This is the readme file for the NOAA Climet OPC processed data for Kosan during the ACE-Asia experiment, March-April 2001. Measurements were made at Gosan (33.292 N, 126.162 E, Time = UTC + 9 hrs, Elevation = 50 m) during the period of April 5 to April 27, 2001 during the ACE-Asia intensive period. The only day with no data at all is April 12, although there are a number of days with very limited amounts of data (4/17 to 4/20) Contact person: Patrick Chuang pchuang@es.ucsc.edu 831.459.1501 (w) The NOAA Climet OPC is a white light counter, and therefore we expect it to be less sensitive to changes in refractive index versus single wavelength OPCs. The size range that we feel it can reliably measure is 0.5 to 8.7 microns in 9 nearly equally spaced bins. The specific values are shown in the below table. Column 1: The channel number (1 through 9). Column 2: The geometric mean bin diameters = square root of (upper bin boundary diameter*lower bin boundary diameter), in micrometers. Column 3: The geometric bin width = (Upper bin boundary diameter/lower bin boundary diameter). 1 0.50 1.60 2 0.77 1.50 3 1.12 1.40 4 1.57 1.40 5 2.20 1.40 6 3.07 1.40 7 4.30 1.40 8 6.02 1.40 9 8.72 1.50 In reality, the OPC actually measures 64 channels worth of data (although the first 8 exhibit too much instrumental noise to be worth anything), which we then bin into the 9 channels shown above. Nine channels were chosen because it reflects a reasonable bin width compared to the transfer function of the instrument (i.e., particles of size 1.12 microns are very unlikely to be measured as belonging in either bin 2 or bin 4). IMPORTANT NOTE: The reported concentrations are actually dN, in units of cm-3, rather than dN/dlogDp. To obtain the latter from the reported values, divide the reported dN values by the logarithm of the geometric bin width (column 3). --- The uncertainty in the concentration of each bin is reported. A number of different error sources are considered: 1. The width of the OPC transfer function. Based on calibrations of the OPC using PSL and glass bead aerosols, the maximum broadening of a monodisperse aerosol was measured. This is then used in calculating the uncertainty in counting for any particular bin. 2. Counting statistics. Counting errors based on a low sample size can be expressed (assuming Poisson statistics) as square root(counts). This is also factored into the reported uncertainty. 3. Flowrate uncertainty. This is assumed to be 10% of the total flowrate. By correctly propagating these uncertainties, a concentration uncertainty can be reported. These can be considered the one (1) sigma uncertainty in concentration. --- The format of the data files, named opc_spec_day???.txt is as follows: Column 1: Year Column 2: Day of Year (1 to 365) Column 3: Hour (1 to 24) Column 4: Minute (0 to 59) Column 5: Second (0 to 59) Column 6: Decimal day (1 to 265.999). Column 7: Input file name (not really useful information for anyone but myself) Column 8: Integrated OPC measured concentration in units cm-3. That is, measured concentration of all particles in the OPC size range (no uncertainty for this value is presently reported). Column 9 through 17: Concentration for channels 1 through 9 in units cm-3, respectively, i.e. dN(1), dN(2),..., dN(9) where the values in () represents the channel number. NOTE: values are reported as dN, and can be readily converted to dN/dlogDp if desired as described above. Column 18 through 26: One sigma uncertainty in concentration in units cm-3 for channels 1 through 9, respectively, i.e. sigma(dN(1)),..., sigma(dN(9)). Times are reported as UTC, which is Korean Standard Time minus 9 hours. The data are averaged to roughly 1 minute (though not exactly). There are lots of data gaps because of OPC computer crashes, and overheating. --- Patrick Chuang April 8, 2003