FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2032977907> ?p ?o ?g. }

• W2032977907 endingPage "659" @default.
• W2032977907 startingPage "659" @default.
• W2032977907 abstract "We survey, in this paper, the properties of the zones of particle precipitation at high latitudes. We consider the average properties of particle influx from the outer magnetosphere as determined by satellite and rocket observations, as well as ground-based techniques. The point of view of this paper is to try to associate source regions, and, if possible, precipitation mechanisms with each of the families of precipitating particles that collectively form the auroral zone. The precipitation patterns for both electrons and protons exhibit a diurnal variation. The several zones of particle precipitation can be placed in relationship to each other. The zone of electron precipitation is best described as consisting of a region at low latitudes (60° ⪝ Λ ⪝ 70° near local midnight) where electrons with characteristic energies of tens of kev precipitate; this region merges and overlaps at the higher latitudes with another region (70° ⪝ Λ ⪝ 80° near local midnight) characterized by precipitating electrons of ≈0.5 kev. The limited data available indicate that the zone of proton precipitation spatially overlaps the zone of electron precipitation. For example, the peak of precipitation of > 4-kev protons near local midnight is found between Λ = 65° and Λ = 70°. Near local noon a separate region of very soft proton precipitation is found in the vicinity of Λ ≈ 80°, in addition to a region of proton influx at lower latitudes. We consider the plasma sheet, the extraterrestrial ring current, the polar cusp, and the outer radiation belt as source regions of precipitating particles. Brief surveys of the precipitation of helium ions and of possible means of artificially inducing particle precipitation are also included." @default.
• W2032977907 created "2016-06-24" @default.
• W2032977907 creator A5018516265 @default.
• W2032977907 date "1971-01-01" @default.
• W2032977907 modified "2023-09-27" @default.
• W2032977907 title "The patterns and sources of high-latitude particle precipitation" @default.
• W2032977907 cites W1492902404 @default.
• W2032977907 cites W1509309600 @default.
• W2032977907 cites W1579237429 @default.
• W2032977907 cites W1581482862 @default.
• W2032977907 cites W1831994195 @default.
• W2032977907 cites W1843350233 @default.
• W2032977907 cites W186013726 @default.
• W2032977907 cites W1966096191 @default.
• W2032977907 cites W1966246397 @default.
• W2032977907 cites W1966334975 @default.
• W2032977907 cites W1969674063 @default.
• W2032977907 cites W1970704563 @default.
• W2032977907 cites W1971516607 @default.
• W2032977907 cites W1973896217 @default.
• W2032977907 cites W1975053019 @default.
• W2032977907 cites W1976053921 @default.
• W2032977907 cites W1977793564 @default.
• W2032977907 cites W1978269355 @default.
• W2032977907 cites W1980082619 @default.
• W2032977907 cites W1980317470 @default.
• W2032977907 cites W1983081051 @default.
• W2032977907 cites W1983156489 @default.
• W2032977907 cites W1983229147 @default.
• W2032977907 cites W1983316540 @default.
• W2032977907 cites W1989663207 @default.
• W2032977907 cites W1992457370 @default.
• W2032977907 cites W1997581761 @default.
• W2032977907 cites W2005970773 @default.
• W2032977907 cites W2006571227 @default.
• W2032977907 cites W2006784400 @default.
• W2032977907 cites W2007676269 @default.
• W2032977907 cites W2009525411 @default.
• W2032977907 cites W2010146306 @default.
• W2032977907 cites W2013551853 @default.
• W2032977907 cites W2014598717 @default.
• W2032977907 cites W2015955640 @default.
• W2032977907 cites W2017593802 @default.
• W2032977907 cites W2018346750 @default.
• W2032977907 cites W2018804466 @default.
• W2032977907 cites W2021074647 @default.
• W2032977907 cites W2022087044 @default.
• W2032977907 cites W2023255301 @default.
• W2032977907 cites W2023306050 @default.
• W2032977907 cites W2029381340 @default.
• W2032977907 cites W2032264251 @default.
• W2032977907 cites W2034291622 @default.
• W2032977907 cites W2037086379 @default.
• W2032977907 cites W2038100229 @default.
• W2032977907 cites W2043744958 @default.
• W2032977907 cites W2045472964 @default.
• W2032977907 cites W2047410059 @default.
• W2032977907 cites W2049119907 @default.
• W2032977907 cites W2049525462 @default.
• W2032977907 cites W2050767790 @default.
• W2032977907 cites W2056176390 @default.
• W2032977907 cites W2057453691 @default.
• W2032977907 cites W2057885388 @default.
• W2032977907 cites W2058210838 @default.
• W2032977907 cites W2058813947 @default.
• W2032977907 cites W2059550909 @default.
• W2032977907 cites W2061785205 @default.
• W2032977907 cites W2061919413 @default.
• W2032977907 cites W2062564072 @default.
• W2032977907 cites W2062851587 @default.
• W2032977907 cites W2063169426 @default.
• W2032977907 cites W2064933235 @default.
• W2032977907 cites W2065380636 @default.
• W2032977907 cites W2068086295 @default.
• W2032977907 cites W2068126016 @default.
• W2032977907 cites W2075516665 @default.
• W2032977907 cites W2075847750 @default.
• W2032977907 cites W2079242722 @default.
• W2032977907 cites W2090130446 @default.
• W2032977907 cites W2091250644 @default.
• W2032977907 cites W2091715317 @default.
• W2032977907 cites W2098668960 @default.
• W2032977907 cites W2104617138 @default.
• W2032977907 cites W2110755258 @default.
• W2032977907 cites W2113093203 @default.
• W2032977907 cites W2117673952 @default.
• W2032977907 cites W2118976177 @default.
• W2032977907 cites W2119474804 @default.
• W2032977907 cites W2119640763 @default.
• W2032977907 cites W2127154723 @default.
• W2032977907 cites W2135741794 @default.
• W2032977907 cites W2137879822 @default.
• W2032977907 cites W2142137830 @default.
• W2032977907 cites W2142818919 @default.
• W2032977907 cites W2148213469 @default.
• W2032977907 cites W2149641874 @default.
• W2032977907 cites W2152157958 @default.
• W2032977907 cites W2157696573 @default.

• next