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KUG, JONG SEONG (국종성)
Div of Environmental Science & Engineering(환경공학부)
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VARIABILITY:9||ENSO:7||ELNINO:6||SEASURFACE TEMPERATURE:6||CLIMATE:4||CLIMATECHANGE:4||El Nino:3||MODEL:3||OSCILLATION:3||ARCTIC SEAICE:3||PACIFIC:3||EARTH SYSTEM MODELS:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||CIRCULATION:2||precipitation (climatology):2||Pacific Ocean:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||OCEAN:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||climate modeling:2||TEMPERATURE:2||TROPICAL PACIFIC:2||INTERANNUAL VARIABILITY:2||MONSOON:2||asymmetry:2||SURFACE TEMPERATURE:2||PRECIPITATION EXTREMES:2||Korea and East Asia:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||Weather extremes:2||MIDLATITUDE WEATHER:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||ICE:1||PRODUCTIVITY:1||LANDSURFACE:1||La Nina:1||REANALYSIS:1||amplification:1||arctic environment:1||FUTURE CLIMATE:1||WEATHER:1||GLOBAL PRECIPITATION:1||ATLANTIC SST:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||EASTERNPACIFIC:1||CO2 GROWTHRATE:1||INDONESIAN SEAS:1||NET PRIMARY PRODUCTION:1||Climate change:1||SYNOPTIC EDDY:1||Arctic climate changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT WAVES:1||PENETRATIVE RADIATION:1||RELEVANCE:1||hydrological response:1||seasonal variation:1||FEEDBACKS:1||MULTIDECADAL VARIABILITY:1||LINE SIMULATION CHARACTERISTICS:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||WINTER MONSOON:1||CALANUSFINMARCHICUS:1||CMIP5:1||PRECIPITATION:1||El NinoSouthern Oscillation:1||WIND:1||TRADE WINDS:1||CARBONCYCLE FEEDBACKS:1||REGION:1||MEAN FLOW:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||SST ANOMALIES:1||ARCTIC OSCILLATION:1||DEEP CONVECTION:1||ATMOSPHERE:1||RAINFOREST:1||GROWTH:1||CLIMATE SENSITIVITY:1||DIOXIDE:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||TOINTERANNUAL PREDICTION:1||MULTIMODEL ENSEMBLE:1||AMO:1||TIBETAN PLATEAU:1||INDIANOCEAN:1||atmospheric circulation:1||global warming:1||Pacific Ocean (Tropical):1||DROUGHT SENSITIVITY:1||airsea interaction:1||Pacific Ocean (West):1||RADIATION:1||DRAWDOWN:1||NORTHERNHEMISPHERE:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||PREDICTABILITY:1||WINTER:1||FLOW:1||intertropical convergence zone:1||ENSO TELECONNECTIONS:1||CMIP:1||TRENDS:1||HYDROLOGICAL CYCLE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||VARIABILITY:9||ENSO:7||ELNINO:6||SEASURFACE TEMPERATURE:6||CLIMATE:4||CLIMATECHANGE:4||El Nino:3||MODEL:3||OSCILLATION:3||ARCTIC SEAICE:3||PACIFIC:3||EARTH SYSTEM MODELS:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||CIRCULATION:2||precipitation (climatology):2||Pacific Ocean:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||OCEAN:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||climate modeling:2||TEMPERATURE:2||TROPICAL PACIFIC:2||INTERANNUAL VARIABILITY:2||MONSOON:2||asymmetry:2||SURFACE TEMPERATURE:2||PRECIPITATION EXTREMES:2||Korea and East Asia:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||Weather extremes:2||MIDLATITUDE WEATHER:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||ICE:1||PRODUCTIVITY:1||LANDSURFACE:1||La Nina:1||REANALYSIS:1||amplification:1||arctic environment:1||FUTURE CLIMATE:1||WEATHER:1||GLOBAL PRECIPITATION:1||ATLANTIC SST:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||EASTERNPACIFIC:1||CO2 GROWTHRATE:1||INDONESIAN SEAS:1||NET PRIMARY PRODUCTION:1||Climate change:1||SYNOPTIC EDDY:1||Arctic climate changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT WAVES:1||PENETRATIVE RADIATION:1||RELEVANCE:1||hydrological