{"id":619,"date":"2026-08-16T12:29:12","date_gmt":"2026-08-16T04:29:12","guid":{"rendered":"https:\/\/hydro.as.ntu.edu.tw\/chia\/?page_id=619"},"modified":"2026-08-20T09:24:36","modified_gmt":"2026-08-20T01:24:36","slug":"2026-poster","status":"publish","type":"page","link":"https:\/\/hydro.as.ntu.edu.tw\/chia\/chia-forum-2026\/2026-poster\/","title":{"rendered":"CHiA Forum 2026 Poster"},"content":{"rendered":"\t\t
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Day 2-3<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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8\/26\u300127 Posters
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Poster Section I<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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Day 2, 8\/26(\u4e09) 13:00-15:00<\/div>\n\n\t\t\t\t\t\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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\u7de8\u865f<\/strong><\/td>\n\u59d3\u540d<\/strong><\/td>\n\u984c\u76ee<\/strong><\/td>\n<\/tr>\n\n
A01-D2<\/td>\n\u674e\u6df3\u5f18<\/td>\nClimate Change Impacts on Typhoon Damage to Wind Turbines in Taiwan: A CLIMADA Assessment Using Multi-Model STORM Synthetic Tracks<\/td>\n<\/tr>\n\n
A03-D2<\/td>\n\u674e\u6e05\u7e22<\/td>\n\u61c9\u7528\u65bc\u81fa\u7063\u5730\u5340\u7684\u9ad8\u89e3\u6790\u5ea6\u964d\u5c3a\u5ea6\u6a21\u64ec\u5668\u958b\u767c<\/td>\n<\/tr>\n\n
A05-D2<\/td>\n\u90ed\u53e1<\/td>\nA Divergence-Based Framework for Predictability in Chaotic and Climate Systems<\/td>\n<\/tr>\n\n
A07-D2<\/td>\n\u8cf4\u67cf\u52f3<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A09-D2<\/td>\n\u90ed\u51a0\u5ef7<\/td>\nTwo-Step Monsoon Onset in Aquaplanet Simulations: The Roles of SST Geometry and Shallow Convection<\/td>\n<\/tr>\n\n
A11-D2<\/td>\n\u7f85\u96c5\u862d<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A13-D2<\/td>\n\u8607\u4fca\u5f65<\/td>\nModulation of Deep Convective Systems in Kilometer-scale Simulations Using a Unified Representation of Deep Moist Convection<\/td>\n<\/tr>\n\n
A15-D2<\/td>\n\u66fe\u5efa\u7ff0<\/td>\nA Propagation\u2013Generation\u2013Evolution Framework for Seasonal Atmospheric Circulation Prediction<\/td>\n<\/tr>\n\n
A17-D2<\/td>\n\u66fe\u5f18\u6bc5<\/td>\nExtratropical Controls on Recent Tropical Pacific SST and Zonal Gradient Biases<\/td>\n<\/tr>\n\n
A19-D2<\/td>\n\u5f90\u4e16\u88f4<\/td>\nThe Role of Eddy Available Potential Energy in the Response of Convectively-Coupled Kelvin Wave in a Warmer Climate<\/td>\n<\/tr>\n\n
A21-D2<\/td>\n\u8a31\u6b23\u6021<\/td>\nEquatorial Zonal SST Gradient Response to Extratropical Forcing: Isolating the Roles of Ocean Heat Flux and South American Topography<\/td>\n<\/tr>\n\n
A23-D2<\/td>\n\u4f0d\u73ee\u6148<\/td>\nDeciphering the Walker Circulation: the role of ocean heat uptake, land and topography in zonally asymmetric circulation<\/td>\n<\/tr>\n\n
