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KUG, JONG SEONG (국종성)

Div of Environmental Science & Engineering(환경공학부)

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ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC SST:1||PERSPECTIVE:1||LANDSURFACE:1||REANALYSIS:1||GLOBAL PRECIPITATION:1||TROPICAL ATLANTIC:1||CONNECTION:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||NET PRIMARY PRODUCTION:1||CLIMATECHANGE:1||INDONESIAN SEAS:1||CHUKCHI:1||EASTERNPACIFIC:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||Climate change:1||SYNOPTIC EDDY:1||LAND BIOSPHERE:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||UPPER OCEAN:1||ATMOSPHERE FEEDBACKS:1||SUMMER MONSOON:1||TELECONNECTION PATTERNS:1||EASTERN EQUATORIAL PACIFIC:1||Indian Ocean Dipole:1||SST:1||MIDWINTER SUPPRESSION:1||LINE SIMULATION CHARACTERISTICS:1||MULTIDECADAL VARIABILITY:1||SEAICE COVER:1||ECOSYSTEMS:1||BLOOMS:1||PENETRATIVE RADIATION:1||SOILMOISTURE:1||HEAT WAVES:1||FEEDBACKS:1||seasonal variation:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||EARTH SYSTEM MODELS:1||CARBONCYCLE FEEDBACKS:1||TRADE WINDS:1||PROJECTIONS:1||CALANUSFINMARCHICUS:1||WINTER MONSOON:1||WIND:1||El NinoSouthern Oscillation:1||REGION:1||MEAN FLOW:1||DIOXIDE:1||GROWTH:1||NITROGEN:1||GENERALCIRCULATION MODEL:1||DEEP CONVECTION:1||ATMOSPHERE:1||SST ANOMALIES:1||CIRCULATION:1||ARCTIC OSCILLATION:1||CLIMATE SENSITIVITY:1||precipitation (climatology):1||Pacific Ocean:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||MULTIMODEL ENSEMBLE:1||TOINTERANNUAL PREDICTION:1||OCEAN:1||INDIANOCEAN:1||TIBETAN PLATEAU:1||airsea interaction:1||Pacific Ocean (West):1||CHINA SEA:1||TEMPERATURE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||EASTERN EDGE:1||NORTHERNHEMISPHERE:1||FLOW:1||PREDICTABILITY:1||HYDROLOGICAL CYCLE:1||El Nino:1||climate modeling:1||CMIP:1||KUROSHIO:1||ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC SST:1||PERSPECTIVE:1||LANDSURFACE:1||REANALYSIS:1||GLOBAL PRECIPITATION:1||TROPICAL ATLANTIC:1||CONNECTION:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||NET PRIMARY PRODUCTION:1||CLIMATECHANGE:1||INDONESIAN SEAS:1||CHUKCHI:1||EASTERNPACIFIC:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||Climate change:1||SYNOPTIC EDDY:1||LAND BIOSPHERE:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||UPPER OCEAN:1||ATMOSPHERE FEEDBACKS:1||SUMMER MONSOON:1||TELECONNECTION PATTERNS:1||EASTERN EQUATORIAL PACIFIC:1||Indian Ocean Dipole:1||SST:1||MIDWINTER SUPPRESSION:1||LINE SIMULATION CHARACTERISTICS:1||MULTIDECADAL VARIABILITY:1||SEAICE COVER:1||ECOSYSTEMS:1||BLOOMS:1||PENETRATIVE RADIATION:1||SOILMOISTURE:1||HEAT WAVES:1||FEEDBACKS:1||seasonal variation:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||EARTH SYSTEM MODELS:1||CARBONCYCLE FEEDBACKS:1||TRADE WINDS:1||PROJECTIONS:1||CALANUSFINMARCHICUS:1||WINTER MONSOON:1||WIND:1||El NinoSouthern Oscillation:1||REGION:1||MEAN FLOW:1||DIOXIDE:1||GROWTH:1||NITROGEN:1||GENERALCIRCULATION MODEL:1||DEEP CONVECTION:1||ATMOSPHERE:1||SST ANOMALIES:1||CIRCULATION:1||ARCTIC OSCILLATION:1||CLIMATE SENSITIVITY:1||precipitation (climatology):1||Pacific Ocean:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||MULTIMODEL ENSEMBLE:1||TOINTERANNUAL PREDICTION:1||OCEAN:1||INDIANOCEAN:1||TIBETAN PLATEAU:1||airsea interaction:1||Pacific Ocean (West):1||CHINA SEA:1||TEMPERATURE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||EASTERN EDGE:1||NORTHERNHEMISPHERE:1||FLOW:1||PREDICTABILITY:1||HYDROLOGICAL CYCLE:1||El Nino:1||climate modeling:1||CMIP:1||KUROSHIO:1||ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC