FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2054754950> ?p ?o ?g. }

• W2054754950 endingPage "878" @default.
• W2054754950 startingPage "843" @default.
• W2054754950 abstract "Seasonal data for pCO 2 and the concentrations of CO 2 and nutrients in high‐latitude surface oceans obtained by the Lamont‐Doherty CO 2 group and Marine Research Institute, Reykjavik, are presented and analyzed. The seasonal progression and relationships between these properties are described, and their inter‐ocean variation is compared. Spring phytoplankton blooms in the surface water of the North Atlantic Ocean and Iceland Sea caused a precipitous reduction of surface water pCO 2 and the concentrations of CO 2 and nutrients within two weeks, and proceeded until the nutrient salts were exhausted. This type of seasonal behavior is limited to the high‐latitude (north of approximately 40°N) North Atlantic Ocean and adjoining seas. In contrast, seasonal changes in CO 2 and nutrients were more gradual in the North Pacific and the nutrients were only partially consumed in the surface waters of the subarctic North Pacific Ocean and Southern Ocean. The magnitude of seasonal changes in nutrient concentrations in the North Pacific and Southern Oceans was similar to that observed in the North Atlantic and adjoining seas. In the subpolar and polar waters of the North and South Atlantic and North Pacific Oceans, pCO 2 and the concentrations Of CO 2 and nutrients were much higher during winter than summer. During winter, the high latitude areas of the North Atlantic, North Pacific, and Weddell Sea were sources for atmospheric CO 2 ; during summer, they became CO 2 sinks. This is attributed to the upwelling of deep waters rich in CO 2 and nutrients during winter, and the intense photosynthesis occurring in strongly stratified upper layers during summer. On the other hand, subtropical waters were a CO 2 source in summer and a sink in winter. Since these waters were depleted of nutrients and could only sustain low levels of primary production, the seasonal variation of pCO 2 in subtropical waters and the CO 2 sink/source condition were governed primarily by temperature. An intense CO 2 sink zone was found along the confluence of the subtropical and subpolar waters (or the subtropical convergence). Its formation is attributed to the combined effects of cooling in subtropical waters and photosynthetic drawdown of CO 2 in subpolar waters." @default.
• W2054754950 created "2016-06-24" @default.
• W2054754950 creator A5003234164 @default.
• W2054754950 creator A5012096760 @default.
• W2054754950 creator A5056628802 @default.
• W2054754950 creator A5075338570 @default.
• W2054754950 creator A5087867347 @default.
• W2054754950 date "1993-12-01" @default.
• W2054754950 modified "2023-10-10" @default.
• W2054754950 title "Seasonal variation of CO₂ and nutrients in the high‐latitude surface oceans: A comparative study" @default.
• W2054754950 cites W1503478730 @default.
• W2054754950 cites W1516684646 @default.
• W2054754950 cites W1584048389 @default.
• W2054754950 cites W1644379584 @default.
• W2054754950 cites W1963851862 @default.
• W2054754950 cites W1976628086 @default.
• W2054754950 cites W1997219061 @default.
• W2054754950 cites W2014641666 @default.
• W2054754950 cites W2018516735 @default.
• W2054754950 cites W2019254993 @default.
• W2054754950 cites W2028075627 @default.
• W2054754950 cites W2028344926 @default.
• W2054754950 cites W2029254108 @default.
• W2054754950 cites W2030098873 @default.
• W2054754950 cites W2031815256 @default.
• W2054754950 cites W2034739718 @default.
• W2054754950 cites W2043177704 @default.
• W2054754950 cites W2048638736 @default.
• W2054754950 cites W2058433393 @default.
• W2054754950 cites W2073721556 @default.
• W2054754950 cites W2074247901 @default.
• W2054754950 cites W2076879941 @default.
• W2054754950 cites W2092092007 @default.
• W2054754950 cites W2095051466 @default.
• W2054754950 cites W2101131858 @default.
• W2054754950 cites W2109364530 @default.
• W2054754950 cites W2125776675 @default.
• W2054754950 cites W2155410124 @default.
• W2054754950 cites W3207181308 @default.
• W2054754950 cites W4233649882 @default.
• W2054754950 cites W4246647555 @default.
• W2054754950 doi "https://doi.org/10.1029/93gb02263" @default.
• W2054754950 hasPublicationYear "1993" @default.
• W2054754950 type Work @default.
• W2054754950 sameAs 2054754950 @default.
• W2054754950 citedByCount "932" @default.
• W2054754950 countsByYear W20547549502012 @default.
• W2054754950 countsByYear W20547549502013 @default.
• W2054754950 countsByYear W20547549502014 @default.
• W2054754950 countsByYear W20547549502015 @default.
• W2054754950 countsByYear W20547549502016 @default.
• W2054754950 countsByYear W20547549502017 @default.
• W2054754950 countsByYear W20547549502018 @default.
• W2054754950 countsByYear W20547549502019 @default.
• W2054754950 countsByYear W20547549502020 @default.
• W2054754950 countsByYear W20547549502021 @default.
• W2054754950 countsByYear W20547549502022 @default.
• W2054754950 countsByYear W20547549502023 @default.
• W2054754950 crossrefType "journal-article" @default.
• W2054754950 hasAuthorship W2054754950A5003234164 @default.
• W2054754950 hasAuthorship W2054754950A5012096760 @default.
• W2054754950 hasAuthorship W2054754950A5056628802 @default.
• W2054754950 hasAuthorship W2054754950A5075338570 @default.
• W2054754950 hasAuthorship W2054754950A5087867347 @default.
• W2054754950 hasConcept C111368507 @default.
• W2054754950 hasConcept C122523270 @default.
• W2054754950 hasConcept C125403950 @default.
• W2054754950 hasConcept C127313418 @default.
• W2054754950 hasConcept C13280743 @default.
• W2054754950 hasConcept C140302290 @default.
• W2054754950 hasConcept C142796444 @default.
• W2054754950 hasConcept C149348798 @default.
• W2054754950 hasConcept C18903297 @default.
• W2054754950 hasConcept C2780892065 @default.
• W2054754950 hasConcept C39432304 @default.
• W2054754950 hasConcept C39665741 @default.
• W2054754950 hasConcept C81447805 @default.
• W2054754950 hasConcept C83133772 @default.
• W2054754950 hasConcept C8625798 @default.
• W2054754950 hasConcept C86803240 @default.
• W2054754950 hasConcept C87717796 @default.
• W2054754950 hasConceptScore W2054754950C111368507 @default.
• W2054754950 hasConceptScore W2054754950C122523270 @default.
• W2054754950 hasConceptScore W2054754950C125403950 @default.
• W2054754950 hasConceptScore W2054754950C127313418 @default.
• W2054754950 hasConceptScore W2054754950C13280743 @default.
• W2054754950 hasConceptScore W2054754950C140302290 @default.
• W2054754950 hasConceptScore W2054754950C142796444 @default.
• W2054754950 hasConceptScore W2054754950C149348798 @default.
• W2054754950 hasConceptScore W2054754950C18903297 @default.
• W2054754950 hasConceptScore W2054754950C2780892065 @default.
• W2054754950 hasConceptScore W2054754950C39432304 @default.
• W2054754950 hasConceptScore W2054754950C39665741 @default.
• W2054754950 hasConceptScore W2054754950C81447805 @default.
• W2054754950 hasConceptScore W2054754950C83133772 @default.
• W2054754950 hasConceptScore W2054754950C8625798 @default.
• W2054754950 hasConceptScore W2054754950C86803240 @default.
• W2054754950 hasConceptScore W2054754950C87717796 @default.

• next