Solar forcing of the semi-annual variation of length-of-day
We study the evolution of the amplitude A of the semi‐annual variation of the length‐of‐day (lod) from 1962 to 2009. We show that A is strongly modulated (up to 30%) by the 11‐yr cycle monitored by the sunspot number WN. A and WN are anticorrelated, WN leading A by 1‐yr. A is therefore directly corr...
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Veröffentlicht in: | Geophysical research letters 2010-08, Vol.37 (15), p.n/a |
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creator | Le Mouël, Jean-Louis Blanter, Elena Shnirman, Mikhail Courtillot, Vincent |
description | We study the evolution of the amplitude A of the semi‐annual variation of the length‐of‐day (lod) from 1962 to 2009. We show that A is strongly modulated (up to 30%) by the 11‐yr cycle monitored by the sunspot number WN. A and WN are anticorrelated, WN leading A by 1‐yr. A is therefore directly correlated with galactic cosmic ray intensity. The main part of the semi‐annual variation in lod is due to the variation in mean zonal winds. We conclude that variations in mean zonal winds are modulated by the solar activity cycle through variations in irradiance, solar wind or cosmic ray intensity. |
doi_str_mv | 10.1029/2010GL043185 |
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We show that A is strongly modulated (up to 30%) by the 11‐yr cycle monitored by the sunspot number WN. A and WN are anticorrelated, WN leading A by 1‐yr. A is therefore directly correlated with galactic cosmic ray intensity. The main part of the semi‐annual variation in lod is due to the variation in mean zonal winds. 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Res. Lett</addtitle><description>We study the evolution of the amplitude A of the semi‐annual variation of the length‐of‐day (lod) from 1962 to 2009. We show that A is strongly modulated (up to 30%) by the 11‐yr cycle monitored by the sunspot number WN. A and WN are anticorrelated, WN leading A by 1‐yr. A is therefore directly correlated with galactic cosmic ray intensity. The main part of the semi‐annual variation in lod is due to the variation in mean zonal winds. We conclude that variations in mean zonal winds are modulated by the solar activity cycle through variations in irradiance, solar wind or cosmic ray intensity.</description><subject>Annual variations</subject><subject>Climate change</subject><subject>Cosmic rays</subject><subject>Cryosphere</subject><subject>Earth</subject><subject>Geodetics</subject><subject>length of day</subject><subject>Ocean-atmosphere interaction</subject><subject>Sciences of the Universe</subject><subject>semi-annual line</subject><subject>Solar activity</subject><subject>solar forcing</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp90EtLxDAQB_AgCq6Pmx-geBSrk0ebBk_ioysUBVcR9hKm3dSN1kaT7up-e7tUxJOnGZjffxiGkAMKJxSYOmVAIS9AcJolG2RElRBxBiA3yQhA9T2T6TbZCeEFADhwOiJnE9egj2rnK9s-R66OurmJgnmzMbbtAptoid5iZ127Hjamfe7msavjGa72yFaNTTD7P3WXPF5fPVyM4-Iuv7k4L-JK0FTFJsmoMhWjiIoL5DNaqyqtRImUsZqWMpGACYrEMMZKJjOhalnxlCblrOwh3yVHw945Nvrd2zf0K-3Q6vF5oW0bFhp4CgkHtqQ9Phzwu3cfCxM6_eIWvu3v0zKlgnMl1uh4QJV3IXhT_66loNev1H9f2XM28E_bmNW_Vuf3BZMgVB-Kh5ANnfn6DaF_1ankMtFPt7meTi6zPJ1O9S3_Bs6dgW4</recordid><startdate>201008</startdate><enddate>201008</enddate><creator>Le Mouël, Jean-Louis</creator><creator>Blanter, Elena</creator><creator>Shnirman, Mikhail</creator><creator>Courtillot, Vincent</creator><general>Blackwell Publishing Ltd</general><general>John Wiley & Sons, Inc</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>1XC</scope><scope>VOOES</scope></search><sort><creationdate>201008</creationdate><title>Solar forcing of the semi-annual variation of length-of-day</title><author>Le Mouël, Jean-Louis ; 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Res. Lett</addtitle><date>2010-08</date><risdate>2010</risdate><volume>37</volume><issue>15</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>We study the evolution of the amplitude A of the semi‐annual variation of the length‐of‐day (lod) from 1962 to 2009. We show that A is strongly modulated (up to 30%) by the 11‐yr cycle monitored by the sunspot number WN. A and WN are anticorrelated, WN leading A by 1‐yr. A is therefore directly correlated with galactic cosmic ray intensity. The main part of the semi‐annual variation in lod is due to the variation in mean zonal winds. We conclude that variations in mean zonal winds are modulated by the solar activity cycle through variations in irradiance, solar wind or cosmic ray intensity.</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2010GL043185</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Annual variations Climate change Cosmic rays Cryosphere Earth Geodetics length of day Ocean-atmosphere interaction Sciences of the Universe semi-annual line Solar activity solar forcing |
title | Solar forcing of the semi-annual variation of length-of-day |
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