Nicolas Bellouin

ORCID: 0000-0003-2109-9559
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About
Contact & Profiles
Research Areas
  • Atmospheric chemistry and aerosols
  • Atmospheric aerosols and clouds
  • Atmospheric Ozone and Climate
  • Atmospheric and Environmental Gas Dynamics
  • Climate variability and models
  • Air Quality and Health Impacts
  • Advanced Aircraft Design and Technologies
  • Meteorological Phenomena and Simulations
  • Climate Change Policy and Economics
  • Vehicle emissions and performance
  • Aeolian processes and effects
  • Air Traffic Management and Optimization
  • Radiative Heat Transfer Studies
  • Climate Change and Geoengineering
  • Cryospheric studies and observations
  • Geophysics and Gravity Measurements
  • Air Quality Monitoring and Forecasting
  • Particle Dynamics in Fluid Flows
  • Geological and Geophysical Studies
  • Plant responses to elevated CO2
  • Ionosphere and magnetosphere dynamics
  • Plant Water Relations and Carbon Dynamics
  • Gas Dynamics and Kinetic Theory
  • Aviation Industry Analysis and Trends
  • Icing and De-icing Technologies

University of Reading
2016-2025

Institut Pierre-Simon Laplace
2022-2025

Sorbonne Université
2022-2025

Centre National de la Recherche Scientifique
2003-2025

National Institute of Meteorology
2019-2024

Laboratoire de Météorologie Dynamique
2022

University of Cambridge
2021

University of Maryland, Baltimore County
2020

Met Office
2006-2015

Laboratoire d'Optique Atmosphérique
2003-2005

Abstract Black carbon aerosol plays a unique and important role in Earth's climate system. is type of carbonaceous material with combination physical properties. This assessment provides an evaluation black‐carbon forcing that comprehensive its inclusion all known relevant processes quantitative providing best estimates uncertainties the main terms: direct solar absorption; influence on liquid, mixed phase, ice clouds; deposition snow ice. These effects are calculated models, but when...

10.1002/jgrd.50171 article EN cc-by-nc-nd Journal of Geophysical Research Atmospheres 2013-04-22

Abstract. We describe here the development and evaluation of an Earth system model suitable for centennial-scale climate prediction. The principal new components added to physical are terrestrial ocean ecosystems gas-phase tropospheric chemistry, along with their coupled interactions. individual described briefly relevant interactions between explained. Because multiple could lead unstable feedbacks, we go through a careful process spin up ensure that all stable balanced. This spun-up...

10.5194/gmd-4-1051-2011 article EN cc-by Geoscientific model development 2011-11-29

Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, terrestrial biosphere in a changing climate is critical to better understand global cycle, support development policies, project future change. Here we describe synthesize datasets methodology quantify five major components budget uncertainties. Fossil CO2 (EFOS) are based on energy statistics cement production data, while from land-use change (ELUC), mainly...

10.5194/essd-14-1917-2022 article EN cc-by Earth system science data 2022-04-26
Pierre Friedlingstein Michael O’Sullivan Matthew W. Jones Robbie M. Andrew Luke Gregor and 95 more Judith Hauck Corinne Le Quéré Ingrid T. Luijkx Are Olsen Glen P. Peters Wouter Peters Julia Pongratz Clemens Schwingshackl Stephen Sitch Josep G. Canadell Philippe Ciais Robert B. Jackson Simone R. Alin Ramdane Alkama Almut Arneth Vivek Arora Nicholas R. Bates Meike Becker Nicolas Bellouin Henry C. Bittig Laurent Bopp Frédéric Chevallier Louise Chini Margot Cronin Wiley Evans Stefanie Falk Richard A. Feely Thomas Gasser Marion Gehlen Thanos Gkritzalis Lucas Gloege Giacomo Grassi Nicolas Gruber Özgür Gürses Ian Harris Matthew Hefner R. A. Houghton G. C. Hurtt Yosuke Iida Tatiana Ilyina Atul K. Jain Annika Jersild Koji Kadono Etsushi Kato Daniel Kennedy Kees Klein Goldewijk Jürgen Knauer Jan Ivar Korsbakken Peter Landschützer Nathalie Lefèvre Keith Lindsay Junjie Liu Zhu Liu Gregg Marland Nicolas Mayot Matthew J. McGrath Nicolas Metzl Natalie Monacci David R. Munro Shin‐Ichiro Nakaoka Yosuke Niwa Kevin O’Brien Tsuneo Ono Paul I. Palmer Naiqing Pan Denis Pierrot Katie Pocock Benjamin Poulter Laure Resplandy Eddy Robertson Christian Rödenbeck Carmen Dolores Arbelo Rodríguez Thais M. Rosan Jörg Schwinger Roland Séférian Jamie D. Shutler Ingunn Skjelvan Tobias Steinhoff Qing Sun Adrienne J. Sutton Colm Sweeney Shintaro Takao Toste Tanhua Pieter P. Tans Xiangjun Tian Hanqin Tian Bronte Tilbrook Hiroyuki Tsujino Francesco N. Tubiello Guido R. van der Werf Anthony P. Walker Rik Wanninkhof Chris Whitehead Anna Willstrand Wranne Rebecca Wright

Abstract. Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, terrestrial biosphere in a changing climate is critical to better understand global cycle, support development policies, project future change. Here we describe synthesize data sets methodologies quantify five major components budget uncertainties. Fossil CO2 (EFOS) are based on energy statistics cement production data, while from land-use change (ELUC), mainly...

