Radar Meteorology

Total Page:16

File Type:pdf, Size:1020Kb

Radar Meteorology RADAR METEOROLOGY P.S.Biju [email protected] Courtesy: Presentations of Dr.D.Pradhan, Scientist-G, DDGM(UI),New Delhi, Shri.S.B.Thampi,DDGM,Chennai & Dr.Y.K.Reddi, Scientist-F,MCHyderabad Chapter 1: Introduction RADAR is an acronym for Radio Detection and Ranging. Similar principle is Light Detection and Ranging (LIDAR) used in ceilometers. So many other similar principles are there with Detection and Ranging (DAR) having the same equation for range measurement. Radar principle is explained in the following figure: The similar principle LIDAR is illustrated below: 1 Range of Radar Radar is an electronic device which is capable of transmitting an electromagnetic signal, receiving back an echo from a target, and determining various things about the target from the characteristics of the received signal. Range is the distance of the target given by the values of c and t , which is explained as h = ct/2 . Milestones of weather radar • 1842 : Doppler effect • 1888: Electromagnetic waves discovered by Hertz • 1922 : Detection of ships by radio waves by Marconi • 1947: The first weather radar in Washington D.C. • 1990: Introduction of Doppler weather radar • 2000: Doppler weather radars in India 2 Electromagnetic wave A wave propagation containing mutually perpendicular electric and magnetic fields perpendicular to the direction of propagation. Light wave is an example of electromagnetic wave Polarisation of radar signal The direction of propagation of electric field in an electromagnetic wave is known as polarisation. Hence an electromagnetic wave used in radar is either horizontally or vertically polarised. S-band Doppler weather radar of IMD is horizontally polarised and C-band is dual polarised (both horizontal and vertical). 3 Wavelength ( λλλ)and frequency( ννν) Length of one wave is known as wavelength Time taken to travel one complete wavelength is known as period (T) . Number of wavelengths travelled in one second is known as frequency( ν) . Hence T = 1/ ν and Velocity C= λ/T = νλ Electromagnetic spectrum The arrangement of electromagnetic wave according the order of wavelength is known as electromagnetic spectrum. Radar signal uses wavelength in the microwave region ( 1mm to 1 m) in the following bands. 4 IMD utilised S (10 cm), C ( 5 cm) and X ( 3 cm) bands in DWR, Polarised radar and Multimet radar respectively. 5 X-band become obsolete in IMD ? Attenuation of radar signal while passing through a medium is inversely proportional to wavelength as per the following equation: X-band radars are not suitable for the tracking of clouds, cyclones etc due its smaller wavelength gives more attenuation while passing through it. Hence Cyclone detection radars and Doppler weather radars at coastal stations uses S –band only. Doppler effect Doppler effect observed in sound was described by Christian Andreas Doppler that the sound waves from a source coming closer to a standing person have a higher frequency while the sound waves from a source going away from a standing person have a lower frequency. The approach of Doppler in sound waves proved to be valid for light waves also. Light waves from a source coming closer to an observer have a higher frequency (lower wavelength-Blue shift) while the light waves from a source 6 going away from an observer have a lower frequency (Larger wavelength-Red shift). Doppler effect in Radar In Doppler weather radar (DWR) this principle is adopted by considering radar as observer and the moving target as the source of light ( In fact the original source is also radar, but the scattered light is reflected is from the target. Hence for the radar (observer) the source is the target) Doppler shift in frequency ( ∆ν) is given by the basic equation; Where V is the velocity of target. Hence Doppler weather radar will give both range and velocity of the target. Distinguish between conventional radar and DWR Conventional radar 1. Gives only position of a target 2. Analog technology and mostly black and white pictures 3. No provision for unattended operation Doppler weather radar 1. DWR gives both position and velocity of a target 2. Automatic control and Mostly unattended operation 3. User friendly colour images 4. Large number of products for various applications like aviation, hydrology, weather forecasting etc 7 Block diagram of a Radar Transmitter: This part requires high power for the transmission of electromagnetic signal upto 500 Km range. The basic component is a Radio Frequency generator (RF Generator). The generated RF frequency signal is amplified to high power electromagnetic signals by the one of the following transmitters: 