Relevant bibliographies by topics / Coupled climate model simulations

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Coupled climate model simulations'

Author: Grafiati
Published: 4 June 2025
Last updated: 1 August 2025

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Journal articles on the topic "Coupled climate model simulations"

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Chen, Hua, Edwin K. Schneider, Ben P. Kirtman, and Ioana Colfescu. "Evaluation of Weather Noise and Its Role in Climate Model Simulations*." Journal of Climate 26, no. 11 (2013): 3766–84. http://dx.doi.org/10.1175/jcli-d-12-00292.1.

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Abstract The relationship between coupled atmosphere–ocean general circulation model simulations and uncoupled simulations made with specified SST and sea ice is investigated using the Community Climate System Model, version 3. Experiments are carried out in a perfect model framework. Two closely related questions are investigated: 1) whether the statistics of the atmospheric weather noise in the atmospheric model are the same as in the coupled model, and 2) whether the atmospheric model reproduces the SST-forced response of the coupled model. The weather noise in both the coupled and uncouple
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Falquina, Rafael, la Vara Alba de, William Cabos, Dmitry Sein, and Clemente Gallardo. "Impact of ocean-atmosphere coupling on present and future Köppen-Geiger climate classification in Europe." Atmospheric Research 275 (May 5, 2022): 106223. https://doi.org/10.1016/j.atmosres.2022.106223.

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The effect of air-sea coupling in the simulation of the European climate is assessed through a climate type classification that uses surface temperature and precipitation from a regional atmosphere-ocean coupled model and from its atmospheric component. The atmospheric setup in both models is the same, differing only in the representation of the oceanic fields. The simulations cover the present and future-time climate under the RCP8.5 CMIP5 scenario. Climate type distributions obtained from both coupled and uncoupled simulations are similar to those obtained from ERA5 for the 1976&nd
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Nobre, Paulo, Leo S. P. Siqueira, Roberto A. F. de Almeida, et al. "Climate Simulation and Change in the Brazilian Climate Model." Journal of Climate 26, no. 17 (2013): 6716–32. http://dx.doi.org/10.1175/jcli-d-12-00580.1.

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Abstract The response of the global climate system to atmospheric CO2 concentration increase in time is scrutinized employing the Brazilian Earth System Model Ocean–Atmosphere version 2.3 (BESM-OA2.3). Through the achievement of over 2000 yr of coupled model integrations in ensemble mode, it is shown that the model simulates the signal of recent changes of global climate trends, depicting a steady atmospheric and oceanic temperature increase and corresponding marine ice retreat. The model simulations encompass the time period from 1960 to 2105, following the phase 5 of the Coupled Model Interc
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Bogenschutz, Peter A., Andrew Gettelman, Cecile Hannay, et al. "The path to CAM6: coupled simulations with CAM5.4 and CAM5.5." Geoscientific Model Development 11, no. 1 (2018): 235–55. http://dx.doi.org/10.5194/gmd-11-235-2018.

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Abstract. This paper documents coupled simulations of two developmental versions of the Community Atmosphere Model (CAM) towards CAM6. The configuration called CAM5.4 introduces new microphysics, aerosol, and ice nucleation changes, among others to CAM. The CAM5.5 configuration represents a more radical departure, as it uses an assumed probability density function (PDF)-based unified cloud parameterization to replace the turbulence, shallow convection, and warm cloud macrophysics in CAM. This assumed PDF method has been widely used in the last decade in atmosphere-only climate simulations but
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Nobre, Paulo, Marta Malagutti, Domingos F. Urbano, Roberto A. F. de Almeida, and Emanuel Giarolla. "Amazon Deforestation and Climate Change in a Coupled Model Simulation." Journal of Climate 22, no. 21 (2009): 5686–97. http://dx.doi.org/10.1175/2009jcli2757.1.

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Abstract The effects of Amazon deforestation on climate change are investigated using twin numerical experiments of an atmospheric general circulation model (AGCM) with prescribed global sea surface temperature and the same AGCM coupled to an ocean GCM (CGCM) over the global tropics. An ensemble approach is adopted, with 10-member ensemble averages of a control simulation compared with perturbed simulations for three scenarios of Amazon deforestation. The latest 20 yr of simulation from each experiment are analyzed. Local surface warming and rainfall reduction are simulated by both models over
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Varma, V., M. Prange, and M. Schulz. "Transient simulations of the present and the last interglacial climate using a coupled general circulation model: effects of orbital acceleration." Geoscientific Model Development Discussions 8, no. 7 (2015): 5619–41. http://dx.doi.org/10.5194/gmdd-8-5619-2015.

