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Options for mapping foF2

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(Pandora, Scotlands Drive, Farnham Common, Slough SL2 3ES, UK) ... Early foF2 studies for HF radio circuit planning and operation ... – PowerPoint PPT presentation

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Title: Options for mapping foF2


1
Options for mapping foF2
  • P A Bradley
  • (Pandora, Scotlands Drive, Farnham Common, Slough
    SL2 3ES, UK)

2
Early foF2 studies for HF radio circuit planning
and operation
  • Determination of MUF and field strength assuming
    great-circle propagation with mid-path or two
    control point foF2
  • Active groups UK (Marconi), USA (NBS), Germany
    (Bundespost), France (CNET), Japan (Radio
    Research Labs.)
  • Various representations of diurnal, seasonal,
    solar cycle and geographical changes
  • - UT or LT
  • - world or regional maps
  • - geographic or magnetic latitude
  • - each year separately or once-and-for-all maps
  • - solar cycle or ionospheric indices (R12, ?,
    IF2)

3
Jones-Gallet foF2 mapping procedure adopted by
the CCIR in 1969 for international radio service
planning
  • 24 separate reference world maps, one for each
    month for two high and low levels of solar
    activity (R12100 and 0)
  • based on vertical-incidence ionosonde
    measurements for all available locations for
    1954, 1955 and 1964 (solar minimum) and 1956-58
    (solar maximum)
  • mapping in UT and mixed geographic/magnetic
    latitude parameters
  • given by spherical harmonic latitude and
    longitude functions with associated numerical
    coefficients

4
The Jones-Gallet functional representation
  • foF2 (?, ?, T) SkU0,k Gk(?, ?, X) SH cos
    jTSk U2j,k.Gk(?, ?, X)
  • sin jTSk U2j-1.Gk(?, ?, X)
  • with ? geographic latitude
  • ? geographic longitude
  • T UT
  • X mixed geographic/magnetic latitude
    parameter
  • The functional form of G is determined by the
    value of k
  • H is the maximum harmonic time order 6 and the
    Us are numerical coefficients
  • k is chosen to minimise the RMS residual between
    measurements and representation leading to 488
    coefficients per map

5
WORLD MAPS OF MEDIAN foF2 (MHz) FROM CCIR
MODEL
6
Disquiet with the CCIR maps
  • based on old years of data for highest ever solar
    cycle
  • some southern hemisphere data points simulated
    from northern hemisphere with a seasonal flip
  • no measurements over the oceans

7
URSI Mapping Working Group activities (1985-89)
  • Charged to produce improved maps using
    thermospheric wind theory to simulate ocean data
    points
  • Chose to retain Jones-Gallet mapping with same
    maximum harmonic orders as CCIR for
    compatibility with existing computer codes
  • Minority view that higher-order harmonics should
    have been adopted(IPS alternative Fox/Wilkinson
    mapping)

8
Relative merits of CCIR and URSI maps
  • maps can only be tested where there are
    measurement data ie over land
  • CCIR maps test more accurate than URSI maps, but
    unproven feeling that over oceans URSI maps
    should be more accurate
  • both available as an option in IRI computer code

9
Requirements for foF2 maps for HF propagation
studies
  • Activity Service
    Circuit Circuit Frequency
    Planning Planning Diagnostics
    ManagementGlobal Average Past
    X X Maps Recent Past X X XRegion
    al Average Past X Maps Recent
    Past X Nowcast/Real Time X X

10
Requirements for foF2 maps for studies of
Earth-Space propagation effects and aeronomy
investigations
  • Activity Service and
    Circuit Circuit Aeronomy Planning
    DiagnosticsGlobal Average
    Past X XMaps Recent Past X XRegiona
    l Average Past X X XMaps Recent
    Past X X X Nowcast/Real Time X X

11
Requirements for foF2 maps
  • Conclusions
  • Different requirements dictate the need for
    different maps
  • The CCIR and URSI maps should not necessarily be
    seen as standards to compare with other maps

12
Latest ITU-R mapping proposals
  • Digitise existing CCIR maps on a 2.5o
    latitude/longitude grid so available isolated
    measurements can replace once-and-for all values

13
Options for combining isolated measured foF2
values with background predictions
  • Between equally spaced and smoothly varying
    grid-point values
  • (i) replace the nearest predicted grid-point
    value with the measured value
  • (ii) replace the nearest predicted grid-point
    value with a weighted average of the measured and
    predicted values
  • (iii) smooth between measured and predicted
    values over a linear traverse within a buffer
    zone of arbitrary size providing gradient
    continuity (the COST238 solution)

14
What should the IRI (and COST296) now be doing in
foF2 mapping?
  • Establish a Joint (?) Steering Group to
  • - review available options and make
    recommendations for reference procedures that can
    be used to generate user-specific
  • (i) global maps for future epoch radio-circuit
    planning,
  • (ii) regional maps for past epochs, also
    incorporating
  • available measured values
  • - comment on the ITU-R proposals for adoption of
    grid-point values and the separations these
    should have, and
  • - review the feasibility and possible
    geographical extent of additional foF2 values
    determined from GPS, and other navigational
    satellites, or from occultation observations, eg
    COSMIC
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