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 802.15-15-11-0765-00-0thzISSASI 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