INVESTIGATION OF NON-STANDARD REFRACTION IN A COASTAL AREA OF NIGERIA USING RADIOSONDE DATA
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Date
2015-02-05
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Publisher
FUTA Journal of Research in Sciences
Abstract
ABSTRACT
Radio meteorological data obtained by radiosonde measurements in Lagos (3.350E, 6.060N)
were used to calculate the refractivity, N at different altitudes as well as at the ground surface,
in order to derive the refractivity gradient. The values were computed to a height of about
12km being the highest level for which complete radiosonde data were available. The
refractivity profile were plotted versus altitude for all the data analysed. The observed
refractivity distribution is more nearly an exponential function of height than a linear function
as assumed by the 4/3 earth atmosphere. It was also observed that the N-values decrease with
altitude from the earth surface. Other parameters, such as the k-factor and the values of the
gradient exceeded for given percentages of the time were also derived. The analysis of the
results have shown that most of the values of the refractivity gradient for this coastal area are
larger than the standard (normal) value of -40 N-units/km and therefore the propagation
conditions are super-refractive. The shapes of the curves have confirmed the exponential
dependence of refractivity on height, irrespective of the season.
Description
ABSTRACT
Radio meteorological data obtained by radiosonde measurements in Lagos (3.350E, 6.060N)
were used to calculate the refractivity, N at different altitudes as well as at the ground surface,
in order to derive the refractivity gradient. The values were computed to a height of about
12km being the highest level for which complete radiosonde data were available. The
refractivity profile were plotted versus altitude for all the data analysed. The observed
refractivity distribution is more nearly an exponential function of height than a linear function
as assumed by the 4/3 earth atmosphere. It was also observed that the N-values decrease with
altitude from the earth surface. Other parameters, such as the k-factor and the values of the
gradient exceeded for given percentages of the time were also derived. The analysis of the
results have shown that most of the values of the refractivity gradient for this coastal area are
larger than the standard (normal) value of -40 N-units/km and therefore the propagation
conditions are super-refractive. The shapes of the curves have confirmed the exponential
dependence of refractivity on height, irrespective of the season.
Keywords
Radiosonde data, non-standard refraction, refractivity gradient
