Assessment of the CO2 fluxes between the ocean and the atmosphere in the eastern part of the Laptev Sea in the ice-free period; Doklady Earth Sciences; Vol. 467, iss. 2

Assessment of the CO2 fluxes between the ocean and the atmosphere in the eastern part of the Laptev Sea in the ice-free period; Doklady Earth Sciences; Vol. 467, iss. 2

Λεπτομέρειες βιβλιογραφικής εγγραφής
Parent link:	Doklady Earth Sciences.— , 1933- Vol. 467, iss. 2.— 2016.— [P. 398–401]
Κύριος συγγραφέας:	Pipko I. I. Irina Ivanovna
Συλλογικό Έργο:	Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра геологии и разведки полезных ископаемых, Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра геологии и разведки полезных ископаемых Международная научно-образовательная лаборатория изучения углерода арктических морей
Άλλοι συγγραφείς:	Pugach S. P. Svetlana Petrovna, Semiletov I. P. Igor Petrovich
Περίληψη:	Title screen 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. Режим доступа: по договору с организацией-держателем ресурса
Γλώσσα:	Αγγλικά
Έκδοση:	2016
Θέματα:	электронный ресурс труды учёных ТПУ
Διαθέσιμο Online:	http://dx.doi.org/10.1134/S1028334X16040127
Μορφή:	Ηλεκτρονική πηγή Κεφάλαιο βιβλίου
KOHA link:	https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=651025

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