https://spdf.gsfc.nasa.gov/pub/data/wind/swe/ascii/swe_kp_unspike/aareadme.txt Readme file for SWE KP data This directory contains a twice-improved version of Wind/SWE key parameter (KP) data originally computed in near real time at the ISTP Central Data Handling Facility and subsequently at the "Polar-Wind-Geotail Facility," both at GSFC. The data consist of ~92-s resolution plasma (proton) flow velocities (speed, Cartesian components and/or angles), densities and thermal speeds (or temperatures). In particular, the version in this directory contains flow speed, Cartesian components of the flow velocity, density and temperature. As described in the readme associated with the MIT-accessible version of these data at ftp://space.mit.edu/pub/plasma/wind/kp_files/, the parameters are derived by assuming convecting isotropic Maxwellian distributions, and by combining the results of 3-point fits to observations made along each of several look directions. The originally computed version of the data are CDAWeb- accessible at http://cdaweb.gsfc.nasa.gov/ A version of the data from which many single-point data spikes have been removed at MIT is ftp-accessible as daily ASCII files from MIT at ftp://space.mit.edu/pub/plasma/wind/kp_files/. MIT tested for the relative difference between the value of flow speed (V), density (N) or thermal speed (W) and the median value of the seven points centered on the point being tested. If this relative difference exceeded 0.1, 0.5, or 1.0 for V, N or W, respectively, the record was rejected. For example, if |N - Median(N)| / Median(N) > 0.5, the record was rejected. Both the CDAWeb and MIT-accessible versions of the data have both flow angles and Cartesian components, and have thermal speeds rather than temperatures. Both of these versions also contain, in addition to solar wind data, data from the non-solar wind phases of the Wind orbit. The data files in this directory were created in 2005-6, from the MIT-resident files, as part of the effort to create ACE, Wind and IMP 8 data files shifted to the Earth's bow shock nose, and a merger thereof called the high-resolution OMNI data set. It should be noted that we were encouraged by the instrument team at MIT to use this product for our purposes rather than the also-available non-linear anisotropic fit based or moments analysis based SWE parameters, owing to the greater "robustness" of the KP data. Further discussion of this choice, as well as comparisons among the various SWE plasma parameter data sets, is available in the documentation of the high-resolution OMNI data product at TBD. The format for the records of this new product is given below. Note that in the process, we have eliminated the flow angles (in favor of the Cartesian components), have converted the thermal speeds to equivalent temperatures (T = 60.5 * W**2, where T is temperature in deg K and W is thermal speed in km/s), and have created annual files rather than the daily files MIT holds. More significantly, we undertook to further clean the data files. First, we eliminated all non-interplanetary time intervals using (1) the Wind bow shock timing information given by the Wind/MFI team at http://wind.nasa.gov/mfi/bow_shock.html through 2003, day 286, and our own identifications of the very few bow shock crossings past that date. MIT offers its own identifications at http://web.mit.edu/afs/athena/org/s/space/www/wind/wind_data_appendix.html Secondly, we removed some single point spikes which had survived the MIT spike removal program For each parameter P (P = V, Vx, Vy, Vz, N, T in sequence), we assessed the goodness of each point by forming a 4-point average
of the two points most immediately preceding and following the point being tested. The average
has the rms standard deviation "sigma." Given the natural ~92 sec resolution of the data, the first and last point in each test were typically separated by about six minutes. But this could be longer in the presence of data gaps. To test a point, we required that the first and last point used in the test lay within 60 minutes of each other. Otherwise we have a new data segment. The first and last two points of each such data segment were assumed to be good points. Two conditions were required to declare a spike. First, it was required that |P-
| > 4 * sigma, for each P. Second, for P = V, N or T, it was required that |P-
| > k *
, where k = 0.1 for P = V and k = 0.3 if P = N or T. For P = Vx, Vy, or Vz, the second condition was that |P-
| > 0.1 *