## Presentation on theme: "Radar: Acronym for Radio Detection and Ranging"— Presentation transcript:

Radar is a remote sensing technique: Capable of gathering information about objects located at remote distances from the sensing device. Two distinguishing characteristics: Employs EM waves that fall into the microwave portion of the electromagnetic spectrum (1 mm < l < 75 cm) 2. Active technique: radiation is emitted by radar – radiation scattered by objects is detected by radar.

Why microwaves? Microwaves can penetrate haze, fog and snow readily, and rain and hail less readily, so radar can “see through” these conditions. An elementary radar system

What does a conventional radar measure?
1. Distance to an object or collection of objects Determined by the time it takes energy to travel to the objects and return at the speed of light. r = km Dt = 6.67 ms r = 100 km Dt = ms 2. Azimuth and elevation angle to the object(s) Determined by the pointing angles of the antenna. 3. Physical properties of the object(s) Determined by the magnitude of the backscattered power.

Pulse duration (t, ms) and pulse length (h, meters)
Meteorological radars send out pulses of energy with relatively long periods of “listening” between pulses. Pulses are required, rather than continuous waves, to determine the distance to the target. Pulse duration (t, ms) and pulse length (h, meters) Pulse repetition period (msec) and pulse repetition frequency (s-1) Duty Cycle (= t/Tr)

Resolution along the direction of the beam:
half the pulse length (h) The back of the pulse at “a” will arrive at “b” at the same time that radiation scattered from objects at the front end of the pulse at “c” will arrive back at “b”. When energy arrives back at the radar, an instantaneous sample will include all radiation scattered between locations b and c: the sample volume is half the pulse length (h/2).

Second Trip Echo: an echo from a pulse that is not the most recent pulse

Definitions Pulse repetition frequency (PRF): The frequency that pulses are transmitted, measured in hertz (s-1) Pulse repetition period (Tr): The time between pulses (typical value 1 ms) Maximum Unambiguous Range (rmax): The maximum distance that an object can be located such that a pulse arriving at the object can return to the radar before another pulse is emitted.

Maximum unambiguous range vs. pulse repetition frequency

Note weird velocities (characteristic of distant storm)
Second trip echoes

Why not use a low PRF, insuring a large rmax?
Measurements are not made with a single pulse, but rather with the average of many pulses – since the antenna is rotating, dwell time (observing the same location) is an issue. 2. Measurement of Doppler velocities require a high PRF How can you eliminate second trip echoes automatically? Change the PRF Use a different PRF every 2-3 pulses, if echo moves, get rid of it!  This is the methodology employed by the 88-Ds

Other quantities used to describe the transmitted signal:
Wavelength (l, cm, mm) and Frequency (ft, Ghz, Mhz) Band designation Frequency range Wavelength range Common Frequency Common Wavelength (Ghz) (cm) UHF 30-100 0.42 71 L 15-30 1.3 23 S 7.5-15 2.8 10.7 C 5.5 X 9.4 3.2 Ku 15.5 1.94 K 24 1.25 Ka 35 0.86 Millimeter 40-300 94 (W band) 0.3

Major wavelength choice issues:
Size of equipment Attenuation Size of scatterers relative to wavelength (Rayleigh vs Mie scattering) Peak power (without arcing in waveguide – e.g., 3 MW in unpressurized waveguide for S band, 0.4 MW for K band) S (10 cm) band radar antenna K (0.8 cm) band radar antenna

Duplexer Fast acting Switch that protects sensitive receiver from high energy pulse from magnetron Modulator Stores power Between pulses Magnetron Generates Microwaves when high voltage pulse sent from Modulator Frequency Determined by characteristics of magnetron STALO Oscillator Generates a steady frequency COHO Oscillates at lower frequency with same phase as transmitted pulse

Quantities used to describe weather echoes
Wavelength (l   l, cm, mm) and Frequency (ft  fD) Ghz, Mhz) fD is the Doppler shift, the change in frequency that occurs because scatterers are moving toward or away from the radar. Doppler shift is typically no more than a few kilohertz, while The transmitted frequency is typically gigahertz! 3,000,000,000 3,000,001,000

Quantities used to describe weather echoes
Received Power: typical value: nanowatts Compare the received power with the transmitted power: Peak transmitted power: 106 watts Received power: watts Receiver must be very sensitive, and must be protected from main pulse of energy transmitted by the radar!

Modulator Stores power Between pulses Duplexer Protects Sensitive Receiver from High energy Pulse from magnetron Klystron Amplifier that creates microwaves at frequency determined by STALO and COHO STALO Oscillator Generates a steady frequency COHO Oscillates at lower frequency with same phase as transmitted pulse

Amplitude determination:
Phase determination:

Ratio (db) of input power that causes the video output to reach its maximum (saturation) level, to the lowest power that produces a detectable input. Dynamic range of precipitation echoes Ratio (db) of maximum echo power received from a very intense storm close to the radar to the minimum power received from the weakest cloud that can be detected at the greatest range of interest.

WOULD LIKE THESE TO BE THE SAME!
Dynamic range of a receiver Dynamic range of precipitation echoes

Linear receivers: Output voltage is linear with input power
Single linear receivers Typically have only half of the dynamic range of precipitation echoes, so two receivers are often used in tandem with automatic switching depending on the magnitude of the returned signal Receiver 1: Strong echoes Receiver 2: Weak echoes