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Abstract. Numerical simulations provide a considerable aid in studying past climates. Out of the various approaches taken in designing numerical climate experiments, transient simulations have been found to be the most optimal when it comes to comparison with proxy data. However, multi-millennial or longer simulations using fully coupled general circulation models are computationally very expensive such that acceleration techniques are frequently applied. In this study, we compare the results from transient simulations of the present and the last interglacial with and without acceleration of t
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Varma, Vidya, Matthias Prange, and Michael Schulz. "Transient simulations of the present and the last interglacial climate using the Community Climate System Model version 3: effects of orbital acceleration." Geoscientific Model Development 9, no. 11 (2016): 3859–73. http://dx.doi.org/10.5194/gmd-9-3859-2016.

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Abstract. Numerical simulations provide a considerable aid in studying past climates. Out of the various approaches taken in designing numerical climate experiments, transient simulations have been found to be the most optimal when it comes to comparison with proxy data. However, multi-millennial or longer simulations using fully coupled general circulation models are computationally very expensive such that acceleration techniques are frequently applied. In this study, we compare the results from transient simulations of the present and the last interglacial with and without acceleration of t
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Xie, Zhiang, Dietmar Dommenget, Felicity S. McCormack, and Andrew N. Mackintosh. "GREB-ISM v1.0: A coupled ice sheet model for the Globally Resolved Energy Balance model for global simulations on timescales of 100 kyr." Geoscientific Model Development 15, no. 9 (2022): 3691–719. http://dx.doi.org/10.5194/gmd-15-3691-2022.

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Abstract. We introduce a newly developed global ice sheet model coupled to the Globally Resolved Energy Balance (GREB) climate model for the simulation of global ice sheet evolution on timescales of 100 kyr or longer (GREB-ISM v1.0). Ice sheets and ice shelves are simulated on a global grid, fully interacting with the climate simulation of surface temperature, precipitation, albedo, land–sea mask, topography and sea level. Thus, it is a fully coupled atmosphere, ocean, land and ice sheet model. We test the model in ice sheet stand-alone and fully coupled simulations. The ice sheet model dynami
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Cowling, S. A., Y. Shin, E. Pinto, and C. D. Jones. "Water recycling by Amazonian vegetation: coupled versus uncoupled vegetation–climate interactions." Philosophical Transactions of the Royal Society B: Biological Sciences 363, no. 1498 (2008): 1865–71. http://dx.doi.org/10.1098/rstb.2007.0035.

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To demonstrate the relationship between Amazonian vegetation and surface water dynamics, specifically, the recycling of water via evapotranspiration (ET), we compare two general circulation model experiments; one that couples the IS92a scenario of future CO 2 emissions to a land-surface scheme with dynamic vegetation (coupled) and the other to fixed vegetation (uncoupled). Because the only difference between simulations involves vegetation coupling, any alterations to surface energy and water balance must be due to vegetation feedbacks. The proportion of water recycled back to the atmosphere i
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Forster, Piers Mde F., and Karl E. Taylor. "Climate Forcings and Climate Sensitivities Diagnosed from Coupled Climate Model Integrations." Journal of Climate 19, no. 23 (2006): 6181–94. http://dx.doi.org/10.1175/jcli3974.1.

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Abstract A simple technique is proposed for calculating global mean climate forcing from transient integrations of coupled atmosphere–ocean general circulation models (AOGCMs). This “climate forcing” differs from the conventionally defined radiative forcing as it includes semidirect effects that account for certain short time scale responses in the troposphere. First, a climate feedback term is calculated from reported values of 2 × CO2 radiative forcing and surface temperature time series from 70-yr simulations by 20 AOGCMs. In these simulations carbon dioxide is increased by 1% yr−1. The der
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Dissertations / Theses on the topic "Coupled climate model simulations"

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Austin, J., L. L. Hood, and B. E. Soukharev. "Solar cycle variations of stratospheric ozone and temperature in simulations of a coupled chemistry-climate model." COPERNICUS, 2007. http://hdl.handle.net/10150/623329.

