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A Description of the Advanced Research WRF Version 2
Open accessAbstract
The Technical Note series provides an outlet for a variety of NCAR manuscripts that contribute in specialized ways to the body of scientific knowledge but which are not suitable for journal, monograph, or book publication. Reports in this series are issued by the NCAR Scientific Di-visions; copies may be obtained on request from the Publications Office of NCAR. Designation symbols for the series include: EDD: Engineering, Design, or Development Reports Equipment descriptions, test results, instrumentation, and operating and maintenance manuals. IA: Instructional Aids Instruction manuals, bibliographies, film supplements, and other research or instructional aids. PPR: Program Progress Reports Field program reports, interim and working reports, survey reports, and plans for experiments. PROC: Proceedings Documentation of symposia, colloquia, conferences, workshops, and lectures. (Distribution may be limited to attendees.) STR: Scientific and Technical Reports Data compilations, theoretical and numerical investigations, and experimental results. The National Center for Atmospheric Research (NCAR) is operated by the University Corpora-tion for Atmospheric Research (UCAR) and is sponsored by the National Science Foundation. Any opinions, findings, conclusions, or recommendations expressed in this publication are those of the authors and do not necessarily reflect the views of the National Science Foundation.
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Plougonven, R., & Snyder, C. (2007) · doi:10.1175/jas3953.1 · Cited by 198
Rasmussen, R., Ikeda, K., Liu, C., Gochis, D., Clark, M., Dai, A., Gutmann, E., Dudhia, J., Chen, F., Barlage, M., et al. (2014) · Journal of Hydrometeorology · doi:10.1175/jhm-d-13-0118.1 · Cited by 194
“…high-resolution dynamical downscaling technique of Rasmussen et al. (2011) and Ikeda et al. (2010) using the Weather Research and Forecasting (WRF) (Skamarock et al. 2005) climate model at 6-km grid spacing or less is able to accurately estimate verticalmotions driven by topography and, as a…”
MethodSelf-citationTropical cyclogenesis sensitivity to environmental parameters in radiative–convective equilibrium
Nolan, D. S., Rappin, E., & Emanuel, K. A. (2007) · doi:10.1002/qj.170 · Cited by 192
“WRF is a fully compressible model of the atmosphere designed for mesoscale and convective-scale simulations of real-case and idealized weather phenomena (Skamarock et al., 2005).”
BackgroundCurrent and future levels of mercury atmospheric pollution on a global scale
Pacyna, J., Travnikov, O., Simone, F. D., Hedgecock, I., Sundseth, K., Pacyna, E., Steenhuisen, F., Pirrone, N., Munthe, J., & Kindbom, K. (2016) · doi:10.5194/acp-16-12495-2016 · Cited by 190
“The atmospheric transport of tracers is driven by meteorological fields generated by the Weather Research and Forecasting (WRF) modelling system (Skamarock et al., 2007) and fed by the operational analysis data from ECMWF (ECMWF, 2016).”
MethodGbobaniyi, E., Sarr, A., Sylla, M., Diallo, I., Lennard, C., Dosio, A., Dhiédiou, A., Kamga, A., Klutse, N., Hewitson, B., et al. (2014) · doi:10.1002/joc.3834 · Cited by 190
Lin, Y.-L., & Colle, B. (2011) · doi:10.1175/2010mwr3293.1 · Cited by 189
Nazemi, A., & Wheater, H. S. (2015) · Hydrology and earth system sciences · doi:10.5194/hess-19-33-2015 · Cited by 210
The Beijing extreme rainfall of 21 July 2012: “Right results” but for wrong reasons
Zhang, D.-L., Lin, Y., Zhao, P., Yu, X.-D., Wang, S., Kang, H., & Ding, Y.-H. (2013) · doi:10.1002/grl.50304 · Cited by 187
Trier, S., Davis, C., Ahijevych, D., Weisman, M., & Bryan, G. (2006) · doi:10.1175/jas3768.1 · Cited by 185
Climate projections for ecologists
Harris, R. M. B., Grose, M., Lee, G., Bindoff, N. L., Porfirio, L. L., & Fox‐Hughes, P. (2014) · Wiley Interdisciplinary Reviews Climate Change · doi:10.1002/wcc.291 · Cited by 177
Time-adaptive quantile-copula for wind power probabilistic forecasting
Bessa, R., Miranda, V., Botterud, A., Zhou, Z., & Wang, J.-H. (2012) · doi:10.1016/j.renene.2011.08.015 · Cited by 184
“The NWP data was generated by the WRF model [34] at Argonne National Laboratory for one reference point located in the wind farm at 6 AM every day.”
