Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Nino Amvrosiadi"'
Publikováno v:
Journal of Hydrology. 553:798-804
Soil moisture is an important variable for hillslope and catchment hydrology. There are various computational methods to estimate soil moisture and their complexity varies greatly: from one box wit ...
Autor:
Michael F. Billett, Mats G. Öquist, Nino Amvrosiadi, Mark H. Garnett, Marcus B. Wallin, Audrey Campeau, Hjalmar Laudon, Kevin Bishop
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
Nature Communications
Nature Communications
Stream CO2 emissions contribute significantly to atmospheric climate forcing. While there are strong indications that groundwater inputs sustain these emissions, the specific biogeochemical pathways and timescales involved in this lateral CO2 export
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::834dd4fb1ef2e8c3e884035ea58fe47d
https://eprints.gla.ac.uk/183701/1/183701.pdf
https://eprints.gla.ac.uk/183701/1/183701.pdf
Models must effectively represent velocities and celerities if they are to address the old water paradox. Celerity information is recorded indirectly in hydrograph observations, whereas velocity information is more difficult to measure and simulate e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::57cd871916d60403c79f6ea45a06eab1
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-331732
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-331732
Autor:
Irena F. Creed, Jeffrey J. McDonnell, Ali Ameli, Thomas Grabs, Nino Amvrosiadi, Kevin Bishop, Hjalmar Laudon
Publikováno v:
Journal of Hydrology. 543:17-30
Summary Defining the catchment transit time distribution remains a challenge. Here, we used a new semi-analytical physically-based integrated subsurface flow and advective–dispersive particle movement model to assess the subsurface controls on subs
Publikováno v:
Hydrological Processes. 31:4-14
Studies on hydrology, biogeochemistry, or mineral weathering often rely on assumptions about flow paths, water storage dynamics, and transit times. Testing these assumptions requires detailed hydro ...