ACE1 Model BoM GASP/HYSPLIT trajectory data from the Smart Balloon flights have been put together into a single composite file. The 24 separate files are demarked in the composite file by a Start and End message next to the original file name. ------------------------------------------------------------------------------- These trajectories are designed to aid in the analysis of the balloon observations and the Lagrangian experiments. For Lagrangian A balloon 10 is examined. For Lagrangian B balloons 00, 06 and 08 are examined. The trajectories are begun on locations based upon the data of Steve Businger. For each balloon there are six files. f97_B??_b5_data.dat - backwards 5-day trajectory using vertical winds f97_B??_f2_data.dat - forwards 2-day trajectory using vertical winds f97_B??_f2_isob.dat - forwards 2-day trajectory assuming an isobaric trajectory f97_B??_f2_topl.dat - forwards 2-day trajectory using vertical winds. This trajectory is an approximate UPPER limit starting at 1000m altitude. f97_B??_f2_botl.dat - forwards 2-day trajectory using vertical winds. This trajectory is an approximate LOWER limit starting at 100m altitude. f97_B??_f2_COMP.dat - forwards 2-day COMPOSITE isobaric trajectory. The pressure was readjusted hourly to match the balloon observations. For each series of trajectories we provide an ASCII file which contains the time, lat, lon, pressure, U, V, vertical velocity in pressure, temperature, relative humidity and surface pressure. These fields come from the GASP data set. Trajectories will fail if the track hits the surface, rises above approx 500 HPa or flows off the restricted domain of the GASP data. Also, the lowest interpolated GASP data is to the 0.991 omega level. This corresponds to roughly 110 meters height. Trajectories below this level are not accurate. Most likely they will be moving too quickly as they do not reflect the physics of the surface drag on the air flow. They still provide a good estimate of the air motion for the first 12-24 hours. These various trajectories were made in an effort to determine the impact that the vertical motion of the balloon had on the air mass trajectory. The differences between trajectories is not negligible as there is strong wind shear for all days. It is again important to note that the GASP winds are only accurate to roughly 110 meters altitude. All four balloons drop below this level on a number of occasions. As a result of this, the trajectories track more quickly than the actual balloon motion. START of latlon.00.dat -45.56 #balloon 00 position at 951208 02Z 144.15 END of latlon.00.dat START of latlon.06.dat -45.56 #balloon 06 position at 951208 03Z 144.15 END of latlon.06.dat START of latlon.08.dat -45.61 #balloon 08 position at 951208 01Z 144.71 END of latlon.08.dat START of latlon.10.dat -44.97 #balloon 10 position at 951201 13Z 141.10 END of latlon.10.dat Please contact steve siems (s.siems@sci.monash.edu.au) regarding questions.