cris.boxmetadata.label.title
Three-dimensional coherent radar imaging at Jicamarca: Comparison of different inversion techniques
cris.boxmetadata.label.dateissued
22 browse.startsWith.months.march 2001
cris.boxmetadata.label.accesslevel
metadata only access
cris.boxmetadata.label.resourcetype
journal article
cris.boxmetadata.label.authors
cris.boxmetadata.label.abstract
We have implemented an eight-antenna module configuration at Jicamarca to perform a three-dimensional imaging of the atmospheric brightness distribution. As an initial test, measurements have been made in the troposphere (5-10 km) and in the equatorial electrojet (EEJ) (95-105 km). Even though the EEJ irregularities are aligned with the magnetic field, i.e., only a two-dimensional approach is needed, we decided to make these observations (1) to calibrate our eight-module configuration, and (2) to study the performance of different imaging methods. These two goals are feasible, given the fact that we have a good knowledge of the EEJ's mean position, orientation, and aspect sensitivity. Four different methods have been implemented to solve for the inverse problem, i.e., to get the atmospheric brightness from the visibility samples on the ground. We used Fourier-based, Capon, and maximum entropy (MaxEnt) methods that were originally used in radar astronomy. In addition, we implemented a fitting technique where a brightness distribution, characterized by a number of anisotropic Gaussian blobs, is assumed. From the EEJ results, (1) there is good agreement between Capon and MaxEnt methods, particularly when the signal-to-noise ratio (SNR) is high, (2) under low SNR, MaxEnt works better than the other techniques, and (3) our fitting technique using two Gaussian blobs seems to work very well, but it is very sensitive to the initial parameters needed to start the fitting procedure. Finally, the tropospheric images indicate that the troposphere over Jicamarca was too homogeneous and no significant gain in information was attained by using more than three-receiving antennas, particularly when long integration times were used (>2 min). The situation could be different in a troposphere less stable than the one at Jicamarca, where the Peruvian coast temperature inversion and stability are prevalent. In the future, efforts will be made to extend the three-dimensional approach to the tropopause and lower stratosphere, where we expect to get more interesting images. © 2001 Elsevier Science Ltd. All rights reserved.
cris.boxmetadata.label.citationstartpage
253
cris.boxmetadata.label.citationendpage
261
cris.boxmetadata.label.volume
63
cris.boxmetadata.label.issue
browse.startsWith.months.march 2
cris.boxmetadata.label.language
English
cris.boxmetadata.label.ocdeknowledgeArea
Ciencias naturales
Meteorología y ciencias atmosféricas
cris.boxmetadata.label.subjects
cris.boxmetadata.label.doi
cris.boxmetadata.label.scopusidentifier
2-s2.0-0035093676
cris.boxmetadata.label.source
Journal of Atmospheric and Solar-Terrestrial Physics
cris.boxmetadata.label.containerissn
13646826
cris.boxmetadata.label.sponsor
The Jicamarca Radio Observatory is operated by the Geophysical Institute of Perú, with support from the NSF Cooperative Agreement ATM-9408441. The authors gratefully acknowledge helpful inputs from D. T. Farley, D. L. Hysell, E. Kudeki, and R. D. Palmer. J. L. C. was supported by the National Science Foundation under agreement ATM-9813910.
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