During the ECHO‐94 campaign PMSE have been observed with the ALOMAR‐SOUSY radar on 53.5 MHz at Andenes (69.28°N; 16.02°E) and with the EISCAT‐VHF radar on 224 MHz at Tromsø (69.58°N; 19.21°E). Comparisons of simultaneous measurements demonstrate generally good agreement between PMSE structures derived by both equipments. A detailed comparison shows differences caused by the mesospheric mean wind field as well as differences of the local dynamic or thermodynamic state at both measuring places.
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Bremer et al. (1996) studied this question.
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