Articles | Volume 21, issue 11
Research article
16 Jun 2021
Research article |  | 16 Jun 2021

Local evaporation controlled by regional atmospheric circulation in the Altiplano of the Atacama Desert

Felipe Lobos-Roco, Oscar Hartogensis, Jordi Vilà-Guerau de Arellano, Alberto de la Fuente, Ricardo Muñoz, José Rutllant, and Francisco Suárez


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2020-1300', Anonymous Referee #2, 23 Mar 2021
    • AC1: 'Reply on RC1', Felipe Lobos Roco, 27 Mar 2021
  • RC2: 'Comment on acp-2020-1300', Anonymous Referee #1, 04 Apr 2021
    • AC2: 'Reply on RC2', Felipe Lobos Roco, 05 Apr 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Felipe Lobos Roco on behalf of the Authors (21 Apr 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (22 Apr 2021) by Stefano Galmarini
AR by Felipe Lobos Roco on behalf of the Authors (22 Apr 2021)
Short summary
We investigate the influence of regional atmospheric circulation on the evaporation of a saline lake in the Altiplano region of the Atacama Desert through a field experiment and regional modeling. Our results show that evaporation is controlled by two regimes: (1) in the morning by local conditions with low evaporation rates and low wind speed and (2) in the afternoon with high evaporation rates and high wind speed. Afternoon winds are connected to the regional Pacific Ocean–Andes flow.
Final-revised paper