1. Magnetron 2. Klystron 3. Solid state transmitters Magnetron has Lighter weight, Easy to carry and 200 MW or more power. But its frequencies are not purer, which is essential for Doppler weather radar. Conventional radars used magnetron as the transmitter Klystron has Heavier weight, Purer frequencies, Wave forms can be controlled and generate power of more than 200 MW. Doppler weather radar uses Klystron as the transmitter. Solid state transmitters have power only up to 50 W, but desirable power can be achieved by making an array of a large numbers of transmitters. But seldom used for meteorological purposes. Modulator : Modulator is the ON/OFF switch of the Radar Transmitter. When and which duration it should transmit will be decided by the modulator. It also decides the correct wave form of the transmitted signal. Master clock and PRF: Master clock controls the entire radar system. It determines how often the radar will transmit signal into space. The rate at 8 which the radar transmits is called Pulse Repetition Frequency (PRF). Usually its value is between 200Hz to 3000 Hz. The duration of transmitter signal names either pulse duration or pulse length. Typical value of Pulse duration is 0.1 to 10 µs. DWR of IMD uses two Pulse widths 1 µs and 2 µs. Antenna: Antenna is a device for radiating and receiving of EM waves. It can be isotropic or non isotropic. An antenna that sends the radiation equally in all directions is called isotropic antenna. It is similar to the light of a candle except the bottom portion. Radar antennas are more like flash lights Main parameters in the selection of an antenna are: Wave length Diameter of reflector ( small as a foot to 30 ft) Gain Gain is the ratio of power received at a point in space on the centre of the beam axis to the power received at the same point from an isotropic antenna. As shown above, gain has no unit. But logarithm of gain multiplied by 10 has a unit called deciBell. Typical gain is 20 dB to 45 dB. 9 Ideal antenna would direct all of the radar energy into a single direction and this is practically impossible. Practically radar signal have a bright spot called the main lobe and also having energy off to the side of the main lobe called side lobes. Radar signal also have energy behind the antenna called back lobes. Relation between gain and beam width: Beam width is the angular distance across the antenna beam at the point where the power is reduced to one half of the peak power which exists along the centre axis of the antenna beam pattern k2 depends on the kind and shape of the antenna and for circular reflector k2=1 10 deci Bell (dB) unit For example the output power of Klystron is about 800kW. It can be expressed in dB as: In dBm as Half power in dB 10 log (1/2) = - 3 dB, i.e. the power reduced to half means power is reduced by 3 dB For example power reduced from 8W to 4W 10 log (8)=9 dB and 10 log (4) = 6 dB. Clearly the reduction is 3 dB 10 log (1/4)=-6 dB i.e. the power reduced to one-fourth means power reduced by 6 dB For example power reduced from 8W to 2W 10 log (8)=9 dB and 10 log (2) = 3 dB. Clearly the reduction is 6 11 Wave guide Regular wires and coaxial cables cause so much loss of signals that they are not useful at radar frequencies Wave guide is a conductor connecting transmitter/receiver and antenna .Wave guide is usually a hollow, rectangular, metal conductor whose interior dimensions depend upon of the wavelength of the signal being carried. T/R Switch or Duplexer Most of the radars transmit power from 1000 W to more than 1 MW. At the same time it is capable of receiving powers as small as 10 -10 W or less. If transmitter sent power in to the receiver it would burn up quickly. An automatic switch known as T/R switch or Duplexer is added in the radar system to protect the receiver from the high power of the transmitter. When the transmitter is turned on , the duplexer acts to direct the strong pulse of energy to the antenna and as soon as the transmitter stops sending a signal, 12 the duplexer switches to connect antenna with the receiver and transmitter will be disconnected from the antenna. Receiver Receivers detect and amplify the very weak signal received by the antenna. Most of the radars used super heterodyne type receivers where the high frequency received signal is mixed with a reference signal and converts it into a much lower frequency (typically 30 to 60 Hz).,which can be easily processed. Co-axial cables can be used to connect receivers with displays since frequency and distance are less. 13 Display The earliest and easiest display is to put the radar data in to an oscilloscope where horizontal axis is time and vertical axis is signal strength.
