Impacts of climate and land use changes on the hydrological and erosion processes of two contrasting Mediterranean catchments
Autor: | Dalila Serpa, Júlio Lima, João Osvaldo Rodrigues Nunes, Sandro F. Veiga, Juliana Marisa Santos, Madalena Moreira, Rita Jacinto, João Corte-Real, Elsa Sampaio, Nelson Abrantes, Jan Jacob Keizer |
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Přispěvatelé: | Barcelo, D. |
Rok vydání: | 2015 |
Předmět: |
Mediterranean climate
Hydrology geography Environmental Engineering geography.geographical_feature_category Land use Drainage basin Climate change Mediterranean Pollution Erosion Streamflow Environmental Chemistry Environmental science Land use land-use change and forestry SWAT model Land use change Waste Management and Disposal |
Zdroj: | Science of the Total Environment, 538, 64-77 Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação instacron:RCAAP Science of the Total Environment 538 (2015) |
ISSN: | 1879-1026 0048-9697 |
Popis: | The impacts of climate and land use changes on streamflow and sediment export were evaluated for a humid (São Lourenço) and a dry (Guadalupe) Mediterranean catchment, using the SWAT model. SWAT was able to produce viable streamflow and sediment export simulations for both catchments, which provided a baseline for investigating climate and land use changes under the A1B and B1 emission scenarios for 2071-2100. Compared to the baseline scenario (1971-2000), climate change scenarios showed a decrease in annual rainfall for both catchments (humid: - 12%; dry: - 8%), together with strong increases in rainfall during winter. Land use changes were derived from a socio-economic storyline in which traditional agriculture is replaced by more profitable land uses (i.e. corn and commercial forestry at the humid site; sunflower at the dry site). Climate change projections showed a decrease in streamflow for both catchments, whereas sediment export decreased only for the São Lourenço catchment. Land use changes resulted in an increase in streamflow, but the erosive response differed between catchments. The combination of climate and land use change scenarios led to a reduction in streamflow for both catchments, suggesting a domain of the climatic response. As for sediments, contrasting results were observed for the humid (A1B: - 29%; B1: - 22%) and dry catchment (A1B: + 222%; B1: + 5%), which is mainly due to differences in the present-day and forecasted vegetation types. The results highlight the importance of climate-induced land-use change impacts, which could be similar to or more severe than the direct impacts of climate change alone. |
Databáze: | OpenAIRE |
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