FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2029296939> ?p ?o ?g. }

• W2029296939 abstract "[1] The impact of the atmospheric forcing on the winter ocean convection in the Mediterranean Sea was studied with a high-resolution ocean general circulation model. The major areas of focus are the Levantine basin, the Aegean-Cretan Sea, the Adriatic Sea, and the Gulf of Lion. Two companion simulations differing by the horizontal resolution of the atmospheric forcing were compared. The first simulation (MED16-ERA40) was forced by air-sea fields from ERA40, which is the ECMWF reanalysis. The second simulation (MED16-ECMWF) was forced by the ECMWF-analyzed surface fields that have a horizontal resolution twice as high as those of ERA40. The analysis of the standard deviations of the atmospheric fields shows that increasing the resolution of the atmospheric forcing leads in all regions to a better channeling of the winds by mountains and to the generation of atmospheric mesoscale patterns. Comparing the companion ocean simulation results with available observations in the Adriatic Sea and in the Gulf of Lion shows that MED16-ECMWF is more realistic than MED16-ERA40. In the eastern Mediterranean, although deep water formation occurs in the two experiments, the depth reached by the convection is deeper in MED16-ECMWF. In the Gulf of Lion, deep water formation occurs only in MED16-ECMWF. This larger sensitivity of the western Mediterranean convection to the forcing resolution is investigated by running a set of sensitivity experiments to analyze the impact of different time-space resolutions of the forcing on the intense winter convection event in winter 1998–1999. The sensitivity to the forcing appears to be mainly related to the effect of wind channeling by the land orography, which can only be reproduced in atmospheric models of sufficient resolution. Thus, well-positioned patterns of enhanced wind stress and ocean surface heat loss are able to maintain a vigorous gyre circulation favoring efficient preconditioning of the area at the beginning of winter and to drive realistic buoyancy loss and mixing responsible for strong convection at the end of winter." @default.
• W2029296939 created "2016-06-24" @default.
• W2029296939 creator A5015457320 @default.
• W2029296939 creator A5025010372 @default.
• W2029296939 creator A5026563721 @default.
• W2029296939 creator A5035621017 @default.
• W2029296939 creator A5041462382 @default.
• W2029296939 creator A5047277878 @default.
• W2029296939 creator A5077421764 @default.
• W2029296939 creator A5079453133 @default.
• W2029296939 creator A5081190838 @default.
• W2029296939 creator A5087344696 @default.
• W2029296939 date "2010-12-01" @default.
• W2029296939 modified "2023-10-15" @default.
• W2029296939 title "Impact of the spatial distribution of the atmospheric forcing on water mass formation in the Mediterranean Sea" @default.
• W2029296939 cites W1625444431 @default.
• W2029296939 cites W1975069371 @default.
• W2029296939 cites W1975776489 @default.
• W2029296939 cites W1976284326 @default.
• W2029296939 cites W1978093381 @default.
• W2029296939 cites W1980358177 @default.
• W2029296939 cites W2002942427 @default.
• W2029296939 cites W2003626279 @default.
• W2029296939 cites W2011939928 @default.
• W2029296939 cites W2013686371 @default.
• W2029296939 cites W2023585822 @default.
• W2029296939 cites W2026734904 @default.
• W2029296939 cites W2029471957 @default.
• W2029296939 cites W2030467288 @default.
• W2029296939 cites W2031461020 @default.
• W2029296939 cites W2038157101 @default.
• W2029296939 cites W2051867183 @default.
• W2029296939 cites W2055132216 @default.
• W2029296939 cites W2058479858 @default.
• W2029296939 cites W2060342943 @default.
• W2029296939 cites W2061835407 @default.
• W2029296939 cites W2068397569 @default.
• W2029296939 cites W2070496250 @default.
• W2029296939 cites W2074169447 @default.
• W2029296939 cites W2084806537 @default.
• W2029296939 cites W2089460342 @default.
• W2029296939 cites W2090249381 @default.
• W2029296939 cites W2094542249 @default.
• W2029296939 cites W2094746911 @default.
• W2029296939 cites W2120478110 @default.
• W2029296939 cites W2120867630 @default.
• W2029296939 cites W2140424451 @default.
• W2029296939 cites W2144056518 @default.
• W2029296939 cites W2171483221 @default.
• W2029296939 cites W2531133227 @default.
• W2029296939 cites W3004432981 @default.
• W2029296939 cites W97966767 @default.
• W2029296939 doi "https://doi.org/10.1029/2009jc005648" @default.
• W2029296939 hasPublicationYear "2010" @default.
• W2029296939 type Work @default.
• W2029296939 sameAs 2029296939 @default.
• W2029296939 citedByCount "65" @default.
• W2029296939 countsByYear W20292969392012 @default.
• W2029296939 countsByYear W20292969392013 @default.
• W2029296939 countsByYear W20292969392014 @default.
• W2029296939 countsByYear W20292969392015 @default.
• W2029296939 countsByYear W20292969392016 @default.
• W2029296939 countsByYear W20292969392017 @default.
• W2029296939 countsByYear W20292969392018 @default.
• W2029296939 countsByYear W20292969392019 @default.
• W2029296939 countsByYear W20292969392020 @default.
• W2029296939 countsByYear W20292969392021 @default.
• W2029296939 countsByYear W20292969392022 @default.
• W2029296939 countsByYear W20292969392023 @default.
• W2029296939 crossrefType "journal-article" @default.
• W2029296939 hasAuthorship W2029296939A5015457320 @default.
• W2029296939 hasAuthorship W2029296939A5025010372 @default.
• W2029296939 hasAuthorship W2029296939A5026563721 @default.
• W2029296939 hasAuthorship W2029296939A5035621017 @default.
• W2029296939 hasAuthorship W2029296939A5041462382 @default.
• W2029296939 hasAuthorship W2029296939A5047277878 @default.
• W2029296939 hasAuthorship W2029296939A5077421764 @default.
• W2029296939 hasAuthorship W2029296939A5079453133 @default.
• W2029296939 hasAuthorship W2029296939A5081190838 @default.
• W2029296939 hasAuthorship W2029296939A5087344696 @default.
• W2029296939 hasBestOaLocation W20292969391 @default.
• W2029296939 hasConcept C10899652 @default.
• W2029296939 hasConcept C109007969 @default.
• W2029296939 hasConcept C111368507 @default.
• W2029296939 hasConcept C118365302 @default.
• W2029296939 hasConcept C127313418 @default.
• W2029296939 hasConcept C140302290 @default.
• W2029296939 hasConcept C151730666 @default.
• W2029296939 hasConcept C153294291 @default.
• W2029296939 hasConcept C166957645 @default.
• W2029296939 hasConcept C197115733 @default.
• W2029296939 hasConcept C205649164 @default.
• W2029296939 hasConcept C2779043415 @default.
• W2029296939 hasConcept C39432304 @default.
• W2029296939 hasConcept C40382383 @default.
• W2029296939 hasConcept C4646841 @default.
• W2029296939 hasConcept C49204034 @default.
• W2029296939 hasConcept C91586092 @default.
• W2029296939 hasConceptScore W2029296939C10899652 @default.
• W2029296939 hasConceptScore W2029296939C109007969 @default.

• next