MethodMcFarquhar, G., Bretherton, C., Marchand, R., Protat, A., DeMott, P., Alexander, S., Roberts, G., Twohy, C., Toohey, D., Siems, S., et al. (2020) · Bulletin of The American Meteorological Society - (BAMS) · doi:10.1175/bams-d-20-0132.1 · Cited by 183
Banks, R., Tiana-Alsina, J., Baldasano, J., Rocadenbosch, F., Papayannis, A., Solomos, S., & Tzanis, C. (2016) · doi:10.1016/j.atmosres.2016.02.024 · Cited by 183
“1 with the Advanced Research WRF (ARW) dynamical solver (Skamarock et al., 2005).”
MethodInfluentialPathirana, A., Denekew, H. B., Veerbeek, W., Zevenbergen, C., & Banda, A. T. (2013) · Atmospheric Research · doi:10.1016/j.atmosres.2013.10.005 · Cited by 192
“This model is further explained in Skamarock et al. (2007).”
MethodGustafson, W. I., Chapman, E. G., Ghan, S. J., Easter, R. C., & Fast, J. D. (2007) · Geophysical Research Letters · doi:10.1029/2007gl030021 · Cited by 178
Coniglio, M., Correia, J., Marsh, P. T., & Kong, F. (2013) · doi:10.1175/waf-d-12-00103.1 · Cited by 180
Kesarkar, A., Dalvi, M., Kaginalkar, A., & Ojha, A. (2007) · doi:10.1016/j.atmosenv.2006.10.042 · Cited by 178
Wang, Y., Long, C., Leung, L., Dudhia, J., McFarlane, S., Mather, J., Ghan, S., & Liu, X. (2009) · doi:10.1029/2009jd012729 · Cited by 176
“…Research Forecasting (WRF, version 3) model, developed at the National Center for Atmospheric Research (NCAR) [Michalakes et al., 2001, 2005; Skamarock et al., 2005; Skamarock and Klemp, 2008], with support from multiple partners (the National Centers for Environmental Prediction (NCEP) and…”
BackgroundMethodInfluentialSelf-citationMeng, Z., & Zhang, F. (2008) · Monthly Weather Review · doi:10.1175/2007mwr2106.1 · Cited by 172
“WRF is a fully compressible, nonhydrostatic mesoscale model ( Skamarock et al. 2005 ).”
BackgroundZhang, F., Weng, Y., Gamache, J. F., & Marks, F. D. (2011) · Geophysical Research Letters · doi:10.1029/2011gl048469 · Cited by 192
“mesoscale and regional scale weather predictions [Skamarock et al., 2005], and an ensemble Kalman filter (EnKF) which uses ensemble forecasts to estimate flow‐dependent background error covariance or other probabilistic aspects of the background forecast [Evensen, 1994].”
MethodInfluentialAssessment of wave energy resources in Hawaii
Stopa, J., Cheung, K.-F., & Chen, Y.-L. (2011) · doi:10.1016/j.renene.2010.07.014 · Cited by 174
Reliability of ERA5 Reanalysis Data for Wind Resource Assessment: A Comparison against Tall Towers
Gualtieri, G. (2021) · Energies · doi:10.3390/en14144169 · Cited by 189
Yair, Y., Lynn, B., Price, C., Kotroni, V., Lagouvardos, K., Morin, E., Mugnai, A., & Llasat, M. D. C. (2010) · doi:10.1029/2008jd010868 · Cited by 172
Chen, S., Huang, J., Zhao, C., Qian, Y., Leung, L.-Y. R., & Yang, B. (2013) · Journal of Geophysical Research Atmospheres · doi:10.1002/jgrd.50122 · Cited by 192
Proposal of a regressive model for the hourly diffuse solar radiation under all sky conditions
Ruiz-Arias, J., Alsamamra, H., Tovar-Pescador, J., & Pozo-Vázquez, D. (2010) · doi:10.1016/j.enconman.2009.11.024 · Cited by 168
Lauvaux, T., Schuh, A. E., Uliasz, M., Richardson, S., Miles, N. L., Andrews, A. E., Sweeney, C., Diaz, L. I., Martins, D. K., Shepson, P. B., et al. (2012) · Atmospheric chemistry and physics · doi:10.5194/acp-12-337-2012 · Cited by 157
An advanced stochastic weather generator for simulating 2‐D high‐resolution climate variables
Peleg, N., Fatichi, S., Paschalis, A., Molnár, P., & Burlando, P. (2017) · Journal of Advances in Modeling Earth Systems · doi:10.1002/2016ms000854 · Cited by 178
Kim, S.-W., Heckel, A., Frost, G., Richter, A., Gleason, J., Burrows, J., Mckeen, S., Hsie, E., Granier, C., & Trainer, M. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2008jd011343 · Cited by 163
Impacts of land cover data quality on regional climate simulations
Sertel, E., Robock, A., & Ormeci, C. (2010) · doi:10.1002/joc.2036 · Cited by 162
THE MIDLATITUDE CONTINENTAL CONVECTIVE CLOUDS EXPERIMENT (MC3E).
