Javascript must be enabled to continue!
Hot flow anomalies and magnetosheath high speed jets observed by Cluster and MMS during a Cluster large separation campaign 
View through CrossRef
Various mechanisms have been proposed to explain magnetosheath High Speed Jets (HSJs), such as bow shock ripples, solar wind discontinuities, foreshock transients, pressure pulses, nano dust clouds or shock reformation. It is however difficult to directly associate these mechanisms to HSJs due to the lack of simultaneous measurements at key locations, near the bow shock and both upstream and downstream of it.  We will use a special Cluster campaign, where Cluster 1 was lagged 5 hours behind Cluster 2 and 8 hours behind Cluster 3/Cluster 4 (with separation distances ranging of 3.8 RE and 5.1 RE respectively), to obtain near-Earth solar wind measurements upstream of the bow shock, together with simultaneous measurements in the magnetosheath. The event of interest is first observed by ACE on 13 January 2019, around 07:30 UT, as a short 20-minute period of large IMF-Bx (with a cone angle around 140 deg.). This large IMF-Bx period is also observed, one hour later, by THEMIS B and C (ARTEMIS) and Geotail, which were at 60 and 25 RE from Earth on the dawn side. Cluster 1 and Cluster 2 just upstream of the bow shock, at 17 RE from Earth, observed also such large IMF-Bx period together with energetic ions reflected from the bow shock and Hot Flows Anomalies (HFAs) at the beginning and end of the large IMF-Bx interval. Finally, Cluster 3 and 4 and MMS1-4, a few RE from each other downstream of the shock, observed HSJs embedded in a turbulent magnetosheath for 15 minutes around 08:30 UT. In the first part of the interval, Cluster 3/4 and MMS1-4 observed five HSJs quasi-simultaneously and in the second part, Cluster 3/4 observed three HSJs and MMS only one. The end of the first part is associated with an increase of the magnetic field at MMS in the magnetosheath and upstream in the foreshock at Cluster and Geotail. ACE observed a discontinuity where IMF-By becomes dominant for a few minutes in the middle of the large IMF-Bx interval. These observations will be discussed as possible additional HFA or short, large-amplitude magnetic structure (SLAMS). Ground-based observations from all-sky imager at Yellow River Station and the magnetometer data from SuperMAG showed diffuse auroral brightening and Pc5 ULF waves during the observations of magnetosheath HSJs.
Title: Hot flow anomalies and magnetosheath high speed jets observed by Cluster and MMS during a Cluster large separation campaign 
Description:
Various mechanisms have been proposed to explain magnetosheath High Speed Jets (HSJs), such as bow shock ripples, solar wind discontinuities, foreshock transients, pressure pulses, nano dust clouds or shock reformation.
It is however difficult to directly associate these mechanisms to HSJs due to the lack of simultaneous measurements at key locations, near the bow shock and both upstream and downstream of it.
 We will use a special Cluster campaign, where Cluster 1 was lagged 5 hours behind Cluster 2 and 8 hours behind Cluster 3/Cluster 4 (with separation distances ranging of 3.
8 RE and 5.
1 RE respectively), to obtain near-Earth solar wind measurements upstream of the bow shock, together with simultaneous measurements in the magnetosheath.
The event of interest is first observed by ACE on 13 January 2019, around 07:30 UT, as a short 20-minute period of large IMF-Bx (with a cone angle around 140 deg.
).
This large IMF-Bx period is also observed, one hour later, by THEMIS B and C (ARTEMIS) and Geotail, which were at 60 and 25 RE from Earth on the dawn side.
Cluster 1 and Cluster 2 just upstream of the bow shock, at 17 RE from Earth, observed also such large IMF-Bx period together with energetic ions reflected from the bow shock and Hot Flows Anomalies (HFAs) at the beginning and end of the large IMF-Bx interval.
Finally, Cluster 3 and 4 and MMS1-4, a few RE from each other downstream of the shock, observed HSJs embedded in a turbulent magnetosheath for 15 minutes around 08:30 UT.
In the first part of the interval, Cluster 3/4 and MMS1-4 observed five HSJs quasi-simultaneously and in the second part, Cluster 3/4 observed three HSJs and MMS only one.
The end of the first part is associated with an increase of the magnetic field at MMS in the magnetosheath and upstream in the foreshock at Cluster and Geotail.
ACE observed a discontinuity where IMF-By becomes dominant for a few minutes in the middle of the large IMF-Bx interval.
These observations will be discussed as possible additional HFA or short, large-amplitude magnetic structure (SLAMS).
Ground-based observations from all-sky imager at Yellow River Station and the magnetometer data from SuperMAG showed diffuse auroral brightening and Pc5 ULF waves during the observations of magnetosheath HSJs.
Related Results
L᾽«unilinguisme» officiel de Constantinople byzantine (VIIe-XIIe s.)
L᾽«unilinguisme» officiel de Constantinople byzantine (VIIe-XIIe s.)
<p>Νίκος Οικονομίδης</...
Ballistic landslides on comet 67P/Churyumov–Gerasimenko
Ballistic landslides on comet 67P/Churyumov–Gerasimenko
<p><strong>Introduction:</strong></p><p>The slow ejecta (i.e., with velocity lower than escape velocity) and l...
Cometary Physics Laboratory: spectrophotometric experiments
Cometary Physics Laboratory: spectrophotometric experiments
<p><strong><span dir="ltr" role="presentation">1. Introduction</span></strong&...
North Syrian Mortaria and Other Late Roman Personal and Utility Objects Bearing Inscriptions of Good Luck
North Syrian Mortaria and Other Late Roman Personal and Utility Objects Bearing Inscriptions of Good Luck
<span style="font-size: 11pt; color: black; font-family: 'Times New Roman','serif'">ΠΗΛΙΝΑ ΙΓ&Delta...
Morphometry of an hexagonal pit crater in Pavonis Mons, Mars
Morphometry of an hexagonal pit crater in Pavonis Mons, Mars
<p><strong>Introduction:</strong></p>
<p>Pit craters are peculiar depressions found in almost every terrestria...
Case Study of Geological Risk Factors for Earthquake Hazard Mapping in the South Eastern Korea
Case Study of Geological Risk Factors for Earthquake Hazard Mapping in the South Eastern Korea
  In order to interpret geological risk assessment for Earthquake hazard by mapping work, since geotechnical...
The use of ERDDAP in a self-monitoring and nowcast hazard alerting coastal flood system
The use of ERDDAP in a self-monitoring and nowcast hazard alerting coastal flood system
<div>
<p>In the UK,&#160;&#163;150bn of assets and 4 million people are at risk from coastal flooding. With reductions in public funding...
Un manoscritto equivocato del copista santo Theophilos († 1548)
Un manoscritto equivocato del copista santo Theophilos († 1548)
<p><font size="3"><span class="A1"><span style="font-family: 'Times New Roman','serif'">ΕΝΑ ΛΑΝ&...


