ASCENT Project 019 2019 Annual Report.V5 Edited EIC+UNC CS EIC
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Climate Models and Their Evaluation
8 Climate Models and Their Evaluation Coordinating Lead Authors: David A. Randall (USA), Richard A. Wood (UK) Lead Authors: Sandrine Bony (France), Robert Colman (Australia), Thierry Fichefet (Belgium), John Fyfe (Canada), Vladimir Kattsov (Russian Federation), Andrew Pitman (Australia), Jagadish Shukla (USA), Jayaraman Srinivasan (India), Ronald J. Stouffer (USA), Akimasa Sumi (Japan), Karl E. Taylor (USA) Contributing Authors: K. AchutaRao (USA), R. Allan (UK), A. Berger (Belgium), H. Blatter (Switzerland), C. Bonfi ls (USA, France), A. Boone (France, USA), C. Bretherton (USA), A. Broccoli (USA), V. Brovkin (Germany, Russian Federation), W. Cai (Australia), M. Claussen (Germany), P. Dirmeyer (USA), C. Doutriaux (USA, France), H. Drange (Norway), J.-L. Dufresne (France), S. Emori (Japan), P. Forster (UK), A. Frei (USA), A. Ganopolski (Germany), P. Gent (USA), P. Gleckler (USA), H. Goosse (Belgium), R. Graham (UK), J.M. Gregory (UK), R. Gudgel (USA), A. Hall (USA), S. Hallegatte (USA, France), H. Hasumi (Japan), A. Henderson-Sellers (Switzerland), H. Hendon (Australia), K. Hodges (UK), M. Holland (USA), A.A.M. Holtslag (Netherlands), E. Hunke (USA), P. Huybrechts (Belgium), W. Ingram (UK), F. Joos (Switzerland), B. Kirtman (USA), S. Klein (USA), R. Koster (USA), P. Kushner (Canada), J. Lanzante (USA), M. Latif (Germany), N.-C. Lau (USA), M. Meinshausen (Germany), A. Monahan (Canada), J.M. Murphy (UK), T. Osborn (UK), T. Pavlova (Russian Federationi), V. Petoukhov (Germany), T. Phillips (USA), S. Power (Australia), S. Rahmstorf (Germany), S.C.B. Raper (UK), H. Renssen (Netherlands), D. Rind (USA), M. Roberts (UK), A. Rosati (USA), C. Schär (Switzerland), A. Schmittner (USA, Germany), J. Scinocca (Canada), D. Seidov (USA), A.G. -
Documentation and Software User’S Manual, Version 4.1
The Canadian Seasonal to Interannual Prediction System version 2 (CanSIPSv2) Canadian Meteorological Centre Technical Note H. Lin1, W. J. Merryfield2, R. Muncaster1, G. Smith1, M. Markovic3, A. Erfani3, S. Kharin2, W.-S. Lee2, M. Charron1 1-Meteorological Research Division 2-Canadian Centre for Climate Modelling and Analysis (CCCma) 3-Canadian Meteorological Centre (CMC) 7 May 2019 i Revisions Version Date Authors Remarks 1.0 2019/04/22 Hai Lin First draft 1.1 2019/04/26 Hai Lin Corrected the bias figures. Comments from Ryan Muncaster, Bill Merryfield 1.2 2019/05/01 Hai Lin Figures of CanSIPSv2 uses CanCM4i plus GEM-NEMO 1.3 2019/05/03 Bill Merrifield Added CanCM4i information, sea ice Hai Lin verification, 6.6 and 9 1.4 2019/05/06 Hai Lin All figures of CanSIPSv2 with CanCM4i and GEM-NEMO, made available by Slava Kharin ii © Environment and Climate Change Canada, 2019 Table of Contents 1 Introduction ............................................................................................................................. 4 2 Modifications to models .......................................................................................................... 6 2.1 CanCM4i .......................................................................................................................... 6 2.2 GEM-NEMO .................................................................................................................... 6 3 Forecast initialization ............................................................................................................. -
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). -
Table of Contents
CALPUFF Modeling System Version 6 User Instructions April 2011 Section 1: Introduction Table of Contents Page 1. OVERVIEW ...................................................................................................................... 1-1 1.1 CALPUFF Version 6 Modeling System............................................................... 1-1 1.2 Historical Background .......................................................................................... 1-2 1.3 Overview of the Modeling System ....................................................................... 1-7 1.4 Major Model Algorithms and Options................................................................. 1-19 1.4.1 CALMET................................................................................................ 1-19 1.4.2 CALPUFF............................................................................................... 1-23 1.5 Summary of Data and Computer Requirements .................................................. 1-28 2. GEOPHYSICAL DATA PROCESSORS.......................................................................... 2-1 2.1 TERREL Terrain Preprocessor............................................................................. 2-3 2.2 Land Use Data Preprocessors (CTGCOMP and CTGPROC) ............................. 2-27 2.2.1 Obtaining the Data.................................................................................. 2-27 2.2.2 CTGCOMP - the CTG land use data compression program .................. 2-29 2.2.3 CTGPROC - the land use preprocessor -
Atmospheric Dispersion of Radioactive Material in Radiological Risk Assessment and Emergency Response
