The impact of the freeze–melt cycle of land-fast ice on the distribution of dissolved organic matter in the Laptev and East Siberian seas (Siberian Arctic)
Jens A. Hölemann et al.
Viewed
Total article views: 1,883 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,271
587
25
1,883
17
33
HTML: 1,271
PDF: 587
XML: 25
Total: 1,883
BibTeX: 17
EndNote: 33
Views and downloads (calculated since 05 Jan 2021)
Cumulative views and downloads
(calculated since 05 Jan 2021)
Total article views: 1,132 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
819
302
11
1,132
14
23
HTML: 819
PDF: 302
XML: 11
Total: 1,132
BibTeX: 14
EndNote: 23
Views and downloads (calculated since 18 Jun 2021)
Cumulative views and downloads
(calculated since 18 Jun 2021)
Total article views: 751 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
452
285
14
751
3
10
HTML: 452
PDF: 285
XML: 14
Total: 751
BibTeX: 3
EndNote: 10
Views and downloads (calculated since 05 Jan 2021)
Cumulative views and downloads
(calculated since 05 Jan 2021)
Viewed (geographical distribution)
Total article views: 1,676 (including HTML, PDF, and XML)
Thereof 1,673 with geography defined
and 3 with unknown origin.
Total article views: 986 (including HTML, PDF, and XML)
Thereof 986 with geography defined
and 0 with unknown origin.
Total article views: 690 (including HTML, PDF, and XML)
Thereof 687 with geography defined
and 3 with unknown origin.
The Arctic Ocean receives large amounts of river water rich in terrestrial dissolved organic matter (tDOM), which is an important component of the Arctic carbon cycle. Our analysis shows that mixing of three major freshwater sources is the main factor that regulates the distribution of tDOM concentrations in the Siberian shelf seas. In this context, the formation and melting of the land-fast ice in the Laptev Sea and the peak spring discharge of the Lena River are of particular importance.
The Arctic Ocean receives large amounts of river water rich in terrestrial dissolved organic...
