Coupled Changes in the Arctic Carbon Cycle Between the Land, Marine, and Social Domains

Author:

Wu Xiaodong123ORCID,Macdonald Robie4,Wu Tonghua1ORCID

Affiliation:

1. Cryosphere Research Station on the Qinghai–Tibet Plateau State Key Laboratory of Cryospheric Science Northwest Institute of Eco‐Environment and Resources Chinese Academy of Sciences Lanzhou China

2. Heilongjiang Province Key Laboratory of Geographical Environment Monitoring and Spatial Information Service in Cold Regions Harbin Normal University Harbin China

3. University of Chinese Academy of Sciences Beijing China

4. Institute of Ocean Science (IOS) Sidney BC Canada

Abstract

AbstractThe Arctic has experienced rapid change associated with warming since the 1970s. The rapid retreat of the terrestrial cryosphere can release a large amount greenhouse gas from the permafrost regions into the air, and the sea ice decline will affect the CO2 and CH4 balance in the ocean. Changes in the Arctic provide feedback mechanisms that can also impinge on the global ocean’s thermohaline circulation. During the past years, the overall natural processes in the Arctic have been studied although the magnitude and timing of carbon release from the cryosphere changes require further investigation. However, few studies have been conducted to link the natural and social systems in the Arctic. Scientists and policymakers must consider the coupled Arctic land, ocean, and social systems in their decisions for coping with climate change.

Funder

National Key Research and Development Program of China

West Light Foundation, Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),General Environmental Science

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