ScholarWorks@Hanyang University ERICA Campus: Yeh, Sang Wook

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Yeh, Sang Wook (예상욱)

ERICA 공학대학 (ERICA 해양융합공학과)

Research Area: 기후역학/해양-대기 상호작용, 기후 진단, 기후 변화 역학, Climate Dynamics/Ocean-Atmosphere Interactions, Climate Diagnosis, Climate Change Dynamics

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ENSO:34||CLIMATE:16||OCEAN:15||SEASURFACE TEMPERATURE:13||ELNINO:13||El Nino:13||TROPICAL PACIFIC:8||VARIABILITY:7||sea surface temperature:7||EVENTS:7||ANOMALIES:6||Pacific decadal oscillation:6||Sea surface temperature:6||CMIP5:5||North Pacific:5||North Pacific Oscillation:5||DECADAL VARIABILITY:5||East Asia:5||PACIFIC:5||INTERANNUAL VARIABILITY:5||CIRCULATION:5||Atmospheric circulation:5||Precipitation:5||precipitation:4||El Niño:4||internal climate variability:4||PRECIPITATION:4||NORTH PACIFIC:4||Climate variability:4||MODEL:4||regime shift:4||EQUATORIAL PACIFIC:4||WARM POOL:4||Pacific Decadal Oscillation:4||LANINA:4||Atmosphereocean interaction:4||Southern Oscillation:3||GENERALCIRCULATION MODEL:3||SST variability:3||anthropogenic forcing:3||Climate change:3||OSCILLATION:3||REANALYSIS:3||TELECONNECTION:3||Mixed layer depth:3||TELECONNECTIONS:3||WINTER:3||PDO:3||ATMOSPHERIC BRIDGE:3||REGIME SHIFTS:3||climate model:3||CONCEPTUALMODEL:3||East Asian summer monsoon:3||CMIP5 climate models:3||Teleconnection:2||DYNAMICS:2||Temperature:2||western North Pacific subtropical high:2||western tropical Pacific:2||Central Pacific El Nino:2||CLIMATE VARIABILITY:2||Heat budget of the mixed layer:2||PM2.5:2||East/Japan Sea:2||EASTASIA:2||Particulate matter:2||MODULATION:2||EASTERNPACIFIC:2||ECHOG:2||RAINFALL:2||marine heatwaves:2||WARMING HIATUS:2||IMPACT:2||El Nino diversity:2||Walker circulation:2||Warm Pool El Nino:2||Chemistryclimate model:2||INTERDECADAL VARIABILITY:2||SEASURFACE TEMPERATURES:2||Western North Pacific subtropical high:2||China:2||CMIP6:2||ITCZ:2||NINOSOUTHERNOSCILLATION:2||1000YR CONTROL SIMULATION:2||SOUTHERNOSCILLATION:2||SST:2||SST ANOMALIES:2||El Ninolike warming:2||ENSO diversity:2||Climate change projections:2||SUMMER MONSOON:2||atmospheric circulation:2||CO2 concentration:2||SURFACETEMPERATURE:2||Arctic Oscillation:2||Interannual variability:2||Arctic amplification:2||Aerosol:2||Sea surface temperature (SST):2||JAPAN:2||Cold Tongue El Nino:2||CESMLE:2||Coupled general circulation models:2||COUPLED CLIMATE MODEL:2||COUPLED CLIMATE MODELS:2||teleconnection:2||GEOSChem:2||COUPLED GCM:2||EXTRATROPICAL SST ANOMALIES:2||COUPLED MODEL:2||tropical cyclone:2||GRIMs:2||TEMPERATURE:2||CGCM:2||Global warming:2||EVOLUTION:1||EXTREMES:1||Earth system models:1||East Asia marginal seas:1||East Asian:1||East Asian CO2 concentrations:1||East Asian Summer Monsoon:1||East Asian precipitation:1||East Asian winter monsoon:1||East Asian winter temperatures:1||East Asia’s extreme hot day:1||East China Sea:1||East China Sea modeling:1||Eastern Pacific El