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doc.: IEEE 802.15-15-11-0765-00-0thz Project: IEEE P802.15 Working Group for Wireless PersonalArea Networks (WPANs) Project: IEEE P802.15 Working Group for Wireless PersonalArea Networks (WPANs) November 2011 Project: IEEE P802.15 Working Group for Wireless Personal Area Networks (WPANs) Project: IEEE P802.15 Working Group for Wireless Personal Area Networks (WPANs) Submission Title: Applications and Requirements for Environmental Remote Sensing Date Submitted: 9 November, 2011 Source: Albin J. Gasiewski University of Colorado at Boulder 0425 UCB, Boulder, CO 80309-0425, USA Voice:303-492-9688, FAX: 303-492-2758, E-Mail:[email protected] Voice:303 492 9688, FAX: 303 492 2758, E Mail:[email protected] Re: Invited on behalf of GRSS Frequency Allocations in Remote Sensing (FARS) Technical Group Abstract: Several emerging applications of THz frequencies to active and passive remote sensing of the i t i d Th i f h ifi f b d t h l i d environment are reviewed. The review focuses on he specific frequency bands, technology issues, and potential interference modalities that may be encountered in THz remote sensing., along with a discussion of interference and sharing issues. Purpose: Briefing to the 802.15 THz IG on THz remote sensing technologies for environmental applications. Notice: This document has been prepared to assist the IEEE P802.15. It is offered as a basis for di i di t bi di th t ib ti i di id l( ) i ti ( ) Th t ili thi discussion and is not binding on the contributing individual(s) or organization(s). The material in this document is subject to change in form and content after further study. The contributor(s) reserve(s) the right to add, amend or withdraw material contained herein. Release: The contributor acknowledges and accepts that this contribution becomes the property of IEEE Submission Slide 1 and may be made publicly available by P802.15. A.J. Gasiewski, University of Colorado at Boulder
Transcript

doc.: IEEE 802.15-15-11-0765-00-0thz

Project: IEEE P802.15 Working Group for Wireless Personal Area Networks (WPANs)Project: IEEE P802.15 Working Group for Wireless Personal Area Networks (WPANs)November 2011

Project: IEEE P802.15 Working Group for Wireless Personal Area Networks (WPANs)Project: IEEE P802.15 Working Group for Wireless Personal Area Networks (WPANs)

Submission Title: Applications and Requirements for Environmental Remote SensingDate Submitted: 9 November, 2011Source: Albin J. GasiewskiUniversity of Colorado at Boulder0425 UCB, Boulder, CO 80309-0425, USAVoice:303-492-9688, FAX: 303-492-2758, E-Mail:[email protected]:303 492 9688, FAX: 303 492 2758, E Mail:[email protected]: Invited on behalf of GRSS Frequency Allocations in Remote Sensing (FARS) Technical Group

Abstract: Several emerging applications of THz frequencies to active and passive remote sensing of the i t i d Th i f h ifi f b d t h l i denvironment are reviewed. The review focuses on he specific frequency bands, technology issues, and

potential interference modalities that may be encountered in THz remote sensing., along with a discussion of interference and sharing issues.

Purpose: Briefing to the 802.15 THz IG on THz remote sensing technologies for environmental applications.Notice: This document has been prepared to assist the IEEE P802.15. It is offered as a basis for di i d i t bi di th t ib ti i di id l( ) i ti ( ) Th t i l i thidiscussion and is not binding on the contributing individual(s) or organization(s). The material in this document is subject to change in form and content after further study. The contributor(s) reserve(s) the right to add, amend or withdraw material contained herein.Release: The contributor acknowledges and accepts that this contribution becomes the property of IEEE

Submission Slide 1

g p p p yand may be made publicly available by P802.15.

