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CP | Articles | Volume 14, issue 4
Clim. Past, 14, 559–575, 2018
https://doi.org/10.5194/cp-14-559-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 14, 559–575, 2018
https://doi.org/10.5194/cp-14-559-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 26 Apr 2018

Research article | 26 Apr 2018

Recent climate variations in Chile: constraints from borehole temperature profiles

Carolyne Pickler et al.

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Cited articles

Beltrami, H. and Mareschal, J.-C.: Ground temperature histories for central and eastern Canada from geothermal measurements: Little Ice Age signature, Geophys. Res. Lett., 19, 689–692, https://doi.org/10.1029/92GL00671, 1992. a
Beltrami, H., Cheng, L., and Mareschal, J. C.: Simultaneous inversion of borehole temperature data for determination of ground surface temperature history, Geophys. J. Int., 129, 311–318, https://doi.org/10.1111/j.1365-246X.1997.tb01584.x, 1997. a
Benfield, A.: The effect of uplift and denudation on underground temperatures, J. Appl. Phys., 20, 66–70, https://doi.org/10.1063/1.1698238, 1949. a
Bobst, A. L., Lowenstein, T. K., Jordan, T. E., Godfrey, L. V., Ku, T.-L., and Luo, S.: A 106ka paleoclimate record from drill core of the Salar de Atacama, northern Chile, Palaeogeogr. Palaeocl., 173, 21–42, https://doi.org/10.1016/S0031-0182(01)00308-X, 2001. a
Braconnot, P., Harrison, S. P., Kageyama, M., Bartlein, P. J., Masson-Delmotte, V., Abe-Ouchi, A., Otto-Bliesner, B., and Zhao, Y.: Evaluation of climate models using palaeoclimatic data, Nature Clim. Change, 2, 417–424, https://doi.org/10.1038/nclimate1456, 2012. a
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We compiled 31 temperature–depth profiles to reconstruct the ground surface temperature of the last 500 years in northern Chile. They suggest that the region experienced a cooling from 1850 to 1980 followed by a warming of 1.9 K. The cooling could coincide with a cooling interval in 1960. The warming is greater than that of proxy reconstructions for nearby regions and model simulations. These differences could be due to differences in spatial and temporal resolution between data and models.
We compiled 31 temperature–depth profiles to reconstruct the ground surface temperature of the...
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