Data Set Information
|
DATA_SET_NAME |
VL1/VL2 MARS METEOROLOGY DATA CALIBRATED DATA PRESSURE V1.0
|
DATA_SET_ID |
VL1/VL2-M-MET-3-P-V1.0
|
NSSDC_DATA_SET_ID |
75-075C-07K
75-083C-07K
|
DATA_SET_TERSE_DESCRIPTION |
VL1/VL2 MARS METEOROLOGY CALIBRATED DATA PRESSURE
|
DATA_SET_DESCRIPTION |
Data Set Overview
=================
This data set contains the martian surface atmospheric pressure
readings obtained through much of the duration of the Viking
Lander 1 and 2 missions (data are included for Viking Lander 1
sols 0 - 2245 and Viking Lander 2 sols 0 - 1050). The data are
derived from the ambient pressure sensor carried onboard the
Landers and values are presented on a point by point basis.
The sampling rate was variable throughout the mission; the
maximum sampling rate was one measurement per second, but
ranged up to 65 minutes for Lander 1 and 105 minutes for Lander
2. For further background information on the Viking
Meteorology Instrument System (VMIS) and results from this
experiment, see CHAMBERLAIN_ETAL1976, HESS_ETAL_1976A,
HESS_ETAL_1976B, and HESS_ETAL_1977. For discussions of
analyses of experiment data, see also TILLMAN_1977,
HESS_ETAL_1980, and TILLMAN_1988. An earlier version of this
data set is archived at the NSSDC (NSSDC ID 75-075C-07D and
75-083C-07D).
This data set is composed of the following fields (listed as
the field name followed by a description):
SC_ID
Spacecraft id
SOL_LON
Areocentric longitude of the Sun (Ls), derived for the
local time of each measurement
VIKING_YEAR
Viking mission year, starting at 1 when the Viking
spacecraft reached Mars, and incremented at Ls = 0
every martian year
MARTIAN_DAY
The martian solar day (sol), starting at day 0 when
each Lander touched down
LOCAL_HOUR
Local hour (Earth hour), beginning at midnight (hr 0)
LOCAL_MINUTE
Local minute (Earth minute)
LOCAL_SECOND
Local second (Earth second)
PRESSURE
Surface atmospheric pressure
Processing Level Id : 3
Software Flag : Y
Processing Start Time : UNK
Processing Stop Time : UNK
Native Start Time : 97.1 AREOCENTRIC SOL LON,
EARTH YR 1976
Native Stop Time : 226.7 AREOCENTRIC SOL LON,
EARTH YR 1982
Parameters
==========
Data Set Parameter 'ATMOSPHERIC PRESSURE'
-----------------------------------------
The force per unit area exerted by an atmosphere, measured in
millibars (10**3 dyne cm**-2).
Data Set Parameter Name : ATMOSPHERIC PRESSURE
Data Set Parameter Unit : MILLIBAR
Sampling Parameter Name : TIME
Sampling Parameter Unit : SECOND
Minimum Sampling Parameter : N/A
Maximum Sampling Parameter : N/A
Sampling Parameter Resolution : N/A
Sampling Parameter Interval : N/A
Minimum Available Sampling Int : 1.000000
Noise Level : N/A
Source Instrument Parameters
============================
Instrument Host ID : VL1
Data Set Parameter Name : ATMOSPHERIC PRESSURE
Instrument Parameter Name : PRESSURE
Important Instrument Parameters : 1
Instrument Host ID : VL2
Data Set Parameter Name : ATMOSPHERIC PRESSURE
Instrument Parameter Name : PRESSURE
Important Instrument Parameters : 1
Processing
==========
Processing History
------------------
Source Data Set ID : MASTER DATA RECORD (MDR)
Software : UNK
Product Data Set ID : VL1/VL2-M-MET-3-P-V1.0
|
DATA_SET_RELEASE_DATE |
1989-11-01T00:00:00.000Z
|
START_TIME |
1976-07-20T12:00:00.000Z
|
STOP_TIME |
1982-11-13T12:00:00.000Z
|
MISSION_NAME |
VIKING
|
MISSION_START_DATE |
1975-08-20T12:00:00.000Z
|
MISSION_STOP_DATE |
1983-02-01T12:00:00.000Z
|
TARGET_NAME |
MARS
|
TARGET_TYPE |
PLANET
|
INSTRUMENT_HOST_ID |
VL1
VL2
|
INSTRUMENT_NAME |
VIKING METEOROLOGY INSTRUMENT SYSTEM
VIKING METEOROLOGY INSTRUMENT SYSTEM
|
INSTRUMENT_ID |
MET
MET
|
INSTRUMENT_TYPE |
METEOROLOGY
METEOROLOGY
|
NODE_NAME |
Planetary Atmospheres
|
ARCHIVE_STATUS |
ARCHIVED
|
CONFIDENCE_LEVEL_NOTE |
Overview
========
The pressure transducers were calibrated to approximately 0.01
to 0.02 millibars accuracy over the ranges expected for martian
atmospheric pressure variation. Calibrations to accuracies
greater than allowed by the digitizing system were accomplished
by test support instrumentation. Repeatability from year to
year of the daily average pressures indicates that the
transducers have remained stable to significantly better than
0.04 millibars throughout the mission, possibly maintaining
stabilities on the order of 0.01 millibars. The pressure
measurements were digitized into 255 approximately equal
increments (digital numbers or DNs), giving a basic pressure
digitization interval of 0.088 millibars. Raw DNs between 0
and 255 were converted to pressures by linear interpolation
between calibration points. Due to the limited pressure range
on Mars, the only calibration points used are those for DNs
100, 120, and 160. DN 140 was left out of the calibration
table, producing a maximum error of 0.0425 millibar for VL1 and
0.008 millibar for VL2; corrections have been applied to the
data set to correct for this missing calibration point.
As the output of the pressure transducer is quantized in 0.088
millibar increments, the resolution of a single measurement is
limited to 0.088 millibar. On average, half of the
measurements producing a given pressure value are at least one
half a quantum above the indicated value and that value is
actually the lower bound of the actual value. By adding 0.044
millibar to each measurement, any estimate of the average
pressure (generally having greater resolution than one DN) will
not be biased (see HESS_ETAL_1980). Such accuracy is important
as features of the annual pressure cycle repeat within 0.02
millibar or less and it is important to establish the actual
value for comparison between years and for future missions to
Mars.
|
CITATION_DESCRIPTION |
Citation TBD
|
ABSTRACT_TEXT |
This data set contains the martian surface atmospheric pressure
readings obtained through much of the duration of the Viking
Lander 1 and 2 missions (data are included for Viking Lander 1
sols 0 - 2245 and Viking Lander 2 sols 0 - 1050). The data are
derived from the ambient pressure sensor carried onboard the
Landers and values are presented on a point by point basis. The
sampling rate was variable throughout the mission maximum
sampling rate was one measurement per second, but ranged up to 65
minutes for Lander 1 and 105 minutes for Lander 2. For further
background information on the Viking Meteorology Instrument
System (VMIS) and results from this experiment, see
CHAMBERLAIN_ETAL1976, HESS_ETAL_1976A, HESS_ETAL_1976B, and
HESS_ETAL_1977. For discussions of analyses of experiment data,
see also TILLMAN_1977, HESS_ETAL_1980, and TILLMAN_1988. An
earlier version of this data set is archived at the NSSDC (NSSDC
ID 75-075C-07D and 75-083C-07D).
|
PRODUCER_FULL_NAME |
JAMES E. TILLMAN
|
SEARCH/ACCESS DATA |
Atmospheres Online Archives
Atmospheres Online Archives
|
|