FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2100821405> ?p ?o ?g. }

• W2100821405 endingPage "133" @default.
• W2100821405 startingPage "125" @default.
• W2100821405 abstract "Abstract. A statistical investigation of the location of onset of intermediate and gyrating ion populations in the Earth's foreshock is presented based on Fixed Voltage Analyzer data from ISEE 1. This study reveals the existence of a spatial boundary for intermediate and gyrating ion populations that coincides with the reported ULF wave boundary. This boundary position in the Earth's foreshock depends strongly upon the magnetic cone angle θBX and appears well defined for relatively large cone angles, though not for small cone angles. As reported in a previous study of the ULF wave boundary, the position of the intermediate-gyrating ion boundary is not compatible with a fixed growth rate of the waves resulting from the interaction between a uniform beam and the ambient plasma. The present work examines the momentum associated with protons which travel along this boundary, and we show that the variation of the boundary position (or equivalently, the associated particle momentum) with the cone angle is related to classical acceleration mechanisms at the bow shock surface. The same functional behavior as a function of the cone angle is obtained for the momentum predicted by an acceleration model and for the particle momentum associated with the boundary. However, the model predicts systematically larger values of the momentum than the observation related values by a constant amount; we suggest that this difference may be due to some momentum exchange between the incident solar-wind population and the backstreaming particles through a wave-particle interaction resulting from a beam plasma instability.Key words. Intermediate ion boundary · Statistical investigation · Earth's foreshock · ISEE 1 spacecraft" @default.
• W2100821405 created "2016-06-24" @default.
• W2100821405 creator A5076774785 @default.
• W2100821405 creator A5077207656 @default.
• W2100821405 date "1998-02-28" @default.
• W2100821405 modified "2023-10-06" @default.
• W2100821405 title "A statistical study of the upstream intermediate ion boundary in the Earth's foreshock" @default.
• W2100821405 cites W1966878267 @default.
• W2100821405 cites W1973197582 @default.
• W2100821405 cites W1978666354 @default.
• W2100821405 cites W1984363762 @default.
• W2100821405 cites W1984613089 @default.
• W2100821405 cites W1989366355 @default.
• W2100821405 cites W1995784485 @default.
• W2100821405 cites W1996932723 @default.
• W2100821405 cites W2001322864 @default.
• W2100821405 cites W2008128909 @default.
• W2100821405 cites W2010778424 @default.
• W2100821405 cites W2013238650 @default.
• W2100821405 cites W2013240257 @default.
• W2100821405 cites W2014070818 @default.
• W2100821405 cites W2023777998 @default.
• W2100821405 cites W2026002287 @default.
• W2100821405 cites W2027430236 @default.
• W2100821405 cites W2043748428 @default.
• W2100821405 cites W2050115595 @default.
• W2100821405 cites W2050329605 @default.
• W2100821405 cites W2052553667 @default.
• W2100821405 cites W2054999853 @default.
• W2100821405 cites W2056505279 @default.
• W2100821405 cites W2056610687 @default.
• W2100821405 cites W2058671478 @default.
• W2100821405 cites W2062201263 @default.
• W2100821405 cites W2063655532 @default.
• W2100821405 cites W2071108951 @default.
• W2100821405 cites W2073641147 @default.
• W2100821405 cites W2083427452 @default.
• W2100821405 cites W2091459562 @default.
• W2100821405 cites W2092119255 @default.
• W2100821405 cites W2105458279 @default.
• W2100821405 cites W2116390699 @default.
• W2100821405 cites W2118141437 @default.
• W2100821405 cites W2160434377 @default.
• W2100821405 cites W2162127027 @default.
• W2100821405 cites W2166721068 @default.
• W2100821405 cites W2170645754 @default.
• W2100821405 doi "https://doi.org/10.1007/s00585-998-0125-7" @default.
• W2100821405 hasPublicationYear "1998" @default.
• W2100821405 type Work @default.
• W2100821405 sameAs 2100821405 @default.
• W2100821405 citedByCount "15" @default.
• W2100821405 countsByYear W21008214052013 @default.
• W2100821405 countsByYear W21008214052015 @default.
• W2100821405 countsByYear W21008214052016 @default.
• W2100821405 countsByYear W21008214052018 @default.
• W2100821405 countsByYear W21008214052020 @default.
• W2100821405 countsByYear W21008214052023 @default.
• W2100821405 crossrefType "journal-article" @default.
• W2100821405 hasAuthorship W2100821405A5076774785 @default.
• W2100821405 hasAuthorship W2100821405A5077207656 @default.
• W2100821405 hasBestOaLocation W21008214051 @default.
• W2100821405 hasConcept C10138342 @default.
• W2100821405 hasConcept C108411613 @default.
• W2100821405 hasConcept C121332964 @default.
• W2100821405 hasConcept C127313418 @default.
• W2100821405 hasConcept C130443932 @default.
• W2100821405 hasConcept C134306372 @default.
• W2100821405 hasConcept C144024400 @default.
• W2100821405 hasConcept C147412999 @default.
• W2100821405 hasConcept C149923435 @default.
• W2100821405 hasConcept C155991500 @default.
• W2100821405 hasConcept C156801008 @default.
• W2100821405 hasConcept C162324750 @default.
• W2100821405 hasConcept C165205528 @default.
• W2100821405 hasConcept C2908647359 @default.
• W2100821405 hasConcept C30475298 @default.
• W2100821405 hasConcept C33923547 @default.
• W2100821405 hasConcept C57879066 @default.
• W2100821405 hasConcept C60718061 @default.
• W2100821405 hasConcept C62354387 @default.
• W2100821405 hasConcept C62520636 @default.
• W2100821405 hasConcept C70477161 @default.
• W2100821405 hasConcept C74650414 @default.
• W2100821405 hasConcept C8058405 @default.
• W2100821405 hasConcept C82706917 @default.
• W2100821405 hasConceptScore W2100821405C10138342 @default.
• W2100821405 hasConceptScore W2100821405C108411613 @default.
• W2100821405 hasConceptScore W2100821405C121332964 @default.
• W2100821405 hasConceptScore W2100821405C127313418 @default.
• W2100821405 hasConceptScore W2100821405C130443932 @default.
• W2100821405 hasConceptScore W2100821405C134306372 @default.
• W2100821405 hasConceptScore W2100821405C144024400 @default.
• W2100821405 hasConceptScore W2100821405C147412999 @default.
• W2100821405 hasConceptScore W2100821405C149923435 @default.
• W2100821405 hasConceptScore W2100821405C155991500 @default.
• W2100821405 hasConceptScore W2100821405C156801008 @default.
• W2100821405 hasConceptScore W2100821405C162324750 @default.
• W2100821405 hasConceptScore W2100821405C165205528 @default.

• next