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The results from three 45-year simulations of a coupled chemistry climate model are analysed for solar cycle influences on ozone and temperature. The simulations include UV forcing at the top of the atmosphere, which includes a generic 27-day solar rotation effect as well as the observed monthly values of the solar fluxes. The results are analysed for the 27-day and 11-year cycles in temperature and ozone. In accordance with previous results, the 27-day cycle results are in good qualitative agreement with observations, particularly for ozone. However, the results show significant variations, t
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Stockdale, Timothy N. "Simulation and prediction of tropical SST with a coupled ocean-atmosphere model." Thesis, University of Oxford, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305416.

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Handiani, Dian Noor [Verfasser], André [Akademischer Betreuer] Paul, Michael [Akademischer Betreuer] Schulz, and Michal [Akademischer Betreuer] Kucera. "Tropical climate and vegetation cover during Heinrich event 1: Simulations with coupled climate vegetation models / Dian Noor Handiani. Gutachter: Michael Schulz ; Michal Kucera. Betreuer: André Paul." Bremen : Staats- und Universitätsbibliothek Bremen, 2012. http://d-nb.info/1072046652/34.

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Zhang, Xu [Verfasser], Gerrit [Akademischer Betreuer] Lohmann, and Peter [Akademischer Betreuer] Lemke. "Simulating the Last Glacial Maximum and abrupt glacial climate shifts in a coupled Earth System Model / Xu Zhang. Gutachter: Gerrit Lohmann ; Peter Lemke. Betreuer: Gerrit Lohmann." Bremen : Staats- und Universitätsbibliothek Bremen, 2014. http://d-nb.info/1072226073/34.

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Rosch, Jan, Thijs Heus, Marc Salzmann, Johannes Mülmenstädt, Linda Schlemmer, and Johannes Quaas. "Analysis of diagnostic climate model cloud parameterisations using large-eddy simulations: Analysis of diagnostic climate model cloud parameterisations usinglarge-eddy simulations." Journal of the Royal Meteorological Society (2015), 141, 691, Part B, S. 2199–2205, 2015. https://ul.qucosa.de/id/qucosa%3A14689.

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Current climate models often predict fractional cloud cover on the basis of a diagnostic probability density function (PDF) describing the subgrid-scale variability of the total water specific humidity, qt, favouring schemes with limited complexity. Standard shapes are uniform or triangular PDFs the width of which is assumed to scale with the gridbox mean qt or the grid-box mean saturation specific humidity, qs. In this study, the qt variability is analysed from large-eddy simulations for two stratocumulus, two shallow cumulus, and one deep convective cases. We find that in most cases, triangl
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Abiven, Claude. "Studies of climate variability in a simple coupled model." Thesis, Massachusetts Institute of Technology, 2007. http://hdl.handle.net/1721.1/40977.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2007.<br>Includes bibliographical references (p. 74-76).<br>The mechanisms of variability of a coupled atmosphere-ocean model are investigated through the study of two coupled configurations: an aquaplanet in which gyres are absent, and an aquaplanet in which a ridge extending from pole to pole supports gyres. Empirical Orthogonal Functions (EOFs) are used to explore the main features of variability exhibited by extended integrations of both configurations. In the aquaplanet a decadal var
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LEE, Han Soo. "Regional Disaster Events and Environment Simulations by Atmosphere-Ocean Coupled Model." 京都大学 (Kyoto University), 2007. http://hdl.handle.net/2433/49135.

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学位授与大学：京都大学 ; 取得学位: 博士(工学) ; 学位授与年月日: 2007-09-25 ; 学位の種類: 新制・課程博士 ; 学位記番号: 工博第2844号 ; 請求記号: 新制/工/1418 ; 整理番号: 25529<br>An atmosphere-ocean coupled model was developed based on a preexisting non-hydrostatic mesoscale atmosphere model (MM5) and non-hydrostatic ocean circulation model (MITgcm). This model together with a pre-established wind-wave-currents coupled model was applied to a number of regional environmental issue and disaster events to reproduce the present status and past situations and to help our understanding of the physical processes of such problems in terms of atmosphere-ocean i
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Wrzesien, Melissa Leigh. "Estimating North American montane snowpack with regional climate model simulations." The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu1522762079858684.

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Van, Aalderen Victor. "Modéliser l'évolution du climat global et de la calotte eurasienne pendant la dernière déglaciation." Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ029.

