author_facet Yordanova, E.
Balogh, A.
Noullez, A.
von Steiger, R.
Yordanova, E.
Balogh, A.
Noullez, A.
von Steiger, R.
author Yordanova, E.
Balogh, A.
Noullez, A.
von Steiger, R.
spellingShingle Yordanova, E.
Balogh, A.
Noullez, A.
von Steiger, R.
Journal of Geophysical Research: Space Physics
Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
Paleontology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Earth-Surface Processes
Geochemistry and Petrology
Soil Science
Water Science and Technology
Ecology
Aquatic Science
Forestry
Oceanography
Geophysics
author_sort yordanova, e.
spelling Yordanova, E. Balogh, A. Noullez, A. von Steiger, R. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/2009ja014067 <jats:p>We study the nonuniform solar wind turbulence using high‐resolution Ulysses magnetic field data measured at different solar activity level, heliospheric latitudes, and distance. We define several types of solar wind dependent of the coronal region of origin and also of the dynamical behavior of the different streams, namely, “pure” fast wind, fast streams, “pure” slow wind, and slow streams. The turbulent properties of the solar wind types were investigated in terms of their scaling properties and spatial inhomogeneity. A clear trend in the power spectrum of the solar wind magnetic field magnitude is observed: the “pure” fast wind has a slope ∼−1.33 (1/<jats:italic>f</jats:italic>‐like), the fast streams ∼−1.48 (Kraichnan‐like), the “pure” slow wind ∼−1.67 (Kolmogorov‐like), and the slow streams ∼−1.72. We find that the “pure” fast wind in the polar heliolatitudes is less intermittent than the other types: “pure” slow wind and both slow and fast streams, which is because of the absence of dynamical interactions between streams with different speeds. On the other hand, fast streams are more intermittent than the “pure” fast wind, and slow streams are less intermittent than the “pure” slow winds. A clear radial and latitudinal evolution of the intermittency is observed only for the “pure” fast wind, while in the equatorial plane, the fast streams, the “pure” slow wind, and the slow streams do not show evolution either in heliolatitude or in heliocentric distance.</jats:p> Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind Journal of Geophysical Research: Space Physics
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Chemie und Pharmazie
Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
Biologie
Allgemeine Naturwissenschaft
Physik
Technik
Geologie und Paläontologie
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series Journal of Geophysical Research: Space Physics
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title Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_unstemmed Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_full Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_fullStr Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_full_unstemmed Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_short Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_sort turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
topic Paleontology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Earth-Surface Processes
Geochemistry and Petrology
Soil Science
Water Science and Technology
Ecology
Aquatic Science
Forestry
Oceanography
Geophysics
url http://dx.doi.org/10.1029/2009ja014067
publishDate 2009
physical
description <jats:p>We study the nonuniform solar wind turbulence using high‐resolution Ulysses magnetic field data measured at different solar activity level, heliospheric latitudes, and distance. We define several types of solar wind dependent of the coronal region of origin and also of the dynamical behavior of the different streams, namely, “pure” fast wind, fast streams, “pure” slow wind, and slow streams. The turbulent properties of the solar wind types were investigated in terms of their scaling properties and spatial inhomogeneity. A clear trend in the power spectrum of the solar wind magnetic field magnitude is observed: the “pure” fast wind has a slope ∼−1.33 (1/<jats:italic>f</jats:italic>‐like), the fast streams ∼−1.48 (Kraichnan‐like), the “pure” slow wind ∼−1.67 (Kolmogorov‐like), and the slow streams ∼−1.72. We find that the “pure” fast wind in the polar heliolatitudes is less intermittent than the other types: “pure” slow wind and both slow and fast streams, which is because of the absence of dynamical interactions between streams with different speeds. On the other hand, fast streams are more intermittent than the “pure” fast wind, and slow streams are less intermittent than the “pure” slow winds. A clear radial and latitudinal evolution of the intermittency is observed only for the “pure” fast wind, while in the equatorial plane, the fast streams, the “pure” slow wind, and the slow streams do not show evolution either in heliolatitude or in heliocentric distance.</jats:p>
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author Yordanova, E., Balogh, A., Noullez, A., von Steiger, R.
author_facet Yordanova, E., Balogh, A., Noullez, A., von Steiger, R., Yordanova, E., Balogh, A., Noullez, A., von Steiger, R.
author_sort yordanova, e.
container_issue A8
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container_title Journal of Geophysical Research: Space Physics
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description <jats:p>We study the nonuniform solar wind turbulence using high‐resolution Ulysses magnetic field data measured at different solar activity level, heliospheric latitudes, and distance. We define several types of solar wind dependent of the coronal region of origin and also of the dynamical behavior of the different streams, namely, “pure” fast wind, fast streams, “pure” slow wind, and slow streams. The turbulent properties of the solar wind types were investigated in terms of their scaling properties and spatial inhomogeneity. A clear trend in the power spectrum of the solar wind magnetic field magnitude is observed: the “pure” fast wind has a slope ∼−1.33 (1/<jats:italic>f</jats:italic>‐like), the fast streams ∼−1.48 (Kraichnan‐like), the “pure” slow wind ∼−1.67 (Kolmogorov‐like), and the slow streams ∼−1.72. We find that the “pure” fast wind in the polar heliolatitudes is less intermittent than the other types: “pure” slow wind and both slow and fast streams, which is because of the absence of dynamical interactions between streams with different speeds. On the other hand, fast streams are more intermittent than the “pure” fast wind, and slow streams are less intermittent than the “pure” slow winds. A clear radial and latitudinal evolution of the intermittency is observed only for the “pure” fast wind, while in the equatorial plane, the fast streams, the “pure” slow wind, and the slow streams do not show evolution either in heliolatitude or in heliocentric distance.</jats:p>
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spelling Yordanova, E. Balogh, A. Noullez, A. von Steiger, R. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/2009ja014067 <jats:p>We study the nonuniform solar wind turbulence using high‐resolution Ulysses magnetic field data measured at different solar activity level, heliospheric latitudes, and distance. We define several types of solar wind dependent of the coronal region of origin and also of the dynamical behavior of the different streams, namely, “pure” fast wind, fast streams, “pure” slow wind, and slow streams. The turbulent properties of the solar wind types were investigated in terms of their scaling properties and spatial inhomogeneity. A clear trend in the power spectrum of the solar wind magnetic field magnitude is observed: the “pure” fast wind has a slope ∼−1.33 (1/<jats:italic>f</jats:italic>‐like), the fast streams ∼−1.48 (Kraichnan‐like), the “pure” slow wind ∼−1.67 (Kolmogorov‐like), and the slow streams ∼−1.72. We find that the “pure” fast wind in the polar heliolatitudes is less intermittent than the other types: “pure” slow wind and both slow and fast streams, which is because of the absence of dynamical interactions between streams with different speeds. On the other hand, fast streams are more intermittent than the “pure” fast wind, and slow streams are less intermittent than the “pure” slow winds. A clear radial and latitudinal evolution of the intermittency is observed only for the “pure” fast wind, while in the equatorial plane, the fast streams, the “pure” slow wind, and the slow streams do not show evolution either in heliolatitude or in heliocentric distance.</jats:p> Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind Journal of Geophysical Research: Space Physics
spellingShingle Yordanova, E., Balogh, A., Noullez, A., von Steiger, R., Journal of Geophysical Research: Space Physics, Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind, Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics
title Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_full Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_fullStr Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_full_unstemmed Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_short Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_sort turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
title_unstemmed Turbulence and intermittency in the heliospheric magnetic field in fast and slow solar wind
topic Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics
url http://dx.doi.org/10.1029/2009ja014067