Jensen, M. P., Petersen, W., Bansemer, A., Bharadwaj, N., Carey, L., Cecil, D. J., Collis, S., Genio, A. D., Dolan, B., Gerlach, J., et al. (2016) · Bulletin of The American Meteorological Society - (BAMS) · doi:10.1175/bams-d-14-00228.1 · Cited by 161
Kawase, H., Takao, Y., Hara, M., Kimura, F., Yasunari, T., Ailikun, B., Ueda, H., & Inoue, T. (2009) · doi:10.1029/2009jd011803 · Cited by 161
“We used the Advanced Research of Weather Research and Forecasting (WRF) model version 2.2 [Skamarock et al., 2005].”
MethodInfluentialFiori, E., Comellas, A., Molini, L., Rebora, N., Siccardi, F., Gochis, D., Tanelli, S., & Parodi, A. (2014) · Atmospheric Research · doi:10.1016/j.atmosres.2013.10.007 · Cited by 160
Large-Eddy Simulation of an Idealized Tropical Cyclone
Rotunno, R., Chen, Y., Wang, W., Davis, C., Dudhia, J., & Holland, G. (2009) · doi:10.1175/2009bams2884.1 · Cited by 159
Self-citationLiu, C., Xiao, Q., & Wang, B. (2008) · Monthly Weather Review · doi:10.1175/2008mwr2699.1 · Cited by 148
“Using such techniques, ensemble-based data assimilation algorithms have proven useful in either global atmospheric data assimilation (Mitchell et al. 2002; Houtekamer and Mitchell 2005; Buehner 2005) or regional mesoscale atmospheric data assimilation (Snyder and Zhang 2003; Xue et al. 2006).”
MethodResultCreating the Dataset for the Western Wind and Solar Integration Study (U.S.A.)
Potter, C., Lew, D., McCaa, J., Cheng, S., Eichelberger, S., & Grimit, E. (2008) · doi:10.1260/0309-524x.32.4.325 · Cited by 158
“2 Model Configuration The Weather Research and Forecasting (WRF) model [12] is generally considered to be the most advanced mesoscale model in North America and has superseded the previous industry standard, the MM5 model [13].”
Osuri, K., Mohanty, U. C., Routray, A., Kulkarni, M., & Mohapatra, M. (2012) · Natural Hazards · doi:10.1007/s11069-011-9862-0 · Cited by 157
“The drag formulation follows Charnock (1955), the surface exchange coefficient for water vapor follows Carlson and Boland (1978), and the heat flux uses a similarity relationship (Skamarock et al. 2005).”
BackgroundKhain, A., Lynn, B., & Dudhia, J. (2010) · doi:10.1175/2009jas3210.1 · Cited by 156
“a. Spectral bin microphysics scheme The SBM scheme implemented into the WRF (version 3; Skamarock et al. 2005) has been described by Khain et al. (2004) and Lynn and Khain (2007).”
MethodSelf-citationDevelopment and testing of Polar Weather Research and Forecasting model: 2. Arctic Ocean
Bromwich, D., Hines, K., & Bai, L. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2008jd010300 · Cited by 156
“Over open ocean, WRF does not invoke the LSM, and surface fluxes are calculated by the surface layer component of the boundary layer parameterization [Skamarock et al., 2005].”
