of radar reflectivity, temperature levels within storms, and lightning flash rate. Example tables of a simplified versions of such relationships are shown below:
The derivation of these relationships is based on dividing a region under observation into units of equal area and determining the number of lightning flashes per minute within the area and the percentage of each unit of area that contained reflectivity of each value (20, 25, 30, etc. dBZ). Consequently, for a given flash rate, the area of a given reflectivity value can be derived by processor 208 using an equation based on the slope given in the first table above for that reflectivity. Because the original data were gathered in terms of radar reflectivity, this fundamental relationship is also in terms of reflectivity. The data may be further adjusted by the processor 208 to a threat level value by taking into account the variation in storm intensity associated with a given reflectivity level depending upon the geographical location (tropics, subtropics, temperate zone and oceanic or over land) and the time of year and day.
The reflectivity relationship provides an area for a given flash rate, location type, and reflectivity level, but the tables provide additional information. The correlation coefficient is an indicator of how reliable a given flash-rate to area relationship is. Depending on the situation, it may be desirable to omit reflectivity regions that have a low correlation coefficient relative to the maximum coefficient, because these relationships are less consistent.
The temperature table may allow positioning of a particular reflectivity area at a corresponding altitude. This positioning my include information regarding the temperature lapse rate of the atmosphere with altitude (pressure level), which is available from numerical forecasting and analysis models executed on the processor 208.
Referring again to
If the temperature variation is disregarded as a simplification, or if two reflectivity areas lie at the same temperature level (e.g., 35 and 40 dBZ are at −10 degrees in the subtropical land case), then a technique can be implemented that allocates the various areas. The processor 208 can assign the maximum reflectivity to a circle of the area derived above. Because it is normal in weather radar images for a core region of high reflectivity to be surrounded by regions of successively lower reflectivity, the processor 208 may assign the next lower reflectivity to a circle surrounding the maximum reflectivity circle. The area of the circle is the area derived above. By assuming the areas of reflectivity are numbered from 1 to M, lowest to highest, the processor 208 can calculate the area of the maximum reflectivity inner circle and the outer radius of the circle.
In some embodiments, the processor 208 may perform the computations on a uniform grid (e.g., a 1 kilometer grid) in order to easily create a map (e.g.,
Referring to
Referring to
Similar to the processes described above relating lightning data, statistical data, location data, and time of year/day data, processor 208 may estimate reflectivity based on satellite data using statistical relationships between TRMM satellite radar and infrared or visible satellite features (including satellite trend data). Statistical data 314 may include statistics of a satellite related to geographic location, time of year, time of day, temperature/altitudes, etc. Processor 208 may access the statistical data 314 to derive reflectivity or threat information from the satellite statistics.
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In some embodiments, processor 208 combine satellite based reflectivity/threats, lightning derived reflectivity/threats, and numerical weather model reflectivity/threats to generate weather threat map 324 using the maximum or average threat value based upon the contributions of each source. The processor 208 may combine or weight the source data using statistics to determine a weighting based upon the historical statistical relationship between the threat levels of each source and geographic location, time day, time of year, altitude and temperature. For example, over the pacific ocean, the satellite infrared height in excess of 30,000 ft. agl and presence of Global Forecast Reflectivity along with the presence of lightning indicates an area of higher reflectivity and higher threat level.
According to various exemplary embodiments, the process flow of
While the detailed drawings, specific examples, detailed algorithms and particular configurations given describe preferred and exemplary embodiments, they serve the purpose of illustration only. The inventive concepts disclosed herein are not limited to the specific forms shown. For example, the methods may be performed in any of a variety of sequence of steps or according to any of a variety of mathematical formulas. The graphic representations shown are exemplary only. The hardware and software configurations shown and described may differ depending on the chosen performance characteristics and physical characteristics of the weather radar and processing devices. For example, the type of system components and their interconnections may differ. The systems and methods depicted and described are not limited to the precise details and conditions disclosed. The flow charts show preferred exemplary operations only. The specific data types, graphical symbols and operations are shown in a non-limiting fashion. Further, other substitutions, modifications, changes, and omissions may be made in the design, operating conditions, and arrangement of the exemplary embodiments without departing from the broad scope of the inventive concepts disclosed herein as expressed in the appended claims.