SST:1||PERSPECTIVE:1||LANDSURFACE:1||REANALYSIS:1||GLOBAL PRECIPITATION:1||TROPICAL ATLANTIC:1||CONNECTION:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||NET PRIMARY PRODUCTION:1||CLIMATECHANGE:1||INDONESIAN SEAS:1||CHUKCHI:1||EASTERNPACIFIC:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||Climate change:1||SYNOPTIC EDDY:1||LAND BIOSPHERE:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||UPPER OCEAN:1||ATMOSPHERE FEEDBACKS:1||SUMMER MONSOON:1||TELECONNECTION PATTERNS:1||EASTERN EQUATORIAL PACIFIC:1||Indian Ocean Dipole:1||SST:1||MIDWINTER SUPPRESSION:1||LINE SIMULATION CHARACTERISTICS:1||MULTIDECADAL VARIABILITY:1||SEAICE COVER:1||ECOSYSTEMS:1||BLOOMS:1||PENETRATIVE RADIATION:1||SOILMOISTURE:1||HEAT WAVES:1||FEEDBACKS:1||seasonal variation:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||EARTH SYSTEM MODELS:1||CARBONCYCLE FEEDBACKS:1||TRADE WINDS:1||PROJECTIONS:1||CALANUSFINMARCHICUS:1||WINTER MONSOON:1||WIND:1||El NinoSouthern Oscillation:1||REGION:1||MEAN FLOW:1||DIOXIDE:1||GROWTH:1||NITROGEN:1||GENERALCIRCULATION MODEL:1||DEEP CONVECTION:1||ATMOSPHERE:1||SST ANOMALIES:1||CIRCULATION:1||ARCTIC OSCILLATION:1||CLIMATE SENSITIVITY:1||precipitation (climatology):1||Pacific Ocean:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||MULTIMODEL ENSEMBLE:1||TOINTERANNUAL PREDICTION:1||OCEAN:1||INDIANOCEAN:1||TIBETAN PLATEAU:1||airsea interaction:1||Pacific Ocean (West):1||CHINA SEA:1||TEMPERATURE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||EASTERN EDGE:1||NORTHERNHEMISPHERE:1||FLOW:1||PREDICTABILITY:1||HYDROLOGICAL CYCLE:1||El Nino:1||climate modeling:1||CMIP:1||KUROSHIO:1||ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC SST:1||PERSPECTIVE:1||LANDSURFACE:1||REANALYSIS:1||GLOBAL PRECIPITATION:1||TROPICAL ATLANTIC:1||CONNECTION:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||NET PRIMARY PRODUCTION:1||CLIMATECHANGE:1||INDONESIAN SEAS:1||CHUKCHI:1||EASTERNPACIFIC:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||Climate change:1||SYNOPTIC EDDY:1||LAND BIOSPHERE:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||UPPER OCEAN:1||ATMOSPHERE FEEDBACKS:1||SUMMER MONSOON:1||TELECONNECTION PATTERNS:1||EASTERN EQUATORIAL PACIFIC:1||Indian Ocean Dipole:1||SST:1||MIDWINTER SUPPRESSION:1||LINE SIMULATION CHARACTERISTICS:1||MULTIDECADAL VARIABILITY:1||SEAICE COVER:1||ECOSYSTEMS:1||BLOOMS:1||PENETRATIVE RADIATION:1||SOILMOISTURE:1||HEAT WAVES:1||FEEDBACKS:1||seasonal variation:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||EARTH SYSTEM MODELS:1||CARBONCYCLE FEEDBACKS:1||TRADE WINDS:1||PROJECTIONS:1||CALANUSFINMARCHICUS:1||WINTER MONSOON:1||WIND:1||El NinoSouthern Oscillation:1||REGION:1||MEAN FLOW:1||DIOXIDE:1||GROWTH:1||NITROGEN:1||GENERALCIRCULATION MODEL:1||DEEP CONVECTION:1||ATMOSPHERE:1||SST ANOMALIES:1||CIRCULATION:1||ARCTIC OSCILLATION:1||CLIMATE SENSITIVITY:1||precipitation (climatology):1||Pacific Ocean:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||MULTIMODEL ENSEMBLE:1||TOINTERANNUAL PREDICTION:1||OCEAN:1||INDIANOCEAN:1||TIBETAN PLATEAU:1||airsea interaction:1||Pacific Ocean (West):1||CHINA SEA:1||TEMPERATURE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||EASTERN EDGE:1||NORTHERNHEMISPHERE:1||FLOW:1||PREDICTABILITY:1||HYDROLOGICAL CYCLE:1||El Nino:1||climate modeling:1||CMIP:1||KUROSHIO:1||ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC SST:1||PERSPECTIVE:1||LANDSURFACE:1||REANALYSIS:1||GLOBAL PRECIPITATION:1||TROPICAL ATLANTIC:1||CONNECTION:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||NET PRIMARY PRODUCTION:1||CLIMATECHANGE:1||INDONESIAN SEAS:1||CHUKCHI:1||EASTERNPACIFIC:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||Climate