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La calotte marine de l'Antarctique de l'Ouest présente la particularité d'être en grande partie en contact avec l'océan. Les dernières observations révèlent une accélération de sa perte de masse sur les dernières décennies, essentiellement provoquée par l'augmentation de la fonte sous les plateformes de glace flottante. En revanche, son évolution future reste très incertaine, du fait de notre mauvaise compréhension des processus physiques mis en jeu entre la calotte et l'océan.La dernière déglaciation (-21 000 - -11 000 ans), constitue l'un des changements climatiques majeurs les plus récents
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Wiebe, Edward Carl. "Climate change and sub-grid-scale mixing in a coupled model." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0002/MQ36625.pdf.

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Books on the topic "Coupled climate model simulations"

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Kulkarni, Ashwini. Examining Indian monsoon variability in coupled climate model simulations and projections. Indian Institute of Tropical Meteorology, 2010.

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Kulkarni, Ashwini. Examining Indian monsoon variability in coupled climate model simulations and projections. Indian Institute of Tropical Meteorology, 2010.

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Nozawa, Tōru. Climate change simulations with a coupled ocean-atmosphere GCM called the model for interdisciplinary research on climate: MIROC. Center for Global Environmental Research, National Institute for Environmental Studies, 2007.

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Okazaki, Atsushi. Development of stable water isotope incorporated atmosphere-land coupled model and comparison with climate proxies. Division of Climate System Research, Atmosphere and Ocean Research Institute, The University of Tokyo, 2018.

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Ann-Maree, Hansen, ed. Climate change atlas: Greenhouse simulations from the Model Evaluation Consortium for Climate Assessment. Kluwer Academic Publishers, 1995.

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Hengeveld, Henry. Projections for Canada's climate future: A discussion of recent simulations with the Canadian global climate model. Environment Canada, 2000.

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M, Cox Peter, ed. Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Macmillan Journals, 2000.

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W, Zack John, Karyampudi V. Mohan, and United States. National Aeronautics and Space Administration., eds. Development of high resolution simulations of the atmospheric environment using the MASS model. MESO Inc., 1990.

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Nese, Jon M. Predictability of weather and climate in a coupled ocean-atmosphere model: A dynamical systems approach. Pennsylvania State University, Graduate School, Dept. of Meteorology, 1989.

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Fleming, Gordon H. Development of a large-scale coupled sea-ice model for interannual simulations of ice cover in the Arctic. Naval Postgraduate School, 1989.

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Book chapters on the topic "Coupled climate model simulations"

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Sharma, Kamal, and Peter Korn. "Numerical Simulation of an idealized coupled Ocean-Atmosphere Climate Model." In Lecture Notes in Computational Science and Engineering. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-45158-4_7.

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Song, Yi, Fredrick H. M. Semazzi, and Lian Xie. "Development of a Coupled Regional Climate Simulation Model for the Lake Victoria Basin." In Advances in Global Change Research. Springer Netherlands, 2002. http://dx.doi.org/10.1007/0-306-48201-0_5.

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Zhang, Zhenyu, Patrick Laux, Jussi Baade, Hassane Moutahir, and Harald Kunstmann. "Regional Land–Atmosphere Interactions in Southern Africa: Potential Impact and Sensitivity of Forest and Plantation Change." In Sustainability of Southern African Ecosystems under Global Change. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-10948-5_10.

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AbstractSouthern Africa is experiencing increasing land transformation and natural vegetation losses. Deforestation is one type of this land degradation where there are indigenous forests present, and afforestation of other nature ecosystems with timber plantations. This study performs regional coupled land–atmosphere model simulations using the Weather Research and Forecast (WRF) model with a resolution of 12 km, to assess the impact of forest and plantation cover change on regional climate in southern Africa. Three WRF simulations were designed for different land covers: (i) MODIS-derived la
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Bryan, Kirk. "Efficient Methods for Finding the Equilibrium Climate of Coupled Ocean-Atmosphere Models." In Physically-Based Modelling and Simulation of Climate and Climatic Change. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-3041-4_13.

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Capotondi, Antonietta. "El Niño–Southern Oscillation ocean dynamics: Simulation by coupled general circulation models." In Climate Dynamics: Why Does Climate Vary? American Geophysical Union, 2010. http://dx.doi.org/10.1029/2008gm000796.