Number | Name | Date | Kind |
---|---|---|---|
650275 | Reeve | May 1900 | A |
3251057 | Buehler et al. | May 1966 | A |
3359557 | Fow et al. | Dec 1967 | A |
3404396 | Buchler et al. | Oct 1968 | A |
3465339 | Marner | Sep 1969 | A |
3491358 | Hicks | Jan 1970 | A |
3508259 | Andrews | Apr 1970 | A |
3540829 | Collinson et al. | Nov 1970 | A |
3567915 | Altshuler et al. | Mar 1971 | A |
3646555 | Atlas | Feb 1972 | A |
3715748 | Hicks | Feb 1973 | A |
3764719 | Dell | Oct 1973 | A |
3781530 | Britland et al. | Dec 1973 | A |
3781878 | Kirkpatrick | Dec 1973 | A |
3803609 | Lewis et al. | Apr 1974 | A |
3885237 | Kirkpatrick | May 1975 | A |
3943511 | Evans et al. | Mar 1976 | A |
3964064 | Brandao et al. | Jun 1976 | A |
3968490 | Gostin | Jul 1976 | A |
4015257 | Fetter | Mar 1977 | A |
4043194 | Tanner | Aug 1977 | A |
4179693 | Evans et al. | Dec 1979 | A |
4223309 | Payne | Sep 1980 | A |
4240108 | Levy | Dec 1980 | A |
4283715 | Choisnet | Aug 1981 | A |
4283725 | Chisholm | Aug 1981 | A |
4318100 | Shimizu et al. | Mar 1982 | A |
4346595 | Frosch et al. | Aug 1982 | A |
4430654 | Kupfer | Feb 1984 | A |
4435707 | Clark | Mar 1984 | A |
4459592 | Long | Jul 1984 | A |
4533915 | Lucchi et al. | Aug 1985 | A |
4555703 | Cantrell | Nov 1985 | A |
4600925 | Alitz et al. | Jul 1986 | A |
4613937 | Batty, Jr. | Sep 1986 | A |
4613938 | Hansen et al. | Sep 1986 | A |
4649388 | Atlas | Mar 1987 | A |
4658255 | Nakamura et al. | Apr 1987 | A |
4684950 | Long | Aug 1987 | A |
4742353 | D'Addio et al. | May 1988 | A |
4761650 | Masuda et al. | Aug 1988 | A |
4835536 | Piesinger et al. | May 1989 | A |
RE33152 | Atlas | Jan 1990 | E |
4914444 | Pifer et al. | Apr 1990 | A |
4928131 | Onozawa | May 1990 | A |
4940987 | Frederick | Jul 1990 | A |
5036334 | Henderson et al. | Jul 1991 | A |
5047775 | Alitz | Sep 1991 | A |
5049886 | Seitz et al. | Sep 1991 | A |
5057820 | Markson et al. | Oct 1991 | A |
5077558 | Kuntman | Dec 1991 | A |
5105191 | Keedy | Apr 1992 | A |
5159407 | Churnside et al. | Oct 1992 | A |
5164731 | Borden et al. | Nov 1992 | A |
5173704 | Buehler et al. | Dec 1992 | A |
5177487 | Taylor et al. | Jan 1993 | A |
5198819 | Susnjara | Mar 1993 | A |
5202690 | Frederick | Apr 1993 | A |
5208587 | Cornman | May 1993 | A |
5208600 | Rubin | May 1993 | A |
5221924 | Wilson, Jr. | Jun 1993 | A |
5262773 | Gordon | Nov 1993 | A |
5291208 | Young | Mar 1994 | A |
5296865 | Lewis | Mar 1994 | A |
5311183 | Mathews et al. | May 1994 | A |
5311184 | Kuntman | May 1994 | A |
5331330 | Susnjara | Jul 1994 | A |
5396220 | Markson et al. | Mar 1995 | A |
5402116 | Ashley | Mar 1995 | A |
5469168 | Anderson | Nov 1995 | A |
5479173 | Yoshioka et al. | Dec 1995 | A |
5485157 | Long | Jan 1996 | A |
5517193 | Allison et al. | May 1996 | A |
5521603 | Young | May 1996 | A |
5534868 | Gjessing et al. | Jul 1996 | A |
5568151 | Merritt | Oct 1996 | A |
5583972 | Miller | Dec 1996 | A |
5592171 | Jordan | Jan 1997 | A |
5602543 | Prata et al. | Feb 1997 | A |