MethodInfluentialImpacts of Climate Change on Rainfall Extremes and Urban Drainage Systems
Williems, P., Olsson, J., Arnbjerg-Nielsen, K., Beecham, S., Pathirana, A., Gregersen, I. B., Madsen, H., & Nguyen, V. (2012) · doi:10.2166/9781780401263 · Cited by 153
Fierro, A., Rogers, R., Marks, F. D., & Nolan, D. (2009) · doi:10.1175/2009mwr2946.1 · Cited by 153
“The model used for this study was the WRF-ARW dynamical core (version 2.2; Skamarock et al. 2005).”
MethodInfluentialToward a climate downscaling for the Eastern Mediterranean at high-resolution
Hahmann, A., Rostkier-Edelstein, D., Warner, T., Liu, Y.-W., Vandenberghe, F., & Swerdlin, S. (2008) · doi:10.5194/adgeo-12-159-2008 · Cited by 153
“…(hahmann@ucar.edu) We use the PSU/NCAR mesoscale model, version 5 (MM5, Grell et al., 1995), and the community Weather Research and Forecast model (ARW-WRF, Skamarock et al., 2005) to dynamically downscale the climate of the eastern Mediterranean and the adjacent countries of the Middle East.”
Kort, E., Eluszkiewicz, J., Stephens, B., Miller, J. B., Gerbig, C., Nehrkorn, T., Daube, B., Kaplan, J., Houweling, S., & Wofsy, S. (2008) · doi:10.1029/2008gl034031 · Cited by 152
“3.1. Meteorological Input and Footprint Estimation [7] We drove STILT with meteorological fields from the Weather Research and Forecasting (WRF) model [ Skamarock et al., 2005 ].”
MethodInfluentialHara, M., Takao, Y., Kawase, H., & Kimura, F. (2008) · doi:10.3178/hrl.2.61 · Cited by 152
“2 (Skamarock et al., 2005).”
Llasat, M., Marcos, R., Turco, M., Gilabert, J., & Llasat-Botija, M. (2016) · Journal of Hydrology · doi:10.1016/j.jhydrol.2016.05.040 · Cited by 151
“…models such as AROME (Applications of Research to Operations at Mesoscale model, Seity et al., 2011), WRF (Weather Research and Forecasting model, Skamarock et al., 2005) and MESO-NH (Non-Hydrostatic Mesoscale atmospheric model, Lafore et al., 1998), or using a combination of rain gauges and…”
MethodPractical and Intrinsic Predictability of Severe and Convective Weather at the Mesoscales
Melhauser, C., & Zhang, F.-Q. (2012) · doi:10.1175/jas-d-11-0315.1 · Cited by 151
“The effect ofmoist convection on themesoscale predictability was further generalized to the idealized moist baroclinic waves in Tan et al. (2004) and Zhang et al. (2007).”
BackgroundChawla, I., Osuri, K., Mujumdar, P., & Niyogi, D. (2018) · doi:10.5194/hess-22-1095-2018 · Cited by 150
“The model description and updates can be found from Skamarock et al. (2005) and the WRF user web page (http://www2. mmm.ucar.edu/wrf/users/).”
BackgroundMethodInfluentialThe Impact of Future Climate Change on TC Intensity and Structure: A Downscaling Approach
Hill, K. A., & Lackmann, G. (2011) · doi:10.1175/2011jcli3761.1 · Cited by 150
Cui, Y. Y., & de Foy, B. (2012) · Journal of Applied Meteorology and Climatology · doi:10.1175/jamc-d-11-0104.1 · Cited by 147
The Role of Entrainment in the Diurnal Cycle of Continental Convection
Genio, A. D., & Wu, J. (2010) · Journal of Climate · doi:10.1175/2009jcli3340.1 · Cited by 148
Comparison of WRF Model-Simulated and MODIS-Derived Cloud Data
Otkin, J., & Greenwald, T. (2008) · Monthly Weather Review · doi:10.1175/2007mwr2293.1 · Cited by 148
Response of fine particulate matter concentrations to changes of emissions and temperature in Europe
Megaritis, A., Fountoukis, C., Charalampidis, P., Pilinis, C., & Pandis, S. (2012) · Atmospheric chemistry and physics · doi:10.5194/acp-13-3423-2013 · Cited by 147
Clark, A., Gallus, W., & Weisman, M. (2010) · doi:10.1175/2010waf2222404.1 · Cited by 147
Effects of aerosols on precipitation from orographic clouds
Lynn, B. H., Khain, A. P., Rosenfeld, D., & Woodley, W. L. (2007) · Journal of Geophysical Research Atmospheres · doi:10.1029/2006jd007537 · Cited by 143
“Here, the full SBM scheme has been coupled to WRF [ Skamarock et al., 2005 ] using the same approach for embedding the microphysics within the model dynamic time step as in Lynn et al. [2005a, 2005b].”
