FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3158093721> ?p ?o ?g. }

• W3158093721 abstract "Given the crucial role of low-level circulation in convective events, this study presents a climatological characterization of the moisture sources and sinks associated with the occurrence of nocturnal low-level jets (NLLJs) in South America. Six selected NLLJ cores are identified according to the jet index that considers a vertical wind speed shear of the lower troposphere at 00:00 local time (LT). The Lagrangian FLEXible PARTicle (FLEXPART) model was used to provide the outputs for tracking atmospheric air masses to determine the moisture sources and sinks for the NLLJ cores (Argentina, Venezuela, and the regions of Brazil: south—Brazil-S, southeast—Brazil-SE, north—Brazil-N, and northeast—Brazil-NE). The analysis is based on 37 years (1980–2016) of the ERA-Interim reanalysis. We found that the NLLJ index is stronger in the warm periods of a year (austral spring and summer) for the six selected regions. The NLLJ frequency is also higher in the warm months of the year, except in Brazil-NE where it is very frequent in all months. In Brazil-NE, the NLLJ also persists for 8 or more days, while the other NLLJs frequently persist for 1–2 days. The NLLJs occupy a broad low-level layer (from 1000 to 700 hPa) and exhibit a mean speed between 7 and 12 ms –1 , which peaks mostly at 900 hPa. The moisture transport for each NLLJ shows that in addition to the intense local moisture sources, the NLLJs in Argentina and Brazil-S receive moisture from the tropical-subtropical South Atlantic Ocean and the Amazon basin, while the tropical-subtropical South Atlantic Ocean is the main moisture source for the NLLJ in Brazil-SE. Both moisture sources and sinks are stronger in the austral summer and fall. The NLLJ in Brazil receives moisture from the tropical South Atlantic (TSA) Ocean, which has weak seasonality. The moisture sources for the NLLJs in Brazil-N and Venezuela come from the tropical North Atlantic (TNA) Ocean in the austral summer and fall, while the TSA Ocean appears as an additional moisture source in the austral winter. This research contributes to improving our understanding of the NLLJs and their role in transporting moisture and controlling precipitation over the continent according to the seasons of a year, helping to improve seasonal climate forecasting." @default.
• W3158093721 created "2021-05-10" @default.
• W3158093721 creator A5028514691 @default.
• W3158093721 creator A5031020263 @default.
• W3158093721 creator A5057726556 @default.
• W3158093721 creator A5062755610 @default.
• W3158093721 creator A5071999275 @default.
• W3158093721 date "2021-04-22" @default.
• W3158093721 modified "2023-10-16" @default.
• W3158093721 title "Assessing the Moisture Transports Associated With Nocturnal Low-Level Jets in Continental South America" @default.
• W3158093721 cites W1504967735 @default.
• W3158093721 cites W1546521836 @default.
• W3158093721 cites W1749048564 @default.
• W3158093721 cites W1968866843 @default.
• W3158093721 cites W1975528969 @default.
• W3158093721 cites W1980160079 @default.
• W3158093721 cites W1986817756 @default.
• W3158093721 cites W2000463910 @default.
• W3158093721 cites W2003681189 @default.
• W3158093721 cites W2004381803 @default.
• W3158093721 cites W2026550805 @default.
• W3158093721 cites W2027108147 @default.
• W3158093721 cites W2029126077 @default.
• W3158093721 cites W2037470474 @default.
• W3158093721 cites W2039781911 @default.
• W3158093721 cites W2039959083 @default.
• W3158093721 cites W2040720410 @default.
• W3158093721 cites W2045474363 @default.
• W3158093721 cites W2048982016 @default.
• W3158093721 cites W2051175712 @default.
• W3158093721 cites W2054373890 @default.
• W3158093721 cites W2055030964 @default.
• W3158093721 cites W2066849867 @default.
• W3158093721 cites W2067827709 @default.
• W3158093721 cites W2068043851 @default.
• W3158093721 cites W2068521033 @default.
• W3158093721 cites W2070989528 @default.
• W3158093721 cites W2082235517 @default.
• W3158093721 cites W2092503747 @default.
• W3158093721 cites W2098256695 @default.
• W3158093721 cites W2099985906 @default.
• W3158093721 cites W2108350374 @default.
• W3158093721 cites W2110198356 @default.
• W3158093721 cites W2117353383 @default.
• W3158093721 cites W2117642639 @default.
• W3158093721 cites W2121745948 @default.
• W3158093721 cites W2124639193 @default.
• W3158093721 cites W2126546370 @default.
• W3158093721 cites W2132321424 @default.
• W3158093721 cites W2141799867 @default.
• W3158093721 cites W2142585837 @default.
• W3158093721 cites W2148671084 @default.
• W3158093721 cites W2149964376 @default.
• W3158093721 cites W2150572267 @default.
• W3158093721 cites W2151903232 @default.
• W3158093721 cites W2160486139 @default.
• W3158093721 cites W2175912784 @default.
• W3158093721 cites W2176179542 @default.
• W3158093721 cites W2178174715 @default.
• W3158093721 cites W2179343545 @default.
• W3158093721 cites W2302862193 @default.
• W3158093721 cites W2346002026 @default.
• W3158093721 cites W2346394128 @default.
• W3158093721 cites W2414700885 @default.
• W3158093721 cites W2462773594 @default.
• W3158093721 cites W2515488138 @default.
• W3158093721 cites W2560760363 @default.
• W3158093721 cites W2764029999 @default.
• W3158093721 cites W2774651450 @default.
• W3158093721 cites W2807283223 @default.
• W3158093721 cites W2888504372 @default.
• W3158093721 cites W2908384851 @default.
• W3158093721 cites W2946802326 @default.
• W3158093721 cites W2954439820 @default.
• W3158093721 cites W2955733788 @default.
• W3158093721 cites W2977933770 @default.
• W3158093721 cites W2979561857 @default.
• W3158093721 cites W3048702436 @default.
• W3158093721 doi "https://doi.org/10.3389/fenvs.2021.657764" @default.
• W3158093721 hasPublicationYear "2021" @default.
• W3158093721 type Work @default.
• W3158093721 sameAs 3158093721 @default.
• W3158093721 citedByCount "6" @default.
• W3158093721 countsByYear W31580937212021 @default.
• W3158093721 countsByYear W31580937212022 @default.
• W3158093721 countsByYear W31580937212023 @default.
• W3158093721 crossrefType "journal-article" @default.
• W3158093721 hasAuthorship W3158093721A5028514691 @default.
• W3158093721 hasAuthorship W3158093721A5031020263 @default.
• W3158093721 hasAuthorship W3158093721A5057726556 @default.
• W3158093721 hasAuthorship W3158093721A5062755610 @default.
• W3158093721 hasAuthorship W3158093721A5071999275 @default.
• W3158093721 hasBestOaLocation W31580937211 @default.
• W3158093721 hasConcept C121332964 @default.
• W3158093721 hasConcept C127313418 @default.
• W3158093721 hasConcept C1276947 @default.
• W3158093721 hasConcept C14168384 @default.
• W3158093721 hasConcept C142756592 @default.
• W3158093721 hasConcept C153294291 @default.
• W3158093721 hasConcept C176864760 @default.

• next