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KUG, JONG SEONG(국종성)

Department: Div of Environmental Science & Enginrg(환경공학부)

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ENSO:6||VARIABILITY:6||PACIFIC:4||SEASURFACE TEMPERATURE:3||MIDLATITUDE STORM TRACKS:2||DYNAMICS:2||CLIMATECHANGE:2||SYNOPTIC EDDY:2||asymmetry:2||TROPICAL PACIFIC:2||MIDWINTER SUPPRESSION:2||MODEL:2||2LAYER MODEL:2||CLIMATE VARIABILITY:2||MEAN FLOW:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||ANNULAR MODES:2||OSCILLATION:2||CLIMATE:2||El Nino:2||ZONAL FLOW FEEDBACK:2||ELNINO:2||INTERDECADAL CHANGES:1||ICE:1||PRODUCTIVITY:1||La Nina:1||Weather extremes:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||MADDENJULIAN OSCILLATION:1||EASTASIA:1||Climate change:1||Arctic climate changes:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||Korea and East Asia:1||ARCTIC SEAICE:1||PRECIPITATION EXTREMES:1||SURFACE TEMPERATURE:1||biogeophysical feedback:1||PENETRATIVE RADIATION:1||RELEVANCE:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||CALANUSFINMARCHICUS:1||CMIP5:1||MIDLATITUDE WEATHER:1||REGION:1||WESTERN PACIFIC:1||SOUTHERNOSCILLATION:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||CIRCULATION:1||climate variability and change:1||ASIANAUSTRALIAN MONSOON:1||AMO:1||OCEAN:1||climate extremes:1||SOUTHKOREA:1||QUANTILE REGRESSION:1||RADIATION:1||DRAWDOWN:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||SUMMER INTRASEASONAL OSCILLATION:1||ATMOSPHERIC RESPONSE:1||

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