| The CAMEX-3 DC-8 Meteorological Measurement System Table of Contents  Introduction
 The NASA DC-8 Meteorological Measurement System consists of three major systems: an air-motion sensing system to measure air velocity with respect to the aircraft, an aircraft-motion sensing system to measure the aircraft velocity with respect to the earth, and a data acquisition system to sample, process, and record the measured quantities. System Description The air-motion system consists of two airflow-angle probes, three total temperature probes each with a different response time, a pitot-static pressure probe, and a dedicated static pressure system. All probes and sensors are judiciously located at specific positions of the fuselage. The aircraft-motion sensing system consists of an embedded GPS ring laser inertial navigation system (Litton LN-100G), and a multiple-antenna GPS attitude reference system (Trimble TANS Vector). The data system rack is located near station 840, and customized software was developed to control, sample, and process all sensors and hardware. Data Reported to MMS The primary dataset collecting all parameter types (listed in the data format section below), is gathered at 5Hz. Post flight, a subset of these data are created by averaging data over one second intervals, and reporting a 1Hz dataset of a reduced number of parameters. Thus, two datasets are available for every flight and are called 1Hz and 5Hz data. Primary and secondary products used by MMS are listed below. Primary Products (1Hz & 5Hz) Typical value at 40,000 ft: 
                    Pressure =~ 200 mb +/- 0.3 mb or =~ 0.5% br>Temperature =~ 220 K +/- 0.3 K or =~ 0.2%
 Horizontal Wind =~ 30 m s-1 +/- 1 m s-1 or =~ 4.0%
 Vertical Wind < 1 ms-1 (Resolution: 0.1 m s-1)
 Secondary Products: (1Hz & 5Hz)  
                    Data FormatMeasured 
                       positions velocities
 accelerations
 pitch
 roll
 heading
 angle of attack
 angle of sideslip
 dynamic & total pressures
 total temperature
 Calculated  
                      potential temperaturetrue-air-speed
 turbulence (0.8 - 1.5 Hz)
 The file name is of the form [Mm0803-5Hz], which tells the date of the flight (yy.ddd) and the type of data (1 or 5Hz). Each of the data files contain a header which describes the data which follows, and an example of the header portion of each type of data file is shown below.  The examples below are from the files [Mm0803-5Hz] and [Mm0803-1Hz] respectively. 5Hz Data As seen in the table shown below, most of the entries in the header section of the file are self explanatory, but several are of note:  Line #1 (56 1001) indicates that there are 56 lines in the header (line 57 is the first line of data). The first reported parameter is GMT in seconds and tenths: e.g. (from the first data line in purple) GMT is 66362.1 which converts to 18:26:02 GMT.
 Line #11 & 12 (in blue) indicates the scaling factors for each of the reported parameters beginning with the second parameter. In this case, the scaling factor is 0.1.
 Lines #13 and 14 (in green) gives the number of digits reported for each parameter in each data cycle.
 Thus, when the first scaling factor from line #11 (.1) is applied to the first number (99999) in line #13, you can determine that the second data parameter is going to have five digits, and will be in tenths. Thus, 9380 reported in the first data line represents 938.0.
 Units for the data parameters (again, beginning with the second because the first is GMT seconds) are listed next, and we find that the units of the second data parameter are millibars of static pressure, in the previous example: 938.0 mb.
 A format line is provided six lines above the data lines for use with automated output.
 
                    
                      