Recommended publications
  • A Real-Time System to Estimate Weather Conditions at High Resolution
    12.1 A Real-Time System to Estimate Weather Conditions at High Resolution Peter P. Neilley1 Weather Services International, Inc. Andover, MA 01810 And Bruce L. Rose The Weather Channel Atlanta, GA the earth’s surface (the so-called current 1. Introduction1 conditions). b) We do not necessarily produce weather The purpose of this paper is to describe an observations on a regular grid, but at an operational system used to estimate current irregular set of arbitrary locations or points weather conditions at arbitrary places in real- that are relevant to the consumers of the time. The system, known as High Resolution information. Assimilation of Data (or HiRAD), is designed to generate synthetic weather observations in a c) In addition to producing quantitative manner equivalent in scope, timeliness and observational elements (e.g. temperature, quality to a arbitrarily dense physical observing pressure and wind speed) our system network. Our approach is, first, to collect produces common, descriptive terminology information from a variety of relevant sources of the sensible weather such as including gridded analyses, traditional surface “Thundershowers”, “Patchy Fog”, and weather reports, radar, satellite and lightning “Snow Flurries”. observations. Then we continuously synthesize these data into weather condition estimates at d) We do not strive to produce a state of the prescribed locations. An operational system atmosphere optimized for fidelity with based on this approach has been built and is Numerical Weather Prediction (NWP) commercially deployed in the United States. models. Instead, the system is optimized to produce the most accurate estimate of the In most regards, our approach is analogous to observed state at the surface that can be modern data assimilation techniques.
    [Show full text]
  • Fire W Eather
    Fire Weather Fire Weather Fire weather depends on a combination of wildland fuels and surface weather conditions. Dead and live fuels are assessed weekly from a satellite that determines the greenness of the landscape. Surface weather conditions are monitored every 5-minutes from the Oklahoma Mesonet. This fire weather help page highlights the surface weather ingredients to monitor before wildfires and also includes several products to monitor once wildfires are underway. Fire Weather Ingredients: WRAP While the presence of wildland fuels is one necessary component for wildfires, weather conditions ultimately dictate whether or not a day is primed for wildfires to occur. There are four key fire weather ingredients and they include: high Winds, low Relative humidity, high Air temperature, and no/minimal recent Precipitation (WRAP). High Winds are the second most critical weather ingredient for wildfires. In general, winds of 20 mph or greater 20+ mph winds increase spot fires and make for most of the containment considerably more difficult. state Low Relative humidity is the most 30-40+ critical weather ingredient for wildfires mph winds and is most common in the afternoon when the air temperature is at its warmest. When relative humidity is at or below 20% extreme fire behavior can result and spot fires become freQuent. Watch out for areas of 20% or below relative humidity and 20 mph or higher winds à 20/20 rule! Extremely low relative humidity Warm Air temperatures are another values key weather ingredient for wildfires as warming can lower the relative humidity, reduce moisture for smaller dead fuels, and bring fuels closer to their ignition point.
    [Show full text]
  • Weather Charts Natural History Museum of Utah – Nature Unleashed Stefan Brems
    Weather Charts Natural History Museum of Utah – Nature Unleashed Stefan Brems Across the world, many different charts of different formats are used by different governments. These charts can be anything from a simple prognostic chart, used to convey weather forecasts in a simple to read visual manner to the much more complex Wind and Temperature charts used by meteorologists and pilots to determine current and forecast weather conditions at high altitudes. When used properly these charts can be the key to accurately determining the weather conditions in the near future. This Write-Up will provide a brief introduction to several common types of charts. Prognostic Charts To the untrained eye, this chart looks like a strange piece of modern art that an angry mathematician scribbled numbers on. However, this chart is an extremely important resource when evaluating the movement of weather fronts and pressure areas. Fronts Depicted on the chart are weather front combined into four categories; Warm Fronts, Cold Fronts, Stationary Fronts and Occluded Fronts. Warm fronts are depicted by red line with red semi-circles covering one edge. The front movement is indicated by the direction the semi- circles are pointing. The front follows the Semi-Circles. Since the example above has the semi-circles on the top, the front would be indicated as moving up. Cold fronts are depicted as a blue line with blue triangles along one side. Like warm fronts, the direction in which the blue triangles are pointing dictates the direction of the cold front. Stationary fronts are frontal systems which have stalled and are no longer moving.
