FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2071114828> ?p ?o ?g. }

• W2071114828 endingPage "152" @default.
• W2071114828 startingPage "133" @default.
• W2071114828 abstract "An elongated intense precipitation system associated with a stationary front delivered enhanced rainfall to the northern lateral and lee sides of an isolated mountain on Jeju Island on 6 July 2007. The convective region of the system passed around the mountain (Mt. Halla; height 1950 m, width 35 km, length 78 km) under moist synoptic conditions (relative humidity ~ 95% below 3 km) during the rainy season. In this study, the detailed 3-dimensional structure and enhancement mechanisms of this precipitation system are examined using dual-Doppler radar observations. Analysis of the Doppler radar indicates that the precipitation system was organized in an elongated shape that extended southwest–northeast about 20 km off the northwestern shore of Jeju Island. The development of this precipitation system with respect to Mt. Halla can be divided into three stages: approaching stage, lateral-side stage, and lee-side stage. During the approaching stage, variational wind analysis indicates that the updraft region was aligned with the convergence zone of relatively strong westerlies and weak southwesterlies on the western side of the system. The southwesterlies accelerated gradually, generating local updrafts between the system and the northwestern slope of the mountain that were crucial to the enhancement of the southern part of the system. The enhanced convective region intensified further as it reached the northwestern shore of the island. The elliptical shape and isolated terrain of Jeju Island played an important role in this intensification by modifying the low-level winds, with a relatively low Froude number of 0.2. This modification of the low-level wind by the terrain provided a plentiful supply of moist air to the convective region of the system, maintaining the enhanced convection. During the lee-side stage, the system was characterized by relatively weak westerlies at low altitude as it approached the eastern slope of the mountain. The convergence of these weak westerlies and relatively strong southwesterlies over the southeastern slope of the mountain induced a stationary updraft region and re-enhancement of convection on the lee-side of the mountain. The regional enhancement of this precipitation system on the lateral and lee sides of Mt. Halla resulted from localized terrain-induced low-level convergence under moist environmental conditions with predominant west-southwesterly winds. These environmental conditions are well organized when a stationary front is located off the northern shore of Jeju Island." @default.
• W2071114828 created "2016-06-24" @default.
• W2071114828 creator A5012366628 @default.
• W2071114828 creator A5048679347 @default.
• W2071114828 creator A5054052206 @default.
• W2071114828 creator A5082593092 @default.
• W2071114828 date "2012-11-01" @default.
• W2071114828 modified "2023-10-03" @default.
• W2071114828 title "Dual-Doppler radar analysis of the enhancement of a precipitation system on the northern side of Mt. Halla, Jeju Island, Korea on 6 July 2007" @default.
• W2071114828 cites W1423198670 @default.
• W2071114828 cites W1823032471 @default.
• W2071114828 cites W2003873030 @default.
• W2071114828 cites W2006451105 @default.
• W2071114828 cites W2015118078 @default.
• W2071114828 cites W2025274119 @default.
• W2071114828 cites W2039060968 @default.
• W2071114828 cites W2059709460 @default.
• W2071114828 cites W2063834802 @default.
• W2071114828 cites W2074959601 @default.
• W2071114828 cites W2078981665 @default.
• W2071114828 cites W2087337809 @default.
• W2071114828 cites W2145204366 @default.
• W2071114828 cites W2152663878 @default.
• W2071114828 cites W2160108788 @default.
• W2071114828 cites W2173790700 @default.
• W2071114828 cites W2174868853 @default.
• W2071114828 cites W2177975269 @default.
• W2071114828 cites W2178269757 @default.
• W2071114828 cites W2180790387 @default.
• W2071114828 cites W2256743162 @default.
• W2071114828 cites W2465502897 @default.
• W2071114828 cites W2606485351 @default.
• W2071114828 doi "https://doi.org/10.1016/j.atmosres.2012.06.017" @default.
