TY - JOUR
T1 - Plasma Depletion Bays in the Equatorial Ionosphere Observed by FORMOSAT-3/COSMIC During 2007–2014
AU - Chang, F. Y.
AU - Liu, J. Y.
AU - Fang, T. W.
AU - Rajesh, P. K.
AU - Lin, C. H.
N1 - Funding Information:
The authors gratefully acknowledge the Taiwan Analysis Center for COSMIC (TACC) and COSMIC Data Analysis and Archive Center (CDAAC) for providing FORMOSAT‐3/COSMIC data ( https://tacc.cwb.gov.tw/ , http://cdaac-www.cosmic.ucar.edu/ ). This work was financially supported by the Center for Astronautical Physics and Engineering (CAPE) from the Featured Area Research Center program within the framework of Higher Education Sprout Project by the Ministry of Education (MOE) in Taiwan. This study is supported by the Ministry of Science and Technology (MOST) Grant MOST 106‐2628‐M‐008‐002 in Taiwan and the ISSI‐Bern International Team of “Ionospheric Space Weather Studied by RO and Ground‐based GNSS TEC Observations” (the team leader Liu, J. Y. Tiger [TW]).
Publisher Copyright:
©2020. American Geophysical Union. All Rights Reserved.
PY - 2020/9/1
Y1 - 2020/9/1
N2 - A new feature of plasma depletion bay (PDB) on the longitudinal structure over the equatorial and low latitudes is observed by the FORMOSAT-3/COSMIC (F3/C) electron density profiles. The existence of the PDB feature is confirmed by the OI 135.6 nm radiance from TIMED/GUVI, which together with F3/C electron density shows that one North PDB extending to the Southern Hemisphere prominently appears over Southwest America while three South PDBs extending to the Northern Hemisphere occur over North Atlantic, India Ocean, and Southeast Asia. Three-dimensional F3/C ionospheric electron densities are further used to examine PDB structures at various local times, seasons, solar activities, and altitudes during 2007−2014. It is found that the north PDB is observed during October−March, while the south PDBs mostly exist during April−September. These PDBs can be observed within 250–350 km altitudes in the nighttime, appearing pronounced over 275–300 km altitudes around 2300–0100 LT, in the low solar activity year of 2007. Global effective wind patterns computed using the horizontal wind model HWM93 in solstice months suggest that summer-to-winter field-aligned winds projected from zonal neutral winds play an important role.
AB - A new feature of plasma depletion bay (PDB) on the longitudinal structure over the equatorial and low latitudes is observed by the FORMOSAT-3/COSMIC (F3/C) electron density profiles. The existence of the PDB feature is confirmed by the OI 135.6 nm radiance from TIMED/GUVI, which together with F3/C electron density shows that one North PDB extending to the Southern Hemisphere prominently appears over Southwest America while three South PDBs extending to the Northern Hemisphere occur over North Atlantic, India Ocean, and Southeast Asia. Three-dimensional F3/C ionospheric electron densities are further used to examine PDB structures at various local times, seasons, solar activities, and altitudes during 2007−2014. It is found that the north PDB is observed during October−March, while the south PDBs mostly exist during April−September. These PDBs can be observed within 250–350 km altitudes in the nighttime, appearing pronounced over 275–300 km altitudes around 2300–0100 LT, in the low solar activity year of 2007. Global effective wind patterns computed using the horizontal wind model HWM93 in solstice months suggest that summer-to-winter field-aligned winds projected from zonal neutral winds play an important role.
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U2 - 10.1029/2019JA027501
DO - 10.1029/2019JA027501
M3 - Article
AN - SCOPUS:85092568295
SN - 2169-9402
VL - 125
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 9
M1 - e2019JA027501
ER -