|
|
|
Dynamic range |
|
Interferences |
|
Calibration |
|
Ionospheric disturbances |
|
|
|
|
|
|
|
|
Bursts expected in the range 10-2 to
104 SFU |
|
Dynamic in RF channels (before correlation) |
|
Wide bandwidth channels: interference is the
main problem, the power level may be dominated by interferences ~constant
over a wide frequency band. |
|
|
|
Narrow bandwidth channels: |
|
Assuming Tsys = noise + sky
background + |
|
|
|
For a large antenna (50 m2), dynamic
range is 300 - 106 K (40 db) |
|
For a small antenna (1m2 - dipole),
it is ~23 db |
|
|
|
|
|
|
|
|
|
|
Power variations may be > 20 db/sec. |
|
Implications: |
|
High dynamic electronics needed |
|
Automatic attenuators or very fast AGC may be be
needed in narrow band channels. |
|
Correlation is better made by 1 bit correlator
+power measurement (or many bits correlator - challenging ?) |
|
If a spectrum is computed before correlation, it
will have the dynamic of narrow channels (neglecting interferences) |
|
Note: Dynamic on images (Tb) may be
much higher |
|
|
|
|
|
Low frequencies
( < 2 GHz) are crowded: |
|
Very powerful transmitters (TV and FM) (emitters
~100 kW) |
|
Low power transmissions and GSM (emitters of 10
- 100 W) |
|
Satellites |
|
Protected (for radioastronomy) bands are very
few and difficult to keep free of interferences: |
|
151, 327, 408, 610, 1400 MHz
with bandwidth
from 3 to a few ten MHz, in principle . |
|
Satellites emissions may occur very close (149.9
MHz) to astronomy band |
|
Antennas provide usually a poor rejection ( 10
db) |
|
|
|
|
150 - 250 MHz band Nançay (interference survey
antenna) |
|
Wide band example |
|
|
|
|
150 - 152 MHz band Nançay (interference survey
antenna) |
|
Narrow band examples |
|
|
|
|
|
|
Strong interferences: may be the main challenge: |
|
|
|
Power of TV is 80 db above quiet sun emission at
200 MHz (Nançay) |
|
A stop band filter may be required for each
strong emitter |
|
The power is very high in the wide band
electronic |
|
Very high dynamic components are needed in order
to avoid intermodulation (which can generate thousands of parasitic lines) |
|
That level may be to high for digital filtering
and interference excision. |
|
|
|
Site quality is very important. |
|
|
|
|
|
|
|
|
Mean level interferences ( <40db above quiet
sun) |
|
At the lower end of the band (< 300 MHz): |
|
It is very difficult to find a 1 Mhz clean band |
|
Interferences have a small bandwidth ( 5-20 kHz) |
|
This imply: |
|
Small observing bandwidth, very good filters. |
|
Digital interference excision will require high
dynamic, high resolution spectra and filters. |
|
There are (at present) less problems above 300
MHz
|
|
|
|
Don t forget internal interferences,
mainly from high speed digital electronics. |
|
|
|
|
|
|
|
|
|
|
General |
|
|
|
Based on stability (over days and weeks) |
|
Stability is achieved by buried electronics and
transmission lines |
|
Stability allows observation of calibrators
outside sun observing time. |
|
Calibration provides complex gains for each
antenna and frequency valid for days and weeks. |
|
|
|
|
|
|
|
|
Calibrators |
|
Very few (5 ?) strong calibrators |
|
All of them have structure above 1000 l. |
|
Calibrators are not polarized |
|
No signal on X-Y correlators: corrected by
rotating some antennas by 45 degrees during calibrations. |
|
Calibrators flux decreases strongly with
increasing frequency |
|
|
|
|
|
Nançay present solution: |
|
|
|
Uses only Cygnus A radio-galaxy, which gives a
strong signal at 5000 l and 500 MHz |
|
Uses a 2 components model, and fits fringes |
|
Accuracy could be better for long baselines |
|
Starting a new procedure based on redundancies
and short baselines: antennas are calibrated step by step, and almost no
source model is needed. |
|
|
|
|
|
|
|
|
|
|
Conclusions |
|
|
|
Phase/gain stability is mandatory |
|
Self-cal on calibrators should be the best
solution |
|
The array design is important: |
|
Redundancies are useful |
|
Antennas involved only in long baselines are
difficult to calibrate. |
|
|
|
|
|
|
Ionosphere at 164 MHz |
|
Very severe case (includes some distorsion) |
|
In most cases: smaller motion and no distorsion. |
|
Likely to occur at low site angle |
|
|
|
|
|
Generalities |
|
|
|
Density inhomogeneities due to Travelling
Ionospheric Disturbances (TIDs) may affect radio observations at dam to dm
wavelength. |
|
TIDs most often due to gravity waves, sometimes
to other phenomena (including magnetosphere). |
|
Effects are proportionnal to f-2 |
|
Gravity waves are neutral atmosphere phenomenon
, which couples through collisions to electrons and ions |
|
|
|
|
|
|
|
Observations |
|
|
|
Many techniques, including radio interferometry |
|
Large database in Nançay (C. Mercier), sun and
other sources, day and night |
|
Very large database in Los Alamos, made with a 9
antennas VLBI array and satellites beacons (A. Jacobson) |
|
Some observations at VLA (cosmic radio sources) |
|
|
|
|
|
|
|
Ionospheric gravity wave schema |
|
|
|
~horizontal wave plan |
|
~horizontal energy propagation |
|
~horizontal atmosphere motions |
|
Amplitude increases with decreasing density |
|
|
|
|
|
|
Properties of gravity waves: |
|
Auroral origin: |
|
T ~1h, lhoriz
~1000 km, Vf > 400 m/sec southward, usually at night. |
|
Meteorological origin: |
|
T = 15-60 mn, lhoriz = 150-250 km, Vf
~100 m/sec, usually southward |
|
Mostly during the day, quickly damped over ~1000
km. |
|
Origin (local) is strongly site dependant |
|
TEC gradient 2. 1011 m-3
typically |
|
Electronic density changes (1-10%) occur in F2
layer( ~250 km) |
|
|
|
|
|
|
|
|
|
|
|
|
Gravity effects on observations |
|
|
|
Due to first and second derivative of TEC |
|
Very dependent on geometry: maximum when line of
sight is along wave fronts, small when perpendicular to wavefronts, or //B. |
|
|
|
Typical image motion +/- 1 arcmin at 169 MHz,
typical timescale: 30 mn. |
|
At least
10x in worst conditions (+ some image distorsion) |
|
10x less at nightime. |
|
Focusing may occur at low frequencies,
exceptionnal cases up to 50 MHz at low elevation. |
|
|
|
|
|
|
|
|
|
|
Conclusions: |
|
In order to minimize most effects, it is
important to avoid low elevation angles (high latitudes, sunrise and
sunset) |
|
Remaining effects: |
|
Distortion should be corrected by self-cal (but
who can self-cal quiet sun emission ?). |
|
Image shifts should be detected by images
correlation, or observation of stable small source (Noise Storms), and
corrected within less than 1 beamwidth. |
|
For transient bursts (ex. Type II/III/IV/V
bursts) in the absence of Noise Storms, there is no trivial position
correction. |
|