URSI GA 2008

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The New Digisonde: DPS-4D B Reinisch , I Galkin, G Khmyrov, K Bibl, I Lisysyan, A Kozlov, G Cheney, Y Luo, D Kitrosser, R Hamel, V Paznukhov, J Grochmal University of Massachusetts Lowell Environmental, Earth, & Atmospheric Sciences Department Center for Atmospheric Research The New Digisonde: DPS-4D B Reinisch , I Galkin, G Khmyrov, K Bibl, I Lisysyan, A Kozlov, G Cheney, Y Luo, D Kitrosser, R Hamel, V Paznukhov, J Grochmal University of Massachusetts Lowell Environmental, Earth, & Atmospheric Sciences Department Center for Atmospheric Research URSI GA 2008 Chicago 14 August 2008

Transcript of URSI GA 2008

The New Digisonde:

DPS-4DB Reinisch, I Galkin, G Khmyrov, K Bibl, I Lisysyan, A Kozlov, G Cheney, Y Luo,

D Kitrosser, R Hamel, V Paznukhov, J Grochmal

University of Massachusetts LowellEnvironmental, Earth, & Atmospheric Sciences Department

Center for Atmospheric Research

The New Digisonde:

DPS-4DB Reinisch, I Galkin, G Khmyrov, K Bibl, I Lisysyan, A Kozlov, G Cheney, Y Luo,

D Kitrosser, R Hamel, V Paznukhov, J Grochmal

University of Massachusetts LowellEnvironmental, Earth, & Atmospheric Sciences Department

Center for Atmospheric Research

URSI GA 2008Chicago 14 August 2008

umlcar.uml.eduURSI GA Chicago August 2008

High quality ionogramsReal time autoscaling and EDPsStandardized format of user data (SAOXML)Real time data disseminationRemote controlFlexibility for research and campaignsAnalysis software toolsLow transmit power for reduced RFIEase of maintenance

Important Issues for Ionosondes

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New Face of the DPS

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History of the Digisonde Development

Starting in 1969Digisondes 128, 128P, 128PSDigisondes 256, including DISSDPSDPS-4D

Today: Majority of Digisondes report in real time data and EDPs to Data Centers like

Digital Ionogram Data Base “DIDBase” at UML World Data Center, Boulder → NOAA SPIDRWorld Data Center, London US AFWA → GAIMDIAS / COSTCOST 251 Vertical Incidence Sounding Database

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Digisonde Network

4DHermanus

4D

4D

4D 4D

4D installations in 2008:

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Hermanus, South Africa, 9 Aug 2008

Daytime

Courtesy L-A McKinnell

http://ulcar.uml.edu/DIDBase/

Courtesy L-A McKinnell

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Summary of DPS Key Features

2x150 W low-power solid-state transmitters with half octave filters reduce RFICircular polarized transmission/reception identify O and X echoesFour-element receiving antenna array identifies angles of arrivalMultiple levels of DSP:

Spread spectrum transmissionPhase-coded waveform for pulse compressionDoppler spectrum analysis (2, 4, …, 128 pulse sequence)Precise radar range measurements with bi-frequency transmission

Remote commanding & real time data disseminationRemote diagnostic with Built-In-Test (BIT)ARTIST autoscaling and EDPs

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DPS-4D Innovations (1)Digital transceiver technology

Superior accuracy, precision, and resolution of amplitude and phase measurements

• 16 bit ADCs and receivers• Improved angle of arrival processing• High resolution h’(f) in routine operation

High speed interfaces between embedded processorsTime domain raw-data output for user processingNew RFI Mitigation technique improves SNR by up to 40 dBPassive mode for monitoring transmitters-of-opportunityFaster measurements (2-second ionograms)

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Millstone Hill: 2-second ionograms,10 sec cadence

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DPS-4D Innovations (2)New embedded software

Real-time operating system RTEMS • Superior clarity, reliability, scalability, quality control, and technical

support of the codeJava environment for online data processing

• Superior development tools and graphics libraries• Reusable code from and for other projects

– SAO and Drift Explorers,– ARTIST- 5 with profile error bars, – DIDBase and Drift-Base

• Superior visualization, control, and debugging environment for DPS operations

– Data capture, replay for processing, interim data– Stepping through processing stages– Operational logs for troubleshooting

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Profile Error Bounds

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New Hardware

Transmitter/Timing 8-Channel Receiver Preprocessor

Four tracking bandpass filters CNTL and DATA computers

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New Hardware

Transmitter/Timing 8-Channel Receiver Pre-processor

Four tracking bandpass filters CNTL and DATA computers

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18:00 LT

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One day atMillstone Hill15 April 2008

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fN(h,t)fN(h,t)

The profiles for the same day

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RF Interference Mitigation Algorithm RFIM(patented)

1. For strongest interferer: determine precisefrequency, amplitude, and phase

2. Subtract the interferer signal from input data3. Proceed with second strongest interferer4. Etc. …

~40 dB signal-to-noise enhancement

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With R

FIMThe power of RFIM

No R

FIM

TIME-DOMAIN Data

Es

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Precision Ranging using Phase-difference Technique

Conventional Display

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Precision Ranging using Phase-difference Technique – more accurate h’(f) traces!

( )( ) ( )( ) ( ) ( ) ( )

( )( ) ( )

( )( ) ( )

0

0

0

00

0

0

2 2 , ,

(Leibniz Theorem)

2 since , 0, and 0.

But ' . Therefore:

R

R

R

R

h

hh RrecRh

hrecRh

h

rec

d kdh n dh hd dhdh n h n hd d c d d

nd dhdh n hd c d

ndh h

dd

ω

ω

ω

ω

ωφ ω ω ω ωω ω ω ω ω

ωφ ωω ω ω

ωω

ωφ

⎡ ⎤∂ ⎛ ⎞ ⎛ ⎞= = + −⎢ ⎥⎜ ⎟ ⎜ ⎟∂ ⎝ ⎠⎢ ⎥⎝ ⎠⎣ ⎦

∂⎡ ⎤ ⎛ ⎞= = =⎢ ⎥ ⎜ ⎟∂ ⎝ ⎠⎣ ⎦∂

=∂

∫∫

( )

( ) ( ) ( )2 2

1 1

' '1 2

'

2 ' , or

2 2' , where ' '

4

rec i i

i rec

hc

d d h d h h h hd c c

chf

ω ω

ω ω ω

ω

ωω

φφ ω ω ω ω ω ωω

φπ

=

Δ = = = Δ < <

∴ = ΔΔ

∫ ∫

Reinisch et al., 2008 in “Radio Sounding and Plasma Physics”AIP Conf. Proc. 974

279 km Δφ4πch'

fΔ=

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The effect of Precision Ranging (PR)

Classic Ionogram Display Ionogram Display with PR

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Doppler-Interferometry: Skymaps & Drift

Kozlov and Paznukhov 2008, in “Radio Sounding and Plasma Physics”, AIP Conf. Proc. 974

Data courtesy O. Veliz

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One day atJicamarca

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VZ (t), VN(t), VE(t) for same day

SS SR

VZ

VN

VE

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Time log of spread F occurence

West / km East / km

UT

/ h

Blue = eastward driftRead = westward drift

Off-vertical Echoes(compressed ionograms)

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DPS-4D at Millstone Hill Receiving EISCAT Heater Signal

+/- 100 HzFourier Spectrum

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SummaryReal time assessment of ionosphere now possible with modern networked ionosondesReal time data dissemination and assimilation: GAIM ….Automatic error assessment of EDPs

Fleet of topside vertical ionospheric sounders for accurate globalassessment of the ionosphere

What is still missing??