Samantha Stevenson, Ph.D.
Affiliations: | 2011 | Atmospheric and Oceanic Sciences | University of Colorado, Boulder, Boulder, CO, United States |
Area:
Physical Oceanography, Atmospheric Sciences, Paleoclimate ScienceGoogle:
"Samantha Stevenson"Parents
Sign in to add mentor| Baylor Fox-Kemper | grad student | 2011 | CU Boulder | |
| (The Past, Present and Future of the El Nino/Southern Oscillation.) | ||||
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Publications
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| Zhu F, Emile-Geay J, Anchukaitis KJ, et al. (2023) A pseudoproxy emulation of the PAGES 2k database using a hierarchy of proxy system models. Scientific Data. 10: 624 |
| Falster G, Konecky B, Coats S, et al. (2023) Forced changes in the Pacific Walker circulation over the past millennium. Nature |
| Xu T, Newman M, Capotondi A, et al. (2022) An increase in marine heatwaves without significant changes in surface ocean temperature variability. Nature Communications. 13: 7396 |
| Touma D, Stevenson S, Swain DL, et al. (2022) Climate change increases risk of extreme rainfall following wildfire in the western United States. Science Advances. 8: eabm0320 |
| Feng X, Ding Q, Wu L, et al. (2021) A Multidecadal-Scale Tropically Driven Global Teleconnection over the Past Millennium and Its Recent Strengthening Journal of Climate. 34: 2549-2565 |
| Zhao Y, Di Lorenzo E, Sun D, et al. (2021) Tropical Pacific Decadal Variability and ENSO Precursor in CMIP5 Models Journal of Climate. 34: 1023-1045 |
| Stevenson S, Wittenberg AT, Fasullo J, et al. (2021) Understanding Diverse Model Projections of Future Extreme El Niño Journal of Climate. 34: 449-464 |
| Coupe J, Stevenson S, Lovenduski NS, et al. (2021) Nuclear Niño response observed in simulations of nuclear war scenarios Communications Earth & Environment. 2 |
| Konecky BL, McKay NP, (Sidorova) OVC, et al. (2020) The Iso2k Database: A global compilation of paleo-δ 18 O and δ 2 Hrecords to aid understanding of Common Era climate Earth System Science Data Discussions. 1-49 |
| Brown JR, Brierley CM, An S, et al. (2020) Comparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models Climate of the Past Discussions. 1-44 |