Temporal dynamics of evapotranspiration in semiarid native forests in Brazil and Spain using remote sensing

• Published in: Hydrological processes Vol. 35; no. 3
• Main Authors: Alcântara Costa, Juliana, Navarro‐Hevia, Joaquín, Costa, Carlos Alexandre Gomes, de Araújo, José Carlos
• Format: Journal Article
• Language: English
• Published: Hoboken, USA John Wiley & Sons, Inc 01-03-2021; Wiley Subscription Services, Inc
• Subjects: Algorithms; Biodiversity; Caatinga; drylands; Dynamics; Energy balance; Evapotranspiration; Forests; Hydrologic data; Hydrology; Landsat; Landsat satellites; Potential evapotranspiration; Remote sensing; Resource management; Satellite imagery; SEBAL; Semi arid areas; Semiarid lands; Semiarid zones; Soil water; Spatial variations; Stability; Surface energy; Surface energy balance; Surface properties; Tierra de Pinares; Trends; Vulnerability; Water availability; Water balance; Water resources; Water resources management; Water resources planning; Brazil; Spain
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/hyp.14070

Evapotranspiration (ET) plays an important role in integrated water resource planning, development and management. This process is particularly relevant in semiarid regions. The aim of this study is, hence, to compare spatial and temporal patterns of actual ET, as well as the temporal trends in two different semiarid forests, Caatinga (Brazil) and Tierra de Pinares (Spain). We used the surface energy balance algorithm for land (SEBAL) to assess actual evapotranspiration (ETa) in both areas. In the Brazilian semiarid forest, Caatinga is the main vegetation, while it is Pinares in Spain. For this purpose, 69 Landsat‐5 and 42 Landsat‐8 images (1995–2019) were used. The Mann–Kendall test was applied to assess the occurrence of trends in precipitation, temperature and potential ET data; and the Temporal Stability Index (TSI) to know which areas have greater seasonal ETa. The annual amplitude of the potential evapotranspiration (ET0) is the same in both areas, however, the Caatinga values are higher. In the Caatinga forest, when ET0 presents its highest values throughout the year, ETa presents the lowest, and vice versa. In the Pinares forest, ETa follows the ET0 dynamics during the year, and the difference between ET0 and ETa is maximum during the summer. The Caatinga forest showed a greater spatial variation of ETa than the Pinares forest as well as a greater extension with lower temporal stability of ETa than the Pinares forest. Both the Caatinga forest and the Pinares forest showed significant positive trends in annual ET0 and ETa. We estimate that the value of ETa increases more rapidly in Pinares than in the Brazilian Caatinga. Taking Caatinga as a hydrological mirror, some consequences are expected to Pinares, such as significant changes in the water balance, increase of biodiversity vulnerability, and reduction of water availability in soil and reservoirs.
Actual evapotranspiration increases more rapidly in Pinares than in the Caatinga. Taking Caatinga as a hydrological mirror, some consequences are expected to Pinares, such as significant changes in the water balance, increase of biodiversity vulnerability and reduction of water availability in soil and reservoirs.