Zobrazeno 1 - 10
of 13
pro vyhledávání: '"W. M. J . Luxemburg"'
Autor:
M. C. Westhoff, H. H. G. Savenije, W. M. J . Luxemburg, G. S. Stelling, N. C. van de Giesen, J. S. Selker, L. Pfister, S. Uhlenbrook
Publikováno v:
Hydrology and Earth System Sciences, Vol 11, Iss 4, Pp 1469-1480 (2007)
Distributed temperature data are used as input and as calibration data for an energy based temperature model of a first order stream in Luxembourg. A DTS (Distributed Temperature Sensing) system with a fiber optic cable of 1500 m was used to measure
Externí odkaz:
https://doaj.org/article/253230edec0c4d0a9009cdec233d5dcb
Autor:
M. C. Westhoff, H. H. G. Savenije, W. M. J . Luxemburg, G. S. Stelling, N. C. van de Giesen, J. S. Selker, L. Pfister, S. Uhlenbrook
Publikováno v:
Hydrology and Earth System Sciences, Vol 15, Iss 10, Pp 3091-3091 (2011)
No abstract available.
Externí odkaz:
https://doaj.org/article/f8f7f16e66cb451e999ec3fbbd42f891
Publikováno v:
Hydrology and Earth System Sciences, Vol 18, Iss 7, Pp 2599-2613 (2014)
In this paper we present a novel method to determine the time of occurrence of tidal slack with a GPS receiver mounted on an anchored buoy commonly used to delineate shipping lanes in estuaries and tidal channels. Slack tide occurs when the tide c
Externí odkaz:
https://doaj.org/article/81783ac2ea344df5b548aeeae6e2df30
Autor:
Nick van de Giesen, Andrés Cózar, Matthieu de Schipper, Daniel González-Fernández, Tim van Emmerik, W. M. J. Luxemburg, Sophie Broere
Publikováno v:
Frontiers in Earth Science, 9
Frontiers in earth science, 9
Frontiers in Earth Science 9 (2021)
Front. Earth Sci. 9:628704
RODIN. Repositorio de Objetos de Docencia e Investigación de la Universidad de Cádiz
instname
Frontiers in Earth Science, Vol 9 (2021)
Frontiers in earth science, 9
Frontiers in Earth Science 9 (2021)
Front. Earth Sci. 9:628704
RODIN. Repositorio de Objetos de Docencia e Investigación de la Universidad de Cádiz
instname
Frontiers in Earth Science, Vol 9 (2021)
Plastics originating from land are mainly transported to the oceans by rivers. The total plastic transport from land to seas remains uncertain because of difficulties in measuring and the lack of standard observation techniques. A large focus in obse
Autor:
Nick van de Giesen, W. M. J. Luxemburg, Andrés Cózar, Tim van Emmerik, Daniel González-Fernández, Matthieu de Schipper, Sophie Broere
Riverine plastics cause severe global problems, regarding the risk for human health and environmental damage. The major part of the plastic waste that ends up in the oceans is transported via rivers. However, estimations of global quantities of plast
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5196d131e0c95581f740f8c9fe4260b0
https://doi.org/10.5194/egusphere-egu2020-8321
https://doi.org/10.5194/egusphere-egu2020-8321
Autor:
Hubert Samboko, Ivar Abas, Hubert H. G. Savenije, Hodson Makurira, Hessel Winsemius, W. M. J. Luxemburg, Kawawa Banda
Publikováno v:
Physics and Chemistry of the Earth (Print), 117
Rapid advancements in technologies open up possibilities for water resource authorities to increase their ability to accurately, safely and efficiently establish river flow observation through remote and non-intrusive observation methods. Low-cost Un
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::101cec533b7e542a48a2da5a150cd5fc
http://resolver.tudelft.nl/uuid:8b5aefc7-27b8-4904-968b-c348e2ac35ef
http://resolver.tudelft.nl/uuid:8b5aefc7-27b8-4904-968b-c348e2ac35ef
Autor:
Tanja Euser, W. M. J. Luxemburg, A. D. Clulow, Colin S. Everson, M. G. Mengistu, Wim G.M. Bastiaanssen
Publikováno v:
Hydrology and Earth System Sciences, 18, 2014
Hydrology and Earth System Sciences, Vol 18, Iss 6, Pp 2021-2032 (2014)
Hydrology and Earth System Sciences, Vol 18, Iss 6, Pp 2021-2032 (2014)
The Bowen ratio surface energy balance method is a relatively simple method to determine the latent heat flux and the actual land surface evaporation. The Bowen ratio method is based on the measurement of air temperature and vapour pressure gradients
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dfad9331e7dc3867a8c51e5b7a1d2e3b
https://www.hydrol-earth-syst-sci.net/18/2021/2014/
https://www.hydrol-earth-syst-sci.net/18/2021/2014/
Autor:
Hubert H. G. Savenije, Miriam Coenders-Gerrits, Bart Schilperoort, César Jiménez Rodríguez, W. M. J. Luxemburg, César Cisneros Vaca
Publikováno v:
Hydrology and earth system sciences, 22(1), 819-830. Copernicus
Hydrology and Earth System Sciences, 22(1)
Hydrology and Earth System Sciences, Vol 22, Pp 819-830 (2018)
Hydrology and Earth System Sciences Discussions
Hydrology and Earth System Sciences, 22(1)
Hydrology and Earth System Sciences, Vol 22, Pp 819-830 (2018)
Hydrology and Earth System Sciences Discussions
Rapid improvements in the precision and spatial resolution of distributed temperature sensing (DTS) technology now allow its use in hydrological and atmospheric sciences. Introduced by ) is the use of DTS for measuring the Bowen ratio (BR-DTS), to es
Publikováno v:
Hydrology and Earth System Science, 18, 2014
Hydrology and Earth System Sciences Discussions, 10 (11), 2013
Hydrology and Earth System Sciences, Vol 18, Iss 7, Pp 2599-2613 (2014)
Hydrology and Earth System Sciences Discussions, 10 (11), 2013
Hydrology and Earth System Sciences, Vol 18, Iss 7, Pp 2599-2613 (2014)
In this paper we present a novel method to determine the time of occurrence of tidal slack with a GPS receiver mounted on an anchored buoy commonly used to delineate shipping lanes in estuaries and tidal channels. Slack tide occurs when the tide chan
Autor:
Martijn Westhoff, W. M. J. Luxemburg, Laurent Pfister, Stefan Uhlenbrook, Guus S. Stelling, Hubert H. G. Savenije, John S. Selker, N.C. Van de Giesen
Publikováno v:
Hydrology and Earth System Sciences, Vol 15, Iss 10, Pp 3091-3091 (2011)
Distributed temperature data are used as input and as calibration data for an energy based temperature model of a first order stream in Luxembourg. A DTS (Distributed Temperature Sensing) system with a fiber optic cable of 1500m was used to measure s