b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China

Variations of the atmospheric angular momentum "AAM # is responsible for almost all of the observed length!of!day "LOD # variation on time scales from several days to several years \ and much of the observed polar motion on the intra!seasonal time scale [ El Nino:Southern Oscillation "...

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Main Author: Benjamin Fong
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.7746
http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.613.7746 2023-05-15T17:33:22+02:00 b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China Benjamin Fong The Pennsylvania State University CiteSeerX Archives 886 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.7746 http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.7746 http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf text ftciteseerx 2016-01-08T14:38:27Z Variations of the atmospheric angular momentum "AAM # is responsible for almost all of the observed length!of!day "LOD # variation on time scales from several days to several years \ and much of the observed polar motion on the intra!seasonal time scale [ El Nino:Southern Oscillation "ENSO # and Quasi!Biennial Oscillation "QBO # have been singled out to successfully explain interannual LOD variations [ However\ excitation sources for the interannual polar motion \ including the 03 month Chandler wobble \ have not been positively identi_ed [ This paper studies the correlation of the observed polar motion C with the North Atlantic Oscillation "NAO# \ an interannual \ mid!latitude \ north!south seesaw in the atmosphere!ocean system [ An index "NAOI # used as a proxy to measure the strength of NAO is compared with the observed interannual polar motion excitation during 08530883 [ Cross!correlation functions and coherence spectra demonstrate signi_cant correlations between NAOI and C \ especially in the x component as expected from NAO|s location and general pattern [ This constitutes a positive identi_cation of excitation of interannual polar motion by a meteorological system [ Furthermore \ our corresponding results with respect to ENSO strongly suggest that a combination of meteorological systems will better explain the observed interannual Text North Atlantic North Atlantic oscillation Unknown Chandler ENVELOPE(-59.682,-59.682,-64.490,-64.490)
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description Variations of the atmospheric angular momentum "AAM # is responsible for almost all of the observed length!of!day "LOD # variation on time scales from several days to several years \ and much of the observed polar motion on the intra!seasonal time scale [ El Nino:Southern Oscillation "ENSO # and Quasi!Biennial Oscillation "QBO # have been singled out to successfully explain interannual LOD variations [ However\ excitation sources for the interannual polar motion \ including the 03 month Chandler wobble \ have not been positively identi_ed [ This paper studies the correlation of the observed polar motion C with the North Atlantic Oscillation "NAO# \ an interannual \ mid!latitude \ north!south seesaw in the atmosphere!ocean system [ An index "NAOI # used as a proxy to measure the strength of NAO is compared with the observed interannual polar motion excitation during 08530883 [ Cross!correlation functions and coherence spectra demonstrate signi_cant correlations between NAOI and C \ especially in the x component as expected from NAO|s location and general pattern [ This constitutes a positive identi_cation of excitation of interannual polar motion by a meteorological system [ Furthermore \ our corresponding results with respect to ENSO strongly suggest that a combination of meteorological systems will better explain the observed interannual
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Benjamin Fong
spellingShingle Benjamin Fong
b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China
author_facet Benjamin Fong
author_sort Benjamin Fong
title b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China
title_short b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China
title_full b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China
title_fullStr b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China
title_full_unstemmed b Shan‘hai Astronomical Observatory \ Chinese Academy of Sciences \ Shan‘hai \ China
title_sort b shan‘hai astronomical observatory \ chinese academy of sciences \ shan‘hai \ china
publishDate
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.613.7746
http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf
long_lat ENVELOPE(-59.682,-59.682,-64.490,-64.490)
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North Atlantic oscillation
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North Atlantic oscillation
op_source http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf
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http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1999-Chao-JG-Meteorological excitation of interannual polar motion by the North Atlantic Oscillation.pdf
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