Jon Baker

Li, Y., Yang, Y.,  Wang, X.,  Luo, W.,  Zhao, J., Sun, Z., Ye, Z., Chen, X., Shi, X., Xu, Y., Baker, J.L. (2024): Sources and transport of CO2 in the karst system of Jiguan Cave, Funiu Mountains, China. - Science of The Total Environment, 918, 170507, DOI: 10.1016/j.scitotenv.2024.170507.

Wolf, A., Baker, J.L., Tjallingii, R., Cai, Y., Osinzev, A., Antonosyan, M., Amano, N., Johnson, K.R., Skiba, V., McCormack, J., Kwiecien, O., Chervyatsova, O.Y., Dublyansky, Y.V., Dbar, R.S., Cheng, H., Breitenbach, S.F.M. (2024): Western Caucasus regional hydroclimate controlled by cold-season temperature variability since the Last Glacial Maximum. - Communications Earth & Environment, 5:66, doi:10.1038/s43247-023-01151-3.

Dong, X., Kathayat, G., Rasmussen, S.O.,  Svensson, A., Severinghaus, J., Li, H., Sinha, A., Yao, X.,. Zhang, H., Shi, Z., Cai, Y., Pérez-Mejías, C., Baker, J., Zhao, J., Spötl, C., Columbu, A., Ning, Y., Stríkis, N., Chen, S., Wang, X., Gupta, A.K., Dutt, S., Zhang, F., Cruz, F., An, Z., Edwards, R.L., Cheng, H. (2022): Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2. – Nature Communications, 13: 5867, doi: 10.1038/s41467-022-33583-4.

Cheng, H., Zhang, H., Cai, Y., Shi, Z., Yi, L., Deng, C., Hao, Q., Peng, Y., Sinha, A., Li, H., Zhao, J., Tian, Y., Baker, J.L., Perez-Mejias, C. (2021): Orbital-scale Asian summer monsoon variations: Paradox and exploration. - Sci. China Earth Sci., 64, 529-544, doi.org/10.1007/s11430-020-9720-y.

Cheng, H., Xu, Y., Dong, X., Zhao, J., Li, H., Baker, J., Sinha, A., Spötl, C., Zhang, H., Du, W., Zong, B., Jia, X., Kathayat, G., Liu, D., Cai, Y., Wang, X., Strikis, N.M., Cruz, F.W., Auler, A.S., Gupta, A.K., Singh, R.K., Jaglan, S., Dutt, S., Liu, Z., Edwards, R.L. (2021): Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics. – Communications Earth & Environment, 2:230, https://doi.org/10.1038/s43247-021-00304-6.

Li, T-.Y., Baker, J.L., Wang, T., Zhang, J., Wu, Y., Li, H., Blyakharchuk, T., Yu, T., Shen, C., Cheng, H., Kong, X., Xie, W., and Edwards, L.R. (2021): Early Holocene permafrost retreat in Siberia amplified by reorganization of westerly circulation. - Communications Earth & Environment, 2, 199, doi.org/10.1038/s43247-021-00238-z.

Zhang, H., Zhang, X., Cai, Y., Sinha, A., Spötl, C., Baker, J., Kathayat, G., Liu, Z., Tian, Y., Lu, J., Wang, Z., Zhao, J., Jia, X., Du, W., Ning, Y., An, Z., Edwards, R.L., Cheng, H. (2021): A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon. – Quaternary Science Reviews, 261, 106911.

Sha, L., Mahata, S., Duan, P., Luz, B., Zhang, P., Zong, B., Ning, Y., Zhang, H., Baker, J.L., Edwards, L.R., Cheng, H. (2020): A novel application of triple oxygen isotope ratios of speleothems. - Geochimica et Cosmochimica Acta, 270, 360–378, doi.org/10.1016/j.gca.2019.12.003.

Cheng, H., Zhang, H.,  Spötl, C., Baker, J., Sinha, A., Li, H., Bartolomé, M., Moreno, A., Kathayat, G., Zhao, J., Dong, X., Li, Y., Ning, Y., Jia, X., Zong, B., Ait Brahim, Y., Pérez-Mejías, C., Cai, Y., Novello, V.F., Cruz, F.C., Severinghaus, J.P., An, Z., Edwards, R.L. (2020): Timing and structure of the Younger Dryas event and its underlying climate dynamics. - Proceedings of the National Academy of Sciences, 117, 23408-23417.

Zhang, H., Ait Brahim, Y., Li, H., Zhao, J., Kathayat, G., Tian, Y., Baker, J.L., Wang, J., Zhang, F., Ning, Y., Edwards, R.L., Cheng, H. (2019): The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records. - Quaternary, 2,1–38, doi:10.3390/quat2030026.

Zhao, X., Cheng, H., Sinha, A., Zhang, H., Baker, J.L., Chen, S., Kong, X., Wang, Y., Edwards, R.L., Ning, Y., and Zhao, J. (2019): A High-Resolution Speleothem Record of Marine Isotope Stage 11 as a Natural Analog to Holocene Asian Summer Monsoon Variations. - Geophysical Research Letters, 46, 1–9, doi.org/10.1029/2019GL083836.

Baker, J.L., Lachniet, M.S.L., Chervyatsova, O., Asmerom, Y., and Polyak, V. (2017): Holocene Warming in Western Continental Eurasia Driven By Glacial Retreat and Greenhouse Forcing. - Nature Geoscience, 10, 430–435.