10.5194/essd-14-4811-2022 article EN cc-by Earth system science data 2022-11-11

Abstract The WFDEI meteorological forcing data set has been generated using the same methodology as widely used WATCH Forcing Data (WFD) by making use of ERA‐Interim reanalysis data. We discuss specifics how changes in and processing have led to improvement over WFD. attribute improvements precipitation wind speed latest basis improved downward shortwave fluxes aerosol corrections. Covering 1979–2012, will allow more thorough comparisons hydrological Earth System model outputs with...

10.1002/2014wr015638 article EN Water Resources Research 2014-08-19

Abstract. We report on the AeroCom Phase II direct aerosol effect (DAE) experiment where 16 detailed global models have been used to simulate changes in distribution over industrial era. All estimated radiative forcing (RF) of anthropogenic DAE, and taken into account sulphate, black carbon (BC) organic aerosols (OA) from fossil fuel, biofuel, biomass burning emissions. In addition several simulated DAE nitrate influenced secondary (SOA). The model all-sky RF total has a range −0.58 −0.02...

10.5194/acp-13-1853-2013 article EN cc-by Atmospheric chemistry and physics 2013-02-19

Abstract. We describe the HadGEM2 family of climate configurations Met Office Unified Model, MetUM. The concept a model "family" comprises range specific incorporating different levels complexity but with common physical framework. includes atmosphere and ocean components, without vertical extension to include well-resolved stratosphere, an Earth-System (ES) component which dynamic vegetation, biology atmospheric chemistry. improvements designed address systematic errors encountered in...

10.5194/gmd-4-723-2011 article EN cc-by Geoscientific model development 2011-09-07

Abstract The Water and Global Change (WATCH) project evaluation of the terrestrial water cycle involves using land surface models general hydrological to assess hydrologically important variables including evaporation, soil moisture, runoff. Such require meteorological forcing data, this paper describes creation WATCH Forcing Data for 1958–2001 based on 40-yr ECMWF Re-Analysis (ERA-40) 1901–57 reordered reanalysis data. It also discusses analyses model-independent estimates reference crop...

10.1175/2011jhm1369.1 article EN Journal of Hydrometeorology 2011-03-18

Abstract. The scientific understanding of the Earth's climate system, including central question how system is likely to respond human-induced perturbations, comprehensively captured in GCMs and Earth System Models (ESM). Diagnosing simulated response, comparing responses across different models, crucially dependent on transparent assumptions GCM/ESM has been driven – especially because implementation can involve subjective decisions may differ between modelling groups performing same...

10.5194/gmd-4-543-2011 article EN cc-by Geoscientific model development 2011-07-01
Pierre Friedlingstein Michael O’Sullivan Matthew W. Jones Robbie M. Andrew Dorothée C. E. Bakker and 95 more Judith Hauck Peter Landschützer Corinne Le Quéré Ingrid T. Luijkx Glen P. Peters Wouter Peters Julia Pongratz Clemens Schwingshackl Stephen Sitch Josep G. Canadell Philippe Ciais Robert B. Jackson Simone R. Alin Peter Anthoni Leticia Barbero Nicholas R. Bates Meike Becker Nicolas Bellouin Bertrand Decharme Laurent Bopp Ida Bagus Mandhara Brasika Patricia Cadule Matthew A. Chamberlain Naveen Chandra Thi Tuyet Trang Chau Frédéric Chevallier Louise Chini Margot Cronin Xinyu Dou Kazutaka Enyo Wiley Evans Stefanie Falk Richard A. Feely Liang Feng Daniel J. Ford Thomas Gasser Joséfine Ghattas Thanos Gkritzalis Giacomo Grassi Luke Gregor Nicolas Gruber Özgür Gürses Ian Harris Matthew Hefner Jens Heinke R. A. Houghton G. C. Hurtt Yosuke Iida Tatiana Ilyina A. R. Jacobson Atul K. Jain Tereza Jarníková Annika Jersild Fei Jiang Zhe Jin Fortunat Joos Etsushi Kato Ralph F. Keeling Daniel Kennedy Kees Klein Goldewijk Jürgen Knauer Jan Ivar Korsbakken Arne Körtzinger Xin Lan Nathalie Lefèvre Hongmei Li Junjie Liu Zhiqiang Liu Lei Ma G. Marland Nicolas Mayot Patrick McGuire Galen A. McKinley Gesa Meyer Eric J. Morgan David R. Munro Shin‐Ichiro Nakaoka Yosuke Niwa Kevin O’Brien Are Olsen Abdirahman M Omar Tsuneo Ono Melf Paulsen Denis Pierrot Katie Pocock Benjamin Poulter Carter M. Powis Gregor Rehder Laure Resplandy Eddy Robertson Christian Rödenbeck Thais M. Rosan Jörg Schwinger Roland Séférian T. Luke Smallman

Abstract. Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, terrestrial biosphere in a changing climate is critical to better understand global cycle, support development policies, project future change. Here we describe synthesize data sets methodology quantify five major components budget uncertainties. Fossil CO2 (EFOS) are based on energy statistics cement production data, while from land-use change (ELUC), mainly...

