Zobrazeno 1 - 7
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pro vyhledávání: '"Manuel A. Arriagada"'
Autor:
Manuel Salinas Arriagada
Publikováno v:
ARS Medica, Vol 24, Iss 1 (2018)
Sin resumen
Externí odkaz:
https://doaj.org/article/7b4ad7b1c08b407da0a44ea51cd2598b
Autor:
Manuel Salinas Arriagada
Publikováno v:
ARS Medica, Vol 23, Iss 1 (2018)
Sin resumen
Externí odkaz:
https://doaj.org/article/8ceac18afb2d4a8bb3b2ea51b2900f0f
Publikováno v:
Advances in Space Research. 58:2026-2036
Ionosonde observations have been made at Great Wall station (62.22°S; 58.97°W), King George Island, and at further south Vernadsky station (65.25°S; 64.27°W), Argentine Islands, for many years. For several days at the two locations the magnetic m
Publikováno v:
Advances in Space Research. 51:1878-1882
A simple semi-empirical model to determine the maximum electron concentration in the ionosphere (N mF 2) for South American locations is used to calculate N mF 2 for a northern hemisphere station in the same longitude sector. N mF 2 is determined as
Publikováno v:
JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Diurnal variations of the magnetic meridional component of the thermospheric neutral wind have been derived for Port Stanley (51.7°S;57.8°W), King George Island (62.2°S,58.8°W) and Argentine Islands (65.3°S;64.3°W). A servo-model based algorith
Publikováno v:
Journal of Atmospheric and Solar-Terrestrial Physics. 60:1007-1012
Diurnal variations of the magnetic meridional component of the thermospheric neutral wind have been derived from both a servo model based algorithm with ionosonde data input, and the HWM-90 empirical wind model for the 4–6 and 11–13 June 1991 geo
Publikováno v:
Journal of Atmospheric and Solar-Terrestrial Physics. 59:1405-1410
Diurnal variations of the magnetic meridional component of thermospheric neutral winds are derived for King George Island (62.2 °S; 58.8 °W). Calculations are made using a servo theory based algorithm. Input values are F-region peak heights determi