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Ruth M. Doherty

Researcher at University of Edinburgh

Publications -  144
Citations -  13172

Ruth M. Doherty is an academic researcher from University of Edinburgh. The author has contributed to research in topics: Climate change & Tropospheric ozone. The author has an hindex of 49, co-authored 134 publications receiving 11618 citations. Previous affiliations of Ruth M. Doherty include National Center for Atmospheric Research & University of East Anglia.

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African climate change: 1900-2100

TL;DR: In this article, the authors present a range of climate change scenarios for Africa, focusing on changes in both continental and regional seasonal-mean temperature and rainfall, and estimate the associated changes in global CO2 concentration and global mean sea-level change.
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Multimodel ensemble simulations of present-day and near-future tropospheric ozone

TL;DR: In this article, an ensemble of 26 state-of-the-art atmospheric chemistry models have been compared and synthesized as part of a wider study into both the air quality and climate roles of ozone.
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Nitrogen and sulfur deposition on regional and global scales:a multimodel evaluation

TL;DR: This paper used 23 atmospheric chemistry transport models to calculate current and future (2030) deposition of reactive nitrogen (NOy, NHx) and sulfate (SOx) to land and ocean surfaces.
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Pre-industrial to end 21st century projections of tropospheric ozone from the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP)

TL;DR: In this article, present day tropospheric ozone and its changes between 1850 and 2100 are considered, analysing 15 global models that participated in the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP).
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Linear solvation energy relationship. 46. An improved equation for correlation and prediction of octanol/water partition coefficients of organic nonelectrolytes (including strong hydrogen bond donor solutes)

TL;DR: Les coefficients de partage octanol/eau de 245 composes aliphatiques et aromatiques sont bien correles par la relation d'energie de solvatation lineaire: logK ow = 0,35+5,35V I /100-1,04(π*−0,35δ)-3,84 β m +0,10α m (r=0,9959, SD= 0,131) ou V I est le volume molaire intrinseque, π*, β