author_facet Siscoe, G. L.
Crooker, N. U.
Siebert, K. D.
Siscoe, G. L.
Crooker, N. U.
Siebert, K. D.
author Siscoe, G. L.
Crooker, N. U.
Siebert, K. D.
spellingShingle Siscoe, G. L.
Crooker, N. U.
Siebert, K. D.
Journal of Geophysical Research: Space Physics
Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
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 siscoe, g. l.
spelling Siscoe, G. L. Crooker, N. U. Siebert, K. D. 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/10.1029/2001ja009176 <jats:p>MHD simulations give about the same dependence of transpolar potential on solar wind electric field (IEF) as the Hill model of transpolar potential, including saturation and dependence on ram pressure. In the Hill model, feedback of the region 1 current system is presumed to limit the rate of reconnection at the magnetopause thereby causing transpolar potential saturation. MHD simulations add as relevant information that in the saturation domain the region 1 current system usurps the role of the Chapman‐Ferraro current system, which disappears. This means that the region 1 current system takes on the role of providing the current and generating most of the magnetic field in the <jats:bold>J</jats:bold> × <jats:bold>B</jats:bold> force at the magnetopause that balances solar wind ram pressure. Viewed from this perspective, transpolar potential saturation results not from the region 1 current system limiting the rate of reconnection at the magnetopause but instead from ram pressure (more accurately, total solar wind stresses) limiting the total amount of current that can flow in the region 1 current system. Transpolar potential saturation is then the limit on transpolar potential that corresponds to the ram‐pressure limit on total region 1 current.</jats:p> Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure Journal of Geophysical Research: Space Physics
doi_str_mv 10.1029/2001ja009176
facet_avail Online
Free
finc_class_facet Technik
Geologie und Paläontologie
Geographie
Chemie und Pharmazie
Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
Biologie
Allgemeine Naturwissenschaft
Physik
format ElectronicArticle
fullrecord blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDAxamEwMDkxNzY
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDAxamEwMDkxNzY
institution DE-Gla1
DE-Zi4
DE-15
DE-Pl11
DE-Rs1
DE-105
DE-14
DE-Ch1
DE-L229
DE-D275
DE-Bn3
DE-Brt1
DE-Zwi2
DE-D161
imprint American Geophysical Union (AGU), 2002
imprint_str_mv American Geophysical Union (AGU), 2002
issn 0148-0227
issn_str_mv 0148-0227
language English
mega_collection American Geophysical Union (AGU) (CrossRef)
match_str siscoe2002transpolarpotentialsaturationrolesofregion1currentsystemandsolarwindrampressure
publishDateSort 2002
publisher American Geophysical Union (AGU)
recordtype ai
record_format ai
series Journal of Geophysical Research: Space Physics
source_id 49
title Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_unstemmed Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_full Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_fullStr Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_full_unstemmed Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_short Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_sort transpolar potential saturation: roles of region 1 current system and solar wind ram pressure
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/10.1029/2001ja009176
publishDate 2002
physical
description <jats:p>MHD simulations give about the same dependence of transpolar potential on solar wind electric field (IEF) as the Hill model of transpolar potential, including saturation and dependence on ram pressure. In the Hill model, feedback of the region 1 current system is presumed to limit the rate of reconnection at the magnetopause thereby causing transpolar potential saturation. MHD simulations add as relevant information that in the saturation domain the region 1 current system usurps the role of the Chapman‐Ferraro current system, which disappears. This means that the region 1 current system takes on the role of providing the current and generating most of the magnetic field in the <jats:bold>J</jats:bold> × <jats:bold>B</jats:bold> force at the magnetopause that balances solar wind ram pressure. Viewed from this perspective, transpolar potential saturation results not from the region 1 current system limiting the rate of reconnection at the magnetopause but instead from ram pressure (more accurately, total solar wind stresses) limiting the total amount of current that can flow in the region 1 current system. Transpolar potential saturation is then the limit on transpolar potential that corresponds to the ram‐pressure limit on total region 1 current.</jats:p>
container_issue A10
container_start_page 0
container_title Journal of Geophysical Research: Space Physics
container_volume 107
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
_version_ 1792338352063643653
geogr_code not assigned
last_indexed 2024-03-01T15:30:39.035Z
geogr_code_person not assigned
openURL url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Transpolar+potential+saturation%3A+Roles+of+region+1+current+system+and+solar+wind+ram+pressure&rft.date=2002-10-01&genre=article&issn=0148-0227&volume=107&issue=A10&jtitle=Journal+of+Geophysical+Research%3A+Space+Physics&atitle=Transpolar+potential+saturation%3A+Roles+of+region+1+current+system+and+solar+wind+ram+pressure&aulast=Siebert&aufirst=K.+D.&rft_id=info%3Adoi%2F10.1029%2F2001ja009176&rft.language%5B0%5D=eng
SOLR
_version_ 1792338352063643653
author Siscoe, G. L., Crooker, N. U., Siebert, K. D.