5615118 | Frank | Mar 1997 | A |
5648782 | Albo et al. | Jul 1997 | A |
5654700 | Prata et al. | Aug 1997 | A |
5657009 | Gordon | Aug 1997 | A |
5686919 | Jordan et al. | Nov 1997 | A |
5726656 | Frankot | Mar 1998 | A |
5757322 | Ray et al. | May 1998 | A |
5771020 | Markson et al. | Jun 1998 | A |
5828332 | Frederick | Oct 1998 | A |
5831570 | Ammar et al. | Nov 1998 | A |
5838239 | Stern et al. | Nov 1998 | A |
5839080 | Muller et al. | Nov 1998 | A |
5907568 | Reitan, Jr. | May 1999 | A |
5920276 | Frederick | Jul 1999 | A |
5936552 | Wichgers et al. | Aug 1999 | A |
5945926 | Ammar et al. | Aug 1999 | A |
5973635 | Albo | Oct 1999 | A |
6018307 | Wakayama et al. | Jan 2000 | A |
6034760 | Rees | Mar 2000 | A |
6043756 | Bateman et al. | Mar 2000 | A |
6043757 | Patrick | Mar 2000 | A |
6081220 | Fujisaka et al. | Jun 2000 | A |
6138060 | Conner et al. | Oct 2000 | A |
6154151 | McElreath et al. | Nov 2000 | A |
6154169 | Kuntman | Nov 2000 | A |
6177873 | Cragun | Jan 2001 | B1 |
6184816 | Zheng et al. | Feb 2001 | B1 |
6201494 | Kronfeld | Mar 2001 | B1 |
6208284 | Woodell et al. | Mar 2001 | B1 |
6236351 | Conner et al. | May 2001 | B1 |
6240369 | Foust | May 2001 | B1 |
6246367 | Markson et al. | Jun 2001 | B1 |
6281832 | McElreath | Aug 2001 | B1 |
6289277 | Feyereisen et al. | Sep 2001 | B1 |
6297772 | Lewis | Oct 2001 | B1 |
6339747 | Daly et al. | Jan 2002 | B1 |
6340946 | Wolfson et al. | Jan 2002 | B1 |
6377202 | Kropfli et al. | Apr 2002 | B1 |
6381538 | Robinson et al. | Apr 2002 | B1 |
6384830 | Baron et al. | May 2002 | B2 |
6388607 | Woodell | May 2002 | B1 |
6388608 | Woodell et al. | May 2002 | B1 |
RE37725 | Yamada | Jun 2002 | E |
6405134 | Smith et al. | Jun 2002 | B1 |
6424288 | Woodell | Jul 2002 | B1 |
6441773 | Kelly et al. | Aug 2002 | B1 |
6448922 | Kelly | Sep 2002 | B1 |
6456226 | Zheng et al. | Sep 2002 | B1 |
6480142 | Rubin | Nov 2002 | B1 |
6496252 | Whiteley | Dec 2002 | B1 |
6501392 | Gremmert et al. | Dec 2002 | B2 |
6512476 | Woodell | Jan 2003 | B1 |
6518914 | Peterson et al. | Feb 2003 | B1 |
6549161 | Woodell | Apr 2003 | B1 |
6560538 | Schwinn et al. | May 2003 | B2 |
6563452 | Zheng et al. | May 2003 | B1 |
6577947 | Kronfeld et al. | Jun 2003 | B1 |
6590520 | Steele et al. | Jul 2003 | B1 |
6597305 | Szeto et al. | Jul 2003 | B2 |
6603425 | Woodell | Aug 2003 | B1 |
6606564 | Schwinn et al. | Aug 2003 | B2 |
6614382 | Cannaday et al. | Sep 2003 | B1 |
6650275 | Kelly et al. | Nov 2003 | B1 |
6650972 | Robinson et al. | Nov 2003 | B1 |
6667710 | Cornell et al. | Dec 2003 | B2 |
6670908 | Wilson et al. | Dec 2003 | B2 |
6677886 | Lok | Jan 2004 | B1 |
6683609 | Baron et al. | Jan 2004 | B1 |
6690317 | Szeto et al. | Feb 2004 | B2 |
6703945 | Kuntman et al. | Mar 2004 | B2 |
6720906 | Szeto et al. | Apr 2004 | B2 |
6738010 | Steele et al. | May 2004 | B2 |
6741203 | Woodell | May 2004 | B1 |
6744382 | Lapis et al. | Jun 2004 | B1 |
6771207 | Lang | Aug 2004 | B1 |
6788043 | Murphy et al. | Sep 2004 | B2 |
6791311 | Murphy et al. | Sep 2004 | B2 |
