atmospheric scintillation
DESCRIPTION
Research on atmospheric scintillation.TRANSCRIPT
Scintillation Occurrences and Analysis
What is Scintillation?
From past several centuries’ educators who are actively
interested and keen to known the truth and hidden knowledge
of nature and sky upon us have observed sparkling light like
crystals spreaded across the sky in the backdrop. Twinkling
effect gives beautiful effect on the vast open skies. The
astronomers were very much inspired from this strange
phenomenon.
This phenomena is termed as Scintillation, the technical term
for the twinkling of stars, is defined as the rapid and irregular
variation of intensity of celestial objects. [5]
Scintillation is although appears beautiful of the sky lines but it
has negative impact on astronomy. Relatively small fractions of
S to the order of 0.04 to the incident energy E is converted into
N fluorescence photons of mean energy Ep, which provide the
scintillation.
The fluctuation in amplitude and phase caused are termed and
classified as scintil lation. Thereby it is stated that Scintil lation refers
to the rapid fluctuation in signal amplitude and phase often observed
on satellite links. These fluctuations are caused by random spatial
and temporal changes of the atmosphere’s radio refractive index
within the link’s first Fresnel ellipsoid. Scintil lation statistics are
necessary for experiment planning and in design of signal processing
procedures. [1]
Phase scintil lation paused by propagation through solar wind,
ionosphere and troposphere irregularities is a noise process for
many spacecraft radio science experiments. In precision Doppler
tracking observation, scintil lation can be the domain noise process.
[2]
A well known stellar scintil lation phenomena that arises when
observing the stars through the earth atmosphere. The data
reliability is also required before analysis of the current that is
effect of the element of effectiveness. The scintil lation emission is
same as fluorescence spectrum when modelled and its categorized
into different types depending upon the sky region is it effecting
such as equatorial scintil lation, high latitude scintil lation etc.
Scintillation Properties
• The absolute scintil lation efficiency index S4 fallen data comm;
• The scintil lation emission is spectrum;
• The scintil lation has decay time Ƭ.
• Slow is scintil lation component on the dependence of the pulse
shape on the nature of the incident radiation.
Scintillation Models
There are number of scintil lation models for analyzing the effective
generated fluctuation caused.
• Global Ionospheric Scintil lation Model (GISM)
• WBMOD Ionospheric Scintil lation Model
• DPSP, MSP
• STH2, STN2 Model induced in sept
• STHV2, STHV2
Past Work
• GPS phase scintil lation observed over a high-latitude Antarctic
station during solar minimum, Chigomezyo M.Ngwira a,b, Lee-
AnneMcKinnell a,b, PierreJ.Cill iers, 2010, Journal of
Atmospheric and Solar-Terrestrial Physics , 72 (2010) 718–725
• Forecasting Ionospheric Real-time Scintil lation Tool (FIRST)
Anderson, D. N.; Redmon, R.; Bullett, T.; Caton, R. G.;
Retterer, J. M.
American Geophysical Union, Spring Meeting 2009, abstract
#SA11B-05
• Co-ordinated studies using imaging riometer and incoherent
scatter radar, Journal of Atmospheric and Solar-Terrestrail, P.
N. Collis* and J. K. Hargreaves, 1996, Physical Vol. 59. No. 8.
pp. 873 890. 1997
• Scintil lation and cycle slips observed at high latitudes during
solar minimum, P. Prikryl1, P. T. Jayachandran2, S. C. Mushini2,
D. Pokhotelov2, J.W. MacDougall3, E. Donovan4, E. Spanswick4,
and J.-P. St.-Maurice5, June 2010, GPS TEC, Ann. Geophys., 28,
1307–1316, 2010
• Climatology of GNSS ionospheric scintil lation at high latitudes,
L. Spogli, L. Alfonsi, G. De Franceschi, V. Romano, M. H. O.
Aquino, A. Dodson, 2008 American Geophysical Union, Fall
Meeting 2009, abstract #SM33A-1562
• ISACCO: an Italian project to monitor the high latitudes
ionosphere by means of GPS receivers, Giorgiana De Franceschi
Æ Lucilla Alfonsi Æ Vincenzo Romano, 2006, GPS Solut (2006)
10:263–267; DOI 10.1007/s10291-006-0036-6
Resources Available
Electromagnetism vs Non Electromagnetism
• The Rytov and Born Approximation
She showed that variances of logarithm amplitude variations should
be less than unity in all situations. The electromagnetism theory:
Born condition : (∞)^2 + (x)^2 < 1
Phase and amplitude should be less than 1 where ∞ denotes phase
and x amplitude.
• Longitudinal waves
Including sound waves as example (alternation in pressure, particle
displacement, or particle velocity propagated in an elastic material).
In this form the amplitude of the wave is pressure of the
undistributed wave and maximum pressure.
Prediction and Software
Name Input Outputs
Cornell Scintil lation Model Coordinates Simulation
SCINDA (Scintil lation Network
Decision)
Requires
GPS
coordinate
values
Stream of GPS
scintil lation
data from the
server.
NWR Ionospheric Scintil lation
Predictions
- Stores all the
recorded data
from Nasa.
Model-Based Prediction of Amplitude
Scintil lation Variance
Radio
Sounding
Data
Graphs
Haystack InterPlanetary Scintil lation
Software
Frequency
band
Scans the
beam, record
data
SimGEN Coordinates Simulation
Scintil lation Prediction Using
Improved Pre-Processed
Radiosounding Data
Pre-
processed
radiosonde
data
Structure
constant C2n of
the
troposphere
A Forecasting Ionospheric Real-time
Scintil lation Tool (FIRST)
Coordinates Graphs
References
1) GURVICH Alexandre ; CHUNCHUZOV Igor ; “ Estimates of
characteristics scales in the spectrum of internal waves in the
stratosphere obtained from the space observations of stellar
scintil lation” : Journal of Geophysics research ISSN 0148-0227
2005, vol. 110
2) E.N Bramley; “The accuracy of computing ionosphere radio-
wave scintil lation by the thin-phase-screen approximation”:
Journal of Atmospheric and Terrestrial Physics Volume 39, Issue
3, March 1977
3) Armstrong, J. W. (1998), “Radio wave phase scintil lation and
precision Doppler tracking of spacecraft” , Radio Sci. , 33(6),
1727–1738, doi:10.1029/98RS02317.
4) Canadian High Artic Ionospheric Network
http://chain.physics.unb.ca ; Date Accessed 22 Dec 2010
5) Jayachandran, P. T., et al. (2009), Canadian High Arctic Ionospheric
Network (CHAIN), Radio Sci., 44, RS0A03, doi:10.1029/2008RS004046
6) Imaging Riometer for Ionospheric Studies
http://www.dcs.lancs.ac.uk/iono/iris/ Date Accessed: 20-Dec-
2010
7) M. Colleen Gino “
http://www.astrophys-assist.com/educate/starry/starrynight.ht
m ”
Date Accessed : 05/01/2011