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Thomas M. Smith

Researcher at National Oceanic and Atmospheric Administration

Publications -  75
Citations -  23110

Thomas M. Smith is an academic researcher from National Oceanic and Atmospheric Administration. The author has contributed to research in topics: Sea surface temperature & Precipitation. The author has an hindex of 34, co-authored 75 publications receiving 20532 citations. Previous affiliations of Thomas M. Smith include University of Maryland, College Park.

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A long-term record of blended satellite and in situ sea-surface temperature for climate monitoring, modeling and environmental studies

TL;DR: In this article, a blended sea-surface temperature (SST) data set that is part of the National Oceanic and Atmospheric Administration (NOAA) Climate Data Record (CDR) program suite is described.
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Global temperature change and its uncertainties since 1861

TL;DR: In this article, the authors present the first analysis of global and hemispheric surface warming trends that attempts to quantify the major sources of uncertainty, such as urbanization, changing land-based observing practices and SST bias corrections.
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A Global Merged Land–Air–Sea Surface Temperature Reconstruction Based on Historical Observations (1880–1997)

TL;DR: In this article, a merged land-air-sea surface temperature reconstruction analysis is developed for monthly anomalies, and the reconstruction is global and spatially complete, and it is shown that the average reconstruction is similar to simple averages of the unanalyzed data for most of the analysis period.
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Improvements of the Daily Optimum Interpolation Sea Surface Temperature (DOISST) Version 2.1

TL;DR: The DOISST v2.0.1 dataset as discussed by the authors is an upgraded version of version 2.0, which is derived from merging BUFR and TAC, as well as by including Argo observations above 5m depth.
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Interdecadal Changes of 30-Yr SST Normals during 1871–2000

TL;DR: In this article, a new 30-yr normal for the 1971-2000 base period is constructed, and the interdecadal changes of seasonal CM, seasonal SD, and seasonal persistence are discussed.