A Review of Operational, Regional-Scale, Chemical Weather Forecasting Models in Europe
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Chapter 6: Ensemble Forecasting and Atmospheric Predictability
Chapter 6: Ensemble Forecasting and Atmospheric Predictability Introduction Deterministic Chaos (what!?) In 1951 Charney indicated that forecast skill would break down, but he attributed it to model errors and errors in the initial conditions… In the 1960’s the forecasts were skillful for only one day or so. Statistical prediction was equal or better than dynamical predictions, Like it was until now for ENSO predictions! Lorenz wanted to show that statistical prediction could not match prediction with a nonlinear model for the Tokyo (1960) NWP conference So, he tried to find a model that was not periodic (otherwise stats would win!) He programmed in machine language on a 4K memory, 60 ops/sec Royal McBee computer He developed a low-order model (12 d.o.f) and changed the parameters and eventually found a nonperiodic solution Printed results with 3 significant digits (plenty!) Tried to reproduce results, went for a coffee and OOPS! Lorenz (1963) discovered that even with a perfect model and almost perfect initial conditions the forecast loses all skill in a finite time interval: “A butterfly in Brazil can change the forecast in Texas after one or two weeks”. In the 1960’s this was only of academic interest: forecasts were useless in two days Now, we are getting closer to the 2 week limit of predictability, and we have to extract the maximum information Central theorem of chaos (Lorenz, 1960s): a) Unstable systems have finite predictability (chaos) b) Stable systems are infinitely predictable a) Unstable dynamical system b) Stable dynamical -
Model Error in Weather and Climate Forecasting £ Myles Allen £ , Jamie Kettleborough† and David Stainforth
Model error in weather and climate forecasting £ Myles Allen £ , Jamie Kettleborough† and David Stainforth Department£ of Physics, University of Oxford †Space Science and Technology Department, Rutherford Appleton Laboratory “As if someone were to buy several copies of the morning newspaper to assure himself that what it said was true” Ludwig Wittgenstein 1 Introduction We review various interpretations of the phrase “model error”, choosing to focus here on how to quantify and minimise the cumulative effect of model “imperfections” that either have not been eliminated because of incomplete observations/understanding or cannot be eliminated because they are intrinsic to the model’s structure. We will not provide a recipe for eliminating these imperfections, but rather some ideas on how to live with them because, no matter how clever model-developers, or fast super-computers, become, these imperfections will always be with us and represent the hardest source of uncertainty to quantify in a weather or climate forecast. We spend a little time reviewing how uncertainty in the current state of the atmosphere/ocean system is used in the initialisation of ensemble weather or seasonal forecasting, because it might appear to provide a reasonable starting point for the treatment of model error. This turns out not to be the case, because of the fundamental problem of the lack of an objective metric or norm for model error: we have no way of measuring the distance between two models or model-versions in terms of their input parameters or structure in all but a trivial and irrelevant subset of cases. Hence there is no way of allowing for model error by sampling the space of “all possible models” in a representative way, because distance within this space is undefinable. -
Large-Scale Tropospheric Transport in the Chemistry–Climate Model Initiative (CCMI) Simulations
