Fig. 3: Comparison of CB2 δ18O to various potential forcings. | Nature Communications

Fig. 3: Comparison of CB2 δ18O to various potential forcings.

From: Dynamic and thermodynamic influences on precipitation in Northeast Mexico on orbital to millennial timescales

Fig. 3: Comparison of CB2 δ18O to various potential forcings.

a Autumn (SON, r = −0.48, p < 0.14, orange) and Summer (JJA, r = −0.26 p = 0.46 black) insolation. b Atmospheric pCO2 (r = −0.61, p < 0.01, maroon109). c SSTs from Gulf of Mexico (r = −0.52, p < 0.03, silver59), Caribbean (r = −0.59, p < 0.05, lime green58), Tropical N. Pacific (r = −0.55, p < 0.03, magenta56) and Tropical N. Atlantic (r = −0.73, p < 0.01, teal57). d Greenland temperatures (r = −0.61, p < 0.01, indigo110).

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