Agne Burauskaite-Harju, Division of Statistics, Department of Computer and Information Science Linköpings Universitet Trends in Precipitation Extremes Abstract It is generally believed that global warming is accompanied by extreme weather events. Assessments of trends in intensity and frequency of extreme rainfall events are of considerable practical importance and have been presented in numerous publications. Nevertheless, we believe there are aspects that have not previously received enough of attention. In the seminar I will present a procedure for trend testing in precipitation extremes for entire network of meteorological stations. In our developed procedure we first make separate estimates of tail probabilities of precipitation amounts for each combination of station and year by fitting a Generalized Pareto Distribution (GPD) to data above a user-defined threshold. Then, the resulting time series of annual percentile estimates are fed into a multivariate Mann-Kendall (MK) test for monotonic trends. Extensive simulations involving artificially generated precipitation data showed that the power of tests for temporal trends was substantially enhanced when ordinary percentiles were substituted for GPD-percentiles. Furthermore, we found that: the trend detection was robust to misspecification of the extreme-value distribution. The MK test has the advantage that it can accommodate nonlinear trends and takes into account the dependencies between stations in a network. Further in the seminar I will highlight the importance of data resolution choice. We demonstrate that trends in rainfall intensity can differ in direction and significance for choice of resolution (duration) and quantile. We also show that sub-daily rainfall data can contain important information about climate change that cannot be detected in daily data. We suggest that trend tests be performed for different resolutions and quantiles, and that the results be presented as tables that allow further interpretation (analogous to intensity-duration-frequency tables used in hydrology). To illustrate methods simulated, observational and regional climate model output data will be used. A short overview of meteorological variables, of global and regional climate modeling, climate change and future greenhouse gas emission scenarios will be given to help understanding properties of data sets and potential difficulties. For more information on methodology and software please visit http://www.ida.liu.se/~agbur/index.htm