English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The distributions of carbonate system parameters in Hudson Bay,which not only receives nearly one-third of Canada's river discharge butis also subject to annual cycles of sea-ice formation and melt,indicate that the timing and magnitude of freshwater inputs play animportant role in carbon biogeochemistry and acidification in this uniqueArctic ecosystem. This study uses basin-wide measurements of dissolvedinorganic carbon (DIC) and total alkalinity (TA), as well as stable isotopetracers (δ18O and δ13CDIC), to provide adetailed assessment of carbon cycling processes within the bay. Surfacedistributions of carbonate parameters reveal the particular importance offreshwater inputs in the southern portion of the bay. Based on TA, wesurmise that the deep waters in the Hudson Bay are largely of Pacificorigin. Riverine TA end-members vary significantly both regionally and withsmall changes in near-surface depths, highlighting the importance of carefulsurface water sampling in highly stratified waters. In an along-shoretransect, large increases in subsurface DIC are accompanied by equivalentdecreases in δ13CDIC with no discernable change in TA,indicating a respiratory DIC production on the order of 100 µmol kg−1 DIC during deep water circulation around the bay

Inorganic carbon cycling and biogeochemical processes in an Arctic inland sea (Hudson Bay)