In:
Journal of Geophysical Research: Biogeosciences, American Geophysical Union (AGU), Vol. 125, No. 4 ( 2020-04)
Abstract:
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
Type of Medium:
Online Resource
ISSN:
2169-8953
,
2169-8961
DOI:
10.1029/2019JG005161
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
3094167-2
detail.hit.zdb_id:
2220777-6
SSG:
16,13
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