MethodPatricola, C. M., & Cook, K. H. (2009) · Climate Dynamics · doi:10.1007/s00382-009-0623-7 · Cited by 143
“The regional model used for all simulations is the Weather Research and Forecasting Model (WRF; Skamarock et al. 2005 ) version 2.2.”
MethodInfluentialLiao, Z., Hong, Y., Wang, J., Fukuoka, H., Sassa, K., Karnawati, D., & Fathani, F. (2010) · doi:10.1007/s10346-010-0219-7 · Cited by 146
“On the other hand, the WRF model version 3.0.1 used in this study includes the Advanced Research WRF dynamical core (WRF- ARW; Michalakes et al. 2001; Skamarock et al. 2005), which is a non-hydrostatic, fully compressible, primitive equation model.”
MethodInfluentialFalasca, S., Ciancio, V., Salata, F., Golasi, I., Rosso, F., & Curci, G. (2019) · Building and Environment · doi:10.1016/j.buildenv.2019.106242 · Cited by 147
A Review of Progress and Applications of Pulsed Doppler Wind LiDARs
Liu, Z.-L., Barlow, J., Chan, P., Fung, J., Li, Y.-G., Ren, C., Mak, H. W. L., & Ng, E. (2019) · Remote Sensing · doi:10.3390/rs11212522 · Cited by 145
Effect of increased renewables generation on operation of thermal power plants
Eser, P., Singh, A., Chokani, N., & Abhari, R. (2016) · doi:10.1016/j.apenergy.2015.12.017 · Cited by 145
Hurricane Sandy before 1900 and after 2100
Lackmann, G. M. (2014) · Bulletin of the American Meteorological Society · doi:10.1175/bams-d-14-00123.1 · Cited by 176
“A set of numerical model simulations was produced using the Weather Research and Fore-casting (WRF) Model (Skamarock et al. 2007); WRF has proven capable in the analysis and prediction of tropical cyclones (e.g., Davis et al. 2008; Munsell and Zhang 2014; Bassill 2014, 2015).”
MethodMeng, Z., & Zhang, F. (2008) · Monthly Weather Review · doi:10.1175/2008mwr2270.1 · Cited by 119
Mesoscale Processes Contributing to Extreme Rainfall in a Midlatitude Warm-Season Flash Flood*
Schumacher, R., & Johnson, R. H. (2008) · doi:10.1175/2008mwr2471.1 · Cited by 145
Development and Testing of Polar WRF. Part III: Arctic Land*
Hines, K., Bromwich, D., Bai, L., Barlage, M., & Slater, A. (2011) · Journal of Climate · doi:10.1175/2010jcli3460.1 · Cited by 145
“The land surface model (LSM) is the four-layer unified Noah 3.0 scheme (Ek et al. 2003; Skamarock et al. 2005; Chen et al. 2007; Slater et al. 2007), with the polar updates from Hines and Bromwich (2008).”
BackgroundMethodResultInfluentialUrbanization, climate change and flood policy in the United States
Ntelekos, A. A., Oppenheimer, M., Smith, J. A., & Miller, A. J. (2010) · Climatic Change · doi:10.1007/s10584-009-9789-6 · Cited by 144
Weng, Y., & Zhang, F. (2011) · Monthly Weather Review · doi:10.1175/2011mwr3602.1 · Cited by 163
“The advantage of the EnKF over variational data assimilation methods is its ability to estimate model forecast uncertainties and its ability to assimilate observations from convective to regional scales (e.g., Snyder and Zhang 2003; Dowell et al. 2004; Zhang and Snyder 2007).”
BackgroundSatellite cloud and precipitation assimilation at operational NWP centres
Bauer, P., Auligne, T., Bell, W., Geer, A., Guidard, V., Heilliette, S., Kazumori, M., Kim, M.-J., Liu, E., McNally, A. P., et al. (2011) · doi:10.1002/qj.905 · Cited by 144
“Assimilation of 3D radar reflectivity and lightning data (Weygandt et al., 2008) is performed by specification of estimated 3D latent heating within a digital filter initialization (DFI) already applied for 1 h cycling within both the RUC model and more recently, the ARW-WRF model.”
