Matches in SemOpenAlex for { <https://semopenalex.org/work/W1979964761> ?p ?o ?g. }
- W1979964761 endingPage "15980" @default.
- W1979964761 startingPage "15965" @default.
- W1979964761 abstract "Pc3–4 (15–50 mHz) pulsations are often observed during daytime hours in the Earth's magnetosphere and on the ground. The ion foreshock region of the solar wind upstream of Earth is now understood to be a major source of these waves, and the general dependence of their occurrence in the magnetosphere on the cone angle of the interplanetary magnetic field (IMF) is well attested. However, there have also been suggestions that the IMF clock angle should introduce latitudinal or local time asymmetries in wave occurrence, and in particular, that Pc3–4 pulsations might preferentially reach northern versus southern high‐latitude regions. In order to test this latter suggestion, we have compared a full year's (1997) data from two cusp‐latitude stations, Sondrestromfjord, Greenland, and South Pole, Antarctica, both near 74° corrected geomagnetic latitude. Our data show the usual strong IMF cone angle control of Pc3–4 wave occurrence/amplitude but also indicate that occurrence and relative amplitude are essentially identical near both cusps; any clock angle control is at most a second‐order effect, not detectable in our analysis. We further find little seasonal dependence in the ratio of power in the two cusp regions other than that attributable to differences in solar illumination. These observations, in conjunction with the well‐known sharp cutoff in wave activity for cone angles above 45°, indicate that only those perturbations occurring at the subsolar bow shock can reach the magnetopause and propagate to any location in the dayside magnetosphere. In addition, the absence of a clock angle effect supports earlier suggestions that Pc3–4 signals in the magnetosheath do not cross streamlines and thus do not propagate as waves, but are rather convected as spatial structures in the highly turbulent, high‐beta downstream magnetosheath plasma." @default.
- W1979964761 created "2016-06-24" @default.
- W1979964761 creator A5036976679 @default.
- W1979964761 creator A5067627276 @default.
- W1979964761 creator A5070333810 @default.
- W1979964761 creator A5080918414 @default.
- W1979964761 date "2000-07-01" @default.
- W1979964761 modified "2023-10-14" @default.
- W1979964761 title "A conjugate study of Pc3-4 pulsations at cusp latitudes: Is there a clock angle effect?" @default.
- W1979964761 cites W1514910154 @default.
- W1979964761 cites W1560574346 @default.
- W1979964761 cites W1580755478 @default.
- W1979964761 cites W1625916355 @default.
- W1979964761 cites W1650150849 @default.
- W1979964761 cites W1676082254 @default.
- W1979964761 cites W1680413291 @default.
- W1979964761 cites W1971122347 @default.
- W1979964761 cites W1981216752 @default.
- W1979964761 cites W1991852577 @default.
- W1979964761 cites W2005220896 @default.
- W1979964761 cites W2008611694 @default.
- W1979964761 cites W2016160898 @default.
- W1979964761 cites W2028734173 @default.
- W1979964761 cites W2033745782 @default.
- W1979964761 cites W2075994730 @default.
- W1979964761 cites W2080846694 @default.
- W1979964761 cites W2085037851 @default.
- W1979964761 cites W2109726013 @default.
- W1979964761 cites W2121152507 @default.
- W1979964761 cites W4362209264 @default.
- W1979964761 cites W2133561855 @default.
- W1979964761 doi "https://doi.org/10.1029/1999ja000328" @default.
- W1979964761 hasPublicationYear "2000" @default.
- W1979964761 type Work @default.
- W1979964761 sameAs 1979964761 @default.
- W1979964761 citedByCount "7" @default.
- W1979964761 countsByYear W19799647612012 @default.
- W1979964761 countsByYear W19799647612014 @default.
- W1979964761 countsByYear W19799647612019 @default.
- W1979964761 crossrefType "journal-article" @default.
- W1979964761 hasAuthorship W1979964761A5036976679 @default.
- W1979964761 hasAuthorship W1979964761A5067627276 @default.
- W1979964761 hasAuthorship W1979964761A5070333810 @default.
- W1979964761 hasAuthorship W1979964761A5080918414 @default.
- W1979964761 hasBestOaLocation W19799647611 @default.
- W1979964761 hasConcept C102988692 @default.
- W1979964761 hasConcept C105795698 @default.
- W1979964761 hasConcept C108411613 @default.
- W1979964761 hasConcept C115260700 @default.
- W1979964761 hasConcept C116403925 @default.
- W1979964761 hasConcept C121332964 @default.
- W1979964761 hasConcept C122523270 @default.
- W1979964761 hasConcept C127313418 @default.
- W1979964761 hasConcept C1276947 @default.
- W1979964761 hasConcept C130443932 @default.
- W1979964761 hasConcept C13280743 @default.
- W1979964761 hasConcept C140161248 @default.
- W1979964761 hasConcept C155991500 @default.
- W1979964761 hasConcept C163258240 @default.
- W1979964761 hasConcept C180205008 @default.
- W1979964761 hasConcept C199635899 @default.
- W1979964761 hasConcept C2524010 @default.
- W1979964761 hasConcept C2778400075 @default.
- W1979964761 hasConcept C2780182046 @default.
- W1979964761 hasConcept C33923547 @default.
- W1979964761 hasConcept C41479618 @default.
- W1979964761 hasConcept C44870925 @default.
- W1979964761 hasConcept C57879066 @default.
- W1979964761 hasConcept C61922881 @default.
- W1979964761 hasConcept C62520636 @default.
- W1979964761 hasConcept C70477161 @default.
- W1979964761 hasConcept C8058405 @default.
- W1979964761 hasConcept C91586092 @default.
- W1979964761 hasConceptScore W1979964761C102988692 @default.
- W1979964761 hasConceptScore W1979964761C105795698 @default.
- W1979964761 hasConceptScore W1979964761C108411613 @default.
- W1979964761 hasConceptScore W1979964761C115260700 @default.
- W1979964761 hasConceptScore W1979964761C116403925 @default.
- W1979964761 hasConceptScore W1979964761C121332964 @default.
- W1979964761 hasConceptScore W1979964761C122523270 @default.
- W1979964761 hasConceptScore W1979964761C127313418 @default.
- W1979964761 hasConceptScore W1979964761C1276947 @default.
- W1979964761 hasConceptScore W1979964761C130443932 @default.
- W1979964761 hasConceptScore W1979964761C13280743 @default.
- W1979964761 hasConceptScore W1979964761C140161248 @default.
- W1979964761 hasConceptScore W1979964761C155991500 @default.
- W1979964761 hasConceptScore W1979964761C163258240 @default.
- W1979964761 hasConceptScore W1979964761C180205008 @default.
- W1979964761 hasConceptScore W1979964761C199635899 @default.
- W1979964761 hasConceptScore W1979964761C2524010 @default.
- W1979964761 hasConceptScore W1979964761C2778400075 @default.
- W1979964761 hasConceptScore W1979964761C2780182046 @default.
- W1979964761 hasConceptScore W1979964761C33923547 @default.
- W1979964761 hasConceptScore W1979964761C41479618 @default.
- W1979964761 hasConceptScore W1979964761C44870925 @default.
- W1979964761 hasConceptScore W1979964761C57879066 @default.
- W1979964761 hasConceptScore W1979964761C61922881 @default.
- W1979964761 hasConceptScore W1979964761C62520636 @default.