                        | 56 1001 BUI, T. P.; S. Bowen; C. Chang; J. Dean-Day; L. Pfister; A. Trias
 NASA - Ames Research Center
 Meteorological Data from DC-8 MMS
 CAMEX-3
 1 1
 1998 08 03   1999 11 02                     ;flight-date    process-date
 0
 Elapsed UT seconds of flight date
 24
 .1 .01 .01 .01 .01 .001 .01 .001 .001 .1 .01 .01
 .01 .01 .01 .01 .001 .01 .01 .01  .0001 .001 .001 .001
 99999 99999 99999 999999 999999 999999 99999 999999 9999999 999999 99999 99999
 99999 99999 999999 999999 999999 999999 99999 99999 999999 999999 999999 999999
 Static Pressure                    (Psta)     mb       0.1        99999
 Static Temperature            *    (Tsta)      K       0.01       99999
 True Air Speed                *    (TAS)     m/s       0.01       99999
 E-W Horizontal Wind Speed     *    (U)       m/s       0.01       999999
 N-S Horizontal Wind Speed     *    (V)       m/s       0.01       999999
 Vertical Wind Speed           *@   (W)       m/s       0.001      999999
 Log10 Turbulent Dissipation   *    (TEDR)    kW/kg     0.01       99999
 Latitude +N                        (LAT)     deg       0.001      999999
 Longitude +E                       (LONG)    deg       0.001      9999999
 Hydrostatic Altitude               (HALT)      m       0.1        999999
 Potential Temperature         *    (POT)       K       0.01       99999
 Roll Angle +right wing down        (ROLL)    deg       0.01       99999
 Heading Angle                      (HDG)     deg       0.01       99999
 Pitch Angle                        (PITCH)   deg       0.01       99999
 N-S Ground Speed +N                (Ydot)    m/s       0.01       999999
 E-W Ground Speed +E                (Xdot)    m/s       0.01       999999
 Vertical Speed   +U           @    (Zdot)    m/s       0.001      999999
 Q (Compressible Dynamic Pressure)  (q)       mb        0.01       999999
 Yaw Angle (sideslip angle)         (YAW)     deg       0.01       99999
 Angle of Attack                    (AOA)     deg       0.01       99999
 Mach Number                        (MACH)              0.0001     999999
 Vertical Acceleration +U           (Zdotdot) m/ss      0.001      999999
 Yaw delta P                        (Ydp)      mb       0.001      999999
 AOA delta P                        (Adp)      mb       0.001      999999
 3
 EGI navigation data
 Hydrostatic Altitude is an estimate of geometric altitude, accurate to 50 m.
 FINAL DATA
 13
 @ Supressed when data gap is greater than 10 seconds.
 Log10 turbulence values (normally < 0) are sign-reversed when the turbulent
 sampling wavenumber is less than the buoyancy wavenumber.  Under such
 conditions, computed dissipation rates may not be quantitative.  See explanation
 in Chan et al., "Turbulence Measurements by the DC-8 Meteorological Measurement
 System", Geophys. Res. Letters, 25-9, 1355-1358, 1998.
 FORMAT(F8.1,3I6,3I7,I6,I7,I8,I7,2I6,/,1x,2I6,4I7,2I6,4I7) (87 & 81-byte per line) At the request of users in the meteorological community, more significant
 \camex.cv\d_980803.cv
   GMTS    Psta Tsta   TAS     U      V      W    TURB   LAT    LONG   HALT   POT   ROLL HDG    PIT   Ydot  Xdot    Zdot    Q     YAW   AOA   MACH  Zdotdot  Ydp    Adp
 66362.1  9380 30677  8008   -455   -492    309  -619  34906 -117882   6458 31243   -96
 23891   642  -4632  -7309    -36   3460   -14   666   2281    442  -4878  15819
 66362.3  9380 30679  8024   -459   -507    207  -653  34906 -117882   6460 31245   -87
 23899   659  -4645  -7333     54   3474   -13   670   2285    530  -4849  16109
 66362.5  9380 30683  8057   -442   -514    465  -693  34906 -117883   6461 31249   -79
 23909   676  -4657  -7352    179   3502   -13   697   2294    731  -4849  17582
 66362.7  9380 30681  8111   -409   -509    828  -668  34906 -117883   6463 31248   -68
 23917   691  -4670  -7371    336   3550   -11   726   2310    797  -4847  19201
 66362.9  9380 30680  8181   -367   -495    822  -922  34906 -117883   6465 31246   -57
 23926   703  -4681  -7396    510   3613   -10   725   2330    980  -4780  19175
 66363.1  9379 30685  8254   -317   -473    874  -783  34906 -117883   6468 31252   -44
 23933   714  -4688  -7414    708   3678    -9   725   2351    918  -4781  19186
 |  1Hz Data Line #1 (42 1001) indicates that there are 42 lines in the header (line 43 is the first line of data). The first reported parameter is GMT in seconds and tenths: e.g. (from the first data line in purple) GMT is 66364.9 which converts to 18:26:05 GMT.
 Line #11(in blue) indicates the scaling factors for each of the reported parameters beginning with the second parameter. In this case, the scaling factor is 0.1.
 Line #12 (in green) gives the number of digits reported for each parameter in each data cycle.
 Thus, when the first scaling factor from line #11 (.1) is applied to the first number (99999) in line #13, you can determine that the second data parameter is going to have five digits, and will be in tenths. Thus, 9371 reported in the first data line represents 937.1.
 Units for the data parameters (again, beginning with the second because the first is GMT seconds) are listed next, and we find that the units of the second data parameter are millibars of static pressure, in the previous example: 937.1 mb.
 
