The Transformation and Export of Organic Carbon Across an Arctic River‐Delta‐Ocean Continuum

• Main Authors: Clark, J Blake, Mannino, Antonio, Tzortziou, Maria, Spencer, Robert GM, Hernes, Peter
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2022
• Subjects: Earth Sciences; Oceanography; Atmospheric Sciences; Geochemistry; Life Below Water; arctic; biogeochemical modeling; carbon cycle; climate change; land‐ocean continuum; Geophysics; Arctic Ocean; Climate change; Phytoplankton; Yukon river; Yukon
• Online Access: https://escholarship.org/uc/item/0hq6w8cm

The Arctic Ocean is surrounded by land that feeds highly seasonal rivers with water enriched in high concentrations of dissolved and particulate organic carbon (DOC and POC). Explicit estimates of the flux of organic carbon across the land-ocean interface are difficult to quantify and many interdependent processes makes source attribution difficult. A high-resolution 3-D biogeochemical model was built for the lower Yukon River and coastal ocean to estimate biogeochemical cycling across the land-ocean continuum. The model solves for complex reactions related to organic carbon transformation, including mechanistic photodegradation and multi-reactivity microbial processing, DOC-POC flocculation, and phytoplankton dynamics. The baseline DOC and POC flux out of the delta from April to September 2019, was 977 and 536GgC (∼80% of the annual total), but only 50% of the DOC and 25% of the POC exited the plume across the 10m isobath. Microbial breakdown of DOC accounted for a net loss of 168GgC (17% of delta export) within the plume and photodegradation accounted for a net loss of 46.6GgC DOC (5% of delta export) in 2019. Flocculation decreased the total organic carbon flux by only 6.4GgC (∼1%), while POC sinking accounted for 63.3GgC (10%) settling in the plume. The loss of chromophoric dissolved organic matter due to photodegradation increased the light available for phytoplankton growth throughout the coastal ocean, demonstrating the secondary effects that organic carbon reactions can have on biological processes and the net coastal carbon flux.