6828922 | Gremmert et al. | Dec 2004 | B1 |
6828923 | Anderson | Dec 2004 | B2 |
6839018 | Szeto et al. | Jan 2005 | B2 |
6850185 | Woodell | Feb 2005 | B1 |
6856908 | Devarasetty et al. | Feb 2005 | B2 |
6879280 | Bull et al. | Apr 2005 | B1 |
6882302 | Woodell et al. | Apr 2005 | B1 |
6917860 | Robinson et al. | Jul 2005 | B1 |
6977608 | Anderson et al. | Dec 2005 | B1 |
7030805 | Ormesher et al. | Apr 2006 | B2 |
7039505 | Southard et al. | May 2006 | B1 |
7042387 | Ridenour et al. | May 2006 | B2 |
7082382 | Rose et al. | Jul 2006 | B1 |
7109912 | Paramore et al. | Sep 2006 | B1 |
7109913 | Paramore et al. | Sep 2006 | B1 |
7116266 | Vesel et al. | Oct 2006 | B1 |
7129885 | Woodell et al. | Oct 2006 | B1 |
7132974 | Christianson | Nov 2006 | B1 |
7139664 | Kelly et al. | Nov 2006 | B2 |
7145503 | Abramovich et al. | Dec 2006 | B2 |
7161525 | Finley et al. | Jan 2007 | B1 |
7200491 | Rose et al. | Apr 2007 | B1 |
7205928 | Sweet | Apr 2007 | B1 |
7242343 | Woodell | Jul 2007 | B1 |
7259714 | Cataldo | Aug 2007 | B1 |
7292178 | Woodell et al. | Nov 2007 | B1 |
7307576 | Koenigs | Dec 2007 | B1 |
7307577 | Kronfeld et al. | Dec 2007 | B1 |
7307583 | Woodell et al. | Dec 2007 | B1 |
7307586 | Peshlov et al. | Dec 2007 | B2 |
7307756 | Walmsley | Dec 2007 | B2 |
7352317 | Finley et al. | Apr 2008 | B1 |
7352929 | Hagen et al. | Apr 2008 | B2 |
7365674 | Tillotson et al. | Apr 2008 | B2 |
7372394 | Woodell et al. | May 2008 | B1 |
7383131 | Wey et al. | Jun 2008 | B1 |
7411519 | Kuntman et al. | Aug 2008 | B1 |
7417578 | Woodell et al. | Aug 2008 | B1 |
7417579 | Woodell | Aug 2008 | B1 |
7427943 | Kronfeld et al. | Sep 2008 | B1 |
7436361 | Paulsen et al. | Oct 2008 | B1 |
7471995 | Robinson | Dec 2008 | B1 |
7486219 | Woodell et al. | Feb 2009 | B1 |
7486220 | Kronfeld et al. | Feb 2009 | B1 |
7492304 | Woodell et al. | Feb 2009 | B1 |
7492305 | Woodell et al. | Feb 2009 | B1 |
7515087 | Woodell et al. | Apr 2009 | B1 |
7515088 | Woodell et al. | Apr 2009 | B1 |
7528613 | Thompson et al. | May 2009 | B1 |
7541971 | Woodell et al. | Jun 2009 | B1 |
7557735 | Woodell et al. | Jul 2009 | B1 |
7576680 | Woodell | Aug 2009 | B1 |
7581441 | Barny et al. | Sep 2009 | B2 |
7598901 | Tillotson et al. | Oct 2009 | B2 |
7598902 | Woodell et al. | Oct 2009 | B1 |
7633428 | McCusker et al. | Dec 2009 | B1 |
7633431 | Wey et al. | Dec 2009 | B1 |
7656343 | Hagen et al. | Feb 2010 | B1 |
7664601 | Daly, Jr. | Feb 2010 | B2 |
7696920 | Finley et al. | Apr 2010 | B1 |
7696921 | Finley et al. | Apr 2010 | B1 |
7698058 | Chen et al. | Apr 2010 | B2 |
7714767 | Kronfeld et al. | May 2010 | B1 |
7728758 | Varadarajan et al. | Jun 2010 | B2 |
7733264 | Woodell et al. | Jun 2010 | B1 |
7859448 | Woodell et al. | Dec 2010 | B1 |
7868811 | Woodell et al. | Jan 2011 | B1 |
7869953 | Kelly | Jan 2011 | B1 |
7889118 | Finley et al. | Feb 2011 | B1 |
7917255 | Finley | Mar 2011 | B1 |
7932853 | Woodell et al. | Apr 2011 | B1 |
7973698 | Woodell et al. | Jul 2011 | B1 |