change:1||SYNOPTIC EDDY:1||LAND BIOSPHERE:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||UPPER OCEAN:1||ATMOSPHERE FEEDBACKS:1||SUMMER MONSOON:1||TELECONNECTION PATTERNS:1||EASTERN EQUATORIAL PACIFIC:1||Indian Ocean Dipole:1||SST:1||MIDWINTER SUPPRESSION:1||LINE SIMULATION CHARACTERISTICS:1||MULTIDECADAL VARIABILITY:1||SEAICE COVER:1||ECOSYSTEMS:1||BLOOMS:1||PENETRATIVE RADIATION:1||SOILMOISTURE:1||HEAT WAVES:1||FEEDBACKS:1||seasonal variation:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||EARTH SYSTEM MODELS:1||CARBONCYCLE FEEDBACKS:1||TRADE WINDS:1||PROJECTIONS:1||CALANUSFINMARCHICUS:1||WINTER MONSOON:1||WIND:1||El NinoSouthern Oscillation:1||REGION:1||MEAN FLOW:1||DIOXIDE:1||GROWTH:1||NITROGEN:1||GENERALCIRCULATION MODEL:1||DEEP CONVECTION:1||ATMOSPHERE:1||SST ANOMALIES:1||CIRCULATION:1||ARCTIC OSCILLATION:1||CLIMATE SENSITIVITY:1||precipitation (climatology):1||Pacific Ocean:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||MULTIMODEL ENSEMBLE:1||TOINTERANNUAL PREDICTION:1||OCEAN:1||INDIANOCEAN:1||TIBETAN PLATEAU:1||airsea interaction:1||Pacific Ocean (West):1||CHINA SEA:1||TEMPERATURE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||EASTERN EDGE:1||NORTHERNHEMISPHERE:1||FLOW:1||PREDICTABILITY:1||HYDROLOGICAL CYCLE:1||El Nino:1||climate modeling:1||CMIP:1||KUROSHIO:1||ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC SST:1||PERSPECTIVE:1||LANDSURFACE:1||REANALYSIS:1||GLOBAL PRECIPITATION:1||TROPICAL ATLANTIC:1||CONNECTION:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||NET PRIMARY PRODUCTION:1||CLIMATECHANGE:1||INDONESIAN SEAS:1||CHUKCHI:1||EASTERNPACIFIC:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||Climate change:1||SYNOPTIC EDDY:1||LAND BIOSPHERE:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||UPPER OCEAN:1||ATMOSPHERE FEEDBACKS:1||SUMMER MONSOON:1||TELECONNECTION PATTERNS:1||EASTERN EQUATORIAL PACIFIC:1||Indian Ocean Dipole:1||SST:1||MIDWINTER SUPPRESSION:1||LINE SIMULATION CHARACTERISTICS:1||MULTIDECADAL VARIABILITY:1||SEAICE COVER:1||ECOSYSTEMS:1||BLOOMS:1||PENETRATIVE RADIATION:1||SOILMOISTURE:1||HEAT WAVES:1||FEEDBACKS:1||seasonal variation:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||EARTH SYSTEM MODELS:1||CARBONCYCLE FEEDBACKS:1||TRADE WINDS:1||PROJECTIONS:1||CALANUSFINMARCHICUS:1||WINTER MONSOON:1||WIND:1||El NinoSouthern Oscillation:1||REGION:1||MEAN FLOW:1||DIOXIDE:1||GROWTH:1||NITROGEN:1||GENERALCIRCULATION MODEL:1||DEEP CONVECTION:1||ATMOSPHERE:1||SST ANOMALIES:1||CIRCULATION:1||ARCTIC OSCILLATION:1||CLIMATE SENSITIVITY:1||precipitation (climatology):1||Pacific Ocean:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||MULTIMODEL ENSEMBLE:1||TOINTERANNUAL PREDICTION:1||OCEAN:1||INDIANOCEAN:1||TIBETAN PLATEAU:1||airsea interaction:1||Pacific Ocean (West):1||CHINA SEA:1||TEMPERATURE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||EASTERN EDGE:1||NORTHERNHEMISPHERE:1||FLOW:1||PREDICTABILITY:1||HYDROLOGICAL CYCLE:1||El Nino:1||climate modeling:1||CMIP:1||KUROSHIO:1||ELNINO:7||VARIABILITY:6||ENSO:4||SEASURFACE TEMPERATURE:4||CLIMATE:3||ARCTIC SEAICE:3||Korea and East Asia:2||PRECIPITATION EXTREMES:2||SURFACE TEMPERATURE:2||MONSOON:2||TROPICAL PACIFIC:2||WINTER:2||MIDLATITUDE WEATHER:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||TRENDS:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||INTERANNUAL VARIABILITY:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||OSCILLATION:2||PACIFIC:2||Weather extremes:2||MODEL:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||WEATHER:1||ATLANTIC 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