10.5194/essd-15-5301-2023 article EN cc-by Earth system science data 2023-11-30

[1] The latest Hadley Centre climate model, HadGEM2-ES, includes Earth system components such as interactive chemistry and eight species of tropospheric aerosols. It has been run for the period 1860–2100 in support fifth phase Climate Model Intercomparison Project (CMIP5). Anthropogenic aerosol emissions peak between 1980 2020, resulting a present-day all-sky top atmosphere forcing −1.6 −1.4 W m−2 with without ammonium nitrate aerosols, respectively, sum direct first indirect forcings....

10.1029/2011jd016074 article EN Journal of Geophysical Research Atmospheres 2011-08-16

<strong class="journal-contentHeaderColor">Abstract.</strong> This paper evaluates the current status of global modeling organic aerosol (OA) in troposphere and analyzes differences between models as well observations. Thirty-one chemistry transport (CTMs) general circulation (GCMs) have participated this intercomparison, framework AeroCom phase II. The simulation OA varies greatly terms magnitude primary emissions, secondary (SOA) formation, number species used (2 to 62), complexity...

10.5194/acp-14-10845-2014 article EN cc-by Atmospheric chemistry and physics 2014-10-15

Abstract. Aerosol indirect effects continue to constitute one of the most important uncertainties for anthropogenic climate perturbations. Within international AEROCOM initiative, representation aerosol-cloud-radiation interactions in ten different general circulation models (GCMs) is evaluated using three satellite datasets. The focus on stratiform liquid water clouds since GCMs do not include ice nucleation effects, and none model explicitly parameterises aerosol convective clouds. We...

10.5194/acp-9-8697-2009 article EN cc-by Atmospheric chemistry and physics 2009-11-16

Abstract. This paper presents a summary of the work done within European Union's Seventh Framework Programme project ECLIPSE (Evaluating Climate and Air Quality Impacts Short-Lived Pollutants). had unique systematic concept for designing realistic effective mitigation scenario short-lived climate pollutants (SLCPs; methane, aerosols ozone, their precursor species) quantifying its air quality impacts, this results in context overarching strategy. The first step was to create new emission...

10.5194/acp-15-10529-2015 article EN cc-by Atmospheric chemistry and physics 2015-09-24

The main uncertainty in anthropogenic forcing of the Earth's climate stems from pollution aerosols, particularly their “indirect effect” whereby aerosols modify cloud properties. We develop a new methodology to derive measurement‐based estimate using almost exclusively information an Earth radiation budget instrument (CERES) and radiometer (MODIS). statistical relationship between planetary albedo properties, and, further, properties column aerosol concentration. Combining these...

10.1029/2007jd008962 article EN Journal of Geophysical Research Atmospheres 2008-03-11

Abstract. The WFDE5 dataset has been generated using the WATCH Forcing Data (WFD) methodology applied to surface meteorological variables from ERA5 reanalysis. WFDEI had previously by applying WFD ERA-Interim. is provided at 0.5∘ spatial resolution but higher temporal (hourly) compared (3-hourly). It also variability since it was aggregation of higher-resolution rather than interpolation lower-resolution ERA-Interim data. Evaluation against observations 13 globally distributed FLUXNET2015...

10.5194/essd-12-2097-2020 article EN cc-by Earth system science data 2020-09-08

Radiative forcing is a useful tool for predicting equilibrium global temperature change. However, it not so precipitation changes, as changes in strongly depend on the climate change mechanism and how perturbs atmospheric surface energy budgets. Here suite of model experiments radiative transfer calculations are used to quantify assess this dependency across range mechanisms. It shown that response can be split into two parts: fast correlates with component forcing, slower independent...

10.1029/2010gl043991 article EN Geophysical Research Letters 2010-07-01

Abstract. The impact of black carbon (BC) aerosols on the global radiation balance is not well constrained. Here twelve aerosol models are used to show that at least 20% present uncertainty in modeled BC direct radiative forcing (RF) due diversity simulated vertical profile mass. Results from phases 1 and 2 model intercomparison project (AeroCom). Additionally, a significant fraction variability shown come high altitudes, as, globally, more than 40% total RF exerted above 5 km. emission...

10.5194/acp-13-2423-2013 article EN cc-by Atmospheric chemistry and physics 2013-03-01
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