Over 12 months of Freja electric field data have been scanned for suba
uroral electric fields (SAEF) to enable a comprehensive study of the i
onospheric signatures of such electric fields. SAEF are encountered fr
om 1800 to 0200 MLT in agreement with an earlier study. However, a lar
ge majority of the SAEF are encountered at a time slightly premidnight
(2200 - 2300 MLT), with rather few occurrences before 2000 MLT and af
ter 2400 MLT. Furthermore, the strength of the subauroral electric fie
ld is generally much larger for events close to 2200 MLT than for othe
r events. The data confirm that SAEF occur during the substorm recover
y phase but also show that SAEF occur earlier during recovery when loc
ated close to 2200 MLT than at other local times. The dependence on se
ason and geomagnetic activity is studied, and it is found that the SAE
F are more commonly observed at times of high activity when the subaur
oral electric fields are also generally stronger, except close to wint
er solstice, when strong electric fields are observed during low activ
ity. The potentials associated with the SAEF and the relation to inter
planetary magnetic field B-y are also studied. The observations are di
scussed in context with substorm-related field-aligned currents and th
e midlatitude trough, and we present evidence that support and refine
one of the proposed production mechanisms.