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Hasselmann, K. "Some Problems in the Numerical Simulation of Climate Variability Using High-Resolution Coupled Models." In Physically-Based Modelling and Simulation of Climate and Climatic Change. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-3041-4_14.

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Duffy, Philip B., Eric Maloney, and Justin Sheffield. "Global Climate Model Simulations of North America." In Regional Climate Studies. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-03768-4_4.

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Tobias, S. M., and N. O. Weiss. "Resonance in a Coupled Solar-Climate Model." In Solar Variability and Climate. Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-010-0888-4_15.

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Schlesinger, Michael E. "Quantitative Analysis of Feedbacks in Climate Model Simulations." In Understanding Climate Change. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm052p0177.

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Lin, Charles A., Lei Wen, Diane Chaumont, and Michel Béland. "The Use of Coupled Meteorological and Hydrological Models for Flash Flood Simulation." In Climate and Hydrology in Mountain Areas. John Wiley & Sons, Ltd, 2006. http://dx.doi.org/10.1002/0470858249.ch15.

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Conference papers on the topic "Coupled climate model simulations"

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Nitcheva, Olga, Albena Vatralova, Donka Shopova, and Polya Dobreva. "INTEGRATED ANALYSIS OF SEAWATER INTRUSION DYNAMICS IN THE NORTHERN BLACK SEA COAST OF BULGARIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/3.2/s14.24.

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Managing water deficits in coastal areas presents significant challenges amid current climate fluctuations. This study examines the hydrological and water management factors contributing to seawater intrusion along the Bulgarian Black Sea coast. Utilizing data from field monitoring and hydrological model simulations, the research highlights the anthropogenic impacts shaped by the structure and dynamics of water supply. Findings reveal that rainfall levels in the Bulgarian Black Sea coastal region are below the national average. Coupled with excessive groundwater extraction for domestic purpose
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Hall, Garth D., Kenneth M. Lies, and Sarah K. Flock. "How Vapor Resistance Properties of Coatings Affect Exterior Wall Moisture Performance." In Paint and Coatings Expo (PACE) 2006. SSPC, 2006. https://doi.org/10.5006/s2006-00031.

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Abstract Vapor resistance properties of architectural coatings that are used on or within an exterior wall can directly influence the moisture performance of the assembly. Through the use of computer modeling, the effect that various coating applications have on common exterior wall assemblies are studied using varying indoor and outdoor climatic conditions. Such analysis is useful in the selection of appropriate coatings for both new and retrofit construction, and also in diagnosing performance problems in existing construction. Coatings are selected for use on or within building wall assembl
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Wen, H., and Q. Z. Zhang. "Kinetic simulations of low pressure miniaturized RF inductively coupled plasma: an implicit electromagnetic PIC/MCC Model." In 2024 IEEE International Conference on Plasma Science (ICOPS). IEEE, 2024. http://dx.doi.org/10.1109/icops58192.2024.10626861.

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Saetti, Umberto, Dan Wachspress, Joseph Horn, Kenneth Brentner, and Willca Villafana. "Rotorcraft Simulations with Coupled Flight Dynamics, Free Wake, and Acoustics." In Vertical Flight Society 72nd Annual Forum & Technology Display. The Vertical Flight Society, 2016. http://dx.doi.org/10.4050/f-0072-2016-11492.

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This study presents the integration of a flight simulation code (PSUHeloSim), a high fidelity rotor aeromechanics model with free wake (CHARM Rotor Module), and an industry standard noise prediction tool (PSU-WOPWOP) into a comprehensive noise prediction system. The flight simulation uses an autonomous controller to follow a prescribed trajectory for both steady and maneuvering flight conditions. The aeromechanical model calculates blade loads and blade motion that couple to the vehicle flight dynamics with suitable resolution to allow high fidelity acoustics analysis (including prediction of
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Zischler, Lucas, Ruby S. B. Ospina, Menno van den Hout, Chigo Okonkwo, and Darli A. A. Mello. "Analytical Model for the Information Rate of Coupled SDM Systems with MMSE Equalizers." In Optical Fiber Communication Conference. Optica Publishing Group, 2025. https://doi.org/10.1364/ofc.2025.m1h.4.