A25-D2<\/td>\n\u6e38\u6770\u5ead<\/td>\nImpact of Climate Change and Global Warming on the Microclimate Characteristics of the Alishan Tea Plantation<\/td>\n<\/tr>\n\n
A27-D2<\/td>\n\u65bd\u749f\u5b8f<\/td>\nA Diagnostic Framework for Atmospheric Moistening and Surface Evaporation Controls on Diurnal Hysteresis between Temperature and Relative Humidity<\/td>\n<\/tr>\n\n
A29-D2<\/td>\n\u65bd\u6625\u7034<\/td>\n\u4e2d\u570b\u5169\u5343\u5e74\u6c23\u5019\u8b8a\u5316\u8207\u71b1\u4e8b\u4ef6\u5206\u6790<\/td>\n<\/tr>\n\n
A31-D2<\/td>\n\u5f35\u74ca\u6587<\/td>\nEnhanced Influences from North Pacific Oscillation and Pacific Meridional Mode on Southern China Spring Rainfall since 2000<\/td>\n<\/tr>\n\n
A33-D2<\/td>\n\u84b2\u91d1\u6a19<\/td>\n\u5eb7\u745e\u98b1\u98a8\u4fb5\u8972\u671f\u9593\u677e\u5c71\u6a5f\u5834\u4f4e\u7a7a\u98a8\u5207\u8207\u6c23\u58d3\u5927\u6ce2\u52d5\u4e4b\u500b\u6848\u5206\u6790\u7814\u7a76 \u2212 \u897f\u51432024\u5e7410\u670831\u65e5<\/td>\n<\/tr>\n\n
A35-D2<\/td>\n\u8d99\u54c1\u8aed<\/td>\nTBD<\/td>\n<\/tr>\n\n
A37-D2<\/td>\n\u5468\u81f3\u4e2d<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A39-D2<\/td>\n\u694a\u60e0\u5fc3<\/td>\n\u6771\u4e9e\u5927\u6c23\u6cb3\u4e8b\u4ef6\u5075\u6e2c\u654f\u611f\u5ea6\u6e2c\u8a66\u8207\u964d\u6c34\u8ca2\u737b\u7387<\/td>\n<\/tr>\n\n
A41-D2<\/td>\n\u9673\u8a60\u83d6<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B01-D2<\/td>\n\u6797\u6600\u975c<\/td>\n\u81fa\u7063\u9ad8\u89e3\u6790\u5ea6\u96e8\u91cf\u964d\u5c3a\u5ea6\u9810\u5831\u80fd\u529b\u8a55\u4f30<\/td>\n<\/tr>\n\n
B03-D2<\/td>\n\u9673\u6977\u85aa<\/td>\nHow does controlling the simplified entrainment convection scheme affect model output across models of different complexity?<\/td>\n<\/tr>\n\n
B05-D2<\/td>\n\u6d2a\u6668\u54f2<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B07-D2<\/td>\n\u9673\u9038\u660c<\/td>\nProgressive Diffusion Models for Atmospheric Downscaling: A Framework for Orographic Wind and Precipitation Synthesis<\/td>\n<\/tr>\n\n
B09-D2<\/td>\n\u984f\u5b50\u5091<\/td>\nSensitivity of Thermal Stratification to Convective Entrainment: Does the Impact on GMS Hold Across a Model Hierarchy?<\/td>\n<\/tr>\n\n
B11-D2<\/td>\nNGAI SHEAU TIEH \u9b4f\u66c9\u8776<\/td>\nProjected Changes in Diurnal Rainfall over the Maritime Continent from High-Resolution CORDEX-SEA Simulations<\/td>\n<\/tr>\n\n
B13-D2<\/td>\n\u8a79\u5091\u52db<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B15-D2<\/td>\n\u6797\u5ba5\u5ef7<\/td>\nAnalyzing Ocean\u2013Atmosphere Coupling Dynamics in Triple-Dip La Ni\u00f1a Events of the 20th and 21st Centuries<\/td>\n<\/tr>\n\n
