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  The influence of spectral solar irradiance data on stratospheric heating rates during the 11 year solar cycle

Oberländer, S., Langematz, U., Matthes, K., Kunze, M., Kubin, A., Harder, J., Krivova, N. A., Solanki, S. K., Pagaran, J., Weber, M. (2012): The influence of spectral solar irradiance data on stratospheric heating rates during the 11 year solar cycle. - Geophysical Research Letters, 39, L01801.
https://doi.org/10.1029/2011GL049539

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Datensatz-Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_245420 Versions-Permalink: -
Genre: Zeitschriftenartikel

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Oberländer, S.1, Autor
Langematz, U.1, Autor
Matthes, K.1, Autor
Kunze, M.1, Autor
Kubin, A.1, Autor
Harder, J.1, Autor
Krivova, N. A.1, Autor
Solanki, S. K.1, Autor
Pagaran, J.1, Autor
Weber, Michael2, Autor              
1.3 Earth System Modelling, 1.0 Geodesy and Remote Sensing, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, Autor              
Affiliations:
1External Organizations, ou_persistent22              
2Deutsches GeoForschungsZentrum, ou_persistent13              

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Schlagwörter: Solar minimum and solar cycle differences in SW heating rates and temperature; Comparison of three spectral solar input data sets for solar cycle 22; Comparison of the newly compiled SORCE-data with the commonly used NRLSSI-data
 DDC: 550 - Earth sciences
 Zusammenfassung: Heating rate calculations with the FUBRad shortwave (SW) radiation parameterization have been performed to examine the effect of prescribed spectral solar fluxes from the NRLSSI, MPS and IUP data sets on SW heating rates over the 11 year solar cycle 22. The corresponding temperature response is derived from perpetual January General Circulation Model (GCM) simulations with prescribed ozone concentrations. The different solar flux input data sets induce clear differences in SW heating rates at solar minimum, with the established NRLSSI data set showing the smallest solar heating rates. The stronger SW heating in the middle and upper stratosphere in the MPS data warms the summer upper stratosphere by 2 K. Over the solar cycle, SW heating rate differences vary up to 40% between the irradiance data sets, but do not result in a significant change of the solar temperature signal. Lower solar fluxes in the newer SIM data lead to a significantly cooler stratosphere and mesosphere when compared to NRLSSI data for 2007. Changes in SW heating from 2004 to 2007 are however up to six times stronger than for the NRLSSI data.

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 Datum: 2012
 Publikationsstatus: Final veröffentlicht
 Seiten: -
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: -
 Identifikatoren: eDoc: 18877
GFZPOF: PT1 Planet Earth: Global Processes and Change
DOI: 10.1029/2011GL049539
 Art des Abschluß: -

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Titel: Geophysical Research Letters
Genre der Quelle: Zeitschrift, SCI, Scopus, ab 2023 oa
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Seiten: - Band / Heft: 39 (L01801) Artikelnummer: - Start- / Endseite: - Identifikator: CoNE: https://gfzpublic.gfz-potsdam.de/cone/journals/resource/journals182