Thermal conditions control the elevation to which trees persist in alpine settings. Long-term historical data suggests a correlation between periods of anomalously warm regional temperatures and treeline advance on Pike’s Peak (Southern Rocky Mountains, Colorado, USA) (Kummel et al., W.I.P). Still, treelines do not uniformly respond to warming and treeline form is shown to be an indicator of sensitivity to warming (Harsch & Bader, 2011). This dependence suggests that further investigation of the relationship between climate and treeline movement is warranted. While alpine vegetation are controlled by the climate at treeline, they also interact with the air around them and in this way influence local climate. This report focuses on the microclimatology of air parcels surrounding individual trees and the relationship between microclimatology and tree growth. We found important results that indicate the formation of distinct microclimatological regions around individual trees. Specifically, it seems that trees act as a barrier to upslope airflow and in so doing cause the formation of eddies on the leeward side of trees. The longer residence times of entrained air tends to correspond with elevated temperature and moisture conditions. This microclimate formation suggests that trees process and shape their local climate in interesting ways. Understanding the sensitivity of treeline to climate change will be a question of understanding the interaction of local tree climate with that of the overall treeline.