FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2036690020> ?p ?o ?g. }

• W2036690020 abstract "[1] While isotope records from ice cores are known to reflect temperature, this must be associated with zonally symmetric circulation. A new conceptual depiction of the isotopic cycling is established by considering the overturning circulation in isentropic coordinates. In this depiction, poleward transport of air and water vapor is non-diffusive, in a way that is similar to that depicted by Rayleigh models. However, the equatorward return flow is also important since it is this which is supplied with water by surface evaporation. The isotopic state emerges as a balance between evaporative supply and poleward advection, and removes the need to assume some initial source condition for an open distillation. Model experiments that simulate a wide range of circulation strengths show the isotopic composition of Antarctic snow is strongly linked to the strength of midlatitude (eddy driven) circulation, which in turn is driven by meridional temperature differences. Antarctic isotopes are largely independent of the tropical (Hadley) circulation because the rate of advective transport from the tropics to the polar region exceeds the rate at which surface sources replenish the poleward moving air stream. Across all simulations and between seasons, the relationship between δ18O in Antarctica above 1500 m and local surface air temperature is found to be remarkably robust at around 0.69‰/K in winter, 0.85‰/K in summer and with a seasonal slope of 0.60‰/K. Because these slopes result from changes in circulation, isotope records from the continent interior can be considered indicative of the history of overturning circulation." @default.
• W2036690020 created "2016-06-24" @default.
• W2036690020 creator A5014595026 @default.
• W2036690020 date "2008-02-19" @default.
• W2036690020 modified "2023-10-09" @default.
• W2036690020 title "The influence of midlatitude and tropical overturning circulation on the isotopic composition of atmospheric water vapor and Antarctic precipitation" @default.
• W2036690020 cites W1523048426 @default.
• W2036690020 cites W1551670230 @default.
• W2036690020 cites W1800256646 @default.
• W2036690020 cites W1966282214 @default.
• W2036690020 cites W1966715393 @default.
• W2036690020 cites W1976190405 @default.
• W2036690020 cites W1980673006 @default.
• W2036690020 cites W1992131528 @default.
• W2036690020 cites W1994981206 @default.
• W2036690020 cites W1997110993 @default.
• W2036690020 cites W1999433668 @default.
• W2036690020 cites W2001532020 @default.
• W2036690020 cites W2003318865 @default.
• W2036690020 cites W2007074215 @default.
• W2036690020 cites W2008729862 @default.
• W2036690020 cites W2017369899 @default.
• W2036690020 cites W2030473815 @default.
• W2036690020 cites W2031492422 @default.
• W2036690020 cites W2032143062 @default.
• W2036690020 cites W2033474054 @default.
• W2036690020 cites W2036711636 @default.
• W2036690020 cites W2059584513 @default.
• W2036690020 cites W2061350806 @default.
• W2036690020 cites W2065094221 @default.
• W2036690020 cites W2065161282 @default.
• W2036690020 cites W2075895046 @default.
• W2036690020 cites W2094845868 @default.
• W2036690020 cites W2098812404 @default.
• W2036690020 cites W2121051459 @default.
• W2036690020 cites W2122511023 @default.
• W2036690020 cites W2124143154 @default.
• W2036690020 cites W2129629920 @default.
• W2036690020 cites W2140744076 @default.
• W2036690020 cites W2143733309 @default.
• W2036690020 cites W2147783720 @default.
• W2036690020 cites W2150808612 @default.
• W2036690020 cites W2152854884 @default.
• W2036690020 cites W2155905859 @default.
• W2036690020 cites W2155951929 @default.
• W2036690020 cites W2156599179 @default.
• W2036690020 cites W2159322951 @default.
• W2036690020 cites W2164235511 @default.
• W2036690020 cites W2164810656 @default.
• W2036690020 cites W2173693605 @default.
• W2036690020 cites W2173716148 @default.
• W2036690020 cites W2213305380 @default.
• W2036690020 cites W265413368 @default.
• W2036690020 cites W311727958 @default.
• W2036690020 cites W4232473186 @default.
• W2036690020 cites W4235935210 @default.
• W2036690020 cites W4240540686 @default.
• W2036690020 cites W4248948983 @default.
• W2036690020 cites W4256468369 @default.
• W2036690020 doi "https://doi.org/10.1029/2007jd008892" @default.
• W2036690020 hasPublicationYear "2008" @default.
• W2036690020 type Work @default.
• W2036690020 sameAs 2036690020 @default.
• W2036690020 citedByCount "69" @default.
• W2036690020 countsByYear W20366900202012 @default.
• W2036690020 countsByYear W20366900202013 @default.
• W2036690020 countsByYear W20366900202014 @default.
• W2036690020 countsByYear W20366900202016 @default.
• W2036690020 countsByYear W20366900202017 @default.
• W2036690020 countsByYear W20366900202018 @default.
• W2036690020 countsByYear W20366900202019 @default.
• W2036690020 countsByYear W20366900202020 @default.
• W2036690020 countsByYear W20366900202021 @default.
• W2036690020 countsByYear W20366900202022 @default.
• W2036690020 countsByYear W20366900202023 @default.
• W2036690020 crossrefType "journal-article" @default.
• W2036690020 hasAuthorship W2036690020A5014595026 @default.
• W2036690020 hasBestOaLocation W20366900201 @default.
• W2036690020 hasConcept C111368507 @default.
• W2036690020 hasConcept C121332964 @default.
• W2036690020 hasConcept C127313418 @default.
• W2036690020 hasConcept C132651083 @default.
• W2036690020 hasConcept C141452985 @default.
• W2036690020 hasConcept C147534773 @default.
• W2036690020 hasConcept C150284090 @default.
• W2036690020 hasConcept C153294291 @default.
• W2036690020 hasConcept C18629457 @default.
• W2036690020 hasConcept C39432304 @default.
• W2036690020 hasConcept C49204034 @default.
• W2036690020 hasConcept C5072599 @default.
• W2036690020 hasConcept C91586092 @default.
• W2036690020 hasConcept C97355855 @default.
• W2036690020 hasConceptScore W2036690020C111368507 @default.
• W2036690020 hasConceptScore W2036690020C121332964 @default.
• W2036690020 hasConceptScore W2036690020C127313418 @default.
• W2036690020 hasConceptScore W2036690020C132651083 @default.
• W2036690020 hasConceptScore W2036690020C141452985 @default.
• W2036690020 hasConceptScore W2036690020C147534773 @default.
• W2036690020 hasConceptScore W2036690020C150284090 @default.
• W2036690020 hasConceptScore W2036690020C153294291 @default.

• next