7982658 | Kauffman et al. | Jul 2011 | B2 |
8022859 | Bunch et al. | Sep 2011 | B2 |
8054214 | Bunch | Nov 2011 | B2 |
8072368 | Woodell | Dec 2011 | B1 |
8081106 | Yannone | Dec 2011 | B2 |
8089391 | Woodell et al. | Jan 2012 | B1 |
8098188 | Costes et al. | Jan 2012 | B2 |
8098189 | Woodell et al. | Jan 2012 | B1 |
8111186 | Bunch et al. | Feb 2012 | B2 |
8159369 | Koenigs et al. | Apr 2012 | B1 |
8217828 | Kirk | Jul 2012 | B2 |
8228227 | Bunch et al. | Jul 2012 | B2 |
8314730 | Musiak et al. | Nov 2012 | B1 |
8332084 | Bailey et al. | Dec 2012 | B1 |
8902100 | Woodell et al. | Dec 2014 | B1 |
9019146 | Finley et al. | Apr 2015 | B1 |
9134418 | Kronfeld et al. | Sep 2015 | B1 |
9244166 | Finley et al. | Jan 2016 | B1 |
9507022 | Breiholz et al. | Nov 2016 | B1 |
9535158 | Breiholz et al. | Jan 2017 | B1 |
9720082 | Dana et al. | Aug 2017 | B1 |
20020039072 | Gremmert et al. | Apr 2002 | A1 |
20020126039 | Dalton et al. | Sep 2002 | A1 |
20030001770 | Cornell et al. | Jan 2003 | A1 |
20030025627 | Wilson et al. | Feb 2003 | A1 |
20030117311 | Funai | Jun 2003 | A1 |
20030193411 | Price | Oct 2003 | A1 |
20040183695 | Ruokangas et al. | Sep 2004 | A1 |
20040239550 | Daly, Jr. | Dec 2004 | A1 |
20050049789 | Kelly et al. | Mar 2005 | A1 |
20050174350 | Ridenour et al. | Aug 2005 | A1 |
20050222770 | McKewon | Oct 2005 | A1 |
20060036366 | Kelly et al. | Feb 2006 | A1 |
20070005249 | Dupree et al. | Jan 2007 | A1 |
20070152867 | Randall | Jul 2007 | A1 |
20080040038 | Southard et al. | Feb 2008 | A1 |
20080158049 | Southard et al. | Jul 2008 | A1 |
20080169967 | Wood et al. | Jul 2008 | A1 |
20080180282 | Brosius | Jul 2008 | A1 |
20090177343 | Bunch et al. | Jul 2009 | A1 |
20090219197 | Bunch | Sep 2009 | A1 |
20100019938 | Bunch | Jan 2010 | A1 |
20100019958 | Bunch et al. | Jan 2010 | A1 |
20100042275 | Kirk | Feb 2010 | A1 |
20100110431 | Ray et al. | May 2010 | A1 |
20100194628 | Christianson et al. | Aug 2010 | A1 |
20100201565 | Khatwa | Aug 2010 | A1 |
20100245164 | Kauffman | Sep 2010 | A1 |
20100245165 | Kauffman et al. | Sep 2010 | A1 |
20100302093 | Bunch et al. | Dec 2010 | A1 |
20100302094 | Bunch et al. | Dec 2010 | A1 |
20100315265 | Smith et al. | Dec 2010 | A1 |
20100328143 | Kirk | Dec 2010 | A1 |
20100332056 | Kirk | Dec 2010 | A1 |
20110074624 | Bunch | Mar 2011 | A1 |
20110148692 | Christianson | Jun 2011 | A1 |
20110148694 | Bunch et al. | Jun 2011 | A1 |
20120029786 | Calandra et al. | Feb 2012 | A1 |
20120086596 | Insanic et al. | Apr 2012 | A1 |
20120133551 | Pujol et al. | May 2012 | A1 |
20120139778 | Bunch et al. | Jun 2012 | A1 |
20130226452 | Watts | Aug 2013 | A1 |
20130234884 | Bunch et al. | Sep 2013 | A1 |
20130321442 | Van Os et al. | Dec 2013 | A1 |
20130345982 | Liu | Dec 2013 | A1 |
20140156133 | Cullinane et al. | Jun 2014 | A1 |
20140176362 | Sneed | Jun 2014 | A1 |
20140361923 | Bunch et al. | Dec 2014 | A1 |
20140362088 | Veillette et al. | Dec 2014 | A1 |
20150310747 | Frolik et al. | Oct 2015 | A1 |
20160180718 | Shapiro et al. | Jun 2016 | A1 |
