FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3203420432> ?p ?o ?g. }

• W3203420432 endingPage "104975" @default.
• W3203420432 startingPage "104975" @default.
• W3203420432 abstract "In this study we present projected changes in the Eastern Bering Sea shelf (EBS) biophysical processes in response to climate forcing scenarios from the Coupled Model Intercomparison Phase 6 (CMIP6). These changes are obtained by dynamical downscaling using a Bering Sea regional model. Surface atmospheric and ocean boundary forcing from three Earth System Models (ESMs) in CMIP6, and a low and a high emission scenario of Shared Socioeconomic Pathway (SSP126 and SSP585) of each of the ESMs are considered. Ensemble mean results suggest that, contrary to an anticipated increase in ocean stratification under warming, diminishing ice cover in response to climate forcing and resultant reduced surface freshening weakens EBS stratification in the melt season. Modeled ensemble mean phytoplankton and zooplankton biomass on the EBS exhibits subsurface maxima during the growing season; the amplitude of these maxima decreases with warming, along with a reduction in primary productivity and oxygen concentration over much of the EBS water column. Phenology of both phytoplankton and zooplankton biomass on the EBS shifts earlier, leading to an increase (decrease) in biomass averaged between April–July (August–November), while annually averaged biomass decreases under warming. Projected changes of primary and secondary plankton biomass at the end of the 21st century are not well separated between the SSP126 and SSP585 scenario in light of the large across model spread under each scenario. The projected ensemble mean warming amplitude of the EBS summer bottom temperature is largely unchanged between results forced by the Coupled Model Intercomparison Phase 5 Representative Concentration Pathway 8.5 (CMIP5 RCP8.5) and CMIP6 SSP585 scenarios. Likewise, the reduction rate of annual mean phytoplankton and large zooplankton biomass are comparable between RCP8.5 and SSP585 projections, even though the absolute amplitudes of biomass are sensitive to modeling parameters such as the solar irradiance attenuation curve. Hence, within the Bering Sea dynamical downscaling framework, projected long-term warming trends in EBS bottom temperature and plankton biomass reduction rates are robust responses to climate forcing." @default.
• W3203420432 created "2021-10-11" @default.
• W3203420432 creator A5022308549 @default.
• W3203420432 creator A5026274765 @default.
• W3203420432 creator A5027553933 @default.
• W3203420432 creator A5045926279 @default.
• W3203420432 creator A5067734640 @default.
• W3203420432 creator A5073852205 @default.
• W3203420432 creator A5078801706 @default.
• W3203420432 creator A5084425301 @default.
• W3203420432 date "2021-11-01" @default.
• W3203420432 modified "2023-09-26" @default.
• W3203420432 title "Eastern Bering Sea shelf environmental and lower trophic level responses to climate forcing: Results of dynamical downscaling from CMIP6" @default.
• W3203420432 cites W1192405041 @default.
• W3203420432 cites W1479924536 @default.
• W3203420432 cites W1964308073 @default.
• W3203420432 cites W1970631800 @default.
• W3203420432 cites W1973233492 @default.
• W3203420432 cites W1975360915 @default.
• W3203420432 cites W1980925557 @default.
• W3203420432 cites W1996653992 @default.
• W3203420432 cites W2004551471 @default.
• W3203420432 cites W2007583931 @default.
• W3203420432 cites W2021780037 @default.
• W3203420432 cites W2030053119 @default.
• W3203420432 cites W2032114743 @default.
• W3203420432 cites W2040160302 @default.
• W3203420432 cites W2047599526 @default.
• W3203420432 cites W2063930866 @default.
• W3203420432 cites W2066305270 @default.
• W3203420432 cites W2067814097 @default.
• W3203420432 cites W2069384562 @default.
• W3203420432 cites W2070333780 @default.
• W3203420432 cites W2073389607 @default.
• W3203420432 cites W2104345346 @default.
• W3203420432 cites W2104626677 @default.
• W3203420432 cites W2123944661 @default.
• W3203420432 cites W2125634634 @default.
• W3203420432 cites W2127811724 @default.
• W3203420432 cites W2128112802 @default.
• W3203420432 cites W2141707502 @default.
• W3203420432 cites W2142037275 @default.
• W3203420432 cites W2163323074 @default.
• W3203420432 cites W2193139599 @default.
• W3203420432 cites W2193503481 @default.
• W3203420432 cites W2195624566 @default.
• W3203420432 cites W2337225114 @default.
• W3203420432 cites W2504294470 @default.
• W3203420432 cites W2516269908 @default.
• W3203420432 cites W2760562574 @default.
• W3203420432 cites W2762984108 @default.
• W3203420432 cites W2900131078 @default.
• W3203420432 cites W2901023271 @default.
• W3203420432 cites W2909634955 @default.
• W3203420432 cites W2968605318 @default.
• W3203420432 cites W2969805903 @default.
• W3203420432 cites W2977849507 @default.
• W3203420432 cites W2998500935 @default.
• W3203420432 cites W2998885490 @default.
• W3203420432 cites W2999300534 @default.
• W3203420432 cites W3012019457 @default.
• W3203420432 cites W3024077375 @default.
• W3203420432 cites W3035749668 @default.
• W3203420432 cites W3040588293 @default.
• W3203420432 cites W3048932873 @default.
• W3203420432 cites W3058227715 @default.
• W3203420432 cites W3080366116 @default.
• W3203420432 cites W3084792728 @default.
• W3203420432 cites W3173877905 @default.
• W3203420432 cites W3206345888 @default.
• W3203420432 cites W4242990314 @default.
• W3203420432 doi "https://doi.org/10.1016/j.dsr2.2021.104975" @default.
• W3203420432 hasPublicationYear "2021" @default.
• W3203420432 type Work @default.
• W3203420432 sameAs 3203420432 @default.
• W3203420432 citedByCount "4" @default.
• W3203420432 countsByYear W32034204322022 @default.
• W3203420432 countsByYear W32034204322023 @default.
• W3203420432 crossrefType "journal-article" @default.
• W3203420432 hasAuthorship W3203420432A5022308549 @default.
• W3203420432 hasAuthorship W3203420432A5026274765 @default.
• W3203420432 hasAuthorship W3203420432A5027553933 @default.
• W3203420432 hasAuthorship W3203420432A5045926279 @default.
• W3203420432 hasAuthorship W3203420432A5067734640 @default.
• W3203420432 hasAuthorship W3203420432A5073852205 @default.
• W3203420432 hasAuthorship W3203420432A5078801706 @default.
• W3203420432 hasAuthorship W3203420432A5084425301 @default.
• W3203420432 hasBestOaLocation W32034204321 @default.
• W3203420432 hasConcept C100701293 @default.
• W3203420432 hasConcept C108469399 @default.
• W3203420432 hasConcept C111368507 @default.
• W3203420432 hasConcept C115343472 @default.
• W3203420432 hasConcept C122846477 @default.
• W3203420432 hasConcept C127313418 @default.
• W3203420432 hasConcept C132651083 @default.
• W3203420432 hasConcept C134097258 @default.
• W3203420432 hasConcept C142796444 @default.
• W3203420432 hasConcept C158836135 @default.

• next