assessment of ne quick model for low latitude region · microsoft powerpoint - 08 - parikh -...
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Assessment of Ne Quick Modelfor Low Latitude Region
K S Parikh
ISRO, India
ICG-10, Boulder, Colorado, US
Nov 1-6, 2015
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Ne Quick Ionospheric Model
• The NeQuick is a Global electron density
model and is adopted by Galileo as the single
frequency ionospheric error correction algorithm
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Ne Quick Ionospheric Model
0 30 60
TEC in TECU
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Ne Quick Ionospheric Model
Basics of Ne Quick (G)
• Physico-empirical model
• Input :
3 coefficients to derive Ionization factor Az
Location (Geographic coordinates)
Time in UT
• Output :
TEC (Integrated electron density)
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Ne Quick Ionospheric Model
TEC derived using GAGAN data
for 21.03.2012
TEC derived using Ne Quick
Model
Error TEC
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Ne Quick Ionospheric Model
Constraints :
Coefficients are not currently being transmitted
by Galileo
Way out approaches :
• Use Solar Activity parameter F10.7 instead of Az
• Derive Proxy Az
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Ne Quick Ionospheric Model
Summary:
� GAGAN (SBAS) derived TEC compared with
that obtained from Ne Quick Model
� Strong correlation is observed between the
TEC obtained from two models
� Obtain coefficients in real time to run Ne
Quick model (methodology to be
established)
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Ne Quick Ionospheric ModelBasics of Ne Quick (Approach)
• MoDip is derived from
geographic coordinates
• Effective ionization AzR is
obtained from MoDip and coefficients
• Solar zenith angle derived using local time and
location coordinates
• f0E, f0F1 are derived using them and NmE and
NmF1 are obtained
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Ne Quick Ionospheric ModelBasics of Ne Quick (Approach)
• f0F2 and NmF2 : Sensitive to solar activity, have seasonal
dependence and contribute most ; hence precisely derived
• 2 sets of predetermined coefficients for spherical harmonics are
used; one for high and other for lower solar activity for each month
• These coefficients are interpolated using current AzR to obtain the
set of spherical harmonics appropriate for current solar activity
• Spherical harmonics used to derive 6 modal components of f0F2 and 4 of
M(3000)F2
• The modal components are then used to get the f0F2 and M(3000)F2
values for a given place for a given time. NmF2 is obtained from that
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Ne Quick Ionospheric ModelBasics of Ne Quick (Approach)
• f0F2 and NmF2 : Sensitive to solar activity, have seasonal
dependence and contribute most ; hence precisely derived
• 2 sets of predetermined coefficients for spherical harmonics are
used; one for high and other for lower solar activity for each month
• These coefficients are interpolated using current AzR to obtain the
set of spherical harmonics appropriate for current solar activity
• Spherical harmonics used to derive 6 modal components of f0F2 and 4 of
M(3000)F2
• The modal components are then used to get the f0F2 and M(3000)F2
values for a given place for a given time. NmF2 is obtained from that
![Page 26: Assessment of Ne Quick Model for Low Latitude Region · Microsoft PowerPoint - 08 - Parikh - Assessment of NeQuick for low latitudes.ppt [Compatibility Mode] Author: gadimova Created](https://reader035.vdocuments.us/reader035/viewer/2022071103/5fdd059ea3fb3e6b06799978/html5/thumbnails/26.jpg)
Ne Quick Ionospheric Model
Basics of Ne Quick (Approach)
• Characteristic thickness for all the three layers, viz. E, F1
and F2 are obtained separately for top and bottom side
• Effective amplitudes are obtained from Nm parameters
separately for each E, F1 and F2 layers
• Electron density profile is then determined from these
values for given heights. Top side of F2 remains
unaffected by lower layers
• Electron density integrated over the path to get TEC
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Ne Quick Ionospheric Model
• Results: The first plot