MethodInfluentialSmith, B. L., Yuter, S., Neiman, P., & Kingsmill, D. (2010) · doi:10.1175/2009mwr2939.1 · Cited by 144
“We employ the Weather Research and Forecasting (WRF) model version 2.2 (Skamarock et al. 2005) to obtain high-resolution information on water vapor and its transport both over the ocean and land.”
MethodInfluentialFog Prediction from a Multimodel Mesoscale Ensemble Prediction System
Zhou, B., & Du, J. (2009) · Weather and Forecasting · doi:10.1175/2009waf2222289.1 · Cited by 158
“…Nonhydrostatic Mesoscale Model (NMM; Janjić et al. 2001) component of the National Centers for Environmental Prediction’s (NCEP) Weather Research and Forecasting (WRF) model and the National Center for Atmospheric Research’s (NCAR) Advanced Research version of the WRF (ARW; Skamarock et al. 2005).”
MethodSobash, R., Kain, J., Bright, D., Dean, A., Coniglio, M., & Weiss, S. (2011) · Weather and Forecasting · doi:10.1175/waf-d-10-05046.1 · Cited by 141
“For the period examined in this study, the modeling system used version 2.2 of the Advanced Research WRF (ARW) dynamic core (Skamarock et al. 2005) to produce daily 36-h forecasts, initialized at 0000 UTC, over the eastern three-fourths of the conterminous United States (CONUS; see Fig.”
MethodInfluentialQian, Y., Gustafson, W., Leung, L. R., & Ghan, S. (2009) · doi:10.1029/2008jd011039 · Cited by 141
“[30] The regional climate model used in this study is based on the Weather Research and Forecasting (WRF) model [Skamarock et al., 2005], with modifications described by Leung et al. [2005], which includes the use of a wider D03108 QIAN ET AL.”
MethodMiglietta, M., Moscatello, A., Conte, D., Mannarini, G., Lacorata, G., & Rotunno, R. (2011) · doi:10.1016/j.atmosres.2011.04.006 · Cited by 140
“The model used in this study is the Weather Research and Forecasting (WRF) Model, version 2.2 (Skamarock et al. 2005; Michalakes et al. 2004; see also www.wrf-model.org).”
MethodInfluentialMukhopadhyay, P., Taraphdar, S., Goswami, B., & Krishnakumar, K. (2010) · doi:10.1175/2009waf2222320.1 · Cited by 140
“a. Model The nonhydrostatic, fully compressible, terrain-following sigma coordinate mesoscale model Weather Research Forecast (WRF), version 2.2 (Skamarock et al. 2005), developed by NCAR, was used in the present study.”
MethodInfluentialMid-Twenty-First-Century Changes in Extreme Events over Northern and Tropical Africa
Vizy, E. K., & Cook, K. H. (2012) · Journal of Climate · doi:10.1175/jcli-d-11-00693.1 · Cited by 130
“The National Center for Atmospheric Research– National Oceanic and Atmospheric Administration (NCAR–NOAA) Weather Research and Forecasting (WRF) (Skamarock et al. 2005) regional model V3.”
BackgroundLin, C.-Y., Chen, W.-C., Chang, P., & Sheng, Y.-F. (2011) · doi:10.1175/2010jamc2504.1 · Cited by 139
Saiz-Lopez, A., Sitkiewicz, S. P., Roca-Sanjuán, D., Oliva-Enrich, J. M., Davalos, J., Notario, R., Jiskra, M., Xu, Y., Wang, F.-Y., Thackray, C., et al. (2018) · Nature Communications · doi:10.1038/s41467-018-07075-3 · Cited by 138
de Lima, F. J. L., Martins, F. R., Pereira, Ê. B., Lorenz, E., & Heinemann, D. (2015) · Renewable Energy · doi:10.1016/j.renene.2015.11.005 · Cited by 164
Fan, J.-W., Leung, L., DeMott, P., Comstock, J., Singh, B., Rosenfeld, D., Tomlinson, J., White, A., Prather, K., Minnis, P., et al. (2013) · doi:10.5194/acp-14-81-2014 · Cited by 138
“model (SBM) (Khain et al., 2004; Khain and Lynn, 2009; Fan et al., 2012a) coupled with the Weather Research and Forecasting (WRF) model (Skamarock et al., 2005).”
