Figure 2
From: Roman water management impacted the hydrological functioning of wetlands during drought periods
(a) Evolution of Lake Zóñar water level and water electrical conductivity (maximum and minimum annual values) from 1985 to 2020 (ref.38). No electrical conductivity data are available until 1992; (b) Discharge of Zóñar and Escobar springs to Lake Zóñar. No data are available until 1988 and from 2011 to 2020 for Zóñar spring; (c) Annual rainfall amount recorded by the meteorological station at Lake Zóñar (two year-moving average is displayed).
