Integration of Air Quality Modelling and Monitoring Methods: Review and Applications
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On the Uses of a New Linear Scheme for Stratospheric Methane in Global Models: Water Source, Transport Tracer and Radiative Forc
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Atmos. Chem. Phys. Discuss., 12, 479–523, 2012 Atmospheric www.atmos-chem-phys-discuss.net/12/479/2012/ Chemistry doi:10.5194/acpd-12-479-2012 and Physics © Author(s) 2012. CC Attribution 3.0 License. Discussions This discussion paper is/has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP if available. On the uses of a new linear scheme for stratospheric methane in global models: water source, transport tracer and radiative forcing B. M. Monge-Sanz1, M. P. Chipperfield1, A. Untch2, J.-J. Morcrette2, A. Rap1, and A. J. Simmons2 1Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK 2European Centre for Medium-Range Weather Forecasts, Reading, UK Received: 10 October 2011 – Accepted: 5 November 2011 – Published: 6 January 2012 Correspondence to: B. M. Monge-Sanz ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 479 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract A new linear parameterisation for stratospheric methane (CoMeCAT) has been devel- oped and tested. The scheme is derived from a 3-D full chemistry transport model (CTM) and tested within the same chemistry model itself, as well as in an independent 5 general circulation model (GCM). The new CH4/H2O scheme is suitable for any global model and here is shown to provide realistic profiles in the 3-D TOMCAT/SLIMCAT CTM and in the ECMWF (European Centre for Medium-Range Weather Forecasts) GCM. -
University of Reading Boundary-Layer Type Classification and Pollutant Mixing
University of Reading Department of Meteorology Boundary-layer type classification and pollutant mixing Natalie Jane Harvey A thesis submitted for the degree of Doctor of Philosophy March 2013 Declaration I confirm that this is my own work and the use of all material from other sources has been properly and fully acknowledged. Natalie Harvey Page ii Abstract In the atmospheric boundary layer the vertical distribution of heat, momentum, water and pollutants is controlled by mixing that is turbulent. This complex mixing is param- eterized in weather forecast and climate models. But are the parameterizations imple- mented in these models representative of the real world? For the first time, Doppler lidar and sonic anemometer data are used to objectively classify the observed boundary layer into nine different types based on the Met Office scheme. Examples of these types are decoupled stratocumulus cloud, cumulus capped and stable with no turbulent cloud. This method is applied to three years of data from the Chilbolton Observatory, UK, to create a climatology of boundary-layer type. This climatology exhibits clear seasonal and diurnal cycles with the most common type over the three years being a cloud-free stable boundary layer. The decoupled stratocumulus type and the cumulus cloud under a stratocumulus layer type are diagnosed 10.3% and 1.0% of the period respectively. This new observationally based boundary layer classification is used to evaluate the boundary-layer type diagnosed by the 4 km and 12 km resolution versions of the Met Office Unified Model. The model is found to predict too many decoupled stratocumulus boundary layers by a factor of 1.8, in both the stable and unstable regime. -
Effects of Stratospheretroposphere Chemistry Coupling on Tropospheric Ozone
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115, D00M04, doi:10.1029/2009JD013515, 2010 Effects of stratosphere‐troposphere chemistry coupling on tropospheric ozone Wenshou Tian,1,2 Martyn P. Chipperfield,2 David S. Stevenson,3 Richard Damoah,3,4 Sandip Dhomse,2 Anu Dudhia,5 Hugh Pumphrey,3 and Peter Bernath6 Received 6 November 2009; revised 23 March 2010; accepted 13 April 2010; published 17 September 2010. [1] A new, computationally efficient coupled stratosphere‐troposphere chemistry‐climate model (S/T‐CCM) has been developed based on three well‐documented components: a64‐level general circulation model from the UK Met Office Unified Model, the tropospheric chemistry transport model (STOCHEM), and the UMSLIMCAT stratospheric chemistry module. This newly developed S/T‐CCM has been evaluated with various observations, and it shows good performance in simulating important chemical species and their interdependence in both the troposphere and stratosphere. The modeled total column ozone agrees well with Total Ozone Mapping Spectrometer observations. Modeled ozone profiles in the upper troposphere and lower stratosphere are significantly improved compared to runs with the