FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2952165045> ?p ?o ?g. }

• W2952165045 abstract "Stratification of the water column, consisting of the three layers (upper, intermediate, and deep layer), is an important factor for the functioning of the brackish Baltic Sea. In the present work, changes in the vertical structure of temperature and salinity, as well as heat content, salt mass and stratification conditions were estimated on the basis of in-situ and remote sensing data in 1982-2016. The seasonal thermocline and the halocline have strengthened in most of the sea by a rate of 0.33 – 0.39 kg m-3 and 0.70 – 0.88 kg m-3, respectively, during 35 years. The upper layer has warmed by 0.03 – 0.06 °C year-1 and sub-halocline deep layer 0.04 – 0.06 °C year-1 in most of the sea. The total warming trend in the whole Baltic has been 1.07 °C for 35 years, being approximately twice higher compared to the upper 100 m in the Atlantic Ocean. Average upper layer warming of the sea from May to September has been 0.07 – 0.08 °C year-1 while in winter, trends were mostly statistically not significant. More rapid warming during summers has occurred in shallower, closed-end areas of gulfs. Possible reasons for high warming there might be shallow depths and limited water exchange, stronger stratification, and/or higher turbidity. Sea surface temperature trends estimated by in-situ and satellite data agree well. Trends of freshening (-0.005 to -0.014 g kg-1 year-1) of the upper layer and increasing salinity (0.02 to 0.04 g kg-1 year-1) in the sub-halocline deep layer were detected. Increased salinity in the deep layer is likely caused by the increased lateral import of saltier water from the North Sea. Changes in the upper layer salinity might not be related to the accumulated river runoff only, but decadal changes of vertical salt flux might also contribute. The vertically distinct changes cancel each other and no significant trend in the mean salinity of the Baltic Sea was detected. No remarkable changes have occurred in the cold intermediate layer. In conclusion, different dominating processes have caused distinct long-term trends in the three layers of the Baltic Sea." @default.
• W2952165045 created "2019-06-27" @default.
• W2952165045 creator A5008970655 @default.
• W2952165045 creator A5078013957 @default.
• W2952165045 date "2019-07-02" @default.
• W2952165045 modified "2023-10-10" @default.
• W2952165045 title "Stratification Has Strengthened in the Baltic Sea – An Analysis of 35 Years of Observational Data" @default.
• W2952165045 cites W1547207864 @default.
• W2952165045 cites W1548061610 @default.
• W2952165045 cites W1964403676 @default.
• W2952165045 cites W1966706331 @default.
• W2952165045 cites W1972465154 @default.
• W2952165045 cites W1981758507 @default.
• W2952165045 cites W1986927488 @default.
• W2952165045 cites W1987018305 @default.
• W2952165045 cites W1996206440 @default.
• W2952165045 cites W1999217751 @default.
• W2952165045 cites W1999666074 @default.
• W2952165045 cites W2003518895 @default.
• W2952165045 cites W2009691979 @default.
• W2952165045 cites W2018356981 @default.
• W2952165045 cites W2024895749 @default.
• W2952165045 cites W2027743198 @default.
• W2952165045 cites W2039647785 @default.
• W2952165045 cites W2053653343 @default.
• W2952165045 cites W2070137604 @default.
• W2952165045 cites W2072039498 @default.
• W2952165045 cites W2075665768 @default.
• W2952165045 cites W2083285598 @default.
• W2952165045 cites W2092351456 @default.
• W2952165045 cites W2093813915 @default.
• W2952165045 cites W2101875061 @default.
• W2952165045 cites W2125270372 @default.
• W2952165045 cites W2129847237 @default.
• W2952165045 cites W2151750351 @default.
• W2952165045 cites W2180542869 @default.
• W2952165045 cites W2241381421 @default.
• W2952165045 cites W2242457454 @default.
• W2952165045 cites W2271432601 @default.
• W2952165045 cites W2324965185 @default.
• W2952165045 cites W2331764059 @default.
• W2952165045 cites W2345100637 @default.
• W2952165045 cites W2478491076 @default.
• W2952165045 cites W249577657 @default.
• W2952165045 cites W2501416184 @default.
• W2952165045 cites W2506535885 @default.
• W2952165045 cites W2508480293 @default.
• W2952165045 cites W2529258801 @default.
• W2952165045 cites W2585202830 @default.
• W2952165045 cites W2779351554 @default.
• W2952165045 cites W2808538404 @default.
• W2952165045 cites W2861254206 @default.
• W2952165045 cites W2888638902 @default.
• W2952165045 cites W2891428028 @default.
• W2952165045 cites W2892942880 @default.
• W2952165045 cites W2894341745 @default.
• W2952165045 cites W2943913936 @default.
• W2952165045 cites W335755937 @default.
• W2952165045 cites W4247673353 @default.
• W2952165045 cites W96301576 @default.
• W2952165045 doi "https://doi.org/10.3389/feart.2019.00174" @default.
• W2952165045 hasPublicationYear "2019" @default.
• W2952165045 type Work @default.
• W2952165045 sameAs 2952165045 @default.
• W2952165045 citedByCount "38" @default.
• W2952165045 countsByYear W29521650452020 @default.
• W2952165045 countsByYear W29521650452021 @default.
• W2952165045 countsByYear W29521650452022 @default.
• W2952165045 countsByYear W29521650452023 @default.
• W2952165045 crossrefType "journal-article" @default.
• W2952165045 hasAuthorship W2952165045A5008970655 @default.
• W2952165045 hasAuthorship W2952165045A5078013957 @default.
• W2952165045 hasBestOaLocation W29521650451 @default.
• W2952165045 hasConcept C100701293 @default.
• W2952165045 hasConcept C105824904 @default.
• W2952165045 hasConcept C111368507 @default.
• W2952165045 hasConcept C118178180 @default.
• W2952165045 hasConcept C122120755 @default.
• W2952165045 hasConcept C122846477 @default.
• W2952165045 hasConcept C127313418 @default.
• W2952165045 hasConcept C129513315 @default.
• W2952165045 hasConcept C140302290 @default.
• W2952165045 hasConcept C192943249 @default.
• W2952165045 hasConcept C23715911 @default.
• W2952165045 hasConcept C3527866 @default.
• W2952165045 hasConcept C39432304 @default.
• W2952165045 hasConcept C49204034 @default.
• W2952165045 hasConcept C56905729 @default.
• W2952165045 hasConcept C59822182 @default.
• W2952165045 hasConcept C86803240 @default.
• W2952165045 hasConcept C88548481 @default.
• W2952165045 hasConceptScore W2952165045C100701293 @default.
• W2952165045 hasConceptScore W2952165045C105824904 @default.
• W2952165045 hasConceptScore W2952165045C111368507 @default.
• W2952165045 hasConceptScore W2952165045C118178180 @default.
• W2952165045 hasConceptScore W2952165045C122120755 @default.
• W2952165045 hasConceptScore W2952165045C122846477 @default.
• W2952165045 hasConceptScore W2952165045C127313418 @default.
• W2952165045 hasConceptScore W2952165045C129513315 @default.
• W2952165045 hasConceptScore W2952165045C140302290 @default.

• next