FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4380866460> ?p ?o ?g. }

• W4380866460 endingPage "108152" @default.
• W4380866460 startingPage "108152" @default.
• W4380866460 abstract "The Last Interglacial (LIG) experienced substantial changes in seasonal insolation compared with the present day, which may have affected the hydrography and water-mass exchange in the North Sea and Baltic Sea region. Here we investigate the effects of solar radiation and greenhouse gas (GHG) forcing on the regional climate by analyzing model simulations of the LIG (127 ka BP), pre-industrial (PI, 1850 CE), and present-day (PD, 1990 CE) climates. We also interpret the reconstructed seasonal bottom water conditions using benthic foraminifera and geochemistry data. Our simulations reveal that during the LIG, the Baltic Sea region (including the Kattegat and the Danish Straits) experienced more saline and colder bottom waters than those in the PD, in agreement with the reconstruction data. This can be attributed to lower GHG levels and enhanced water exchange of cooler, saline North Sea water into the Baltic Sea during the LIG. The thermocline was stronger during the summer months in the LIG, mainly due to the higher sea surface temperature (SST) compared to that of the PD resulting from increased summer insolation. Further, the temperature anomalies (LIG–PD) show significant inverse correlations with the precipitation–minus–evaporation (P–E) at the Baltic Sea entrance. However, the P–E balance appears to have had minimal impact on salinity changes in the North Sea, the Baltic Proper, and the open sea area. Our findings indicate that monthly surface and bottom water salinity anomalies of LIG-PI exhibit strong positive correlations with the North Atlantic Oscillation (NAO) anomalies in the Baltic entrance region. During the LIG, a more positive phase of the NAO index in autumn played a crucial role in wind-driven major inflows and led to more intensive water exchange in the North Sea–Baltic Sea region compared to the late Holocene." @default.
• W4380866460 created "2023-06-16" @default.
• W4380866460 creator A5028290542 @default.
• W4380866460 creator A5036484370 @default.
• W4380866460 creator A5037898520 @default.
• W4380866460 creator A5040282662 @default.
• W4380866460 creator A5058645318 @default.
• W4380866460 creator A5062624455 @default.
• W4380866460 creator A5078830084 @default.
• W4380866460 date "2023-07-01" @default.
• W4380866460 modified "2023-09-26" @default.
• W4380866460 title "Last interglacial seasonal hydroclimate in the North Sea–Baltic Sea region" @default.
• W4380866460 cites W1510944435 @default.
• W4380866460 cites W1608751539 @default.
• W4380866460 cites W1970315054 @default.
• W4380866460 cites W1972925337 @default.
• W4380866460 cites W1981102897 @default.
• W4380866460 cites W1986927488 @default.
• W4380866460 cites W1999641222 @default.
• W4380866460 cites W2000444336 @default.
• W4380866460 cites W2006262369 @default.
• W4380866460 cites W2013878295 @default.
• W4380866460 cites W2016129638 @default.
• W4380866460 cites W2016508847 @default.
• W4380866460 cites W2016824727 @default.
• W4380866460 cites W2020733016 @default.
• W4380866460 cites W2024066884 @default.
• W4380866460 cites W2029868252 @default.
• W4380866460 cites W2033530520 @default.
• W4380866460 cites W2035378323 @default.
• W4380866460 cites W2041371274 @default.
• W4380866460 cites W2045798746 @default.
• W4380866460 cites W2060977891 @default.
• W4380866460 cites W2066248944 @default.
• W4380866460 cites W2069469030 @default.
• W4380866460 cites W2082130975 @default.
• W4380866460 cites W2088206730 @default.
• W4380866460 cites W2088370188 @default.
• W4380866460 cites W2090756614 @default.
• W4380866460 cites W2096727849 @default.
• W4380866460 cites W2131477567 @default.
• W4380866460 cites W2135968678 @default.
• W4380866460 cites W2139629354 @default.
• W4380866460 cites W2140477756 @default.
• W4380866460 cites W2158794107 @default.
• W4380866460 cites W2160908174 @default.
• W4380866460 cites W2163211095 @default.
• W4380866460 cites W2472727018 @default.
• W4380866460 cites W2505673590 @default.
• W4380866460 cites W2556872521 @default.
• W4380866460 cites W2557951249 @default.
• W4380866460 cites W2598283438 @default.
• W4380866460 cites W2883853161 @default.
• W4380866460 cites W2885251602 @default.
• W4380866460 cites W3082582251 @default.
• W4380866460 cites W3111663217 @default.
• W4380866460 cites W3123157889 @default.
• W4380866460 cites W3206002240 @default.
• W4380866460 cites W4226178852 @default.
• W4380866460 cites W4234701862 @default.
• W4380866460 cites W4247690047 @default.
• W4380866460 cites W4306293736 @default.
• W4380866460 cites W2036729241 @default.
• W4380866460 doi "https://doi.org/10.1016/j.quascirev.2023.108152" @default.
• W4380866460 hasPublicationYear "2023" @default.
• W4380866460 type Work @default.
• W4380866460 citedByCount "0" @default.
• W4380866460 crossrefType "journal-article" @default.
• W4380866460 hasAuthorship W4380866460A5028290542 @default.
• W4380866460 hasAuthorship W4380866460A5036484370 @default.
• W4380866460 hasAuthorship W4380866460A5037898520 @default.
• W4380866460 hasAuthorship W4380866460A5040282662 @default.
• W4380866460 hasAuthorship W4380866460A5058645318 @default.
• W4380866460 hasAuthorship W4380866460A5062624455 @default.
• W4380866460 hasAuthorship W4380866460A5078830084 @default.
• W4380866460 hasBestOaLocation W43808664601 @default.
• W4380866460 hasConcept C105824904 @default.
• W4380866460 hasConcept C111368507 @default.
• W4380866460 hasConcept C114793014 @default.
• W4380866460 hasConcept C127313418 @default.
• W4380866460 hasConcept C129513315 @default.
• W4380866460 hasConcept C134097258 @default.
• W4380866460 hasConcept C136894858 @default.
• W4380866460 hasConcept C140302290 @default.
• W4380866460 hasConcept C15739521 @default.
• W4380866460 hasConcept C17093552 @default.
• W4380866460 hasConcept C186240526 @default.
• W4380866460 hasConcept C2780275952 @default.
• W4380866460 hasConcept C2780368712 @default.
• W4380866460 hasConcept C39432304 @default.
• W4380866460 hasConcept C49204034 @default.
• W4380866460 hasConcept C76256466 @default.
• W4380866460 hasConcept C83042747 @default.
• W4380866460 hasConceptScore W4380866460C105824904 @default.
• W4380866460 hasConceptScore W4380866460C111368507 @default.
• W4380866460 hasConceptScore W4380866460C114793014 @default.
• W4380866460 hasConceptScore W4380866460C127313418 @default.
• W4380866460 hasConceptScore W4380866460C129513315 @default.

• next