Decadal Covariability of the Northern Wintertime Land Surface Temperature and Atmospheric Circulation
Abstract
The decadal covariability of northern wintertime land surface temperature and 500-hPa geopotential anomalies is examined using the National Centers for Environmental Prediction–National Center for Atmospheric Research and the Twentieth-Century Reanalyses over the twentieth century and a 996-yr preindustrial climate simulation from the Canadian Earth System Model. Based on the reanalysis data, the covariability is dominated by two leading maximum covariance analysis (MCA) modes. MCA1 is characterized by temperature anomalies over most of Canada, the eastern United States, Mexico, and Eurasian mid- to high latitudes, accompanied by anomalies of opposite sign elsewhere over northern landmasses. MCA2 features temperature anomalies over most of North America, Eurasia, and Greenland with opposite anomalies elsewhere. In the upper troposphere the synoptic vorticity fluxes reinforce the anomalous circulation, while in the lower troposphere advection by the anomalous mean flow offsets the eddy forcing and maintains the decadal temperature perturbation. The MCA1-associated variability has a broad spectrum over decadal–interdecadal time scales, while the MCA2-related variability has a significant power peak around 20 yr. The change of temperature and geopotential trends around 1990 tends to be a decadal-scale shift in winter and has significant features of the leading mode of the decadal covariability. The climate model has broadlymore »
- Authors:
-
- Environment Canada, Toronto, ON (Canada). Climate Research Division, Climate Data Analysis Section
- Environment Canada, Victoria, BC (Canada). Canadian Centre for Climate Modelling and Analysis, Climate Research Division
- Publication Date:
- Research Org.:
- Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1565237
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Climate
- Additional Journal Information:
- Journal Volume: 27; Journal Issue: 2; Journal ID: ISSN 0894-8755
- Publisher:
- American Meteorological Society
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Meteorology & Atmospheric Sciences; Atmospheric circulation; Climate change; Climate variability; Surface temperature; Model evaluation/performance
Citation Formats
Yu, B., Wang, X. L., Zhang, X. B., Cole, J., and Feng, Y. Decadal Covariability of the Northern Wintertime Land Surface Temperature and Atmospheric Circulation. United States: N. p., 2014.
Web. doi:10.1175/jcli-d-13-00266.1.
Yu, B., Wang, X. L., Zhang, X. B., Cole, J., & Feng, Y. Decadal Covariability of the Northern Wintertime Land Surface Temperature and Atmospheric Circulation. United States. https://doi.org/10.1175/jcli-d-13-00266.1
Yu, B., Wang, X. L., Zhang, X. B., Cole, J., and Feng, Y. Fri .
"Decadal Covariability of the Northern Wintertime Land Surface Temperature and Atmospheric Circulation". United States. https://doi.org/10.1175/jcli-d-13-00266.1. https://www.osti.gov/servlets/purl/1565237.
@article{osti_1565237,
title = {Decadal Covariability of the Northern Wintertime Land Surface Temperature and Atmospheric Circulation},
author = {Yu, B. and Wang, X. L. and Zhang, X. B. and Cole, J. and Feng, Y.},
abstractNote = {The decadal covariability of northern wintertime land surface temperature and 500-hPa geopotential anomalies is examined using the National Centers for Environmental Prediction–National Center for Atmospheric Research and the Twentieth-Century Reanalyses over the twentieth century and a 996-yr preindustrial climate simulation from the Canadian Earth System Model. Based on the reanalysis data, the covariability is dominated by two leading maximum covariance analysis (MCA) modes. MCA1 is characterized by temperature anomalies over most of Canada, the eastern United States, Mexico, and Eurasian mid- to high latitudes, accompanied by anomalies of opposite sign elsewhere over northern landmasses. MCA2 features temperature anomalies over most of North America, Eurasia, and Greenland with opposite anomalies elsewhere. In the upper troposphere the synoptic vorticity fluxes reinforce the anomalous circulation, while in the lower troposphere advection by the anomalous mean flow offsets the eddy forcing and maintains the decadal temperature perturbation. The MCA1-associated variability has a broad spectrum over decadal–interdecadal time scales, while the MCA2-related variability has a significant power peak around 20 yr. The change of temperature and geopotential trends around 1990 tends to be a decadal-scale shift in winter and has significant features of the leading mode of the decadal covariability. The climate model has broadly similar decadal covariability, including the leading MCA patterns as well as the temporal evolution of the patterns. The decadal temperature and geopotential anomalies primarily covary with the North Atlantic Oscillation but also with the variability of the North Pacific index, while the Southern Oscillation index variability tends to be the least important predictor for the northern decadal temperature and geopotential anomalies.},
doi = {10.1175/jcli-d-13-00266.1},
journal = {Journal of Climate},
number = 2,
volume = 27,
place = {United States},
year = {Fri Jan 17 00:00:00 EST 2014},
month = {Fri Jan 17 00:00:00 EST 2014}
}
Web of Science
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