The Twentieth Century Reanalysis Project

By Gilbert P. Compo, J. Whitaker, P. Sardeshmukh, N. Matsui, R. Allan, Xiaobo Yin, B. Gleason, R. Vose, G. Rutledge, P. Bessemoulin and 17 more. 2009

3,267 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/006c5ab6c4d2f779151889a9714c9380d6bdd34e

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Citations in the corpus

Atlantic forcing of Pacific decadal variability (2016, methodology): “The NOAA-CIRES 20th Century Reanalysis version 2 (Compo et al. 2011; 1900 to present) is used for surface winds, and the CMAP (Xi and Arkin 1997) dataset is used for rainfall verification of the model.”
GRACE-REC: a reconstruction of climate-driven water storage changes over the last century (2019, methodology): “The Global Soil Wetness Project Phase 3 (GSWP3) forcing dataset (Kim, 2017) is based on the 20th Century Reanalysis (20CR) version 2c (Compo et al., 2011).”
The LAGRANTO Lagrangian analysis tool – version 2.0 (2015, methodology): “Preliminary LAGRANTO versions, for which not all functionalities have been implemented and tested yet, are also available for the UK Met office Unified Model (MetUM), the Weather Research and Forecasting (WRF) modeling system and the 20CR re-analysis data set (Compo et al., 2011).”
Causes of climate change over the historical record (2019, background): “Global coverage of the 3D atmosphere is available from historical reanalyses that assimilate surface and sea level pressure and, in some products,marine winds (Compo et al 2011, Poli et al 2016, Laloyaux et al 2018).”
An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models (2020, methodology): “Two twentieth century reanalysis products: ECMWF's ERA20C (Poli et al., 2016) and NOAA's twentieth century reanalysis, 20CR (Compo et al., 2011), are considered, partly for the purpose of assessing those reanalysis products compared to others and also for the purpose of providing a longer‐term…”
The ERA5 global reanalysis (2020, methodology): “The production of such a model-based reanalysis that extends back more than one century was first pursued in the 20CR Project (Compo et al., 2006) at NOAA's Earth Systems Research Laboratory, where a reanalysis spanning the period 1871–2010 was conducted (Compo et al., 2011).”
Dynamical Adjustment of the Northern Hemisphere Surface Air Temperature Field: Methodology and Application to Observations* (2015, methodology): “For example, in the first column of Table A1 the first few predictors account for most of the explained variance but the continuing rise in the fraction of explained variance out to 10 predictors raises concerns about overfitting (Davis 1976).”