                    
                      
                        | 42 1001  BUI, T. P.; S. Bowen; C. Chang; J. Dean-Day; L. Pfister; A. Trias
 NASA - Ames Research Center
 Meteorological Data from DC-8 MMS
 CAMEX-3
 1 1                                         ;ivol nvol
 1998 08 03   1999 11 02                     ;flight-date    process-date
 0                                           ;0=non-uniform time increment
 Elapsed UT seconds of flight date
 11                                          ;number of primary variables
 0.1   0.1  0.1  0.1  0.1  0.1  0.01  1.0   0.001  0.001   1.0   ;scale factors
 99999 9999 9999 9999 9999 9999 99999 99999 999999 9999999 99999 ;missing values
 Static Pressure (mb)
 Static Temperature (K)
 Theta - potential temperature (K)
 U - horizontal E-W wind speed (m/s)
 V - horizontal N-S wind speed (m/s)
 W - vertical wind speed (m/s)
 TEDR - LOG10 of Turbulent energy dissipation rate (kW/kg) (see note below)
 Hydrostatic Altitude (m)
 Latitude +N (deg)
 Longitude +E (deg)
 Differental GPS Altitude (m)
 4
 EGI navigation data
 Hydrostatic altitude is an estimate of geometric altitude, accurate to 50 m.
 Differential GPS altitude is available only when DGPS signals were received.
 FINAL DATA
 13
 Log10 turbulence values (normally < 0) are sign-reversed when the turbulent
 sampling wavenumber is less than the buoyancy wavenumber.  Under such
 conditions, computed dissipation rates may not be quantitative.  For
 explanation, see Chan et al., "Turbulence Measurements by the DC-8
 Meteorological Measurement System", Geophys. Res. Letters, SUCCESS special
 section, 1998.
 1Hz data are desampled from 5Hz data.  5Hz data file is available upon request, containing: GMTS,Psta,Tsta,TAS,
 U,V,W,TURB,LAT,LONG,PALT,POT,ROLL,HDG,PIT,Ydot,Xdot,Zdot,Q,YAW,AOA,MACH,
 Zdotdot,YAWdp,AOAdp.                   (approx. 3 Mbyte per flight hour)
 \camex.cv\d_980803.cv
 GMTsec   Psta Tsta Thta   U    V    W   TEDR H_ALT  LAT    LONG   DGPS_ALT
 66364.9  9371 3068 3126  -16  -40    2  -737   655  34905 -117885 99999
 66365.9  9365 3067 3125  -17  -39   10  -770   660  34905 -117885 99999
 66366.9  9361 3066 3125  -14  -35    1  -807   664  34904 -117886 99999
 66367.9  9353 3066 3125  -22  -36    6  -850   672  34904 -117887 99999
 66368.9  9347 3065 3125  -14  -36    6  -799   678  34904 -117888 99999
 66369.9  9341 3065 3125  -12  -34    3  -857   684  34903 -117889 99999
 66370.9  9333 3064 3125  -12  -34    0  -762   691  34903 -117890 99999
 |  References
 Chan, K. R., S. W. Bowen, and J. D. Day, Observation of Turbulence by DC-8 MMS, presented at the AEAP Virginia Beach Meeting, VA, April 1997.  Bui, T. P., DC-8 Meteorological Measurement System, presented at the SONEX Workshop, NASA Ames Research Center, February 1997.  Contact Information To order these data or for further information, please contact:
                   
                     Global Hydrology Resource CenterUser Services
 320 Sparkman Drive
 Huntsville, AL 35805
 Phone: 256-961-7932
 E-mail: support-ghrc@earthdata.nasa.gov
 Web: http://ghrc.nsstc.nasa.gov/
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