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KUG, JONG SEONG (국종성)

Div of Environmental Science & Engineering(환경공학부)

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

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