Warming mean temperatures over the past century 1 have probably shifted distributions 2 , altered phenologies 3 , increased extinction risks 4,5 , and impacted agriculture 6 and human health 7 . However, knowledge of mean temperatures alone does not provide a complete understanding either of changes in the climate itself or of how changing climate will a ect organisms 8-11 . Temporal temperature variation, primarily driven by daily and annual temperature cycles, has profound e ects on organism physiology 8,9 and ecology 12 , yet changes in temperature cycling over the past 40 years are still poorly understood 1,13 . Here we estimate global changes in the magnitudes of diurnal and annual temperature cycles from 1975 to 2013 from an analysis of over 1.4 billion hourly temperature measurements from 7,906 weather stations. Increases in daily temperature variation since 1975 in polar (1.4 • C), temperate (1.0 • C) and tropical (0.3 • C) regions parallel increases in mean temperature. Concurrently, magnitudes of annual temperature cycles decreased by 0.6 • C in polar regions, increased by 0.4 • C in temperate regions, and remained largely unchanged in tropical regions. Stronger increases in daily temperature cycling relative to changes in annual temperature cycling in temperate and polar regions mean that, with respect to diurnal and annual cycling, the world is flattening as temperate and polar regions converge on tropical temperature cycling profiles.The global increase in mean temperature 1 and its effects on organisms 4,12,14,15 are well documented. However, knowledge of mean temperature alone has important limitations when applied to problems of ecology 16,17 . Temperature has nonlinear effects on rates of biochemical processes, organism physiology, life history and population growth 18,19 , and ecological interactions 20 . Because of these ubiquitous nonlinear effects of temperature, changes in temperature variation can have profound physiological and ecological impacts that match or even exceed the effects of mean temperatures 8,9,21 . Understanding and predicting the biological consequences of climate change will require knowledge not only of changes in mean temperatures, but also of changes in temperature variation 22 .So far, temporal temperature variation has primarily been described in terms of changing extremes 1,23 . Analyses of monthly and yearly averages of daily temperature extremes reveal that daily and annual minimum and maximum temperatures have increased across the globe since 1950 1 . Larger increases in minimum temperatures have driven reductions in the differences between daily and seasonal extremes (diurnal temperature range and extreme temperature range), suggesting a global decrease in daily and annual temperature variation 1 . However, the time window over which data are averaged can strongly affect not only the likelihood of detecting trends in temperature variability, but also the direction of those trends 22 . Further, the monthly and yearly temperature means analysed for these studies ma...