Progress in NUCLEAR SCIENCE and TECHNOLOGY, Vol. 1, p.7-13 (2011) REVIEW Atmospheric Dispersion of Radioactive Material in Radiological Risk Assessment and Emergency Response YAO Rentai * China Institute for Radiation Protection, P.O.Box 120, Taiyuan, Shanxi 030006, China The purpose of a consequence assessment system is to assess the consequences of specific hazards on people and the environment. In this paper, the studies on technique and method of atmospheric dispersion modeling of radioactive material in radiological risk assessment and emergency response are reviewed in brief. Some current statuses of nuclear accident consequences assessment in China were introduced. In the future, extending the dispersion modeling scales such as urban building scale, establishing high quality experiment dataset and method of model evaluation, improved methods of real-time modeling using limited inputs, and so on, should be promoted with high priority of doing much more work. KEY WORDS: atmospheric model, risk assessment, emergency response, nuclear accident 11) I. Introduction from U.S. NOAA, and SPEEDI/WSPEEDI from The studies and developments of techniques and methods Japan/JAERI. However, the needs of emergency of atmospheric dispersion modeling of radioactive material management may not be well satisfied by existing models in radiological risk assessment and emergency response which are not well designed and confronted with difficulty have evolved over the past 50-60 years. The three marked in detailed constructions of local wind and turbulence -
Lecture 29. Introduction to Atmospheric Chemical Transport Models
Lecture 29. Introduction to atmospheric chemical transport models. Part 1. Objectives: 1. Model types. 2. Box models. 3. One-dimensional models. 4. Two-dimensional models. 5. Three-dimensional models. Readings: Graedel T. and P.Crutzen. “Atmospheric change: an earth system perspective”. Chapter 15.”Bulding environmental chemical models”, 1992. 1. Model types. Mathematical models provide the necessary framework for integration of our understanding of individual atmospheric processes and study of their interactions. Note, that atmosphere is a complex reactive system in which numerous physical and chemical processes occur simultaneously. • Atmospheric chemical transport models are defined according to their spatial scale: Model Typical domain scale Typical resolution Microscale 200x200x100 m 5 m Mesoscale(urban) 100x100x5 km 2 km Regional 1000x1000x10 km 20 km Synoptic(continental) 3000x3000x20 km 80 km Global 65000x65000x20km 50x50 1 Figure 29.1 Components of a chemical transport model (Seinfeld and Pandis, 1998). 2 • Domain of the atmospheric model is the area that is simulated. The computation domain consists of an array of computational cells, each having uniform chemical composition. The size of cells determines the spatial resolution of the model. • Atmospheric chemical transport models are also characterized by their dimensionality: zero-dimensional (box) model; one-dimensional (column) model; two-dimensional model; and three-dimensional model. • Model time scale depends on a specific application varying from hours (e.g., air quality model) to hundreds of years (e.g., climate models) 3 Two principal approaches to simulate changes in the chemical composition of a given air parcel: 1) Lagrangian approach: air parcel moves with the local wind so that there is no mass exchange that is allowed to enter the air parcel and its surroundings (except of species emissions). -
A Brief Summary of Plans for the GMAO Core Priorities and Initiatives for the Next 5 Years
A Brief Summary of Plans for the GMAO Core Priorities and Initiatives for the Next 5 years Provided as information for ROSES 2012 A.13 – MAP Developments in the GMAO are focused on the next generation systems, GEOS-6, and an Integrated Earth System Analysis and the associated modeling system that supports that analysis. GEOS-6 and IESA (1) The GEOS-6 system will be built around the next generation, non-hydrostatic atmospheric model with aerosol-cloud microphysics (advances upon the Morrison-Gettelman cloud microphysics and the Modal Aerosol Model (MAM) aerosol microphysics module for the inclusion of aerosol indirect effects) and an accompanying hybrid (ensemble-variational) 4DVar atmospheric assimilation system. (2) IESA capabilities for other parts of the earth system, including atmospheric chemical constituents and aerosols, ocean circulation, land hydrology, and carbon budget will be built upon our existing separate assimilation capabilities. The GEOS Model Our modeling strategy is driven by the need to have a comprehensive global model valid for both weather and climate and for use in both simulation and assimilation. Our main task in atmospheric modeling during the next five years will be to make the transition to GEOS-6. This direction is driven by (i) the need to improve the representation of clouds and precipitation to enable use of cloud- and precipitation-contaminated satellite radiance observations in NWP, and (ii) the research goal of understanding and predicting weather- climate connections. Development will focus on 1km to 10km resolutions that will be needed for the data assimilation system (DAS). Climate resolutions (10-100km) will not be ignored, but developments for resolutions coarser than 50 km will have lower priority. -
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 ........................................................................................... -
Technical Assistance for Improving Emissions Control the Role Of
