In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 34, No. 10 ( 2020-10)
Abstract:
Specific yield of dissolved organic carbon (Mg/km 2 /year) is similar between Greenlandic glacial and deglaciated watersheds Sources and potential reactivity differ between glacial (algal) and nonglacial (terrestrial vegetation and soils) watersheds Upscaled organic carbon export from deglaciated watersheds is currently similar to that from glacial watersheds but may increase with future warming
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2020GB006614
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13