DATA_SET_DESCRIPTION |
Data Set Overview
=================
THIS DATA SET CONTAINS THE ION PARAMETERS IN THE PLS VOLTAGE
RANGE (10-5950 EV/Q) WITH FORMAL 1 SIGMA ERRORS OBTAINED FROM
VOYAGER 1 DATA AT SATURN BY FITTING THE MEASURED SPECTRA WITH
ISOTROPIC MAXWELLIAN DISTRIBUTIONS TO OBTAIN PLASMA DENSITIES,
TEMPERATURES, AND VELOCITY. ONLY SPECTRA WHICH HAD DISTINCT
CURRENT PEAKS WERE FIT. SPECTRA WERE FIT USING ONE OR TWO ION
SPECIES, PROTONS AND/OR A HEAVY ION WHICH WAS TAKEN TO BE
OXYGEN. OUTSIDE L~10 ION SPECTRA CHANGE RAPIDLY, SO THE VALUES
IN THIS DATA SET DO NOT REPRESENT AVERAGE PLASMA CONDITIONS IN
THE OUTER MAGNETOSPHERE. THE VALUES FOR POSITION AND MAGNETIC
FIELD GIVEN IN THE DATA SET ARE ONLY APPROXIMATE AND SHOULD NOT
BE USED FOR PUBLICATION. PARAMETERS WHICH ARE IDENTICALLY 0
AND HAVE UNCERTAINTIES OF 0 WERE NOT FIT DUE TO INSUFFICIENT
DATA; THESE NUMBERS ARE THUS NOT REAL VALUES. A COMPLETE
DESCRIPTION OF THIS DATA SET IS GIVEN IN RICHARDSON (1986).
DATA FORMAT: EACH DATA RECORD CONSISTS OF 5+2N LINES, WHERE N
IS THE NUMBER OF IONS FIT. LINE 1: S (A1, INDICATES THE START
OF A NEW FIT); TIME OF SPECTRUM; YR(I4), DY(I3),
HRMIN(I5),SEC.MSEC(F7.3); SPACECRAFT LOCATION;
RADIUS(F7.3),RHO(F7.3); MAGNETIC FIELD; BRHO,BPHI,BZ(3F7.3);
MODE; L OR M(I2); DATE FIT WAS DONE; MONTHDAYYEAR(I7); INITIALS
OF FITTER(I4); NUMBER OF ANALYSIS ROUTINE USED; (EQUALS 4 IN
THIS DATA SET, INDICATING PROGRAMS INCORPORATING THE FULL
RESPONSE FUNCTION OF THE INSTRUMENT FOR L MODES DATA):
CHI-SQUARE FROM FIT (E7.3); NUMBER OF IONS FIT (I2): LINES 2-5
TELL WHICH CHANNELS WERE FIT: CUP IDENTIFIER (A,B,C,D) (A1);
NUMBER OF SETS OF CHANNELS FIT (I3); BEGINNING AND ENDING
CHANNEL OF EACH SET (2-20I3): LINE 6; FIT PARAMETERS FOR IONS:
F (LINE IDENTIFIER) (A1); ION SPECIES NUMBER (1-8) (I1)ION
MASS, CHARGE (I3,I2); DEN,XDEN,VR,XVR,VPHI,XVPHI (6E10.3),
WHERE THE X* VARIABLES ARE FORMAL 1 SIGMA UNCERTAINTIES: LINE
7; REMAINING FIT PARAMETERS: G (LINE IDENTIFIER), ION SPECIES
NUMBER (A1, I1); VZ,XVZ,WPAR,XWPAR, WPER,XWPER (6E10.3). LINES
6 AND 7 REPEAT ONCE FOR EACH ION SPECIES. A CYLINDRICAL
COORDINATE SYSTEM CENTERED ON THE PLANET IS USED, WITH RHO
OUTWARDS FROM THE SPIN AXIS, PHI IN THE DIRECTION OF ROTATION,
AND Z THE DISTANCE ABOVE THE EQUATOR. V'S ARE VELOCITIES IN
KM/S, W'S THERMAL SPEEDS IN KM/S, AND DENSITIES IN CM-3.
