They discussed the effect of variables being non-iid on the extreme value analysis, and after taking that into account, propose that
changes in extreme
precipitation are likely to be larger than the
corresponding changes in annual mean
precipitation under a global warming.
Although, in the tropics, glacier mass balance responds sensitively to
changes in
precipitation and humidity (see Lemke et al., 2007, Section 4.5.3), the fast glacier shrinkage of Chacaltaya is consistent with an ascent of the 0 °C isotherm of about 50 m / decade in the tropical Andes since the 1980s (Vuille et al., 2003), resulting in a
corresponding rise in the equilibrium line of glaciers in the region (Coudrain et al., 2005).