Radio Acoustic Sounding Techniques for Temperature Profiling Mrs Jyoti Chande Head Atmospheric Remote Sensing Division SAMEER, IIT Campus, Powai, Mumbai.

Slides:



Advertisements
Similar presentations
Foundations of Medical Ultrasonic Imaging
Advertisements

Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
7. Radar Meteorology References Battan (1973) Atlas (1989)
Chapter 11 Waves. Waves l A wave is a disturbance/oscillation generated from its source and travels over long distances. l A wave transports energy but.
1 Transmission Fundamentals Chapter 2 (Stallings Book)
Water vapor estimates using simultaneous S and Ka band radar measurements Scott Ellis, Jothiram Vivekanandan NCAR, Boulder CO, USA.
Thermometer Variable: temperature Units: Degrees Celsius ( o C) Accuracy: marked to 0.5 o C Cost: £10 Site: in the shade (e.g. a Stevenson Screen) Mercury.
MR P.Durkee 5/20/2015 MR3522Winter 1999 MR Remote Sensing of the Atmosphere and Ocean - Winter 1999 Active Microwave Radar.
Millimeter Wave Sensor: An Overview
Distance observations
SURVEYING II UNIT IV PRESENTATION II.
ECE 501 Introduction to BME
Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
Antennas Lecture 9.
Introduction to Wireless Communications. Wireless Comes of Age Guglielmo Marconi invented the wireless telegraph in 1896 Communication by encoding alphanumeric.
Antennas and Propagation
1 Sinusoidal Waves The waves produced in SHM are sinusoidal, i.e., they can be described by a sine or cosine function with appropriate amplitude, frequency,
How can we get a vertical profile of the wind in the atmosphere?
Satellite observation systems and reference systems (ae4-e01) Signal Propagation E. Schrama.
Remote Sensing: John Wilkin Active microwave systems (4) Coastal HF Radar IMCS Building Room 214C ext 251 Dunes of sand.
Module 3.0: Data Transmission
COPS-GOP-WS3 Hohenheim 2006_04_10 Micro- Rain- Radar Local Area Weather Radar Cloud Radar Meteorological Institute University Hamburg Gerhard Peters.
Remote Sensing: John Wilkin Active microwave systems Coastal HF Radar IMCS Building Room 214C ph: Dunes of sand and seaweed,
Lecture 4b Fiber Optics Communication Link 1. Introduction 2
Electromagnetic Wave Theory
SeaSonde Overview.
How can we get a vertical profile of the atmosphere?
Balloon-Borne Sounding System (BBSS) Used for atmospheric profiling Measures P, T, RH, wind speed and direction Uncertainties arise from incorrect surface.
Radar: Acronym for Radio Detection and Ranging
Lecture Notes #5 Antennas and Propagation
Doppler Radar From Josh Wurman NCAR S-POL DOPPLER RADAR.
Doppler Radar From Josh Wurman Radar Meteorology M. D. Eastin.
Radar Principles and Systems Part I
Basic RADAR Principles Prof. Sandra Cruz-Pol, Ph.D. Electrical and Computer Engineering UPRM.
Profilers. Wind profilers are phased array radars that measure the wind as a function of height above a fixed location. Characteristics: Wavelength: 33.
Tutorial I: Radar Introduction and basic concepts
Review Doppler Radar (Fig. 3.1) A simplified block diagram 10/29-11/11/2013METR