VALUES OF B AND POSITION INFORMATION MAY BE UNRELIABLE AND
SHOULD BE VERIFIED BEFORE USE. ADDITIONAL INFORMATION ABOUT
THIS DATASET AND THE INSTRUMENT WHICH PRODUCED IT CAN BE FOUND
ELSEWHERE IN THIS CATALOG. AN OVERVIEW OF THE DATA IN THIS
DATA SET CAN BE FOUND IN RICHARDSON (1986) AND A COMPLETE
INSTRUMENT DESCRIPTION CAN BE FOUND IN BRIDGE (1977).
Processing Level Id : 5
Software Flag : Y
Parameters
==========
Sampling Parameter Name : TIME
Data Set Parameter Name : ION DENSITY
Sampling Parameter Resolution : 96.000000
Sampling Parameter Interval : 96.000000
Minimum Available Sampling Int : 96.000000
Data Set Parameter Unit : CM-3
Sampling Parameter Unit : SECOND
Description
-----------
A DERIVED PARAMETER EQUALING THE VECTOR MOMENTUM FRAME OR
VELOCITY FRAME TO WHICH ONE MUST TRANSFORM IN A derived
parameter equaling the number of ions per unit ION THERMAL
SPEED: A measure of the velocity associated with ORDER TO
YIELD ION ANGULAR DISTRIBUTIONS AND-OR the temperature of the
ions. It is formally defined as the volume over a specified
range of ion energy, energy/charge, ELECTRON ANGULAR
DISTRIBUTIONS THAT ARE ANGULARLY Ion Thermal Speed squared
equals two times K (Boltzmann's or energy/nucleon.
Discrimination with regard to mass and or ISOTROPIC AT ALL
ENERGIES. SUCH A FRAME CAN BE constant) times T (temperature
of ion) divided by M (ion charge state is necessary to obtain
this quantity, however, FOUND ONLY IF OTHER EFFECTS THAT CAN
YIELD ANGULAR mass). Each component of a plasma has a
thermal speed mass and charge state are often assumed due to
instrument limitations. associated with it. ANISOTROPIES
(E.G. SPATIAL GRADIENTS) ARE
FACTORED OUT. THE COMPONENT OF THE TRANSFORM VELOCITY VECTOR
PERPENDICULAR TO THE LOCAL Many different forms of ion
density are derived. Some are MAGNETIC FIELD VECTOR IS
COUPLED TO THE distinguished by their composition (N+,
proton, ion, etc.) APPROXIMATELY TIME STATIONARY ELECTRIC
FIELD. or their method of derivation (Maxwellian fit, method
of PARALLEL TO THE LOCAL MAGNETIC FIELD VECTOR A FLOW
moments). In some cases, more than one type of density will
VELOCITY FRAME MAY OR MAY NOT BE A WELL DEFINED be provided
in a single dataset. In general, if more than QUANTITY. one
ion species is analyzed, either by moment or fit, a total
density will be provided which is the sum of the ion
densities. If a plasma component does not have a Maxwellian
distribution the actual distribution can be represented as
the sum of several Maxwellians, in which case the density of
each Maxwellian is given.
