FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2110183780> ?p ?o ?g. }

• W2110183780 endingPage "205" @default.
• W2110183780 startingPage "193" @default.
• W2110183780 abstract "Abstract The occurrence of subtropical cyclones over the central North Pacific Ocean has a significant impact on Hawaii’s weather and climate. In this study, 70 upper-level lows that formed during the period 1980–2002 are documented. In each case the low became cut off from the polar westerlies south of 30°N over the central Pacific, during the Hawaiian cool season (October–April). The objectives of this research are to document the interannual variability in the occurrence of upper-level lows, to chart the locations of their genesis and their tracks, and to investigate the physical mechanisms important in associated surface development. Significant interannual variability in the occurrence of upper-level lows was found, with evidence suggesting the influence of strong El Niño–Southern Oscillation events on the frequency of subtropical cyclogenesis in this region. Of the 70 upper-level lows, 43 were accompanied by surface cyclogenesis and classified as kona lows. Kona low formation is concentrated to the west-northwest of Hawaii, especially during October and November, whereas lows without surface development are concentrated in the area to the east-northeast of Hawaii. Kona low genesis shifts eastward through the cool season, favoring the area to the east-northeast of Hawaii during February and March, consistent with a shift in the climatological position of the trough aloft during the cool season. Consistent with earlier studies, surface deepening is well correlated with positive vorticity advection by the thermal wind. Static stability and advection of low-level moisture are less well correlated to surface deepening. These results suggest that kona low formation, to first order, is a baroclinic instability that originates in the midlatitudes, and that convection and latent-heat release play a secondary role in surface cyclogenesis." @default.
• W2110183780 created "2016-06-24" @default.
• W2110183780 creator A5064249050 @default.
• W2110183780 creator A5069340216 @default.
• W2110183780 date "2006-04-01" @default.
• W2110183780 modified "2023-10-16" @default.
• W2110183780 title "Subtropical Cyclogenesis over the Central North Pacific*" @default.
• W2110183780 cites W1535218940 @default.
• W2110183780 cites W1968387547 @default.
• W2110183780 cites W1975491829 @default.
• W2110183780 cites W1979860080 @default.
• W2110183780 cites W1998765615 @default.
• W2110183780 cites W2000147919 @default.
• W2110183780 cites W2030447458 @default.
• W2110183780 cites W2049176012 @default.
• W2110183780 cites W2056672051 @default.
• W2110183780 cites W2059304700 @default.
• W2110183780 cites W2059682899 @default.
• W2110183780 cites W2066144143 @default.
• W2110183780 cites W2070025094 @default.
• W2110183780 cites W2101466419 @default.
• W2110183780 cites W2103676934 @default.
• W2110183780 cites W2122986456 @default.
• W2110183780 cites W2135157795 @default.
• W2110183780 cites W2140712517 @default.
• W2110183780 cites W2171072599 @default.
• W2110183780 cites W2172358404 @default.
• W2110183780 cites W2172580218 @default.
• W2110183780 cites W2172770337 @default.
• W2110183780 cites W2172996726 @default.
• W2110183780 cites W2173251738 @default.
• W2110183780 cites W2173692403 @default.
• W2110183780 cites W2174098597 @default.
• W2110183780 cites W2175440780 @default.
• W2110183780 cites W2176884493 @default.
• W2110183780 cites W2177625874 @default.
• W2110183780 cites W2179478161 @default.
• W2110183780 cites W2888191710 @default.
• W2110183780 cites W4245810818 @default.
• W2110183780 doi "https://doi.org/10.1175/waf914.1" @default.
• W2110183780 hasPublicationYear "2006" @default.
• W2110183780 type Work @default.
• W2110183780 sameAs 2110183780 @default.
• W2110183780 citedByCount "38" @default.
• W2110183780 countsByYear W21101837802012 @default.
• W2110183780 countsByYear W21101837802015 @default.
• W2110183780 countsByYear W21101837802016 @default.
• W2110183780 countsByYear W21101837802017 @default.
• W2110183780 countsByYear W21101837802018 @default.
• W2110183780 countsByYear W21101837802019 @default.
• W2110183780 countsByYear W21101837802020 @default.
• W2110183780 countsByYear W21101837802021 @default.
• W2110183780 countsByYear W21101837802022 @default.
• W2110183780 countsByYear W21101837802023 @default.
• W2110183780 crossrefType "journal-article" @default.
• W2110183780 hasAuthorship W2110183780A5064249050 @default.
• W2110183780 hasAuthorship W2110183780A5069340216 @default.
• W2110183780 hasBestOaLocation W21101837801 @default.
• W2110183780 hasConcept C107054158 @default.
• W2110183780 hasConcept C111368507 @default.
• W2110183780 hasConcept C121332964 @default.
• W2110183780 hasConcept C127313418 @default.
• W2110183780 hasConcept C139719470 @default.
• W2110183780 hasConcept C14168384 @default.
• W2110183780 hasConcept C142756592 @default.
• W2110183780 hasConcept C153294291 @default.
• W2110183780 hasConcept C160945548 @default.
• W2110183780 hasConcept C162324750 @default.
• W2110183780 hasConcept C205649164 @default.
• W2110183780 hasConcept C2777864850 @default.
• W2110183780 hasConcept C29141058 @default.
• W2110183780 hasConcept C32239851 @default.
• W2110183780 hasConcept C41008148 @default.
• W2110183780 hasConcept C42935608 @default.
• W2110183780 hasConcept C49204034 @default.
• W2110183780 hasConcept C505870484 @default.
• W2110183780 hasConcept C5072599 @default.
• W2110183780 hasConcept C72319357 @default.
• W2110183780 hasConcept C86803240 @default.
• W2110183780 hasConcept C9390403 @default.
• W2110183780 hasConcept C97302686 @default.
• W2110183780 hasConcept C97355855 @default.
• W2110183780 hasConceptScore W2110183780C107054158 @default.
• W2110183780 hasConceptScore W2110183780C111368507 @default.
• W2110183780 hasConceptScore W2110183780C121332964 @default.
• W2110183780 hasConceptScore W2110183780C127313418 @default.
• W2110183780 hasConceptScore W2110183780C139719470 @default.
• W2110183780 hasConceptScore W2110183780C14168384 @default.
• W2110183780 hasConceptScore W2110183780C142756592 @default.
• W2110183780 hasConceptScore W2110183780C153294291 @default.
• W2110183780 hasConceptScore W2110183780C160945548 @default.
• W2110183780 hasConceptScore W2110183780C162324750 @default.
• W2110183780 hasConceptScore W2110183780C205649164 @default.
• W2110183780 hasConceptScore W2110183780C2777864850 @default.
• W2110183780 hasConceptScore W2110183780C29141058 @default.
• W2110183780 hasConceptScore W2110183780C32239851 @default.
• W2110183780 hasConceptScore W2110183780C41008148 @default.
• W2110183780 hasConceptScore W2110183780C42935608 @default.

• next