Spatial Variation in the Responses of the Surface External and Induced Magnetic Field to the Solar Wind

التفاصيل البيبلوغرافية
العنوان: Spatial Variation in the Responses of the Surface External and Induced Magnetic Field to the Solar Wind
المؤلفون: Evan G. Thomas, John C. Coxon, Mervyn P. Freeman, Robert Shore, Nils Olsen, Jesper Gjerloev
المصدر: Journal of Geophysical Research (JGR): Space Physics
Shore, R M, Freeman, M P, Coxon, J C, Thomas, E G, Gjerløv, J W & Olsen, N 2019, ' Spatial variation in the responses of the surface external and induced magnetic field to the solar wind ', Journal of Geophysical Research: Atmospheres, vol. 16, no. 7, pp. 6195-6211 . https://doi.org/10.1029/2019JA026543
بيانات النشر: arXiv, 2021.
سنة النشر: 2021
مصطلحات موضوعية: 010504 meteorology & atmospheric sciences, FOS: Physical sciences, F800, F500, Atmospheric sciences, 01 natural sciences, Space Physics (physics.space-ph), Latitude, Solar wind, Geophysics, Earth's magnetic field, Physics - Space Physics, Space and Planetary Science, Local time, Physics::Space Physics, Polar, Environmental science, Astrophysics::Solar and Stellar Astrophysics, Spatial variability, Astrophysics::Earth and Planetary Astrophysics, Interplanetary magnetic field, Ionosphere, Physics::Atmospheric and Oceanic Physics, 0105 earth and related environmental sciences
الوصف: We analyze the spatial variation in the response of the surface geomagnetic field (or the equivalent ionospheric current) to variations in the solar wind. Specifically, we regress a reanalysis of surface external and induced magnetic field (SEIMF) variations onto measurements of the solar wind. The regression is performed in monthly sets, independently for 559 regularly spaced locations covering the entire northern polar region above 50° magnetic latitude. At each location, we find the lag applied to the solar wind data that maximizes the correlation with the SEIMF. The resulting spatial maps of these independent lags and regression coefficients provide a model of the localized SEIMF response to variations in the solar wind, which we call “Spatial Information from Distributed Exogenous Regression.” We find that the lag and regression coefficients vary systematically with ionospheric region, season, and solar wind driver. In the polar cap region the SEIMF is best described by the B y component of the interplanetary magnetic field (50–75% of total variance explained) at a lag ∼20–25 min. Conversely, in the auroral zone the SEIMF is best described by the solar wind ϵ function (60–80% of total variance explained), with a lag that varies with season and magnetic local time (MLT), from ∼15–20 min for dayside and afternoon MLT (except in Oct–Dec) to typically 30–40 min for nightside and morning MLT and even longer (60–65 min) around midnight MLT. publishedVersion
وصف الملف: text; application/pdf
تدمد: 2169-9380
DOI: 10.48550/arxiv.2108.01370
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aea12b69272a484222c7293fcf202ec2
حقوق: OPEN
رقم الأكسشن: edsair.doi.dedup.....aea12b69272a484222c7293fcf202ec2
قاعدة البيانات: OpenAIRE
الوصف
تدمد:21699380
DOI:10.48550/arxiv.2108.01370