@Article{RawatEcheGonz:2018:HoDiAr,
author = "Rawat, Rashmi and Echer, Ezequiel and Gonzalez Alarcon, Walter
Dem{\'e}trio",
affiliation = "{National Centre for Antarctic and Ocean Research} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "How Different Are the Solar Wind-Interplanetary Conditions and the
Consequent Geomagnetic Activity During the Ascending and Early
Descending Phases of the Solar Cycles 23 and 24?",
journal = "Journal of Geophysical Research: Space Physics",
year = "2018",
volume = "123",
number = "8",
pages = "6621--6638",
month = "Aug.",
abstract = "The current work investigates the possible solar
wind-interplanetary (SW-IP) drivers of geomagnetic storms during
the longest period (ascending to early descending phases) of the
ongoing solar cycle (24). We present a comparative analysis
between the two consecutive solar cycles (SCs) 23 and 24. Both the
cycles exhibited dual peak feature as observed in the smoothed
sunspot numbers SSNsmoothed. For both the cycles, second peak in
the SSNsmoothed is higher than the first one as exhibited in the
revised SSNsmoothed version. During the entire interval between
the ascending to early descending phases (December 2008 to
December 2016) of SC-24, the southward directed Bz and the
dawn-dusk electric field (Ey) were consistently weaker as compared
to that during similar interval of SC-23 (May 1996 to July 2004).
The geomagnetic field response represented by Dst index
concurrently exhibited similar variation patterns during both the
periods. A striking reduction in the intense storm occurrence rate
by \∼75% was observed during the considered period of the
current solar cycle in comparison to the previous cycle. However,
moderate storm occurrence was reduced only by 32% in SC-24 as
compared to SC-23, which could be attributed to the dominance of
corotating interaction regions during SC-24. No significant
difference is found between the intense storm rates around the
vernal and autumnal equinoxes in cycle 24, whereas distinct
autumnal equinoctial dominance is evident for cycle 23. Further,
within each cycle, there is no significant difference in the
moderate storm rates around vernal and autumnal equinoxes.",
doi = "10.1029/2018JA025683",
url = "http://dx.doi.org/10.1029/2018JA025683",
issn = "2169-9402",
language = "en",
targetfile = "rawat_how.pdf",
urlaccessdate = "27 abr. 2024"
}