Abstract

AbstractThe heat wave in East Asia is examined by using empirical orthogonal function analysis to isolate dominant heat-wave patterns in the ground-based temperature observations over the Korean Peninsula and China and related large-scale atmospheric circulations obtained from the National Centers for Environmental Prediction–National Center for Atmospheric Research Reanalysis 1 during 1973–2012. This study focuses particularly on the interannual variability of heat waves and its decadal change. The analysis identifies two major atmospheric teleconnection patterns playing an important role in developing typical heat-wave patterns in East Asia—the Scandinavian (SCAND) and the circumglobal teleconnection (CGT) patterns, which exhibit a significant decadal change in the interannual variability in the mid-1990s. Before the mid-1990s, heat-wave occurrence was closely related to the CGT pattern, whereas the SCAND pattern is more crucial to explain heat-wave variability in the recent period. The stationary wave model experiments suggest an intensification of the SCAND pattern in the recent period driven by an increase in land–atmosphere interaction over Eurasia and decadal change in the dominant heat-wave patterns in East Asia.

Highlights

  • The heat wave is an extreme heat event

  • Considering the summer Pacific decadal oscillation (PDO) index that has been negative since the mid-1990s on the decadal time scale, there should be another mechanism other than El Niño–Southern Oscillation (ENSO) that may explain the interannual variability of heat waves in East Asia in recent years

  • This study further examines whether there was any significant change in the Scandinavian pattern in the recent period by conducting rotated EOF (REOF) analysis on the reanalysis data

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Summary

Introduction

The heat wave is an extreme heat event. The heat wave in 2003 in Europe caused approximately 35 000 deaths (Larsen 2003), and in Russia a heat wave in 2010 claimed approximately 55 000 lives (Barriopedro et al 2011). Considering the summer PDO index that has been negative since the mid-1990s on the decadal time scale, there should be another mechanism other than ENSO that may explain the interannual variability of heat waves in East Asia in recent years.

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