Dual-frequency transmissions from the Global Positioning System satellites
can be used to measure and map ionospheric total electron content (TEC) on
global scales, Using data exclusively from ground-based GPS networks, globa
l ionosphere mapping has been successfully applied using either two- or thr
ee-dimensional techniques. Two-dimensional TEC maps retrieve a horizontally
-varying distribution of total electron content, assuming a fixed vertical
electron density profile. In three-dimensional mapping, both the horizontal
and vertical distribution density are adjusted to fit the data. We describ
e a three-dimensional TEC mapping algorithm that uses three independent con
stant-density slabs stacked vertically to model the electron density, and c
ompare with a more conventional two-dimensional approach using a single sla
b. One apparent benefit of the new method is reduction in a level error of
the TEC maps, which decreased by 1.7 TECU using the three-dimensional retri
eval on simulated data (1 TEC Unit corresponds to 10(16) electrons/m(2)). A
nother benefit of the multilayer approach is improved slant TEC modeling, U
sing actual data from an equatorial site at Cocos Islands (96.8E, 12.2 S),
three slab modeling improved estimates of slant TEC by a factor of 2 for el
evation angles between 10 and 20 degrees (9 versus 4.4 TECU, root-mean-squa
re). However, the global structure of the vertical TEC retrievals we analyz
ed did not improve using three-dimensional modeling. This may be due to a c
ritical approximation shared by both techniques that TEC persists unchanged
at a given local time. This assumption is required to produce global maps
from observations acquired from widely scattered ground receivers, Further
improving the retrieval of global TEC structure with ground-based data prob
ably requires improved dynamical models of TEC behavior. New data available
from GPS receivers in low Earth orbit is also promising. (C) 2000 Elsevier
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