Atmos. Chem. Phys., 18, 7217–7235, 2018 https://doi.org/10.5194/acp-18-7217-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Large-scale tropospheric transport in the Chemistry–Climate Model Initiative (CCMI) simulations Clara Orbe1,2,3,a, Huang Yang3, Darryn W. Waugh3, Guang Zeng4, Olaf Morgenstern 4, Douglas E. Kinnison5, Jean-Francois Lamarque5, Simone Tilmes5, David A. Plummer6, John F. Scinocca7, Beatrice Josse8, Virginie Marecal8, Patrick Jöckel9, Luke D. Oman10, Susan E. Strahan10,11, Makoto Deushi12, Taichu Y. Tanaka12, Kohei Yoshida12, Hideharu Akiyoshi13, Yousuke Yamashita13,14, Andreas Stenke15, Laura Revell15,16, Timofei Sukhodolov15,17, Eugene Rozanov15,17, Giovanni Pitari18, Daniele Visioni18, Kane A. Stone19,20,b, Robyn Schofield19,20, and Antara Banerjee21 1Goddard Earth Sciences Technology and Research (GESTAR), Columbia, MD, USA 2Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA 3Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland, USA 4National Institute of Water and Atmospheric Research, Wellington, New Zealand 5National Center for Atmospheric Research (NCAR), Atmospheric Chemistry Observations and Modeling (ACOM) Laboratory, Boulder, USA 6Climate Research Branch, Environment and Climate Change Canada, Montreal, QC, Canada 7Climate Research Branch, Environment and Climate Change Canada, Victoria, BC, Canada 8Centre National de Recherches Météorologiques UMR 3589, Météo-France/CNRS, -
Description and Evaluation of the Model for Ozone and Related Chemical Tracers, Version 4 (MOZART-4)
Geosci. Model Dev., 3, 43–67, 2010 www.geosci-model-dev.net/3/43/2010/ Geoscientific © Author(s) 2010. This work is distributed under Model Development the Creative Commons Attribution 3.0 License. Description and evaluation of the Model for Ozone and Related chemical Tracers, version 4 (MOZART-4) L. K. Emmons1, S. Walters1, P. G. Hess1,*, J.-F. Lamarque1, G. G. Pfister1, D. Fillmore1,**, C. Granier2,3, A. Guenther1, D. Kinnison1, T. Laepple1,***, J. Orlando1, X. Tie1, G. Tyndall1, C. Wiedinmyer1, S. L. Baughcum4, and S. Kloster5,* 1National Center for Atmospheric Research, Boulder, CO, USA 2Centre National de la Recherche Scientifique, Paris, France 3NOAA, Earth System Research Laboratory, Boulder, CO, USA 4Boeing Company, Seattle, WA, USA 5Max-Planck-Institute for Meteorology, Hamburg, Germany *now at: Department of Biological and Environmental Engineering, Cornell University, Ithaca, NY, USA **now at: Tech-X Corporation, Boulder, CO, USA ***now at: Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany Received: 6 August 2009 – Published in Geosci. Model Dev. Discuss.: 27 August 2009 Revised: 7 December 2009 – Accepted: 8 December 2009 – Published: 12 January 2010 Abstract. The Model for Ozone and Related chemical Tra- teorological observations. MOZART is built on the frame- cers, version 4 (MOZART-4) is an offline global chemical work of the Model of Atmospheric Transport and Chemistry transport model particularly suited for studies of the tropo- (MATCH) (Rasch et al., 1997). Convective mass fluxes are sphere. The updates of the model from its previous version diagnosed by the model, using the shallow and mid-level MOZART-2 are described, including an expansion of the convective transport formulation of Hack (1994) and deep chemical mechanism to include more detailed hydrocarbon convection scheme of Zhang and MacFarlane (1995). -
A Machine Learning Based Ensemble Forecasting Optimization Algorithm for Preseason Prediction of Atlantic Hurricane Activity
atmosphere Article A Machine Learning Based Ensemble Forecasting Optimization Algorithm for Preseason Prediction of Atlantic Hurricane Activity Xia Sun 1 , Lian Xie 1,*, Shahil Umeshkumar Shah 2 and Xipeng Shen 2 1 Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Box 8208, Raleigh, NC 27695-8208, USA; [email protected] 2 Department of Computer Sciences, North Carolina State University, Raleigh, NC 27695-8206, USA; [email protected] (S.U.S.); [email protected] (X.S.) * Correspondence: [email protected] Abstract: In this study, nine different statistical models are constructed using different combinations of predictors, including models with and without projected predictors. Multiple machine learning (ML) techniques are employed to optimize the ensemble predictions by selecting the top performing ensemble members and determining the weights for each ensemble member. The ML-Optimized Ensemble (ML-OE) forecasts are evaluated against the Simple-Averaging Ensemble (SAE) forecasts. The results show that for the response variables that are predicted with significant skill by individual ensemble members and SAE, such as Atlantic tropical cyclone counts, the performance of SAE is comparable to the best ML-OE results. However, for response variables that are poorly modeled by Citation: Sun, X.; Xie, L.; Shah, S.U.; individual ensemble members, such as Atlantic and Gulf of Mexico major hurricane counts, ML-OE Shen, X. A Machine Learning Based predictions often show higher skill score than individual model forecasts and the SAE predictions. Ensemble Forecasting Optimization Algorithm for Preseason Prediction of However, neither SAE nor ML-OE was able to improve the forecasts of the response variables when Atlantic Hurricane Activity. -