A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Applications and Requirements for THz Environmental Remote SensingTHz Environmental Remote Sensing

Prof Albin J GASIEWSKIProf. Albin J. GASIEWSKIUniversity of Colorado at Boulder

andandIEEE-GRSS Frequency Allocations in Remote Sensing

(FARS) Technical Group( S) ec ca G [email protected]

IEEE 802.15 THz Interest GroupAtlanta, GA, November 9, 2011

Submission

, , ,

A.J. Gasiewski, University of Colorado at BoulderSlide 2

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission <author>, <company>Slide 3

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• Active applicationspp– Standoff detection– All weather landing imagerg g– Short range security imaging– Double resonance transmission spectroscopyDouble resonance transmission spectroscopy– MMW cloud radar (90, 140, 210 GHz)

Submission Slide 4 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission Slide 5 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzClear Air THz Propagation

Submission Slide 6Klein & Gasiewski, JGR, July 2000

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Effects of Hydrometeors on Propagation

Liquid IceLiquid Ice

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 7

doc.: IEEE 802.15-15-11-0765-00-0thz

Fast B Spline Mie AbsorptionNovember 2011

Fast B-Spline Mie AbsorptionLiquid Iceq

0oC Exponential Polydispersion

Submission

p y pSandeep and Gasiewski, 2011

A.J. Gasiewski, University of Colorado at BoulderSlide 8

doc.: IEEE 802.15-15-11-0765-00-0thz

Fast B Spline Mie ScatteringNovember 2011

Fast B-Spline Mie ScatteringLiquid Iceq

0oC Exponential Polydispersion

Submission

p y pSandeep and Gasiewski, 2011

A.J. Gasiewski, University of Colorado at BoulderSlide 9

doc.: IEEE 802.15-15-11-0765-00-0thz

F t B S li Mi A tNovember 2011

Fast B-Spline Mie AsymmetryLiquid Iceq

0oC Exponential Polydispersion

Submission

0 C Exponential PolydispersionSandeep and Gasiewski, 2011

A.J. Gasiewski, University of Colorado at BoulderSlide 10

doc.: IEEE 802.15-15-11-0765-00-0thz

S iti it f B i ht T t M d l t W tNovember 2011

Sensitivity of Brightness Temperature Model to Water Vapor from 22.235 to 340 GHz

Submission

Cimini, D., E. R. Westwater, A. Gasiewski, M. Klein, V. Leuski, J. Liljegren, TGARS, 2007

A.J. Gasiewski, University of Colorado at BoulderSlide 11

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission Slide 12 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thz

V ti l S di C bilitiNovember 2011

Vertical Sounding CapabilitiesClear-airClear air incementalweighting f tifunctions

O22118.750 GHz424.763 GHz

H2O 183.310 GHz380 19 /340Klein & Gasiewski, JGR-ATM

380.197/340

Submission

JGR-ATM, July 2000

A.J. Gasiewski, University of Colorado at BoulderSlide 13

doc.: IEEE 802.15-15-11-0765-00-0thz

S b S i H i htNovember 2011

Spaceborne Sensing Heights- Clear Air -

Midlatitude (30-60o) Annual Averaged AtmosphereAnnual-Averaged AtmosphereNadir view

1 opticaldepthdepth 2 optical

depths

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 14

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission Slide 15 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzNadir IWP Brightness Signatures

Brightness temperature depressionsusing discrete dipole approximationusing discrete dipole approximationfor several ice crystal habits.

THz frequencies provide greaterTHz frequencies provide greatersensitivity to IWP and mean ice particle size.

Submission

Evans et al., JAM, 1998

doc.: IEEE 802.15-15-11-0765-00-0thzCloud Ice Sensing using MMW/SMMW Bands

SubmissionF. Evans, et al., 1998

doc.: IEEE 802.15-15-11-0765-00-0thz<month year>

Submission <author>, <company>Slide 18

doc.: IEEE 802.15-15-11-0765-00-0thzISSASI and CIWSIR THz Passive Bands107.5-119 163-184 311-339 408-428 670

ISSASI = International Space Station Atmospheric Sounding of Ice (red)CIWSIR = Cloud Ice Water Submillimeter Imaging Radiometer (gray)

SubmissionBuehler et al., QJRMS, 2007

Calculations for clear air and 8-10 km ice cloud with 80 g/m2 IWP, Dme=100 μm

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission Slide 20 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Ground based Scanning Radiometer (GSR)Ground-based Scanning Radiometer (GSR)