author_facet Siscoe, G. L., Crooker, N. U., Siebert, K. D., Siscoe, G. L., Crooker, N. U., Siebert, K. D.
author_sort siscoe, g. l.
container_issue A10
container_start_page 0
container_title Journal of Geophysical Research: Space Physics
container_volume 107
description <jats:p>MHD simulations give about the same dependence of transpolar potential on solar wind electric field (IEF) as the Hill model of transpolar potential, including saturation and dependence on ram pressure. In the Hill model, feedback of the region 1 current system is presumed to limit the rate of reconnection at the magnetopause thereby causing transpolar potential saturation. MHD simulations add as relevant information that in the saturation domain the region 1 current system usurps the role of the Chapman‐Ferraro current system, which disappears. This means that the region 1 current system takes on the role of providing the current and generating most of the magnetic field in the <jats:bold>J</jats:bold> × <jats:bold>B</jats:bold> force at the magnetopause that balances solar wind ram pressure. Viewed from this perspective, transpolar potential saturation results not from the region 1 current system limiting the rate of reconnection at the magnetopause but instead from ram pressure (more accurately, total solar wind stresses) limiting the total amount of current that can flow in the region 1 current system. Transpolar potential saturation is then the limit on transpolar potential that corresponds to the ram‐pressure limit on total region 1 current.</jats:p>
doi_str_mv 10.1029/2001ja009176
facet_avail Online, Free
finc_class_facet Technik, Geologie und Paläontologie, Geographie, Chemie und Pharmazie, Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft, Biologie, Allgemeine Naturwissenschaft, Physik
format ElectronicArticle
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
geogr_code not assigned
geogr_code_person not assigned
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDAxamEwMDkxNzY
imprint American Geophysical Union (AGU), 2002
imprint_str_mv American Geophysical Union (AGU), 2002
institution DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161
issn 0148-0227
issn_str_mv 0148-0227
language English
last_indexed 2024-03-01T15:30:39.035Z
match_str siscoe2002transpolarpotentialsaturationrolesofregion1currentsystemandsolarwindrampressure
mega_collection American Geophysical Union (AGU) (CrossRef)
physical
publishDate 2002
publishDateSort 2002
publisher American Geophysical Union (AGU)
record_format ai
recordtype ai
series Journal of Geophysical Research: Space Physics
source_id 49
spelling Siscoe, G. L. Crooker, N. U. Siebert, K. D. 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/10.1029/2001ja009176 <jats:p>MHD simulations give about the same dependence of transpolar potential on solar wind electric field (IEF) as the Hill model of transpolar potential, including saturation and dependence on ram pressure. In the Hill model, feedback of the region 1 current system is presumed to limit the rate of reconnection at the magnetopause thereby causing transpolar potential saturation. MHD simulations add as relevant information that in the saturation domain the region 1 current system usurps the role of the Chapman‐Ferraro current system, which disappears. This means that the region 1 current system takes on the role of providing the current and generating most of the magnetic field in the <jats:bold>J</jats:bold> × <jats:bold>B</jats:bold> force at the magnetopause that balances solar wind ram pressure. Viewed from this perspective, transpolar potential saturation results not from the region 1 current system limiting the rate of reconnection at the magnetopause but instead from ram pressure (more accurately, total solar wind stresses) limiting the total amount of current that can flow in the region 1 current system. Transpolar potential saturation is then the limit on transpolar potential that corresponds to the ram‐pressure limit on total region 1 current.</jats:p> Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure Journal of Geophysical Research: Space Physics
spellingShingle Siscoe, G. L., Crooker, N. U., Siebert, K. D., Journal of Geophysical Research: Space Physics, Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure, 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 Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_full Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_fullStr Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_full_unstemmed Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_short Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
title_sort transpolar potential saturation: roles of region 1 current system and solar wind ram pressure
title_unstemmed Transpolar potential saturation: Roles of region 1 current system and solar wind ram pressure
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/10.1029/2001ja009176