In:
Journal of Geophysical Research: Biogeosciences, American Geophysical Union (AGU), Vol. 125, No. 4 ( 2020-04)
Kurzfassung:
Dissolved organic carbon concentrations can be estimated in glacial outflow from the fluorescence intensity of red‐shifted fluorescence Optical tracers can be used to differentiate subglacial from supraglacial inputs Optical properties in July highlight microbial sources of dissolved organic matter, with implications for downstream bioavailability
Materialart:
Online-Ressource
ISSN:
2169-8953
,
2169-8961
DOI:
10.1029/2019JG005161
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2020
ZDB Id:
3094167-2
ZDB Id:
2220777-6
SSG:
16,13