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We propose an analytical model for the information rates of MDG-impaired strongly-coupled SDM systems employing MMSE equalizers. The results are validated through simulations of long-distance links and experiments carried out in a 73-km 3-mode setup.
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Linton, Daniel, George Barakos, Ronny Widjaja, and Ben Thornber. "A New Actuator Surface Model with Improved Wake Model for CFD Simulations of Rotorcraft." In Vertical Flight Society 73rd Annual Forum & Technology Display. The Vertical Flight Society, 2017. http://dx.doi.org/10.4050/f-0073-2017-12010.

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Simulations of rotorcraft operating in unsteady flow-fields, manoeuvring flight, or with complex rotor configurations pose a significant challenge to current simulation methods. Simplified rotor models lack the generality required for the diverse range of operating conditions that a rotor may be exposed to, while higher-fidelity Navier-Stokes CFD simulations with fully-resolved rotors are expensive in terms of computational resources, simulation time, and preprocessing time. Here we present a new rotor and wake model which is fully-coupled to a CFD solver and is based on the actuator surface m
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Concina, Wendell, Suresh Sadineni, and Robert Boehm. "Solar Assisted Desiccant Cooling Simulation for Different Climate Zones." In ASME 2011 5th International Conference on Energy Sustainability. ASMEDC, 2011. http://dx.doi.org/10.1115/es2011-54296.

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Evaporative cooling is among the most cost effective methods of air conditioning, but is less efficient in humid climates. An evaporative system coupled with a desiccant wheel can operate effectively in broader climatic conditions. These cooling systems can substitute traditional vapor compression air conditioning systems as they involve environmentally friendly cooling processes with reduced electricity demand (which is commonly generated from fossil fuels) along with no harmful CFC based refrigerant usage. Furthermore, direct utilization of low grade energy sources such as solar thermal ener
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"Development of an Atmosphere-Ocean-Geosphere-Coupled Climate Model and its application to the Kanto plain, Japan." In 23rd International Congress on Modelling and Simulation (MODSIM2019). Modelling and Simulation Society of Australia and New Zealand, 2019. http://dx.doi.org/10.36334/modsim.2019.k9.vuillaume.

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Stefanakos, Christos N., and Erik Vanem. "Climatic Forecasting of Wind and Waves Using Fuzzy Inference Systems." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-61968.

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Wind and wave climatic simulations are of great interest in a number of different applications, including the design and operation of ships and offshore structures, marine energy generation, aquaculture and coastal installations. In a climate change perspective, projections of such simulations to a future climate are of great importance for risk management and adaptation purposes. This work investigates the applicability of FIS/ANFIS models for climatic simulations of wind and wave data. The models are coupled with a nonstationary time series modelling, which decomposes the initial time series
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Adam, Moritz, Heather J. Andres, and Kira Rehfeld. "The role of dynamic sea ice in a simplified general circulation model used for palaeoclimate studies." In VI ECCOMAS Young Investigators Conference. Editorial Universitat Politècnica de València, 2021. http://dx.doi.org/10.4995/yic2021.2021.12383.

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AbstractObservational records provide a strong basis for constraining sea ice models within a narrow range of climate conditions. Given current trends away from these conditions, models need to be tested over a wider range of climate states. The past provides many such examples based on paleoclimate data, including abrupt tipping points. However, the millennial-duration of typical paleoclimatesimulations necessitates balancing the inclusion and sophistication of model processes against computational cost. We investigate the impact on climate mean states and variability of introducing sea ice d
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Reports on the topic "Coupled climate model simulations"

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Sperber, K., P. Gleckler, C. Covey, et al. An Appraisal of Coupled Climate Model Simulations. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/15014011.

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Ronneberger, Kerstin, Maria Berrittella, Francesco Bosello, and Richard Tol. KLUM@GTAP: Spatially-Explicit, Biophysical Land Use in a Computable General Equilibrium Model. GTAP Working Paper, 2008. http://dx.doi.org/10.21642/gtap.wp50.

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*Chapter 12 of the forthcoming book "Economic Analysis of Land Use in Global Climate Change Policy," edited by Thomas W. Hertel, Steven Rose, and Richard S.J. Tol In this paper the global agricultural land use model KLUM is coupled to an extended version of the computable general equilibrium model (CGE) GTAP in order to consistently assess the integrated impacts of climate change on global cropland allocation and its implications for economic development. The methodology is innovative as it introduces dynamic economic land-use decisions based also on the biophysical aspects of land into a stat
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Jensen, M., K. Johnson, J. Mather, and D. Randall. Atmospheric Properties from the 2006 Niamey Deployment and Climate Simulation with a Geodesic Grid Coupled Climate Model. Office of Scientific and Technical Information (OSTI), 2008. http://dx.doi.org/10.2172/1021001.

