Extended Data Fig. 2: Minimum temperature velocity in the northern mountain range of Trinidad.
From: Microclimates slow and alter the direction of climate velocities in tropical forests
Climate velocity for minimum temperature of the coldest month in the northern mountain range of Trinidad calculated from free-air, land surface, and within-canopy climates at 1 km, 100 m, and 20 m spatial resolutions. Free-air velocities account for effects of topography but not vegetation on climate variability and are derived from CHELSA climate data (1 km resolution) and mechanistic microclimate models (100 m resolution). Land surface and within-canopy velocities account for effects of topography and vegetation on climate variability and are derived from mechanistic microclimate models. Within canopy velocities represent the average of 3D velocities in the top half of the canopy. Basemaps adapted from the Database of Global Administrative Areas (GADM).
