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This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.

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A list of all pages that have property "Basis" with value "Alkenone calibration to SST". Since there have been only a few results, also nearby values are displayed.

Showing below up to 17 results starting with #1.

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List of results

    • Unknown.5b9f845cc5a5b  + (The coral 18O record from this site re- flects primarily SST; a linear regression of coral 18O versus SST yields a slope of0.24 per mil (‰) 18O per 1°C, explaining 47% of the SST variance (20).)
    • Unknown.5bc0f85b7c9e8  + (The coral 18O record from this site re- flects primarily SST; a linear regression of coral 18O versus SST yields a slope of0.24 per mil (‰) 18O per 1°C, explaining 47% of the SST variance (20).)
    • Unknown.5c88860999eff  + (The coral 18O record from this site re- flects primarily SST; a linear regression of coral 18O versus SST yields a slope of0.24 per mil (‰) 18O per 1°C, explaining 47% of the SST variance (20).)
    • Unknown.58faccab23daf  + (annual growth anomaly calibration to SST)
    • Unknown.58fac3fa34c68  + (correlation)
    • Unknown.58fac957e94de  + (correlation with local meteorological correlation)
    • Unknown.58fac9bb64635  + (correlation with local meteorological correlation)
    • Unknown.58faca0fa5453  + (correlation with local meteorological correlation)
    • Unknown.58facf8a0fb97  + (d18O calibration to T assuming constant d18Ow)
    • Unknown.5b9f845cc5aa0  + (dditional variability in coral 18O may ari …
      dditional variability in coral 18O may arise from vari- ations in the 18O of seawater due to precip- itation, evaporation, or runoff, but at this site these changes are likely to be secondary be- cause local rainfall 18O is not strongly de- pleted from average seawater (21) and salin- ity gradients are small (22). Rainfall and SST influences are likely to be additive in terms of annual effect on coral 18O because warmer years tend to be wetter at this site.
      rmer years tend to be wetter at this site.)
    • Unknown.5bc0f85b7ca31  + (dditional variability in coral 18O may ari …
      dditional variability in coral 18O may arise from vari- ations in the 18O of seawater due to precip- itation, evaporation, or runoff, but at this site these changes are likely to be secondary be- cause local rainfall 18O is not strongly de- pleted from average seawater (21) and salin- ity gradients are small (22). Rainfall and SST influences are likely to be additive in terms of annual effect on coral 18O because warmer years tend to be wetter at this site.
      rmer years tend to be wetter at this site.)
    • Unknown.5c88860999f47  + (dditional variability in coral 18O may ari …
      dditional variability in coral 18O may arise from vari- ations in the 18O of seawater due to precip- itation, evaporation, or runoff, but at this site these changes are likely to be secondary be- cause local rainfall 18O is not strongly de- pleted from average seawater (21) and salin- ity gradients are small (22). Rainfall and SST influences are likely to be additive in terms of annual effect on coral 18O because warmer years tend to be wetter at this site.
      rmer years tend to be wetter at this site.)
    • Unknown.58fabe93022d1  + (linear regression, correlation with CRU data)
    • Unknown.58facf8a0f684  + (lower limit of 95% ci of difference in Sr/Ca between -20 and -125m, divided by difference in observed T at those depths.)
    • Unknown.58fa5a0f43a02  + (monthly Sr/Ca calibrated to observed SST (DRTO))
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