FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2783271523> ?p ?o ?g. }

• W2783271523 endingPage "10" @default.
• W2783271523 startingPage "1" @default.
• W2783271523 abstract "The partial pressure of CO2 in surface water (pCO2sw) measured within the Canadian Arctic Archipelago (CAA) and Baffin Bay was highly variable with values ranging from strongly undersaturated (118 µatm) to slightly supersaturated (419 µatm) with respect to the atmospheric levels (~386 μatm) during summer and autumn 2011. During summer, melting sea ice contributed to cold and fresh surface water and enhanced the ice-edge bloom, resulting in strong pCO2sw undersaturation. Coronation Gulf was the only area with supersaturated pCO2sw, likely due to warm CO2-enriched freshwater input from the Coppermine River. During autumn, the entire CAA (including Coronation Gulf) was undersaturated, despite generally increasing pCO2sw. Coronation Gulf was the one place where pCO2sw decreased, likely due to seasonal reduction in discharge from the Coppermine River and the decreasing sea surface temperature. The seasonal summer-to-autumn increase in pCO2sw across the archipelago is attributed in part to the continuous uptake of atmospheric CO2 through both summer and autumn and to the seasonal deepening of the surface mixed layer, bringing CO2-rich waters to the surface. These observations demonstrate how freshwater from sea ice melt and rivers affect pCO2sw differently. The general pCO2sw undersaturation during summer-autumn 2011 throughout the CAA and Baffin Bay give an estimated net oceanic sink for atmospheric CO2 over the study period of 11.4 mmol CO2 m−2 d−1, assuming no sea-air CO2 flux exchange across the sea-ice covered areas." @default.
• W2783271523 created "2018-01-26" @default.
• W2783271523 creator A5024271329 @default.
• W2783271523 creator A5027045277 @default.
• W2783271523 creator A5030729455 @default.
• W2783271523 creator A5037384896 @default.
• W2783271523 creator A5045074908 @default.
• W2783271523 creator A5053310197 @default.
• W2783271523 creator A5066947319 @default.
• W2783271523 creator A5076110163 @default.
• W2783271523 creator A5080810978 @default.
• W2783271523 creator A5087722620 @default.
• W2783271523 date "2018-03-01" @default.
• W2783271523 modified "2023-09-27" @default.
• W2783271523 title "Spatial and temporal variability of seawater pCO2 within the Canadian Arctic Archipelago and Baffin Bay during the summer and autumn 2011" @default.
• W2783271523 cites W1524738791 @default.
• W2783271523 cites W1530628957 @default.
• W2783271523 cites W1547681715 @default.
• W2783271523 cites W1550108143 @default.
• W2783271523 cites W1550911434 @default.
• W2783271523 cites W1562201821 @default.
• W2783271523 cites W1600897084 @default.
• W2783271523 cites W1627787412 @default.
• W2783271523 cites W1742743498 @default.
• W2783271523 cites W1878965460 @default.
• W2783271523 cites W1928512854 @default.
• W2783271523 cites W1936193285 @default.
• W2783271523 cites W1960586518 @default.
• W2783271523 cites W1965624816 @default.
• W2783271523 cites W1968973672 @default.
• W2783271523 cites W1975343289 @default.
• W2783271523 cites W1983747596 @default.
• W2783271523 cites W1991448376 @default.
• W2783271523 cites W1995329629 @default.
• W2783271523 cites W1999773550 @default.
• W2783271523 cites W2009925919 @default.
• W2783271523 cites W2010122553 @default.
• W2783271523 cites W2018516735 @default.
• W2783271523 cites W2019753174 @default.
• W2783271523 cites W2020361195 @default.
• W2783271523 cites W2024417959 @default.
• W2783271523 cites W2030348009 @default.
• W2783271523 cites W2030604405 @default.
• W2783271523 cites W2039735622 @default.
• W2783271523 cites W2047175623 @default.
• W2783271523 cites W2051460181 @default.
• W2783271523 cites W2054754950 @default.
• W2783271523 cites W2055198031 @default.
• W2783271523 cites W2067081409 @default.
• W2783271523 cites W2074565009 @default.
• W2783271523 cites W2079240018 @default.
• W2783271523 cites W2086674830 @default.
• W2783271523 cites W2090470557 @default.
• W2783271523 cites W2094425331 @default.
• W2783271523 cites W2094510745 @default.
• W2783271523 cites W2098226271 @default.
• W2783271523 cites W2109672953 @default.
• W2783271523 cites W2110492323 @default.
• W2783271523 cites W2111167715 @default.
• W2783271523 cites W2112582491 @default.
• W2783271523 cites W2117194284 @default.
• W2783271523 cites W2118659175 @default.
• W2783271523 cites W2123376261 @default.
• W2783271523 cites W2125776675 @default.
• W2783271523 cites W2125905259 @default.
• W2783271523 cites W2131250175 @default.
• W2783271523 cites W2142193430 @default.
• W2783271523 cites W2144366724 @default.
• W2783271523 cites W2147271764 @default.
• W2783271523 cites W2148944925 @default.
• W2783271523 cites W2149705278 @default.
• W2783271523 cites W2151209927 @default.
• W2783271523 cites W2161454991 @default.
• W2783271523 cites W2162966874 @default.
• W2783271523 cites W2239313876 @default.
• W2783271523 cites W2259406178 @default.
• W2783271523 cites W2287584321 @default.
• W2783271523 cites W4245608973 @default.
• W2783271523 cites W4251198235 @default.
• W2783271523 doi "https://doi.org/10.1016/j.csr.2018.01.006" @default.
• W2783271523 hasPublicationYear "2018" @default.
• W2783271523 type Work @default.
• W2783271523 sameAs 2783271523 @default.
• W2783271523 citedByCount "8" @default.
• W2783271523 countsByYear W27832715232019 @default.
• W2783271523 countsByYear W27832715232020 @default.
• W2783271523 countsByYear W27832715232022 @default.
• W2783271523 countsByYear W27832715232023 @default.
• W2783271523 crossrefType "journal-article" @default.
• W2783271523 hasAuthorship W2783271523A5024271329 @default.
• W2783271523 hasAuthorship W2783271523A5027045277 @default.
• W2783271523 hasAuthorship W2783271523A5030729455 @default.
• W2783271523 hasAuthorship W2783271523A5037384896 @default.
• W2783271523 hasAuthorship W2783271523A5045074908 @default.
• W2783271523 hasAuthorship W2783271523A5053310197 @default.
• W2783271523 hasAuthorship W2783271523A5066947319 @default.
• W2783271523 hasAuthorship W2783271523A5076110163 @default.
• W2783271523 hasAuthorship W2783271523A5080810978 @default.

• next