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, -
Air Quality Modelling in the Summer Over the Eastern Mediterranean Using WRF-Chem: Chemistry and Aerosol Mechanism Intercomparison
Atmos. Chem. Phys., 18, 1555–1571, 2018 https://doi.org/10.5194/acp-18-1555-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Air quality modelling in the summer over the eastern Mediterranean using WRF-Chem: chemistry and aerosol mechanism intercomparison George K. Georgiou1, Theodoros Christoudias2, Yiannis Proestos1, Jonilda Kushta1, Panos Hadjinicolaou1, and Jos Lelieveld3,1 1Energy, Environment and Water Research Center, The Cyprus Institute, Nicosia, Cyprus 2Computation-based Science and Technology Research Centre (CaSToRC), The Cyprus Institute, Nicosia, Cyprus 3Atmospheric Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany Correspondence: Theodoros Christoudias ([email protected]) Received: 22 August 2017 – Discussion started: 19 September 2017 Revised: 14 December 2017 – Accepted: 24 December 2017 – Published: 2 February 2018 Abstract. We employ the WRF-Chem model to study sum- ozone precursors is not captured (hourly correlation coef- mertime air pollution, the intense photochemical activity and ficients for O3 ≤ 0.29). This might be attributed to the un- their impact on air quality over the eastern Mediterranean. derestimation of NOx concentrations by local emissions by We utilize three nested domains with horizontal resolutions up to 50 %. For the fine particulate matter (PM2:5), the low- of 80, 16 and 4 km, with the finest grid focusing on the island est mean bias (9 µg m−3) is obtained with the RADM2- of Cyprus, where the CYPHEX campaign took place in July MADE/SORGAM mechanism, with overestimates in sulfate 2014. Anthropogenic emissions are based on the EDGAR and ammonium aerosols. Overestimation of sulfate aerosols HTAP global emission inventory, while dust and biogenic by this mechanism may be linked to the SO2 oxidation emissions are calculated online. -
Attribution of Projected Changes in Summertime US Ozone and PM2.5 Concentrations to Global Changes
Atmos. Chem. Phys., 9, 1111–1124, 2009 www.atmos-chem-phys.net/9/1111/2009/ Atmospheric © Author(s) 2009. This work is distributed under Chemistry the Creative Commons Attribution 3.0 License. and Physics Attribution of projected changes in summertime US ozone and PM2.5 concentrations to global changes J. Avise1,*, J. Chen1,**, B. Lamb1, C. Wiedinmyer2, A. Guenther2, E. Salathe´3, and C. Mass3 1Laboratory for Atmospheric Research, Washington State University, Pullman, Washington, USA 2National Center for Atmospheric Research, Boulder, Colorado, USA 3University of Washington, Seattle, Washington, USA *now at: California Air Resources Board, Sacramento, CA, USA **now at: National Research Council of Canada, Ottawa, ON, Canada Received: 12 June 2008 – Published in Atmos. Chem. Phys. Discuss.: 11 August 2008 Revised: 6 January 2009 – Accepted: 15 January 2009 – Published: 16 February 2009 Abstract. The impact that changes in future climate, an- sidered simultaneously, the average DM8H ozone decreases thropogenic US emissions, background tropospheric com- due to a reduction in biogenic VOC emissions ( 2.6 ppbv). − position, and land-use have on summertime regional US Changes in average 24-h (A24-h) PM2.5 concentrations are ozone and PM2.5 concentrations is examined through a ma- dominated by projected changes in anthropogenic emissions 3 trix of downscaled regional air quality simulations, where (+3 µg m− ), while changes in chemical boundary condi- each set of simulations was conducted for five months of July tions have a negligible effect. On average, climate change 3 climatology, using the Community Multi-scale Air Quality reduces A24-h PM2.5 concentrations by 0.9 µg m− , but (CMAQ) model. -
Modelling of the Atmospheric Dispersion of Mercury Emitted from the Power Sector in Poland J
