Scintillations principle, working, merits & demerits & applications
URSIGA, New Delhi, 23-29 Oct 2005 Coordinated Observations of Ionospheric Scintillations, Density...
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Transcript of URSIGA, New Delhi, 23-29 Oct 2005 Coordinated Observations of Ionospheric Scintillations, Density...
URSIGA, New Delhi, 23-29 Oct 2005
Coordinated Observations of Ionospheric Scintillations, Density Profiles and Total Electron
Content on a Common Magnetic Flux Tube
K. M. Groves1, S. Basu1, T. R. Pedersen1 T. L. Beach1, J. M. Quinn1, B. Taliaferro1
E. R. de Paula, I. S. Batista, M. A. Abdu, R.C. Livingston, P. Ning, C. Carrano
1Space Vehicles Directorate
Space Weather Center of Excellence
Air Force Research Laboratory
2005 URSI General Assembly, New Delhi, IndiaGF1B: Atmosphere-Ionosphere Sounding by Using Global Navigation Satellite Systems
URSIGA, New Delhi, 23-29 Oct 2005
Spread F Meridional Dependence
• Motivation: Regional specification from 1-D measurements
• COPEX Campaign Overview
• Ionospheric variations at conjugate locations
• Summary
Outline
URSIGA, New Delhi, 23-29 Oct 2005
Data Assimilation Methods
• Constraining model output
• Developing statistical interpolation techniques
• Adjusting model drivers– Kalman filter– Adjoint methods
Real-time Scintillation Nowcastingfrom Space
The satellite provides only a one-dimensional sampling of the parameters.
Need to specify the ionosphere in 3-D
Communication/Navigation Outage Forecast System (C/NOFS)
URSIGA, New Delhi, 23-29 Oct 2005
Motivation: Observation Extrapolation
The Challenge: Map 1-D scintillation estimates into 2-D representations
Satellite measurement ground track
Current assumption: Symmetry about the magnetic equator—Inconsistent with asymmetric density structure near solstice
Current assumption: Symmetry about the magnetic equator—Inconsistent with asymmetric density structure near solstice
Simulated scintillation structures
URSIGA, New Delhi, 23-29 Oct 2005
COPEX CampaignOct-Nov 2002
• Magnetic equator & conjugate location observations
• Conducted by INPE with AFRL & University collaboration
• Objective is to understand initiation, growth and dynamics of young plume structures
• Critical to understanding large-scale structure of depletion development
• Multi-diagnostics at three locations will measure required ionospheric parameters
URSIGA, New Delhi, 23-29 Oct 2005
Principal Instrumentation
• Instruments operated from Oct to 07 Dec 2002• Sites on common flux tube; Campo Grande and Boa
Vista magnetically conjugate• Combination of these data with available ROCSAT
passes and other ancillary data sets provide basis to investigate meridional variations in detail
Campo Grande Cachimbo/ *Alta Floresta Boa Vista
Digisonde
VHF scint & drift
GPS TEC & scint
All-sky imager
Digisonde
VHF scint & drift
GPS TEC & scint
All-sky imager
Digisonde
VHF scint & drift*
GPS TEC & scint*
All-sky imager
VHF coherent
backscatter radar*
GEO 20.5S 54.7W 9.5S 54.8W/ 9.9S 56.1W 2.8N 60.7W
MAG 10.8S 14.0E 0.7S 15.2E 12.6N 13.5E
URSIGA, New Delhi, 23-29 Oct 2005
Mla
t
VTEC
TEC Structure Oct-Nov 2002
• TEC data reveals asymmetric anomaly structure driven by inter-hemispheric neutral wind
• Mean TEC levels decreasing ~30%+ from October to December
Local Time
VTEC
Mla
t
Local Time
VTEC
13-19 October
3-9 November1-7 December
URSIGA, New Delhi, 23-29 Oct 2005
Mla
t
S4
S4 Structure Oct-Nov 2002GPS L1 (1575 MHz) Scintillation
• Scintillation activity and intensity peak in December despite ~20% decrease in overall peak density
• Scintillation intensity symmetric as a function of magnetic latitude
Local Time
S4
Mla
t
Local Time
S4
13-19 October
3-9 November 1-7 December
URSIGA, New Delhi, 23-29 Oct 2005
• Examine daily plots between 0000-0200 UT (~2030-2230 LT)
• No observations below 30° elevation angle used in analysis
• Consider results statistically
when scintillation occurred and data was present at both “high latitude” stations
CGR AFL BVB
Analysis Approach
URSIGA, New Delhi, 23-29 Oct 2005
TEC Characterization
• Overall TEC decreases 20-50% from October to December• Largest decreases observed in southern anomaly• North/South TEC ratio increases from 1.2 in October to about 1.4
in December (40% higher!)
Avg TEC 00-02 UT North/South Ratio
URSIGA, New Delhi, 23-29 Oct 2005
Peak Density Characterization
• On average, F0F2 remains relatively constant over observing period• Largest decreases observed in southern anomaly• North/South F0F2 ratio increases from unity in October to about 1.1
in December (approximately 20% higher peak density)• Variations increase significantly during latter half of campaign
– May be related to reading ionograms with increased spread F
Avg F0F2 00-02 UT North/South F0F2 Ratio
URSIGA, New Delhi, 23-29 Oct 2005
Slab Thickness
• Effective slab thickness (TEC/NmF2) exhibits similar decrease over time
• Thicknesses generally 10-20% greater in northern hemisphere, becoming quite variable during 2nd half of campaign (Nov-Dec)
Avg Slab Thickness 00-02 UT North/South Slab Thickness Ratio
URSIGA, New Delhi, 23-29 Oct 2005
What About Scintillation?
• ~10% decrease in S4 ( N) over campaign period not entirely consistent with decrease in NmF2 (~20%)
• North/south ratio is
essentially unity (no asymmetry)
URSIGA, New Delhi, 23-29 Oct 2005
Statistical View
• Distribution of scintillation activity and intensity are statistically identical in both hemispheres despite differences in TEC and, to lesser extent, F0F2
• Activity increases in frequency during latter half of campaign
• Intensity distribution is essentially unchanged (2-3% decrease in monthly statistics)
795 Samples
Percentile S4
25: 0.333
50: 0.371
75: 0.426
90: 0.479
877 Samples
Percentile S4
25: 0.329
50: 0.363
75: 0.417
90: 0.482
895 Samples
Percentile S4
25: 0.328
50: 0.366
75: 0.416
90: 0.467
1083 Samples
Percentile S4
25: 0.324
50: 0.357
75: 0.408
90: 0.457
a) b)
c) d)
URSIGA, New Delhi, 23-29 Oct 2005
• Scintillation intensity appears relatively independent of background TEC variations near the anomaly crests
• TEC decreases markedly approaching summer solstice, particularly in the southern magnetic hemisphere; change in NmF2 less than half observed TEC decrease
• On average TEC, NmF2 and slab thickness greater in the northern magnetic hemisphere during this time period (Oct-Dec 2002)
• S4 appears to be essentially symmetric at the same magnetic latitude in both hemispheres, despite variations in TEC, slab thickness, and NmF2
• Vertical distribution of irregularities non-homogenous; propagation effects dominated by layer near F-region peak
Conclusions