Lakes are critical freshwater resources that are highly sensitive to stressors such as climate change (Woolway et al., 2020) and altered land use (Martinuzzi et al., 2014). Globally, these stressors are shortening the duration of ice cover (Sharma et al., 2019), increasing rates of lake carbon burial (Heathcote & Downing, 2012), increasing evaporative water loss (Wang et al., 2018), warming surface waters (O'Reilly et al., 2015), and changing mixing regimes (Maberly et al., 2020), all of which influence lake productivity and ecological state. These changes manifest themselves in the seasonality of lake processes. Just like a deciduous forest that comes to life in the spring, inland water bodies are characterized by a predictable seasonal succession of biological processes (Sommer et al., 2012). In the spring, many lakes experience a diatom bloom, followed by a "clear-water" phase where zooplankton rapidly devour the newly plentiful phytoplankton (Matsuzaki et al., 2020). Summer algal biomass is constrained by nutrient availability, with nutrient-rich eutrophic lakes experiencing near-constant summer phytoplankton blooms, and nutrient-poor oligotrophic lakes experiencing relatively clear waters (Sommer et al., 1986). The difference between these states is visible to the Abstract Lakes are often defined by seasonal cycles. The seasonal timing, or phenology, of many lake processes are changing in response to human activities. However, long-term records exist for few lakes, and extrapolating patterns observed in these lakes to entire landscapes is exceedingly difficult using the limited number of available in situ observations. Limited landscape-level observations mean we do not know how common shifts in lake phenology are at macroscales. Here, we use a new remote sensing data set, LimnoSat-US, to analyze U.S. summer lake color phenology between 1984 and 2020 across more than 26,000 lakes. Our results show that summer lake color seasonality can be generalized into five distinct phenology groups that follow well-known patterns of phytoplankton succession. The frequency with which lakes transition from one phenology group to another is tied to lake and landscape level characteristics. Lakes with high inflows and low variation in their seasonal surface area are generally more stable, while lakes in areas with high interannual variations in climate and catchment population density show less stability. Our results reveal previously unexamined spatiotemporal patterns in lake seasonality and demonstrate the utility of LimnoSat-US, which, with over 22 million remote sensing observations of lakes, creates novel opportunities to examine changing lake ecosystems at a national scale.Plain Language Summary Lakes have seasonal cycles that result in yearly peaks in algal growth. The size and timing of these peak periods depends on the amount of nutrients available and the timing of key events such as freezing and thawing. Bluer lakes with little algae typically have one peak in the spring, while greener, high algae lakes can have m...