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Daniel T. McCoy

Researcher at University of Leeds

Publications -  31
Citations -  2471

Daniel T. McCoy is an academic researcher from University of Leeds. The author has contributed to research in topics: Cloud cover & Radiative forcing. The author has an hindex of 16, co-authored 26 publications receiving 1469 citations. Previous affiliations of Daniel T. McCoy include University of Washington & University of Wyoming.

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Causes of Higher Climate Sensitivity in CMIP6 Models

TL;DR: In this article, the authors show that the global surface temperature response to CO2 doubling has increased substantially in the Coupled Model Intercomparison Project phase 6 (CMIP6), with values spanning 1.8-5.6k across 27 GCMs and exceeding 4.5K in 10 of them.
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Bounding global aerosol radiative forcing of climate change

TL;DR: A new range of aerosol radiative forcing over the industrial era is provided based on multiple, traceable, and arguable lines of evidence, including modeling approaches, theoretical considerations, and observations, to constrain the forcing from aerosol‐radiation interactions.
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Remote Sensing of Droplet Number Concentration in Warm Clouds: A Review of the Current State of Knowledge and Perspectives

TL;DR: Issues with current standard satellite retrievals are summarized, new ideas to use additional information from existing and upcoming spaceborne instruments are discussed, and approaches using high‐quality ground‐based observations are examined.
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Natural aerosols explain seasonal and spatial patterns of Southern Ocean cloud albedo

TL;DR: It is shown that modeled natural aerosols, principally marine biogenic primary and secondary aerosol sources, explain more than half of the spatiotemporal variability in satellite-observed cloud droplet concentration.
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On the relationships among cloud cover, mixed-phase partitioning, and planetary albedo in GCMs

TL;DR: In this article, the authors investigated possible reasons for these relationships by analyzing the mixed-phase parameterizations in 26 GCMs and found that models with more supercooled liquid water would also have a higher planetary albedo.