This Project is Co-Financed by the European Union and the Republic of Turkey This Project is c This project is co-financed by the European Union and the Republic of Turkey Technical Assistance for Improving Emissions Control Service Contract No: TR0802.03-02/001 Identification No: EuropeAid/128897/D/SER/TR The Role of Emissions Dispersion Modelling in Cost Benefit Analysis Applied to Urban Air Quality Management: Part 1-the Approach (Version 2: 18 May 2012) This publication has been produced with the assistance of the European Union. The content of this publication is the sole responsibility of the Consortium led by PM Group and can in no way be taken to reflect the views of the European Union. Contracting Authority: Central Finance and Contracting Unit, Turkey Implementing Authority / Beneficiary: Ministry of Environment and Urbanisation Project Title: Improving Emissions Control Service Contract Number: TR0802.03-02/001 Identification Number: EuropeAid/128897/D/SER/TR PM Project Number: 300424 This project is co-financed by the European Union and the Republic of Turkey The Role of Emissions Dispersion Modelling in Cost Benefit Analysis Applied to Urban Air Quality Management: Part 1 – the Approach Version 2: 18 May 2012 PM File Number: 300424-06-RP-200 PM Document Number: 300424-06-205(2) CURRENT ISSUE Issue No.: 2 Date: 18/05/2012 Reason for Issue: Final Version for Client Approval Customer Approval Sign-Off Originator Reviewer Approver (if required) Scott Hamilton, Peter Print Name Russell Frost Jim McNelis Faircloth, Chris Dore Signature Date PREVIOUS ISSUES (Type Names) Issue No. Date Originator Reviewer Approver Customer Reason for Issue 1 14/03/2012 Scott Hamilton, Peter Russell Frost Jim McNelis For client review / comment Faircloth, Chris Dore CFCU / MoEU 300424-06-RP-205 (2) TA for Improving Emissions Control 18 May 2012 CONTENTS GLOSSARY OF ACRONYMS ...................................................................................... -
DJ Karoly Et
Supporting Online Material “Detection of a human influence on North American climate”, D. J. Karoly et al. (2003) Materials and Methods Description of the climate models GFDL R30 is a spectral atmospheric model with rhomboidal truncation at wavenumber 30 equivalent to 3.75° longitude × 2.2° latitude (96 × 80) with 14 levels in the vertical. The atmospheric model is coupled to an 18 level gridpoint (192 × 80) ocean model where two ocean grid boxes underlie each atmospheric grid box exactly. Both models are described by Delworth et al. (S1) and Dixon et al. (S2). HadCM2 and HadCM3 use the same atmospheric horizontal resolution, 3.75°× 2.5° (96 × 72) finite difference model (T42/R30 equivalent) with 19 levels in the atmosphere and 20 levels in the ocean (S3, S4). For HadCM2, the ocean horizontal grid lies exactly under that of the atmospheric model. The ocean component of HadCM3 uses much higher resolution (1.25° × 1.25°) with six ocean grid boxes for every atmospheric grid box. In the context of results shown here, the main difference between the two models is that HadCM3 includes improved representations of physical processes in the atmosphere and the ocean (S5). For example, HadCM3 employs a radiation scheme that explicitly represents the radiative effects of minor greenhouse gases as well as CO2, water vapor and ozone (S6), as well as a simple parametrization of background aerosol (S7). ECHAM4/OPYC3 is an atmospheric T42 spectral model equivalent to 2.8° longitude × 2.8° latitude (128 × 64) with 19 vertical layers. The ocean model OPYC3 uses isopycnals as the vertical coordinate system. -
Climate Reanalysis
from Newsletter Number 139 – Spring 2014 METEOROLOGY Climate reanalysis doi:10.21957/qnreh9t5 Dick Dee interviewed by Bob Riddaway Climate reanalysis This article appeared in the Meteorology section of ECMWF Newsletter No. 139 – Spring 2014, pp. 15–21. Climate reanalysis Dick Dee interviewed by Bob Riddaway Dick Dee is the Head of the Reanalysis Section at ECMWF. He is responsible for leading a group of scientists producing state-of-the art global climate datasets. This has involved coordinating two international research projects: ERA-CLIM and ERA-CLIM2. The ERA-CLIM2 project has recently started – what is its purpose? This exciting new project extends and expands the work begun in the ERA-CLIM project that ended in December 2013. The aim is to produce physically consistent reanalyses of the global atmosphere, ocean, land-surface, cryosphere and the carbon cycle – see Box A for more information about what is involved in reanalysis. The project is at the heart of a concerted effort in Europe to build the information infrastructure needed to support climate monitoring, climate research and climate services, based on the best available science and observations. The ERA-CLIM2 project will rely on ECMWF’s expertise in modelling and data assimilation to develop a first th coupled ocean-atmosphere reanalysis spanning the 20 century. It includes activities aimed at improving the available observational record (e.g. through data rescue and reprocessing), the assimilating model (primarily by coupling the atmosphere with the ocean) and the data assimilation techniques (e.g. related to data assimilation in coupled models). The project will also develop improved data services in order to prepare for the need to support new classes of users, including providers of climate services and European policy makers. -
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.