Methods of detection and estimation errors in ST radar studies

Details Methods of detection and estimation errors in ST radar studies Methods of detection and estimation errors in ST radar studies

Jun 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994angeo..12..489f&link_type=abstract

Annales Geophysicae, vol. 12, Issue 6, pp.489-496

Mathematics

Probability

7

Scientific paper

The classical theory of detection using the Neyman-Pearson principle is applied to stratosphere-troposphere (ST) radar signals. It is extended to provide information regarding the detection of weak signals which complements the detectability method usually employed in ST radar studies. It is shown that for ST radar signals of low amplitude and a detectability around 3 (a value commonly invoked in literature), the probability of detection is about equal to the probability of false alarm. The question of threshold detectability is also discussed.

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