Observational networks are important for an improved understanding of ecohydrological processes and for improving gridded climate products, yet few studies employing these networks have been undertaken at higher latitudes. We evaluated physiographic controls on summer temperature in Denali National Park and Preserve in Alaska, United States while accounting for synoptic temperature conditions, finding shallow minimum temperature lapse rates, effects of solar radiation, and interactions between physiography and synoptic conditions. Average temperature from monthly gridded climate data was overall warmer than observed while lapse rates from observed data were somewhat steeper and more variable over time than gridded data.