response:1||seasonal variation:1||FEEDBACKS:1||MULTIDECADAL VARIABILITY:1||LINE SIMULATION CHARACTERISTICS:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||WINTER MONSOON:1||CALANUSFINMARCHICUS:1||CMIP5:1||PRECIPITATION:1||El NinoSouthern Oscillation:1||WIND:1||TRADE WINDS:1||CARBONCYCLE FEEDBACKS:1||REGION:1||MEAN FLOW:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||SST ANOMALIES:1||ARCTIC OSCILLATION:1||DEEP CONVECTION:1||ATMOSPHERE:1||RAINFOREST:1||GROWTH:1||CLIMATE SENSITIVITY:1||DIOXIDE:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||TOINTERANNUAL PREDICTION:1||MULTIMODEL ENSEMBLE:1||AMO:1||TIBETAN PLATEAU:1||INDIANOCEAN:1||atmospheric circulation:1||global warming:1||Pacific Ocean (Tropical):1||DROUGHT SENSITIVITY:1||airsea interaction:1||Pacific Ocean (West):1||RADIATION:1||DRAWDOWN:1||NORTHERNHEMISPHERE:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||PREDICTABILITY:1||WINTER:1||FLOW:1||intertropical convergence zone:1||ENSO TELECONNECTIONS:1||CMIP:1||TRENDS:1||HYDROLOGICAL CYCLE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||VARIABILITY:9||ENSO:7||ELNINO:6||SEASURFACE TEMPERATURE:6||CLIMATE:4||CLIMATECHANGE:4||El Nino:3||MODEL:3||OSCILLATION:3||ARCTIC SEAICE:3||PACIFIC:3||EARTH SYSTEM MODELS:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||CIRCULATION:2||precipitation (climatology):2||Pacific Ocean:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||OCEAN:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||climate modeling:2||TEMPERATURE:2||TROPICAL PACIFIC:2||INTERANNUAL VARIABILITY:2||MONSOON:2||asymmetry:2||SURFACE TEMPERATURE:2||PRECIPITATION EXTREMES:2||Korea and East Asia:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||Weather extremes:2||MIDLATITUDE WEATHER:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||ICE:1||PRODUCTIVITY:1||LANDSURFACE:1||La Nina:1||REANALYSIS:1||amplification:1||arctic environment:1||FUTURE CLIMATE:1||WEATHER:1||GLOBAL PRECIPITATION:1||ATLANTIC SST:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||EASTERNPACIFIC:1||CO2 GROWTHRATE:1||INDONESIAN SEAS:1||NET PRIMARY PRODUCTION:1||Climate change:1||SYNOPTIC EDDY:1||Arctic climate changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT WAVES:1||PENETRATIVE RADIATION:1||RELEVANCE:1||hydrological response:1||seasonal variation:1||FEEDBACKS:1||MULTIDECADAL VARIABILITY:1||LINE SIMULATION CHARACTERISTICS:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||WINTER MONSOON:1||CALANUSFINMARCHICUS:1||CMIP5:1||PRECIPITATION:1||El NinoSouthern Oscillation:1||WIND:1||TRADE WINDS:1||CARBONCYCLE FEEDBACKS:1||REGION:1||MEAN FLOW:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||SST ANOMALIES:1||ARCTIC OSCILLATION:1||DEEP CONVECTION:1||ATMOSPHERE:1||RAINFOREST:1||GROWTH:1||CLIMATE SENSITIVITY:1||DIOXIDE:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||TOINTERANNUAL PREDICTION:1||MULTIMODEL ENSEMBLE:1||AMO:1||TIBETAN PLATEAU:1||INDIANOCEAN:1||atmospheric circulation:1||global warming:1||Pacific Ocean (Tropical):1||DROUGHT SENSITIVITY:1||airsea interaction:1||Pacific Ocean (West):1||RADIATION:1||DRAWDOWN:1||NORTHERNHEMISPHERE:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||PREDICTABILITY:1||WINTER:1||FLOW:1||intertropical convergence zone:1||ENSO TELECONNECTIONS:1||CMIP:1||TRENDS:1||HYDROLOGICAL CYCLE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||VARIABILITY:9||ENSO:7||ELNINO:6||SEASURFACE TEMPERATURE:6||CLIMATE:4||CLIMATECHANGE:4||El Nino:3||MODEL:3||OSCILLATION:3||ARCTIC SEAICE:3||PACIFIC:3||EARTH SYSTEM MODELS:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||CIRCULATION:2||precipitation (climatology):2||Pacific Ocean:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||OCEAN:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||climate modeling:2||TEMPERATURE:2||TROPICAL PACIFIC:2||INTERANNUAL VARIABILITY:2||MONSOON:2||asymmetry:2||SURFACE TEMPERATURE:2||PRECIPITATION EXTREMES:2||Korea and East Asia:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||Weather extremes:2||MIDLATITUDE WEATHER:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||ICE:1||PRODUCTIVITY:1||LANDSURFACE:1||La Nina:1||REANALYSIS:1||amplification:1||arctic environment:1||FUTURE CLIMATE:1||WEATHER:1||GLOBAL PRECIPITATION:1||ATLANTIC SST:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||EASTERNPACIFIC:1||CO2 GROWTHRATE:1||INDONESIAN SEAS:1||NET PRIMARY PRODUCTION:1||Climate change:1||SYNOPTIC EDDY:1||Arctic climate changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT WAVES:1||PENETRATIVE RADIATION:1||RELEVANCE:1||hydrological response:1||seasonal variation:1||FEEDBACKS:1||MULTIDECADAL VARIABILITY:1||LINE SIMULATION CHARACTERISTICS:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||WINTER MONSOON:1||CALANUSFINMARCHICUS:1||CMIP5:1||PRECIPITATION:1||El NinoSouthern Oscillation:1||WIND:1||TRADE WINDS:1||CARBONCYCLE FEEDBACKS:1||REGION:1||MEAN FLOW:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||SST ANOMALIES:1||ARCTIC OSCILLATION:1||DEEP CONVECTION:1||ATMOSPHERE:1||RAINFOREST:1||GROWTH:1||CLIMATE SENSITIVITY:1||DIOXIDE:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||TOINTERANNUAL PREDICTION:1||MULTIMODEL ENSEMBLE:1||AMO:1||TIBETAN PLATEAU:1||INDIANOCEAN:1||atmospheric circulation:1||global warming:1||Pacific Ocean (Tropical):1||DROUGHT SENSITIVITY:1||airsea interaction:1||Pacific Ocean (West):1||RADIATION:1||DRAWDOWN:1||NORTHERNHEMISPHERE:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||PREDICTABILITY:1||WINTER:1||FLOW:1||intertropical convergence zone:1||ENSO TELECONNECTIONS:1||CMIP:1||TRENDS:1||HYDROLOGICAL CYCLE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||VARIABILITY:9||ENSO:7||ELNINO:6||SEASURFACE TEMPERATURE:6||CLIMATE:4||CLIMATECHANGE:4||El Nino:3||MODEL:3||OSCILLATION:3||ARCTIC SEAICE:3||PACIFIC:3||EARTH SYSTEM MODELS:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||CIRCULATION:2||precipitation (climatology):2||Pacific Ocean:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||OCEAN:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||climate modeling:2||TEMPERATURE:2||TROPICAL PACIFIC:2||INTERANNUAL VARIABILITY:2||MONSOON:2||asymmetry:2||SURFACE TEMPERATURE:2||PRECIPITATION EXTREMES:2||Korea and East Asia:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||Weather extremes:2||MIDLATITUDE WEATHER:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||ICE:1||PRODUCTIVITY:1||LANDSURFACE:1||La Nina:1||REANALYSIS:1||amplification:1||arctic environment:1||FUTURE CLIMATE:1||WEATHER:1||GLOBAL PRECIPITATION:1||ATLANTIC SST:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||EASTERNPACIFIC:1||CO2 GROWTHRATE:1||INDONESIAN SEAS:1||NET PRIMARY PRODUCTION:1||Climate change:1||SYNOPTIC EDDY:1||Arctic climate changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT WAVES:1||PENETRATIVE RADIATION:1||RELEVANCE:1||hydrological response:1||seasonal variation:1||FEEDBACKS:1||MULTIDECADAL VARIABILITY:1||LINE SIMULATION CHARACTERISTICS:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||WINTER MONSOON:1||CALANUSFINMARCHICUS:1||CMIP5:1||PRECIPITATION:1||El NinoSouthern Oscillation:1||WIND:1||TRADE WINDS:1||CARBONCYCLE FEEDBACKS:1||REGION:1||MEAN FLOW:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||SST ANOMALIES:1||ARCTIC OSCILLATION:1||DEEP