15We analyzed monitoring data from small Boreal Shield lakes to understand how 16 variations in air temperature and precipitation affect the phenology and amount of habitat for 17 lake trout (Salvelinus namaycush). Annual air temperatures increased by ~2 ºC (significant in 18 fall and winter). In response, ice-cover was reduced by ~19 d. Despite earlier ice-offs, springs 19 became longer, allowing lake trout longer access to littoral regions when water temperatures 20 were cool. Although summer surface water temperatures increased, the summer did not 21 lengthen. Instead, later spring-warming and fall-cooling of lakes caused summer to shift later in 22 the year, potentially delaying fall spawning. Complete loss of optimal oxythermal habitat volume 23 occurred in all lakes and became more prevalent over time, moreso in the darkest lakes. 24Although air temperatures did not become more variable, several habitat measures did, 25 including mean summer surface water temperatures, duration of ice-cover, timing of ice-off, and 26 minimum volumes of optimal oxythermal habitat. Our results suggest that future warming will 27 impose greater thermal stress on lake trout, but may be tempered by longer springs. 28 29