stratospheric chemistry and tropospheric chemistry models alone, and they are in good agreement with Michelson Interferometer for Passive Atmospheric Sounding satellite ozone profiles. The observed CO tape recorder is also successfully captured by the new CCM, and ozone‐CO correlations are in accordance with Atmospheric Chemistry Experiment observations. However, because of limitations in vertical resolution, intrusion of CO‐rich air in the stratosphere from the mesosphere could not be simulated in the current version of S/T‐CCM. Additionally, the simulated stratosphere‐to‐troposphere ozone flux, which controls upper tropospheric OH and O3 concentrations, is found to be more realistic in the new coupled model compared to STOCHEM. -
Assimila Blank
NERC NERC Strategy for Earth System Modelling: Technical Support Audit Report Version 1.1 December 2009 Contact Details Dr Zofia Stott Assimila Ltd 1 Earley Gate The University of Reading Reading, RG6 6AT Tel: +44 (0)118 966 0554 Mobile: +44 (0)7932 565822 email: [email protected] NERC STRATEGY FOR ESM – AUDIT REPORT VERSION1.1, DECEMBER 2009 Contents 1. BACKGROUND ....................................................................................................................... 4 1.1 Introduction .............................................................................................................. 4 1.2 Context .................................................................................................................... 4 1.3 Scope of the ESM audit ............................................................................................ 4 1.4 Methodology ............................................................................................................ 5 2. Scene setting ........................................................................................................................... 7 2.1 NERC Strategy......................................................................................................... 7 2.2 Definition of Earth system modelling ........................................................................ 8 2.3 Broad categories of activities supported by NERC ................................................. 10 2.4 Structure of the report ........................................................................................... -
Review of the Global Models Used Within Phase 1 of the Chemistry–Climate Model Initiative (CCMI)
Geosci. Model Dev., 10, 639–671, 2017 www.geosci-model-dev.net/10/639/2017/ doi:10.5194/gmd-10-639-2017 © Author(s) 2017. CC Attribution 3.0 License. Review of the global models used within phase 1 of the Chemistry–Climate Model Initiative (CCMI) Olaf Morgenstern1, Michaela I. Hegglin2, Eugene Rozanov18,5, Fiona M. O’Connor14, N. Luke Abraham17,20, Hideharu Akiyoshi8, Alexander T. Archibald17,20, Slimane Bekki21, Neal Butchart14, Martyn P. Chipperfield16, Makoto Deushi15, Sandip S. Dhomse16, Rolando R. Garcia7, Steven C. Hardiman14, Larry W. Horowitz13, Patrick Jöckel10, Beatrice Josse9, Douglas Kinnison7, Meiyun Lin13,23, Eva Mancini3, Michael E. Manyin12,22, Marion Marchand21, Virginie Marécal9, Martine Michou9, Luke D. Oman12, Giovanni Pitari3, David A. Plummer4, Laura E. Revell5,6, David Saint-Martin9, Robyn Schofield11, Andrea Stenke5, Kane Stone11,a, Kengo Sudo19, Taichu Y. Tanaka15, Simone Tilmes7, Yousuke Yamashita8,b, Kohei Yoshida15, and Guang Zeng1 1National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand 2Department of Meteorology, University of Reading, Reading, UK 3Department of Physical and Chemical Sciences, Universitá dell’Aquila, L’Aquila, Italy 4Environment and Climate Change Canada, Montréal, Canada 5Institute for Atmospheric and Climate Science, ETH Zürich (ETHZ), Zürich, Switzerland 6Bodeker Scientific, Christchurch, New Zealand 7National Center for Atmospheric Research (NCAR), Boulder, Colorado, USA 8National Institute of Environmental Studies (NIES), Tsukuba, Japan 9CNRM UMR 3589, Météo-France/CNRS, -
The Met Office Unified Model Global Atmosphere 7.0/7.1 and JULES Global Land 7.0 Configurations
The Met Office Unified Model Global Atmosphere 7.0/7.1 and JULES Global Land 7.0 configurations Article Published Version Creative Commons: Attribution 4.0 (CC-BY) Open Access Walters, D., Baran, A. J., Boutle, I., Brooks, M., Earnshaw, P., Edwards, J., Furtado, K., Hill, P., Lock, A., Manners, J., Morcrette, C., Mulcahy, J., Sanchez, C., Smith, C., Stratton, R., Tennant, W., Tomassini, L., Van Weverberg, K., Vosper, S., Willett, M., Browse, J., Bushell, A., Carslaw, K., Dalvi, M., Essery, R., Gedney, N., Hardiman, S., Johnson, B., Johnson, C., Jones, A., Jones, C., Mann, G., Milton, S., Rumbold, H., Sellar, A., Ujiie, M., Whitall, M., Williams, K. and Zerroukat, M. (2019) The Met Office Unified Model Global Atmosphere 7.0/7.1 and JULES Global Land 7.0 configurations. Geoscientific Model Development, 12 (5). pp. 1909-1963. ISSN 1991-9603 doi: https://doi.org/10.5194/gmd-12-1909- 2019 Available at http://centaur.reading.ac.uk/83821/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . To link to this article DOI: http://dx.doi.org/10.5194/gmd-12-1909-2019 Publisher: EGU All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online Geosci. Model Dev., 12, 1909–1963, 2019 https://doi.org/10.5194/gmd-12-1909-2019 © Author(s) 2019. -
