Zobrazeno 1 - 10
of 53
pro vyhledávání: '"Catalina Segura"'
Publikováno v:
Water, Vol 10, Iss 7, p 904 (2018)
Water-stable isotopic (WSI) data are widely used in hydrological modelling investigations. However, the long-term monitoring of these tracers at high-temporal resolution (sub-hourly) remains challenging due to technical and financial limitations. Thu
Externí odkaz:
https://doaj.org/article/a237f734432c45fbb293c1a3dc22c701
Seventy years of watershed response to floods and changing forestry practices in western Oregon, USA
Publikováno v:
Earth Surface Processes and Landforms. 48:1103-1118
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::763d656c590544f7e68e7cc56026a686
https://doi.org/10.1002/esp.5537
https://doi.org/10.1002/esp.5537
Publikováno v:
Biogeochemistry. 160:243-258
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbbd11c036569b96ce78a2ceffbaa6ae
https://doi.org/10.1007/s10533-022-00953-5
https://doi.org/10.1007/s10533-022-00953-5
Communities downstream from mountainous regions rely on snowmelt for water supply. As climate change reduces the reliability of the snowpack in these regions it is important to understand how and when rain and melt water are stored and released as ru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c9f7e8131acb65b000b5b334e4792ce
https://doi.org/10.5194/egusphere-egu23-9603
https://doi.org/10.5194/egusphere-egu23-9603
Publikováno v:
Hydrological Processes. 37
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9360cd6539310812fc60922bbb88fb9d
https://doi.org/10.1002/hyp.14795
https://doi.org/10.1002/hyp.14795
Publikováno v:
North American Journal of Fisheries Management. 41:466-473
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9dd4760fbe3df5f26d9efccb61818501
https://doi.org/10.1002/nafm.10549
https://doi.org/10.1002/nafm.10549
Autor:
Catalina Segura
Knowledge of water transit times through watersheds is fundamental to understand hydrological and biogeochemical processes. However, its prediction is still elusive, particularly in mountainous terrain where physiography and precipitation change over
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1a3cb1be3b56e81158e6a21cb9444e3e
https://doi.org/10.5194/egusphere-egu22-10842
https://doi.org/10.5194/egusphere-egu22-10842
Publikováno v:
Hydrological Processes. 36
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb1c6acc91d6472952112450387574a1
https://doi.org/10.1002/hyp.14517
https://doi.org/10.1002/hyp.14517
Publikováno v:
Earth Surface Dynamics, Vol 8, Pp 825-839 (2020)
Bed load transport formulations for gravel-bed rivers are often based on reach-averaged shear stress values. However, the complexity of the flow field in these systems results in wide distributions of shear stress, whose effects on bed load transport
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e0fe2b42de2944b8b32221e3d4319186
https://doi.org/10.5194/esurf-8-825-2020
https://doi.org/10.5194/esurf-8-825-2020