@Article{LiNOAALSW:2021:ChEqPl,
author = "Li, Guozhu and Ning, Baiqi and Otsuka, Yuichi and Abdu,
Mangalathayil Ali and Abadi, Prayitno and Liu, Zhizhao and Spogli,
Luca and Wan, Weixing",
affiliation = "{Chinese Academy of Sciences} and {Chinese Academy of Sciences}
and {Nagoya University} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Indonesian National Institute of
Aeronautics and Space (LAPAN)} and {The HongKong Polytechnic
University} and {Istituto Nazionale di Geofsicae Vulcanologia} and
{Chinese Academy of Sciences}",
title = "Challenges to Equatorial Plasma Bubble and Ionospheric
Scintillation Short-Term Forecasting and Future Aspects in East
and Southeast Asia",
journal = "Surveys in Geophysics",
year = "2021",
volume = "42",
number = "1",
pages = "201--238",
month = "Jan.",
keywords = "s Ionospheric scintillation · Equatorial plasma bubble ·
Short-term variability · The East and Southeast Asia.",
abstract = "Equatorial plasma bubbles (EPBs) can cause rapid fluctuations in
amplitude and phase of radio signals traversing the ionosphere and
in turn produce serious ionospheric scintillations and disrupt
satellite-based communication links. Whereas numerous studies on
the generation and evolution of EPBs have been performed, the
prediction of EPB and ionospheric scintillation occurrences still
remains unresolved. The generalized RayleighTaylor (RT)
instability has been widely accepted as the physical mechanism
responsible for the generation of EPBs. But how the factors, which
seed the development of RT instability and control the dynamics of
EPBs and resultant ionospheric scintillations, change on a
short-term basis are not clear. In the East and Southeast Asia,
there exist significant differences in the generation rates of
EPBs at closely located stations, for example, Kototabang (0.2°S,
100.3°E) and Sanya (18.3°N, 109.6°E), indicating that the
decorrelation distance of EPB generation is small (hundreds of
kilometers) in longitude. In contrast, after the initial
generation of EPBs at one longitude, they can drift zonally more
than 2000 km and extend from the magnetic equator to middle
latitudes of 40° or higher under some conditions. These features
make it difficult to identify the possible seeding sources for the
EPBs and to accurately predict their occurrence, especially when
the onset locations of EPBs are far outside the observation
sector. This paper presents a review on the current knowledge of
EPBs and ionospheric scintillations in the East and Southeast
Asia, including their generation mechanism and occurrence
morphology, and discusses some unresolved issues related to their
short-term forecasting, including (1) what factors control the
generation of EPBs, its day-to-day variability and storm-time
behavior, (2) what factors control the evolution and lifetime of
EPBs, and (3) how to accurately determine ionospheric
scintillation from EPB measurements. Special focus is given to the
whole process of the EPB generation, development and disruption.
The current observing capabilities, future new facilities and
campaign observations in the East and Southeast Asia in helping to
better understand the short-term variability of EPBs and
ionospheric scintillations are outlined.",
doi = "10.1007/s10712-020-09613-5",
url = "http://dx.doi.org/10.1007/s10712-020-09613-5",
issn = "0169-3298",
language = "en",
targetfile = "li_challenges.pdf",
urlaccessdate = "20 maio 2024"
}