Monday, 29 January 2024
Hall E (The Baltimore Convention Center)
The subtropical southeast Pacific hosts one of the most extensive
stratocumulus cloud layer fields, with great importance in the global energy balance
of the climate system. These clouds exist in the upper portion of the marine
atmospheric boundary layer (ABL), whose correct simulation by numerical models has
been a persistent challenge due to the close interaction of multiple physical
processes and the sparseness of in-situ observations, especially in the vertical. In
this work we use AMDAR data to characterize the coastal ABL over four sites along
north-central Chile, between 19° and 30°S. AMDAR data refer to vertical profiles of
temperature and winds measured by commercial aircrafts and made available to weather
services through a WMO program. We use AMDAR data for years 2017-2019 and describe
the diurnal and annual variation of ABL height, winds and temperatures.

