TY - JOUR
T1 - The Temperature Anomaly Pattern of the Pacific–North American Teleconnection
T2 - Growth and Decay
AU - Clark, Joseph P.
AU - Feldstein, Steven B.
N1 - Funding Information:
We thank three anonymous reviewers for their helpful comments and questions. This study benefitted from research discussions with Sukyoung Lee, Ying Pan, David Stensrud, Cory Baggett, Mingyu Park, Dong Wan Kim, Colton Milcarek, and Allen Mewhinney. This study was supported by National Science Foundation Grants OPP-1723832 and AGS-1822015.
Funding Information:
Acknowledgments. We thank three anonymous reviewers for their helpful comments and questions. This study benefitted from research discussions with Sukyoung Lee, Ying Pan, David Stensrud, Cory Baggett, Mingyu Park, Dong Wan Kim, Colton Milcarek, and Allen Mewhinney. This study was supported by National Science Foundation Grants OPP-1723832 and AGS-1822015.
Publisher Copyright:
© 2022 American Meteorological Society.
PY - 2022
Y1 - 2022
N2 - Applying composite analysis to ERA-Interim data, the surface air temperature (SAT) anomaly pattern of the Pacific–North American (PNA) teleconnection is shown to include both symmetric and asymmetric SAT anomalies with respect to the PNA phase. The symmetric SAT anomalies, overlying the Russian Far East and western and eastern North America, grow through advection of the climatological temperature by the anomalous meridional wind and vertical mixing. The asymmetric SAT anomalies, overlying Siberia during the positive PNA and the subtropical North Pacific during the negative PNA, grow through vertical mixing only. For all SAT anomalies, vertical mixing relocates the temperature anomalies of the PNA teleconnection pattern from higher in the boundary layer downward to the level of the SAT. Above the level of the SAT, temperature anomaly growth is caused by horizontal temperature advection in all locations except for the subtropical North Pacific, where adiabatic cooling dominates. SAT anomaly decay is caused by longwave radiative heating/cooling, except over Siberia, where SAT anomaly decay is caused by vertical mixing. Additionally, temperature anomaly decay higher in the boundary layer due to nonlocal mixing contributes indirectly to SAT anomaly decay by weakening downgradient diffusion. These results highlight a diverse array of mechanisms by which individual anomalies within the PNA pattern grow and decay. Furthermore, with the exception of Siberia, throughout the growth and decay stages, horizontal temperature advection and/or vertical mixing is nearly balanced by longwave radiative heating/cooling, with the former being slightly stronger during the growth stage and the latter during the decay stage.
AB - Applying composite analysis to ERA-Interim data, the surface air temperature (SAT) anomaly pattern of the Pacific–North American (PNA) teleconnection is shown to include both symmetric and asymmetric SAT anomalies with respect to the PNA phase. The symmetric SAT anomalies, overlying the Russian Far East and western and eastern North America, grow through advection of the climatological temperature by the anomalous meridional wind and vertical mixing. The asymmetric SAT anomalies, overlying Siberia during the positive PNA and the subtropical North Pacific during the negative PNA, grow through vertical mixing only. For all SAT anomalies, vertical mixing relocates the temperature anomalies of the PNA teleconnection pattern from higher in the boundary layer downward to the level of the SAT. Above the level of the SAT, temperature anomaly growth is caused by horizontal temperature advection in all locations except for the subtropical North Pacific, where adiabatic cooling dominates. SAT anomaly decay is caused by longwave radiative heating/cooling, except over Siberia, where SAT anomaly decay is caused by vertical mixing. Additionally, temperature anomaly decay higher in the boundary layer due to nonlocal mixing contributes indirectly to SAT anomaly decay by weakening downgradient diffusion. These results highlight a diverse array of mechanisms by which individual anomalies within the PNA pattern grow and decay. Furthermore, with the exception of Siberia, throughout the growth and decay stages, horizontal temperature advection and/or vertical mixing is nearly balanced by longwave radiative heating/cooling, with the former being slightly stronger during the growth stage and the latter during the decay stage.
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U2 - 10.1175/JAS-D-21-0030.1
DO - 10.1175/JAS-D-21-0030.1
M3 - Article
AN - SCOPUS:85128634498
SN - 0022-4928
VL - 79
SP - 1237
EP - 1252
JO - Journal of the Atmospheric Sciences
JF - Journal of the Atmospheric Sciences
IS - 5
ER -