Ecologists have long understood that precipitation is the most important climate filter in the low latitudes for determining the distribution of terrestrial biomes, and the structure, composition, and function of ecosystems (Holdridge & Grenke, 1971; Richards, 1952). To understand how water availability influences ecosystems, tropical ecologists have traditionally considered spatial gradients of mean annual precipitation (MAP) and interannual variability of yearly rainfall totals within sites, which are often the first-order drivers of differences among ecosystems in space and time (e.g., Poorter et al., 2016; Santiago et al., 2004; Schuur, 2003). Yet, beyond annual rainfall totals or their year-to-year variability, the timing, intensity, and duration of rainfall in the tropics, on both sub-and super-annual timescales, drive variability in water availability that impacts biota from the organismal to ecosystem level. Tropical precipitation variability leads to periods of resource abundance and scarcity and thus influences biological processes and properties via a variety of mechanisms. For example, some organisms experience high mortality rates during dry months when water or other resources are scarce. Dry season rainfall is a strong predictor of spatial and interannual variation in Australian rainforest bird abundance because food shortages drive high mortality rates during particularly severe dry seasons (Williams & Middleton, 2008). Similarly, seasonal drought can drive high mortality in tree seed