Influence of Kuroshio Extension's sea surface temperature variability on the North Pacific atmosphere and Pacific Decadal Precession

被引:0
作者
Silva, E. Nishchitha S. [1 ,2 ]
Anderson, Bruce T. [1 ]
机构
[1] Boston Univ, Dept Earth & Environm, Boston, MA 02215 USA
[2] Verisk Atmospher & Environm Res, Lexington, MA 02421 USA
关键词
Kuroshio current system; North Pacific climate; Ocean-atmosphere interactions; Pacific decadal precession; Decadal climate variability; Mesoscale and large-scale ocean currents; EXTRATROPICAL SST ANOMALIES; GULF-STREAM; RESPONSES; EDDIES; MODEL; CIRCULATION; DYNAMICS; STATE; WAVE; JET;
D O I
10.1007/s00382-024-07372-2
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Recent research has revealed links between a quasi-decadal mode of climate variability over the North Pacific - the Pacific Decadal Precession (PDP) - and the North Pacific's western boundary current's extension - the Kuroshio Extension (KE). It is suggested that on decadal time scales the PDP both responds to and influences the KE variability. A question yet to be answered is whether it is the large-scale or the mesoscale variations of the KE region that link with the PDP evolution. Using high-resolution sea surface temperature data (1981-2018) from the global ocean Operational Sea Surface Temperature (SST) and Sea Ice Analysis, low-resolution Extended Reconstructed SST (ERSST) version 3b data (1949-2018), geopotential height reanalysis data from the European Centre for Medium-Range Weather Forecasts (ECMWF) and the National Centers for Environmental Prediction (NCEP) we find that it is the large-scale variations in the KE region that correlate best with the PDP-like response in the overlying and downstream atmosphere as compared to the mesoscale variations. In particular, the second mode of the large-scale KE region, which is characterized by the warming (cooling) of the ocean south (north) of the KE, sets up a PDP-like north-south atmospheric pressure dipole over the North Pacific Ocean by altering the large-scale baroclinicity of the atmosphere and zonal intensification of the subtropical jet stream. In turn, there is a reduction in the zonal propagation of stationary wave energy and an enhancement of the climatological zonal wave heights over North America, which results in a downstream response over the North American continent and the formation of a subsequent east-west pressure dipole over the North Pacific and North American continent. As a result, there is a strong correlation between large-scale SST variations in the KE region and the evolution of the PDP over the next three years.
引用
收藏
页码:8947 / 8960
页数:14
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