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Mather, JH, DA Randall, and CJ Flynn. Atmospheric Properties from the 2006 Niamey Deployment and Climate Simulation with a Geodesic Grid Coupled Climate Model Fourth Quarter 2008. Office of Scientific and Technical Information (OSTI), 2008. http://dx.doi.org/10.2172/947993.

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JH Mather, DA Randall, and CJ Flynn. Atmospheric Properties from the 2006 Niamey Deployment and Climate Simulation with a Geodesic Grid Coupled Climate Model Third Quarter 2008. Office of Scientific and Technical Information (OSTI), 2008. http://dx.doi.org/10.2172/948018.

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JH Mather and D Randall. Atmospheric Properties from the 2006 Niamey Deployment and Climate Simulation with a Geodesic Grid Coupled Climate Model - First Quarter 2008. Office of Scientific and Technical Information (OSTI), 2007. http://dx.doi.org/10.2172/948094.

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Hasan, Abdulghani. Flood Modelling Tool : an integrated GIS and hydrological modelling tool for planning nature-based solutions in the urban environment. Faculty of Landscape Architecture, Horticulture and Crop Production Science, Swedish University of Agricultural Sciences, 2024. http://dx.doi.org/10.54612/a.5s9t2ca774.

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The risk of pluvial flooding is going to increase as climate change causes an increase in intense precipitation along with urbanisation leading to an increase in impermeable surfaces. In the last decade, cities such as Malmö and Copenhagen have already experienced severe pluvial flooding that has caused extensive damage. Adapting to climate change by creating flood resilient urban areas is therefore important and blue-green infrastructure (BGI) may be one measure to accomplish this. A hydrological model called TFM-DYN has been used to investigate whether BGI can aid the mitigation of pluvial f
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Ginis, Isaac, Deborah Crowley, Peter Stempel, and Amanda Babson. The impact of sea level rise during nor?easters in New England: Acadia National Park, Boston Harbor Islands, Boston National Historical Park, and Cape Cod National Seashore. National Park Service, 2024. http://dx.doi.org/10.36967/2304306.

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This study examines the potential impact of sea level rise (SLR) caused by climate change on the effects of extratropical cyclones, also known as nor?easters, in four New England coastal parks: Acadia National Park (ACAD), Boston Harbor Islands National Recreation Area (BOHA), Boston National Historical Park (BOST) and Cape Cod National Seashore (CACO). A multi-method approach is employed, including a literature review, observational data analysis, coupled hydrodynamic-wave numerical modeling, 3D visualizations, and communication of findings. The literature review examines previous studies of
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Ruosteenoja, Kimmo. Applicability of CMIP6 models for building climate projections for northern Europe. Finnish Meteorological Institute, 2021. http://dx.doi.org/10.35614/isbn.9789523361416.

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In this report, we have evaluated the performance of nearly 40 global climate models (GCMs) participating in Phase 6 of the Coupled Model Intercomparison Project (CMIP6). The focus is on the northern European area, but the ability to simulate southern European and global climate is discussed as well. Model evaluation was started with a technical control; completely unrealistic values in the GCM output files were identified by seeking the absolute minimum and maximum values. In this stage, one GCM was rejected totally, and furthermore individual output files from two other GCMs. In evaluating t
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Muri, Helene, and Anusha Sathyanadh. Report on carbon cycle interactions and efficacy of land-based CDRs (e.g. BECCS), when combined with oceanic CDRs (individually or in a portfolio). OceanNets, 2024. http://dx.doi.org/10.3289/oceannets_d4.8.

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In this deliverable 4.8, we analyze the Norwegian Earth System Model (NorESM) simulations from Deliverable 4.6 and 4.7 on land-based and ocean-based Carbon Dioxide Removal (CDR) scenarios. We focus the analysis on BioEnergy coupled to CCS (BECCS) using sugarcane as feedstock, and ocean alkalinity enhancement (OAE), applied individually and in combinations. We find that a higher amount of carbon captured by making use of the carbon sequestration potential of land and ocean together, as expected. The sugarcane yield is unaffected by the OAE deployment, however, carbon uptake by other parts of th
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