Articles | Volume 13, issue 12
https://doi.org/10.5194/cp-13-1851-2017
https://doi.org/10.5194/cp-13-1851-2017
Review article
 | 
20 Dec 2017
Review article |  | 20 Dec 2017

Comparing proxy and model estimates of hydroclimate variability and change over the Common Era

PAGES Hydro2k Consortium

Related subject area

Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Centennial-Decadal
Drought reconstruction since 1796 CE based on tree-ring widths in the upper Heilongjiang (Amur) River basin in Northeast Asia and its linkage to Pacific Ocean climate variability
Yang Xu, Heli Zhang, Feng Chen, Shijie Wang, Mao Hu, Martín Hadad, and Fidel Roig
Clim. Past, 19, 2079–2092, https://doi.org/10.5194/cp-19-2079-2023,https://doi.org/10.5194/cp-19-2079-2023, 2023
Short summary
A past and present perspective on the European summer vapour pressure deficit
Viorica Nagavciuc, Simon L. L. Michel, Daniel F. Balting, Gerhard Helle, Mandy Freund, Gerhard H. Schleser, David N. Steger, Gerrit Lohmann, and Monica Ionita
Clim. Past Discuss., https://doi.org/10.5194/cp-2023-35,https://doi.org/10.5194/cp-2023-35, 2023
Revised manuscript accepted for CP
Short summary
Drought increase since the mid-20th century in the northern South American Altiplano revealed by a 389-year precipitation record
Mariano S. Morales, Doris B. Crispín-DelaCruz, Claudio Álvarez, Duncan A. Christie, M. Eugenia Ferrero, Laia Andreu-Hayles, Ricardo Villalba, Anthony Guerra, Ginette Ticse-Otarola, Ernesto C. Rodríguez-Ramírez, Rosmery LLocclla-Martínez, Joali Sanchez-Ferrer, and Edilson J. Requena-Rojas
Clim. Past, 19, 457–476, https://doi.org/10.5194/cp-19-457-2023,https://doi.org/10.5194/cp-19-457-2023, 2023
Short summary
Climate change detection and attribution using observed and simulated tree-ring width
Jörg Franke, Michael N. Evans, Andrew Schurer, and Gabriele C. Hegerl
Clim. Past, 18, 2583–2597, https://doi.org/10.5194/cp-18-2583-2022,https://doi.org/10.5194/cp-18-2583-2022, 2022
Short summary
Integrating plant wax abundance and isotopes for paleo-vegetation and paleoclimate reconstructions: a multi-source mixing model using a Bayesian framework
Deming Yang and Gabriel J. Bowen
Clim. Past, 18, 2181–2210, https://doi.org/10.5194/cp-18-2181-2022,https://doi.org/10.5194/cp-18-2181-2022, 2022
Short summary

Cited articles

Aggarwal, P. K., Frohlich, K., Kulkarni, K. M., and Gourcy, L. L.: Stable isotope evidence for moisture sources in the Asian summer monsoon under present and past climate regimes, Geophys. Res. Lett., 31, L08203, https://doi.org/10.1029/2004gl019911, 2004.
Aggarwal, P. K., Alduchov, O. A., Froehlich, K. O., Araguas-Araguas, L. J., Sturchio, N. C., and Kurita, N.: Stable isotopes in global precipitation: A unified interpretation based on atmospheric moisture residence time, Geophys. Res. Lett., 39, L11705, https://doi.org/10.1029/2012gl051937, 2012.
Allen, K. J., Nichols, S. C., Evans, R., Cook, E. R., Allie, S., Carson, G., Ling, F., and Baker, P. J.: Preliminary December–January inflow and streamflow reconstructions from tree rings for western Tasmania, southeastern Australia, Water Resour. Res., 51, 5487–5503, https://doi.org/10.1002/2015wr017062, 2015.
Alpert, A. E., Cohen, A. L., Oppo, D. W., DeCarlo, T. M., Gove, J. M., and Young, C. W.: Comparison of equatorial Pacific sea surface temperature variability and trends with Sr∕Ca records from multiple corals, Paleoceanography, 31, 252–265, https://doi.org/10.1002/2015pa002897, 2016.
Ammann, C. M., Joos, F., Schimel, D. S., Otto-Bliesner, B. L., and Tomas, R. A.: Solar influence on climate during the past millennium: results from transient simulations with the NCAR Climate System Model, P. Natl. Acad. Sci. USA, 104, 3713–3718, https://doi.org/10.1073/pnas.0605064103, 2007.
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Short summary
Water availability is fundamental to societies and ecosystems, but our understanding of variations in hydroclimate (including extreme events, flooding, and decadal periods of drought) is limited due to a paucity of modern instrumental observations. We review how proxy records of past climate and climate model simulations can be used in tandem to understand hydroclimate variability over the last 2000 years and how these tools can also inform risk assessments of future hydroclimatic extremes.