An analytical model for the streamwise velocity space-time correlations in turbulent flows is derived and applied to the special case of velocity fluctuations in large wind farms. The model is based on the Kraichnan-Tennekes random sweeping hypothesis, capturing the decorrelation in time while including a mean wind velocity in the streamwise direction. In the resulting model, the streamwise velocity space-time correlation is expressed as a convolution of the pure space correlation with an analytical temporal decorrelation kernel. Hence, the spatiotemporal structure of velocity fluctuations in wind farms can be derived from the spatial correlations only. We then explore the applicability of the model to predict spatiotemporal correlations in turbulent flows in wind farms. Comparisons of the model with data from a large eddy simulation of flow in a large, spatially periodic wind farm are performed, where needed model parameters such as spatial and temporal integral scales and spatial correlations are determined from the large eddy simulation.Good agreement is obtained between the model and large eddy simulation data showing that spatial data may be used to model the full spatiotemporal structure of fluctuations in wind farms. KEYWORDS large eddy simulation, power output fluctuations, space-time correlations, turbulent flows, wind farms 1 INTRODUCTION The wind energy market is strongly growing with a record in new installations in 2015 1,2 and increasing importance expected over the next years. 3 Wind energy is a fluctuating resource that is converted into electrical power in a nonlinear fashion (see, eg, Burton et al 4 ). These characteristics constitute challenges with respect to power quality and grid stability, cf Milan et al, 5 which raise significant interest in predicting short-term power output fluctuations in wind farms. Understanding and predicting the spatiotemporal structure of velocity fluctuations in wind farms, which is a main source of the power output fluctuations, is a crucial step towards this goal. The atmospheric conditions of wind approaching a wind farm can be described by basic atmospheric boundary layer (ABL) theory. For a recent overview, we refer to Stevens and Meneveau. 6 Wind speed fluctuations in the ABL occur on different time scales, ranging from annual or seasonal variations, down to minutes and seconds. 4,7 The short-term fluctuations on scales shorter than around, say, 10 minutes are usually referred to as turbulent fluctuations. 4 An introduction to the characteristics of atmospheric wind including typical turbulence intensities and naturally occurring extreme wind gusts (cf Böttcher et al 8 ), as well as other factors such as geographical (onshore and offshore), landscape, and climate influences is given in Burton et al. 4 The evolution of wind velocities in the wind farm itself is influenced by the aerodynamics of the turbines (see, eg, Hansen andButterfield 9 ), the design of the whole wind farm, eg, in terms of turbine spacing, 10,11 and by the influence of turbines onto each ...