Solar X-Ray Spectral Irradiance Variability
Solar spectral irradiance at X-ray wavelengths show large variations over a period of solar cycle. We use X-ray irradiance data in three narrow spectral regimes deduced from Yohkoh SXT measurements to study coronal irradiance and their possible association with the activity in the lower atmosphere....
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Veröffentlicht in: | Solar physics 2006-04, Vol.234 (2), p.393-408 |
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creator | Ramesh, K B Raman, K Sundara |
description | Solar spectral irradiance at X-ray wavelengths show large variations over a period of solar cycle. We use X-ray irradiance data in three narrow spectral regimes deduced from Yohkoh SXT measurements to study coronal irradiance and their possible association with the activity in the lower atmosphere. Time variation of the X-ray irradiance is important in understanding the emergence of magnetic flux and the effects of such variation on the upper atmosphere of the Earth. We note that about 66% of the total (2 - 30 Å) X-ray irradiance arise from 10 to 20 Å spectral range, while 2 - 10 Å contribute only about 3% of the total. The time variation in 2 - 10 and 10 - 20 Å ranges follow each other closely. Further they follow closely the solar indices such as sunspot, F^sub 10.7^, and plage indices, although similarity in the variation of 10 - 20 Å is quite apparent. However, the variation in the other spectral band (20 - 30 Å) differ to a large extent except for the solar cycle dependent variation. We infer that in addition to the active regions, the remnants of active regions contribute considerably to the emission in this spectral range.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1007/s11207-006-1973-5 |
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We use X-ray irradiance data in three narrow spectral regimes deduced from Yohkoh SXT measurements to study coronal irradiance and their possible association with the activity in the lower atmosphere. Time variation of the X-ray irradiance is important in understanding the emergence of magnetic flux and the effects of such variation on the upper atmosphere of the Earth. We note that about 66% of the total (2 - 30 Å) X-ray irradiance arise from 10 to 20 Å spectral range, while 2 - 10 Å contribute only about 3% of the total. The time variation in 2 - 10 and 10 - 20 Å ranges follow each other closely. Further they follow closely the solar indices such as sunspot, F^sub 10.7^, and plage indices, although similarity in the variation of 10 - 20 Å is quite apparent. However, the variation in the other spectral band (20 - 30 Å) differ to a large extent except for the solar cycle dependent variation. 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We infer that in addition to the active regions, the remnants of active regions contribute considerably to the emission in this spectral range.[PUBLICATION ABSTRACT]</description><subject>Atmosphere</subject><subject>Solar physics</subject><subject>Sunspots</subject><subject>Upper atmosphere</subject><subject>Wavelengths</subject><issn>0038-0938</issn><issn>1573-093X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kLFOwzAQhi0EEqXwAGwRAwwocPbFdjyiqkClSkgUUDfr4rhSqrQpdjr07XFUJgZuuRu--0_3MXbN4YED6MfIuQCdA6icG425PGEjLtMABpenbASA5TCX5-wixjXAsCVH7H7RtRSyZf5Oh2yx864P1GazEKhuaOt89kWhoappm_5wyc5W1EZ_9dvH7PN5-jF5zedvL7PJ0zx3iLLPyQvvC4OyKlMVpFeOGw_cGyG5r5EKobwCUQllsFZOuwqBVEkCq0rIGsfs7pi7C9333sfebprofNvS1nf7aHWBSqRTkMjbf0luhFGqKBN48wdcd_uwTV9YjUUKLA1PED9CLnQxBr-yu9BsKBwsBzv4skfLNlm2g2Ur8Qe6D20r</recordid><startdate>20060401</startdate><enddate>20060401</enddate><creator>Ramesh, K B</creator><creator>Raman, K Sundara</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20060401</creationdate><title>Solar X-Ray Spectral Irradiance Variability</title><author>Ramesh, K B ; Raman, K Sundara</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c335t-ae2ee4935b88884a7fc19e01e9251ed3a426e602b2693d6c7cb30a68a23bb25d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Atmosphere</topic><topic>Solar physics</topic><topic>Sunspots</topic><topic>Upper atmosphere</topic><topic>Wavelengths</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ramesh, K B</creatorcontrib><creatorcontrib>Raman, K Sundara</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><jtitle>Solar physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ramesh, K B</au><au>Raman, K Sundara</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Solar X-Ray Spectral Irradiance Variability</atitle><jtitle>Solar physics</jtitle><date>2006-04-01</date><risdate>2006</risdate><volume>234</volume><issue>2</issue><spage>393</spage><epage>408</epage><pages>393-408</pages><issn>0038-0938</issn><eissn>1573-093X</eissn><abstract>Solar spectral irradiance at X-ray wavelengths show large variations over a period of solar cycle. 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title | Solar X-Ray Spectral Irradiance Variability |
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