MethodGreen Roof Mitigation Potential for a Proxy Future Climate Scenario in Chicago, Illinois
Smith, K., & Roebber, P. (2011) · doi:10.1175/2010jamc2337.1 · Cited by 138
Temporal variations of elemental carbon in Beijing
Han, S., Kondo, Y., Oshima, N., Takegawa, N., Miyazaki, Y., Hu, M., Lin, P., Deng, Z., Zhao, Y., Sugimoto, N., et al. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2009jd012027 · Cited by 140
Very extreme seasonal precipitation in the NARCCAP ensemble: model performance and projections
Wehner, M. F. (2013) · Climate Dynamics · doi:10.1007/s00382-012-1393-1 · Cited by 137
“Two versions of the Weather Research Forecasting model were contributed to the NARCCAP project (Skamarock et al. 2005) One of these, referred to as WRFG, was forced by output from the Community Climate System Model version 3.0 (ccsm) and the Coupled Global Climate Model Version 3 (cgcm3) in…”
MethodInfluentialKuffour, B. N. O., Engdahl, N. B., Woodward, C. S., Condon, L. E., Kollet, S. J., & Maxwell, R. M. (2020) · Geoscientific model development · doi:10.5194/gmd-13-1373-2020 · Cited by 160
“WRF is a widely used model that provides a common framework for idealized dynamical studies, full-physics numerical weather prediction, air-quality simulations, and regional climate simulations (Michalakes et al., 1999, 2001; Skamarock et al., 2005).”
MethodTsumune, D., Tsubono, T., Aoyama, M., Uematsu, M., Misumi, K., Maeda, Y., Yoshida, Y., & Hayami, H. (2013) · doi:10.5194/bg-10-5601-2013 · Cited by 137
“2.1 (WRF; Skamarock et al., 2008).”
BackgroundInfluentialJiménez, P., González-Rouco, J. F., García-Bustamante, E., Navarro, J., Montávez, J., de Arellano, J. V., Dudhia, J., & Muñoz-Roldan, A. (2010) · doi:10.1175/2009jamc2175.1 · Cited by 137
“The mesoscale model used is the WRF modeling system (version 2.1.2; Skamarock et al. 2005).”
MethodInfluentialSelf-citationOshima, N., Kondo, Y., Moteki, N., Takegawa, N., Koike, M., Kita, K., Matsui, H., Kajino, M., Nakamura, H., Jung, J., et al. (2011) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jd016552 · Cited by 152
“[14] We used the 3-D Weather Research and Forecasting (WRF) model [Skamarock et al., 2005] to estimate precipitation and PBL height.”
MethodTime Evolution of the Surface Urban Heat Island
Stewart, I. D., Krayenhoff, E. S., Voogt, J., Lachapelle, J., Allen, M., & Broadbent, A. (2021) · Earth's Future · doi:10.1029/2021ef002178 · Cited by 135
How building energy models take the local climate into account in an urban context – A review
Lauzet, N., Rodler, A., Musy, M., Azam, M.-H., Guernouti, S., Mauree, D., & Colinart, T. (2019) · doi:10.1016/j.rser.2019.109390 · Cited by 135
Ruiz, J., Saulo, C., & Nogués-Paegle, J. (2010) · doi:10.1175/2010mwr3358.1 · Cited by 135
“a. Model experiments All runs are conducted with the Advanced Research WRF (ARW-WRF) version 2.0 (Skamarock et al. 2005).”
MethodInfluentialJiang, X.-Y., Niu, G., & Yang, Z.-L. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2008jd010756 · Cited by 135
“[7] A nonhydrostatic, fully compressible model, the Weather Research and Forecasting (WRF) model, is used as an investigative tool in this study [Skamarock et al., 2005].”
BackgroundMethodResultInfluentialSeasonal dependence of the urban heat island on the street canyon aspect ratio
Theeuwes, N., Steeneveld, G., Ronda, R., Heusinkveld, B., Hove, L. V., & Holtslag, A. (2014) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.2289 · Cited by 134
Ukhov, A., Mostamandi, S., da Silva, A. M., Flemming, J., Alshehri, Y., Shevchenko, I., & Stenchikov, G. (2020) · Atmospheric Chemistry and Physics · doi:10.5194/acp-2020-17 · Cited by 133
“To calculate fine-resolution PM and sulfate fields, we use the Weather Research and Forecasting (WRF) model (Skamarock et al., 2005) coupled with chemistry (WRFChem v3.”