20160266249 | Kauffman et al. | Sep 2016 | A1 |
Number | Date | Country |
---|---|---|
1 329 738 | Jul 2003 | EP |
2658617 | Aug 1991 | FR |
WO-9807047 | Feb 1998 | WO |
WO-9822834 | May 1998 | WO |
WO-03005060 | Jan 2003 | WO |
WO-2009137158 | Nov 2009 | WO |
Entry |
---|
U.S. Appl. No. 14/086,844, filed Nov. 21, 2013, Rockwell Collins, Inc. |
U.S. Appl. No. 14/162,035, filed Jan. 23, 2014, Kevin M. Kronfeld et al. |
U.S. Appl. No. 14/323,766, filed Jul. 3, 2014, Weichbrod et al. |
U.S. Appl. No. 14/465,730, filed Aug. 21, 2014, Breiholz et al. |
U.S. Appl. No. 14/465,753, filed Aug. 21, 2014, Arlen E. Breiholz et al. |
U.S. Appl. No. 14/608,071, filed Jan. 28, 2015, Breiholz et al. |
Liu, Chuntao et al., Relationships between lightning flash rates and radar reflectivity vertical structures in thunderstorms over the tropics and subtropics, Journal of Geophysical Research, vol. 177, D06212, doi:10.1029/2011JDo17123,2012, American Geophysical Union, 2012, 19 pages. |
Zipser, Edward J. et al., The Vertical Profile of Radar Reflectivity of Convective Cells: A Strong Indicator of Storm Intensity and Lightning Probability?, American Meteorological Society, Aug. 1994, 9 pages. |
Final Office Action on U.S. Appl. No. 13/717,052, dated Nov. 13, 2015, 10 pages. |
Final Office Action on U.S. Appl. No. 14/207,034, dated Oct. 13, 2016, 15 pages. |
Non-Final Office Action on U.S. Appl. No. 14/162,035 dated Jul. 11, 2016, 10 pages. |
Non-Final Office Action on U.S. Appl. No. 14/206,239 dated Jun. 16, 2016, 12 pages. |
Non-Final Office Action on U.S. Appl. No. 14/206,651 dated Jun. 23, 2016, 12 pages. |
Non-Final Office Action on U.S. Appl. No. 14/207,034 dated Jun. 23, 2016, 14 pages. |
Non-Final Office Action on U.S. Appl. No. 14/323,766, dated Feb. 8, 2017, 21 pages. |
Non-Final Office Action on U.S. Appl. No. 14/465,730, dated Oct. 21, 2016, 6 pages. |
Non-Final Office Action on U.S. Appl. No. 14/608,071, dated Jan. 23, 2017, 15 pages. |
Non-Final Office Action on U.S. Appl. No. 15/137,645 dated Aug. 8, 2016, 6 pages. |
Notice of Allowance on U.S. Appl. No. 14/162,035, dated Nov. 9, 2016, 7 pages. |
Notice of Allowance on U.S. Appl. No. 14/465,753, dated Aug. 29, 2016, 8 pages. |
Notice of Allowance on U.S. Appl. No. 15/287,673, dated Nov. 18, 2016, 8 pages. |
U.S. Appl. No. 12/075,103, filed Mar. 7, 2008, Woodell et al. |
U.S. Appl. No. 13/246,769, filed Sep. 27, 20101, Rockwell Collins. |
U.S. Appl. No. 13/717,052, filed Dec. 17, 2012, Woodell et al. |
U.S. Appl. No. 13/837,538, filed Mar. 15, 2013, Kronfeld et al. |
U.S. Appl. No. 13/841,893, filed Mar. 15, 2013, Rockwell Collins, Inc. |
U.S. Appl. No. 13/919,406, filed Jun. 17, 2013, Rockwell Collins, Inc. |
U.S. Appl. No. 14/206,239, filed Mar. 12, 2014, Rockwell Collins. |
U.S. Appl. No. 14/206,651, filed Mar. 12, 2014, Rockwell Collins, Inc. |
U.S. Appl. No. 14/207,034, filed Mar. 12, 2014, Rockwell Collins, Inc. |
3-D Weather Hazard and Avoidance System, Honeywell InteVue Brochure dated Nov. 2008, 4 pages. |