Niño:1||Eastern Tropical Pacific:1||El NiñoSouthern Oscillation:1||El Ni & ntilde:1||El Nino Modoki:1||El Nino and Southern Oscillation:1||El Nino onset:1||El Nino onset regime shift:1||El Nino's transition:1||El NinoLa Nina asymmetry:1||El NinoSouthern Oscillation:1||El NinoSouthern Oscillation (ENSO):1||ElNino:1||Emission control policy:1||Emission inventories (EIs):1||Equatorial Pacific:1||Eurasian climate:1||Eurasian pattern:1||Eurasian snow cover:1||Extreme El Nino event:1||Extreme events:1||FALLOUT:1||FIELD:1||Fast El Nino transition:1||Forest fire aerosols:1||Fukushima:1||Future climate:1||GESOChem:1||GLOBAL CLIMATECHANGE:1||GLOBAL OCEAN:1||GLOBAL OCEANS:1||GRIMSCCM:1||General circulation models:1||GloSea5:1||Global warming, El Nino Modoki:1||HEAT FLUXES:1||HEATTRANSPORT:1||HEIGHT FIELD:1||HEMISPHERE CIRCULATION:1||HYSPLIT:1||Hadley circulation:1||Health:1||Heating:1||Heavytails law:1||Highfreqeuncy variability:1||HilbertHuang transform:1||Hot days:1||Humidity:1||Hydrological cycle:1||ICEAGE:1||IMPACTS:1||INDIANOCEAN:1||INDIANOCEAN DIPOLE:1||INDOPACIFIC:1||INTERMEDIATE WATER:1||INTERNAL VARIABILITY:1||IRRADIANCE:1||Ice loss/growth:1||Indian Ocean:1||Indian Ocean SST variability:1||Indian Ocean warming:1||Indian monsoon rainfall:1||Indian ocean:1||IndoPacific Warm Pool:1||Interdecadal variability:1||Intraseasonal variability:1||Intrinsic atmospheric circulation:1||JAPAN SEA:1||Jets:1||Kmean clustering:1||KIOSTESM:1||KUROSHIO EXTENSION REGION:1||KUROSHIOOYASHIO EXTENSION:1||Kinetic energy:1||Korea and East Asia:1||Korean climate:1||Korean climate variation:1||Korean heat wave:1||Korean peninsula:1||Korean summer temperature:1||Korean winter temperature:1||Kuroshio Current:1||Kuroshio intrusion:1||Kuroshio recirculation gyre:1||LINEARRESPONSE:1||La Niña:1||La Nina:1||La Ninalike:1||La Ninalike mean state:1||Largescale motions:1||Last millennium:1||Latent heat:1||Linear baroclinic model:1||Longrange transport:1||Lowfrequency variability:1||MARGINAL SEA:1||MERIDIONAL MODE:1||MJO:1||MODES:1||MODOKI:1||MOM4:1||MONSOON:1||MULTIMODEL ENSEMBLE:1||MYRIADHESA:1||Madden–Julian Oscillation:1||Mean state:1||Meteorology:1||Mt. Baekdu:1||Multiple linear regression model:1||NAO:1||NEC bifurcation region:1||NEPARTAK:1||NINO:1||NINO SOUTHERN OSCILLATION:1||NINO SOUTHERNOSCILLATION:1||NINO/SOUTHERN OSCILLATION:1||NONLINEARITY:1||NORTHAMERICA:1||NORTHPACIFIC:1||NORTHERN WINTER:1||NORTHERNHEMISPHERE:1||NPO's southern lobe:1||NPOlike sea level pressure:1||Nonlinearity:1||North Atlantic Tripolelike:1||North Pacific Gyre Oscillation:1||North Pacific Ocean:1||North Pacific high:1||North Pacific subtropical high:1||Northeast Asia:1||Northeast Asian summer precipitation:1||Northern Hemisphere:1||Northern Hemisphere land monsoon:1||Northwest Pacific anticyclone:1||OCEAN COLOR OBSERVATIONS:1||OCEAN HEAT UPTAKE:1||OCEANATMOSPHERE:1||OCEANS:1||OGCM SIMULATION:1||Ocean general circulation model:1||Ozone:1||PACIFIC CONVERGENCE ZONE:1||PACIFIC