ARCOPOL the Atlantic Regions' Coastal Pollution Response
Airborne Pollution Propagation from water incidents: State of the art of air pollution models Activity 4 Task 4.2.1 ARCOPOL The Atlantic Regions’ Coastal Pollution Response Version: Version 2 Last updated on: 05/11/2010 Author: Meteogalicia Responsible partner: IST Involved partners: CETMAR, Meteogalicia, INTECMAR, IST, CIIMAR, EGMASA, Irish Marine Institute, Bretagne Region, Aquitaine Region Table of contents 1. Executive Summary .............................................................................................................. 3 2. Context and aims of the task ............................................................................................... 3 2.1. Summary of the 2008 Air Quality Directive ..................................................... 4 2.1.1. Concepts and definitions..................................................................................... 4 2.2. Where does the Air Quality Directive apply? .................................................. 6 2.2.1. Limits and target values for the protection of human health......................... 7 2.2.2. Limits and target values for the protection of vegetation............................... 9 2.2.3. Air quality web portals in Europe .................................................................... 9 3. Methodology........................................................................................................................ 12 3.1. When can models be used for the assessment of existing air quality? ....... 12 3.2. Combined use of measurements -
On the Uses of a New Linear Scheme for Stratospheric Methane in Global Models: Water Source, Transport Tracer and Radiative Forcing
This is a repository copy of On the uses of a new linear scheme for stratospheric methane in global models: water source, transport tracer and radiative forcing. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/76980/ Version: Published Version Article: Monge-Sanz, BM, Chipperfield, MP, Untch, A et al. (3 more authors) (2013) On the uses of a new linear scheme for stratospheric methane in global models: water source, transport tracer and radiative forcing. Atmospheric Chemistry and Physics, 13 (18). 9641 - 9660. ISSN 1680-7316 https://doi.org/10.5194/acp-13-9641-2013 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Atmos. Chem. Phys., 13, 9641–9660, 2013 Atmospheric Open Access www.atmos-chem-phys.net/13/9641/2013/ doi:10.5194/acp-13-9641-2013 Chemistry © Author(s) 2013. -
Climate Change
TRANSPORTATION RESEARCH Number E-C271 May 2021 Critical Issues in Aviation and the Environment 2021 TRANSPORTATION RESEARCH BOARD 2020 EXECUTIVE COMMITTEE OFFICERS Chair: Carlos M. Braceras, Executive Director, Utah Department of Transportation, Salt Lake City Vice Chair: Susan A. Shaheen, Adjunct Professor, Co-Director, Transportation Sustainability Research Center, University of California, Berkeley Division Chair for NRC Oversight: Chris Hendrickson, Hamerschlag University Professor Emeritus, Carnegie Mellon University, Pittsburgh, Pennsylvania Executive Director: Neil J. Pedersen, Transportation Research Board TRANSPORTATION RESEARCH BOARD 2020–2021 TECHNICAL ACTIVITIES COUNCIL Chair: Hyun-A C. Park, President, Spy Pond Partners, LLC, Arlington, Massachusetts Technical Activities Director: Ann M. Brach, Transportation Research Board Richard Bornhorst, Principal, FACTOR, Inc., Silver Spring, Maryland, Freight Systems Group Chair Michael Griffith, Director, Office of Safety Technologies, Federal Highway Administration, Washington, D.C., Safety and Operations Group Chair George Avery Grimes, CEO Advisor, Patriot Rail Company, Denver, Colorado, Rail Group Chair Brendon Hemily, Principal, Hemily and Associates, Toronto, Ontario, Public Transportation Group Chair Nikola Ivanov, Deputy Director, Center for Advanced Transportation Technology Laboratory, University of Maryland, College Park, Young Members Council Chair Pamela Keidel-Adams, Regional Vice President, Kimley-Horn and Associates, Inc., Mesa, Arizona, Aviation Group Chair C. James -
The New Hadley Centre Climate Model (Hadgem1): Evaluation of Coupled Simulations
