In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 126, No. 2 ( 2021-02)
Kurzfassung:
Along‐channel saltwater fluxes are controlled by advective and shear dispersion fluxes, and influenced by branch morphology Future saltwater intrusion (SWI) is projected to increase up to 80% further into the river, while persistence up to 100% longer River discharge reduction is expected to affect SWI more than sea‐level rise
Materialart:
Online-Ressource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1029/2020JC016437
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2021
ZDB Id:
2016804-4
ZDB Id:
161667-5
ZDB Id:
3094219-6
SSG:
16,13
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