ElectroScience Lab IGARSS 2011 Vancouver Jul 26th, 2011 Chun-Sik Chae and Joel T. Johnson ElectroScience Laboratory Department of Electrical and Computer.
Radar equation review 1/19/10. Radar eq (Rayleigh scatter) The only variable is h, the pulse length Most radars have a range of h values. Rewrite the.
July 2001Zanjan, Iran1 Atmospheric Profilers Marc Sarazin (European Southern Observatory)
General Licensing Class G8A – G8B Signals and Emissions Your organization and dates here.
Wind Profiler Signal & Data Processing -Anil Anant Kulkarni SAMEER, IIT Campus,Powai Mumbai
EM propagation paths 1/17/12. Introduction Motivation: For all remote sensing instruments, an understanding of propagation is necessary to properly interpret.
10. Satellite Communication & Radar Sensors
Certified Wireless Network Administrator (CWNA) PW0-105 Chapter 2 Radio Frequency Fundamentals.
Pegasus Lectures, Inc. COPYRIGHT 2006 Volume I Companion Presentation Frank R. Miele Pegasus Lectures, Inc. Ultrasound Physics & Instrumentation 4 th Edition.
Polarimetric Solid State Radar Design for CASA Student Test Bed
Review of Ultrasonic Imaging
Fig. 3 Wind measurements experimental setup Lidar (light detection and ranging) operates using the same concept of microwave RADAR, but it employs a lot.
UPenn NROTC Unit, dtd Fall 2004 Naval Weapons Systems Energy Fundamentals.
By Ya Bao1 Antennas and Propagation. 2 By Ya Bao Introduction An antenna is an electrical conductor or system of conductors Transmission - radiates electromagnetic.
Adaphed from Rappaport’s Chapter 5
SPECTRUM ANALYZER 9 kHz GHz
RF Propagation No. 1  Seattle Pacific University Basic RF Transmission Concepts.
WEATHER SIGNALS Chapter 4 (Focus is on weather signals or echoes from radar resolution volumes filled with countless discrete scatterers---rain, insects,
Antennas and Propagation Chapter 5. Introduction An antenna is an electrical conductor or system of conductors Transmission - radiates electromagnetic.
A new method for first-principles calibration
1 A conical scan type spaceborne precipitation radar K. Okamoto 1),S. Shige 2), T. Manabe 3) 1: Tottori University of Environmental Studies, 2: Kyoto University.
Signal Propagation Basics
EEE381B Pulsed radar A pulsed radar is characterized by a high power transmitter that generates an endless sequence of pulses. The rate at which the pulses.
By Saneeju m salu. Radio waves are one form of electromagnetic radiation RADIO WAVES.
Estimation of temperature and humidity with a wind profiling radar-RASS measurements Toshitaka Tsuda Research Institute for Sustainable Humanosphere, Kyoto.
Fundamentals of Communications. Communication System Transmitter: originates the signal Receiver: receives transmitted signal after it travels over the.
Dr. Clincy Professor of CS
BME 312 BIOMEDICAL INSTRUMENTATION II LECTURER: ALİ IŞIN
presented by: Reham Mahmoud AbD El-fattah ali
Tropo-Scatter Link Budget
Introduction and Basic Concepts
Chap II. Radar Hardware (PART 1)
Radio Links.
Presentation transcript:

