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Kentaroh Suzuki

Researcher at University of Tokyo

Publications -  112
Citations -  4100

Kentaroh Suzuki is an academic researcher from University of Tokyo. The author has contributed to research in topics: Precipitation & Aerosol. The author has an hindex of 24, co-authored 107 publications receiving 3416 citations. Previous affiliations of Kentaroh Suzuki include National Institute of Information and Communications Technology & Colorado State University.

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Dreary state of precipitation in global models

TL;DR: In this paper, the authors used CloudSat data to assess the realism of global model precipitation and found that the observed and modeled precipitation are significantly different from the character of liquid precipitation produced by global weather and climate models.
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A study of the direct and indirect effects of aerosols using global satellite data sets of aerosol and cloud parameters

TL;DR: In this paper, the authors investigated the correlations between aerosol and cloud parameters derived from satellite remote sensing for evaluating the radiative forcing of the aerosol indirect effect and found that positive correlations between the cloud optical thickness and cloud fraction with the column number concentration exist in most regions consistent with the global mean statistics, but the effective cloud particle radius showed a tendency similar to the global correlation only around the seashore regions.
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Droplet Growth in Warm Water Clouds Observed by the A-Train. Part II: A Multisensor View

TL;DR: In this paper, a combination of Aqua/Moderate Resolution Imaging Spectroradiometer (MODIS) cloud particle size observations and CloudSat/Cloud Profiling Radar (CPR) observations of warm water clouds was used to infer the hydrometeor droplet growth process from cloud to rain via drizzle.
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Droplet Growth in Warm Water Clouds Observed by the A-Train. Part I: Sensitivity Analysis of the MODIS-Derived Cloud Droplet Sizes

TL;DR: In this paper, the authors examined the sensitivity of the retrieved cloud droplet radii to the vertical inhomogeneity of droplet radius, including the existence of a drizzle mode in clouds.