  <eprint xmlns="http://eprints.org/ep2/data/2.0">
    <eprintid>6993</eprintid>
    <rev_number>32</rev_number>
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    <datestamp>2008-07-25 03:23:21</datestamp>
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    <type>article</type>
    <metadata_visibility>show</metadata_visibility>
    <contact_email>Christopher.Watson@utas.edu.au</contact_email>
    <creators>
      <item>
        <name>
          <family>King</family>
          <given>MA</given>
        </name>
        <id></id>
      </item>
      <item>
        <name>
          <family>Watson</family>
          <given>CS</given>
        </name>
        <id>Christopher.Watson@utas.edu.au</id>
      </item>
      <item>
        <name>
          <family>Penna</family>
          <given>NT</given>
        </name>
        <id></id>
      </item>
      <item>
        <name>
          <family>Clarke</family>
          <given>PJ</given>
        </name>
        <id></id>
      </item>
    </creators>
    <title>Subdaily signals in GPS observations and their effect at semiannual and annual periods</title>
    <ispublished>pub</ispublished>
    <for08>
      <item>040499</item>
      <item>040402</item>
    </for08>
    <seo08>
      <item>969902</item>
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    <full_text_status>restricted</full_text_status>
    <keywords>GPS; sub-daily signals; geophysical loading</keywords>
    <note>Copyright 2008 by the American Geophysical Union.</note>
    <abstract>Estimates of seasonal geophysical loading from GPS&#13;
may be biased by propagated unmodeled subdaily signals.&#13;
Although the major geophysical signals at semidiurnal and&#13;
diurnal frequencies are now routinely modeled in GPS&#13;
analyses, the characteristics of unmodeled or mismodeled&#13;
subdaily signals are not well known. Here, using site&#13;
coordinates estimated every 5 minutes, we examine the&#13;
subdaily coordinate spectral characteristics for ~90 global&#13;
GPS sites. Unmodeled signals with amplitudes at the 10 mm&#13;
level are present at frequencies between ~1/day and the&#13;
Nyquist frequency. These are shown to propagate into 24 h&#13;
solutions with (among other frequencies) annual and&#13;
semiannual periods with amplitudes up to 5 mm, with a&#13;
median amplitude in the height component of 0.8 mm&#13;
(annual) and 0.6 mm (semiannual). They are shown to bias&#13;
low-degree spherical harmonics estimates of geophysical&#13;
loading at the level of 5–10%, although the exact effect will be network dependent.</abstract>
    <date>2008</date>
    <date_type>published</date_type>
    <publication>Geophysical Research Letters</publication>
    <volume>35</volume>
    <number>L03302</number>
    <pagerange>1-5</pagerange>
    <id_number>10.1029/2007GL032252</id_number>
    <refereed>TRUE</refereed>
    <issn>0094-8276</issn>
    <official_url>http://dx.doi.org/10.1029/2007GL032252</official_url>
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