We investigate the impact of the diabatic heating (Q1) over the Indian subcontinent and Tibetan Plateau (TP) sensible heat on the heat waves in South Korea in July and August over a recent 42-year period. In particular, we emphasize the role of the convective activity across the region from northeastern Pakistan to northwestern India (PWI) induced by the heat from the TP, especially over the western and eastern TP. A composite analysis indicates that the composite differences between the heat-wave summers (HWS) and non-heat-wave summers (NHWS) resemble the circum-global teleconnection (CGT) pattern, which generates a high-pressure anomaly over the Korean Peninsula, producing favourable conditions for heat waves in South Korea. The first cou...
Global warming and abnormal climate change have resulted in an increase in the frequency of severe h...
Abstract The negative impact of extreme high-temperature days (EHDs) on people’s livelihood has incr...
The characteristics of a strong northeast Asian summer monsoon (NEASM) with and without (A and B typ...
It is important to understand the dynamical processes that cause heat waves at regional scales. This...
This study identified three distinct convection structures over the Indo-western Pacific that caused...
This study investigates the interannual variation of heat wave frequency (HWF) in South Korea during...
The NCEP/NCAR pentad mean reanalysis data from 1980 to 1994 are employed to examine the activities o...
In the Northwestern Pacific, the meridionally propagating Rossby waves, known as the Pacific-Japan (...
In the Northwestern Pacific, the meridionally propagating Rossby waves, known as the Pacific-Japan (...
South Korea's heat wave events over 39 years (1980-2018) were defined by spatiotemporal criteri...
The characteristics of heat waves (HWs) in South Korea are studied using data from the European Cent...
This study analyzed and compared development mechanisms leading to heat waves of 2016 and 2018 in Ko...
This study analyzes differences in the mechanisms leading to anomalously high-temperature weather ev...
An analysis based on July-August precipitation reveals that there is a tripole pattern of the precip...
The thermal forcing of the Tibetan Plateau (TP) is analyzed to investigate the formation and variabi...
Global warming and abnormal climate change have resulted in an increase in the frequency of severe h...
Abstract The negative impact of extreme high-temperature days (EHDs) on people’s livelihood has incr...
The characteristics of a strong northeast Asian summer monsoon (NEASM) with and without (A and B typ...
It is important to understand the dynamical processes that cause heat waves at regional scales. This...
This study identified three distinct convection structures over the Indo-western Pacific that caused...
This study investigates the interannual variation of heat wave frequency (HWF) in South Korea during...
The NCEP/NCAR pentad mean reanalysis data from 1980 to 1994 are employed to examine the activities o...
In the Northwestern Pacific, the meridionally propagating Rossby waves, known as the Pacific-Japan (...
In the Northwestern Pacific, the meridionally propagating Rossby waves, known as the Pacific-Japan (...
South Korea's heat wave events over 39 years (1980-2018) were defined by spatiotemporal criteri...
The characteristics of heat waves (HWs) in South Korea are studied using data from the European Cent...
This study analyzed and compared development mechanisms leading to heat waves of 2016 and 2018 in Ko...
This study analyzes differences in the mechanisms leading to anomalously high-temperature weather ev...
An analysis based on July-August precipitation reveals that there is a tripole pattern of the precip...
The thermal forcing of the Tibetan Plateau (TP) is analyzed to investigate the formation and variabi...
Global warming and abnormal climate change have resulted in an increase in the frequency of severe h...
Abstract The negative impact of extreme high-temperature days (EHDs) on people’s livelihood has incr...
The characteristics of a strong northeast Asian summer monsoon (NEASM) with and without (A and B typ...