01854nas a2200133 4500008004100000245006700041210006700108300001100175490000700186520140500193100001301598700001801611856009101629 2006 eng d00aImpact of hydroclimatic fluctuations on the soil water balance0 aImpact of hydroclimatic fluctuations on the soil water balance a4606 -0 v423 a[1] We analyze the propagation of daily fluctuations in rainfall and potential evapotranspiration to soil moisture dynamics, using a stochastic model that accounts for these two different forms of hydroclimatic variability. The pulsing, intermittent behavior of daily precipitation is described by a compound Poisson process that models the unpredictability of both frequency and amount of rainfall events, while fluctuations in potential evapotranspiration that act continuously in time are assumed to be Gaussian. The resulting model for the soil water balance is thus a stochastic differential equation, forced by a state-dependent compound Poisson noise and a multiplicative Gaussian noise. Steady state probability distribution functions (pdfs) of soil moisture are obtained analytically along with the equations for the expected water balance and its variability. The multiplicative effect of temporal fluctuations in potential evapotranspiration on soil moisture reduces the soil water losses caused by evapotranspiration compared to the case when they are not present. Most importantly, the analysis also shows that because of their different forms and state dependence the impact of rainfall variability on soil moisture dynamics is much more significant than that of potential evapotranspiration, the fluctuations of which do not affect appreciably the soil moisture statistical properties.1 aDaly, E.1 aPorporato, A. uhttp://lter.konza.ksu.edu/content/impact-hydroclimatic-fluctuations-soil-water-balance01414nas a2200145 4500008004100000245009000041210006900131300001200200490000700212520088300219100001801102700001301120700001401133856012101147 2006 eng d00aSuperstatistics of hydro-climatic fluctuations and interannual ecosystem productivity0 aSuperstatistics of hydroclimatic fluctuations and interannual ec a15402 -0 v333 a[1] Ecosystems driven by hydro-climatic fluctuations at different time scales can be interpreted as non-equilibrium dynamical systems. Here we explore the propagation of daily and interannual rainfall fluctuations through the soil-plant system using the theory of superstatistics. With the help of simplified stochastic models of rainfall, we show how interactions of daily and interannual rainfall fluctuations may qualitatively change the probability distributions of rainfall toward higher frequencies of extreme droughts and intense storms. This in turn is likely to induce marked changes in productivity of mesic ecosystems, while more xeric ecosystems might be insensitive or even benefit from them. This study provides a theoretical basis for predictions of ecosystem responses to the increased precipitation variability expected in future North American climate regimes.1 aPorporato, A.1 aVico, G.1 aFay, P.A. uhttp://lter.konza.ksu.edu/content/superstatistics-hydro-climatic-fluctuations-and-interannual-ecosystem-productivity