Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Joep Storms"'
Autor:
Florin Zăinescu, Helena van der Vegt, Joep Storms, Alexis Nutz, Guilherme Bozetti, Jan-Hendrik May, Sagy Cohen, Frederic Bouchette, Simon Matthias May, Mathieu Schuster
Publikováno v:
Journal of Great Lakes Research, 49(2)
A complete annual cycle of the dynamics of fine-grained sediment supplied by the Omo and smaller rivers is simulated for Lake Turkana, one of the world’s large lakes, with the hydrodynamic, wave and sediment transport model Delft3D. The model is fo
Autor:
Youwei WANG, Timothy Baars, Hiranya Sahoo, Joep Storms, Allard Martinius, Philip Gingerich, Hemmo Abels
The lower Eocene Willwood Formation of the Bighorn Basin, Wyoming, USA, is an alluvial succession with a sand content varying around 25%. It has been studied intensively for palaeontology, palaeoenvironments and palaeoclimates, as well as sedimentolo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6cae96e24a93b87b366b4d51d4e4934
https://doi.org/10.31223/x5qp63
https://doi.org/10.31223/x5qp63
Autor:
Florin Zainescu, Mathieu Schuster, Helena van der Vegt, Joep Storms, Alexis Nutz, Guilherme Bozetti, Jan-Hendrik May, Frederic Bouchette, Simon Matthias May
Depositional models for clastic sedimentation in large lakes, notably in rift lakes, emphasize on downslope river and gravity-driven processes. Wind-driven waterbodies (WWB), a recently-defined category of lakes, display features created by wave rela
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b3c458776b678b390057d1dcd6017ce
https://doi.org/10.5194/egusphere-egu22-11771
https://doi.org/10.5194/egusphere-egu22-11771
Autor:
Maria Azpiroz-Zabala, Joep Storms, Joris T. Eggenhuissen, Helena van der Vegt, Bert Jagers, Dirk-Jan Walstra, Arnau Obradors-Latre, Anna Pontén
Turbidity currents are powerful submarine density flows that travel towards the deep-sea carrying huge amounts of suspended sediment. The flow capacity of keeping sediment suspended in turbidity currents controls the flow duration, which can last fro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2fdfda1d1f6a189f325cf302adf55691
https://doi.org/10.5194/egusphere-egu2020-10439
https://doi.org/10.5194/egusphere-egu2020-10439
Autor:
Jos Timmermans, Joep Storms, Eric-Jan Pleijster, Geert van der Meulen, Jos van Alphen, Marjolein Haasnoot, Flm, Diermanse, Cohen, Kim M., Philip Minderhoud, Leuven, Jasper R. F. W., Kari-Anne Gerritsen, Michaël van Buuren, Elma van Boxel, Kristian Koreman, Sanaan Bensi, N.
Publikováno v:
TU Delft DeltaLinks
ISSUE=Feb;TITLE=TU Delft DeltaLinks
Delft University of Technology
ISSUE=Feb;TITLE=TU Delft DeltaLinks
Delft University of Technology
How can the Netherlands adapt to sea level rise on the long term: maintain, advance or retreat? This article compares the results of seven plans and designs from a diverse group of scholars and professionals that offer very different answers to this
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e93ec81212a2d63a20e013b6f623aa2e
http://resolver.tudelft.nl/uuid:7bea091d-d7d8-4bd4-a9c7-33d42369216e
http://resolver.tudelft.nl/uuid:7bea091d-d7d8-4bd4-a9c7-33d42369216e
Autor:
Törnqvist, T. E., Kidder, T. R., Autin, W. J., Borg, K., Jong, A. F. M., Klerks, C. J. W., Snijders, E. M. A., Joep Storms, Dam, R. L., Wiemann, M. C.
Publikováno v:
Scopus-Elsevier
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bbf806b1e88bd72a3f98f72709d74fe7
http://www.scopus.com/inward/record.url?eid=2-s2.0-0029669682&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-0029669682&partnerID=MN8TOARS
Publikováno v:
Scopus-Elsevier
Proceedings ISPRS Commission VII Mid-Term Symposium ?100 Years ISPRS-Advancing Remote Sensing Science?, Vienna, Austria, 5-7 July 2010; IAPRS, XXXVIII (7A), 2010
Proceedings ISPRS Commission VII Mid-Term Symposium ?100 Years ISPRS-Advancing Remote Sensing Science?, Vienna, Austria, 5-7 July 2010; IAPRS, XXXVIII (7A), 2010
The formation of the current Rhine-Meuse delta mainly took place during the last 12 000 years. Consecutive avulsions, i.e. sudden changes in the course of river channels, resulted in a complicated pattern of sandy channel deposits, surrounded by peat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3725e51d9235b30ad795294705fe8b89
http://www.scopus.com/inward/record.url?eid=2-s2.0-84923930246&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-84923930246&partnerID=MN8TOARS
Publikováno v:
Delft University of Technology
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0cd751474207ab2023c166f4ba46be8d
https://research.tudelft.nl/en/publications/8ea30756-85f0-4ca6-be2b-445ca67a5f1a
https://research.tudelft.nl/en/publications/8ea30756-85f0-4ca6-be2b-445ca67a5f1a