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 21

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

G d B d S i R di t Ch lGround Based Scanning Radiometer Channels

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 22Cimini, D., et al., , TGARS, 2007

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Retrieved Water Vapor Profiles d Li id W t P th S iti itand Liquid Water Path Sensitivity

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 23Cimini, D., et al., , TGARS, 2007, 2010

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission Slide 24 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thz

Fill d A t G t tiNovember 2011

Filled Aperture Geostationary Spatial Resolutionp

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 25

doc.: IEEE 802.15-15-11-0765-00-0thzGEosynchronous Microwave (GEM) Sensor

Nodding / MorphingS b fl t

3” Thick Composite Reflector

• Baseline system using 54, 118, 183, 380, and 424 GHz with ~2

di C i Subreflector

Space Calibration Tube

m diameter Cassegrain antenna. • ~16 km subsatellite resolution

(~12 km using oversampling)54GHz Feeds

&Receivers

( 12 km using oversampling) above 2-5 km altitude at highest frequency channels.Th 380 d 424 GH h l

Elevation Motor& Compensator

• The 380 and 424 GHz channels selected to map precipitation through most optically opaque l d t b h l i t l Azimuth Motor

& CompensatorBackupStructure

Estimated Mass ~65 kg

clouds at sub-hourly intervals. (Gasiewski, TGARS, 1992)

• Temperature and humidity

Geosynchronous Microwave Sounder Working Group (GMSWG):

Estimated Mass ~65 kgp ysounding channels penetrate clouds sufficiently to drive NWP models with ~hourly

Submission

Working Group (GMSWG):Chair: D.H. Staelin (MIT)

ydata.

doc.: IEEE 802.15-15-11-0765-00-0thz

Si l t d GEMNovember 2011

T

Simulated GEM 424+/-4 GHz Imagery - 15 min time steps TB

S

15 min time steps

TBBA

TB

TT

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 27

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• THz absorption and scattering spectrum• Passive applications• Passive applications

– Temperature and water vapor profilingWeighting functions• Weighting functions

– Cloud liquid and ice sensing• COSSIR ISSASI SIRICE ISS Ice• COSSIR, ISSASI, SIRICE, ISS Ice

– Ground-based T/Q profiling and LWP measurementmeasurement

– Geostationary microwave imaging/sounding– Interference mitigationInterference mitigation

• Density of Interferers equation

Submission Slide 28 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 29

doc.: IEEE 802.15-15-11-0765-00-0thz

Density of InterferersNovember 2011

AMSR-E C-band Example: PT= 1 mW (0 dBm)

Density of InterferersFrom Friis formula and kTB thermal noise: PT 1 mW (0 dBm)

T = 0.3 K (SA.1029-2 recommendation)B = 350 MHz = 4 3 cm (6 9 GHz)

and kTB thermal noise:

< = 4.3 cm (6.9 GHz)C = 1 (direct isotropic radiation)τ = 0.02 (<0.1 dB atmospheric loss) θ 55 i id WRT di

<

θs = 55o incidence WRT nadir

< 2.3E-3 (km-2)Or, an average transmitter separation distance of more than ~21 km isrequired for non-interference (using

θs

q ( gthe ITU 20% criteria).

6.9 GHz was orignally intended as the primaryAMSR E h l f il i t t

Submission

AMSR-E channel for soil moisture measurement

A.J. Gasiewski, University of Colorado at BoulderSlide 30NRC Report on “Spectrum Management for Science in the 21st Century” http://www.nap.edu/catalog/12800.html

doc.: IEEE 802.15-15-11-0765-00-0thzIdentification of Interfering Sources

SubmissionFebruary 13, 2008

ASEN Remote Sensing Seminar

doc.: IEEE 802.15-15-11-0765-00-0thzIdentification of Interfering Sources

SubmissionFebruary 13, 2008

ASEN Remote Sensing Seminar

doc.: IEEE 802.15-15-11-0765-00-0thzIdentification of Interfering Sources

SubmissionFebruary 13, 2008

ASEN Remote Sensing Seminar

doc.: IEEE 802.15-15-11-0765-00-0thzIdentification of Interfering Sources

SubmissionFebruary 13, 2008

ASEN Remote Sensing Seminar

doc.: IEEE 802.15-15-11-0765-00-0thzPSR/C SGP99 7/14/99 – Oklahoma – SN 0049

Calibrated (uncorrected) Imagery

Interference above geophysical and instrument noise from ground-based active services

