https://repository.kopri.re.kr/handle/201206/5094 2026-04-23T09:30:38Z 2026-04-23T09:30:38Z Kim, Baek-Min An, Soon-Il https://repository.kopri.re.kr/handle/201206/6444 2022-03-24T07:11:33Z 2011-01-01T00:00:00Z

Title: Understanding ENSO Regime Behavior upon an Increase in the Warm-Pool Authors: Kim, Baek-Min; An, Soon-Il Abstract: The regime behavior of the low-order ENSO model, according to an increase in the radiative？convective equilibrium sea surface temperature (SST;Tr) is studied to provide a possible explanation for the observed increase in ENSO irregularity characterized by decadal modulation. A bifurcation analysis with Tr as a control parameter is conducted to reveal that the degree of ENSO irregularity in the model is effectively controlled by the equilibrium states of the model. At a critical value of Tr, bifurcation analysis reveals that period-doubling bifurcation occurs and an amplitude-modulated ENSO emerges. As Tr increases further, nested oscillations are successively generated, illustrating clear decadal modulation of ENSO. The qualitative regime changes revealed in this study are supported by the observation of regime shifts in the 1970s.

2011-01-01T00:00:00Z Kim, Seong-Joong Kim, Yoojin Lee, Hyun-Ha Kim, Baek-Min https://repository.kopri.re.kr/handle/201206/8532 2022-03-24T07:13:37Z 2010-01-01T00:00:00Z

Title: Arctic Oscillation and the Northern Hemisphere Cold Surge at 2009/2010 Winter Authors: Kim, Seong-Joong; Kim, Yoojin; Lee, Hyun-Ha; Kim, Baek-Min Abstract: The cause of the cold surge occurred at 2009/2010 winter over northern hemisphere was investigated. During the boreal winter (December-January-February) of 2009/2010, the surface temperature was extremely lower than normal years by more than 5 degree over North-east Asia, Europe, and North America. The cold air outbreak was due to the stronger northerly winds in troposphere at mid latitudes associated with the substantially weaker Arctic Oscillation (AO) polarity. The weaker AO is associated with the weaker zonal-mean zonal winds and higher geopotential height and associated marked warming anomalies at high northern latitudes, whose signals propagated from the mid-latitude stratosphere at autumn down to troposphere at winter. The marked stratospheric warm anomaly in autumn is produced by the stronger upward propagation of the stationary planetary waves which led to the weaker znoal-mean zonal winds. Analyses indicate that the stronger wave activity is originated from Eurasia/Siberia associated with the anomalously larger snow cover during October and November. The autumn snow cover over these regions tends to increase with time and its increasing rate is becoming larger towards present with the global warming. This result indicates that the anomalously increased autumn snow cover over Siberia at 2009 autumn in part led to the weakening of the AO polarity and consequent cold air outbreak for the 2009/2010 winter.

2010-01-01T00:00:00Z