Modelling of the atmospheric dispersion of mercury emitted from the power sector in Poland J. Zysk, Y. Roustan, A. Wyrwa To cite this version: J. Zysk, Y. Roustan, A. Wyrwa. Modelling of the atmospheric dispersion of mercury emitted from the power sector in Poland. Atmospheric environment, Elsevier, 2015, 112, pp.246-256. 10.1016/j.atmosenv.2015.04.040. hal-01238312 HAL Id: hal-01238312 https://hal-enpc.archives-ouvertes.fr/hal-01238312 Submitted on 8 Feb 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Atmospheric Environment 112 (2015) 246e256 Contents lists available at ScienceDirect Atmospheric Environment journal homepage: www.elsevier.com/locate/atmosenv Modelling of the atmospheric dispersion of mercury emitted from the power sector in Poland * J. Zysk a, , Y. Roustan b, A. Wyrwa a a AGH University of Science and Technology, Faculty of Energy and Fuels, Poland b CEREA Joint Laboratory Ecole des Ponts ParisTech e EDF R&D, Universite Paris-Est, France highlights Applicability of the new chemical model of mercury was demonstrated. Hg reactions with bromine compounds have significant impact on modelling results. The contribution of polish sources in monthly Hg deposition varies from 10 to 22%. -
Coupled Chemistry-Meteorology/ Climate Modelling (CCMM): Status and Relevance for Numerical Weather Prediction, Atmospheric Pollution and Climate Research
GAW Report No. 226 WWRP 2016-1 WCRP Report No. 9/2016 Coupled Chemistry-Meteorology/ Climate Modelling (CCMM): status and relevance for numerical weather prediction, atmospheric pollution and climate research (Geneva, Switzerland, 23-25 February 2015) WEATHER CLIMATE WATER CLIMATE WEATHER WMO-No. 1172 GAW Report No. 226 WWRP 2016-1 WCRP Report No. 9/2016 Coupled Chemistry-Meteorology/ Climate Modelling (CCMM): status and relevance for numerical weather prediction, atmospheric pollution and climate research (Geneva, Switzerland, 23-25 February 2015) WMO-No. 1172 2016 WMO-No. 1172 © World Meteorological Organization, 2016 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate this publication in part or in whole should be addressed to: Chairperson, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 84 03 P.O. Box 2300 Fax: +41 (0) 22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] ISBN 978-92-63-11172-2 NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of WMO concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of itsfrontiers or boundaries. The mention of specific companies or products does not imply that they are endorsed or recommended by WMO in preference to others of a similar nature which are not mentioned or advertised. -
Tropospheric Chemistry in the Integrated Forecasting System of ECMWF
730 Tropospheric Chemistry in the Integrated Forecasting System of ECMWF Johannes Flemming 1, Vincent Huijnen 3, Joaquim Arteta 2, Peter Bechtold 1, Anton Beljaars 1, Anne-Marlene Blechschmidt 5, Michail Diamantakis 1,Richard J. Engelen 1,Audrey Gaudel 7,Antje Inness 1,Luke Jones 1,Eleni Katragkou 6, Vincent-Henri Peuch 1,Andreas Richter 5,Martin G. Schultz 4, Olaf Stein 4 and Athanasios Tsikerdekis 6 Research Department September 2014 1) European Centre for Medium-Range Weather Forecasts, Reading, UK 2) Météo-France, Toulouse, France 3) Royal Netherlands Meteorological Institute, De Bilt, The Netherlands 4) Institute for Energy and Climate Research, FZ Jülich, Germany 5) Universität Bremen, Germany 6) Aristotle University of Thessaloniki, Greece 7) CNRS, Laboratoire d'Aérologie, UMR 5560, Toulouse, France Series: ECMWF Technical Memoranda A full list of ECMWF Publications can be found on our web site under: http://www.ecmwf.int/publications/ Contact: [email protected] © Copyright 2014 European Centre for Medium Range Weather Forecasts Shinfield Park, Reading, Berkshire RG2 9AX, England Literary and scientific copyrights belong to ECMWF and are reserved in all countries. This publication is not to be reprinted or translated in whole or in part without the written permission of the Director. Appropriate non-commercial use will normally be granted under the condition that reference is made to ECMWF. The information within this publication is given in good faith and considered to be true, but ECMWF accepts no liability for error, omission and for loss or damage arising from its use. Abstract A representation of atmospheric chemistry has been included in the Integrated Forecasting System (IFS) of the European Centre for Medium-range Weather Forecasts (ECMWF).