MethodMungall, E., Abbatt, J., Wentzell, J., Lee, A. K. Y., Thomas, J. L., Blais, M., Gosselin, M., Miller, L., Papakyriakou, T., Willis, M., et al. (2017) · Proceedings of the National Academy of Sciences of the United States of America · doi:10.1073/pnas.1620571114 · Cited by 133
“Geosci Model Dev 6:1889–1904.”
MethodGrowth of nucleation mode particles in the summertime Arctic: a case study
Willis, M. D., Burkart, J., Thomas, J. L., Köllner, F., Schneider, J., Bozem, H., Hoor, P. M., Aliabadi, A. A., Schulz, H., Herber, A., et al. (2016) · Atmospheric chemistry and physics · doi:10.5194/acp-16-7663-2016 · Cited by 148
“limited area meteorological forecast from WRF (Skamarock et al., 2001), with the specific WRF”
Explicit Numerical Diffusion in the WRF Model
Knievel, J., Bryan, G., & Hacker, J. (2007) · doi:10.1175/2007mwr2100.1 · Cited by 133
“An appropriate way to avoid the sensitivity described by Xu et al. (2001) is to choose a grid interval that adequately resolves the”
BackgroundImpacts of warming on phytoplankton abundance and phenology in a typical tropical marine ecosystem
Gittings, J. A., Raitsos, D. Ε., Krokos, G., & Hoteit, I. (2018) · Scientific Reports · doi:10.1038/s41598-018-20560-5 · Cited by 157
Urban meteorological modeling using WRF: a sensitivity study
Sharma, A., Fernando, H., Hamlet, A., Hellmann, J., Barlage, M., & Chen, F. (2017) · International Journal of Climatology · doi:10.1002/joc.4819 · Cited by 132
“6 (Skamarock et al., 2005), which is a non-hydrostatic, compressible model.”
BackgroundMethodInfluentialAhmadov, R., Gerbig, C., Kretschmer, R., Koerner, S., Neininger, B., Dolman, A., & Sarrat, C. (2007) · Journal of Geophysical Research Atmospheres · doi:10.1029/2007jd008552 · Cited by 132
“2 version) [Skamarock et al., 2005] to simulate transport of CO2 tracer in on-line mode.”
MethodInfluentialAtmospheric Inverse Estimates of Methane Emissions from Central California
Zhao, C., Andrews, A., Bianco, L., Eluszkiewicz, J., Hirsch, A., Macdonald, C., Nehrkorn, T., & Fischer, M. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2008jd011671 · Cited by 131
“180 We calculate the footprints relating surface fluxes to measured CH4 mixing ratios using the meteorological output from a customized version of the Weather Research and Forecasting model [Skamarock et al., 2005] to drive STILT.”
MethodRegional modeling of dust mass balance and radiative forcing over East Asia using WRF-Chem
Chen, S.-Y., Zhao, C., Qian, Y., Leung, L. R., Huang, J.-P., Huang, Z., Bi, J.-R., Zhang, W., Shi, J.-S., Yang, L., et al. (2014) · doi:10.1016/j.aeolia.2014.02.001 · Cited by 130
Chen, F., Miao, S., Tewari, M., Bao, J., & Kusaka, H. (2011) · doi:10.1029/2010jd015533 · Cited by 130
Dudhia, J., Hong, S.-Y., & Lim, K. (2008) · doi:10.2151/jmsj.86a.33 · Cited by 130
Self-citation
Metadata
- Authors
- Skamarock, W., Klemp, J., Dudhia, J., Gill, D., Barker, D., & Wang, W.
- Venue
- NSF National Center for Atmospheric Research
- Publisher
- NSF National Center for Atmospheric Research
- Published
- 2005
- OpenAlex
- W2152984210
- Cited by
- 2,504
- References
- 0
- Citations by year
- 2026: 9 · 2025: 32 · 2024: 61 · 2023: 76 · 2022: 105 · 2021: 154 · 2020: 129 · 2019: 160 · 2018: 155 · 2017: 118 · 2016: 143 · 2015: 127 · 2014: 123 · 2013: 159 · 2012: 154
- Type
- report
- Language
- en
- Open access
- green
- doi.org
- Locations
- Defense Technical Information Center (DTIC) (submittedVersion)
- UCAR/NCAR
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Physical Sciences › Engineering › Computational Mechanics › Computational Fluid Dynamics and Aerodynamics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- numerical weather prediction, regional climate modeling, WRF model, model description
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