10 research outputs found
Geosynchronous magnetopause crossings and their relationships with magnetic storms and substorms
The paper investigates the strengthening of magnetospheric activity related to geosynchronous magnetopause crossings (GMCs). We make a list of GMC events using the empirical magnetopause model (Lin et al., 2010) and hourly averaged OMNI data and find which solar wind and magnetospheric conditions accompany and follow the GMCs. The GMCs are mostly caused by the impact of interplanetary coronal mass ejections (ICMEs) and/or interplanetary shocks often with a strong increase in the density and a moderate increase in velocity. The average solar wind density during the first GMC hour is higher than 20 cmâ3 in 70 % cases, while the velocity is higher than 500 km/s in 56 % cases. The hourly interplanetary magnetic field (IMF) BZ is negative in 87 % cases. The average over all events SMU (SML), Kp, and PC indices reach maxima (minima) in 1 hour after the GMC beginning, while the delay of the minimum of the Dst index is usually 3â8 hours. These average time delays do not depend on the strength of the storms and substorms. The SML (Dst) minimum is less than -500 nT (-30 nT) in the next 24 hours in 95 % (99 %) cases, i.e. the GMC events are mostly followed by magnetic storms and substorms. We compare solar wind and magnetospheric conditions for GMCs connected with ICMEs and stream interaction regions (SIRs). Our study confirms that the ICME-related events are characterized by stronger ring current and auroral activity than the SIR-related events. The difference might be explained by the different behavior of the solar wind velocity
PC index as a proxy of the solar wind energy that entered into the magnetosphere: 2. Relation to the interplanetary electric field E KL before substorm onset
Geosynchronous Magnetopause Crossings and Their Relationships With Magnetic Storms and Substorms
Magnetic observatory data and metadata : types and availability
The availability of magnetic observatory
data has evolved rapidly with the transition of observatories
from analogue photographic magnetograms
to digital electronic recordings, and the advent of
the internet for instant global access to information
of every sort. Metadata (information about the
data) is undergoing its own transformation in order to
accompany the rapid and extensive dissemination of
these data. This chapter describes the types of data
historically and currently produced by geomagnetic
observatories and introduces new data types such as
one-second and quasi-absolute data recently discussed
at the 11th IAGA Scientific Assembly in Sopron,
Hungary.We review the availability of these data types
from the World Data Centres, INTERMAGNET and
other sources. Finally, we discuss developments in
metadata describing the current efforts in the geomagnetism
community to gather, store and distribute this
information about the data to better assist scientific
discovery