17
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Property:Basis
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Latest revision as of 20:15, 14 September 2016
- Property Type: Text
Pages using the property "Basis"
Showing 17 pages using this property.
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| Unknown.58fa5a0f43a02 + | monthly Sr/Ca calibrated to observed SST (DRTO) + |
| Unknown.58fabe93022d1 + | linear regression, correlation with CRU data + |
| 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.58faca81ad778 + | Alkenone calibration to SST + |
| Unknown.58faca81ae7d3 + | Alkenone calibration to SST + |
| Unknown.58faccab23daf + | annual growth anomaly calibration to SST + |
| 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.58facf8a0fb97 + | d18O calibration to T assuming constant d18Ow + |
| 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.5b9f845cc5aa0 + | 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. + |
| 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.5bc0f85b7ca31 + | 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. + |
| 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.5c88860999f47 + | 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. + |
