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    Rights statement: © 2015 Oberheide et al.; licensee Springer. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.

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The geospace response to variable inputs from the lower atmosphere: a review of the progress made by Task Group 4 of CAWSES-II

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The geospace response to variable inputs from the lower atmosphere: a review of the progress made by Task Group 4 of CAWSES-II. / Oberheide, Jens; Shiokawa, Kazuo; Gurubaran, Subramanian et al.
In: Progress in Earth and Planetary Science, Vol. 2, No. 1, 2, 11.02.2015.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Oberheide, J, Shiokawa, K, Gurubaran, S, Ward, WE, Fujiwara, H, Kosch, MJ, Makela, JJ & Takahashi, H 2015, 'The geospace response to variable inputs from the lower atmosphere: a review of the progress made by Task Group 4 of CAWSES-II', Progress in Earth and Planetary Science, vol. 2, no. 1, 2. https://doi.org/10.1186/s40645-014-0031-4

APA

Oberheide, J., Shiokawa, K., Gurubaran, S., Ward, W. E., Fujiwara, H., Kosch, M. J., Makela, J. J., & Takahashi, H. (2015). The geospace response to variable inputs from the lower atmosphere: a review of the progress made by Task Group 4 of CAWSES-II. Progress in Earth and Planetary Science, 2(1), Article 2. https://doi.org/10.1186/s40645-014-0031-4

Vancouver

Oberheide J, Shiokawa K, Gurubaran S, Ward WE, Fujiwara H, Kosch MJ et al. The geospace response to variable inputs from the lower atmosphere: a review of the progress made by Task Group 4 of CAWSES-II. Progress in Earth and Planetary Science. 2015 Feb 11;2(1):2. doi: 10.1186/s40645-014-0031-4

Author

Oberheide, Jens ; Shiokawa, Kazuo ; Gurubaran, Subramanian et al. / The geospace response to variable inputs from the lower atmosphere : a review of the progress made by Task Group 4 of CAWSES-II. In: Progress in Earth and Planetary Science. 2015 ; Vol. 2, No. 1.

Bibtex

@article{99d2951338d64f2baea3bbbd1542595a,
title = "The geospace response to variable inputs from the lower atmosphere: a review of the progress made by Task Group 4 of CAWSES-II",
abstract = "The advent of new satellite missions, ground-based instrumentation networks, and the development of whole atmosphere models over the past decade resulted in a paradigm shift in understanding the variability of geospace, that is, the region of the atmosphere between the stratosphere and several thousand kilometers above ground where atmosphere-ionosphere-magnetosphere interactions occur. It has now been realized that conditions in geospace are linked strongly to terrestrial weather and climate below, contradicting previous textbook knowledge that the space weather of Earth's near space environment is driven by energy injections at high latitudes connected with magnetosphere-ionosphere coupling and solar radiation variation at extreme ultraviolet wavelengths alone. The primary mechanism through which energy and momentum are transferred from the lower atmosphere is through the generation, propagation, and dissipation of atmospheric waves over a wide range of spatial and temporal scales including electrodynamic coupling through dynamo processes and plasma bubble seeding. The main task of Task Group 4 of SCOSTEP's CAWSES-II program, 2009 to 2013, was to study the geospace response to waves generated by meteorological events, their interaction with the mean flow, and their impact on the ionosphere and their relation to competing thermospheric disturbances generated by energy inputs from above, such as auroral processes at high latitudes. This paper reviews the progress made during the CAWSES-II time period, emphasizing the role of gravity waves, planetary waves and tides, and their ionospheric impacts. Specific campaign contributions from Task Group 4 are highlighted, and future research directions are discussed.",
keywords = "Geospace , Thermosphere, Ionosphere, Tides, Planetary waves, Gravity waves, Traveling ionospheric disturbances, Traveling atmospheric disturbances",
author = "Jens Oberheide and Kazuo Shiokawa and Subramanian Gurubaran and Ward, {William E} and Hitoshi Fujiwara and Kosch, {Michael J.} and Makela, {Jonathan J} and Hisao Takahashi",
note = "{\textcopyright} 2015 Oberheide et al.; licensee Springer. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.",
year = "2015",
month = feb,
day = "11",
doi = "10.1186/s40645-014-0031-4",
language = "English",
volume = "2",
journal = "Progress in Earth and Planetary Science",
issn = "2197-4284",
publisher = "Springer",
number = "1",

