TY - JOUR
T1 - Impacts of wildfire and post-fire land management on hydrological and sediment processes in a humid Mediterranean headwater catchment
AU - Nunes, João Pedro
AU - Bernard-Jannin, Léonard
AU - Rodríguez-Blanco, María Luz
AU - Boulet, Anne Karine
AU - Santos, Juliana Marisa
AU - Keizer, Jan Jacob
N1 - Funding Information:
This work was funded by the Portuguese Foundation for Science and Technology (FCT/MCTES) within the framework of project ERLAND: “Direct and indirect impacts of climate change on soil erosion and land degradation in Mediterranean watersheds” (FCOMP‐01‐0124‐FEDER‐008534), the baseline funding of the CE3C and CESAM research units (UID/BIA/00329/2019, UID/AMB/50017/2019), and the research grants attributed to J.P. Nunes (SFRH/BPD/39721/2007, SFRH/BPD/87571/2012 and IF/00586/2015) and J.J. Keizer (IF/01465/2015). The authors also acknowledge the contributions of Maria Ermitas Rial Rivas and other members of the Earth Surface Processes Team of the University of Aveiro in supporting almost four years of regular fieldwork in the Macieira de Alcôba experimental catchment.
Funding Information:
This work was funded by the Portuguese Foundation for Science and Technology (FCT/MCTES) within the framework of project ERLAND: ?Direct and indirect impacts of climate change on soil erosion and land degradation in Mediterranean watersheds? (FCOMP-01-0124-FEDER-008534), the baseline funding of the CE3C and CESAM research units (UID/BIA/00329/2019, UID/AMB/50017/2019), and the research grants attributed to J.P. Nunes (SFRH/BPD/39721/2007, SFRH/BPD/87571/2012 and IF/00586/2015) and J.J. Keizer (IF/01465/2015). The authors also acknowledge the contributions of Maria Ermitas Rial Rivas and other members of the Earth Surface Processes Team of the University of Aveiro in supporting almost four years of regular fieldwork in the Macieira de Alc?ba experimental catchment.
Publisher Copyright:
© 2020 John Wiley & Sons Ltd
PY - 2020/12
Y1 - 2020/12
N2 - The extensive afforestation of the Mediterranean rim of Europe in recent decades has increased the number of wildfire disturbances on hydrological and sediment processes, but the impacts on headwater catchments is still poorly understood, especially when compared with the previous agricultural landscape. This work monitored an agroforestry catchment in the north-western Iberian Peninsula, with plantation forests mixed with traditional agriculture using soil conservation practices, for one year before the fire and for three years afterwards, during which period the burnt area was ploughed and reforested. During this period, continuous data was collected for meteorology, streamflow and sediment concentration at the outlet, erosion features were mapped and measured after major rainfall events, and channel sediment dynamics were monitored downstream from the agricultural and the burnt forest area. Data from 202 rainfall events with over 10 mm was analysed in detail. Results show that the fire led to a notable impact on sediment processes during the first two post-fire years, but not on streamflow processes; this despite the small size of the burnt area (10% of the catchment) and the occurrence of a severe drought in the first year after the fire. During this period, soil loss at the burnt forest slopes was much larger than that at most traditionally managed fields, and, ultimately, led to sediment exhaustion. At the catchment scale, storm characteristics were the dominant factor behind streamflow and sediment yield both before and after the fire. However, the data indicated a shift from detachment-limited sediment yield before the fire, to transport-limited sediment yield afterwards, with important increases in streamflow sediment concentration. This indicates that even small fires can temporarily change sediment processes in agroforestry catchments, with potential negative consequences for downstream water quality.
AB - The extensive afforestation of the Mediterranean rim of Europe in recent decades has increased the number of wildfire disturbances on hydrological and sediment processes, but the impacts on headwater catchments is still poorly understood, especially when compared with the previous agricultural landscape. This work monitored an agroforestry catchment in the north-western Iberian Peninsula, with plantation forests mixed with traditional agriculture using soil conservation practices, for one year before the fire and for three years afterwards, during which period the burnt area was ploughed and reforested. During this period, continuous data was collected for meteorology, streamflow and sediment concentration at the outlet, erosion features were mapped and measured after major rainfall events, and channel sediment dynamics were monitored downstream from the agricultural and the burnt forest area. Data from 202 rainfall events with over 10 mm was analysed in detail. Results show that the fire led to a notable impact on sediment processes during the first two post-fire years, but not on streamflow processes; this despite the small size of the burnt area (10% of the catchment) and the occurrence of a severe drought in the first year after the fire. During this period, soil loss at the burnt forest slopes was much larger than that at most traditionally managed fields, and, ultimately, led to sediment exhaustion. At the catchment scale, storm characteristics were the dominant factor behind streamflow and sediment yield both before and after the fire. However, the data indicated a shift from detachment-limited sediment yield before the fire, to transport-limited sediment yield afterwards, with important increases in streamflow sediment concentration. This indicates that even small fires can temporarily change sediment processes in agroforestry catchments, with potential negative consequences for downstream water quality.
KW - headwater catchment
KW - hydrological response
KW - Mediterranean
KW - post-fire management
KW - sediment processes
KW - wildfire
U2 - 10.1002/hyp.13926
DO - 10.1002/hyp.13926
M3 - Article
AN - SCOPUS:85092566053
SN - 0885-6087
VL - 34
SP - 5210
EP - 5228
JO - Hydrological Processes
JF - Hydrological Processes
IS - 26
ER -