DECADAL VARIABILITY:1||PACIFIC INTERANNUAL VARIABILITY:1||PART I:1||PHYTOPLANKTON:1||PM (10) transport:1||PM<sub>2.5</sub>:1||PM2.5 concentrations:1||PRECIPITATION VARIABILITY:1||PREDICTABILITY:1||PROJECTIONS:1||Pacific Decadal Oscillation (PDO):1||Pacific Ocean:1||Pacific Ocean (North):1||Pacific Ocean (Tropical):1||Pacific meridional mode:1||Paris agreement:1||Particulate matter 2.5:1||Past sea surface temperature:1||Physical parameterization:1||Pollutant aerosols:1||QBtype ENSO:1||RADIOCESIUM:1||RAINFALL VARIABILITY:1||REANALYSIS PROJECT:1||REDUCTION:1||REFLECTION:1||REGIONAL CLIMATE MODEL:1||Regime shift:1||Regional biases:1||Regional climate change:1||Regional meteorology:1||SEASONAL FOOTPRINTING MECHANISM:1||SENSITIVITY:1||SHIFTS:1||SIMULATION:1||SOLAR:1||SOUTH ASIAN MONSOON:1||SOUTHPACIFIC:1||SST forcing:1||STRATOSPHERIC AEROSOL:1||SUBTROPICAL MODE WATER:1||SUMMER:1||SURFACE TEMPERATURE VARIABILITY:1||SURFACETEMPERATURE ANOMALIES:1||SYSTEM:1||Scale interaction:1||Sea salt:1||Sea surface:1||Sea surface temperatures:1||Seasonal Prediction:1||Seasonal climate prediction:1||Seasonal footprinting mechanism:1||Seasonal prediction:1||Severe PM 10 events:1||Siberian High:1||Siberian high:1||Simple linear regression:1||Simulation:1||South China Sea:1||South Korea:1||South Pacific Meridional Mode:1||Southern Ocean warm bias:1||Southern annular mode:1||Statedependent noise:1||Statistics:1||Stochastic:1||Stratification:1||Surface temperature:1||Synopticscale processes:1||TELECONNECTION PATTERNS:1||TIBETAN PLATEAU:1||TONGUE ELNINO:1||TRAJECTORIES:1||TRANSITION:1||TRENDS:1||TROPICAL WESTERN PACIFIC:1||TROPOSPHERIC BIENNIAL OSCILLATION:1||Taiwan Warm Current:1||Teleconnections:1||Terrestrial vegetation activity:1||Tropical Pacific precipitation:1||Tropical SST warming pattern:1||Tropical convection:1||Tropical cyclone:1||Tropical equatorial pacific:1||Tropical variability:1||Tropicsmidlatitudes coupled system:1||Tropics/midlatitude teleconnections:1||Tropospheric ozone:1||Tsushima Warm Current:1||UNITEDSTATES:1||UPPEROCEAN:1||VERTICAL STRUCTURE:1||Variability:1||Ventilation effect:1||Vertical mixing scheme:1||Vertical stratification:1||Volcanic forcing:1||WACElike pattern:1||WALKER CIRCULATION:1||WARMPOOL:1||WATER TEMPERATURE:1||WAVE DYNAMICS:1||WESTERLY WIND BURSTS:1||WESTERLY WIND EVENTS:1||WESTERN PACIFIC:1||WORLDS OCEANS:1||Warm nights:1||Wave propagation:1||Waves:1||Weather noise:1||Westerlies:1||Western China Autumn Rainfall:1||Winter monsoon:1||Yellow and East China Sea (YECS):1||Yellow sea:1||Yellow/East China Sea:1||a:1||adjustment:1||aerosol forcing:1||aerosol optical depth:1||airsea interaction:1||aleutian low:1||anomalous vertical motion pattern:1||anthropogenic aerosols:1||arctic oscillation:1||asymmetry:1||atmosphere circulation:1||atmosphereocean interaction:1||atmospheric conditions:1||atmospheric energy budget:1||atmospheric teleconnections:1||attribution:1||barrier layer