Source Instrument Parameters
============================
Instrument Host ID : VG1
Data Set Parameter Name : ION DENSITY
Instrument Parameter Name : ION RATE
Important Instrument Parameters : 1
Instrument Host ID : VG1
Data Set Parameter Name : ION DENSITY
Instrument Parameter Name : ION CURRENT
Important Instrument Parameters : 1
Instrument Host ID : VG1
Data Set Parameter Name : ION THERMAL SPEED
Instrument Parameter Name : ION RATE
Important Instrument Parameters : 1
Instrument Host ID : VG1
Data Set Parameter Name : PLASMA VELOCITY
Instrument Parameter Name : ION CURRENT
Important Instrument Parameters : 1
Instrument Host ID : VG1
Data Set Parameter Name : ION THERMAL SPEED
Instrument Parameter Name : ION CURRENT
Important Instrument Parameters : 1
Instrument Host ID : VG1
Data Set Parameter Name : ION DENSITY
Instrument Parameter Name : PARTICLE MULTIPLE PARAMETERS
Important Instrument Parameters : 1
Processing
==========
Processing History
------------------
Source Data Set ID : VG1-PLS
Software : MJSANL
Product Data Set ID : VG1-S-PLS-5-ION-FIT-96.0SEC
Software 'MJSANL'
-----------------
Software Name : MJSANL
Software Type : PIN
Software Release Date : N/A
Node ID : N/A
Cognizant Engineer : N/A
Software Access Description : N/A
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ABSTRACT_TEXT |
THIS DATA SET CONTAINS THE ION PARAMETERS IN THE PLS VOLTAGE
RANGE (10-5950 EV/Q) WITH FORMAL 1 SIGMA ERRORS OBTAINED FROM
VOYAGER 1 DATA AT SATURN BY FITTING THE MEASURED SPECTRA WITH
ISOTROPIC MAXWELLIAN DISTRIBUTIONS TO OBTAIN PLASMA DENSITIES,
TEMPERATURES, AND VELOCITY. ONLY SPECTRA WHICH HAD DISTINCT
CURRENT PEAKS WERE FIT. SPECTRA WERE FIT USING ONE OR TWO ION
SPECIES, PROTONS AND/OR A HEAVY ION WHICH WAS TAKEN TO BE OXYGEN.
OUTSIDE L~10 ION SPECTRA CHANGE RAPIDLY, SO THE VALUES IN THIS
DATA SET DO NOT REPRESENT AVERAGE PLASMA CONDITIONS IN THE OUTER
MAGNETOSPHERE. THE VALUES FOR POSITION AND MAGNETIC FIELD GIVEN
IN THE DATA SET ARE ONLY APPROXIMATE AND SHOULD NOT BE USED FOR
PUBLICATION. PARAMETERS WHICH ARE IDENTICALLY 0 AND HAVE
UNCERTAINTIES OF 0 WERE NOT FIT DUE TO INSUFFICIENT DATA
DESCRIPTION OF THIS DATA SET IS GIVEN IN RICHARDSON (1986). DATA
FORMAT: EACH DATA RECORD CONSISTS OF 5+2N LINES, WHERE N IS THE
NUMBER OF IONS FIT. LINE 1: S (A1, INDICATES THE START OF A NEW
FIT) HRMIN(I5),SEC.MSEC(F7.3) RADIUS(F7.3),RHO(F7.3) MODE OF
FITTER(I4) THIS DATA SET, INDICATING PROGRAMS INCORPORATING THE
FULL RESPONSE FUNCTION OF THE INSTRUMENT FOR L MODES DATA):
CHI-SQUARE FROM FIT (E7.3) TELL WHICH CHANNELS WERE FIT: CUP
IDENTIFIER (A,B,C,D) (A1) NUMBER OF SETS OF CHANNELS FIT (I3)
CHANNEL OF EACH SET (2-20I3): LINE 6 F (LINE IDENTIFIER) (A1)
MASS, CHARGE (I3,I2) WHERE THE X* VARIABLES ARE FORMAL 1 SIGMA
UNCERTAINTIES: LINE 7 NUMBER (A1, I1) 6 AND 7 REPEAT ONCE FOR
EACH ION SPECIES. A CYLINDRICAL COORDINATE SYSTEM CENTERED ON THE
PLANET IS USED, WITH RHO OUTWARDS FROM THE SPIN AXIS, PHI IN THE
DIRECTION OF ROTATION, AND Z THE DISTANCE ABOVE THE EQUATOR.
V'S ARE VELOCITIES IN KM/S, W'S THERMAL SPEEDS IN KM/S,
AND DENSITIES IN CM-3. VALUES OF B AND POSITION INFORMATION MAY
BE UNRELIABLE AND SHOULD BE VERIFIED BEFORE USE. ADDITIONAL
INFORMATION ABOUT THIS DATASET AND THE INSTRUMENT WHICH PRODUCED
IT CAN BE FOUND ELSEWHERE IN THIS CATALOG. AN OVERVIEW OF THE
DATA IN THIS DATA SET CAN BE FOUND IN RICHARDSON (1986) AND A
COMPLETE INSTRUMENT DESCRIPTION CAN BE FOUND IN BRIDGE (1977).
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