Dust Layer Height Leads Atmospheric Boundary Layer Height by 3 hr Over the Taklimakan Desert
The vertical distribution of dust modulates its radiative forcing and long‐range transport, yet the diurnal relationship between dust layer height (DLH) and atmospheric boundary layer height (ABLH) remains poorly constrained by observations. Here, we present the first hourly, 4‐km‐resolution DLH climatology over the Ta...