Some loggers make separate data files for each sensor, so that temperature is separated from its corresponding RH value. This makes calculation difficult by requiring an extra process of fusing the two data sets.
For serious interpretation you will need a spreadsheet or scientific graphing program. A reasonable general purpose spreadsheet for refining data is Microsoft Excel. Its main rival, Lotus 123, is rather hamfisted at importing data, but otherwise OK. I've not tried the latest version of the third of the biggies, Corel Quattro.
These spreadsheets limit the number of data points they will graph to less than one year of data at one point per hour, which is a typical data format, also for official weather data. This is very irritating. It happens because the program designer expects you to want to make relationships in diagonal directions over the spreadsheet, so all the data are read in at once. Weather measurements are basically a long database of numbers, without much need for diagonal interactions. Dealing with such data has been rather neglected by programmers. There are, however, several freeware, and shareware graphing programs that take lots of sets of numbers. They can be downloaded from the net.
On the subject of data points there is one peculiar hazard of interpreting the intermittent data that comes from digital data loggers, in comparison with the continuous trace from the thermohygrograph. It is possible to get quite wrong graphs in air conditioned rooms. Most air conditioners switch between heating and cooling and wetting and drying, at set points. The continuous graph looks like the purple zigzag. The frequency is not constant: it varies with the heating and moisture load. A data logger which just wakes up once an hour to squint at the weather and note the instantaneous value will give a quite different curve: the dotted orange line.
Some data loggers can be told to measure more frequently and then average the result before memorising it. This also can give misleading curves by smoothing out variations that are often useful in diagnosis.
The various formulæ for playing around with units of atmospheric moisture are listed in another chapter. The java script of the calculator, has the formulae in a format close to that required by a spreadsheet. You can download this file and then call it from your own computer without connecting to internet every time.