B17-D2<\/td>\n\u6d2a\u5fd7\u8aa0<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B19-D2<\/td>\n\u8a31\u66f8\u5c09<\/td>\nReconstructing the East Asian Jet Stream During the Ming\u2013Qing Period (1368\u20131911) Using the REACHES Database<\/td>\n<\/tr>\n\n
B21-D2<\/td>\n\u738b\u7dbf<\/td>\nResponses of North Atlantic Rossby wave breaking to Arctic sea-ice loss in Traditional Physical and AI-Hybrid models<\/td>\n<\/tr>\n\n
B23-D2<\/td>\n\u8cf4\u6817\u8466<\/td>\nDo Different Regions of Taiwan Need Different Heat Warning Thresholds? Evidence from apparent temperature, heatwave exposure, and minimum-risk temperature<\/td>\n<\/tr>\n\n
B25-D2<\/td>\n\u674e\u6b63\u5b89<\/td>\n\u5442\u5b8b\u5cf6\u6625\u5b63\u65e5\u964d\u6c34\uff1a\u5e74\u969b\u8b8a\u5316\u53ca\u5176\u6f5b\u5728\u6a5f\u5236<\/td>\n<\/tr>\n\n
B27-D2<\/td>\n\u8607\u5fc3\u543e<\/td>\nInvestigating Tropical Energy Transport and Circulation Changes Driven by Zonal SST Asymmetry under Global Warming<\/td>\n<\/tr>\n\n
B29-D2<\/td>\n\u8303\u7950\u8ed2<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B31-D2<\/td>\n\u674e\u7e7c\u5e38<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B33-D2<\/td>\n\u8521\u9d3b\u9d6c<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B35-D2<\/td>\n\u738b\u6bd3\u7407<\/td>\nHow Terrain Geometry Modulates the Multiple-Peak Diurnal Convection over a Tropical Mountainous Island Using Idealized Large-Eddy Simulations?<\/td>\n<\/tr>\n\n
B37-D2<\/td>\n\u9673\u51a0\u6770<\/td>\nSpatiotemporal Characteristics and Long-Term Changes of Extreme Rainfall Events in Taiwan<\/td>\n<\/tr>\n\n
B39-D2<\/td>\n\u5c24\u5b3f\u81fb<\/td>\nWeather Pattern Classification and Analysis of Recent Changes in Atmospheric Circulation<\/td>\n<\/tr>\n\n
B41-D2<\/td>\n\u5f35\u5bb9\u6148<\/td>\nRecent Pre-Monsoon Warming and Hydroclimatic Changes over Southeast Asia: Land\u2013Atmosphere Feedbacks and Possible Circulation Links<\/td>\n<\/tr>\n\n<\/tbody>\n<\/table>\n<\/div><\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n\n\n\n\t\t\t\t\n\t\t\t\t\t\t\t\t\t\tNext day\t\t\t\t<\/a>\n\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t<\/div>\n\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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Poster Section II<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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Day 3, 8\/27(\u56db) 13:00-15:00<\/div>\n\n\t\t\t\t\t\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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\u7de8\u865f<\/strong><\/td>\n\u59d3\u540d<\/strong><\/td>\n\u984c\u76ee<\/strong><\/td>\n<\/tr>\n\n
A02-D3<\/td>\n\u674e\u6fa4\u9091<\/td>\nAI\u964d\u5c3a\u5ea6\u65bc\u77ed\u671f\u6c23\u5019\u9810\u5831\u7684\u53ef\u884c\u6027\u5206\u6790<\/td>\n<\/tr>\n\n
A04-D3<\/td>\n\u9673\u9d6c\u4efb<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A06-D3<\/td>\n\u9673\u52c7\u5fd7<\/td>\nA Land-to-Ocean Shift in Energy Sources Governs Walker Circulation Evolution under Abrupt CO2 Forcing<\/td>\n<\/tr>\n\n
