Wednesday, 15 January 2020: 3:00 PM
260 (Boston Convention and Exhibition Center)
Radan Huth, Faculty of Science, Charles Univ., Prague, Czech Republic; Institute of Atmospheric Physics, Czech Academy of Sciences, Prague, Czech Republic; and M. Kucerova and L. Pokorna
The picture of long-term changes (trends) of climate is highly multivariate: the trends are detected in multiple variables, at many sites (stations or gridpoints), for different sections of year (seasons, months, or sliding seasons), for different time periods. To fully describe this picture requires either a huge pile of graphs and maps to be drawn, which would be very difficult to comprehend altogether, or an aggregation of all trend characteristics into a smaller set (that is, reduction of their dimensionality), which would be easy to look at and to interpret. The second way has rarely been attempted so far.
We suggest to use principal component analysis (PCA) for this purpose. We examine various possible settings of the input data matrix, that is, how the data are arranged into its columns and rows, and of PCA, including the choice of normalization, similarity matrix, rotation, and number of components to be rotated. This allows us to evaluate relationships among trends in multiple variables and to see, for example, how trends in temperature, daily temperature range, cloudiness, and sunshine duration are related to each other, how their relationships vary in space and during year, as well as whether they vary in the course of time. Another application of the PCA-based analysis of trends is the description of the warming holes, that is, the regions and periods with the lack of warming, which were observed, among others, in North America and Europe in the second half of the 20th century, and their localization in space, time, and within annual cycle.
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