2015
DOI: 10.1002/2015ja021885
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Occurrence climatology of F region field‐aligned irregularities in middle latitudes as observed by a 40.8 MHz coherent scatter radar in Daejeon, South Korea

Abstract: A new 40.8 MHz coherent scatter radar was built in Daejeon, South Korea (36.18°N, 127.14°E, dip latitude: 26.7°N) on 29 December 2009 and has since been monitoring the occurrence of field‐aligned irregularities (FAIs) in the northern middle latitudes. We report on the occurrence climatology of the F region FAIs as observed by the Daejeon radar between 2010 and 2014. The F region FAIs preferentially occur around 250–350 km at 18:00–21:00 local time (postsunset FAI), around 350–450 km near midnight (nighttime FA… Show more

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Cited by 10 publications
(3 citation statements)
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References 29 publications
(44 reference statements)
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“…Point 1 is similar to previous studies by Yang et al. (2015), but our results have a wider region of latitude distribution at mid‐latitudes. These seasonal characteristics are the results of many factors, such as electron density gradient, the occurrence rate of MSTIDs, and the presence of Es in the middle latitudes.…”
Section: Discussionsupporting
confidence: 92%
See 1 more Smart Citation
“…Point 1 is similar to previous studies by Yang et al. (2015), but our results have a wider region of latitude distribution at mid‐latitudes. These seasonal characteristics are the results of many factors, such as electron density gradient, the occurrence rate of MSTIDs, and the presence of Es in the middle latitudes.…”
Section: Discussionsupporting
confidence: 92%
“…The seasonal variation in the F region irregularity occurrence rate in the middle latitude obtained in this study is consistent with the results of Yang et al. (2015). They used the data from a VHF coherent radar located in Daejeon, South Korea, which is close to the Jiamusi radar.…”
Section: Characteristics Of Quiet Time Irregularitiessupporting
confidence: 93%
“…Considering the ionospheric irregularities usually occur at altitudes ~ 95-125 km (~ 250-350 km) in E (F) region (Haldoupis et al 2006;Yang et al 2015), the maximum uncertainty of the phase front structures manifested in the projections on the ground is about 20 km (45 km), under the double-thin-shell approximation with two constant heights. At a given shell ( i = E, F ), the relationship between vertical TECP ( TECP V i ) and slant TECP is…”
Section: Data and Algorithmmentioning
confidence: 99%