English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Knowledge of the transfer of water from a natural surface is of paramount importance in various fields of scientific, especially in the Meteorology and Hydrology applications. The transfer water of any surface to the atmosphere through the processes of evaporation and transpiration is called evapotranspiration, in other words transfer of water from the soil by evaporation and plant transpiration. In this context, the objective of this research was to analyze the anomalies of evapotranspiration on the micro Serido in Rio Grande of the North, from the climatology, using the method of reference evapotranspiration proposed by Hargreaves-Samani, as described by the IPCC scenarios of increased air temperature during wet, transition and dry periods. These results showed that with respect to future scenarios, it appears that there was a great difference in the increase in annual and monthly evapotranspiration for scenario between 2090-2099. Values that exceed the actual climatic classification of Thornthwaite.

ANÁLISE DA EVAPOTRANSPIRAÇÃO SOBRE O SERIDÓ NORDESTINO EM CENÁRIOS DE AQUECIMENTO