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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. -
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. -
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 Research 60:103
Vol. 60: 103–117, 2014 CLIMATE RESEARCH Published online June 17 doi: 10.3354/cr01222 Clim Res Ranking of global climate models for India using multicriterion analysis K. Srinivasa Raju1, D. Nagesh Kumar2,3,* 1Department of Civil Engineering, Birla Institute of Technology and Science-Pilani, Hyderabad campus, India 2Center for Earth Sciences, Indian Institute of Science, 560012 Bangalore, India 3Present address: Department of Civil Engineering, Indian Institute of Science, 560012 Bangalore, India ABSTRACT: Eleven GCMs (BCCR-BCCM2.0, INGV-ECHAM4, GFDL2.0, GFDL2.1, GISS, IPSL- CM4, MIROC3, MRI-CGCM2, NCAR-PCMI, UKMO-HADCM3 and UKMO-HADGEM1) were evaluated for India (covering 73 grid points of 2.5° × 2.5°) for the climate variable ‘precipitation rate’ using 5 performance indicators. Performance indicators used were the correlation coefficient, normalised root mean square error, absolute normalised mean bias error, average absolute rela- tive error and skill score. We used a nested bias correction methodology to remove the systematic biases in GCM simulations. The Entropy method was employed to obtain weights of these 5 indi- cators. Ranks of the 11 GCMs were obtained through a multicriterion decision-making outranking method, PROMETHEE-2 (Preference Ranking Organisation Method of Enrichment Evaluation). An equal weight scenario (assigning 0.2 weight for each indicator) was also used to rank the GCMs. An effort was also made to rank GCMs for 4 river basins (Godavari, Krishna, Mahanadi and Cauvery) in peninsular India. The upper Malaprabha catchment in Karnataka, India, was chosen to demonstrate the Entropy and PROMETHEE-2 methods. The Spearman rank correlation coefficient was employed to assess the association between the ranking patterns. -
Future Predictions of Rainfall and Temperature Using GCM and ANN for Arid Regions: a Case Study for the Qassim Region, Saudi Arabia
water Article Future Predictions of Rainfall and Temperature Using GCM and ANN for Arid Regions: A Case Study for the Qassim Region, Saudi Arabia Khalid Alotaibi 1,*, Abdul Razzaq Ghumman 1 , Husnain Haider 1, Yousry Mahmoud Ghazaw 1,2 and Md. Shafiquzzaman 1 1 Department of Civil Engineering, College of Engineering, Qassim University, Buraydah 51431, Al Qassim, Saudi Arabia; [email protected] (A.R.G.); [email protected] (H.H.); [email protected] (Y.M.G.); shafi[email protected] (M.S.) 2 Department of Irrigation and Hydraulics, College of Engineering, Alexandria University, Alexandria 21544, Egypt * Correspondence: [email protected]; Tel.: +966-531-105-001 Received: 26 July 2018; Accepted: 13 September 2018; Published: 15 September 2018 Abstract: Future predictions of rainfall patterns in water-scarce regions are highly important for effective water resource management. Global circulation models (GCMs) are commonly used to make such predictions, but these models are highly complex and expensive. Furthermore, their results are associated with uncertainties and variations for different GCMs for various greenhouse gas emission scenarios. Data-driven models including artificial neural networks (ANNs) and adaptive neuro fuzzy inference systems (ANFISs) can be used to predict long-term future changes in rainfall and temperature, which is a challenging task and has limitations including the impact of greenhouse gas emission scenarios. Therefore, in this research, results from various GCMs and data-driven models were investigated to study the changes in temperature and rainfall of the Qassim region in Saudi Arabia. Thirty years of monthly climatic data were used for trend analysis using Mann–Kendall test and simulating the changes in temperature and rainfall using three GCMs (namely, HADCM3, INCM3, and MPEH5) for the A1B, A2, and B1 emissions scenarios as well as two data-driven models (ANN: feed-forward-multilayer, perceptron and ANFIS) without the impact of any emissions scenario. -
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.