Boudevillain et al., 2003, Assessment of Vertically Integrated Liquid (VIL) Water Content Radar Measurement, J. Atmos. Oceanic Technol., 20, 807-819. |
Bovith et al., Detecting Weather Radar Clutter by Information Fusion with Satellite Images and Numerical Weather Prediction Model Output; Jul. 31-Aug. 4, 2006, 4 pages. |
Burnham et al., Thunderstorm Turbulence and Its Relationship to Weather Radar Echoes, J. Aircraft, Sep.-Oct. 1969, 8 pages. |
Corridor Integrated Weather System (CIWS), www.II.mit.edu/mission/aviation/faawxsystems/ciws.html, received on Aug. 19, 2009, 3 pages. |
Decision on Appeal for Inter Parties Reexamination Control No. 95/001,860, dated Oct. 17, 2014, 17 pages. |
Doviak et al., Doppler Radar and Weather Observations, 1984, 298 pages. |
Dupree et al.,FAA Tactical Weather Forecasting in the United States National Airspace, Proceedings from the World Weather Research Symposium on Nowcasting and Very Short Term Forecasts, Toulouse, France, 2005, 29 pages. |
Final Office Action on U.S. Appl. No. 12/892,663 dated Mar. 7, 2013, 13 pages. |
Final Office Action on U.S. Appl. No. 13/238,606 dated Apr. 1, 2014, 11 pages. |
Final Office Action on U.S. Appl. No. 13/238,606 dated Jan. 22, 2015, 6 pages. |
Final Office Action on U.S. Appl. No. 13/246,769 dated Sep. 16, 2014, 18 pages. |
Goodman et al., Lisdad Lightning Observations during the Feb. 22-23, 1998 Central Florida. |
Greene et al., 1972, Vertically Integrated Water—A New Analysis Tool, Mon. Wea. Rev., 100, 548-552. |
Hodanish, Integration of Lightning Detection Systems in a Modernized National Weather Service Office, http://www.srh.noaa.gov/mlb/hoepub.html, retrieved on Aug. 6, 2007, 5 pages. |
Keith, Transport Category Airplane Electronic Display Systems, Jul. 16, 1987, 34 pages. |
Klingle-Wilson et al., Description of Corridor Integrated Weather System (CIWS) Weather Products, Aug. 1, 2005, 120 pages. |
Kuntman et al, Turbulence Detection and Avoidance System, Flight Safety Foundation 53rd International Air Safety Seminar (IASS), Oct. 29, 2000. |
Kuntman, Airborne System to Address Leading Cause of Injuries in Non-Fatal Airline Accidents, ICAO Journal, Mar. 2000. |
Kuntman, Satellite Imagery: Predicting Aviation Weather Hazards, ICAO Journal, Mar. 2000, 4 pps. |
Lahiff, 2005, Vertically Integrated Liquid Density and Its Associated Hail Size Range Across the Burlington, Vermont County Warning Area, Eastern Regional Technical Attachment, No. 05-01, 20 pages. |
Meteorological/KSC/L71557/Lighting Detection and Ranging (LDAR), Jan. 2002, 12 pages. |
Nathanson, Fred E., “Radar and Its Composite Environment,” Radar Design Principles, Signal Processing and the Environment, 1969, 5 pages, McGraw-Hill Book Company, New York et al. |
Non-Final Office Action on U.S. Appl. No. 13/238,606 dated May 27, 2015, 14 pages. |
Non-Final Office Action on U.S. Appl. No. 14/452,235 dated Apr. 23, 2015, 9 pages. |
Non-Final Office Action on U.S. Appl. No. 14/681,901 dated Jun. 17, 2015, 21 pages. |