    [Show full text]
  • Weather Observations
    Operational Weather Analysis … www.wxonline.info Chapter 2 Weather Observations Weather observations are the basic ingredients of weather analysis. These observations define the current state of the atmosphere, serve as the basis for isoline patterns, and provide a means for determining the physical processes that occur in the atmosphere. A working knowledge of the observation process is an important part of weather analysis. Source-Based Observation Classification Weather parameters are determined directly by human observation, by instruments, or by a combination of both. Human-based Parameters : Traditionally the human eye has been the source of various weather parameters. For example, the amount of cloud that covers the sky, the type of precipitation, or horizontal visibility, has been based on human observation. Instrument-based Parameters : Numerous instruments have been developed over the years to sense a variety of weather parameters. Some of these instruments directly observe a particular weather parameter at the location of the instrument. The measurement of air temperature by a thermometer is an excellent example of a direct measurement. Other instruments observe data remotely. These instruments either passively sense radiation coming from a location or actively send radiation into an area and interpret the radiation returned to the instrument. Satellite data for visible and infrared imagery are examples of the former while weather radar is an example of the latter. Hybrid Parameters : Hybrid observations refer to weather parameters that are read by a human observer from an instrument. This approach to collecting weather data has been a big part of the weather observing process for many years. Proper sensing of atmospheric data requires proper siting of the sensors.
    [Show full text]
  • Project Stormy Weather Began in 1943
    61 Chapter 8 The Stormy Weather Group (Canada) R.H. Douglas,* McGill University 1 INTRODUCTION nated, and the McGill group carried on as the Stormy Weather Group. years later Project Stormy Weather began in 1943. Thirty Marshall (1973) recalls that "the first contribution of of the Marshall (1973), reviewing the accomplishments Project Stormy Weather, within the CAORG, was time­ meteorology and cloud Stormy Weather Group in radar lapse photography of the PPI scope. (By telephoning an estimated 500 scientists physics, noted that (in 1973) around the Ottawa Valley, it was established that there in weather radar, the around the world were involved was rain where the radar screen glowed, and that rain from a handful in 1943. number having increased linearly started at a given point just after the echo moved over that the Stormy Weather Group, Quoting Marshall, "Activity of point on the screen.) Viewing these films as movies, one roughly one-sixth continuous for thirty years, represented sensed a new approach to storm dynamics and a potential about one­ of the whole until, say, 1963, and represents for short-term forecasting. The showing of Stormy Weather ( 19 73 ) ." Thus Marshall twelfth of the larger activity now films to American scientific meetings did much to stimulate and his colleagues in the Group have enjoyed a continuing interest in weather radar." in the development of and advances and significant role The early radar equipment consisted of a microwave but relatively recent in this (by now) well-established height-finding unit at Ottawa and early warning units at branch of the meteorological sciences.
    [Show full text]
  • ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
    ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere.
    [Show full text]
  • A Brief Overview of Weather Radar Technologies and Instrumentation
    A Brief Overview of Weather Radar Technologies and Instrumentation Mark Yeary, Boon L. Cheong, James M. Kurdzo, Tian-You Yu, and Robert Palmer eather radar technologies and instrumenta- networks, and spectrum sharing. Next, we look at several tion play a vital role in early warning of severe hardware and signal processing technology examples related W weather. For example, the annual impacts of to these lists. adverse weather on the U.S. national highway system and roads are staggering: 7,400 weather–related deaths and 1.5 Hardware and Signal Processing million weather–related crashes [1]. In addition, US$4.2 bil- Technologies lion is lost each year as a result of air traffic delays attributed Severe and hazardous weather such as thunderstorms, down- to weather. Research on high-impact weather is broadly mo- bursts, and tornadoes can take lives in a matter of minutes. To tivated by society’s need to improve the prediction of these improve detection and forecast of such phenomena using ra- weather events. The research approaches to accomplish this dar, one of the key factors is fast scan capability. Conventional goal vary significantly with the inherent predictability of the weather radars, such as the pervasive Next Generation Ra- weather system. For example, the current forecast approaches dar (NEXRAD) developed in the 1980s, are severely limited by for issuing warnings of short-lived events, such as tornadoes mechanical scanning with their large rotating dish. Approxi- and flash floods, are primarily based on observations with a fo- mately 168 of these radars are in a national network to provide cus on advanced Doppler radar measurements.
