FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2079348778> ?p ?o ?g. }

• W2079348778 endingPage "30936" @default.
• W2079348778 startingPage "30913" @default.
• W2079348778 abstract "This paper deals with structure and processes in the marine boundary layer along air mass trajectories over and in the vicinity of the cold water tongue of the eastern equatorial Pacific Ocean. The study is based on three NASA P3-B aircraft missions from Guayaquil, Ecuador, part of the NASA Pacific Exploratory Mission-Tropics experiment. The observations were made during September 1996, which is part of the cold season when the lowest sea surface temperatures are expected. The boundary layer and the overlying free troposphere showed several unique features not observed previously. While the boundary layer was advected over the equatorial cold tongue toward the Intertropical Convergence Zone, the overlying free tropospheric air consisted of warm, moist outflow from the South American continent where deep convection was taking place. The specific humidity just above the inversion was typically I - 2 g kg -t higher than that in the boundary layer. These conditions tend to suppress cloud top radiative cooling and entrainment at the boundary layer top. Over the coldest upwelling areas, shallow thermal internal boundary layers were observed. We discuss changes in cloudiness, sensible and latent heat fluxes, and the scale of turbulence in and above the thermal internal boundary layers, and during the reestablishment of the convective boundary layer upon passing over a warmer sea surface. ularly during the cold season when, as will be shown, the MBL displays some rather unique characteristics, reflecting the influence of cold ocean upwelling and a warm, moist continental outflow in the overlying free troposphere. These observations provide a basis for un- derstanding transport and mixing of trace species, and the formation and dissipation of clouds in this area and season. Both of these topics have implications for cli- mate research. We focus on data from the NASA P3-B research air- craft collected during flights from Guayaquil, Ecuador. The area covered is adjacent to and SE of the area in- vestigated using dropwinsondes in the First Global At- mospheric Research Program (GARP) Global Experi-" @default.
• W2079348778 created "2016-06-24" @default.
• W2079348778 creator A5030927546 @default.
• W2079348778 creator A5033572817 @default.
• W2079348778 creator A5059923412 @default.
• W2079348778 creator A5063644921 @default.
• W2079348778 date "1999-12-01" @default.
• W2079348778 modified "2023-10-16" @default.
• W2079348778 title "Marine boundary layers associated with ocean upwelling over the eastern equatorial Pacific Ocean" @default.
• W2079348778 cites W1509809740 @default.
• W2079348778 cites W1583950957 @default.
• W2079348778 cites W1964530368 @default.
• W2079348778 cites W1971889977 @default.
• W2079348778 cites W1983749084 @default.
• W2079348778 cites W1988738832 @default.
• W2079348778 cites W1988885849 @default.
• W2079348778 cites W1991877017 @default.
• W2079348778 cites W2000966706 @default.
• W2079348778 cites W2005395958 @default.
• W2079348778 cites W2008295354 @default.
• W2079348778 cites W2009306433 @default.
• W2079348778 cites W2014835098 @default.
• W2079348778 cites W2019202783 @default.
• W2079348778 cites W2023578626 @default.
• W2079348778 cites W2025126822 @default.
• W2079348778 cites W2042300322 @default.
• W2079348778 cites W2043302424 @default.
• W2079348778 cites W2056663196 @default.
• W2079348778 cites W2059870106 @default.
• W2079348778 cites W2073095714 @default.
• W2079348778 cites W2075524397 @default.
• W2079348778 cites W2075651803 @default.
• W2079348778 cites W2075753993 @default.
• W2079348778 cites W2090156683 @default.
• W2079348778 cites W2100005957 @default.
• W2079348778 cites W2114388830 @default.
• W2079348778 cites W2121928891 @default.
• W2079348778 cites W2162945727 @default.
• W2079348778 cites W2172560200 @default.
• W2079348778 cites W2176500283 @default.
• W2079348778 cites W2176554644 @default.
• W2079348778 cites W2176648613 @default.
• W2079348778 cites W2177506136 @default.
• W2079348778 cites W2178245170 @default.
• W2079348778 cites W4245813121 @default.
• W2079348778 doi "https://doi.org/10.1029/1999jd900990" @default.
• W2079348778 hasPublicationYear "1999" @default.
• W2079348778 type Work @default.
• W2079348778 sameAs 2079348778 @default.
• W2079348778 citedByCount "11" @default.
• W2079348778 countsByYear W20793487782015 @default.
• W2079348778 countsByYear W20793487782023 @default.
• W2079348778 crossrefType "journal-article" @default.
• W2079348778 hasAuthorship W2079348778A5030927546 @default.
• W2079348778 hasAuthorship W2079348778A5033572817 @default.
• W2079348778 hasAuthorship W2079348778A5059923412 @default.
• W2079348778 hasAuthorship W2079348778A5063644921 @default.
• W2079348778 hasBestOaLocation W20793487781 @default.
• W2079348778 hasConcept C111368507 @default.
• W2079348778 hasConcept C127313418 @default.
• W2079348778 hasConcept C149348798 @default.
• W2079348778 hasConcept C187599188 @default.
• W2079348778 hasConcept C187850051 @default.
• W2079348778 hasConcept C2984876570 @default.
• W2079348778 hasConcept C49204034 @default.
• W2079348778 hasConcept C60069189 @default.
• W2079348778 hasConcept C7228185 @default.
• W2079348778 hasConcept C78091846 @default.
• W2079348778 hasConceptScore W2079348778C111368507 @default.
• W2079348778 hasConceptScore W2079348778C127313418 @default.
• W2079348778 hasConceptScore W2079348778C149348798 @default.
• W2079348778 hasConceptScore W2079348778C187599188 @default.
• W2079348778 hasConceptScore W2079348778C187850051 @default.
• W2079348778 hasConceptScore W2079348778C2984876570 @default.
• W2079348778 hasConceptScore W2079348778C49204034 @default.
• W2079348778 hasConceptScore W2079348778C60069189 @default.
• W2079348778 hasConceptScore W2079348778C7228185 @default.
• W2079348778 hasConceptScore W2079348778C78091846 @default.
• W2079348778 hasIssue "D24" @default.
• W2079348778 hasLocation W20793487781 @default.
• W2079348778 hasOpenAccess W2079348778 @default.
• W2079348778 hasPrimaryLocation W20793487781 @default.
• W2079348778 hasRelatedWork W1506581797 @default.
• W2079348778 hasRelatedWork W1669668512 @default.
• W2079348778 hasRelatedWork W1980868881 @default.
• W2079348778 hasRelatedWork W1990412265 @default.
• W2079348778 hasRelatedWork W2012133009 @default.
• W2079348778 hasRelatedWork W2021809579 @default.
• W2079348778 hasRelatedWork W2099550260 @default.
• W2079348778 hasRelatedWork W2966865324 @default.
• W2079348778 hasRelatedWork W3214374833 @default.
• W2079348778 hasRelatedWork W4241432928 @default.
• W2079348778 hasVolume "104" @default.
• W2079348778 isParatext "false" @default.
• W2079348778 isRetracted "false" @default.
• W2079348778 magId "2079348778" @default.
• W2079348778 workType "article" @default.