Annual report - 2007

Út, 2008-03-11 00:28, František Fárník
PROGRESS REPORT 1/2007 - 12/2007

Introduction

Bepi Colombo is a joint ESA and JAXA mission that consists of two spacecraft, MMO (Mercury magnetospheric orbiter) and MPO (Mercury planetary orbiter). The preparation of MPO is coordinated by ESA, whereas JAXA is responsible for MMO. The present project is related to the MEA electron analyzer that is a part of the scientific payload onboard MMO. The present PECS project was originally proposed for the 2006 - 2009 period, in accord with the schedule of the Mercury Plasma Particle Experiment (MPPE) for MMO. However, the approval process was rather long and thus the project was rescheduled for the 2007-2010 years. The project agreement was signed on April 30, 2007 but the work on the project started at the beginning of 2007.

1. Objectives planned for the reporting period

The objectives of the project can be broken into two parts. First of them deals with the preparation of the calibration system equipped with the UV source for testing of basic parts of the MEA detector system (WP1). The other part consists of several work packages (WP2-5) that are devoted to a detail investigation of plasma processes in different regions of the Sun - Earth system. The main objectives planed for 2007 were (1) to start with construction of the calibration system, (2) to develop software tools for analysis of the Cluster magnetic field and plasma data and to incorporate Cluster data into our database, and (3) to start with the investigation of all regions mentioned in WP2-5.

2. Results achieved
WP1 - calibration facility
In the technical part of the project, we have prepared two vacuum chambers. The large vessel, see Fig.1a, (~80 liters) is aimed for vacuum tests of electronic blocks, whereas the smaller one was equipped with the helium UV source (~22 eV) and electron gun (300 eV - 5 keV). The UV source with an auxiliary pumping unit is now tested. Fig. 1b shows the vacuum vessel with the two main pumping units in the bottom part, UV lamp and corresponding vacuum system on the right hand side and electron gun on the left.

Obr.č.1aObr.č.1a

Obr.č.1bObr.č.1b

WP2-5 - Scientific part.
The results of the scientific part were subject of 6 publications in scientific journals, 8 papers in conference proceedings and 29 contributions to 7 international conferences. All of them are listed in section 7, and copies of major scientific papers are attached. For this reason, we will give here only a very brief overview of the results that were subject of conference contributions and that were not published yet. However, almost all these topics will be a subject of a further investigation and publication in journals in course of oncoming years.

WP2 - Solar wind instabilities.

The major solar wind discontinuities can be classified into two classes - CME generated discontinuities with the front roughly perpendicular to the solar wind flow and CIR driven discontinuities that are generally aligned with the interplanetary magnetic field. The former propagate toward the Earth without any significant evolution, whereas the later class can undergo notable changes in the bow shock vicinity. These changes were temporarily attributed to the foreshock effects but an ultimate conclusion requires further investigations.

WP3 - Interaction of discontinuities with the bow shock.

The papers by Safrankova et al. (see section 7) have shown that the interaction of CME generated interplanetary shocks leads to the deformation of the bow shock and deceleration of the interplanetary shock. A further study has revealed that the interaction of two shocks creates a new discontinuity between them. We were able to classify it as a contact discontinuity and to determine its speed. It was shown that the interplanetary shock remains supersonic in the magnetosheath, whereas the contact discontinuity follows it with approximately magnetosonic speed.

WP4 - Magnetopause processes.

Since the magnetopause is the principal boundary dividing the solar wind and magnetosphere, we have studied it from several points of view. We have found that the magnetosheath plasma flow is significantly decelerated in the magnetopause indentation and, under some circumstances, this flow can be even reversed and can create a vortex - like structure. This fact is very important because the deceleration of the flow increases the rate of plasma penetration into the magnetosphere.

This rate is a function of the magnetic shear across the magnetopause that is determined by an orientation of the magnetic field in the magnetosheath that is often highly fluctuating. For this reason, we have carried out a study of a correlation length of the magnetosheath fluctuations that has brought a very surprising result. This length is only several thousands of kilometers, i.e. much smaller than the wavelength of the plasma waves in the investigated frequency range. Moreover, the correlation length does not depend on the orientation of the magnetosheath flow or magnetic field as can be seen from Fig. 2.

Obr.č.2aObr.č.2a

Obr.č.2bObr.č.2b

Obr.č.3Obr.č.3

 

The investigation of the magnetospheric layer adjacent to the magnetopause (LLBL) has shown that this layer is generally decoupled from the magnetosheath but that its parameters can follow abrupt changes of upstream conditions as Fig. 3 demonstrates.

WP5 - Inner magnetosphere.

We have investigated the plasma penetration into the cusp region. Based on the dispersion patterns observed in this region, it has been shown that the merging of interplanetary and magnetospheric magnetic fields can occur as far as 9 RE tailward of the cusp proper.

The other direction of investigations was the study of propagation of disturbances induced by interplanetary shocks through the inner magnetosphere. The study has provided the speed of shocks and has shown that the shock profile can differ significantly in different positions of the observing spacecraft. A better understanding requires the computer modeling that is in progress now.

 

 


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