Impact of permafrost degradation on the extreme increase of dissolved iron concentration in the Amur river during 1995–1997 ...

• Main Authors: Tashiro, Yuto, Hiyama, Tetsuya, Kanamori, Hironari, Kondo, Masayuki
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: figshare 2024
• Subjects: Environmental Sciences not elsewhere classified; Chemical Sciences not elsewhere classified; Ecology; FOS: Biological sciences; Sociology; FOS: Sociology; Biological Sciences not elsewhere classified; permafrost
• Online Access: https://dx.doi.org/10.6084/m9.figshare.c.7149688; https://springernature.figshare.com/collections/Impact_of_permafrost_degradation_on_the_extreme_increase_of_dissolved_iron_concentration_in_the_Amur_river_during_1995_1997/7149688

Abstract Primary production in the Sea of Okhotsk is largely supported by dissolved iron (dFe) transported by the Amur river, indicating the importance of dFe discharge from terrestrial environments. However, little is known about the mechanisms of dFe discharge into the Amur river, especially in terms of long-term change in dFe concentration. In the Amur river, extreme increase in dFe concentration was observed between 1995 and 1997, the cause of which remains unclear. As a cause of this iron anomaly, we considered the impact of permafrost degradation. To link the permafrost degradation to long-term variation in dFe concentration, we examined the changes in annual air temperature (Ta), accumulated temperature (AT), and net precipitation for three regions (northeast, south, and northwest) of the basin between 1960 and 2006. Ta and AT were relatively high in one out of every few years, and were especially high during 1988–1990 continuously. Net precipitation in late summer (July to September) has increased ...