Radio Acoustic Sounding Techniques for Temperature Profiling Mrs Jyoti Chande Head Atmospheric Remote Sensing Division SAMEER, IIT Campus, Powai, Mumbai

Why we need temperature profiles? For better understanding of Meteorological phenomenon Thermal perturbation excite gravity waves Temperature inversion layers prevent mixing of layers which causes trapping of hazardous chemicals

Temperature profiling - Application areas- Meteorology Atmospheric research Study of thermal inversions, Measurement of heat flux Boundary layer research. Environmental monitoring applications

Observation techniques of temperature profiles Direct (in-situ measurement) –Radiosonde ( Height resolution 30 m, accuracy of 0.5 deg K & time interval 3hr) Remote sensing: –Radiometer –RASS

What is RASS? Radio Acoustic Sounding System - Combines Radio and acoustic probing techniques for obtaining continuous temperature profiles

RASS concept

RASS concept: The basic concept of RASS is tracking of sound waves by means of electromagnetic radar. The compression and rarefaction of air due to transmitted sound waves alters the refractive index of air in periodic fashion causing the reflection of electromagnetic waves. For enhancing the reflected electromagnetic power it is essential that both acoustic and radio wavelength are BRAGG matched

Bragg Matching condition Scattering of radio waves is intensified when the acoustic and radio wavelengths satisfy relation as follows e = 2 a where e : electrical wavelength & a : Acoustic wavelength

RASS measurements Physical quantity inferred by the RASS is Ca Ca : atmospheric sound velocity. The virtual temperature is related to speed of sound Ca is as follows Ca =  Tv Tv: virtual temperature Tv = T( x r) r :the mixing ratio of water vapor in the air and T is the air temperature in deg K

RASS realization RASS can be added to a 1.wind profiler radar (Pulsed radar and FMCW acoustic) 2.Acoustic sounder /Sodar system. (Pulsed Acoustic and CW radar)

Windprofiler- RASS Three or four vertically pointing acoustic antennas are placed around the radar wind profiler's RF antenna Acoustic system is added which contains power amplifier Acoustic Signal generating unit. Acoustic antennas generate periodic scattering structure which is sampled by coherent pulsed electromagnetic radar.

RASS added to an acoustic sounder The radar subsystems are added to transmit and receive radar signals and to process the reflected radar echo information. The sodar transducer are used to transmit the acoustic signals that produces the Bragg scattering of the radar signals. The speed of sound is measured by the CW electromagnetic radar

Height Coverage: The Maximum height coverage for Temperature profiles basically depends on System parameters ( wave length, antenna Size, acoustic power and Radar Power ) Atmospheric parameters ( turbulence, winds and humidity) Distance between the Acoustic and RF systems Acoustic attenuation:

Acoustic attenuation Sound is absorbed in air by several processes. Absorption is a complicated function of Frequency Temperature Humidity...

Signal to Noise Ratio -for Wind profiler/ RASS mode : The back-scattered echo power is given as; (c  /2) P a Ga Pr Pr = 3.7 x x 10 -  R/10 x I ( r R ) 2 B where, Pr : Averaged received power (c  /2) : radar range resolution (m)

SNR c: Speed of light (3 x 10 8 m/s);  : radar pulse width r : radar wavelength in meters R: range in meters; Pa : transmitted acoustic power in watts; Ga: gain of acoustic antenna; Pr: Transmitted radar power in watts; B: 2  b/Ca : acoustic wave number bandwidth ; b: acoustic frequency bandwidth  : acoustic attenuation The factor I in equation describes the attenuation of the received signal due to atmospheric effects

Acoustic Excitation in pulsed radar: CW acoustic excitation A short acoustic pulse completely enclosed within radar pulse. A Long acoustic pulse where only part of acoustic pulse lies within resolution volume FMCW acoustic excitation

RR I Q A T Ca a CW excitation and resulting phasor diagram Peak is always at Ca Transmitted acoustic freq

RR I Q A T Ca a Short acoustic pulse and resulting phasor diagram Peak is at Bragg freq

RR I Q A T Ca a Long Pulse and resulting phasor diagram Two Peaks of approx equal magnitude at Ca & Bragg freq

RR I Q A T Ca a Sharp peaks only at Bragg frequency FMCW FMCW acoustic transmission

RASS installed at India Meteorology Department (IMD) Pune

Atmospheric humidity The relationship between acoustic speed and atmospheric temperature for dry air is given by Ca = A  T Where Ca : Acoustic Speed; T : Atmospheric Temperature in o K. Under the assumption that atmosphere is dry and obeys the ideal gas law We have equation A =  (  R’ / M) = –  is ratio of specific heats –R’ is the gas constant – M is mean molecular weight of air.

