The surface is the interface through which the bedrock interacts with
the boundary-layer. Here, living organisms of various shapes, sizes, and
function intermingle with the mineral soil, organic residue, and canopy
air space that reside there. Together, they breath, absorb momentum,
exchange water and gases, and bask in the heat from the sun and clouds
above and thermal reservoirs below. While many of these functions are
well understood, we knew less about how those functions operate and
behave at different spatial and time scales. More intriguing, surface
variance with scale influences scales of motion in the atmosphere. Here,
I present a generalized look at how land and atmosphere scales interact,
focusing on the lens of the surface energy budget. These processes are
investigated through intensive measurements and high-resolution models
conducted at the CHEESEHEAD19 field experiment in Wisconsin. A
combination of airborne and tower eddy covariance networks, drone and
airborne canopy imaging, and turbulence resolving simulations reveal
persistent mesoscale contributions in the atmosphere enabled by surface
heterogeneity.