• W2071114828 hasPublicationYear "2012" @default.
• W2071114828 type Work @default.
• W2071114828 sameAs 2071114828 @default.
• W2071114828 citedByCount "9" @default.
• W2071114828 countsByYear W20711148282014 @default.
• W2071114828 countsByYear W20711148282017 @default.
• W2071114828 countsByYear W20711148282018 @default.
• W2071114828 countsByYear W20711148282019 @default.
• W2071114828 countsByYear W20711148282022 @default.
• W2071114828 crossrefType "journal-article" @default.
• W2071114828 hasAuthorship W2071114828A5012366628 @default.
• W2071114828 hasAuthorship W2071114828A5048679347 @default.
• W2071114828 hasAuthorship W2071114828A5054052206 @default.
• W2071114828 hasAuthorship W2071114828A5082593092 @default.
• W2071114828 hasBestOaLocation W20711148282 @default.
• W2071114828 hasConcept C107054158 @default.
• W2071114828 hasConcept C10899652 @default.
• W2071114828 hasConcept C111368507 @default.
• W2071114828 hasConcept C127313418 @default.
• W2071114828 hasConcept C133204551 @default.
• W2071114828 hasConcept C134295995 @default.
• W2071114828 hasConcept C142756592 @default.
• W2071114828 hasConcept C146357865 @default.
• W2071114828 hasConcept C151730666 @default.
• W2071114828 hasConcept C152382732 @default.
• W2071114828 hasConcept C153294291 @default.
• W2071114828 hasConcept C194507410 @default.
• W2071114828 hasConcept C205649164 @default.
• W2071114828 hasConcept C2777551076 @default.
• W2071114828 hasConcept C49204034 @default.
• W2071114828 hasConceptScore W2071114828C107054158 @default.
• W2071114828 hasConceptScore W2071114828C10899652 @default.
• W2071114828 hasConceptScore W2071114828C111368507 @default.
• W2071114828 hasConceptScore W2071114828C127313418 @default.
• W2071114828 hasConceptScore W2071114828C133204551 @default.
• W2071114828 hasConceptScore W2071114828C134295995 @default.
• W2071114828 hasConceptScore W2071114828C142756592 @default.
• W2071114828 hasConceptScore W2071114828C146357865 @default.
• W2071114828 hasConceptScore W2071114828C151730666 @default.
• W2071114828 hasConceptScore W2071114828C152382732 @default.
• W2071114828 hasConceptScore W2071114828C153294291 @default.
• W2071114828 hasConceptScore W2071114828C194507410 @default.
• W2071114828 hasConceptScore W2071114828C205649164 @default.
• W2071114828 hasConceptScore W2071114828C2777551076 @default.
• W2071114828 hasConceptScore W2071114828C49204034 @default.
• W2071114828 hasFunder F4320320912 @default.
• W2071114828 hasLocation W20711148281 @default.
• W2071114828 hasLocation W20711148282 @default.
• W2071114828 hasLocation W20711148283 @default.
• W2071114828 hasOpenAccess W2071114828 @default.
• W2071114828 hasPrimaryLocation W20711148281 @default.
• W2071114828 hasRelatedWork W1958377557 @default.
• W2071114828 hasRelatedWork W2049885513 @default.
• W2071114828 hasRelatedWork W2062987318 @default.
• W2071114828 hasRelatedWork W2111228609 @default.
• W2071114828 hasRelatedWork W2558481381 @default.
• W2071114828 hasRelatedWork W2738869444 @default.
• W2071114828 hasRelatedWork W3015295477 @default.
• W2071114828 hasRelatedWork W3181231840 @default.
• W2071114828 hasRelatedWork W4212931864 @default.
• W2071114828 hasRelatedWork W4220929856 @default.
• W2071114828 hasVolume "118" @default.
• W2071114828 isParatext "false" @default.
• W2071114828 isRetracted "false" @default.
• W2071114828 magId "2071114828" @default.

• next