Accuracy of the temperature profiles obtained by the RASS technique depends upon atmospheric variables Humidity Vertical winds.. Effect of Atmospheric Parameters on Measurement Accuracy of RASS

Humidity correction Assumption of dry and still atmosphere is not valid in the lower troposphere. It was observed that at a given temperature, speed of sound varies with humidity. Ca = * A’  T where A’: constant depending on Relative humidity (%) For ex: for 100% humidity A’:

Errors due to Vertical Wind Velocities The vertical winds introduce errors in the temperature measured by RASS.  T = 1.6 * W where W is in m/sec. This error can be reduced by measuring the mean vertical velocity simultaneously and subtracting this from the acoustic speed at that height.

Vertical Doppler (  2 Hz) Acoustic Frequency 970 Hz 805 HZ Frequency L O without Offset

Acoustic Frequency L O with 890 Hz Offset - 80 Hz+80 Hz

Acoustic Frequency Vertical Doppler L O with 445 Hz Offset

Typical RASS spectrum

Temperature profiles derived from RASS spectrum

RASS implemented with Windprofiler Specifications- Transmitted Acoustic Power is 100 W (electrical) Type of Antennas : Parabolic reflector with acoustic transducer/ horn assembly Antenna gain :15 dB 3 dB beam width: 16 degrees. No of Antennas : Three ( switchable) Type of waveform : FMCW

Acoustic waveform design Range of acoustic frequencies to be transmitted depend on the variation of temperature in the desired range. The expected temperature variation is from C to about +50 o C. Sound velocities at these temperatures would be ranging from 298 m/s to m/s (  30 m/s). The corresponding acoustic frequencies are 805 Hz and 960 Hz. Thus a frequency modulated linear sweep of bandwidth 156 Hz ranging from 805 Hz to 961 Hz is required to be transmitted for getting Bragg matched conditions satisfied at all the range bins of our interest..

Temperature resolution Temperature resolution depends on the ability of system to resolve Doppler frequencies For highest temperature ( 45 o C) the velocity resolution should be of the order of 0.16 m/s or the Doppler resolution should be of the order of 0.45 Hz. This is achieved with Wind profiler system by keeping the data observation time for about 2 sec.

RASS II RASS implemented with acoustic sounder

RASS II SPECIFICATIONS  Radio Frequency : MHz  Acoustic Frequency: Hz  Range Resolution: 50 meters  Maximum Range: meters  Minimum range: 50 meters  Temperature measurement range: to 50 0 C  Temperature resolution: K

RASS SUBSYSTEMS 1. Tx and Rx RF Antennas 2. Transmitter (712 MHz) 3. Exciter 4. Receiver 5. Acoustic Source and Antenna 6. Digital Signal Processing

Transmitter Exciter Tx. Antenna Receiver Digital Signal Processing Rx. Antenna antenna Acoustic Source SODAR Antenna Fig.4 Block diagram of RASS system Transmitter Exciter Tx. Antenna Receiver Digital Signal Processing Rx. Antenna antenna Acoustic Source SODAR Antenna Fig.4 Block diagram of RASS system Schematic block diagram of CW RASS

ANTENNA  Type : Parabolic dish  Frequency: MHz  Diameter: 1.5 m  Gain: 20 dB  Bandwidth: 20 MHz Tx. Antenna Rx. Antenna

TRANSMITTER  Frequency :712.5 MHz  Power : 25 W CW  Harmonics : < 30 dBc  Type:Solid State  Bandwidth :10 MHz Radar Hardware

EXCITER  Reference Oscillator, OCXO (70 MHz)  Generation of RF and LO’s  MHz PLL

RECEIVER  Type:Super Heterodyne  Bandwidth: < 250 Hz  Noise Figure : < 3 dB  Receiver Sensitivity: -131 dBm

Acoustic Source & Antenna  Frequency: Hz  Power: 116 Watts (Peak)  Pulse Width: 120 ms (Variable)  PRP: 3 Sec. (Variable)  Beam Width: < 10 0  Transducer Eff.: 25% Acoustic Antenna

Temperature Data comparison with RS/RW

CW RASS Outdoor Field equipment

CW RASS equipment shelter

Thank You