thickness:1||benefit:1||bifurcation latitude:1||biological pump:1||boreal winter:1||carbon neutrality:1||central equatorial Pacific Ocean:1||chemistrytransport model:1||chlorophyll:1||cirrus:1||climate models:1||climate prediction:1||climate projection:1||climate sensitivity:1||climate variability:1||cloud feedback:1||clusters:1||conventional El Nino:1||coupled model:1||decadal change:1||decadal variation:1||definition:1||delay AMOC response:1||diversity:1||drought:1||dust index:1||east asia:1||eastern Pacific cooling:1||emergent relationship:1||ensemble model simulations:1||estimation model:1||extreme event:1||extreme hot days:1||extreme precipitation:1||far East Asia:1||frequency analysis:1||future climate:1||future projection:1||future projection of extreme El Nino:1||general circulation model:1||global atmospheric chemistry model:1||global climate model:1||global cooling hiatus:1||global warming:1||heat budget:1||heat wave:1||heavy rainfall:1||heavyprecipitation extreme:1||hottemperature extreme:1||hysteresis:1||increased CO2:1||interactive ensemble model:1||intermodel diversity</AUTHOR_KEYWORD>:1||intermodel spread:1||intraseasonal oscillation:1||intraseasonal precipitation variability:1||iris effect:1||kmeans clustering:1||korean winter temperature:1||kuoeliassen equation:1||landsea thermal contrast:1||large ensemble:1||largescale environments:1||linear relationship:1||linear trend:1||low level cloud amount feedback:1||marginal sea surface temperature:1||meridional wave:1||meteorological response:1||mid1990s:1||midlatitude climate variation:1||mitigation pathways:1||mixed layer depth:1||monsoon:1||monsoon precipitation:1||netzero CO2 emission:1||nonstationary characteristics:1||numerical weather prediction:1||o and La Ni & ntilde:1||ocean general circulation model:1||ocean mean state:1||oceanic:1||oceanic dynamic adjustment:1||oceanic stratification:1||periodicity:1||polar climate variation:1||polar vortex:1||population exposure:1||power spectral analysis:1||precipitation change:1||precipitation variability:1||quadrupled CO2 experiment:1||reemergence:1||refreshening:1||relationship:1||salt advection feedback:1||sea ice:1||sea ice extent</AUTHOR_KEYWORD>:1||sea level pressure:1||sea surface salinity:1||sea surface temperature gradient:1||seasonal forecast:1||seasonal simulation:1||seasonality:1||sediment trap:1||sensitivity:1||siberian high:1||signal and noise:1||simulation uncertainty:1||sinking particle:1||soil moisture:1||southern annular mode:1||southern ocean condition:1||spatial structure:1||springtime ENSO variability:1||stationary Rossby wave:1||stratification:1||subseasonal to seasonal prediction:1||subseasonal variability:1||sulfate aerosols:1||summer monsoon:1||summer precipitation:1||surface heating:1||surface temperature:1||surface temperature variability:1||temperature and precipitation:1||temperature anomalies:1||the Paris Agreement:1||time of emergence</AUTHOR_KEYWORD>:1||tropical Indian