about
Simulation of Sahel drought in the 20th and 21st centuriesClimate science: Origins of Atlantic decadal swings.Potential for western US seasonal snowpack prediction.Comment on "Multiyear prediction of monthly mean Atlantic Meridional Overturning Circulation at 26.5°N".Robustness of anthropogenically forced decadal precipitation changes projected for the 21st century.THE WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change ResearchDominant Role of Subtropical Pacific Warming in Extreme Eastern Pacific Hurricane Seasons: 2015 and the FutureEstimating Decadal Predictability for the Southern Ocean Using the GFDL CM2.1 ModelCorrigendumSeasonal Prediction Skill of Northern Extratropical Surface Temperature Driven by the StratosphereThe Central Role of Ocean Dynamics in Connecting the North Atlantic Oscillation to the Extratropical Component of the Atlantic Multidecadal OscillationWeakening of the North American monsoon with global warmingDetection, Attribution, and Projection of Regional Rainfall Changes on (Multi-) Decadal Time Scales: A Focus on Southeastern South AmericaEnhanced warming of the Northwest Atlantic Ocean under climate changeImproved Simulation of Tropical Cyclone Responses to ENSO in the Western North Pacific in the High-Resolution GFDL HiFLOR Coupled Climate ModelSeasonal Forecasts of Major Hurricanes and Landfalling Tropical Cyclones using a High-Resolution GFDL Coupled Climate ModelSimulated Connections between ENSO and Tropical Cyclones near Guam in a High-Resolution GFDL Coupled Climate Model: Implications for Seasonal ForecastingThe Impact of Horizontal Resolution on North American Monsoon Gulf of California Moisture Surges in a Suite of Coupled Global Climate ModelsThe North Atlantic Oscillation as a driver of rapid climate change in the Northern HemisphereThe Resolution Dependence of Contiguous U.S. Precipitation Extremes in Response to CO2 ForcingThe Roles of Radiative Forcing, Sea Surface Temperatures, and Atmospheric and Land Initial Conditions in U.S. Summer Warming EpisodesA Link between the Hiatus in Global Warming and North American DroughtInvestigating the Influence of Anthropogenic Forcing and Natural Variability on the 2014 Hawaiian Hurricane SeasonImproved Seasonal Prediction of Temperature and Precipitation over Land in a High-Resolution GFDL Climate ModelSeasonal Predictability of Extratropical Storm Tracks in GFDL’s High-Resolution Climate Prediction ModelSimulation and Prediction of Category 4 and 5 Hurricanes in the High-Resolution GFDL HiFLOR Coupled Climate Model*The Seasonality of the Great Plains Low-Level Jet and ENSO RelationshipTowards predictive understanding of regional climate changeENSO Modulation: Is It Decadally Predictable?On the Seasonal Forecasting of Regional Tropical Cyclone ActivityReply to Comments on “Multiyear Predictions of North Atlantic Hurricane Frequency: Promise and Limitations”Tropical Cyclone Simulation and Response to CO2Doubling in the GFDL CM2.5 High-Resolution Coupled Climate ModelA Predictable AMO-Like Pattern in the GFDL Fully Coupled Ensemble Initialization and Decadal Forecasting SystemHave Aerosols Caused the Observed Atlantic Multidecadal Variability?Multiyear Predictions of North Atlantic Hurricane Frequency: Promise and LimitationsResponse to CO2Doubling of the Atlantic Hurricane Main Development Region in a High-Resolution Climate ModelBiases in the Atlantic ITCZ in Seasonal–Interannual Variations for a Coarse- and a High-Resolution Coupled Climate ModelSimulated Climate and Climate Change in the GFDL CM2.5 High-Resolution Coupled Climate ModelOn the use of IPCC-class models to assess the impact of climate on Living Marine ResourcesGFDL's CM2 Global Coupled Climate Models. Part II: The Baseline Ocean Simulation
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P50
description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Thomas Delworth
@ast
Thomas Delworth
@en
Thomas Delworth
@es
Thomas Delworth
@nl
type
label
Thomas Delworth
@ast
Thomas Delworth
@en
Thomas Delworth
@es
Thomas Delworth
@nl
prefLabel
Thomas Delworth
@ast
Thomas Delworth
@en
Thomas Delworth
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Thomas Delworth
@nl
P106
P31
P496
0000-0003-4865-5391