CONVECTION:1||ATMOSPHERE:1||RAINFOREST:1||GROWTH:1||CLIMATE SENSITIVITY:1||DIOXIDE:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||TOINTERANNUAL PREDICTION:1||MULTIMODEL ENSEMBLE:1||AMO:1||TIBETAN PLATEAU:1||INDIANOCEAN:1||atmospheric circulation:1||global warming:1||Pacific Ocean (Tropical):1||DROUGHT SENSITIVITY:1||airsea interaction:1||Pacific Ocean (West):1||RADIATION:1||DRAWDOWN:1||NORTHERNHEMISPHERE:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||PREDICTABILITY:1||WINTER:1||FLOW:1||intertropical convergence zone:1||ENSO TELECONNECTIONS:1||CMIP:1||TRENDS:1||HYDROLOGICAL CYCLE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||VARIABILITY:9||ENSO:7||ELNINO:6||SEASURFACE TEMPERATURE:6||CLIMATE:4||CLIMATECHANGE:4||El Nino:3||MODEL:3||OSCILLATION:3||ARCTIC SEAICE:3||PACIFIC:3||EARTH SYSTEM MODELS:2||WESTERN PACIFIC:2||SOUTHERNOSCILLATION:2||CLIMATE VARIABILITY:2||climate variability and change:2||CIRCULATION:2||precipitation (climatology):2||Pacific Ocean:2||EQUATORIAL PACIFICOCEAN:2||WARM POOL:2||climate extremes:2||SOUTHKOREA:2||QUANTILE REGRESSION:2||OCEAN:2||SUMMER INTRASEASONAL OSCILLATION:2||ATMOSPHERIC RESPONSE:2||climate modeling:2||TEMPERATURE:2||TROPICAL PACIFIC:2||INTERANNUAL VARIABILITY:2||MONSOON:2||asymmetry:2||SURFACE TEMPERATURE:2||PRECIPITATION EXTREMES:2||Korea and East Asia:2||EASTASIA:2||MADDENJULIAN OSCILLATION:2||Weather extremes:2||MIDLATITUDE WEATHER:2||INTERDECADAL CHANGES:1||ZONAL FLOW FEEDBACK:1||ICE:1||PRODUCTIVITY:1||LANDSURFACE:1||La Nina:1||REANALYSIS:1||amplification:1||arctic environment:1||FUTURE CLIMATE:1||WEATHER:1||GLOBAL PRECIPITATION:1||ATLANTIC SST:1||IMPACT:1||CLIMATE MODELS:1||PHYTOPLANKTON:1||MIDLATITUDE STORM TRACKS:1||DYNAMICS:1||phytoplanktonclimate interaction:1||SOUTHERNOCEAN:1||LANINA:1||NONLINEARITY:1||SURFACETEMPERATURE:1||GEOPOTENTIAL HEIGHT:1||ENSO PREDICTION:1||ENERGETICS:1||ENSEMBLE:1||EASTERNPACIFIC:1||CO2 GROWTHRATE:1||INDONESIAN SEAS:1||NET PRIMARY PRODUCTION:1||Climate change:1||SYNOPTIC EDDY:1||Arctic climate changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT 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changes:1||SUMMER MONSOON:1||ATMOSPHERE FEEDBACKS:1||TELECONNECTIONS:1||ANOMALIES:1||TELECONNECTION PATTERNS:1||Indian Ocean Dipole:1||EASTERN EQUATORIAL PACIFIC:1||INDIANOCEAN DIPOLE:1||ENSO DYNAMICS:1||LAND BIOSPHERE:1||MIDWINTER SUPPRESSION:1||biogeophysical feedback:1||SOILMOISTURE:1||HEAT WAVES:1||PENETRATIVE RADIATION:1||RELEVANCE:1||hydrological response:1||seasonal variation:1||FEEDBACKS:1||MULTIDECADAL VARIABILITY:1||LINE SIMULATION CHARACTERISTICS:1||onsoons:1||ZONAL ADVECTIVE FEEDBACKS:1||2LAYER MODEL:1||WINTER MONSOON:1||CALANUSFINMARCHICUS:1||CMIP5:1||PRECIPITATION:1||El NinoSouthern Oscillation:1||WIND:1||TRADE WINDS:1||CARBONCYCLE FEEDBACKS:1||REGION:1||MEAN FLOW:1||POLAR AMPLIFICATION:1||GENERALCIRCULATION MODEL:1||Atlantic Multidecadal Oscillation:1||SST ANOMALIES:1||ARCTIC OSCILLATION:1||DEEP CONVECTION:1||ATMOSPHERE:1||RAINFOREST:1||GROWTH:1||CLIMATE SENSITIVITY:1||DIOXIDE:1||ASIANAUSTRALIAN MONSOON:1||ANNULAR MODES:1||TOINTERANNUAL PREDICTION:1||MULTIMODEL ENSEMBLE:1||AMO:1||TIBETAN PLATEAU:1||INDIANOCEAN:1||atmospheric circulation:1||global warming:1||Pacific Ocean (Tropical):1||DROUGHT SENSITIVITY:1||airsea interaction:1||Pacific Ocean (West):1||RADIATION:1||DRAWDOWN:1||NORTHERNHEMISPHERE:1||EASTERN EDGE:1||ASYMMETRY:1||EVENTS:1||PREDICTABILITY:1||WINTER:1||FLOW:1||intertropical convergence zone:1||ENSO TELECONNECTIONS:1||CMIP:1||TRENDS:1||HYDROLOGICAL CYCLE:1||WESTERN TROPICAL PACIFIC:1||EQUATORIAL PACIFIC:1||
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