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Kate E. Sinclair

Researcher at GNS Science

Publications -  10
Citations -  467

Kate E. Sinclair is an academic researcher from GNS Science. The author has contributed to research in topics: Glacier & Ice core. The author has an hindex of 7, co-authored 9 publications receiving 363 citations.

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A global multiproxy database for temperature reconstructions of the Common Era

Julien Emile-Geay, +108 more
- 11 Jul 2017 - 
TL;DR: A community-sourced database of temperature-sensitive proxy records from the PAGES2k initiative, suited to investigations of global and regional temperature variability over the Common Era, and is shared in the Linked Paleo Data (LiPD) format, including serializations in Matlab, R and Python.
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Synoptic controls on precipitation pathways and snow delivery to high-accumulation ice core sites in the Ross Sea region, Antarctica

TL;DR: In this article, the authors investigated the seasonality, source regions, and transport pathways of precipitation delivered to two ice core sites on the western margin of the Ross Sea, Antarctica (Skinner Saddle (SKS) and Evans Piedmont Glacier), to establish key synoptic controls on snow accumulation.
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Twentieth century sea-ice trends in the Ross Sea from a high-resolution, coastal ice-core record

TL;DR: The first proxy record of sea-ice area (SIA) in the Ross Sea, Antarctica, from a 130-year coastal ice-core record was presented in this paper.
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Synoptic variability in the Ross Sea region, Antarctica, as seen from back‐trajectory modeling and ice core analysis

TL;DR: In this article, the authors identify two dominant air-mass trajectory clusters: oceanic/West Antarctic and continental/East Antarctic trajectories and demonstrate a causal association between the El Nino Southern Oscillation (ENSO) and the frequency of trajectories originating from the Ross Sea and Amundsen Sea regions.
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Seasonality of Airmass Pathways to Coastal Antarctica: Ramifications for Interpreting High-Resolution Ice Core Records

TL;DR: In this paper, the dominant airmass pathways to a coastal Antarctic ice core site at the Whitehall Glacier in the Ross Sea are modeled using snowfall and high-resolution stable isotope data between 1979 and 2006, combined with back trajectories produced from both NCEP-NCAR and ECMWF Interim Re-Analysis (ERA-Interim) data.