}

RIS

TY - JOUR

T1 - The geospace response to variable inputs from the lower atmosphere

T2 - a review of the progress made by Task Group 4 of CAWSES-II

AU - Oberheide, Jens

AU - Shiokawa, Kazuo

AU - Gurubaran, Subramanian

AU - Ward, William E

AU - Fujiwara, Hitoshi

AU - Kosch, Michael J.

AU - Makela, Jonathan J

AU - Takahashi, Hisao

N1 - © 2015 Oberheide et al.; licensee Springer. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.

PY - 2015/2/11

Y1 - 2015/2/11

N2 - The advent of new satellite missions, ground-based instrumentation networks, and the development of whole atmosphere models over the past decade resulted in a paradigm shift in understanding the variability of geospace, that is, the region of the atmosphere between the stratosphere and several thousand kilometers above ground where atmosphere-ionosphere-magnetosphere interactions occur. It has now been realized that conditions in geospace are linked strongly to terrestrial weather and climate below, contradicting previous textbook knowledge that the space weather of Earth's near space environment is driven by energy injections at high latitudes connected with magnetosphere-ionosphere coupling and solar radiation variation at extreme ultraviolet wavelengths alone. The primary mechanism through which energy and momentum are transferred from the lower atmosphere is through the generation, propagation, and dissipation of atmospheric waves over a wide range of spatial and temporal scales including electrodynamic coupling through dynamo processes and plasma bubble seeding. The main task of Task Group 4 of SCOSTEP's CAWSES-II program, 2009 to 2013, was to study the geospace response to waves generated by meteorological events, their interaction with the mean flow, and their impact on the ionosphere and their relation to competing thermospheric disturbances generated by energy inputs from above, such as auroral processes at high latitudes. This paper reviews the progress made during the CAWSES-II time period, emphasizing the role of gravity waves, planetary waves and tides, and their ionospheric impacts. Specific campaign contributions from Task Group 4 are highlighted, and future research directions are discussed.

AB - The advent of new satellite missions, ground-based instrumentation networks, and the development of whole atmosphere models over the past decade resulted in a paradigm shift in understanding the variability of geospace, that is, the region of the atmosphere between the stratosphere and several thousand kilometers above ground where atmosphere-ionosphere-magnetosphere interactions occur. It has now been realized that conditions in geospace are linked strongly to terrestrial weather and climate below, contradicting previous textbook knowledge that the space weather of Earth's near space environment is driven by energy injections at high latitudes connected with magnetosphere-ionosphere coupling and solar radiation variation at extreme ultraviolet wavelengths alone. The primary mechanism through which energy and momentum are transferred from the lower atmosphere is through the generation, propagation, and dissipation of atmospheric waves over a wide range of spatial and temporal scales including electrodynamic coupling through dynamo processes and plasma bubble seeding. The main task of Task Group 4 of SCOSTEP's CAWSES-II program, 2009 to 2013, was to study the geospace response to waves generated by meteorological events, their interaction with the mean flow, and their impact on the ionosphere and their relation to competing thermospheric disturbances generated by energy inputs from above, such as auroral processes at high latitudes. This paper reviews the progress made during the CAWSES-II time period, emphasizing the role of gravity waves, planetary waves and tides, and their ionospheric impacts. Specific campaign contributions from Task Group 4 are highlighted, and future research directions are discussed.

KW - Geospace

KW - Thermosphere

KW - Ionosphere

KW - Tides

KW - Planetary waves

KW - Gravity waves

KW - Traveling ionospheric disturbances

KW - Traveling atmospheric disturbances

U2 - 10.1186/s40645-014-0031-4

DO - 10.1186/s40645-014-0031-4

M3 - Journal article

VL - 2

JO - Progress in Earth and Planetary Science

JF - Progress in Earth and Planetary Science

SN - 2197-4284

IS - 1

M1 - 2

ER -