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date accessioned2022-05-09T00:48:51Z
date available2022-05-09T00:48:51Z
date copyright11 Apr 2022
date issued2022
identifier otherJAS-D-21-0030.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4285540
description abstractApplying 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.
titleThe Temperature Anomaly Pattern of the Pacific–North American Teleconnection: Growth and Decay
typeJournal Paper
journal volume79
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS-D-21-0030.1
page1237–1252
treeJournal of the Atmospheric Sciences:;2022:;volume( 079 ):;issue: 005
contenttypeFulltext


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