    [Show full text]
  • Singapore Changi Airport Dropsonde for Weather
    41621Y_Vaisala156 6.4.2001 10:05 Sivu 1 156/2001156/2001 Extensive AWOS System: Singapore Changi Airport 2000 NWS Isaac Cline Meteorology Award: Dropsonde for Weather Reconnaissance Short-Term Weather Predictions in Urban Zones: Urban Forecast Issues and Challenges The 81st AMS Annual Meeting: Precipitation Extremes and Climate Variability 41621Y_Vaisala156 6.4.2001 10:05 Sivu 2 Contents President’s Column 3 Vaisala’s high-quality customer Upper Air Obsevations support aims to offer complete solutions for customers’ AUTOSONDE Service and Maintenance measurement needs. Vaisala Contract for Germany 4 and DWD (the German Dropsonde for Weather Reconnaissance in the USA 6 Meteorological Institute) have signed an AUTOSONDE Service Ballistic Meteo System for the Dutch Army 10 and Maintenance Contract. The service benefits are short GPS Radiosonde Trial at Camborne, UK 12 turnaround times, high data Challenge of Space at CNES 14 availability and extensive service options. Surface Weather Observations World Natural Heritage Site in Japan 16 The First MAWS Shipped to France for CNES 18 Finland’s oldest and most Aviation Weather experienced helicopter operator Copterline Oy started scheduled The Extesive AWOS System to route traffic between Helsinki Singapore Changi Airport 18 and Tallinn in May 2000. Accurate weather data for safe The New Athens International Airport 23 journeys and landings is Fast Helicopter Transportation Linking Two Capitals 24 provided by a Vaisala Aviation Weather Reporter AW11 system, European Gliding Champs 26 serving at both ends of the route. Winter Maintenance on Roads Sound Basis for Road Condition Monitoring in Italy 28 Fog Monitoring Along the River Seine 30 The French Air and Space Academy has awarded its year Additional Features 2000 “Grand Prix” to the SAFIR system development teams of Urban Forecast Issues and Challenges 30 Vaisala and ONERA (the The 81st AMS Annual Meeting: French National Aerospace Precipitation Extremes and Climate Variability 38 Research Agency).
    [Show full text]
  • Ront November-Ddecember, 2002 National Weather Service Central Region Volume 1 Number 6
    The ront November-DDecember, 2002 National Weather Service Central Region Volume 1 Number 6 Technology at work for your safety In this issue: Conceived and deployed as stand alone systems for airports, weather sensors and radar systems now share information to enhance safety and efficiency in the National Airspace System. ITWS - Integrated Jim Roets, Lead Forecaster help the flow of air traffic and promote air Terminal Aviation Weather Center safety. One of those modernization com- Weather System The National Airspace System ponents is the Automated Surface (NAS) is a complex integration of many Observing System (ASOS). technologies. Besides the aircraft that fly There are two direct uses for ASOS, you and your family to vacation resorts, and the FAA’s Automated Weather or business meetings, many other tech- Observing System (AWOS). They are: nologies are at work - unseen, but critical Integrated Terminal Weather System MIAWS - Medium to aviation safety. The Federal Aviation (ITWS), and the Medium Intensity Intensity Airport Administration (FAA) is undertaking a Airport Weather System (MIAWS). The Weather System modernization of the NAS. One of the technologies that make up ITWS, shown modernization efforts is seeking to blend in Figure 1, expand the reach of the many weather and aircraft sensors, sur- observing site from the terminal to the en veillance radar, and computer model route environment. Their primary focus weather output into presentations that will is to reduce delays caused by weather, Gust fronts - Evolution and Detection Weather radar displays NWS - Doppler FAA - ITWS ASOS - It’s not just for airport observations anymore Mission Statement To enhance aviation safety by Source: MIT Lincoln Labs increasing the pilots’ knowledge of weather systems and processes Figure 1.
    [Show full text]
  • The Role of Weather Radar in Rainfall Estimation and Its Application in Meteorological and Hydrological Modelling—A Review
    remote sensing Review The Role of Weather Radar in Rainfall Estimation and Its Application in Meteorological and Hydrological Modelling—A Review ZbynˇekSokol 1 , Jan Szturc 2,* , Johanna Orellana-Alvear 3,4 , Jana Popová 1,5 , Anna Jurczyk 2 and Rolando Célleri 3 1 Institute of Atmospheric Physics of the Czech Academy of Sciences, Bocni II, 141 00 Praha 4, Czech Republic; [email protected] (Z.S.); [email protected] (J.P.) 2 Institute of Meteorology and Water Management—National Research Institute, PL 01-673 Warsaw, Poland; [email protected] 3 Departamento de Recursos Hídricos y Ciencias Ambientales and Facultad de Ingeniería, Universidad de Cuenca, Cuenca EC10207, Ecuador; [email protected] (J.O.-A.); [email protected] (R.C.) 4 Laboratory for Climatology and Remote Sensing (LCRS), Faculty of Geography, University of Marburg, D-035032 Marburg, Germany 5 Faculty of Science, Charles University, Albertov 6, 128 00 Praha 2, Czech Republic * Correspondence: [email protected] Abstract: Radar-based rainfall information has been widely used in hydrological and meteorological applications, as it provides data with a high spatial and temporal resolution that improve rainfall representation. However, the broad diversity of studies makes it difficult to gather a condensed overview of the usefulness and limitations of radar technology and its application in particular situations. In this paper, a comprehensive review through a categorization of radar-related topics Citation: Sokol, Z.; Szturc, J.; aims to provide a general picture of the current state of radar research. First, the importance and Orellana-Alvear, J.; Popová, J.; Jurczyk, A.; Célleri, R.
