low-latitude ionospheric sensor network (lisn) c. e. valladares, boston college v. eccles, space...
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Low-latitude Ionospheric Sensor Network (LISN)
C. E. Valladares, Boston College
V. Eccles, Space Environment Corporation
E. Kudeki, University of Illinois
R. F. Woodman, Instituto Geofisico del Peru
J. W. Wright, University of Colorado
Caracas, November 18, 2005
• To build and operate the first Distributed Observatory across the western half of South America to study the low-latitude ionosphere.
• To deploy many small instruments in a region bounded to the north, west and south by the continental boundaries and to the east by the 55° W meridian.
• To transmit real-time measurements to a server that will assimilate the observable parameters and calculate geophysical quantities.
• The instruments to be deployed are: 49 GPS receivers, 5 dynasondes and 5 magnetometers.
Project Goals
• To develop tools to forecast the initiation of the equatorial spread-F (ESF) phenomenon in a regional basis.
• To study the electrodynamics of the low-latitude ionosphere during magnetic quiet and disturbed conditions.
The distributed observatory will be able to measure the conductivity along a flux tube tell us how unstable is a flux tube to the initiation of ESF.
It will measurement E region (100 km) densities at both feet of an unstable field line known to stabilize flux tube.
Scientific Tasks
Pulsed radio waves of up to ~ 20 MHz (15m wavelength) may be totally reflected in the ionosphere, giving strong echoes even with rather low transmitted power (1 kW).
Fundamental principle of the dynasonde
ESF echoes, GPS scintillations and TEC depletions
A westward tilted plume reached 1400 km before 2100 LT. This altitude maps to the F region at 9° N.
UHF Scintillations & Frequency Spread F observed on Jan 27, 2003
0200 0300 0400
Universal Time
TEC values
Real-time data flows of LISN data and assimilation results
Real-time link
Real-time link
(1) Low-latitude Ionospheric model, (2) low-latitude electrodynamics model, (3) model of ground-based magnetic perturbations for a 3-D current system (4) Kalman filter program.
Initial plan of GPS deployment
Venezuela 7 Colombia 6
Peru 5 Brazil 11
Ecuador 2 Bolivia 5
Chile 2 Paraguay 3
Argentina 7 Guyana 1
Scientific and Technological Impact
• We offer a plan to forecast Space Weather (ESF in particular).
• Provide ionospheric corrections to WAAS-type systems. There is a need for real-time specification of ionospheric density.
• Applications to Earth Sciences and Geodesy.
• GPS Meteorology.
BC can provide the following equipment
• GPS receiver and PC (laptop or Portable)
• Local server
• Solar panel, battery or a long-term UPS
• Internet connectivity (DSL)
• Cover some deployment expenses
GPS receiver TEC N
GPS receiver Amplitude and phase scint. ESF
GPS receiver TEC depletion ESF
GPS receiver TEC perturbation TID, AGW
Dynasonde Virtual height vs. frequency Dh/dN, AGW
Dynasonde Ordinary and extraordinary N, redundantly
Dynasonde Echo-locations dN/dx, dN/dy
Dynasonde Vector Velocities Ex, Uy, Ez
Dynasonde Phase structure FunctiondN/N1 km,
spectral index
Fluxgate magnetometer
3D magnetic field B
Sensor Geophysical Quantity Associated with
Observable Parameters