A08-D3<\/td>\n\u5289\u66c9\u8587<\/td>\nTaiESM\u52d5\u529b\u964d\u5c3a\u5ea6\u5c0d\u53f0\u7063\u6975\u7aef\u964d\u96e8\u4e4b\u6a21\u64ec\u8a55\u4f30<\/td>\n<\/tr>\n\n
A10-D3<\/td>\n\u66fe\u5c11\u79b9<\/td>\n <\/td>\n<\/tr>\n\n
A12-D3<\/td>\n\u6b50\u5fb7\u6631<\/td>\nCharacterizing the Impacts of Sub-daily Cloud-Fog on Vegetation Photosynthesis and Transpiration in a Montane Cloud Forest Site<\/td>\n<\/tr>\n\n
A14-D3<\/td>\n\u8b1d\u65fb\u8015<\/td>\nSynoptic Trajectories in a Latent Phase Diagram: Future Changes in Taiwan\u2019s Terrain-Driven Circulation and Pollution Risk<\/td>\n<\/tr>\n\n
A16-D3<\/td>\n\u7f85\u654f\u8f1d<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A18-D3<\/td>\n\u7518\u7950\u9293<\/td>\nRadiative Modulation of Convectively Coupled Kelvin Waves<\/td>\n<\/tr>\n\n
A20-D3<\/td>\n\u856d\u53cb\u54f2<\/td>\nGlobal river warming remains undetectable with the current observing network<\/td>\n<\/tr>\n\n
A22-D3<\/td>\n\u6b50\u9756\u5e73<\/td>\n\u6771\u4e9e\u5927\u6c23\u6cb3\u7279\u5fb5\u53ca\u672a\u4f86\u63a8\u4f30<\/td>\n<\/tr>\n\n
A24-D3<\/td>\n\u5433\u67cf\u6176<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A26-D3<\/td>\n\u5468\u5f65\u5ef7<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
A28-D3<\/td>\n\u8449\u5955\u5ef7<\/td>\nDrivers of North Pacific Cloud Trends (2001-2020): East Asian Aerosols vs. Internal Variability<\/td>\n<\/tr>\n\n
A30-D3<\/td>\nPriya Bharati<\/td>\nArctic sea-ice reduction modulating cross-equatorial upper-level westerly flow and associated tropopause foldings.<\/td>\n<\/tr>\n\n
A32-D3<\/td>\nSho Arakane<\/td>\nTropical Cyclone Removed Dataset and Its Application<\/td>\n<\/tr>\n\n
A34-D3<\/td>\n\u6797\u66f8\u6b63<\/td>\nCharacteristics and Spatiotemporal Variability of Long Stationary Tropical Cyclones (LSTC) in the Western North Pacific (1970\u20132025)<\/td>\n<\/tr>\n\n
A36-D3<\/td>\n\u90ed\u9038\u82b8<\/td>\n <\/td>\n<\/tr>\n\n
A38-D3<\/td>\n\u856d\u7acb\u670b<\/td>\nFrom Historical Performance to Future Projections: Evaluating Tropical Cyclone Genesis Potential Indices in CMIP6 Models<\/td>\n<\/tr>\n\n
A40-D3<\/td>\n\u99f1\u4e16\u8c6a<\/td>\nBeyond Conventional Heatwave Indices: An Event-Based Platform for Global Heatwave Exploration and Risk Assessment<\/td>\n<\/tr>\n\n
A42-D3<\/td>\nYan-Lan Shen<\/td>\n\u3010\u5f85\u5b9a\u3011<\/td>\n<\/tr>\n\n
B02-D3<\/td>\n\u4f59\u73ee\u7487<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B04-D3<\/td>\n\u7c21\u5b5f\u512a<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B06-D3<\/td>\n\u4f55\u4f69\u84c9<\/td>\nRole of Falling Ice Radiative Effects in El Ni\u00f1o Evolution and Indo-Pacific Interactions in CESM1-CAM5<\/td>\n<\/tr>\n\n