1APRIL 2006 J OHNS ET AL. 1327 The New Hadley Centre Climate Model (HadGEM1): Evaluation of Coupled Simulations T. C. JOHNS,* C. F. DURMAN,* H. T. BANKS,* M. J. ROBERTS,* A. J. MCLAREN,* J. K. RIDLEY,* ϩ C. A. SENIOR,* K. D. WILLIAMS,* A. JONES,* G. J. RICKARD, S. CUSACK,* W. J. INGRAM,# M. CRUCIFIX,* D. M. H. SEXTON,* M. M. JOSHI,* B.-W. DONG,* H. SPENCER,@ R. S. R. HILL,* J. M. GREGORY,& A. B. KEEN,* A. K. PARDAENS,* J. A. LOWE,* A. BODAS-SALCEDO,* S. STARK,* AND Y. SEARL* *Met Office, Exeter, United Kingdom ϩNIWA, Wellington, New Zealand #Met Office, Exeter, and Department of Physics, University of Oxford, Oxford, United Kingdom @CGAM, University of Reading, Reading, United Kingdom &Met Office, Exeter, and CGAM, University of Reading, Reading, United Kingdom (Manuscript received 30 May 2005, in final form 9 December 2005) ABSTRACT A new coupled general circulation climate model developed at the Met Office’s Hadley Centre is pre- sented, and aspects of its performance in climate simulations run for the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4) documented with reference to previous models. The Hadley Centre Global Environmental Model version 1 (HadGEM1) is built around a new atmospheric dynamical core; uses higher resolution than the previous Hadley Centre model, HadCM3; and contains several improvements in its formulation including interactive atmospheric aerosols (sulphate, black carbon, biomass burning, and sea salt) plus their direct and indirect effects. The ocean component also has higher resolution and incorporates a sea ice component more advanced than HadCM3 in terms of both dynamics and thermodynamics. -
The Met Office Unified Model Global Atmosphere 6.0/6.1 and JULES Global Land 6.0/6.1 Configurations
The Met Office Unified Model Global Atmosphere 6.0/6.1 and JULES Global Land 6.0/6.1 configurations Article Published Version Creative Commons: Attribution 3.0 (CC-BY) Open Access Walters, D., Brooks, M., Boutle, I., Melvin, T., Stratton, R., Vosper, S., Wells, H., Williams, K., Wood, N., Allen, T., Bushell, A., Copsey, D., Earnshaw, P., Edwards, J., Gross, M., Hardiman, S., Harris, C., Heming, J., Klingaman, N., Levine, R., Manners, J., Martin, G., Milton, S., Mittermaier, M., Morcrette, C., Riddick, T., Roberts, M., Sanchez, C., Selwood, P., Stirling, A., Smith, C., Suri, D., Tennant, W., Vidale, P. L., Wilkinson, J., Willett, M., Woolnough, S. and Xavier, P. (2017) The Met Office Unified Model Global Atmosphere 6.0/6.1 and JULES Global Land 6.0/6.1 configurations. Geoscientific Model Development, 10 (4). pp. 1487-1520. ISSN 1991-9603 doi: https://doi.org/10.5194/gmd-10-1487-2017 Available at http://centaur.reading.ac.uk/69108/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . To link to this article DOI: http://dx.doi.org/10.5194/gmd-10-1487-2017 Publisher: European Geosciences Union All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online Geosci. -
Technical Manual for PRECIS
Technical Manual for PRECIS The Met Office Hadley Centre regional climate modelling system Version 2.0.0 www.metoffice.gov.uk/precis Simon Wilson, David Hassell, David Hein, Changgui Wang, Simon Tucker Richard Jones and Ruth Taylor November 16, 2015 Contents 1 Introduction 11 1.1 Background .............................. 11 1.2 Objectivesandstructureofthemanual . 12 2 Hardware, operating system and software environment 13 2.1 Recommended Hardware Configurations . 13 2.2 Multi-processorsystems . 14 2.3 InstallationofLinux ......................... 14 2.4 Compilers ............................... 16 2.5 System setup before installing PRECIS . 17 3 PRECIS software and installation 19 3.1 Introduction.............................. 19 3.2 Disklayout .............................. 20 3.3 Main steps in installation process . 21 3.4 Installation of PRECIS software and data . 22 3.5 InstallationofMetOfficedata . 26 3.5.1 Boundary data supplied on hard drive . 26 3.6 Installation verification . 28 3.7 InstallationofCDAT ......................... 29 4 Experimental design and setup 30 4.1 Experimentaldesign ......................... 30 4.1.1 Regional climate model . 30 2 4.1.2 Choice of driving model and forcing scenario . 30 4.1.3 CMIP5 Driving GCMs and Representative Concentration Pathways ........................... 37 4.1.4 Simulationlength. 40 4.1.5 Initial condition ensembles . 41 4.1.6 Choice of land surface scheme . 42 4.1.7 Outputdata.......................... 42 4.1.8 Spinup............................. 42 4.1.9 Choice of region . 43 4.1.10 Land-seamask ........................ 43 4.1.11 Altitude ............................ 45 4.1.12 Altitude of inland waters . 45 4.1.13 Soil and land cover . 45 4.1.14 RCM calendar and clock . 46 4.1.15 RCM Resolution . 46 4.1.16 Outputformat .......................