Ocean:1||tropical Pacific SST:1||tropical SST:1||tropical cloud:1||tropical night:1||tropicalextratropical teleconnections:1||tropicsmid latitude teleconnection:1||tropospheric ozone:1||turbulence:1||two types of El Nino:1||twotypes of El Niño:1||uncertainty:1||upper ocean:1||upward trend:1||volcanic eruption:1||volcanic eruptions:1||walker circulation:1||warmer climate:1||warming hole:1||wave power:1||western North Pacific:1||western Pacific cooling:1||western north America:1||winter sea surface temperature:1||zonal wave:1||zonal wind stress:1||기후모델:1||대류권 오존:1||엘니뇨:1||1. tools and methods: dynamic/processes:1||전구대기화학모델:1||1998/1999 regime:1||2. scale: global:1||20152016 El Nino:1||20THCENTURY:1||6. application/context: climate:1||A warming trend:1||ACCIDENT:1||AEROSOLS:1||AIRSEA INTERACTION:1||ALEUTIAN LOW:1||AMIP climate models:1||AMO:1||AMOC overshoot:1||AMPLITUDE:1||AMPLITUDE CHANGES:1||ARABIAN SEA:1||ARGO:1||ASIAN SUMMER MONSOON:1||ASSOCIATION:1||ATMOSPHERE MODEL:1||ATMOSPHERE OCEAN INTERACTION:1||ATMOSPHEREOCEAN INTERACTION:1||ATMOSPHERIC CIRCULATION:1||ATMOSPHERIC RESPONSE:1||Aerosol radiative forcing:1||Aerosols:1||Agricultural:1||Air masses:1||Airsea CO2 exchange:1||Aleutian low:1||Amplitude modulation:1||Antarctic sea ice:1||Anthropogenic effects:1||Anthropogenic forcing:1||Aquaplanet experiments:1||Arctic oscillation:1||Arctic sea ice loss:1||Asian dust:1||Asymmetric rainfall:1||Atlantic SST:1||Atlantic warm pool:1||Atmosphere:1||Atmospheric emissions:1||Atmospheric forcing:1||Atmospheric stagnant:1||Atmospheric teleconnection:1||BACKGROUND MEAN STATE:1||BALANCE:1||BOUNDARIES:1||Basin shift:1||Bering and Chukchi Seas:1||Biogeochemical modeling:1||Bjerknes feedback:1||Borneo:1||CANADA:1||CENTRAL EQUATORIAL PACIFIC:1||CHINA:1||CLIMATE MODEL:1||CMIP3:1||CMIP5 climate model</AUTHOR_KEYWORD>:1||CMIP6 models:1||CO2 removal scenario:1||COLDTONGUE:1||COMBINATIONMODE:1||CONVECTION:1||CP and EP El Nino:1||CYCLOSTATIONARY EOFS:1||California:1||California rainfall:1||Central Pacific El Niño:1||Central Pacific El NinoSouthern oscillation:1||Changma:1||Changma front:1||Chemical transport model:1||Chemistrytransport model:1||Circulation:1||Climate change over the tropics:1||Climate indices:1||Climate model:1||Climate risk assessment:1||Climatological precipitation:1||Common Era:1||Compound droughtheatwave events:1||Coupled models:1||Cs134:1||DA126:1||DATASET:1||DEPTH VARIABILITY:1||DIFFERENT IMPACTS:1||DISPERSION:1||DOWNSTREAM:1||Decadal variability:1||Decadal variation:1||Dynamic factors:1||Dynamics:1||EARTH:1||EASTERN EDGE:1||ENSO (El Niño/Southern Oscillation):1||ENSO AMPLITUDE:1||ENSO MODE:1||ENSO TELECONNECTIONS:1||ENSO amplitude:1||ENSO asymmetry:1||ENSO evolution:1||ENSO feedbacks:1||ENSO flavor:1||ENSO modulation:1||ENSO teleconnections:1||ENSO variability:1||ENSOPDO:1||ENSO/MJO interaction:1||EOF ANALYSIS:1||EOF analysis:1||EQUATORIAL WAVES:1||ERA:1||

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