B08-D3<\/td>\n\u5433\u5b9a\u878d<\/td>\nLinking the Abruptness of South Asian Summer Monsoon Onset to Convection Aggregation: Insights from SP-CAM under Present-day and Warming Climates<\/td>\n<\/tr>\n\n
B10-D3<\/td>\nN\/A<\/td>\nWITHDRAW<\/td>\n<\/tr>\n\n
B12-D3<\/td>\n\u9673\u6021\u6f54<\/td>\nMaritime Continent Deforestation-Induced Extreme Rainfall Regime Shifts During the Early Summer Monsoon Season<\/td>\n<\/tr>\n\n
B14-D3<\/td>\n\u6797\u5b97\u52f3<\/td>\nGlobal Energetic Constraints and Local Physical Processes in the Delayed Seasonal Cycle of the Asian Monsoon<\/td>\n<\/tr>\n\n
B16-D3<\/td>\n\u80e1\u5bb6\u9293<\/td>\nThe role of Indo-Pacific SST warming in the intensification and northward extension of African boreal summer monsoon rainfall in recent decades<\/td>\n<\/tr>\n\n
B18-D3<\/td>\n\u5ed6\u97cb\u7ff0<\/td>\nInvestigating southern Taiwan afternoon thunderstorm using TaiwanVVM: From boundary layer dynamics to deep convection initiation<\/td>\n<\/tr>\n\n
B20-D3<\/td>\n\u8449\u76c8\u79c0<\/td>\nSeasonal Cycle of Solar Insolation Drives Polar Amplification in Ice-free Climates<\/td>\n<\/tr>\n\n
B22-D3<\/td>\nTing Hui Lee<\/td>\nInfluence of Climate Mean-States on Deforestation-Induced Precipitation Variability in the Maritime Continent<\/td>\n<\/tr>\n\n
B24-D3<\/td>\nUndrakh Ganzorig<\/td>\nReduced Aerosol Loading Enhances Warm-Season Heat in Taiwan<\/td>\n<\/tr>\n\n
B26-D3<\/td>\n\u5433\u6069\u6148<\/td>\nSeasonality of Evapotranspiration Driven by Soil Moisture and Non\u2013soil-moisture Pathways<\/td>\n<\/tr>\n\n
B28-D3<\/td>\nSuranjith Bandara Koralegedara<\/td>\nFrom Rainfall to Temperature: Springtime Soil Moisture Decline and Reorganizing Environmental Controls in Subtropical East Asia<\/td>\n<\/tr>\n\n
B30-D3<\/td>\n\u6881\u4fe1\u8b19<\/td>\n\u5f85\u5b9a<\/td>\n<\/tr>\n\n
B32-D3<\/td>\n\u9ec3\u61f7\u9038<\/td>\nLocal Circulation Control of Wintertime Orographic Fog under a Stratocumulus-Topped Boundary Layer in montane cloud forests<\/td>\n<\/tr>\n\n
B34-D3<\/td>\nSaed M. Omar<\/td>\nTBD<\/td>\n<\/tr>\n\n
B36-D3<\/td>\n\u8521\u627f\u8ed2<\/td>\nSpatiotemporal Analysis of Extreme Heat Exposure Risk for the Elderly Population in Taiwan<\/td>\n<\/tr>\n\n
B38-D3<\/td>\nTzu-Ling Lai<\/td>\nPoleward-moving tropical cyclones over the western North Pacific during September-October from 1970 to 2023<\/td>\n<\/tr>\n\n
B40-D3<\/td>\n\u675c\u4f73\u7a4e<\/td>\nApplication of a Regionally Refined GCM with 3-km Resolution over Taiwan for Simulating Extreme Events<\/td>\n<\/tr>\n\n
B42-D3<\/td>\n\u5f35\u5de7\u8587<\/td>\nCapturing Weather Patterns in Northern Hemisphere Winter through the Latent Feature in an Explainable Variational Autoencoder Model<\/td>\n<\/tr>\n\n<\/tbody>\n<\/table>\n<\/div><\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
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