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Nathan J. Steiger

Researcher at Lamont–Doherty Earth Observatory

Publications -  33
Citations -  1156

Nathan J. Steiger is an academic researcher from Lamont–Doherty Earth Observatory. The author has contributed to research in topics: Climate model & Pseudoproxy. The author has an hindex of 13, co-authored 26 publications receiving 797 citations. Previous affiliations of Nathan J. Steiger include University of Washington & Hebrew University of Jerusalem.

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Global hydroclimatic response to tropical volcanic eruptions over the last millennium.

TL;DR: This article analyzed the global hydroclimatic response to all the tropical volcanic eruptions over the past millennium that were larger than the Mount Pinatubo eruption of 1991 using the Paleo Hydrodynamics Data Assimilation product (PHYDA).
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Teleconnections and relationship between the El Niño–Southern Oscillation (ENSO) and the Southern Annular Mode (SAM) in reconstructions and models over the past millennium

TL;DR: In this article, the authors used proxy-based reconstructions and last-millennium climate model simulations to investigate the relationship between the Southern Annular Mode (SAM) and the El Nino-Southern Oscillation (ENSO) over time.
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A pseudoproxy assessment of data assimilation for reconstructing the atmosphere-ocean dynamics of hydroclimate extremes

TL;DR: In this article, the authors explore whether or not data assimilation can be used to skillfully reconstruct global hydroclimate variability along with the driving climate dynamics through a set of idealized pseudoproxy experiments and find that the skill of such reconstructions is generally highest near the proxy sites.
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Multi-timescale data assimilation for atmosphere–ocean state estimates

TL;DR: In this article, the authors present a data assimilation approach that can explicitly incorporate proxy data at arbitrary timescales, and they find that atmosphere-ocean states are most skillfully reconstructed by incorporating proxies across multiple scales compared to using proxies at short (annual) or long (∼ ǫdecadal) timescale alone.