    [Show full text]
  • Weather in the Cockpit: Priorities, Sources, Delivery, and Needs in the Next Generation Air Transportation System
    DOT/FAA/AM-12/7 Office of Aerospace Medicine Washington, DC 20591 Weather in the Cockpit: Priorities, Sources, Delivery, and Needs in the Next Generation Air Transportation System Roger W. Schvaneveldt and Russell J. Branaghan Arizona State University Mesa, AZ 85212 John Lamonica Lamonica Aviation Tucson, AZ 85718 Dennis B. Beringer FAA Civil Aerospace Medical Institute P.O. Box 25082 Oklahoma City, OK 73125 July 2012 Final Report NOTICE This document is disseminated under the sponsorship of the U.S. Department of Transportation in the interest of information exchange. The United States Government assumes no liability for the contents thereof. ___________ This publication and all Office of Aerospace Medicine technical reports are available in full-text from the Civil Aerospace Medical Institute’s publications website: www.faa.gov/go/oamtechreports Technical Report Documentation Page 1. Report No. 2. Government Accession No. 3. Recipient's Catalog No. DOT/FAA/AM-12/7 4. Title and Subtitle 5. Report Date Weather in the cockpit: Priorities, Sources, Delivery, and Needs in the July 2012 Next Generation Air Transportation System 6. Performing Organization Code 7. Author(s) 8. Performing Organization Report No. Schvaneveldt RW,1 Branaghan RJ,1 Lamonica J,2 Beringer, DB3 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) 1 Arizona State University, Mesa, AZ 85212 2 11. Contract or Grant No. Lamonica Aviation, Tucson, AZ 85718 3 FAA Civil Aerospace Medical Institute, P.O. Box 25082 Oklahoma City, OK 73125 12. Sponsoring Agency name and Address 13. Type of Report and Period Covered Office of Aerospace Medicine Federal Aviation Administration 800 Independence Ave., S.W.
    [Show full text]
  • A History of Radar Meteorology: People, Technology, and Theory
    A History of Radar Meteorology: People, Technology, and Theory Jeff Duda Overview • Will cover the period from just before World War II through about 1980 – Pre-WWII – WWII – 1940s post-WWII – 1950s – 1960s – 1970s 2 3 Pre-World War II • Concept of using radio waves established starting in the very early 1900s (Tesla) • U.S. Navy (among others) tried using CW radio waves as a “trip beam” to detect presence of ships • First measurements of ionosphere height made in 1924 and 1925 – E. V. Appleton and M. A. F. Barnett of Britain on 11 December 1924 – Merle A. Tuve (Johns Hopkins) and Gregory Breit (Carnegie Inst.) in July 1925 • First that used pulsed energy instead of CW 4 Pre-World War II • Robert Alexander Watson Watt • “Death Ray” against Germans • Assignment given to Arnold F. “Skip” Wilkins: – “Please calculate the amount of radio frequency power which should be radiated to raise the temperature of eight pints of water from 98 °F to 105 °F at a distance of 5 km and a height of 1 km.” – Not feasible with current power production Watson Watt 5 Pre-World War II • Watson Watt and Wilkins pondered whether radio waves could be used merely to detect aircraft • Memo drafted by Watson Watt on February 12, 1935: “Detection of Aircraft by Radio Methods” – Memo earned Watson Watt the title of “the father of radar” – Term “RADAR” officially coined as an acronym by U.S. Navy Lt. Cmdr. Samuel M. Tucker and F. R. Furth in November 1940 • The Daventry experiment – February 26, 1935 – First recorded detection of aircraft by radio waves – Began the full-speed-ahead
    [Show full text]