author_facet Suess, S. T.
Poletto, G.
Romoli, M.
Neugebauer, M.
Goldstein, B. E.
Simnett, G.
Suess, S. T.
Poletto, G.
Romoli, M.
Neugebauer, M.
Goldstein, B. E.
Simnett, G.
author Suess, S. T.
Poletto, G.
Romoli, M.
Neugebauer, M.
Goldstein, B. E.
Simnett, G.
spellingShingle Suess, S. T.
Poletto, G.
Romoli, M.
Neugebauer, M.
Goldstein, B. E.
Simnett, G.
Journal of Geophysical Research: Space Physics
The May 1997 SOHO‐Ulysses quadrature
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 suess, s. t.
spelling Suess, S. T. Poletto, G. Romoli, M. Neugebauer, M. Goldstein, B. E. Simnett, G. 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/10.1029/2000ja000044 <jats:p>We present results from the May 1997 SOHO‐Ulysses quadrature (SOHO‐Sun‐Ulysses angle=90°), near sunspot minimum. Ulysses was at 5.1 AU, 10° north of the solar equator, and off the east limb. It was also at the very northern edge of the streamer belt. Nevertheless, the Solar Wind Observations Over the Poles of the Sun instrument (SWOOPS) detected only slow, unusually smooth wind and there was no direct evidence of fast wind from the northern polar coronal hole or of mixing with fast wind. The Large‐Angle and Spectrometric Coronagraph (LASCO) images show that the streamer belt at 10°N was narrow and sharp at the beginning and end of the 2 week observation interval, but broadened in the middle. A related change in density, but not flow speed, occurred at Ulysses. Under these conditions it was possible to show that densities derived from the Ultraviolet Coronagraph Spectrometer (UVCS) in the lower corona are closely related to those in the solar wind, both over quiet intervals and in transient events on the limb. Density and velocity in one small transient observed by both LASCO and UVCS are analyzed in detail.</jats:p> The May 1997 SOHO‐Ulysses quadrature Journal of Geophysical Research: Space Physics
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title The May 1997 SOHO‐Ulysses quadrature
title_unstemmed The May 1997 SOHO‐Ulysses quadrature
title_full The May 1997 SOHO‐Ulysses quadrature
title_fullStr The May 1997 SOHO‐Ulysses quadrature
title_full_unstemmed The May 1997 SOHO‐Ulysses quadrature
title_short The May 1997 SOHO‐Ulysses quadrature
title_sort the may 1997 soho‐ulysses quadrature
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/10.1029/2000ja000044
publishDate 2000
physical 25033-25051
description <jats:p>We present results from the May 1997 SOHO‐Ulysses quadrature (SOHO‐Sun‐Ulysses angle=90°), near sunspot minimum. Ulysses was at 5.1 AU, 10° north of the solar equator, and off the east limb. It was also at the very northern edge of the streamer belt. Nevertheless, the Solar Wind Observations Over the Poles of the Sun instrument (SWOOPS) detected only slow, unusually smooth wind and there was no direct evidence of fast wind from the northern polar coronal hole or of mixing with fast wind. The Large‐Angle and Spectrometric Coronagraph (LASCO) images show that the streamer belt at 10°N was narrow and sharp at the beginning and end of the 2 week observation interval, but broadened in the middle. A related change in density, but not flow speed, occurred at Ulysses. Under these conditions it was possible to show that densities derived from the Ultraviolet Coronagraph Spectrometer (UVCS) in the lower corona are closely related to those in the solar wind, both over quiet intervals and in transient events on the limb. Density and velocity in one small transient observed by both LASCO and UVCS are analyzed in detail.</jats:p>
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author Suess, S. T., Poletto, G., Romoli, M., Neugebauer, M., Goldstein, B. E., Simnett, G.
author_facet Suess, S. T., Poletto, G., Romoli, M., Neugebauer, M., Goldstein, B. E., Simnett, G., Suess, S. T., Poletto, G., Romoli, M., Neugebauer, M., Goldstein, B. E., Simnett, G.
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description <jats:p>We present results from the May 1997 SOHO‐Ulysses quadrature (SOHO‐Sun‐Ulysses angle=90°), near sunspot minimum. Ulysses was at 5.1 AU, 10° north of the solar equator, and off the east limb. It was also at the very northern edge of the streamer belt. Nevertheless, the Solar Wind Observations Over the Poles of the Sun instrument (SWOOPS) detected only slow, unusually smooth wind and there was no direct evidence of fast wind from the northern polar coronal hole or of mixing with fast wind. The Large‐Angle and Spectrometric Coronagraph (LASCO) images show that the streamer belt at 10°N was narrow and sharp at the beginning and end of the 2 week observation interval, but broadened in the middle. A related change in density, but not flow speed, occurred at Ulysses. Under these conditions it was possible to show that densities derived from the Ultraviolet Coronagraph Spectrometer (UVCS) in the lower corona are closely related to those in the solar wind, both over quiet intervals and in transient events on the limb. Density and velocity in one small transient observed by both LASCO and UVCS are analyzed in detail.</jats:p>
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spelling Suess, S. T. Poletto, G. Romoli, M. Neugebauer, M. Goldstein, B. E. Simnett, G. 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/10.1029/2000ja000044 <jats:p>We present results from the May 1997 SOHO‐Ulysses quadrature (SOHO‐Sun‐Ulysses angle=90°), near sunspot minimum. Ulysses was at 5.1 AU, 10° north of the solar equator, and off the east limb. It was also at the very northern edge of the streamer belt. Nevertheless, the Solar Wind Observations Over the Poles of the Sun instrument (SWOOPS) detected only slow, unusually smooth wind and there was no direct evidence of fast wind from the northern polar coronal hole or of mixing with fast wind. The Large‐Angle and Spectrometric Coronagraph (LASCO) images show that the streamer belt at 10°N was narrow and sharp at the beginning and end of the 2 week observation interval, but broadened in the middle. A related change in density, but not flow speed, occurred at Ulysses. Under these conditions it was possible to show that densities derived from the Ultraviolet Coronagraph Spectrometer (UVCS) in the lower corona are closely related to those in the solar wind, both over quiet intervals and in transient events on the limb. Density and velocity in one small transient observed by both LASCO and UVCS are analyzed in detail.</jats:p> The May 1997 SOHO‐Ulysses quadrature Journal of Geophysical Research: Space Physics
spellingShingle Suess, S. T., Poletto, G., Romoli, M., Neugebauer, M., Goldstein, B. E., Simnett, G., Journal of Geophysical Research: Space Physics, The May 1997 SOHO‐Ulysses quadrature, 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 The May 1997 SOHO‐Ulysses quadrature
title_full The May 1997 SOHO‐Ulysses quadrature
title_fullStr The May 1997 SOHO‐Ulysses quadrature
title_full_unstemmed The May 1997 SOHO‐Ulysses quadrature
title_short The May 1997 SOHO‐Ulysses quadrature
title_sort the may 1997 soho‐ulysses quadrature
title_unstemmed The May 1997 SOHO‐Ulysses quadrature
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/10.1029/2000ja000044