SubmissionFebruary 13, 2008

ASEN Remote Sensing Seminar

doc.: IEEE 802.15-15-11-0765-00-0thz

Basic Spectral RFI Mitigation AlgorithmNovember 2011

Basic Spectral RFI Mitigation Algorithm4-point

linear fitSeverity 0:

No TB

Severity 2:Two Point

X2,TB,Slope

linear fit (1x)

Min X2

CorrectionTB

OK

wo oCorrection

S i 3

OK

Slope3-point

linear fits (4x)

Severity 1:Single PntCorrection

Severity 3:Unaccept’lTwo Point Correction

Min X2,TB,Slope,Low TB

(4x) CorrectionOK

Severity 4:ReplicateBest TLow TB

TB

2-pointaverages

(6x)

Best TBIn Range

>1

>1OK

TB,Slope

Low TB

Severity 5:Uncorrect-

able

OK

Submission Slide 36 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzPSR/C SGP99 7/14/99 – Oklahoma – SN 0049

Interference-Corrected Imagery

Interference mostly removed for purposes of soil moisture measurement

SubmissionFebruary 13, 2008

ASEN Remote Sensing Seminar

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

RFI t P i S t t TH B dRFI to Passive Systems at THz Bands• There is little concern about RFI above 275 GHz at

present since all activity is nascent• As sources become cheaper and receivers are ablet b i t t d b th i d ti li tito be integrated both passive and active applicationswill expandRFI mitigation efforts and actions at lowerRFI mitigation efforts and actions at lower

frequency bands will be representative• Water vapor screening (producing exponentialWater vapor screening (producing exponentialdecay) can be likely be used to facilitate bandsharing:s g: Requires knowledge of humidity fieldsMay require on-board ROM radiative transfer

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 38

y qcalculations (WRF+MPM on a PDA)

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

• Active applicationspp– Standoff detection– All weather landing imagerAll weather landing imager– Short range security imaging– Double resonance transmission spectroscopyDouble resonance transmission spectroscopy– MMW cloud radar (90, 140, 210 GHz)

Submission Slide 39 A.J. Gasiewski, University of Colorado at Boulder

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

187 GH R d I i f S it I i187 GHz Radar Imaging for Security Imaging

“Design and testing of an activeDesign and testing of an active 190-GHz millimeter-wave imager”

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 40Timms et al., J. Electronic Imaging, 2010

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

675 GHz Radar Imaging for Standoff Detection675 GHz Radar Imaging for Standoff Detection

Siegel group/JPL:

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 41

Cooper et al., Trans. MTT, 2008

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Airborne Imaging Applications

• Passive MMW Imaging for landing during fog Technology for MMIC receiver arrays Technology for MMIC receiver arrays

demonstrated in late 1990’s at 94 GHzMMIC LNA receiver chips being developedMMIC LNA receiver chips being developed

up to ~700 GHz• Radar for landing during brownout being demonstratedRadar for landing during brownout being demonstrated

at frequencies up to 340 GHz

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 42

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Double Resonance Spectroscopy• Proposed active IR/THz technique for remote detection• Proposed active IR/THz technique for remote detectionof trace species.

Submission A.J. Gasiewski, University of Colorado at BoulderSlide 43DeLucia at al., IEEE J. Quantum Electronics, 2009

doc.: IEEE 802.15-15-11-0765-00-0thzNovember 2011

Summary• There is a rapidly growing number of

applications of THz technology for pp gyenvironmental (and related) applications– Both passive and activeBoth passive and active– Highly dependent on power/cost and propagation

requirementsq• Current spectral needs are modest, but could

be expected to become significantbe expected to become significant – Water vapor screening could potentially be

standardized and used to facilitate sharing

Submission Slide 44

g

A.J. Gasiewski, University of Colorado at Boulder


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