Key points are not available for this paper at this time.
Low-level flight data from a small cloud-free area along the periphery of Hurricane Eloise (1975) reveal the existence of a well-mixed boundary layer which is capped by a near-isothermal layer. The isothermal layer is probably created by the combined effect of subsiding air and surface-induced turbulence.
Moss et al. (Thu,) studied this question.