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Ryan L. Fogt

Researcher at Ohio University

Publications -  53
Citations -  4367

Ryan L. Fogt is an academic researcher from Ohio University. The author has contributed to research in topics: Sea ice & Climate model. The author has an hindex of 26, co-authored 50 publications receiving 3594 citations. Previous affiliations of Ryan L. Fogt include Earth System Research Laboratory & Ohio State University.

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Decadal Variability of the ENSO Teleconnection to the High-Latitude South Pacific Governed by Coupling with the Southern Annular Mode

TL;DR: In this paper, the decadal variability of the El Nino-Southern Oscillation (ENSO) teleconnection to the high-latitude South Pacific is examined by correlating the European Centre for Medium-Range Weather Forecasts (ECMWF) 40-yr Re-Analysis (ERA-40) and observations with the SOI over the last two decades.
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Strong Trends in the Skill of the ERA-40 and NCEP–NCAR Reanalyses in the High and Midlatitudes of the Southern Hemisphere, 1958–2001*

TL;DR: In this paper, the European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) and the National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) reanalysis data are compared with Antarctic and other mid- to high-latitude station observations for the complete years of overlap, 1958-2001.
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Understanding the SAM influence on the South Pacific ENSO teleconnection

TL;DR: The relationship between the El Nino Southern Oscillation (ENSO) and the Southern Hemisphere Annular Mode (SAM) is examined in this article, with the goal of understanding how various strong SAM events modulate the ENSO teleconnection to the South Pacific.
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A tropospheric assessment of the ERA-40, NCEP, and JRA-25 global reanalyses in the polar regions

TL;DR: The reliability of the global reanalyses in the polar regions is investigated in this paper, where large circulation differences between the rean analyses are found primarily before 1979, when vast quantities of satellite sounding data started to be assimilated.