Non-Final Office Action on U.S. Appl. No. 12/892,663 dated May 29, 2013, 14 pages. |
Non-Final Office Action on U.S. Appl. No. 13/238,606 dated Jul. 8, 2014, 12 pages. |
Non-Final Office Action on U.S. Appl. No. 13/238,606 dated Sep. 23, 2013, 15 pages. |
Non-Final Office Action on U.S. Appl. No. 13/717,052 dated Feb. 11, 2015, 15 pages. |
Non-Final Office Action on U.S. App. No. 13/717,052 dated Sep. 9, 2014, 8 pages. |
Non-Final Office Action on U.S. Appl. No. 13/841,893 dated Jun. 22, 2015, 27 pages. |
Non-Final Office Action on U.S. Appl. No. 13/913,100 dated May 4, 2015, 25 pages. |
Non-Final Office Action on U.S. Appl. No. 13/919,406 dated Jul. 14, 2015, 23 pages. |
Non-Final Office Action on U.S. Appl. No. 14/162,035, dated Feb. 4, 2016, 9 pages. |
Non-Final Office Action on U.S. Appl. No. 14/465,753 dated Apr. 4, 2016, 12 pages. |
Non-Final Office Action on U.S. Appl. No. 14/086,844, dated Nov. 10, 2015, 17 pages. |
Notice of Allowance on U.S. Appl. No. 12/075,103 dated Aug. 4, 2014, 10 pages. |
Notice of Allowance on U.S. Appl. No. 13/246,769 dated Jan. 8, 2015, 10 pages. |
Notice of Allowance on U.S. Appl. No. 13/707,438 dated Feb. 25, 2015, 11 pages. |
Notice of Allowance on U.S. Appl. No. 14/681,901, dated Dec. 23, 2015, 8 pages. |
Office Action for U.S. Appl. No. 12/892,663, dated Oct. 22, 2012, 12 pages. |
Office Action for U.S. Appl. No. 13/717,052, dated Aug. 22, 2013, 15 pages. |
Office Action on U.S. Appl. No. 12/075,103 dated Jul. 31, 2013, 8 pages. |
Office Action on U.S. Appl. No. 13/246,769 dated Apr. 21, 2014, 18 pages. |
Pessi et al., On the Relationship Between Lightning and Convective Rainfall Over the Central Pacific Ocean, date unknown, 9 pages. |
RDR-4B Honeywell User Manual for Forward Looking Windshear Detection/Weather Radar System, Rev. 6, Jul. 2003, 106 pps. |
Robinson et al., En Route Weather Depiction Benefits of the Nexrad Vertically Integrated Liquid Water Product Utilized by the Corridor Integrated Weather System, 10th Conference on Aviation, Range, and Aerospace Meteorology (ARAM), 2002, 4 pages. |
Stormscope Lightning Detection Systems, L3 Avionics Systems, retrieved on Jul. 11, 2011, 6 pages. |
TOA Technology, printed from website: http://www.toasystems.com/technology.html on Dec. 29, 2010, 2 pages. |
Triangulation, from Wikipedia, printed from website: http://en.wikipedia.org/wiki/Triangulation on Dec. 29, 2010, 6 pages. |
Waldvogel et al., The Kinetic Energy of Hailfalls. Part I: Hailstone Spectra, Journal of Applied Meteorology, Apr. 1978, 8 pages. |
Wilson et al., The Complementary Use of Titan-Derived Radar and Total Lightning Thunderstorm Cells, paper presented on Oct. 16, 2005, 10 pages. |
Corrected Notice of Allowance for U.S. Appl. No. 14/608,071 dated Dec. 15, 2017. 3 pages. |
Notice of Allowance for U.S. Appl. No. 14/323,766 dated Jun. 19, 2017. 7 pages. |
Notice of Allowance on U.S. Appl. No. 14/465,730, dated Feb. 28, 2017, 5 pages. |
Notice of Allowance on U.S. Appl. No. 14/608,071, dated Aug. 31, 2017, 9 pages. |