Abstract
The carbonate system of waters of the inner, middle, and outer shelves was studied for a long period in the eastern part of the Laptev Sea. It is shown that the inner and middle shelves is a heterotrophic province and is a source of CO2 to the atmosphere during August–September. The average CO2 flux is 7.9 mmol m–2 day–1 and during one month waters of inner and middle shelves release into the atmosphere up to 0.7 Tg of carbon (C). The outer part of the shelf absorbs up to ~0.1 Tg C at an average rate of 3.9 mmol m–2 day–1 during the month. Generally, the ice-free zone of the eastern shelf of the Laptev Sea is a source of CO2 in the studied season: the amount of C released into the atmosphere within a month is ~0.6 Tg.
| Original language | English |
|---|---|
| Pages (from-to) | 398-401 |
| Number of pages | 4 |
| Journal | Doklady Earth Sciences |
| Volume | 467 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 1 Apr 2016 |
Fingerprint
ASJC Scopus subject areas
- Earth and Planetary Sciences (miscellaneous)
- Earth and Planetary Sciences(all)
Cite this
Assessment of the CO2 fluxes between the ocean and the atmosphere in the eastern part of the Laptev Sea in the ice-free period. / Pipko, I. I.; Pugach, S. P.; Semiletov, I. P.
In: Doklady Earth Sciences, Vol. 467, No. 2, 01.04.2016, p. 398-401.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Assessment of the CO2 fluxes between the ocean and the atmosphere in the eastern part of the Laptev Sea in the ice-free period
AU - Pipko, I. I.
AU - Pugach, S. P.
AU - Semiletov, I. P.
PY - 2016/4/1
Y1 - 2016/4/1
N2 - The carbonate system of waters of the inner, middle, and outer shelves was studied for a long period in the eastern part of the Laptev Sea. It is shown that the inner and middle shelves is a heterotrophic province and is a source of CO2 to the atmosphere during August–September. The average CO2 flux is 7.9 mmol m–2 day–1 and during one month waters of inner and middle shelves release into the atmosphere up to 0.7 Tg of carbon (C). The outer part of the shelf absorbs up to ~0.1 Tg C at an average rate of 3.9 mmol m–2 day–1 during the month. Generally, the ice-free zone of the eastern shelf of the Laptev Sea is a source of CO2 in the studied season: the amount of C released into the atmosphere within a month is ~0.6 Tg.
AB - The carbonate system of waters of the inner, middle, and outer shelves was studied for a long period in the eastern part of the Laptev Sea. It is shown that the inner and middle shelves is a heterotrophic province and is a source of CO2 to the atmosphere during August–September. The average CO2 flux is 7.9 mmol m–2 day–1 and during one month waters of inner and middle shelves release into the atmosphere up to 0.7 Tg of carbon (C). The outer part of the shelf absorbs up to ~0.1 Tg C at an average rate of 3.9 mmol m–2 day–1 during the month. Generally, the ice-free zone of the eastern shelf of the Laptev Sea is a source of CO2 in the studied season: the amount of C released into the atmosphere within a month is ~0.6 Tg.
UR - http://www.scopus.com/inward/record.url?scp=84971255130&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84971255130&partnerID=8YFLogxK
U2 - 10.1134/S1028334X16040127
DO - 10.1134/S1028334X16040127
M3 - Article
AN - SCOPUS:84971255130
VL - 467
SP - 398
EP - 401
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -